Easier access to scientific data
Brought to you by NOAA NMFS SWFSC ERD
|
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 | Institution | Dataset ID | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_clim_lwr_absolute | https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_clim_lwr_absolute.graph | NOBS for TAO OceanSITES flux data Absolute Wind Speed and LWR climatology | Number of Observations for Tropical Atmosphere/Ocean (TAO) OceanSITES flux data Absolute Wind Speed and LWR climatology\n\ncdm_data_type = Other\nVARIABLES:\ntime (seconds since 1970-01-01T00:00:00Z)\nsite_code\nQLAT\nQSEN\nQRAIN\nSWNET\nWZS\nTAU\nTAUX (Surface Downward Eastward Stress)\nTAUY (Surface Downward Northward Stress)\nTDIR\nRAIN\nEVAP\nEMP\nFLUX_QC\nFLUX_DM\nwmo_platform_code\n | https://data.pmel.noaa.gov/pmel/erddap/info/tao_flux_clim_lwr_absolute/index.htmlTable | https://www.pmel.noaa.gov/gtmba
| https://data.pmel.noaa.gov/pmel/erddap/rss/tao_flux_clim_lwr_absolute.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=tao_flux_clim_lwr_absolute&showErrors=false&email= | NOAA/PMEL/SDIG | tao_flux_clim_lwr_absolute | ||||||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_clim_lwr_relative.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_clim_lwr_relative | https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_clim_lwr_relative.graph | NOBS for TAO OceanSITES flux data Relative Wind Speed and LWR climatology | Monthly Number of Observastions for Tropical Atmosphere/Ocean (TAO) OceanSITES flux data Relative Wind Speed and LWR climatology\n\ncdm_data_type = Other\nVARIABLES:\ntime (seconds since 1970-01-01T00:00:00Z)\nsite_code\nQLAT\nQSEN\nQRAIN\nSWNET\nWZS\nTAU\nTAUX (Surface Downward Eastward Stress)\nTAUY (Surface Downward Northward Stress)\nTDIR\nRAIN\nEVAP\nEMP\nFLUX_QC\nFLUX_DM\nWAVE_DOMINANT_PERIOD (Sea Surface Swell Wave Period)\nWAVE_SIGNIFICANT_HEIGHT (Sea Surface Wave Significant Height)\nwmo_platform_code\n | https://data.pmel.noaa.gov/pmel/erddap/info/tao_flux_clim_lwr_relative/index.htmlTable | https://www.pmel.noaa.gov/gtmba
| https://data.pmel.noaa.gov/pmel/erddap/rss/tao_flux_clim_lwr_relative.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=tao_flux_clim_lwr_relative&showErrors=false&email= | NOAA/PMEL/SDIG | tao_flux_clim_lwr_relative | |||||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_absolute | https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_absolute.graph | NOBS for TAO OceanSITES flux data with LWR and Absolute Wind Speed | Monthly Number of Observations for Tropical Atmosphere/Ocean (TAO) OceanSITES flux data with LWR and Absolute Wind Speed\n\ncdm_data_type = Other\nVARIABLES:\ntime (seconds since 1970-01-01T00:00:00Z)\nsite_code\nQLAT\nQSEN\nQRAIN\nQNET (Net Diabatic Heating)\nLWNET\nSWNET\nWZS\nTAU\nTAUX (Surface Downward Eastward Stress)\nTAUY (Surface Downward Northward Stress)\nTDIR\nRAIN\nEVAP\nEMP\nFLUX_QC\nFLUX_DM\nwmo_platform_code\n | https://data.pmel.noaa.gov/pmel/erddap/info/tao_flux_absolute/index.htmlTable | https://www.pmel.noaa.gov/gtmba
| https://data.pmel.noaa.gov/pmel/erddap/rss/tao_flux_absolute.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=tao_flux_absolute&showErrors=false&email= | NOAA/PMEL/SDIG | tao_flux_absolute | ||||||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_relative | https://data.pmel.noaa.gov/pmel/erddap/tabledap/tao_flux_relative.graph | NOBS for TAO OceanSITES flux data with LWR and Relative Wind Speed | Monthly Number of Observations for Tropical Atmosphere/Ocean (TAO) OceanSITES flux data with LWR and Relative Wind Speed\n\ncdm_data_type = Other\nVARIABLES:\ntime (seconds since 1970-01-01T00:00:00Z)\nsite_code\nQLAT\nQSEN\nQRAIN\nQNET (Net Diabatic Heating)\nLWNET\nSWNET\nWZS\nTAU\nTAUX (Surface Downward Eastward Stress)\nTAUY (Surface Downward Northward Stress)\nTDIR\nRAIN\nEVAP\nEMP\nFLUX_QC\nFLUX_DM\nwmo_platform_code\n | https://data.pmel.noaa.gov/pmel/erddap/info/tao_flux_relative/index.htmlTable | https://www.pmel.noaa.gov/gtmba
| https://data.pmel.noaa.gov/pmel/erddap/rss/tao_flux_relative.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=tao_flux_relative&showErrors=false&email= | NOAA/PMEL/SDIG | tao_flux_relative | ||||||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1005_2017.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1005_2017 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1005_2017.graph | Saildrone PMEL TPOS 2017 Mission, drone 1005 | This file contains the real time data from the Saildrone core sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2017 Mission (Mission 1) to the eastern tropical Pacific (10N, 125W and 0, 125W). These data have not been Quality Control (QC)�d. This was the first of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Mr. Nathan Anderson contributed to the metadata creation. The PMEL TPOS 2017 Mission (aka Mission 1) had two Gen-4 Saildrones, each with a full atmospheric and ocean core sensor suite, an Acoustic Doppler Current Profiler (ADCP), and an ASVCO2 carbon flux and pH system. The two drones were deployed out of Alameda, CA on September 1, 2017 for a mission in the equatorial Pacific. After sailing near the CCE1 mooring off coastal California, the drones proceeded to the area near 10N, 125W. They remained in the area from October 18 - November 13, 2017 to participate in the Salinity Processes in the Upper Ocean Regional Study (SPURS)-2 field study, which included side-by-side data acquisition with a Woods Hole Oceanographic Institution (WHOI) buoy, and the R/V REVELLE. When SPURS-2 ended, the drones sailed south on either side of 125W, stopping for comparisons against Tropical Atmosphere/Ocean (TAO) moorings at 8N, 5N, and 2N. After crossing the equator, the drones returned to California. SD-1005 was recovered in San Luis Obispo Bay on May 6, 2018. SD-1006 was recovered from San Francisco Bay on May 18, 2018.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\nlatitude (degrees_north)\ntime (seconds since 1970-01-01T00:00:00Z)\nTEMP_O2_STDDEV (Seawater temperature SD, degree_C)\nSW_UNMASKED_IRRAD_CENTER_MEAN (Shortwave total radiation measured by unmasked center detector, W m-2)\nCHLOR_MEAN (Chlorophyll concentration, microgram L-1)\nRH_MEAN (Relative humidity, percent)\nLW_IRRAD_MEAN (Longwave downwelling radiation, W m-2)\nCDOM_MEAN (CDOM concentration, ppb)\n... (49 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1005_2017_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1005_2017_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1005_2017/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1005_2017.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1005_2017&showErrors=false&email= | NOAA/PMEL | sd1005_2017 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1006_2017.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1006_2017 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1006_2017.graph | Saildrone PMEL TPOS 2017 Mission, drone 1006 | This file contains the real time data from the Saildrone core sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2017 Mission (Mission 1) to the eastern tropical Pacific (10N, 125W and 0, 125W). These data have not been Quality Control (QC)�d. This was the first of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Mr. Nathan Anderson contributed to the metadata creation. The PMEL TPOS 2017 Mission (aka Mission 1) had two Gen-4 Saildrones, each with a full atmospheric and ocean core sensor suite, an Acoustic Doppler Current Profiler (ADCP), and an ASVCO2 carbon flux and pH system. The two drones were deployed out of Alameda, CA on September 1, 2017 for a mission in the equatorial Pacific. After sailing near the CCE1 mooring off coastal California, the drones proceeded to the area near 10N, 125W. They remained in the area from October 18 - November 13, 2017 to participate in the Salinity Processes in the Upper Ocean Regional Study (SPURS)-2 field study, which included side-by-side data acquisition with a Woods Hole Oceanographic Institution (WHOI) buoy, and the R/V REVELLE. When SPURS-2 ended, the drones sailed south on either side of 125W, stopping for comparisons against Tropical Atmosphere/Ocean (TAO) moorings at 8N, 5N, and 2N. After crossing the equator, the drones returned to California. SD-1005 was recovered in San Luis Obispo Bay on May 6, 2018. SD-1006 was recovered from San Francisco Bay on May 18, 2018.