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wdc-climate.de:3893195 eng; USA collection C6SPMXML2s245 Karl-Hermann Wieners Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Marco Giorgetta Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Johann Jungclaus Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Christian Reick Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Monika Esch Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Matthias Bittner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Veronika Gayler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Helmuth Haak Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Philipp de Vrese Max Planck Institute for Meteorology http://www.mpimet.mpg.de pointOfContact Dr. Thomas Raddatz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Thorsten Mauritsen Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Jin-Song von Storch Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Jörg Behrens Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Dr. Victor Brovkin Max Planck Institute for Meteorology http://www.mpimet.mpg.de pointOfContact Prof. Martin Claussen Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Traute Crueger Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Irina Fast Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Stephanie Fiedler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Stefan Hagemann Helmholtz-Zentrum Hereon www.hereon.de pointOfContact Cathy Hohenegger Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Thomas Jahns Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Silvia Kloster Max Planck Institute for Meteorology http://www.mpimet.mpg.de pointOfContact Dr. Stefan Kinne Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Gitta Lasslop Senckenberg Biodiversity and Climate Research Institue (BiK-F) not filled pointOfContact Dr. Luis Kornblueh Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Prof. Jochem Marotzke Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Daniela Matei Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Katharina Meraner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Uwe Mikolajewicz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Kameswarrao Modali Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Wolfgang Müller Deutscher Wetterdienst not filled pointOfContact Dr. Julia Nabel Max Planck Institute for Meteorology http://www.mpimet.mpg.de pointOfContact Dr. Dirk Notz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Karsten Peters-von Gehlen Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Robert Pincus University of Colorado http://www.colorado.edu/ pointOfContact Dr. Holger Pohlmann Max Planck Institute for Meteorology https://mpimet.mpg.de/ pointOfContact Prof. Julia Pongratz Ludwig-Maximilians-University Munich not filled pointOfContact Dr. Sebastian Rast Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Hauke Schmidt Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Reiner Schnur Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Uwe Schulzweida Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Katharina Six Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Prof. Bjorn Stevens Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Aiko Voigt Karlsruhe Institute of Technology not filled pointOfContact Dr. Erich Roeckner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact 2019-07-10T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: MPI-M MPI-ESM1.2-LR model output prepared for CMIP6 ScenarioMIP ssp245 2023-08-07 publication 1 C6SPMXML2s245 doi:10.26050/WDCC/AR6.C6SPMXML2s245 Karl-Hermann Wieners Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: Karl-Hermann.Wieners@mpimet.mpg.de author Dr. Marco Giorgetta Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: marco.giorgetta@mpimet.mpg.de author Dr. Johann Jungclaus Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: johann.jungclaus@mpimet.mpg.de author Dr. Christian Reick Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: christian.reick@mpimet.mpg.de author Monika Esch Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: monika.esch@mpimet.mpg.de author Matthias Bittner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: matthias.bittner@mpimet.mpg.de author Veronika Gayler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: veronika.gayler@mpimet.mpg.de author Dr. Helmuth Haak Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: helmuth.haak@mpimet.mpg.de author Philipp de Vrese Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: philipp.de-vrese@mpimet.mpg.de author Dr. Thomas Raddatz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: thomas.raddatz@mpimet.mpg.de author Dr. Thorsten Mauritsen Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: thorsten.mauritsen@mpimet.mpg.de author Dr. Jin-Song von Storch Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: jin-song.von.storch@mpimet.mpg.de author Jörg Behrens Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: behrens@dkrz.de author Dr. Victor Brovkin Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: victor.brovkin@mpimet.mpg.de author Prof. Martin Claussen Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: martin.claussen@mpimet.mpg.de author Dr. Traute Crueger Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: traute.crueger@mpimet.mpg.de author Irina Fast Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: fast@dkrz.de author Stephanie Fiedler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: stephanie.fiedler@mpimet.mpg.de author Dr. Stefan Hagemann Helmholtz-Zentrum Hereon https://hereon.de/ Email: stefan.hagemann@hereon.de author Cathy Hohenegger Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: cathy.hohenegger@mpimet.mpg.de author Thomas Jahns Deutsches Klimarechenzentrum http://www.dkrz.de/ author Silvia Kloster Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: silvia.kloster@mpimet.mpg.de author Dr. Stefan Kinne Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: stefan.kinne@mpimet.mpg.de author Gitta Lasslop Senckenberg Biodiversity and Climate Research Institue (BiK-F) not filled Email: gitta.lasslop@senckenberg.de author Dr. Luis Kornblueh Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: luis.kornblueh@mpimet.mpg.de author Prof. Jochem Marotzke Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: jochem.marotzke@mpimet.mpg.de author Dr. Daniela Matei Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: daniela.matei@mpimet.mpg.de author Katharina Meraner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: katharina.meraner@mpimet.mpg.de author Dr. Uwe Mikolajewicz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: uwe.mikolajewicz@mpimet.mpg.de author Kameswarrao Modali Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: modali@dkrz.de author Wolfgang Müller Deutscher Wetterdienst not filled Email: wolfgang.mueller@mpimet.mpg.de author Dr. Julia Nabel Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: julia.nabel@mpimet.mpg.de author Dr. Dirk Notz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: dirk.notz@mpimet.mpg.de author Karsten Peters-von Gehlen Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: peters@dkrz.de author Robert Pincus University of Colorado http://www.colorado.edu/ Email: Robert.Pincus@colorado.edu author Dr. Holger Pohlmann Max Planck Institute for Meteorology https://mpimet.mpg.de/ Email: holger.pohlmann@mpimet.mpg.de author Prof. Julia Pongratz Ludwig-Maximilians-University Munich not filled Email: julia.pongratz@geographie.uni-muenchen.de author Dr. Sebastian Rast Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: sebastian.rast@mpimet.mpg.de author Dr. Hauke Schmidt Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: hauke.schmidt@mpimet.mpg.de author Dr. Reiner Schnur Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: reiner.schnur@mpimet.mpg.de author Uwe Schulzweida Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: uwe.schulzweida@mpimet.mpg.de author Dr. Katharina Six Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: katharina.six@mpimet.mpg.de author Prof. Bjorn Stevens Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: bjorn.stevens@mpimet.mpg.de author Aiko Voigt Karlsruhe Institute of Technology not filled Email: aiko.voigt@kit.edu author Dr. Erich Roeckner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: erich.roeckner@mpimet.mpg.de author WDC Climate at DKRZ publisher These data include the subset used by IPCC AR6 WGI authors of the datasets originally published in ESGF for 'CMIP6.ScenarioMIP.MPI-M.MPI-ESM1-2-LR.ssp245' with the full Data Reference Syntax following the template 'mip_era.activity_id.institution_id.source_id.experiment_id.member_id.table_id.variable_id.grid_label.version'. The MPI-ESM1.2-LR climate model, released in 2017, includes the following components: aerosol: none, prescribed MACv2-SP, atmos: ECHAM6.3 (spectral T63; 192 x 96 longitude/latitude; 47 levels; top level 0.01 hPa), land: JSBACH3.20, landIce: none/prescribed, ocean: MPIOM1.63 (bipolar GR1.5, approximately 1.5deg; 256 x 220 longitude/latitude; 40 levels; top grid cell 0-12 m), ocnBgchem: HAMOCC6, seaIce: unnamed (thermodynamic (Semtner zero-layer) dynamic (Hibler 79) sea ice model). The model was run by the Max Planck Institute for Meteorology, Hamburg 20146, Germany (MPI-M) in native nominal resolutions: aerosol: 250 km, atmos: 250 km, land: 250 km, landIce: none, ocean: 250 km, ocnBgchem: 250 km, seaIce: 250 km. Karl-Hermann Wieners Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Marco Giorgetta Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Johann Jungclaus Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Christian Reick Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Monika Esch Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Matthias Bittner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Veronika Gayler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Helmuth Haak Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Philipp de Vrese Max Planck Institute for Meteorology http://www.mpimet.mpg.de pointOfContact Dr. Thomas Raddatz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Thorsten Mauritsen Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Jin-Song von Storch Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Jörg Behrens Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Dr. Victor Brovkin Max Planck Institute for Meteorology http://www.mpimet.mpg.de pointOfContact Prof. Martin Claussen Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Traute Crueger Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Irina Fast Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Stephanie Fiedler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Stefan Hagemann Helmholtz-Zentrum Hereon www.hereon.de pointOfContact Cathy Hohenegger Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Thomas Jahns Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Silvia Kloster Max Planck Institute for Meteorology http://www.mpimet.mpg.de pointOfContact Dr. Stefan Kinne Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Gitta Lasslop Senckenberg Biodiversity and Climate Research Institue (BiK-F) not filled pointOfContact Dr. Luis Kornblueh Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Prof. Jochem Marotzke Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Daniela Matei Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Katharina Meraner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Uwe Mikolajewicz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Kameswarrao Modali Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Wolfgang Müller Deutscher Wetterdienst not filled pointOfContact Dr. Julia Nabel Max Planck Institute for Meteorology http://www.mpimet.mpg.de pointOfContact Dr. Dirk Notz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Karsten Peters-von Gehlen Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Robert Pincus University of Colorado http://www.colorado.edu/ pointOfContact Dr. Holger Pohlmann Max Planck Institute for Meteorology https://mpimet.mpg.de/ pointOfContact Prof. Julia Pongratz Ludwig-Maximilians-University Munich not filled pointOfContact Dr. Sebastian Rast Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Hauke