netcdf files/d316015/table4/grndtyp_GFDL.nc { dimensions: lon = 576; lat = 360; bnds = 2; variables: double lat(lat=360); :units = "degrees_north"; :long_name = "latitude"; :standard_name = "latitude"; :axis = "Y"; :bounds = "lat_bnds"; double lon(lon=576); :units = "degrees_east"; :long_name = "longitude"; :standard_name = "longitude"; :axis = "X"; :bounds = "lon_bnds"; double lat_bnds(lat=360, bnds=2); :long_name = "latitude bounds"; :units = "degrees_north"; double lon_bnds(lon=576, bnds=2); :long_name = "longitude bounds"; :units = "degrees_east"; float grndtyp(lat=360, lon=576); :standard_name = "ground_cover_index"; :long_name = "Ground-Cover Type"; :units = "none"; :missing_value = -1.0f; // float :_FillValue = -1.0f; // float :description = " \n 1: coarse soil \n 2: medium soil \n 3: fine soil \n 4: coarse/medium mix \n 5: coarse/fine mix \n 6: medium/fine mix \n 7: coarse/medium/fine mix \n 8: organic soil (peat) \n 9: ice \n 10: lake"; // global attributes: :title = "GFDL AM2(fv)/LM2 model output prepared for NARCCAP present day control using HadISST"; :institution = "NOAA GFDL (US Dept of Commerce / NOAA / Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA)"; :source = "GFDL_AM2(fv)/LM2: atmosphere: AM2.1 (am2p14fv, M180L24); ocean: prescribed (HadISST); sea ice: prescribed (HadISST); land: LM2; infrastructure: FMS Memphis release"; :contact = "Isaac.Held@noaa.gov; Bruce.Wyman@noaa.gov"; :project_id = "North American Regional Climate Change Assessment Project"; :experiment_id = "all"; :references = "The GFDL Data Portal (http://nomads.gfdl.noaa.gov/) provides access to NOAA/GFDL\'s publicly available model input and output data sets."; :comment = "This model was run in AMIP mode with SST and sea ice extent determined from the HadISST1 data set. Other forcing agents varied in a manner based upon observations and reconstructions for the 20th century and were consistent with the GFDL IPCC experiment CM2.1U-D4_1860-2000-AllForc_H2. These time varying forcing agents were atmospheric CO2, CH4, N2O, halons, tropospheric and stratospheric O3, anthropogenic tropospheric sulfates, black and organic carbon, volcanic aerosols, solar irradiance, and the distribution of land cover types. The direct effect of tropospheric aerosols is calculated by the model, but not the indirect effects."; :gfdl_experiment_name = "m180_narccap_hist"; }