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\nlatitude (degrees_north)\ntime (seconds since 1970-01-01T00:00:00Z)\nTEMP_O2_STDDEV (Seawater temperature SD, degree_C)\nSW_UNMASKED_IRRAD_CENTER_MEAN (Shortwave total radiation measured by unmasked center detector, W m-2)\nCHLOR_MEAN (Chlorophyll concentration, microgram L-1)\nRH_MEAN (Relative humidity, percent)\nLW_IRRAD_MEAN (Longwave downwelling radiation, W m-2)\nCDOM_MEAN (CDOM concentration, ppb)\n... (49 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1006_2017_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1006_2017_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1006_2017/index.htmlTable | http://saildrone.com/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1006_2017.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1006_2017&showErrors=false&email= | NOAA/PMEL | sd1006_2017 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1005_2018.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1005_2018 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1005_2018.graph | Saildrone PMEL TPOS 2018 Mission, drone 1005 | This file contains the real time data from the Saildrone core sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2018 Mission (Mission 2) to the central equatorial Pacific (0, 140W). These data have not been Quality Control (QC)�d. This was the second of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Mr. Nathan Anderson contributed to the metadata creation. PMEL TPOS 2018 Mission (aka Mission 2) had four Saildrones: SD1005 and SD1006 were Gen 4 drones, and SD1029 and SD1030 were Gen 5 drones equipped with a larger wing designed for equatorial work. The drones were each equipped with full atmospheric and ocean core sensor suite, and an Acoustic Doppler Current Profiler (ADCP) (not included in this file). SD1029 & SD1030 also carried shortwave and longwave radiation (included in core set) and an ASVCO2 carbon flux and pH system; these carbon data are served in a separate file. SD1029 had 3 strap-on SBE56 temperature sensors (at 0.35m, 1.16m, and 1.72m) to study the near-surface stratification. For the Gen5 drones, the core Conductivity, Temperature, Depth (CTD) was an RBR located in the flowthrough tunnel in the keel. The carbon system also had an independent prawler CTD that is higher quality than the RBR. The vehicles were deployed out of Honolulu, HI on October 3, 2018. After sailing near a PMEL Carbon mooring in Kaneohe Bay, HI, the drones proceeded to the Tropical Atmosphere/Ocean (TAO) mooring at 9N, 140W. Three drones completed a circuit around the mooring, and then began their transit south towards the equator. Two drones made it to the equator and sailed near the TAO moorings at 0, 140W. Navigation issues caused the mission to be aborted early (mid-December 2018), before further science tasks could be completed. Three Saildrones were recovered in Honolulu on 01-27-19. SD1030 was recovered in HI later in the spring of 2019.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\ntime (time in seconds, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nSOG (Speed over ground, m s-1)\n... (48 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1005_2018_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1005_2018_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1005_2018/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1005_2018.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1005_2018&showErrors=false&email= | NOAA/PMEL | sd1005_2018 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1006_2018.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1006_2018 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1006_2018.graph | Saildrone PMEL TPOS 2018 Mission, drone 1006 | This file contains the real time data from the Saildrone core sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2018 Mission (Mission 2) to the central equatorial Pacific (0, 140W). These data have not been Quality Control (QC)�d. This was the second of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Mr. Nathan Anderson contributed to the metadata creation. PMEL TPOS 2018 Mission (aka Mission 2) had four Saildrones: SD1005 and SD1006 were Gen 4 drones, and SD1029 and SD1030 were Gen 5 drones equipped with a larger wing designed for equatorial work. The drones were each equipped with full atmospheric and ocean core sensor suite, and an Acoustic Doppler Current Profiler (ADCP) (not included in this file). SD1029 & SD1030 also carried shortwave and longwave radiation (included in core set) and an ASVCO2 carbon flux and pH system; these carbon data are served in a separate file. SD1029 had 3 strap-on SBE56 temperature sensors (at 0.35m, 1.16m, and 1.72m) to study the near-surface stratification. For the Gen5 drones, the core Conductivity, Temperature, Depth (CTD) was an RBR located in the flowthrough tunnel in the keel. The carbon system also had an independent prawler CTD that is higher quality than the RBR. The vehicles were deployed out of Honolulu, HI on October 3, 2018. After sailing near a PMEL Carbon mooring in Kaneohe Bay, HI, the drones proceeded to the Tropical Atmosphere/Ocean (TAO) mooring at 9N, 140W. Three drones completed a circuit around the mooring, and then began their transit south towards the equator. Two drones made it to the equator and sailed near the TAO moorings at 0, 140W. Navigation issues caused the mission to be aborted early (mid-December 2018), before further science tasks could be completed. Three Saildrones were recovered in Honolulu on 01-27-19. SD1030 was recovered in HI later in the spring of 2019.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\ntime (time in seconds, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nSOG (Speed over ground, m s-1)\n... (48 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1006_2018_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1006_2018_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1006_2018/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1006_2018.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1006_2018&showErrors=false&email= | NOAA/PMEL | sd1006_2018 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1029_2018.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1029_2018 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1029_2018.graph | Saildrone PMEL TPOS 2018 Mission, drone 1029 | This file contains the real time data from the Saildrone core sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2018 Mission (Mission 2) to the central equatorial Pacific (0, 140W). These data have not been Quality Control (QC)�d. This was the second of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Mr. Nathan Anderson contributed to the metadata creation. PMEL TPOS 2018 Mission (aka Mission 2) had four Saildrones: SD1005 and SD1006 were Gen 4 drones, and SD1029 and SD1030 were Gen 5 drones equipped with a larger wing designed for equatorial work. The drones were each equipped with full atmospheric and ocean core sensor suite, and an Acoustic Doppler Current Profiler (ADCP) (not included in this file). SD1029 & SD1030 also carried shortwave and longwave radiation (included in core set) and an ASVCO2 carbon flux and pH system; these carbon data are served in a separate file. SD1029 had 3 strap-on SBE56 temperature sensors (at 0.35m, 1.16m, and 1.72m) to study the near-surface stratification. For the Gen5 drones, the core Conductivity, Temperature, Depth (CTD) was an RBR located in the flowthrough tunnel in the keel. The carbon system also had an independent prawler CTD that is higher quality than the RBR. The vehicles were deployed out of Honolulu, HI on October 3, 2018. After sailing near a PMEL Carbon mooring in Kaneohe Bay, HI, the drones proceeded to the Tropical Atmosphere/Ocean (TAO) mooring at 9N, 140W. Three drones completed a circuit around the mooring, and then began their transit south towards the equator. Two drones made it to the equator and sailed near the TAO moorings at 0, 140W. Navigation issues caused the mission to be aborted early (mid-December 2018), before further science tasks could be completed. Three Saildrones were recovered in Honolulu on 01-27-19. SD1030 was recovered in HI later in the spring of 2019.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\ntime (time in seconds, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nSOG (Speed over ground, m s-1)\n... (60 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1029_2018_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1029_2018_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1029_2018/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1029_2018.