__grid_table = "Tables/CMIP6_grids.json" "_control_vocabulary_file" = "CMIP6_CV.json" "_cmip6_option" = "CMIP6" "activity_id" = "CMIP" "outpath" = "CMIP6" "experiment_id" = "piControl" "realization_index" = "1" "initialization_index" = "1" "physics_index" = "1" "forcing_index" = "1" "source_type" = "AOGCM" "sub_experiment" = "none" "sub_experiment_id" = "none" "parent_sub_experiment_id" = "N/A" "parent_mip_era" = "N/A" "mip_era" = "CMIP6" "contact " = "cmip5-mpi-esm@dkrz.de" "institution_id" = "MPI-M" "model_id" = "MPI-ESM-MR" "history" = "Model raw output postprocessing with modelling environment (IMDI) at DKRZ: URL: http://svn-mad.zmaw.de/svn/mad/Model/IMDI/trunk, REV: 3901 2011-10-06T06:31:24Z CMOR rewrote data to comply with CF standards and CMIP5 requirements." "comment" = "" "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: Technical Documentation, http://www.mpimet.mpg.de/fileadmin/models/MPIOM/HAMOCC5.1_TECHNICAL_REPORT.pdf;" "parent_experiment_rip" = "N/A" "parent_experiment_id" = "N/A" "parent_variant_label" = "N/A" "branch_time" = "0" "parent_activity_id" = "N/A" "parent_source_id" = "N/A" "parent_variant_label" = "N/A" "branch_method" = "standard" "grid" = "native atmosphere T63 gaussian grid (64x128 latxlon)" "grid_label" = "gn" "grid_resolution" = "5 km" "institution" = "Max Planck Institute for Meteorology" "run_variant" = "MPI-ESM-MR model output prepared for CMIP5 pre-industrial control" "source_id" = "MPI-ESM" "source" = "MPI-ESM:" "output_path_template" = "" "output_file_template" = "
" "license" = "N/A" # # Rename axis __rename_lev = plev19