netcdf C6_5358348_1_3603083446802935913 {
dimensions:
time = UNLIMITED ; // (7305 currently)
lat = 96 ;
lon = 192 ;
bnds = 2 ;
variables:
double time(time) ;
time:bounds = "time_bnds" ;
time:units = "days since 1850-1-1 00:00:00" ;
time:calendar = "proleptic_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 rlus(time, lat, lon) ;
rlus:standard_name = "surface_upwelling_longwave_flux_in_air" ;
rlus:long_name = "Surface Upwelling Longwave Radiation" ;
rlus:comment = "The surface called \'surface\' means the lower boundary of the atmosphere. \'longwave\' means longwave radiation. Upwelling radiation is radiation from below. It does not mean \'net upward\'. When thought of as being incident on a surface, a radiative flux is sometimes called \'irradiance\'. In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called \'vector irradiance\'. In accordance with common usage in geophysical disciplines, \'flux\' implies per unit area, called \'flux density\' in physics." ;
rlus:units = "W m-2" ;
rlus:cell_methods = "area: time: mean" ;
rlus:cell_measures = "area: areacella" ;
rlus:history = "2024-02-28T01:25:15Z altered by CMOR: Changed sign. 2024-02-28T01:25:15Z altered by CMOR: replaced missing value flag (-9e+33) and corresponding data with standard missing value (1e+20). 2024-02-28T01:25:15Z altered by CMOR: Inverted axis: lat." ;
rlus:missing_value = 1.e+20f ;
rlus:_FillValue = 1.e+20f ;
// global attributes:
:CDO = "Climate Data Operators version 2.2.0 (https://mpimet.mpg.de/cdo)" ;
:Conventions = "CF-1.7 CMIP-6.2" ;
:activity_id = "ScenarioMIP" ;
:branch_method = "standard" ;
:branch_time_in_child = 60265. ;
:branch_time_in_parent = 60265. ;
:contact = "" ;
:creation_date = "2024-02-28T01:25:15Z" ;
:data_specs_version = "01.00.31" ;
:experiment = "update of RCP4.5 based on SSP2" ;
:experiment_id = "ssp245" ;
:external_variables = "areacella" ;
:forcing_index = 1 ;
:frequency = "day" ;
:further_info_url = "https://furtherinfo.es-doc.org/CMIP6.AWI.AWI-ESM-1-REcoM.ssp245.none.r1i1p1f1" ;
:grid = "All grid attributes are set for the native grid and based on information from attribute source." ;
:grid_label = "gn" ;
:history = "2024-02-28T01:25:15Z ; CMOR rewrote data to be consistent with CMIP6, CF-1.7 CMIP-6.2 and CF standards." ;
:initialization_index = 1 ;
:institution = "Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany" ;
:institution_id = "AWI" ;
:mip_era = "CMIP6" ;
:nominal_resolution = "250 km" ;
:parent_activity_id = "CMIP" ;
:parent_experiment_id = "historical" ;
:parent_mip_era = "CMIP6" ;
:parent_source_id = "AWI-ESM-1-REcoM" ;
:parent_time_units = "days since 1850-1-1 00:00:00" ;
:parent_variant_label = "r1i1p1f1" ;
:physics_index = 1 ;
:product = "model-output" ;
:project_id = "CMIP6" ;
:realization_index = 1 ;
:realm = "atmos" ;
:references = "Hauck, J., C. Völker, T. Wang, M. Hoppema, M. Losch, and D. A. Wolf-Gladrow (2013), Seasonally different carbon flux changes in the Southern Ocean in response to the southern annular mode, Global Biogeochem. Cycles, 27, 1236-1245, doi:10.1002/2013GB004600.\n",
"Schourup-Kristensen, V., Sidorenko, D., Wolf-Gladrow, D. A., and Völker, C.: A skill assessment of the biogeochemical model REcoM2 coupled to the Finite Element Sea Ice–Ocean Model (FESOM 1.3), Geosci. Model Dev., 7, 2769–2802, https://doi.org/10.5194/gmd-7-2769-2014, 2014.\n",
"Semmler, T., Danilov, S., Gierz, P., Goessling, H. F., Hegewald, J., Hinrichs, C., et al. (2020). Simulations for CMIP6 with the AWI climate model AWI-CM-1-1. Journal of Advances in Modeling Earth Systems, 12, e2019MS002009. https://doi.org/10.1029/2019MS002009" ;
:source = "AWI-ESM 1 REcoM (2024): \n",
"aerosol: none\n",
"atmos: ECHAM6.3.04p1 (T63L47 native atmosphere T63 gaussian grid; 192 x 96 longitude/latitude; 47 levels; top level 80 km)\n",
"atmosChem: none\n",
"land: JSBACH 3.20 with dynamic vegetation\n",
"landIce: none\n",
"ocean: FESOM 1.4 (unstructured grid in the horizontal with 126859 wet nodes; 46 levels; top grid cell 0-5 m)\n",
"ocnBgchem: REcoM2 (same grid as ocean component)\n",
"seaIce: FESOM 1.4 (same grid as ocean component)" ;
:source_id = "AWI-ESM-1-REcoM" ;
:source_type = "AOGCM BGC" ;
:sub_experiment = "none" ;
:sub_experiment_id = "none" ;
:table_id = "day" ;
:table_info = "Creation Date:(24 July 2019) MD5:816c2357f2fe98074c65bf22f7c9374e" ;
:title = "AWI-ESM-1-REcoM output prepared for CMIP6" ;
:variable_id = "rlus" ;
:variant_label = "r1i1p1f1" ;
:license = "CMIP6 model data produced by Alfred Wegener Institute is licensed under a Creative Commons Attribution 4.0 International License (https://creativecommons.org/licenses). Consult https://pcmdi.llnl.gov/CMIP6/TermsOfUse for terms of use governing CMIP6 output, including citation requirements and proper acknowledgment. Further information about this data, including some limitations, can be found via the further_info_url (recorded as a global attribute in this file). The data producers and data providers make no warranty, either express or implied, including, but not limited to, warranties of merchantability and fitness for a particular purpose. All liabilities arising from the supply of the information (including any liability arising in negligence) are excluded to the fullest extent permitted by law." ;
:cmor_version = "3.6.0" ;
:tracking_id = "hdl:21.14100/81b6c697-ed81-4fe0-99fa-2e7964881918" ;
}