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1029_2018&showErrors=false&email= | NOAA/PMEL | sd1029_2018 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1030_2018.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1030_2018 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1030_2018.graph | Saildrone PMEL TPOS 2018 Mission, drone 1030 | This file contains the real time data from the Saildrone core sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2018 Mission (Mission 2) to the central equatorial Pacific (0, 140W). These data have not been Quality Control (QC)�d. This was the second of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Mr. Nathan Anderson contributed to the metadata creation. PMEL TPOS 2018 Mission (aka Mission 2) had four Saildrones: SD1005 and SD1006 were Gen 4 drones, and SD1029 and SD1030 were Gen 5 drones equipped with a larger wing designed for equatorial work. The drones were each equipped with full atmospheric and ocean core sensor suite, and an Acoustic Doppler Current Profiler (ADCP) (not included in this file). SD1029 & SD1030 also carried shortwave and longwave radiation (included in core set) and an ASVCO2 carbon flux and pH system; these carbon data are served in a separate file. SD1029 had 3 strap-on SBE56 temperature sensors (at 0.35m, 1.16m, and 1.72m) to study the near-surface stratification. For the Gen5 drones, the core Conductivity, Temperature, Depth (CTD) was an RBR located in the flowthrough tunnel in the keel. The carbon system also had an independent prawler CTD that is higher quality than the RBR. The vehicles were deployed out of Honolulu, HI on October 3, 2018. After sailing near a PMEL Carbon mooring in Kaneohe Bay, HI, the drones proceeded to the Tropical Atmosphere/Ocean (TAO) mooring at 9N, 140W. Three drones completed a circuit around the mooring, and then began their transit south towards the equator. Two drones made it to the equator and sailed near the TAO moorings at 0, 140W. Navigation issues caused the mission to be aborted early (mid-December 2018), before further science tasks could be completed. Three Saildrones were recovered in Honolulu on 01-27-19. SD1030 was recovered in HI later in the spring of 2019.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\ntime (time in seconds, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nSOG (Speed over ground, m s-1)\n... (62 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1030_2018_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1030_2018_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1030_2018/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1030_2018.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1030_2018&showErrors=false&email= | NOAA/PMEL | sd1030_2018 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1066_2019.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1066_2019 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1066_2019.graph | Saildrone PMEL TPOS 2019 Mission, drone 1066 | This file contains the real time data from the Saildrone core MetOcean sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2019 Mission (�Mission 3�) to the central equatorial Pacific (0, 140W). These data have not been Quality Control (QC)'d. This was the third of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Dr. Samantha Wills (UW JISAO) was a postdoctoral fellow with the project, acting as a PI and Mission Manager during this mission. Mr. Nathan Anderson contributed to the metadata creation. PMEL TPOS 2019 Mission (aka Mission 3) had four Saildrones: SD1066, SD1067, SD1068 and SD1069. All were standard Gen 5 drones (but with copper paint), with standard wings � not the large wings used in Mission 2. All had an Acoustic Doppler Current Profiler (ADCP) (not included in this file) and the core MetOcean package. The core CTDs were an RBR in the flowthrough tunnel in the keel and a pumped SBE37 at the outflow of the flowthrough tunnel. In addition, SD1066 and SD1067 had ASVCO2 carbon flux and pH system, a SPN1 shielded shortwave radiometer, and an Eppley longwave radiometer. Carbon system data (including its prawler Conductivity, Temperature, Depth (CTD) data) are served through a separate file. The vehicles were deployed out of Honolulu, HI on 9 June 2019. After performing ADCP bottom track testing on Penguin Bank, the drones proceeded to WHOTS for an intercomparison. On 17 June 2019, SD 1067 returned to shore for servicing. Following its ADCP bottom tracking tested again, on 20 June 2019 all 4 drones began their transit to the Tropical Atmosphere/Ocean (TAO) mooring at 9N, 140W, and then south towards the equator. In addition to intercomparisons against the 0N, 140W TAO buoy, several experiments were performed to survey scales of variability in the equatorial region and the structure of the cold tongue front. An experiment in the InterTropical Convergence Zone (ITCZ) was then performed before returning to Hawaii for a final intercomparison against the WHOTS mooring, a newly deployed PMEL test TELOS surface mooring and test PRAWLER mooring which carried a test Z-Cell ADCP on its bridal. The mission ended on December 20, 2019. All four Saildrones were recovered in Honolulu in early January 2020.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\n... (102 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1066_2019_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1066_2019_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1066_2019/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1066_2019.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1066_2019&showErrors=false&email= | NOAA/PMEL | sd1066_2019 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1067_2019.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1067_2019 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1067_2019.graph | Saildrone PMEL TPOS 2019 Mission, drone 1067 | This file contains the real time data from the Saildrone core MetOcean sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2019 Mission (�Mission 3�) to the central equatorial Pacific (0, 140W). These data have not been Quality Control (QC)'d. This was the third of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Dr. Samantha Wills (UW JISAO) was a postdoctoral fellow with the project, acting as a PI and Mission Manager during this mission. Mr. Nathan Anderson contributed to the metadata creation. PMEL TPOS 2019 Mission (aka Mission 3) had four Saildrones: SD1066, SD1067, SD1068 and SD1069. All were standard Gen 5 drones (but with copper paint), with standard wings � not the large wings used in Mission 2. All had an Acoustic Doppler Current Profiler (ADCP) (not included in this file) and the core MetOcean package. The core CTDs were an RBR in the flowthrough tunnel in the keel and a pumped SBE37 at the outflow of the flowthrough tunnel. In addition, SD1066 and SD1067 had ASVCO2 carbon flux and pH system, a SPN1 shielded shortwave radiometer, and an Eppley longwave radiometer. Carbon system data (including its prawler Conductivity, Temperature, Depth (CTD) data) are served through a separate file. The vehicles were deployed out of Honolulu, HI on 9 June 2019. After performing ADCP bottom track testing on Penguin Bank, the drones proceeded to WHOTS for an intercomparison. On 17 June 2019, SD 1067 returned to shore for servicing. Following its ADCP bottom tracking tested again, on 20 June 2019 all 4 drones began their transit to the Tropical Atmosphere/Ocean (TAO) mooring at 9N, 140W, and then south towards the equator. In addition to intercomparisons against the 0N, 140W TAO buoy, several experiments were performed to survey scales of variability in the equatorial region and the structure of the cold tongue front. An experiment in the InterTropical Convergence Zone (ITCZ) was then performed before returning to Hawaii for a final intercomparison against the WHOTS mooring, a newly deployed PMEL test TELOS surface mooring and test PRAWLER mooring which carried a test Z-Cell ADCP on its bridal. The mission ended on December 20, 2019. All four Saildrones were recovered in Honolulu in early January 2020.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\n... (102 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1067_2019_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1067_2019_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1067_2019/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1067_2019.