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Federal
WaveWatch III (WW3) Global Wave Model 16 recent views
National Oceanic and Atmospheric Administration, Department of Commerce —
Through a collaborative effort with NOAA/NCEP and NWS Honolulu, the University of Hawaii has implemented a global-scale WaveWatch III (WW3) 7-day model with a 5-day... -
Federal
Near-Real Time Surface Ocean Velocity, Hawaii, 6 km Resolution 11 recent views
National Oceanic and Atmospheric Administration, Department of Commerce —
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... -
Federal
NOAA Coral Reef Watch Operational Daily Near-Real-Time Global 5-km Satellite Coral Bleaching Monitoring Products
National Oceanic and Atmospheric Administration, Department of Commerce —
Contains the most recent 3 years of a suite of NOAA Coral Reef Watch (CRW) version 3.1 operational global satellite coral bleaching heat stress monitoring products at... -
Federal
Weather Research and Forecasting (WRF) Regional Atmospheric Model: Oahu
National Oceanic and Atmospheric Administration, Department of Commerce —
Weather Research and Forecasting (WRF) mesoscale numerical weather prediction model 3.5-day hourly forecast for the region surrounding the Hawaiian island of Oahu at... -
Federal
Tide Model (Barotropic) for the Pacific Basin
National Oceanic and Atmospheric Administration, Department of Commerce —
Barotropic tide model for the Pacific Ocean. The model is based on harmonics distributed by Oregon State University (OSU) and assimilates satellite altimetry data... -
Federal
Tide Model for the Hawaiian Islands: Main NW Islands
National Oceanic and Atmospheric Administration, Department of Commerce —
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... -
Federal
Tide Model for the Big Island of Hawaii
National Oceanic and Atmospheric Administration, Department of Commerce —
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... -
Federal
Near-Real Time Surface Ocean Velocity, Hawaii, 1 km Resolution
National Oceanic and Atmospheric Administration, Department of Commerce —
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... -
Federal
Near-Real Time Surface Ocean Velocity, Hawaii, 2 km Resolution
National Oceanic and Atmospheric Administration, Department of Commerce —
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... -
Federal
WaveWatch III (WW3) Northwestern Hawaiian Islands (NWHI) Regional Wave Model
National Oceanic and Atmospheric Administration, Department of Commerce —
Through a collaborative effort with NOAA/NCEP and NWS Honolulu, the University of Hawaii has implemented a global-scale WaveWatch III (WW3) model (ww3_global), which... -
Federal
WaveWatch III (WW3) Hawaii Regional Wave Model
National Oceanic and Atmospheric Administration, Department of Commerce —
Through a collaborative effort with NOAA/NCEP and NWS Honolulu, the University of Hawaii has implemented a global-scale WaveWatch III (WW3) model (ww3_global), which... -
Federal
Simulating WAves Nearshore (SWAN) Regional Wave Model: Kauai
National Oceanic and Atmospheric Administration, Department of Commerce —
Simulating WAves Nearshore (SWAN) regional wave model 7-day output with a 5-day hourly forecast for the Hawaiian islands of Kauai and Niihau at approximately 500-m... -
Federal
NOAA Coral Reef Watch Daily Global 5-km Satellite Monitoring Marine Heatwave Watch
National Oceanic and Atmospheric Administration, Department of Commerce —
Marine heatwaves are modelled off their terrestrial namesakes and are prolonged periods of anomalously high sea surface temperature (SST). In effect, they are...