Process_Description:
The data are presented by geographic areas bounded by model grids which were nested within a common global grid. All process steps apply to all data and geographic areas. Download and rewriting of General Circulation Model (GCM)wind (near-surface 10-m height) and sea-ice fields. Specific GCM variants used were as follows: CMCC winds: CMCC-CM2-VHR4_hist-1950_r1i1p1f1_gn (historical time-period) and CMCC-CM2-VHR4_highres-future_r1i1p1f1_gn (projected time-period), 6-hourly, 25 km resolution, CMCC sea-ice: CMCC-CM2-VHR4_hist-1950_r1i1p1f1_gn (historical time-period) and CMCC-CM2-VHR4_highres-future_r1i1p1f1_gn (projected time-period), daily, 25 km resolution, CNRM winds: CNRM-CM6-1-HR_historical_r1i1p1f2_gr (historical time-period)and CNRM-CM6-1-HR_ssp585_r1i1p1f2_gr (projected time-period), 3-hourly, 25 km resolution, CNRM sea-ice: CNRM-CM6-1-HR_historical_r1i1p1f2_gn (historical time-period) and CNRM-CM6-1-HR_ssp585_r1i1p1f2_gn (projected time-period), daily, 25 km resolution, ECEARTH winds: EC-Earth3P-HR_hist1950_r1i1p2f1_gr (historical time-period) and EC-Earth3P-HR_highres-future_r1i1p2f1_gr (projected time-period) 3-hourly, 50 km resolution, ECEARTH sea-ice: EC-Earth3P-HR_hist1950_r1i1p2f1_gn (historical time-period) and EC-Earth3P-HR_highres-future_r1i1p2f1_gn (projected time-period), daily, 25 km resolution, GFDL winds: GFDL-CM4C192_highresSST-present_r1i1p1f1_gr3 (historical time-period) and GFDL-CM4C192_highresSST-future_r1i1p1f1_gr3 (projected time-period), 3-hourly, 50 km resolution, GFDL sea-ice: input4MIPs_SSTsAndSeaIce_HighResMIP_MOHC-HadISST-2-2-0-0-0_gn (historical time-period), GFDL-CM4_ssp585_r1i1p1f1_gr2 (projected time-period), daily, 25 km resolution, HadgemHH winds: HadGEM3-GC31-HH_hist-1950_r1i1p1f1_gn (historical time-period) and HadGEM3-GC31-HH_highres-future_r1i1p1f1_gn (projected time-period), 3-hourly, 50 km resolution. HadgemHH sea-ice: HadGEM3-GC31-HM_hist-1950_r1i1p1f1_gn (historical time-period) and HadGEM3-GC31-HM_highres-future_r1i1p1f1_gn (projected time-period), daily, 25 km resolution, HadgemHM winds: HadGEM3-GC31-HM_hist-1950_r1i1p1f1_gn (historical time-period) and HadGEM3-GC31-HM_highres-future_r1i1p1f1_gn (projected time-period), 3-hourly, 50 km resolution, HadgemHM sea-ice: HadGEM3-GC31-HM_hist-1950-r1i1p1f1_gn (historical time-period) and HadGEM3-GC31-HM_highres-future_r1i1p1f1_gn(projected time-period), daily, 25 km resolution, HadgemSST winds: HadGEM3-GC31-HM_highresSST-present_r1i1p1f1_gn (historical time-period) and HadGEM3-GC31-HM_highresSST-future_r1i1p1f1_gn (projected time-period), forced atmosphere experiment using SST/sea ice derived from CMIP5 RCP8.5, 3-hourly, 50 km resolution. HadgemSST sea-ice: HadGEM3-GC31-HM_highresSST-present_r1i1p1f1_gn (historical time-period) and HadGEM3-GC31-HM_highresSST-future_r1i1p1f1_gn (projected time-period), daily, 25 km resolution native grid. The near-surface wind fields and sea-ice cover were downloaded from ESGF CMIP6 Data Holdings (pcmdi.llnl.gov/CMIP6) in March 2021 (June 2021 for CMCC), and they were interpolated to common 3-hourly time-points and grid resolutions of 0.5 degrees for GFDL and CNRM, 0.35 degrees for Hadgem and ECEARTH, and 0.3125 degrees for CMCC. All data were written to netCDF format files ingestible by the wave model. The GCM wind and ice fields are part of the High-Resolution Model Intercomparison Project (HighResMIP, Haarsma and others, 2016). The primary goal of HighResMIP is to assess the robustness of improvements in the representation of important climate processes with weather-resolving global model resolutions, using the physical climate system only with constrained aerosol forcing (Eyring and others, 2016). The higher resolution and inclusion of more forcings and detailed physics is expected to reduce bias compared to the standard CMIP6 and CMIP5 predecessor.