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1067_2019&showErrors=false&email= | NOAA/PMEL | sd1067_2019 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1068_2019.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1068_2019 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1068_2019.graph | Saildrone PMEL TPOS 2019 Mission, drone 1068 | This file contains the real time data from the Saildrone core MetOcean sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2019 Mission (�Mission 3�) to the central equatorial Pacific (0, 140W). These data have not been Quality Control (QC)'d. This was the third of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Dr. Samantha Wills (UW JISAO) was a postdoctoral fellow with the project, acting as a PI and Mission Manager during this mission. Mr. Nathan Anderson contributed to the metadata creation. PMEL TPOS 2019 Mission (aka Mission 3) had four Saildrones: SD1066, SD1067, SD1068 and SD1069. All were standard Gen 5 drones (but with copper paint), with standard wings � not the large wings used in Mission 2. All had an Acoustic Doppler Current Profiler (ADCP) (not included in this file) and the core MetOcean package. The core CTDs were an RBR in the flowthrough tunnel in the keel and a pumped SBE37 at the outflow of the flowthrough tunnel. In addition, SD1066 and SD1067 had ASVCO2 carbon flux and pH system, a SPN1 shielded shortwave radiometer, and an Eppley longwave radiometer. Carbon system data (including its prawler Conductivity, Temperature, Depth (CTD) data) are served through a separate file. The vehicles were deployed out of Honolulu, HI on 9 June 2019. After performing ADCP bottom track testing on Penguin Bank, the drones proceeded to WHOTS for an intercomparison. On 17 June 2019, SD 1067 returned to shore for servicing. Following its ADCP bottom tracking tested again, on 20 June 2019 all 4 drones began their transit to the Tropical Atmosphere/Ocean (TAO) mooring at 9N, 140W, and then south towards the equator. In addition to intercomparisons against the 0N, 140W TAO buoy, several experiments were performed to survey scales of variability in the equatorial region and the structure of the cold tongue front. An experiment in the InterTropical Convergence Zone (ITCZ) was then performed before returning to Hawaii for a final intercomparison against the WHOTS mooring, a newly deployed PMEL test TELOS surface mooring and test PRAWLER mooring which carried a test Z-Cell ADCP on its bridal. The mission ended on December 20, 2019. All four Saildrones were recovered in Honolulu in early January 2020.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\n... (94 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1068_2019_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1068_2019_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1068_2019/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1068_2019.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1068_2019&showErrors=false&email= | NOAA/PMEL | sd1068_2019 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1069_2019.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1069_2019 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1069_2019.graph | Saildrone PMEL TPOS 2019 Mission, drone 1069 | This file contains the real time data from the Saildrone core MetOcean sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2019 Mission (�Mission 3�) to the central equatorial Pacific (0, 140W). These data have not been Quality Control (QC)'d. This was the third of three missions funded by NOAA Office of Oceanic and Atmospheric Research (OAR)/CPO/GOMO and NOAA/OMAO as a pilot study for the Tropical Pacific Observing System (TPOS)-2020 project. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Joint Institue for the Study of Atmoshere and Ocean (JISAO)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Dr. Samantha Wills (UW JISAO) was a postdoctoral fellow with the project, acting as a PI and Mission Manager during this mission. Mr. Nathan Anderson contributed to the metadata creation. PMEL TPOS 2019 Mission (aka Mission 3) had four Saildrones: SD1066, SD1067, SD1068 and SD1069. All were standard Gen 5 drones (but with copper paint), with standard wings � not the large wings used in Mission 2. All had an Acoustic Doppler Current Profiler (ADCP) (not included in this file) and the core MetOcean package. The core CTDs were an RBR in the flowthrough tunnel in the keel and a pumped SBE37 at the outflow of the flowthrough tunnel. In addition, SD1066 and SD1067 had ASVCO2 carbon flux and pH system, a SPN1 shielded shortwave radiometer, and an Eppley longwave radiometer. Carbon system data (including its prawler Conductivity, Temperature, Depth (CTD) data) are served through a separate file. The vehicles were deployed out of Honolulu, HI on 9 June 2019. After performing ADCP bottom track testing on Penguin Bank, the drones proceeded to WHOTS for an intercomparison. On 17 June 2019, SD 1067 returned to shore for servicing. Following its ADCP bottom tracking tested again, on 20 June 2019 all 4 drones began their transit to the Tropical Atmosphere/Ocean (TAO) mooring at 9N, 140W, and then south towards the equator. In addition to intercomparisons against the 0N, 140W TAO buoy, several experiments were performed to survey scales of variability in the equatorial region and the structure of the cold tongue front. An experiment in the InterTropical Convergence Zone (ITCZ) was then performed before returning to Hawaii for a final intercomparison against the WHOTS mooring, a newly deployed PMEL test TELOS surface mooring and test PRAWLER mooring which carried a test Z-Cell ADCP on its bridal. The mission ended on December 20, 2019. All four Saildrones were recovered in Honolulu in early January 2020.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\n... (94 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1069_2019_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1069_2019_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1069_2019/index.htmlTable | https://www.pmel.noaa.gov/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1069_2019.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1069_2019&showErrors=false&email= | NOAA/PMEL | sd1069_2019 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1065_tpos_2021.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1065_tpos_2021 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1065_tpos_2021.graph | Saildrone PMEL TPOS 2021 Mission, drone 1065 | This file contains data from the Saildrone core MetOcean sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2021 Mission (Mission 4) to the eastern tropical Pacific hurricane genesis region near 10N - 15N, 110W, the near-equatorial Cold Tongue region between 110W - 125W, and the region south of the equator where an Intertropical Convergence Zone (ITCZ) sometimes forms. These data have not been Quality Control (QC)'d. This mission was funded in part by NOAA OMAO and NOAA National Ocean Partnership Program (NOPP) to continue USV observations as part of the Tropical Pacific Observing System (TPOS), with a focus on air-sea heat and momentum exchanges, carbon dioxide fluxes, preconditions for storm activity, and hurricane genesis, which affects moisture transport and rainfall along the west coast of North America in a region undersampled by the existing mooring array. