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Brought to you by NOAA NMFS SWFSC ERD |
| griddap | Subset | tabledap | Make A Graph | wms | files | Title | Summary | FGDC | ISO 19115 | Info | Background Info | RSS | Institution | Dataset ID | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_drogued_drifter_velocity | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_drogued_drifter_velocity.graph | Profile - R4.x265.000.0038 - drogued_drifter_velocity - 29.16N, 89.64W - 2017-04-17 | As part of CARTHE 's SPLASH (Submesoscale Processes and Lagrangian Analysis on the SHelf) experiment, current observations were obtained from a variety of instruments in the Louisiana Bight, northern Gulf of Mexico. On 27 April 2017, between 17:00 UTC and 22:00 UTC, six types of measurements at various depths were taken, which in combination provide the near-surface current shear in the area 89°38.29'W - 89°41.25'W and 29°9.83'N - 29°10.65'N. This dataset contains the current measurements obtained from (1) thin bamboo plates at 0.9 cm depth; (2) an undrogued LASER-style drifter at 1.8 cm depth; (3) a drogued LASER-style drifter at 30 cm depth; (4) polarimetry valid at 0.8 cm - 4.9 cm depth; (5) the Acoustic Doppler Current Profiler (ADCP) mounted on the autonomous REMUS for depths between 0.18 m and 3.77 m; and (6) the bottom-mounted ADCP from the research vessel Walton Smith for depths between 4 m and 13.5 m. In addition, the velocities obtained from a theoretical Stokes drift profile are provided for the top 1 m in steps of 0.1 cm.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (Drogued Drifter Velocity)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Start latitude, degrees_north)\nlongitude (Start longitude, degrees_east)\nlatitude2 (End latitude, degrees_north)\nlongitude2 (End longitude, degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform (RV_Walton_Smith)\ninstrument (drifters)\ninstrument1 (ADCP)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0038_drogued_drifter_velocity_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0038_drogued_drifter_velocity_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0038_drogued_drifter_velocity/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0038
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0038_drogued_drifter_velocity.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0038_drogued_drifter_velocity&showErrors=false&email= | University of New Hampshire / Department of Mechanical Engineering | R4_x265_000_0038_drogued_drifter_velocity | ||||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_plate_velocities.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_plate_velocities | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_plate_velocities.graph | Profile - R4.x265.000.0038 - plate_velocities - 29.16N, 89.64W - 2017-04-17 | As part of CARTHE 's SPLASH (Submesoscale Processes and Lagrangian Analysis on the SHelf) experiment, current observations were obtained from a variety of instruments in the Louisiana Bight, northern Gulf of Mexico. On 27 April 2017, between 17:00 UTC and 22:00 UTC, six types of measurements at various depths were taken, which in combination provide the near-surface current shear in the area 89°38.29'W - 89°41.25'W and 29°9.83'N - 29°10.65'N. This dataset contains the current measurements obtained from (1) thin bamboo plates at 0.9 cm depth; (2) an undrogued LASER-style drifter at 1.8 cm depth; (3) a drogued LASER-style drifter at 30 cm depth; (4) polarimetry valid at 0.8 cm - 4.9 cm depth; (5) the Acoustic Doppler Current Profiler (ADCP) mounted on the autonomous REMUS for depths between 0.18 m and 3.77 m; and (6) the bottom-mounted ADCP from the research vessel Walton Smith for depths between 4 m and 13.5 m. In addition, the velocities obtained from a theoretical Stokes drift profile are provided for the top 1 m in steps of 0.1 cm.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (Plate Velocities)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Start latitude, degrees_north)\nlongitude (Start longitude, degrees_east)\nlatitude2 (End latitude, degrees_north)\nlongitude2 (End longitude, degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform (RV_Walton_Smith)\ninstrument (drifters)\ninstrument1 (ADCP)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0038_plate_velocities_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0038_plate_velocities_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0038_plate_velocities/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0038
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0038_plate_velocities.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0038_plate_velocities&showErrors=false&email= | University of New Hampshire / Department of Mechanical Engineering | R4_x265_000_0038_plate_velocities | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_polarimeter_currents.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_polarimeter_currents | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_polarimeter_currents.graph | Profile - R4.x265.000.0038 - polarimeter_currents - 29.16N, 89.64W - 2017-04-17 | As part of CARTHE 's SPLASH (Submesoscale Processes and Lagrangian Analysis on the SHelf) experiment, current observations were obtained from a variety of instruments in the Louisiana Bight, northern Gulf of Mexico. On 27 April 2017, between 17:00 UTC and 22:00 UTC, six types of measurements at various depths were taken, which in combination provide the near-surface current shear in the area 89°38.29'W - 89°41.25'W and 29°9.83'N - 29°10.65'N. This dataset contains the current measurements obtained from (1) thin bamboo plates at 0.9 cm depth; (2) an undrogued LASER-style drifter at 1.8 cm depth; (3) a drogued LASER-style drifter at 30 cm depth; (4) polarimetry valid at 0.8 cm - 4.9 cm depth; (5) the Acoustic Doppler Current Profiler (ADCP) mounted on the autonomous REMUS for depths between 0.18 m and 3.77 m; and (6) the bottom-mounted ADCP from the research vessel Walton Smith for depths between 4 m and 13.5 m. In addition, the velocities obtained from a theoretical Stokes drift profile are provided for the top 1 m in steps of 0.1 cm.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (Polarimeter Currents)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Start latitude, degrees_north)\nlongitude (Start longitude, degrees_east)\nlatitude2 (End latitude, degrees_north)\nlongitude2 (End longitude, degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform (RV_Walton_Smith)\ninstrument (drifters)\ninstrument1 (ADCP)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0038_polarimeter_currents_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0038_polarimeter_currents_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0038_polarimeter_currents/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0038
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0038_polarimeter_currents.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0038_polarimeter_currents&showErrors=false&email= | University of New Hampshire / Department of Mechanical Engineering | R4_x265_000_0038_polarimeter_currents | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_REMUS_ADCP.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_REMUS_ADCP | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_REMUS_ADCP.graph | Profile - R4.x265.000.0038 - REMUS_ADCP - 29.16N, 89.64W - 2017-04-17 | As part of CARTHE 's SPLASH (Submesoscale Processes and Lagrangian Analysis on the SHelf) experiment, current observations were obtained from a variety of instruments in the Louisiana Bight, northern Gulf of Mexico. On 27 April 2017, between 17:00 UTC and 22:00 UTC, six types of measurements at various depths were taken, which in combination provide the near-surface current shear in the area 89°38.29'W - 89°41.25'W and 29°9.83'N - 29°10.65'N. This dataset contains the current measurements obtained from (1) thin bamboo plates at 0.9 cm depth; (2) an undrogued LASER-style drifter at 1.8 cm depth; (3) a drogued LASER-style drifter at 30 cm depth; (4) polarimetry valid at 0.8 cm - 4.9 cm depth; (5) the Acoustic Doppler Current Profiler (ADCP) mounted on the autonomous REMUS for depths between 0.18 m and 3.77 m; and (6) the bottom-mounted ADCP from the research vessel Walton Smith for depths between 4 m and 13.5 m. In addition, the velocities obtained from a theoretical Stokes drift profile are provided for the top 1 m in steps of 0.1 cm.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (REMUS_ADCP)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Start latitude, degrees_north)\nlongitude (Start longitude, degrees_east)\nlatitude2 (End latitude, degrees_north)\nlongitude2 (End longitude, degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform (RV_Walton_Smith)\ninstrument (drifters)\ninstrument1 (ADCP)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0038_REMUS_ADCP_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0038_REMUS_ADCP_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0038_REMUS_ADCP/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0038
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0038_REMUS_ADCP.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0038_REMUS_ADCP&showErrors=false&email= | University of New Hampshire / Department of Mechanical Engineering | R4_x265_000_0038_REMUS_ADCP | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_Stokes_drift.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_Stokes_drift | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_Stokes_drift.graph | Profile - R4.x265.000.0038 - Stokes_drift - 29.16N, 89.64W - 2017-04-17 | As part of CARTHE 's SPLASH (Submesoscale Processes and Lagrangian Analysis on the SHelf) experiment, current observations were obtained from a variety of instruments in the Louisiana Bight, northern Gulf of Mexico. On 27 April 2017, between 17:00 UTC and 22:00 UTC, six types of measurements at various depths were taken, which in combination provide the near-surface current shear in the area 89°38.29'W - 89°41.25'W and 29°9.83'N - 29°10.65'N. This dataset contains the current measurements obtained from (1) thin bamboo plates at 0.9 cm depth; (2) an undrogued LASER-style drifter at 1.8 cm depth; (3) a drogued LASER-style drifter at 30 cm depth; (4) polarimetry valid at 0.8 cm - 4.9 cm depth; (5) the Acoustic Doppler Current Profiler (ADCP) mounted on the autonomous REMUS for depths between 0.18 m and 3.77 m; and (6) the bottom-mounted ADCP from the research vessel Walton Smith for depths between 4 m and 13.5 m. In addition, the velocities obtained from a theoretical Stokes drift profile are provided for the top 1 m in steps of 0.1 cm.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (Stokes_drift)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Start latitude, degrees_north)\nlongitude (Start longitude, degrees_east)\nlatitude2 (End latitude, degrees_north)\nlongitude2 (End longitude, degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform (RV_Walton_Smith)\ninstrument (drifters)\ninstrument1 (ADCP)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0038_Stokes_drift_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0038_Stokes_drift_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0038_Stokes_drift/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0038
