netcdf BCBMr4MOOthetga111v120714_1_1848942943209891051 {
dimensions:
time = UNLIMITED ; // (1140 currently)
bnds = 2 ;
variables:
double time(time) ;
time:bounds = "time_bnds" ;
time:units = "days since 2006-01-01" ;
time:calendar = "noleap" ;
time:axis = "T" ;
time:long_name = "time" ;
time:standard_name = "time" ;
double time_bnds(time, bnds) ;
float thetaoga(time) ;
thetaoga:standard_name = "sea_water_potential_temperature" ;
thetaoga:long_name = "Global Average Sea Water Potential Temperature" ;
thetaoga:units = "K" ;
thetaoga:original_name = "atemp" ;
thetaoga:cell_methods = "time: mean area: mean where sea" ;
thetaoga:missing_value = 1.e+20f ;
thetaoga:_FillValue = 1.e+20f ;
thetaoga:associated_files = "baseURL: http://cmip-pcmdi.llnl.gov/CMIP5/dataLocation gridspecFile: gridspec_ocean_fx_bcc-csm1-1-m_rcp45_r0i0p0.nc" ;
// global attributes:
:institution = "Beijing Climate Center(BCC),China Meteorological Administration,China" ;
:institute_id = "BCC" ;
:experiment_id = "rcp45" ;
:source = "bcc-csm1-1-m:atmosphere: BCC_AGCM2.2 (T106L26); land: BCC_AVIM1.1;ocean: MOM4_L40v2 (tripolar, 1 lon x (1-1/3) lat, L40);sea ice: SIS (tripolar,1 lon x (1-1/3) lat)" ;
:model_id = "bcc-csm1-1-m" ;
:forcing = "Nat Ant GHG SD Oz Sl SS Ds BC OC" ;
:parent_experiment_id = "historical" ;
:parent_experiment_rip = "r1i1p1" ;
:branch_time = 2006. ;
:contact = "Dr. Tongwen Wu ()" ;
:history = "Output from monthly mean data 2012-07-12T16:41:32Z CMOR rewrote data to comply with CF standards and CMIP5 requirements." ;
:comment = "The main difference between BCC-CSM1-1-M and BCC-CSM1-1 is their horizontal resolutions of the atmospheric component and the corresponding mask of sea-land. Future projection (2006-2100) forced with prescribed concentration scenario of RCP4.5. The carbon cycle in land and ocean component model is considered, but the time-evolution of CO2 concentration in atmospheric component is prescribed. The directions of variables uo and vo are transfered from the native tripolar grid directions to geographical eastward and northward, respectively. This ocean model is a Boussinesq model, and the sea level(zos) is obtained from the model results directly. The variable zosga(global average sea level change) is sum of steric effect(zossga) and the model global mean sea level. The reference for zos was taken with respect to the model at the start time of the experiment." ;
:initialization_method = 1 ;
:physics_version = 1 ;
:tracking_id = "1e41438b-5b46-4d25-b4f1-918d5986f629" ;
:product = "output" ;
:experiment = "RCP4.5" ;
:frequency = "mon" ;
:creation_date = "2012-07-12T16:41:32Z" ;
:Conventions = "CF-1.4" ;
:project_id = "CMIP5" ;
:table_id = "Table Omon (31 January 2011) d2d6beec2b8fea5bbed33920a6e08bbe" ;
:title = "bcc-csm1-1-m model output prepared for CMIP5 RCP4.5" ;
:parent_experiment = "historical" ;
:modeling_realm = "ocean" ;
:realization = 1 ;
:cmor_version = "2.5.6" ;
}