Easier access to scientific data
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ERDDAP
Easier access to scientific data |
| griddap | Subset | tabledap | Make A Graph | wms | files | Title | Summary | FGDC | ISO 19115 | Info | Background Info | RSS | Institution | Dataset ID | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| https://pae-paha.pacioos.hawaii.edu/erddap/tabledap/aco_adcp_vel | https://pae-paha.pacioos.hawaii.edu/erddap/tabledap/aco_adcp_vel.graph | ALOHA Cabled Observatory (ACO): Acoustic Doppler Current Profiler (ADCP): Velocity | The University of Hawaii's ALOHA (\"A Long-term Oligotrophic Habitat Assessment\") Cabled Observatory (ACO) is located 100 km north of the island of Oahu, Hawaii (22 45'N, 158W) in the North Pacific Ocean. It provides real-time oceanographic observations from a depth of about 4,800 m via a submarine fiber optic cable that comes ashore at Makaha on Oahu. This data set provides measurements of ocean current velocity at the ACO from a 250 kHz SonTek acoustic doppler current profiler (ADCP) at 1.83 m above the ocean bottom for the most recent 7 days. Velocities are flagged bad if the amplitude is excessively low or high. An amplitude is high if it exceeds the average of the ping before and the ping after by 20 counts. An amplitude is low if less than 6 counts. After this the velocities are flagged bad if the absolute deviation of the vertical velocity from its ensemble median exceeds 0.15 m/s or if its value is less than -0.25 m/s.\n\ncdm_data_type = Profile\nVARIABLES:\nstation_name\ntime (seconds since 1970-01-01T00:00:00Z)\ndepth (Depth of each location, m)\nlatitude (degrees_north)\nlongitude (degrees_east)\neastward_sea_water_velocity (current east component, meters/second)\nnorthward_sea_water_velocity (current north component, meters/second)\nupward_sea_water_velocity (current upward component, meters/second)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/aco_adcp_vel_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/aco_adcp_vel_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/aco_adcp_vel/index.htmlTable | http://aco-ssds.soest.hawaii.edu
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/aco_adcp_vel.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=aco_adcp_vel&showErrors=false&email= | University of Hawaii at Manoa | aco_adcp_vel | ||||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_marig | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_marig.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_marig/request | Regional Ocean Modeling System (ROMS): Guam: 3-D Variables | Regional Ocean Modeling System (ROMS) 6-day, 3-hourly forecast for the region surrounding Guam and parts of the Commonwealth of the Northern Mariana Islands (CNMI) at approximately 2-km resolution. Boundary conditions provided by the wider ROMS model for the region surrounding the Western North Pacific (roms_mari) at approximately 4-km resolution. Atmospheric forcing generated by the Weather Research and Forecasting (WRF) model for the region surrounding Guam and parts of the Commonwealth of the Northern Mariana Islands (CNMI) (wrf_guam) at approximately 3-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 3 days using all available observations to improve the model estimate of current ocean state (its nowcast) before forecasts are run. Assimilated observations may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; and in-situ water temperature and salinity profiles from ARGO floats. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_marig_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_marig_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_marig/index.htmlTable | https://www.pacioos.hawaii.edu/currents/model-mariana/
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_marig.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_marig&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_marig | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_hiig | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_hiig.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_hiig/request | Regional Ocean Modeling System (ROMS): Main Hawaiian Islands: 3-D Variables | Regional Ocean Modeling System (ROMS) 7-day, 3-hourly forecast for the region surrounding the main Hawaiian Islands at approximately 4-km resolution. Boundary conditions provided by the global, 1/12-degree (~9-km) HYbrid Coordinate Ocean Model (HYCOM). Atmospheric forcing generated by the Weather Research and Forecasting (WRF) model for the region surrounding the main Hawaiian Islands (wrf_hi) at approximately 6-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 3 days using all available observations to improve the model estimate of current ocean state (its nowcast) before forecasts are run. Assimilated observations may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; surface currents from PacIOOS high-frequency radios (HFR); and in-situ water temperature and salinity profiles from ARGO floats and ocean glider autonomous underwater vehicles (AUV). While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_hiig_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_hiig_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_hiig/index.htmlTable | https://www.pacioos.hawaii.edu/currents/model-hawaii/
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_hiig.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_hiig&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_hiig | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_hiig_assim | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_hiig_assim.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_hiig_assim/request | Regional Ocean Modeling System (ROMS): Main Hawaiian Islands: Data Assimilating: 3-D Variables | Regional Ocean Modeling System (ROMS) 3-day, 3-hourly data assimilating hindcast for the region surrounding the main Hawaiian Islands at approximately 4-km resolution. Boundary conditions provided by the global, 1/12-degree (~9-km) HYbrid Coordinate Ocean Model (HYCOM). Atmospheric forcing generated by the Weather Research and Forecasting (WRF) model for the region surrounding the main Hawaiian Islands (wrf_hi) at approximately 6-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 3 days using all available observations to improve the model estimate of current ocean state (its nowcast). Assimilated observations may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; surface currents from PacIOOS high-frequency radios (HFR); and in-situ water temperature and salinity profiles from ARGO floats and ocean glider autonomous underwater vehicles (AUV). While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_hiig_assim_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_hiig_assim_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_hiig_assim/index.htmlTable | https://www.pacioos.hawaii.edu/metadata/roms_hiig_assim.html