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0038_Stokes_drift.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0038_Stokes_drift&showErrors=false&email= | University of New Hampshire / Department of Mechanical Engineering | R4_x265_000_0038_Stokes_drift | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_undrogued_drifter_velocity | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_undrogued_drifter_velocity.graph | Profile - R4.x265.000.0038 - undrogued_drifter_velocity - 29.16N, 89.64W - 2017-04-17 | As part of CARTHE 's SPLASH (Submesoscale Processes and Lagrangian Analysis on the SHelf) experiment, current observations were obtained from a variety of instruments in the Louisiana Bight, northern Gulf of Mexico. On 27 April 2017, between 17:00 UTC and 22:00 UTC, six types of measurements at various depths were taken, which in combination provide the near-surface current shear in the area 89°38.29'W - 89°41.25'W and 29°9.83'N - 29°10.65'N. This dataset contains the current measurements obtained from (1) thin bamboo plates at 0.9 cm depth; (2) an undrogued LASER-style drifter at 1.8 cm depth; (3) a drogued LASER-style drifter at 30 cm depth; (4) polarimetry valid at 0.8 cm - 4.9 cm depth; (5) the Acoustic Doppler Current Profiler (ADCP) mounted on the autonomous REMUS for depths between 0.18 m and 3.77 m; and (6) the bottom-mounted ADCP from the research vessel Walton Smith for depths between 4 m and 13.5 m. In addition, the velocities obtained from a theoretical Stokes drift profile are provided for the top 1 m in steps of 0.1 cm.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (Undrogued Drifter Velocity)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Start latitude, degrees_north)\nlongitude (Start longitude, degrees_east)\nlatitude2 (End latitude, degrees_north)\nlongitude2 (End longitude, degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform (RV_Walton_Smith)\ninstrument (drifters)\ninstrument1 (ADCP)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0038_undrogued_drifter_velocity_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0038_undrogued_drifter_velocity_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0038_undrogued_drifter_velocity/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0038
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0038_undrogued_drifter_velocity.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0038_undrogued_drifter_velocity&showErrors=false&email= | University of New Hampshire / Department of Mechanical Engineering | R4_x265_000_0038_undrogued_drifter_velocity | ||||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_wave_spectrum.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_wave_spectrum | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_wave_spectrum.graph | Profile - R4.x265.000.0038 - wave_spectrum - 29.16N, 89.64W - 2017-04-17 | As part of CARTHE 's SPLASH (Submesoscale Processes and Lagrangian Analysis on the SHelf) experiment, current observations were obtained from a variety of instruments in the Louisiana Bight, northern Gulf of Mexico. On 27 April 2017, between 17:00 UTC and 22:00 UTC, six types of measurements at various depths were taken, which in combination provide the near-surface current shear in the area 89°38.29'W - 89°41.25'W and 29°9.83'N - 29°10.65'N. This dataset contains the current measurements obtained from (1) thin bamboo plates at 0.9 cm depth; (2) an undrogued LASER-style drifter at 1.8 cm depth; (3) a drogued LASER-style drifter at 30 cm depth; (4) polarimetry valid at 0.8 cm - 4.9 cm depth; (5) the Acoustic Doppler Current Profiler (ADCP) mounted on the autonomous REMUS for depths between 0.18 m and 3.77 m; and (6) the bottom-mounted ADCP from the research vessel Walton Smith for depths between 4 m and 13.5 m. In addition, the velocities obtained from a theoretical Stokes drift profile are provided for the top 1 m in steps of 0.1 cm.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (Wave Spectrum)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Start latitude, degrees_north)\nlongitude (Start longitude, degrees_east)\nlatitude2 (End latitude, degrees_north)\nlongitude2 (End longitude, degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform (RV_Walton_Smith)\ninstrument (drifters)\ninstrument1 (ADCP)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0038_wave_spectrum_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0038_wave_spectrum_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0038_wave_spectrum/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0038
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0038_wave_spectrum.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0038_wave_spectrum&showErrors=false&email= | University of New Hampshire / Department of Mechanical Engineering | R4_x265_000_0038_wave_spectrum | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_WH1200kHz_ADCP.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_WH1200kHz_ADCP | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0038_WH1200kHz_ADCP.graph | Profile - R4.x265.000.0038 - WH1200kHz_ADCP - 29.16N, 89.64W - 2017-04-17 | As part of CARTHE 's SPLASH (Submesoscale Processes and Lagrangian Analysis on the SHelf) experiment, current observations were obtained from a variety of instruments in the Louisiana Bight, northern Gulf of Mexico. On 27 April 2017, between 17:00 UTC and 22:00 UTC, six types of measurements at various depths were taken, which in combination provide the near-surface current shear in the area 89°38.29'W - 89°41.25'W and 29°9.83'N - 29°10.65'N. This dataset contains the current measurements obtained from (1) thin bamboo plates at 0.9 cm depth; (2) an undrogued LASER-style drifter at 1.8 cm depth; (3) a drogued LASER-style drifter at 30 cm depth; (4) polarimetry valid at 0.8 cm - 4.9 cm depth; (5) the Acoustic Doppler Current Profiler (ADCP) mounted on the autonomous REMUS for depths between 0.18 m and 3.77 m; and (6) the bottom-mounted ADCP from the research vessel Walton Smith for depths between 4 m and 13.5 m. In addition, the velocities obtained from a theoretical Stokes drift profile are provided for the top 1 m in steps of 0.1 cm.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (WH1200kHz_ADCP)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (Start latitude, degrees_north)\nlongitude (Start longitude, degrees_east)\nlatitude2 (End latitude, degrees_north)\nlongitude2 (End longitude, degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform (RV_Walton_Smith)\ninstrument (drifters)\ninstrument1 (ADCP)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0038_WH1200kHz_ADCP_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0038_WH1200kHz_ADCP_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0038_WH1200kHz_ADCP/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0038
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0038_WH1200kHz_ADCP.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0038_WH1200kHz_ADCP&showErrors=false&email= | University of New Hampshire / Department of Mechanical Engineering | R4_x265_000_0038_WH1200kHz_ADCP | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR1_moored_ADCP_profile.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR1_moored_ADCP_profile | https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR1_moored_ADCP_profile.graph | Profile - R4.x265.239.0003 - MCR1_moored_ADCP_profile - 46.26N, 124.06W - 2013-06-07 | Passive optical observations of the near-surface current profile were made in the Mouth of the Columbia River from June 2-6, 2013. A calibration and validation study was performed in the University of Miami's SUSTAIN facility.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (MCR1_moored_ADCP_profile)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform\ninstrument (drifters)\ninstrument1\ninstrument2 (1200 kHzADCP)\ninstrument3 (R.M. Young sonic anemometer)\ninstrument4 (Gill R2 sonic anemometer)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_239_0003_MCR1_moored_ADCP_profile_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_239_0003_MCR1_moored_ADCP_profile_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_239_0003_MCR1_moored_ADCP_profile/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265..239:0003
| https://erddap.griidc.org/erddap/rss/R4_x265_239_0003_MCR1_moored_ADCP_profile.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_239_0003_MCR1_moored_ADCP_profile&showErrors=false&email= | University of Miami / Rosenstiel School of Marine and Atmospheric Science | R4_x265_239_0003_MCR1_moored_ADCP_profile | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR2_moored_ADCP_profile.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR2_moored_ADCP_profile | https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR2_moored_ADCP_profile.graph | Profile - R4.x265.239.0003 - MCR2_moored_ADCP_profile - 46.26N, 124.06W - 2013-06-07 | Passive optical observations of the near-surface current profile were made in the Mouth of the Columbia River from June 2-6, 2013. A calibration and validation study was performed in the University of Miami's SUSTAIN facility.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (MCR2_moored_ADCP_profile)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nplatform\ninstrument (drifters)\ninstrument1\ninstrument2 (1200 kHzADCP)\ninstrument3 (R.M. Young sonic anemometer)\ninstrument4 (Gill R2 sonic anemometer)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_239_0003_MCR2_moored_ADCP_profile_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_239_0003_MCR2_moored_ADCP_profile_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_239_0003_MCR2_moored_ADCP_profile/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265..239:0003
| https://erddap.griidc.org/erddap/rss/R4_x265_239_0003_MCR2_moored_ADCP_profile.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_239_0003_MCR2_moored_ADCP_profile&showErrors=false&email= | University of Miami / Rosenstiel School of Marine and Atmospheric Science | R4_x265_239_0003_MCR2_moored_ADCP_profile | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR2_pol_profile.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR2_pol_profile | https://erddap.griidc.org/erddap/tabledap/R4_x265_239_0003_MCR2_pol_profile.graph | Profile - R4.x265.239.0003 - MCR2_pol_profile - 46.26N, 124.03W - 2013-06-07 | Passive optical observations of the near-surface current profile were made in the Mouth of the Columbia River from June 2-6, 2013. A calibration and validation study was performed in the University of Miami's SUSTAIN facility.\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (MCR2_pol_profile)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ncurrent_speed (m s-1)\ncurrent_direction (current direction [degrees CW from N], degree)\nwavenumber (rad m-1)\nplatform\ninstrument (drifters)\ninstrument1\ninstrument2 (1200 kHzADCP)\ninstrument3 (R.M. Young sonic anemometer)\ninstrument4 (Gill R2 sonic anemometer)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_239_0003_MCR2_pol_profile_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_239_0003_MCR2_pol_profile_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_239_0003_MCR2_pol_profile/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265..239:0003