Source_Used_Citation_Abbreviation:
CMCC, CNRM projected, CNRM historical, EC-Earth, GFDL wind and projected sea-ice concentrations, GFDL historical sea-ice concentrations, HadgemHH, HadgemHM, HadgemSST
Process_Date: 20210331
Process_Description:
Wave model setup. The third-generation, spectral wave model WAVEWATCHIII (WW3; version 6.07.1; WAVEWATCHIII® Development Group (WW3DG), 2019) was downloaded from GitHub at
https://github.com/NOAA-EMC/WW3/releases). WW3 is a ‘phase-averaged model’ that solves the random phase spectral action density balance equation for wavenumber-direction spectra based on the assumption that water depths, currents, and wave fields vary on time and spatial scales much larger than that of a single wave. This version of the model includes transitional- and shallow-water equations. Source terms for physical processes include parameterizations for wind-driven wave growth, parametrized forms for nonlinear resonant wave-wave interactions, scattering due to wave-bottom interactions, triad interactions, and dissipation due to whitecapping, bottom friction, surf-breaking, and interactions with ice. Model switches used in this study were as follows (see WW3DG, 2019 for further explanations): F90 DIST MPI OMPG OMPH PR3 UQ FLX0 LN1 ST4 STAB0 NL1 BT1 IC4 IS0 REF0 DB0 TR1 MLIM BS0 XX0 WNT1 WNX1 CRT1 CRX1 NOGRB O0 O1 O2 O3 O4 O5 O6 O7 O11 NC4. Model grids consist of one 0.5 x 0.5 degree global grid, 4 nested 10 arc-minute resolution (approximately 18 km) ‘child’ grids, and 3 nested 4 arc-minute resolution (approximately 7 km) ‘grand-child’ grids (grid, geographic coverage, resolution in arc-minutes and approximate km). The finer resolution nested grids each take inputs along their open boundaries from the increasingly coarse grids. The finest resolution wave grids (approximately 7 km) align the outer coast of Alaska, including the Aleutian Islands, and the U.S. East and West coasts, including the Gulf of Mexico, Hawai’i, and Puerto Rico. U.S. territories in the Pacific Ocean are represented by a 10 arc-minute (approximately 18 km) grid. Please see the overview image provided as part of this data release for a visual representation of the spatial grid coverage. Bathymetry and landmasks for all grids were obtained from the 1-arc-minute ETOPO1 global relief model (Amante and Eakins, 2009). In an effort to optimize model output data storage needs, more than 5000 model output points (‘savepoints’) were placed along the approximate 20m, 50m, and 100m isobaths (as derived from the ETOPO1 bathymetry), spaced approximately 10 km in the alongshore direction of all U.S. coastlines or co-located with buoys or other points of interest. Output point locations were snapped to grid points and thus are not necessarily precisely coincident with long-term buoy observation locations.
Process_Date: 20210125
Process_Description:
Wave time-series for the hindcast period were added to the existing data release of wave time-series for the projected period. Corrections were made to the metadata to fix the erroneous version description of EC-Earth projections (EC-Earth3P-HR_highres-future_r1i1p1f1_gr for wind was changed to EC-Earth3P-HR_highres-future_r1i1p2f1_gr, and EC-Earth3P-HR_highres-future_r1i1p2f1_gr was changed to and EC-Earth3P-HR_highres-future_r1i1p2f1_gn). In the previously released data files for the projection period, the global attribute description was also corrected to EC-Earth3P-HR_highres-future_r1i1p2f1_gn. Additionally, erroneous non-zero wave data in the data files for the projection period in the Arctic regions, at times when the Arctic Ocean is usually ice-covered and waves in this region are not expected, were fixed. Erroneous variable datatypes were corrected.
Process_Date: 20240820