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          Title: 
            Regional Ocean Modeling System (ROMS): Main Hawaiian Islands
          Date: 
            Date: 
              Date: 
                Date: 
                  2010-06-01
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                Date_Type_Code: 
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        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. 
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        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 
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        PacIOOS provides timely, reliable, and accurate ocean information to 
        support a safe, clean, productive ocean and resilient coastal zone in 
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        The Pacific Islands Ocean Observing System (PacIOOS) is funded through 
        the National Oceanic and Atmospheric Administration (NOAA) as a 
        Regional Association within the U.S. Integrated Ocean Observing System 
        (IOOS). PacIOOS is coordinated by the University of Hawaii School of 
        Ocean and Earth Science and Technology (SOEST).
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            the data Contributor, University of Hawaii, PacIOOS, NOAA, State 
            of Hawaii nor the United States Government, nor any of their 
            employees or contractors, makes any warranty, express or implied, 
            including warranties of merchantability and fitness for a 
            particular purpose, or assumes any legal liability for the 
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        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 
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      Abstract: 
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        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, 
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      Abstract: 
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        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, 
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        region surrounding the main Hawaiian Islands at approximately 4-km 
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      Lineage: 
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            2015-05-28T00:00:00Z Model grid modified; aggregation now begins 
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            2024-03-27T20:08:00Z Dataset now begins at 2023-01-01T00:00:00Z.
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