| https://erddap.griidc.org/erddap/rss/R4_x265_239_0003_MCR2_pol_profile.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_239_0003_MCR2_pol_profile&showErrors=false&email= | University of Miami / Rosenstiel School of Marine and Atmospheric Science | R4_x265_239_0003_MCR2_pol_profile | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_1.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_1 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_1.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_1 - 28.49N, 88.50W - 2012-07-08 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_1)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_1_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_1_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_1/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_1.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_1&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_1 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_10.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_10 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_10.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_10 - 28.76N, 88.27W - 1997-03-20 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_10)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_10_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_10_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_10/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_10.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_10&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_10 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_11.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_11 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_11.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_11 - 29.07N, 87.86W - 1997-03-22 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_11)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_11_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_11_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_11/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_11.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_11&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_11 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_12.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_12 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_12.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_12 - 29.00N, 87.35W - 1997-03-24 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_12)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_12_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_12_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_12/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_12.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_12&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_12 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_13.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_13 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_13.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_13 - 27.29N, 89.78W - 1999-08-29 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_13)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_13_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_13_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_13/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_13.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_13&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_13 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_14.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_14 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_14.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_14 - 27.22N, 89.97W - 1999-08-29 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_14)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_14_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_14_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_14/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_14.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_14&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_14 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_15.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_15 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_15.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_15 - 27.11N, 89.81W - 1999-08-29 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_15)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_15_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_15_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_15/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_15.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_15&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_15 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_16.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_16 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_16.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_16 - 27.23N, 90.03W - 2001-02-13 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_16)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_16_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_16_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_16/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_16.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_16&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_16 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_17.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_17 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_17.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_17 - 27.19N, 90.28W - 1999-08-28 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_17)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_17_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_17_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_17/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_17.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_17&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_17 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_18.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_18 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_18.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_18 - 26.34N, 90.82W - 2000-02-16 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_18)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_18_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_18_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_18/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_18.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_18&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_18 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_19.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_19 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_19.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_19 - 26.34N, 90.82W - 2000-07-31 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_19)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_19_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_19_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_19/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_19.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_19&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_19 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_2.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_2 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_2.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_2 - 28.74N, 88.75W - 2012-07-07 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_2)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_2_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_2_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_2/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_2.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_2&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_2 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_20.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_20 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_20.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_20 - 26.34N, 90.82W - 2001-07-31 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_20)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_20_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_20_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_20/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_20.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_20&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_20 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_21.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_21 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_21.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_21 - 26.34N, 90.82W - 2003-04-17 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_21)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_21_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_21_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_21/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_21.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_21&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_21 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_22.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_22 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_22.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_22 - 27.60N, 89.22W - 2003-03-19 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_22)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_22_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_22_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_22/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_22.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_22&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_22 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_23.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_23 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_23.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_23 - 27.09N, 91.11W - 2003-03-26 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_23)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_23_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_23_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_23/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_23.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_23&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_23 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_24.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_24 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_24.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_24 - 26.08N, 88.96W - 2003-04-05 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_24)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_24_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_24_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_24/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_24.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_24&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_24 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_25.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_25 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_25.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_25 - 25.92N, 91.13W - 2003-04-01 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_25)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_25_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_25_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_25/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_25.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_25&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_25 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_26.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_26 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_26.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_26 - 27.28N, 89.74W - 2003-03-01 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_26)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_26_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_26_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_26/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_26.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_26&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_26 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_27.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_27 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_27.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_27 - 27.02N, 90.23W - 2003-03-02 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_27)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_27_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_27_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_27/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_27.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_27&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_27 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_28.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_28 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_28.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_28 - 26.83N, 90.64W - 2003-03-23 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_28)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_28_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_28_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_28/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_28.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_28&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_28 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_29.