NOAA ERDDAP
Easier access to scientific data
   
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 Email Institution Dataset ID
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_001.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_001 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_001.graph Profile - R4.x257.230.0019 - DP03_HS6_001 - 28.00N, 88.02W - 2016-05-01 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_001)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_001_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_001_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_001/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_001.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_001&showErrors=false&email= UNKNOWN R4_x257_230_0019_DP03_HS6_001
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_002.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_002 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_002.graph Profile - R4.x257.230.0019 - DP03_HS6_002 - 28.02N, 88.02W - 2016-05-01 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_002)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_002_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_002_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_002/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_002.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_002&showErrors=false&email= UNKNOWN R4_x257_230_0019_DP03_HS6_002
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_003.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_003 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_003.graph Profile - R4.x257.230.0019 - DP03_HS6_003 - 28.04N, 88.05W - 2016-05-02 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_003)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_003_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_003_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_003/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_003.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_003&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_003
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_004.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_004 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_004.graph Profile - R4.x257.230.0019 - DP03_HS6_004 - 27.98N, 87.50W - 2016-05-03 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_004)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_004_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_004_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_004/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_004.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_004&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_004
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_005.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_005 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_005.graph Profile - R4.x257.230.0019 - DP03_HS6_005 - 28.00N, 87.51W - 2016-05-03 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_005)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_005_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_005_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_005/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_005.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_005&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_005
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_006.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_006 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_006.graph Profile - R4.x257.230.0019 - DP03_HS6_006 - 27.99N, 87.00W - 2016-05-04 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_006)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_006_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_006_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_006/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_006.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_006&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_006
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_007.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_007 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_007.graph Profile - R4.x257.230.0019 - DP03_HS6_007 - 28.00N, 87.00W - 2016-05-05 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_007)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_007_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_007_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_007/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_007.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_007&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_007
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_008.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_008 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_008.graph Profile - R4.x257.230.0019 - DP03_HS6_008 - 28.00N, 87.33W - 2016-05-06 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_008)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_008_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_008_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_008/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_008.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_008&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_008
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_009.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_009 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_009.graph Profile - R4.x257.230.0019 - DP03_HS6_009 - 27.46N, 86.91W - 2016-05-07 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_009)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_009_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_009_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_009/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_009.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_009&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_009
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_010.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_010 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_010.graph Profile - R4.x257.230.0019 - DP03_HS6_010 - 27.49N, 86.87W - 2016-05-07 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_010)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_010_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_010_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_010/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_010.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_010&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_010
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_011.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_011 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_011.graph Profile - R4.x257.230.0019 - DP03_HS6_011 - 27.01N, 86.57W - 2016-05-07 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_011)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_011_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_011_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_011/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_011.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_011&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_011
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_012.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_012 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP03_HS6_012.graph Profile - R4.x257.230.0019 - DP03_HS6_012 - 26.96N, 86.43W - 2016-05-08 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP03_HS6_012)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_442nm (Optical backscattering at 140 degree, 442nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_470nm (Optical backscattering at 140 degree, 470nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_532nm (Optical backscattering at 140 degree, 532nm optical_absorption_spectra_at_, 1/m)\n... (9 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP03_HS6_012_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP03_HS6_012_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP03_HS6_012/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP03_HS6_012.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP03_HS6_012&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP03_HS6_012
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_001.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_001 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_001.graph Profile - R4_x257_230_0019 - DP04_HS2_001 - 26.99N, 89.99W - 2016-08-06 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_001)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_001_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_001_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_001/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_001.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_001&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_001
