netcdf files/g/d314000/daily/tmax_daily_1980-1980.nc { dimensions: longitude = 360; latitude = 180; z = 1; time = UNLIMITED; // (366 currently) variables: float longitude(longitude=360); :units = "degrees_east"; :point_spacing = "even"; :modulo = " "; float latitude(latitude=180); :units = "degrees_north"; :point_spacing = "even"; float z(z=1); :units = "level"; :positive = "up"; float time(time=366); :units = "days since 1980-01-01 00:00:00"; :time_origin = "01-JAN-1980:00:00:00"; float tmax(time=366, z=1, latitude=180, longitude=360); :source = "Reanalysis 6-hourly air temperature interpolated to 1.0deg with account for elevation changes, interpolated to 3-hourly and scaled to match the diurnal range and mean of the CRU TS3.0 monthly dataset"; :name = "tmax"; :title = "daily bias corrected maximum temperature"; :date = "01/01/80"; :time = "00:00"; :long_name = "Maximum air temperature"; :units = "K"; :missing_value = 2.0E20f; // float :_FillValue = 2.0E20f; // float :valid_min = 183.55444f; // float :valid_max = 325.03372f; // float // global attributes: :history = "Fri Mar 11 09:45:01 EST 2011: created by JS using convert2alma.sh"; :title = "Princeton University Hydroclimatology Group Bias Corrected 59-yr (1948-2006) Meteorological Forcing Dataset"; :institution = "Princeton University"; :contact = "Justin Sheffield (justin@princeton.edu)"; :source = "Forcings are a hybrid of NCEP/NCAR reanalysis and observations"; :comment = "This is an update to the original version reported in Sheffield et al., J. Climate (2006). Updates include: i) extension to 2006; ii) improved sampling procedure for correction of rain day statistics; iii) use of latest versions of CRU, SRB and TRMM products; iv) improved consistency between specific and relative humidity and air temperature. See Sheffield et al., J. Climate (2006) for details of the observations used and the bias correction and downscaling methodology."; }