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_29 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_29.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_29 - 27.15N, 90.40W - 2003-03-28 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_29)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_29_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_29_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_29/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_29.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_29&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_29 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_3.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_3 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_3.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_3 - 28.74N, 88.25W - 2012-07-07 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_3)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_3_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_3_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_3/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_3.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_3&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_3 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_30.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_30 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_30.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_30 - 27.35N, 89.95W - 2003-03-21 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_30)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_30_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_30_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_30/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_30.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_30&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_30 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_31.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_31 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_31.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_31 - 27.02N, 89.08W - 2003-03-07 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_31)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_31_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_31_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_31/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_31.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_31&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_31 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_32.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_32 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_32.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_32 - 26.89N, 89.80W - 2003-03-01 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_32)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_32_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_32_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_32/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_32.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_32&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_32 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_33.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_33 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_33.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_33 - 26.69N, 90.43W - 2003-03-02 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_33)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_33_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_33_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_33/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_33.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_33&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_33 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_34.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_34 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_34.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_34 - 26.52N, 91.13W - 2003-03-04 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_34)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_34_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_34_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_34/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_34.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_34&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_34 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_35.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_35 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_35.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_35 - 26.48N, 91.73W - 2003-03-05 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_35)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_35_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_35_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_35/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_35.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_35&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_35 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_36.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_36 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_36.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_36 - 26.47N, 89.03W - 2003-03-07 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_36)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_36_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_36_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_36/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_36.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_36&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_36 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_37.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_37 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_37.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_37 - 26.35N, 89.78W - 2003-03-08 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_37)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_37_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_37_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_37/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_37.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_37&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_37 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_38.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_38 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_38.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_38 - 26.31N, 90.70W - 2003-03-04 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_38)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_38_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_38_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_38/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_38.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_38&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_38 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_39.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_39 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_39.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_39 - 26.09N, 91.79W - 2003-03-04 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_39)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_39_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_39_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_39/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_39.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_39&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_39 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_4.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_4 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_4.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_4 - 28.25N, 88.75W - 2012-07-09 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_4)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_4_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_4_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_4/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_4.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_4&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_4 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_40.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_40 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_40.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_40 - 25.96N, 89.81W - 2003-03-07 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_40)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_40_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_40_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_40/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_40.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_40&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_40 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_41.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_41 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_41.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_41 - 25.38N, 95.44W - 2004-08-27 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_41)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_41_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_41_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_41/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_41.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_41&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_41 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_42.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_42 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_42.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_42 - 25.27N, 94.89W - 2004-08-27 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_42)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_42_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_42_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_42/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_42.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_42&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_42 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_43.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_43 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_43.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_43 - 24.65N, 96.08W - 2004-08-26 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_43)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_43_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_43_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_43/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_43.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_43&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_43 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_44.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_44 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_44.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_44 - 24.04N, 96.30W - 2004-08-26 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_44)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_44_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_44_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_44/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_44.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_44&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_44 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_45.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_45 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_45.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_45 - 27.21N, 95.52W - 2004-03-25 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_45)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_45_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_45_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_45/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_45.