-
Gulf of Mexico SSH Anomaly Grid - 2007
Since 1996, global, near-real-time maps of mesoscale anomalies derived from tandem sampling provided by altimeters aboard the Topography Experiment (TOPEX)/Poseidon and European... -
Gulf of Mexico SSH Anomaly Grid - 2008
Since 1996, global, near-real-time maps of mesoscale anomalies derived from tandem sampling provided by altimeters aboard the Topography Experiment (TOPEX)/Poseidon and European... -
Gulf of Mexico SSH Anomaly Grid - 2021
Since 1996, global, near-real-time maps of mesoscale anomalies derived from tandem sampling provided by altimeters aboard the Topography Experiment (TOPEX)/Poseidon and European... -
Gulf of Mexico SSH Anomaly Grid - 2010
Since 1996, global, near-real-time maps of mesoscale anomalies derived from tandem sampling provided by altimeters aboard the Topography Experiment (TOPEX)/Poseidon and European... -
Regional Ocean Modeling System (ROMS): Oregon Coast
Regional Ocean Modeling System (ROMS) 3-day, 4-hourly forecast for the Oregon coast at approximately 2-km resolution. While considerable effort has been made to implement all... -
CMOP Virtual Columbia River (SELFE); f33
Semi-implicit Eulerian-Lagrangian Finite Element (SELFE) model 3 day, 15 minute timestep forecast for the Columbia River estuary and near-field plume. Water levels and surface,... -
Tide Model for the Big Island of Hawaii
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... -
Near-Real Time Surface Ocean Velocity, Hawaii, 6 km Resolution
Surface ocean velocities estimated from HF-Radar (HFR) are representative of the upper 0.3 - 2.5 meters of the ocean. The main objective of near-real time processing is to... -
Tide Model (Barotropic) for the Pacific Basin
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... -
Tide Model for the Hawaiian Islands: Main NW Islands
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... -
Near-Real Time Surface Ocean Velocity, Hawaii, 1 km Resolution
Surface ocean velocities estimated from HF-Radar (HFR) are representative of the upper 0.3 - 2.5 meters of the ocean. The main objective of near-real time processing is to... -
Near-Real Time Surface Ocean Velocity, Hawaii, 2 km Resolution
Surface ocean velocities estimated from HF-Radar (HFR) are representative of the upper 0.3 - 2.5 meters of the ocean. The main objective of near-real time processing is to... -
Regional Ocean Modeling System (ROMS): Main Hawaiian Islands: Reanalysis
Regional Ocean Modeling System (ROMS) 3-hourly data assimilating reanalysis for the region surrounding the main Hawaiian Islands at approximately 4-km resolution. Boundary... -
OSU Chlorophyll Climatology, MODIS Aqua, West US, July 2002-June 2013
This suite of CHLA and SST climatology and anomaly data products are derived from daily, 0.0125 degree x 0.0125 degree, MODIS Aqua CHLA and SST fields that cover the California... -
OSU Chlorophyll Anomaly, MODIS Aqua, West US, July 2002-June 2014
This suite of CHLA and SST climatology and anomaly data products are derived from daily, 0.0125 degree x 0.0125 degree, MODIS Aqua CHLA and SST fields that cover the California... -
OSU SST Climatology, MODIS Aqua, West US, July 2002-June 2013
This suite of CHLA and SST climatology and anomaly data products are derived from daily, 0.0125 degree x 0.0125 degree, MODIS Aqua CHLA and SST fields that cover the California... -
OSU SST Anomaly, MODIS Aqua, West US, July 2002-June 2014
This suite of CHLA and SST climatology and anomaly data products are derived from daily, 0.0125 degree x 0.0125 degree, MODIS Aqua CHLA and SST fields that cover the California...