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_hiig_assim.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_hiig_assim&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_hiig_assim | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_hiig_reanalysis | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_hiig_reanalysis.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_hiig_reanalysis/request | Regional Ocean Modeling System (ROMS): Main Hawaiian Islands: Reanalysis: 3-D Variables | Regional Ocean Modeling System (ROMS) 3-hourly data assimilating reanalysis for the region surrounding the main Hawaiian Islands at approximately 4-km resolution. Boundary conditions provided by the global, 1/12-degree (~9-km) HYbrid Coordinate Ocean Model (HYCOM). Atmospheric forcing generated by the Weather Research and Forecasting (WRF) model for the region surrounding the main Hawaiian Islands (wrf_hi) at approximately 6-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 3 days using all available observations to improve the model estimate of current ocean state (its nowcast). Assimilated observations may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; surface currents from PacIOOS high-frequency radios (HFR); and in-situ water temperature and salinity profiles from ARGO floats and ocean glider autonomous underwater vehicles (AUV). While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_hiig_reanalysis_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_hiig_reanalysis_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_hiig_reanalysis/index.htmlTable | https://doi.org/10.5194/gmd-2018-98
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_hiig_reanalysis.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_hiig_reanalysis&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_hiig_reanalysis | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_hiomsg | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_hiomsg.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_hiomsg/request | Regional Ocean Modeling System (ROMS): Oahu South Shore: 3-D Variables | Regional Ocean Modeling System (ROMS) 3-day, 3-hourly forecast for the region surrounding the south shore of the island of Oahu at approximately 200-m resolution. Boundary conditions provided by the wider ROMS model for the region surrounding the island of Oahu (roms_hiog) at approximately 1-km resolution. Atmospheric forcing generated by the Weather Research and Forecasting (WRF) model for the region surrounding the island of Oahu (wrf_oa) at approximately 1.5-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 3 days using all available observations to improve the model estimate of current ocean state (its nowcast) before forecasts are run. Assimilated observations may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; surface currents from PacIOOS high-frequency radios (HFR); and in-situ water temperature and salinity profiles from ARGO floats and ocean glider autonomous underwater vehicles (AUV). While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_hiomsg_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_hiomsg_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_hiomsg/index.htmlTable | https://www.pacioos.hawaii.edu/currents/model-southoahu/
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_hiomsg.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_hiomsg&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_hiomsg | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_samoa | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_samoa.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_samoa/request | Regional Ocean Modeling System (ROMS): Samoa: 3-D Variables | Regional Ocean Modeling System (ROMS) 7-day, 3-hourly forecast for the region surrounding the islands of Samoa at approximately 3-km resolution. Boundary conditions provided by the global, 1/12-degree (~9-km) HYbrid Coordinate Ocean Model (HYCOM). Atmospheric forcing generated by the Weather Research and Forecasting (WRF) model for the region surrounding the islands of Samoa (wrf_samoa) at approximately 3-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 3 days using all available observations to improve the model estimate of current ocean state (its nowcast) before forecasts are run. Assimilated observations may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; and in-situ water temperature and salinity profiles from ARGO floats. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_samoa_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_samoa_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_samoa/index.htmlTable | https://www.pacioos.hawaii.edu/currents/model-samoa/
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_samoa.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_samoa&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_samoa | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_samoa_assim | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_samoa_assim.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_samoa_assim/request | Regional Ocean Modeling System (ROMS): Samoa: Data Assimilating: 3-D Variables | Regional Ocean Modeling System (ROMS) 3-day, 3-hourly data assimilating hindcast for the region surrounding the islands of Samoa at approximately 3-km resolution. Boundary conditions provided by the global, 1/12-degree (~9-km) HYbrid Coordinate Ocean Model (HYCOM). Atmospheric forcing generated by the Weather Research and Forecasting (WRF) model for the region surrounding the islands of Samoa (wrf_samoa) at approximately 3-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 3 days using all available observations to improve the model estimate of current ocean state (its nowcast). Assimilated observations may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; and in-situ water temperature and salinity profiles from ARGO floats. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_samoa_assim_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_samoa_assim_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_samoa_assim/index.htmlTable | https://www.pacioos.hawaii.edu/metadata/roms_samoa_assim.html