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_45&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_45 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_46.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_46 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_46.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_46 - 26.92N, 94.72W - 2004-03-25 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_46)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_46_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_46_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_46/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_46.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_46&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_46 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_47.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_47 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_47.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_47 - 26.62N, 95.55W - 2004-03-26 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_47)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_47_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_47_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_47/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_47.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_47&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_47 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_48.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_48 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_48.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_48 - 26.50N, 94.81W - 2004-03-29 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_48)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_48_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_48_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_48/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_48.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_48&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_48 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_49.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_49 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_49.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_49 - 26.61N, 93.93W - 2004-03-30 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_49)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_49_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_49_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_49/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_49.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_49&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_49 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_5.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_5 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_5.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_5 - 28.00N, 89.00W - 2012-07-10 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_5)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_5_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_5_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_5/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_5.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_5&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_5 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_50.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_50 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_50.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_50 - 26.04N, 95.58W - 2004-03-22 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_50)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_50_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_50_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_50/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_50.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_50&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_50 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_51.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_51 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_51.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_51 - 26.04N, 94.95W - 2004-03-21 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_51)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_51_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_51_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_51/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_51.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_51&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_51 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_52.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_52 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_52.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_52 - 26.03N, 94.09W - 2004-03-20 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_52)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_52_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_52_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_52/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_52.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_52&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_52 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_53.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_53 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_53.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_53 - 26.13N, 94.88W - 2004-05-24 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_53)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_53_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_53_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_53/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_53.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_53&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_53 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_54.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_54 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_54.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_54 - 25.50N, 86.97W - 2000-05-31 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_54)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_54_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_54_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_54/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_54.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_54&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_54 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_55.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_55 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_55.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_55 - 25.50N, 86.97W - 2001-08-03 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_55)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_55_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_55_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_55/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_55.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_55&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_55 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_56.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_56 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_56.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_56 - 25.50N, 86.97W - 2003-04-19 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_56)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_56_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_56_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_56/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_56.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_56&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_56 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_57.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_57 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_57.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_57 - 25.50N, 86.97W - 2005-05-29 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_57)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_57_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_57_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_57/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_57.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_57&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_57 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_58.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_58 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_58.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_58 - 25.50N, 86.96W - 2006-06-17 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_58)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_58_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_58_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_58/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_58.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_58&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_58 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_59.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_59 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_59.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_59 - 28.34N, 87.55W - 2005-01-21 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_59)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_59_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_59_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_59/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_59.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_59&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_59 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_6.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_6 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_6.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_6 - 28.49N, 88.50W - 2012-07-05 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_6)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_6_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_6_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_6/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_6.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_6&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_6 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_60.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_60 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_60.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_60 - 27.99N, 87.84W - 2005-01-20 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_60)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_60_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_60_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_60/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_60.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_60&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_60 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_61.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_61 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_61.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_61 - 27.60N, 87.53W - 2005-01-19 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_61)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_61_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_61_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_61/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_61.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_61&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_61 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_62.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_62 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_62.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_62 - 27.99N, 87.56W - 2005-01-19 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_62)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_62_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_62_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_62/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_62.