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang, and Dr. Samantha Wills (UW Cooperative Institute for Climate, Ocean, and Ecosystem Studies (UW CICOES), Dr. Adrienne Sutton, Mr. Christian Meinig, and Eugene Burger (all NOAA PMEL), Dr. Yolande Serra (UW/CICOES), Dr. Avichal Mehra (NOAA National Centers for Environmental Prediction (NCEP)), Karen Grissom (NOAA National Data Buoy Center (NDBC)), and Dr. Eric Lindstrom (Saildrone, Inc). Drs. Samantha Wills and Dongxiao Zhang acted as Mission Managers during this mission. Mr. Nathan Anderson (UW CICOES) contributed to the metadata creation. The PMEL TPOS 2021 Mission (aka Mission 4) had two Saildrones: SD1065 and SD1066. Both were standard Gen 6 drones, with an Acoustic Doppler Current Profiler (ADCP) at 1.86m (not included in this file) and the core MetOcean package. The core CTD was an SBE 37-SMP at 1.54m, with an auxiliary SBE prawler at 0.62m and 3x SBE56 T sensors at 0.33m, 0.5m, and 1.03m. Both SD1065 and SD1066 had an ASVCO2 carbon flux and pH system, an SPN1 shielded shortwave radiometer, and an Eppley longwave radiometer. Carbon system data (including its prawler Conductivity, Temperature, Depth (CTD) data) are served through a separate file. The vehicles for the 2021 mission were deployed out of San Francisco Bay, CA on 23 July 2021, transiting to the eastern tropical Pacific, where they spent 160 days collecting data. The drones encountered rough seas associated with Tropical Depression Marty, forcing them into storm mode for several days before entering the hurricane genesis study region. The drones then proceeded south along the 110W Tropical Atmosphere/Ocean (TAO) mooring line, completing two intercomparisons at the 8N, 110W and 5N, 110W TAO buoys. The drones also sampled the strong meridional Sea Surface Temperature (SST) front separating the warm waters of the northern hemisphere ITCZ from the cold waters of the equatorial Cold Tongue. The drones became separated en route to the equatorial study region due to strong easterly ocean currents, with SD1065 eventually crossing the Equator to survey the southern hemisphere double ITCZ regime. The mission ended in the field on 17 February, 2022, with SD1065 positioned near 8S, 117W and SD1066 positioned near 1N, 130W.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\n... (81 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1065_tpos_2021_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1065_tpos_2021_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1065_tpos_2021/index.htmlTable | https://saildrone.com/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1065_tpos_2021.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1065_tpos_2021&showErrors=false&email= | NOAA/PMEL | sd1065_tpos_2021 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1066_tpos_2021.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1066_tpos_2021 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1066_tpos_2021.graph | Saildrone PMEL TPOS 2021 Mission, drone 1066 | This file contains data from the Saildrone core MetOcean sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2021 Mission (Mission 4) to the eastern tropical Pacific hurricane genesis region near 10N - 15N, 110W, the near-equatorial Cold Tongue region between 110W - 125W, and the region south of the equator where an Intertropical Convergence Zone (ITCZ) sometimes forms. These data have not been Quality Control (QC)'d. This mission was funded in part by NOAA OMAO and NOAA National Ocean Partnership Program (NOPP) to continue USV observations as part of the Tropical Pacific Observing System (TPOS), with a focus on air-sea heat and momentum exchanges, carbon dioxide fluxes, preconditions for storm activity, and hurricane genesis, which affects moisture transport and rainfall along the west coast of North America in a region undersampled by the existing mooring array. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang, and Dr. Samantha Wills (UW Cooperative Institute for Climate, Ocean, and Ecosystem Studies (UW CICOES), Dr. Adrienne Sutton, Mr. Christian Meinig, and Eugene Burger (all NOAA PMEL), Dr. Yolande Serra (UW/CICOES), Dr. Avichal Mehra (NOAA National Centers for Environmental Prediction (NCEP)), Karen Grissom (NOAA National Data Buoy Center (NDBC)), and Dr. Eric Lindstrom (Saildrone, Inc). Drs. Samantha Wills and Dongxiao Zhang acted as Mission Managers during this mission. Mr. Nathan Anderson (UW CICOES) contributed to the metadata creation. The PMEL TPOS 2021 Mission (aka Mission 4) had two Saildrones: SD1065 and SD1066. Both were standard Gen 6 drones, with an Acoustic Doppler Current Profiler (ADCP) at 1.86m (not included in this file) and the core MetOcean package. The core CTD was an SBE 37-SMP at 1.54m, with an auxiliary SBE prawler at 0.62m and 3x SBE56 T sensors at 0.33m, 0.5m, and 1.03m. Both SD1065 and SD1066 had an ASVCO2 carbon flux and pH system, an SPN1 shielded shortwave radiometer, and an Eppley longwave radiometer. Carbon system data (including its prawler Conductivity, Temperature, Depth (CTD) data) are served through a separate file. The vehicles for the 2021 mission were deployed out of San Francisco Bay, CA on 23 July 2021, transiting to the eastern tropical Pacific, where they spent 160 days collecting data. The drones encountered rough seas associated with Tropical Depression Marty, forcing them into storm mode for several days before entering the hurricane genesis study region. The drones then proceeded south along the 110W Tropical Atmosphere/Ocean (TAO) mooring line, completing two intercomparisons at the 8N, 110W and 5N, 110W TAO buoys. The drones also sampled the strong meridional Sea Surface Temperature (SST) front separating the warm waters of the northern hemisphere ITCZ from the cold waters of the equatorial Cold Tongue. The drones became separated en route to the equatorial study region due to strong easterly ocean currents, with SD1065 eventually crossing the Equator to survey the southern hemisphere double ITCZ regime. The mission ended in the field on 17 February, 2022, with SD1065 positioned near 8S, 117W and SD1066 positioned near 1N, 130W.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\n... (75 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1066_tpos_2021_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1066_tpos_2021_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1066_tpos_2021/index.htmlTable | https://saildrone.com/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1066_tpos_2021.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1066_tpos_2021&showErrors=false&email= | NOAA/PMEL | sd1066_tpos_2021 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1052_tpos_2022.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1052_tpos_2022 | https://data.pmel.noaa.gov/pmel/erddap/tabledap/sd1052_tpos_2022.graph | Saildrone PMEL TPOS 2022 Mission, drone 1052 | This file contains data from the Saildrone core MetOcean sensors for the Pacific Marine Environmental Laboratory (PMEL) TPOS 2022 Mission (Mission 5) to the eastern tropical Pacific along the 125W meridian. These data have not been Quality Control (QC)'d. This mission was funded by NOAA OMAO to continue USV observations as part of the Tropical Pacific Observing System (TPOS), with a focus on observing air-sea interaction processes and CO2 fluxes associated with the predicted rare 3rd consecutive La Niña, Tropical Instability Waves, and high frequency eddy and frontal variability between the Equatorial Cold Tongue and the Intertropical Convergence Zone. The PIs were Dr. Meghan Cronin (NOAA PMEL), Dr. Dongxiao Zhang (UW Cooperative Institute for Climate, Ocean, and Ecosystem Studies (UW CICOES)), Dr. Adrienne Sutton (NOAA PMEL), and Mr. Christian Meinig (NOAA PMEL). Dr. Samantha Wills (UW CICOES) was a research scientist with the project, acting as a co-PI and Mission Manager during this mission. Mr. Nathan Anderson (UW CICOES) contributed to the metadata creation. The PMEL TPOS 2022 Mission (aka Mission 5) had two Saildrones: SD1033 and SD1052. Both were standard Gen 6 drones, with an Acoustic Doppler Current Profiler (ADCP) at 1.86m (not included in this file) and the core MetOcean package. The core CTD was an SBE 37-SMP at 1.54m, with an auxiliary SBE prawler at 0.62m and 3x SBE56 T sensors at 0.33m, 0.5m, and 1.03m. Both SD1065 and SD1066 had an ASVCO2 carbon flux and pH system, an SPN1 shielded shortwave radiometer, and an Eppley longwave radiometer. Carbon system data (including its prawler Conductivity, Temperature, Depth (CTD) data) are served through a separate file. The vehicles for the 2022 mission were deployed out of San Francisco Bay, CA in early May 2022, arriving on station to initiate the mission on 22 June 2022. The 90-day mission ended 22 Sept 2022.\n\ncdm_data_type = Trajectory\nVARIABLES:\ntrajectory (Trajectory/Drone ID)\ntime (time in seconds, seconds since 1970-01-01T00:00:00Z)\nlatitude (degrees_north)\nlongitude (degrees_east)\nSOG (Speed over ground, m s-1)\nSOG_FILTERED_MEAN (Speed over ground one minute mean, m s-1)\nSOG_FILTERED_STDDEV (Speed over ground one minute stddev, m s-1)\nSOG_FILTERED_MAX (Speed over ground one minute max, m s-1)\n... (69 more variables)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/sd1052_tpos_2022_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/sd1052_tpos_2022_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/sd1052_tpos_2022/index.htmlTable | https://saildrone.com/