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_samoa_assim.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_samoa_assim&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_samoa_assim | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_wpac | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_wpac.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_wpac/request | Regional Ocean Modeling System (ROMS): Western North Pacific: 3-D Variables | Regional Ocean Modeling System (ROMS) 7-day, 3-hourly forecast for the region surrounding the Western North Pacific at approximately 8-km resolution. Boundary conditions provided by the global, 1/12-degree (~9-km) HYbrid Coordinate Ocean Model (HYCOM). Atmospheric forcing generated by the NOAA/NCEP Global Forecast System (GFS) model for the region surrounding the Western North Pacific at approximately 25-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 5 days using all available observations to improve the model estimate of current ocean state (its nowcast) before forecasts are run. Assimilated observations are collected independently of PacIOOS and may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; surface currents around Palau from CORDC High Frequency Radars (HFR), Scripps Institute of Oceanography; and in-situ water temperature and salinity profiles from ARGO floats. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_wpac_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_wpac_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_wpac/index.htmlTable | https://www.pacioos.hawaii.edu/currents/model-wnpacific/
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_wpac.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_wpac&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_wpac | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_wpac_assim | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/roms_wpac_assim.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/roms_wpac_assim/request | Regional Ocean Modeling System (ROMS): Western North Pacific: Data Assimilating: 3-D Variables | Regional Ocean Modeling System (ROMS) 5-day, 3-hourly data assimilating hindcast for the region surrounding the Western North Pacific at approximately 8-km resolution. Boundary conditions provided by the global, 1/12-degree (~9-km) HYbrid Coordinate Ocean Model (HYCOM). Atmospheric forcing generated by the NOAA/NCEP Global Forecast System (GFS) model for the region surrounding the Western North Pacific at approximately 25-km resolution. Tide forcing uses the Oregon State University (OSU) Tidal Prediction Software (OTPS) TOPEX/Poseidon global inverse solution (TPXO) to derive barotropic tidal elevation and velocity. Data are assimilated over the previous 5 days using all available observations to improve the model estimate of current ocean state (its nowcast). Assimilated observations are collected independently of PacIOOS and may include satellite-based sea surface temperatures from MODIS, AVHRR, or OSTIA; satellite-based sea surface height from AVISO; surface currents around Palau from CORDC High Frequency Radars (HFR), Scripps Institute of Oceanography; and in-situ water temperature and salinity profiles from ARGO floats. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use these data with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\ntemp (potential temperature, Celsius)\nsalt (salinity, 1e-3)\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/roms_wpac_assim_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/roms_wpac_assim_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/roms_wpac_assim/index.htmlTable | https://www.pacioos.hawaii.edu/metadata/roms_wpac_assim.html
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/roms_wpac_assim.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=roms_wpac_assim&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | roms_wpac_assim | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/scud_pac | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/scud_pac.graph | Surface CUrrents from a Diagnostic model (SCUD): Pacific | The SCUD data product is an estimate of upper-ocean velocities computed from a diagnostic model (Surface CUrrents from a Diagnostic model). This model makes daily estimates of ocean currents by combining geostrophic and Ekman currents. The estimate is computed through derived coefficients such that the results best match ocean drifting buoys. The currents therefore are a best-estimate of currents at 15 meters (drifting buoys are drogued at 15 meters). The dataset is intended to diagnose trajectories of a tracer floating near the surface such as marine debris, oil spills, etc. The data are provided on a 1/4-degree grid for the Pacific.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nu (sea water velocity: eastward component, meter second-1)\nv (sea water velocity: northward component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/scud_pac_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/scud_pac_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/scud_pac/index.htmlTable | http://apdrc.soest.hawaii.edu/projects/SCUD/
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/scud_pac.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=scud_pac&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | scud_pac | ||||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/scud_pac_lon180 | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/scud_pac_lon180.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/scud_pac_lon180/request | Surface CUrrents from a Diagnostic model (SCUD): Pacific, Lon+/-180 | The SCUD data product is an estimate of upper-ocean velocities computed from a diagnostic model (Surface CUrrents from a Diagnostic model). This model makes daily estimates of ocean currents by combining geostrophic and Ekman currents. The estimate is computed through derived coefficients such that the results best match ocean drifting buoys. The currents therefore are a best-estimate of currents at 15 meters (drifting buoys are drogued at 15 meters). The dataset is intended to diagnose trajectories of a tracer floating near the surface such as marine debris, oil spills, etc. The data are provided on a 1/4-degree grid for the Pacific.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][latitude][longitude]):\nu (sea water velocity: eastward component, meter second-1)\nv (sea water velocity: northward component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/scud_pac_lon180_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/scud_pac_lon180_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/scud_pac_lon180/index.htmlTable | http://apdrc.soest.hawaii.edu/projects/SCUD/