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_62&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_62 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_63.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_63 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_63.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_63 - 28.34N, 87.55W - 2005-08-22 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_63)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_63_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_63_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_63/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_63.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_63&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_63 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_64.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_64 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_64.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_64 - 27.99N, 87.84W - 2005-08-25 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_64)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_64_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_64_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_64/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_64.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_64&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_64 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_65.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_65 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_65.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_65 - 27.60N, 87.54W - 2005-08-23 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_65)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_65_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_65_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_65/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_65.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_65&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_65 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_66.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_66 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_66.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_66 - 28.00N, 87.56W - 2005-08-19 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_66)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_66_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_66_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_66/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_66.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_66&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_66 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_67.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_67 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_67.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_67 - 23.24N, 86.29W - 2009-06-02 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_67)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_67_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_67_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_67/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_67.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_67&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_67 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_68.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_68 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_68.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_68 - 23.60N, 86.02W - 2009-06-01 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_68)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_68_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_68_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_68/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_68.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_68&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_68 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_69.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_69 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_69.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_69 - 24.39N, 87.41W - 2009-05-31 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_69)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_69_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_69_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_69/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_69.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_69&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_69 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_7.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_7 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_7.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_7 - 28.74N, 88.25W - 2013-07-08 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_7)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_7_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_7_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_7/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_7.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_7&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_7 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_70.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_70 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_70.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_70 - 24.95N, 87.08W - 2009-06-01 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_70)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_70_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_70_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_70/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_70.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_70&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_70 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_71.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_71 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_71.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_71 - 21.59N, 86.23W - 2009-06-12 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_71)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_71_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_71_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_71/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_71.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_71&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_71 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_72.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_72 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_72.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_72 - 21.64N, 85.99W - 2009-06-04 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_72)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_72_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_72_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_72/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_72.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_72&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_72 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_73.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_73 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_73.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_73 - 21.63N, 85.72W - 2009-06-03 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_73)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_73_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_73_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_73/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_73.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_73&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_73 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_74.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_74 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_74.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_74 - 25.96N, 88.05W - 2009-05-06 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_74)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_74_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_74_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_74/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_74.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_74&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_74 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_75.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_75 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_75.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_75 - 25.81N, 87.55W - 2009-05-04 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_75)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_75_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_75_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_75/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_75.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_75&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_75 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_76.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_76 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_76.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_76 - 25.67N, 87.05W - 2009-05-01 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_76)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_76_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_76_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_76/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_76.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_76&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_76 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_77.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_77 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_77.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_77 - 25.48N, 86.56W - 2009-04-30 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_77)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_77_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_77_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_77/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_77.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_77&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_77 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_78.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_78 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_78.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_78 - 26.25N, 87.32W - 2009-05-15 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_78)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_78_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_78_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_78/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_78.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_78&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_78 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_79.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_79 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_79.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_79 - 26.11N, 86.84W - 2009-05-11 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_79)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_79_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_79_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_79/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_79.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_79&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_79 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_8.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_8 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_8.