netcdf MXEPlgXAHorog000v150130_1_7680746335488324035 {
dimensions:
lat = 96 ;
lon = 192 ;
bnds = 2 ;
variables:
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 orog(lat, lon) ;
orog:standard_name = "surface_altitude" ;
orog:long_name = "Surface Altitude" ;
orog:comment = "This is code 129 ( surface geopotential in m2 s-2 ) devided by g=9.80665 m s-2. ;Due to the spectral nature of ECHAM6s dynamical core, the values over ocean are not zero., CMIP5_table_comment: height above the geoid; as defined here, \"\"the geoid\"\" is a surface of constant geopotential that, if the ocean were at rest, would coincide with mean sea level. Under this definition, the geoid changes as the mean volume of the ocean changes (e.g., due to glacial melt, or global warming of the ocean). Reported here is the height above the present-day geoid (0.0 over ocean)." ;
orog:units = "m" ;
orog:cell_measures = "area: areacella" ;
orog:missing_value = 1.e+20f ;
orog:_FillValue = 1.e+20f ;
orog:associated_files = "baseURL: http://cmip-pcmdi.llnl.gov/CMIP5/dataLocation gridspecFile: gridspec_atmos_fx_MPI-ESM-P_lgm_r0i0p0.nc areacella: areacella_fx_MPI-ESM-P_lgm_r0i0p0.nc" ;
// global attributes:
:institution = "Max Planck Institute for Meteorology" ;
:institute_id = "MPI-M" ;
:experiment_id = "lgm" ;
:source = "MPI-ESM-P 2011; URL: http://svn.zmaw.de/svn/cosmos/branches/releases/mpi-esm-cmip5/src/mod; atmosphere: ECHAM6 (REV: 4860), T63L47; land: JSBACH (REV: 4860); ocean: MPIOM (REV: 4860), GR15L40; sea ice: (REV: 4860); marine bgc: HAMOCC (REV: 4860);" ;
:model_id = "MPI-ESM-P" ;
:forcing = "N/A" ;
:parent_experiment_id = "N/A" ;
:parent_experiment_rip = "N/A" ;
:branch_time = 0. ;
:contact = " cmip5-mpi-esm@
nulldkrz.de
:history = "Model raw output postprocessing with modelling environment (IMDI) at DKRZ 2015-01-29T08:07:02Z CMOR rewrote data to comply with CF standards and CMIP5 requirements." ;
:comment = "started from lgm spinup run." ;
:references = "ECHAM6: n/a JSBACH: Raddatz et al., 2007. Will the tropical land biosphere dominate the climate-carbon cycle feedback during the twenty first century? Climate Dynamics, 29, 565-574, doi 10.1007/s00382-007-0247-8; MPIOM: Marsland et al., 2003. The Max-Planck-Institute global ocean/sea ice model with orthogonal curvilinear coordinates. Ocean Modelling, 5, 91-127; HAMOCC: http://www.mpimet.mpg.de/fileadmin/models/MPIOM/HAMOCC5.1_TECHNICAL_REPORT.pdf;" ;
:initialization_method = 0 ;
:physics_version = 0 ;
:tracking_id = "8078f118-f948-4710-8ba3-f8706f490b99" ;
:product = "output" ;
:experiment = "last glacial maximum" ;
:frequency = "fx" ;
:creation_date = "2015-01-29T08:07:02Z" ;
:Conventions = "CF-1.4" ;
:project_id = "CMIP5" ;
:table_id = "Table fx (17 July 2013) 3b0d4cb42c006e5b8c33b07e6b313255" ;
:title = "MPI-ESM-P model output prepared for CMIP5 last glacial maximum" ;
:parent_experiment = "N/A" ;
:modeling_realm = "atmos" ;
:realization = 0 ;
:cmor_version = "2.8.0" ;
}