| https://data.pmel.noaa.gov/pmel/erddap/rss/sd1052_tpos_2022.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=sd1052_tpos_2022&showErrors=false&email= | NOAA PMEL | sd1052_tpos_2022 | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyIso.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyIso | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyIso.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1977-present, 20C Isotherm Depth | This dataset has daily 20C Isotherm Depth data (the depth at which the ocean temperature is 20C) from the \nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nISO_6 (20C Isotherm Depth, m)\nQI_5006 (20C Depth Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyIso_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyIso_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyIso/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyIso.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyIso&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyIso | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyAirt.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyAirt | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyAirt.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1977-present, Air Temperature | This dataset has daily Air Temperature data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nAT_21 (Air Temperature, degree_C)\nQAT_5021 (Air Temperature Quality)\nSAT_6021 (Air Temperature Source)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyAirt_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyAirt_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyAirt/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyAirt.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyAirt&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyAirt | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyCur.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyCur | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyCur.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1977-present, Currents | This dataset has daily Currents data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nU_320 (Eastward Sea Water Velocity, cm s-1)\nV_321 (Northward Sea Water Velocity, cm s-1)\nCS_300 (Sea Water Velocity, cm s-1)\nCD_310 (Direction of Sea Water Velocity, degrees_true)\nQCS_5300 (Current Speed Quality)\nQCD_5310 (Current Direction Quality)\nSCS_6300 (Current Speed Source)\nCIC_7300 (Current Instrument Code)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyCur_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyCur_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyCur/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyCur.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyCur&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyCur | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySst.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySst | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySst.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1977-present, Sea Surface Temperature | This dataset has daily Sea Surface Temperature (SST) data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nT_25 (Sea Surface Temperature, degree_C)\nQT_5025 (Sea Surface Temperature Quality)\nST_6025 (Sea Surface Temperature Source)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDySst_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDySst_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDySst/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDySst.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDySst&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDySst | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyT.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyT | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyT.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1977-present, Temperature | This dataset has daily Temperature data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nT_20 (Sea Water Temperature, degree_C)\nQT_5020 (Temperature Quality)\nST_6020 (Temperature Source)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyT_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyT_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyT/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyT.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyT&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyT | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyW.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyW | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyW.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1977-present, Wind | This dataset has daily Wind data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nWU_422 (Zonal Wind, m s-1)\nWV_423 (Meridional Wind, m s-1)\nWS_401 (Wind Speed, m s-1)\nQWS_5401 (Wind Speed Quality)\nSWS_6401 (Wind Speed Source)\nWD_410 (Wind Direction, degrees_true)\nQWD_5410 (Wind Direction Quality)\nSWD_6410 (Wind Direction Source)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyW_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyW_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyW/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyW.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyW&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyW | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyDyn.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyDyn | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyDyn.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1980-present, Dynamic Height | This dataset has daily Dynamic Height data (a measure of the elevation of the sea level, calculated by integrating the specific volume anomaly of the sea water between the sea surface and 500 m depth) from the \nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nDYN_13 (Dynamic Height, dyn-cm)\nQD_5013 (Dynamic Height Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyDyn_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyDyn_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyDyn/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyDyn.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyDyn&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyDyn | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyHeat.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyHeat | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyHeat.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1980-present, Heat Content | This dataset has daily Heat Content data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nHTC_130 (Heat Content, 10**10 J m-2)\nHTC_5130 (Heat Content Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyHeat_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyHeat_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyHeat/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyHeat.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyHeat&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyHeat | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyPos.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyPos | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyPos.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1980-present, Position | This dataset has daily Position data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nLON_502 (Precise Longitude, degree_east)\nQX_5502 (Longitude Quality)\nLAT_500 (Precise Latitude, degree_north)\nQY_5500 (Latitude Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyPos_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyPos_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyPos/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyPos.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyPos&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyPos | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyD.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyD | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyD.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1987-present, Potential Density Anomaly | This dataset has daily Potential Density Anomaly (sigma-theta) data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nSTH_71 (Sigma-Theta, kg m-3)\nQST_5071 (Sigma-Theta Quality)\nSST_6071 (Sigma-Theta Source)\nDIC_7071 (Sigma-Theta Instrument Code)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyD_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyD_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyD/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyD.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyD&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyD | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyS.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyS | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyS.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1987-present, Salinity | This dataset has daily Salinity data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nS_41 (Sea Water Practical Salinity, PSU)\nQS_5041 (Salinity Quality)\nSS_6041 (Salinity Source)\nSIC_8041 (Salinity Instrument Code)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyS_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyS_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyS/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyS.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyS&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyS | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyAdcp.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyAdcp | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyAdcp.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1988-2020, ADCP | This dataset has daily Acoustic Doppler Current Profiler (ADCP) water currents data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. ADCP data are available only after mooring recoveries, which are scheduled on an annual basis. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nu_1205 (Eastward Sea Water Velocity, cm/s)\nQU_5205 (Eastward Sea Water Velocity Quality)\nv_1206 (Northward Sea Water Velocity, cm/s)\nQV_5206 (Northward Sea Water Velocity Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyAdcp_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyAdcp_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyAdcp/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyAdcp.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyAdcp&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyAdcp | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyEvap.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyEvap | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyEvap.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1989-present, Evaporation | This dataset has daily Evaporation data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nE_250 (Evaporation, MM/HR)\nQE_5250 (Evaporation Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyEvap_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyEvap_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyEvap/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyEvap.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyEvap&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyEvap | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQlat.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQlat | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQlat.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1989-present, Latent Heat Flux | This dataset has daily Latent Heat Flux data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nQL_137 (Latent Heat Flux, W m-2)\nQQL_5137 (Latent Heat Flux Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyQlat_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyQlat_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyQlat/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyQlat.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyQlat&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyQlat | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRh.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRh | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRh.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1989-present, Relative Humidity | This dataset has daily Relative Humidity data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nRH_910 (Relative Humidity, percent)\nQRH_5910 (Relative Humidity Quality)\nSRH_6910 (Relative Humidity Source)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyRh_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyRh_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyRh/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyRh.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyRh&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyRh | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQsen.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQsen | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQsen.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1989-present, Sensible Heat Flux | This dataset has daily Sensible Heat Flux data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nQS_138 (Sensible Heat Flux, W m-2)\nQQS_5138 (Sensible Heat Flux Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyQsen_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyQsen_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyQsen/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyQsen.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyQsen&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyQsen | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyTau.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyTau | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyTau.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1989-present, Wind Stress | This dataset has daily Wind Stress data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nTX_442 (Zonal Wind Stress, N/m2)\nTY_443 (Meridional Wind Stress, N/m2)\nTAU_440 (Wind Stress, N/m2)\nTD_445 (Wind Stress Direction, degrees_true)\nQTAU_5440 (Wind Stress Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyTau_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyTau_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyTau/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyTau.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyTau&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyTau | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRad.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRad | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRad.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1991-present, Downgoing Shortwave Radiation | This dataset has daily Downgoing Shortwave Radiation data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nRD_495 (Downgoing Shortwave Radiation, W/M**2)\nQSW_5495 (Shortwave Radiation Quality)\nSSW_6495 (Shortwave Radiation Source)\nRDS_496 (Shortwave Radiation Standard Deviation, W/M**2)\nRDP_497 (Shortwave Radiation Peak, W/M**2)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyRad_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyRad_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyRad/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyRad.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyRad&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyRad | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySwnet.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySwnet | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySwnet.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1991-present, Net Shortwave Radiation | This dataset has daily Net Shortwave Radiation data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nSWN_1495 (Net Shortwave Radiation, W/M**2)\nQSW_5495 (Shortwave Radiation Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDySwnet_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDySwnet_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDySwnet/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDySwnet.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDySwnet&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDySwnet | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySss.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySss | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySss.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1992-present, Sea Surface Salinity | This dataset has daily Sea Surface Salinity data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nS_41 (Sea Water Practical Salinity, PSU)\nQS_5041 (Salinity Quality)\nSS_6041 (Salinity Source)\nSIC_7041 (Salinity Instrument Code)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDySss_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDySss_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDySss/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDySss.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDySss&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDySss | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySsd.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySsd | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDySsd.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1992-present, Sigma-Theta | This dataset has daily Sigma-Theta (Potential Density Anomaly) data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nSTH_71 (Sigma-Theta, kg m-3)\nQST_5071 (Sigma-Theta Quality)\nSST_6071 (Sigma-Theta Source)\nDIC_7071 (Sigma-Theta Instrument Code)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDySsd_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDySsd_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDySsd/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDySsd.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDySsd&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDySsd | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyEmp.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyEmp | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyEmp.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1997-present, Evaporation Minus Precipitation | This dataset has daily Evaporation Minus Precipitation data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nEMP_251 (Evaporation Minus Precipitation, mm/hr)\nQEMP_5251 (Evaporation Minus Precipitation Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyEmp_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyEmp_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyEmp/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyEmp.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyEmp&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyEmp | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRf.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRf | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRf.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1997-present, Heat Flux Due To Rain | This dataset has daily Heat Flux Due To Rain data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nQR_139 (Heat Flux Due To Rain, W m-2)\nQQR_5139 (Heat Flux Due To Rain Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyRf_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyRf_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyRf/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyRf.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyRf&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyRf | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRain.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRain | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyRain.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1997-present, Precipitation | This dataset has daily Precipitation data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nRN_485 (Precipitation, MM/HR)\nQRN_5485 (Precipitation Quality)\nSRN_6485 (Precipitation Source)\nRNS_486 (Precipitation Standard Deviation, MM/HR)\nRNP_487 (Percent Time Raining, percent)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyRain_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyRain_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyRain/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyRain.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyRain&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyRain | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyBp.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyBp | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyBp.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 1998-present, Barometric (Air) Pressure | This dataset has daily Barometric (Air) Pressure data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nBP_915 (Barometric (Air) Pressure, hPa)\nQBP_5915 (Barometric (Air) Pressure Quality)\nSBP_6915 (Barometric (Air) Pressure Source)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyBp_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyBp_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyBp/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyBp.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyBp&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyBp | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyBf.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyBf | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyBf.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 2000-present, Buoyancy Flux | This dataset has daily Buoyancy Flux data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nBF_191 (Buoyancy Flux, 10**6 kg m-2 s-1)\nQBF_5191 (Buoyancy Flux Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyBf_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyBf_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyBf/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyBf.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyBf&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyBf | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyLw.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyLw | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyLw.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 2000-present, Longwave Radiation | This dataset has daily Incoming Longwave Radiation data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nQl_136 (Incoming Longwave Radiation, W m-2)\nQLW_5136 (Longwave Radiation Quality)\nSLW_6136 (Longwave Radiation Source)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyLw_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyLw_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyLw/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyLw.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyLw&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyLw | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyLwnet.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyLwnet | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyLwnet.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 2000-present, Net Longwave Radiation | This dataset has daily Net Longwave Radiation data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nLWN_1136 (Net Longwave Radiation, W m-2)\nQLW_5136 (Longwave Radiation Quality)\nSLW_6136 (Longwave Radiation Source)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyLwnet_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyLwnet_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyLwnet/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyLwnet.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyLwnet&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyLwnet | |||
| https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQnet.subset | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQnet | https://data.pmel.noaa.gov/pmel/erddap/tabledap/pmelTaoDyQnet.graph | TAO/TRITON, RAMA, and PIRATA Buoys, Daily, 2000-present, Total Heat Flux | This dataset has daily Total Heat Flux data from the\nTAO/TRITON (Pacific Ocean, https://www.pmel.noaa.gov/gtmba/ ),\nRAMA (Indian Ocean, https://www.pmel.noaa.gov/gtmba/pmel-theme/indian-ocean-rama ), and\nPIRATA (Atlantic Ocean, https://www.pmel.noaa.gov/gtmba/pirata/ )\narrays of moored buoys which transmit oceanographic and meteorological data to shore in real-time via the Argos satellite system. These buoys are major components of the CLIVAR climate analysis project and the GOOS, GCOS, and GEOSS observing systems. Daily averages are computed starting at 00:00Z and are assigned an observation 'time' of 12:00Z. For more information, see\nhttps://www.pmel.noaa.gov/gtmba/mission .\n\ncdm_data_type = TimeSeries\nVARIABLES:\narray\nstation\nwmo_platform_code\nlongitude (Nominal Longitude, degrees_east)\nlatitude (Nominal Latitude, degrees_north)\ntime (Centered Time, seconds since 1970-01-01T00:00:00Z)\ndepth (m)\nQT_210 (Total Heat Flux, W/M**2)\nQQ0_5210 (Total Heat Flux Quality)\n | https://data.pmel.noaa.gov/pmel/erddap/metadata/fgdc/xml/pmelTaoDyQnet_fgdc.xml | https://data.pmel.noaa.gov/pmel/erddap/metadata/iso19115/xml/pmelTaoDyQnet_iso19115.xml | https://data.pmel.noaa.gov/pmel/erddap/info/pmelTaoDyQnet/index.htmlTable | https://www.pmel.noaa.gov/gtmba/mission
| https://data.pmel.noaa.gov/pmel/erddap/rss/pmelTaoDyQnet.rss | https://data.pmel.noaa.gov/pmel/erddap/subscriptions/add.html?datasetID=pmelTaoDyQnet&showErrors=false&email= | NOAA PMEL, TAO/TRITON, RAMA, PIRATA | pmelTaoDyQnet |