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_8 - 28.25N, 88.75W - 2013-07-10 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_8)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_8_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_8_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_8/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_8.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_8&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_8 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_80.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_80 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_80.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_80 - 25.92N, 86.36W - 2009-05-11 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_80)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_80_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_80_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_80/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_80.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_80&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_80 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_81.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_81 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_81.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_81 - 26.37N, 86.14W - 2009-04-21 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_81)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_81_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_81_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_81/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_81.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_81&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_81 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_82.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_82 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_82.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_82 - 26.17N, 85.65W - 2009-04-22 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_82)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_82_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_82_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_82/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_82.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_82&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_82 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_83.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_83 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_83.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_83 - 26.41N, 87.85W - 2009-05-06 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_83)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_83_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_83_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_83/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_83.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_83&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_83 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_84.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_84 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_84.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_84 - 26.69N, 87.13W - 2009-05-06 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_84)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_84_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_84_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_84/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_84.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_84&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_84 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_85.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_85 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_85.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_85 - 26.54N, 86.62W - 2009-05-09 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_85)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_85_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_85_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_85/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_85.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_85&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_85 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_86.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_86 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_86.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_86 - 25.29N, 86.08W - 2009-04-28 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_86)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_86_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_86_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_86/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_86.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_86&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_86 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_87.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_87 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_87.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_87 - 25.73N, 85.86W - 2009-04-27 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_87)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_87_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_87_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_87/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_87.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_87&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_87 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_88.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_88 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_88.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_88 - 25.55N, 85.38W - 2009-04-21 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_88)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_88_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_88_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_88/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_88.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_88&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_88 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_89.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_89 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_89.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_89 - 25.99N, 85.15W - 2009-04-22 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_89)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_89_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_89_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_89/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_89.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_89&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_89 | |||
| https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_9.subset | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_9 | https://erddap.griidc.org/erddap/tabledap/R6_x820_000_0001_Mooring_current_3hourfilted_9.graph | TimeSeriesProfile - R6.x820.000.0001 - Mooring_current_3hourfilted_9 - 28.00N, 89.00W - 2013-07-10 | Selected Historical Mooring Data in The Gulf of Mexico. This dataset is selected from the existing historical ocean current measurements, mainly from ocean moorings. The usage of this dataset is to investigate the singles of subinertial ocean currents as well as the subinertial modulation of internal waves in the subsurface ocean. The archived data were processed under quality control with a single uniform standard. In particular, unrealistic spikes and clearly bad data that are due to instrument malfunctions have been removed. Most of the raw current data recorded in these instruments have been cleaned and quality controlled, for instance, with calibrations and magnetic variation corrections applied resolved in-water start/stop times, and single point spikes removed. Some records were low-pass filtered with a cutoff period of three hours. Data are filtered to remove obvious outliers with value (zonal or meridional component) larger than eight times standard deviation of the time series. Records shorter than 100 days or having less than 90% completeness are not considered in this study. Although velocity larger than 85 cm/s was observed in water depths of 2000 m (Hamilton and Lugo-Fernandez, 2001), strong currents greater than 1 m/s are rare in deep ocean and might be biased due to instrument errors that can be seen in the collected data. We do not include the record below 1000 m in the following analysis that has maximum zonal or meridional velocity larger than 1.2 m/s. Data record interval is made nearly evenly spaced. For the raw data or those without knowing whether data were filtered, three-hour low-pass filter is applied.\n\ncdm_data_type = TimeSeriesProfile\nVARIABLES:\nstation (Mooring_current_3hourfilted_9)\ntime (decimal days, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (m)\ntotal_water_depth (m)\ncurrent_speed (current speed [knots], cm s-1)\nzonal_sea_water_velocity (Zonal velocity, cm s-1)\nmeridional_sea_water_velocity (meridional velocity, cm s-1)\nflag (quality flag (0 = good; 1 = bad))\n... (5 more variables)\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R6_x820_000_0001_Mooring_current_3hourfilted_9_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R6_x820_000_0001_Mooring_current_3hourfilted_9_iso19115.xml | https://erddap.griidc.org/erddap/info/R6_x820_000_0001_Mooring_current_3hourfilted_9/index.htmlTable | https://data.gulfresearchinitiative.org/data/R6.x820.000:0001
| https://erddap.griidc.org/erddap/rss/R6_x820_000_0001_Mooring_current_3hourfilted_9.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R6_x820_000_0001_Mooring_current_3hourfilted_9&showErrors=false&email= | University of South Florida / College of Marine Science | R6_x820_000_0001_Mooring_current_3hourfilted_9 | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_1_CODE_041_2015723.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_1_CODE_041_2015723 | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_1_CODE_041_2015723.graph | Trajectory - R4.x265.000.0015 - 1-CODE-041_2015723 - 25.73N, 80.14W - 2015-07-23 | Lagrangian Submesoscale Experiment (LASER) drifter calibration. The LASER drifter is a new surface drifter that is compact, cost-effective, and biodegradable. It accurately follows the current over the upper 0.60m, with very limited influence of the wind or waves. A series of experiments was carried out in the ASIST wind-wave flume to evaluate the water following capabilities of the drifter in the presence of strong winds and waves. The trajectories of the CODE drifter and the LASER drifter were compared during short deployments in the ocean. This dataset contains the drifter's velocity measured in the tank under different current, wind and waves conditions. It also contains the trajectories of the drifters in the ocean.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (CODE-041)\ntime (seconds since 1970-01-01T00:00:00Z)\nmatlabTime (matlab serial date number, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nheading (platform heading, degree)\nzonal_velocity (East-West Velocity, m s-1)\nmeridional_velocity (North-South Velocity, m s-1)\ncurrent_speed (m s-1)\nplatform\ninstrument (CODE drifter)\ninstrument1 (LASER drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0015_1_CODE_041_2015723_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0015_1_CODE_041_2015723_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0015_1_CODE_041_2015723/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0015