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/scud_pac_lon180.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=scud_pac_lon180&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | scud_pac_lon180 | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/tide_pac_vel | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/tide_pac_vel.graph | Tide Model (Barotropic) for the Pacific Ocean: Tidal Velocity | Barotropic tide model for the Pacific Ocean. The model is based on harmonics distributed by Oregon State University (OSU) and assimilates satellite altimetry data from TOPEX/Poseidon. It was generated using OSU Tidal Prediction Software (OTPS), modified locally by J. Potemra, using barotropic inverse tidal solutions from OSU. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use this output with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/tide_pac_vel_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/tide_pac_vel_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/tide_pac_vel/index.htmlTable | http://volkov.oce.orst.edu/tides/PO.html
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/tide_pac_vel.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=tide_pac_vel&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | tide_pac_vel | ||||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/tide_pac_vel_lon180 | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/tide_pac_vel_lon180.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/tide_pac_vel_lon180/request | Tide Model (Barotropic) for the Pacific Ocean: Tidal Velocity, Lon+/-180 | Barotropic tide model for the Pacific Ocean. The model is based on harmonics distributed by Oregon State University (OSU) and assimilates satellite altimetry data from TOPEX/Poseidon. It was generated using OSU Tidal Prediction Software (OTPS), modified locally by J. Potemra, using barotropic inverse tidal solutions from OSU. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use this output with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth][latitude][longitude]):\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/tide_pac_vel_lon180_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/tide_pac_vel_lon180_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/tide_pac_vel_lon180/index.htmlTable | http://volkov.oce.orst.edu/tides/PO.html
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/tide_pac_vel_lon180.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=tide_pac_vel_lon180&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | tide_pac_vel_lon180 | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/tide_bi_vel | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/tide_bi_vel.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/tide_bi_vel/request | Tide Model for the Big Island of Hawaii: Tidal Velocity | Tide model for the Big Island of Hawaii. The model is based on climatological stratification, but 64 harmonics are used to model the full-depth baroclinic tides. The model has been run at 1km resolution, hourly, through the end of 2024. Due to computing limitations, the model grid is divided into two pieces, one for the Northwestern main Hawaiian Islands (Kauai, Oahu, Maui) and the other for the Big Island. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use this output with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth_percent][latitude][longitude]):\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/tide_bi_vel_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/tide_bi_vel_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/tide_bi_vel/index.htmlTable | http://apdrc.soest.hawaii.edu/doc/carteretal_revised_pp.pdf
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/tide_bi_vel.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=tide_bi_vel&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | tide_bi_vel | |||
| https://pae-paha.pacioos.hawaii.edu/erddap/griddap/tide_mhi_vel | https://pae-paha.pacioos.hawaii.edu/erddap/griddap/tide_mhi_vel.graph | https://pae-paha.pacioos.hawaii.edu/erddap/wms/tide_mhi_vel/request | Tide Model for the Hawaiian Islands: Main NW Islands: Tidal Velocity | Tide model for the Hawaiian Islands. The model is based on climatological stratification, but 64 harmonics are used to model the full-depth baroclinic tides. The model has been run at 1km resolution, hourly, through the end of 2024. Due to computing limitations, the model grid is divided into two pieces, one for the Northwestern main Hawaiian Islands (Kauai, Oahu, Maui) and the other for the Big Island. While considerable effort has been made to implement all model components in a thorough, correct, and accurate manner, numerous sources of error are possible. As such, please use this output with the caution appropriate for any ocean related activity.\n\ncdm_data_type = Grid\nVARIABLES (all of which use the dimensions [time][depth_percent][latitude][longitude]):\nu (u-velocity component, meter second-1)\nv (v-velocity component, meter second-1)\n | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/fgdc/xml/tide_mhi_vel_fgdc.xml | https://pae-paha.pacioos.hawaii.edu/erddap/metadata/iso19115/xml/tide_mhi_vel_iso19115.xml | https://pae-paha.pacioos.hawaii.edu/erddap/info/tide_mhi_vel/index.htmlTable | http://apdrc.soest.hawaii.edu/doc/carteretal_revised_pp.pdf
| https://pae-paha.pacioos.hawaii.edu/erddap/rss/tide_mhi_vel.rss | https://pae-paha.pacioos.hawaii.edu/erddap/subscriptions/add.html?datasetID=tide_mhi_vel&showErrors=false&email= | Pacific Islands Ocean Observing System (PacIOOS) | tide_mhi_vel |