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/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/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 2025. 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 2025. 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 |