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0015_1_CODE_041_2015723.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0015_1_CODE_041_2015723&showErrors=false&email= | University of Miami / Rosenstiel School of Marine and Atmospheric Science | R4_x265_000_0015_1_CODE_041_2015723 | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_2_NECK_129_2015723.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_2_NECK_129_2015723 | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_2_NECK_129_2015723.graph | Trajectory - R4.x265.000.0015 - 2-NECK-129_2015723 - 25.73N, 80.14W - 2015-07-23 | Lagrangian Submesoscale Experiment (LASER) drifter calibration. The LASER drifter is a new surface drifter that is compact, cost-effective, and biodegradable. It accurately follows the current over the upper 0.60m, with very limited influence of the wind or waves. A series of experiments was carried out in the ASIST wind-wave flume to evaluate the water following capabilities of the drifter in the presence of strong winds and waves. The trajectories of the CODE drifter and the LASER drifter were compared during short deployments in the ocean. This dataset contains the drifter's velocity measured in the tank under different current, wind and waves conditions. It also contains the trajectories of the drifters in the ocean.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory\ntime (seconds since 1970-01-01T00:00:00Z)\nmatlabTime (matlab serial date number, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nheading (platform heading, degree)\nzonal_velocity (East-West Velocity, m s-1)\nmeridional_velocity (North-South Velocity, m s-1)\ncurrent_speed (m s-1)\nplatform\ninstrument (CODE drifter)\ninstrument1 (LASER drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0015_2_NECK_129_2015723_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0015_2_NECK_129_2015723_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0015_2_NECK_129_2015723/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0015
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0015_2_NECK_129_2015723.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0015_2_NECK_129_2015723&showErrors=false&email= | University of Miami / Rosenstiel School of Marine and Atmospheric Science | R4_x265_000_0015_2_NECK_129_2015723 | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_3_LASER074_2015723.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_3_LASER074_2015723 | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_3_LASER074_2015723.graph | Trajectory - R4.x265.000.0015 - 3-LASER074_2015723 - 25.72N, 80.11W - 2015-07-23 | Lagrangian Submesoscale Experiment (LASER) drifter calibration. The LASER drifter is a new surface drifter that is compact, cost-effective, and biodegradable. It accurately follows the current over the upper 0.60m, with very limited influence of the wind or waves. A series of experiments was carried out in the ASIST wind-wave flume to evaluate the water following capabilities of the drifter in the presence of strong winds and waves. The trajectories of the CODE drifter and the LASER drifter were compared during short deployments in the ocean. This dataset contains the drifter's velocity measured in the tank under different current, wind and waves conditions. It also contains the trajectories of the drifters in the ocean.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (LASER074)\ntime (seconds since 1970-01-01T00:00:00Z)\nmatlabTime (matlab serial date number, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nheading (platform heading, degree)\nzonal_velocity (East-West Velocity, m s-1)\nmeridional_velocity (North-South Velocity, m s-1)\ncurrent_speed (m s-1)\nplatform\ninstrument (CODE drifter)\ninstrument1 (LASER drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0015_3_LASER074_2015723_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0015_3_LASER074_2015723_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0015_3_LASER074_2015723/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0015
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0015_3_LASER074_2015723.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0015_3_LASER074_2015723&showErrors=false&email= | University of Miami / Rosenstiel School of Marine and Atmospheric Science | R4_x265_000_0015_3_LASER074_2015723 | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_4_ISPHERE008_2015723.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_4_ISPHERE008_2015723 | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0015_4_ISPHERE008_2015723.graph | Trajectory - R4.x265.000.0015 - 4-ISPHERE008_2015723 - 25.73N, 80.14W - 2015-07-23 | Lagrangian Submesoscale Experiment (LASER) drifter calibration. The LASER drifter is a new surface drifter that is compact, cost-effective, and biodegradable. It accurately follows the current over the upper 0.60m, with very limited influence of the wind or waves. A series of experiments was carried out in the ASIST wind-wave flume to evaluate the water following capabilities of the drifter in the presence of strong winds and waves. The trajectories of the CODE drifter and the LASER drifter were compared during short deployments in the ocean. This dataset contains the drifter's velocity measured in the tank under different current, wind and waves conditions. It also contains the trajectories of the drifters in the ocean.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory\ntime (seconds since 1970-01-01T00:00:00Z)\nmatlabTime (matlab serial date number, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nheading (platform heading, degree)\nzonal_velocity (East-West Velocity, m s-1)\nmeridional_velocity (North-South Velocity, m s-1)\ncurrent_speed (m s-1)\nplatform\ninstrument (CODE drifter)\ninstrument1 (LASER drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0015_4_ISPHERE008_2015723_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0015_4_ISPHERE008_2015723_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0015_4_ISPHERE008_2015723/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0015
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0015_4_ISPHERE008_2015723.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0015_4_ISPHERE008_2015723&showErrors=false&email= | University of Miami / Rosenstiel School of Marine and Atmospheric Science | R4_x265_000_0015_4_ISPHERE008_2015723 | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-19T13-37-47Z_0m - 29.01N, 89.80W - 2017-04-19 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-19T13-37-47Z_0m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_19T13_37_47Z_0m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-19T13-38-00Z_5m - 29.01N, 89.80W - 2017-04-19 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-19T13-38-00Z_5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_19T13_38_00Z_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-20T23-50-03Z_5m - 28.94N, 89.12W - 2017-04-20 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-20T23-50-03Z_5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_20T23_50_03Z_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-21T00-00-59Z_0m - 28.94N, 89.12W - 2017-04-21 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-21T00-00-59Z_0m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_21T00_00_59Z_0m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-21T00-02-47Z_0m - 28.94N, 89.13W - 2017-04-21 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-21T00-02-47Z_0m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_21T00_02_47Z_0m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T13-40-48Z_5m - 29.12N, 89.87W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T13-40-48Z_5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T13_40_48Z_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T13-54-11Z_0m - 29.12N, 89.87W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T13-54-11Z_0m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T13_54_11Z_0m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T14-14-08Z_2.5m - 29.13N, 89.86W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T14-14-08Z_2.5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T14_14_08Z_2_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T15-49-13Z_5m - 28.96N, 89.82W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T15-49-13Z_5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T15_49_13Z_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T16-04-37Z2_5m - 28.96N, 89.82W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T16-04-37Z2_5m)\nobservations\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T16_04_37Z2_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T16-15-59Z_0m - 28.97N, 89.81W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T16-15-59Z_0m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T16_15_59Z_0m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T17-57-04Z_5m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T17-57-04Z_5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T17_57_04Z_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T18-06-08Z_2.5m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T18-06-08Z_2.5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T18_06_08Z_2_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T18-14-08Z_0m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T18-14-08Z_0m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T18_14_08Z_0m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T18-19-25Z_0m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T18-19-25Z_0m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T18_19_25Z_0m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T18-25-59Z_2.5m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T18-25-59Z_2.5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T18_25_59Z_2_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T18-32-11Z_5m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T18-32-11Z_5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T18_32_11Z_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T18-42-19Z_5m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T18-42-19Z_5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T18_42_19Z_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T18-50-38Z_2.5m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T18-50-38Z_2.5m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T18_50_38Z_2_5m | |||
| https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m.subset | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m | https://erddap.griidc.org/erddap/tabledap/R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m.graph | Trajectory - R4.x265.000.0043 - Drifter_2017-04-25T18-56-05Z_0m - 28.90N, 89.50W - 2017-04-25 | SPLASH Conductivity, Temperature, Depth (CTD), drifter, and wave buoy data, Mississippi River delta, April 2017. This dataset includes CTD casts, Global Positioning System (GPS) logs from drifter deployments, and accelerometer data from wave buoy deployments. These data were collected in the Gulf of Mexico near the Mississippi River delta during the SPLASH field campaign between April 19-27, 2017. The CTD was a YSI Castaway. CTD casts were performed near freshwater lenses to investigate the vertical and horizontal temperature and salinity structure associated with the lens. The drifters had three different lengths of drogues: 0 m, 2.5 m, and 5 m. They were equipped with a Bad Elf GPS unit or an iPhone GPS. Drifters with different lengths of drogues were deployed near freshwater lenses to observe the near surface currents. The wave buoy had a Yost accelerometer to determine wave period and height. Deployments were conducted near freshwater lenses to determine different wave structure on each side of the frontal interface.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (D2017-04-25T18-56-05Z_0m)\ntime (seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\ndepth (Depth of vessel's seawater intake, m)\nair_pressure (mbar)\ncurrent_speed (m s-1)\nplatform\ninstrument (Drifter)\ncrs\n | https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m_fgdc.xml | https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m_iso19115.xml | https://erddap.griidc.org/erddap/info/R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m/index.htmlTable | https://data.gulfresearchinitiative.org/data/R4.x265.000:0043
| https://erddap.griidc.org/erddap/rss/R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m.rss | https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m&showErrors=false&email= | Nova Southeastern University / Oceanographic Center | R4_x265_000_0043_Drifter_2017_04_25T18_56_05Z_0m |