netcdf MIM578MAApsladj211v120710_1_4259190082973279524 { dimensions: time = UNLIMITED ; // (120 currently) lat = 128 ; lon = 256 ; bnds = 2 ; variables: double time(time) ; time:bounds = "time_bnds" ; time:units = "days since 1979-1-1" ; time:calendar = "gregorian" ; time:axis = "T" ; time:long_name = "time" ; time:standard_name = "time" ; double time_bnds(time, bnds) ; double lat(lat) ; lat:bounds = "lat_bnds" ; lat:units = "degrees_north" ; lat:axis = "Y" ; lat:long_name = "latitude" ; lat:standard_name = "latitude" ; double lat_bnds(lat, bnds) ; double lon(lon) ; lon:bounds = "lon_bnds" ; lon:units = "degrees_east" ; lon:axis = "X" ; lon:long_name = "longitude" ; lon:standard_name = "longitude" ; double lon_bnds(lon, bnds) ; float pslAdjust(time, lat, lon) ; pslAdjust:standard_name = "air_pressure_at_sea_level" ; pslAdjust:long_name = "Bias-Corrected Sea Level Pressure" ; pslAdjust:comment = "The bias corrected field is obtained as following: Y\'jt = <X> + ( Yjt - <Y> ) - Dt. The Yjt and Y\'jt are the prediction and it\'s bias corrected field, respectively. The model climatology <Y> is the 1971-2000 mean in the historical run (r1i1p1). The observational climatology <X> is taken from the 1971-2000 mean in the ERA40 and interpolated into the model Gaussian T85 grid with triangular truncation at wave 85. The Dt is the model drift estimated from the difference between ensemble mean predictions (6 members) and the assimilations (2 members) averaged over 41 cases (from 1961 to 2001 by every year) as described in Chikamoto et al., (2011): Dt = SUM(Yjt) - SUM(Zt), where Zt is the assimilation corresponding to the time t. Reference Chikamoto Y., et al. (2011): Predictability of a stepwise shift in Pacific climate during the late 1990s in hindcast experiments using MIROC, J. Meteor. Soc. Japan, special issue., CMIP5_table_comment: not, in general, the same as surface pressure" ; pslAdjust:units = "Pa" ; pslAdjust:original_name = "SLPEC" ; pslAdjust:original_units = "hPa" ; pslAdjust:history = "2012-02-03T07:53:27Z altered by CMOR: Converted units from \'hPa\' to \'Pa\'. 2012-02-03T07:53:27Z altered by CMOR: replaced missing value flag (-999) with standard missing value (1e+20). 2012-02-03T07:53:27Z altered by CMOR: Inverted axis: lat." ; pslAdjust:cell_methods = "time: mean" ; pslAdjust:cell_measures = "area: areacella" ; pslAdjust:missing_value = 1.e+20f ; pslAdjust:_FillValue = 1.e+20f ; pslAdjust:associated_files = "baseURL: http://cmip-pcmdi.llnl.gov/CMIP5/dataLocation gridspecFile: gridspec_atmos_fx_MIROC5_decadal1978_r0i0p0.nc areacella: areacella_fx_MIROC5_decadal1978_r0i0p0.nc" ; // global attributes: :institution = "AORI (Atmosphere and Ocean Research Institute, The University of Tokyo, Chiba, Japan), NIES (National Institute for Environmental Studies, Ibaraki, Japan), JAMSTEC (Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan)" ; :institute_id = "MIROC" ; :experiment_id = "decadal1978" ; :source = "MIROC5 2010 atmosphere: MIROC-AGCM6 (T85L40); ocean: COCO (COCO4.5, 256x224 L50); sea ice: COCO (COCO4.5); land: MATSIRO (MATSIRO, L6); aerosols: SPRINTARS (SPRINTARS 5.00, T85L40)" ; :model_id = "MIROC5" ; :forcing = "GHG, SA, Oz, LU, Sl, Vl, SS, Ds, BC, MD, OC (GHG includes CO2, N2O, methane, and fluorocarbons; Oz includes OH and H2O2; LU excludes change in lake fraction)" ; :parent_experiment_id = "N/A" ; :parent_experiment_rip = "N/A" ; :branch_time = 0. ; :contact = "Masahiro Watanabe (