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_002.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_002 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_002.graph Profile - R4_x257_230_0019 - DP04_HS2_002 - 27.01N, 90.03W - 2016-08-06 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_002)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_002_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_002_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_002/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_002.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_002&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_002
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_003.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_003 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_003.graph Profile - R4_x257_230_0019 - DP04_HS2_003 - 26.98N, 87.97W - 2016-08-09 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_003)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_003_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_003_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_003/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_003.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_003&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_003
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_005.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_005 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_005.graph Profile - R4_x257_230_0019 - DP04_HS2_005 - 27.02N, 87.18W - 2016-08-10 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_005)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_005_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_005_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_005/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_005.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_005&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_005
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_006.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_006 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_006.graph Profile - R4_x257_230_0019 - DP04_HS2_006 - 26.95N, 87.51W - 2016-08-11 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_006)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_006_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_006_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_006/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_006.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_006&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_006
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_007.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_007 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_007.graph Profile - R4_x257_230_0019 - DP04_HS2_007 - 26.96N, 88.50W - 2016-08-11 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_007)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_007_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_007_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_007/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_007.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_007&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_007
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_008.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_008 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_008.graph Profile - R4_x257_230_0019 - DP04_HS2_008 - 26.97N, 89.47W - 2016-08-12 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_008)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_008_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_008_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_008/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_008.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_008&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_008
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_009.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_009 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_009.graph Profile - R4_x257_230_0019 - DP04_HS2_009 - 27.52N, 89.01W - 2016-08-14 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_009)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_009_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_009_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_009/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_009.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_009&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_009
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_010.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_010 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_010.graph Profile - R4_x257_230_0019 - DP04_HS2_010 - 28.02N, 87.52W - 2016-08-16 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_010)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_010_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_010_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_010/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_010.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_010&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_010
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_011.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_011 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_011.graph Profile - R4_x257_230_0019 - DP04_HS2_011 - 28.50N, 87.50W - 2016-08-18 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_011)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_011_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_011_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_011/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_011.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_011&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_011
https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_012.subset https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_012 https://erddap.griidc.org/erddap/tabledap/R4_x257_230_0019_DP04_HS2_012.graph Profile - R4_x257_230_0019 - DP04_HS2_012 - 29.02N, 87.49W - 2016-08-19 Near surface fluorescence and optical scattering profiles at Conductivity, Temperature, Depth (CTD) sampling stations. Cruises DP03 and DP04 from January 2016 - December 2016. Optical absorption and scattering are the primary determinants of the flow of radiant energy in the ocean?s surface waters. Particles in the water are the principle source of scattering, and the scattering measurements can indicate the amount and/or type of particles present. While a complete measurement of the scattered light field is complex and cumbersome, a measurement of the backscattering at particular angles can usually be related to the total backscattering of light. The backscattering of light not only provides information about the particle present, it is important for understanding variations in Rrs.  We measure backscattering in the water with either a 2 channel (700 & 532nm at ~117?), 6 channel (442, 488,532,589,620, 680nm at ~140 deg), or 2 channel (420 & 700nm) scattering meter.  We synchronize this instrument with a chlorophyll and Colored Dissolved Organic Matter (CDOM) fluorometer, and lower them on an instrument frame through the upper portion of the water column to obtain vertical profiles of the in situ chl. and CDOM fluorescence, as well as the amount and spectral shape of the backscattering.  These profiles will be made at the CTD sampling stations, but instrument constraints will limit the depth of the profiles to <300m. This data was collected during the same cruise as GRIIDC CTD datasets R4.x257.230:00011 and R4.x257.230:0012\n\ncdm_data_type = Profile\nVARIABLES:\nprofile (DP04_HS2_012)\ntime (seconds since 1970-01-01T00:00:00Z)\ncruise (cruise number)\nlatitude (degrees_north)\nlongitude (degrees_east)\ncastID (Cast ID)\ndepth (m)\noptical_backscattering_420nm (Optical backscattering at 117 degree, 420nm optical_absorption_spectra_at_, 1/m)\noptical_backscattering_700nm (Optical backscattering at 117 degree, 700nm optical_absorption_spectra_at_, 1/m)\nfluorescence_at_700nm (Fluorescence at 700nm optical_absorption_spectra_at_, 1/m)\nCDOM_fluorescence (CDOM_measured_by_fluorescence, 1/m)\n... (5 more variables)\n https://erddap.griidc.org/erddap/metadata/fgdc/xml/R4_x257_230_0019_DP04_HS2_012_fgdc.xml https://erddap.griidc.org/erddap/metadata/iso19115/xml/R4_x257_230_0019_DP04_HS2_012_iso19115.xml https://erddap.griidc.org/erddap/info/R4_x257_230_0019_DP04_HS2_012/index.htmlTable https://data.gulfresearchinitiative.org/data/R4.x257.230:0019 (external link) https://erddap.griidc.org/erddap/rss/R4_x257_230_0019_DP04_HS2_012.rss https://erddap.griidc.org/erddap/subscriptions/add.html?datasetID=R4_x257_230_0019_DP04_HS2_012&showErrors=false&email= University of South Florida / College of Marine Science R4_x257_230_0019_DP04_HS2_012

 
ERDDAP, Version 2.02
Disclaimers | Privacy Policy | Contact