Schmidt Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Reiner Schnur Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Uwe Schulzweida Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Katharina Six Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Prof. Bjorn Stevens Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Aiko Voigt Karlsruhe Institute of Technology not filled pointOfContact Dr. Erich Roeckner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact NetCDF CMIP6 IPCC IPCC-AR6 IPCC-DDC MPI-ESM1-2-LR MPI-M ScenarioMIP climate change model-output ssp245 CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ eng; USA 0.0 360.0 -90.0 90.0 gregorian 2015-01-01 2100-12-31 toa_outgoing_longwave_flux_assuming_clear_sky A phrase assuming_condition indicates that the named quantity is the value which would obtain if all aspects of the system were unaltered except for the assumption of the circumstances specified by the condition. "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 sea_water_salinity sea_water_salinity [CF-Standard Name]; unit: 0.001 air_pressure_at_mean_sea_level Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL. Air pressure is the force per unit area which would be exerted when the moving gas molecules of which the air is composed strike a theoretical surface of any orientation. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. [CF-Standard Name]; unit: Pa sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 sea_ice_area Sea-Ice Area North Comment: total area of sea ice in the Northern hemisphere Used for mip era 'CMIP6' in CMOR MIP table(s): Table SImon, provided in frequency(s): mon, and for Realm(s): seaIce. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: 1e6 km2 surface_temperature The surface called "surface" means the lower boundary of the atmosphere. The surface temperature is the (skin) temperature at the interface, not the bulk temperature of the medium above or below. [CF-Standard Name]; unit: K global_average_thermosteric_sea_level_change Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m sea_ice_area Sea-Ice Area North Comment: total area of sea ice in the Northern hemisphere Used for mip era 'CMIP6' in CMOR MIP table(s): Table SImon, provided in frequency(s): mon, and for Realm(s): seaIce. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: 1e6 km2 surface_downward_eastward_stress The surface called "surface" means the lower boundary of the atmosphere. "Eastward" indicates a vector component which is positive when directed eastward (negative westward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward eastward" indicates the ZX component of a tensor. A downward eastward stress is a downward flux of eastward momentum, which accelerates the lower medium eastward and the upper medium westward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa sea_ice_amount "Amount" means mass per unit area. [CF-Standard Name]; unit: kg m-2 mass_content_of_water_in_soil_layer Total Water Content of Soil Layer Comment: in each soil layer, the mass of water in all phases, including ice. Reported as 'missing' for grid cells occupied entirely by 'sea' Used for mip era 'CMIP6' in CMOR MIP table(s): Table 6hrPlevPt; Table Eday; Table Emon, provided in frequency(s): 6hr; day; mon, and for Realm(s): atmos; land. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: kg m-2 sea_ice_surface_temperature sea_ice_surface_temperature [CF-Standard Name]; unit: K specific_humidity "specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1 surface_air_pressure The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa sea_ice_thickness sea_ice_thickness [CF-Standard Name]; unit: m surface_upward_sensible_heat_flux The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface sensible heat flux, also called "turbulent" heat flux, is the exchange of heat between the surface and the air by motion of air. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2 geopotential_height Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m specific_humidity "specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K land_area_fraction "X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell.[CF-Standard Name]; unit: 0.01 surface_altitude The surface called "surface" means the lower boundary of the atmosphere. Altitude is the (geometric) height above the geoid, which is the reference geopotential surface. The geoid is similar to mean sea level.[CF-Standard Name]; unit: m surface_downward_heat_flux_in_sea_water surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2 sea_surface_salinity The unit of salinity is PSU, which is dimensionless. The units attribute should be given as 1e-3 or 0.001 i.e. parts per thousand if salinity is in PSU. Sea surface salinity is often abbreviated as "SSS". For the salinity of sea water at a particular depth or layer, a data variable of sea_water_salinity with a vertical coordinate axis should be used. [CF-Standard Name]; unit: 0.001 surface_upwelling_longwave_flux_in_air 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. [CF-Standard Name]; unit: W m-2 toa_outgoing_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2 relative_humidity relative_humidity [CF-Standard Name]; unit: 0.01 surface_upward_latent_heat_flux The surface called "surface" means the lower boundary of the atmosphere. "Upward" indicates a vector component which is positive when directed upward (negative downward). The surface latent heat flux is the exchange of heat between the surface and the air on account of evaporation (including sublimation). In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics.[CF-Standard Name]; unit: W m-2 wind_speed Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1 surface_downward_mass_flux_of_carbon_dioxide_expressed_as_carbon surface_downward_mass_flux_of_carbon_dioxide_expressed_as_carbon [CF-Standard Name]; unit: kg m-2 s-1 surface_net_downward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_all_land_processes surface_net_downward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_all_land_processes [CF-Standard Name]; unit: kg m-2 s-1 surface_downwelling_longwave_flux_in_air surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2 snowfall_flux In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1 mass_content_of_water_in_soil Total Soil Moisture Content Comment: the mass per unit area (summed over all soil layers) of water in all phases. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Lmon; Table day, provided in frequency(s): day; mon, and for Realm(s): atmos; land. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: kg m-2 cell_area Model Grid-Cell Area [CF-Standard Name]; unit: m2 toa_outgoing_shortwave_flux "shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA outgoing shortwave flux is the reflected and scattered solar radiative flux i.e. the "upwelling" TOA shortwave flux, sometimes called the "outgoing shortwave radiation" or "OSR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 toa_outgoing_longwave_flux "longwave" means longwave radiation. "toa" means top of atmosphere. The TOA outgoing longwave flux is the upwelling thermal radiative flux, often called the "outgoing longwave radiation" or "OLR". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 specific_humidity "specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: 1 sea_surface_height_above_geoid sea_surface_height_above_geoid [CF-Standard Name]; unit: m air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K surface_downward_mass_flux_of_carbon_dioxide_expressed_as_carbon surface_downward_mass_flux_of_carbon_dioxide_expressed_as_carbon [CF-Standard Name]; unit: kg m-2 s-1 northward_wind "Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1 eastward_wind "Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1 geopotential_height Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m surface_upwelling_shortwave_flux_in_air The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave 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. [CF-Standard Name]; unit: W m-2 surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 soil_temperature Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K precipitation_flux In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K land_ice_area_fraction "X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. "Land ice" means glaciers, ice-caps and ice-sheets resting on bedrock. [CF-Standard Name]; unit: 0.01 soil_moisture_content_at_field_capacity "moisture" means water in all phases contained in soil. "Content" indicates a quantity per unit area. The "soil content" of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used. The field capacity of soil is the maximum content of water it can retain against gravitational drainage. [CF-Standard Name]; unit: kg m-2 sea_surface_temperature Sea surface temperature is usually abbreviated as "SST". It is the temperature of sea water near the surface (including the part under sea-ice, if any), and not the skin temperature, whose standard name is surface_temperature. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used. [CF-Standard Name]; unit: degC surface_downward_northward_stress The surface called "surface" means the lower boundary of the atmosphere. "Northward" indicates a vector component which is positive when directed northward (negative southward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward northward" indicates the ZY component of a tensor. A downward northward stress is a downward flux of northward momentum, which accelerates the lower medium northward and the upper medium southward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa precipitation_flux In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 runoff_flux Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: kg m-2 s-1 eastward_wind "Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1 cell_area Model Grid-Cell Area [CF-Standard Name]; unit: m2 sea_floor_depth_below_geoid Sea Floor Depth [CF-Standard Name]; unit: m air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K sea_water_potential_temperature sea_water_potential_temperature [CF-Standard Name]; unit: degC northward_wind "Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1 atmosphere_mass_content_of_water_vapor atmosphere_mass_content_of_water_vapor [CF-Standard Name]; unit: kg m-2 leaf_area_index "X_area" means the horizontal area occupied by X within the grid cell.[CF-Standard Name]; unit: 1 toa_incoming_shortwave_flux "shortwave" means shortwave radiation. "toa" means top of atmosphere. The TOA incoming shortwave flux is the radiative flux from the sun i.e. the "downwelling" TOA shortwave flux. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 mass_content_of_carbon_in_vegetation_and_litter_and_soil_and_forestry_and_agricultural_products Total Carbon in All Terrestrial Carbon Pools Comment: Report missing data over ocean grid cells. For fractional land report value averaged over the land fraction. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Emon, provided in frequency(s): mon, and for Realm(s): land. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: kg m-2 water_evapotranspiration_flux Snow Evaporation Comment: Water here means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called 'sublimation'.) In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Eday, provided in frequency(s): day, and for Realm(s): land. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: kg m-2 s-1 wind_speed Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1 air_pressure_at_mean_sea_level Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL. Air pressure is the force per unit area which would be exerted when the moving gas molecules of which the air is composed strike a theoretical surface of any orientation. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. [CF-Standard Name]; unit: Pa sea_area_fraction Sea Area Fraction [CF-Standard Name]; unit: 0.01 cloud_area_fraction "X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K gross_primary_productivity_of_biomass_expressed_as_carbon Carbon Mass Flux out of Atmosphere Due to Gross Primary Production on Land Comment: The rate of synthesis of biomass from inorganic precursors by autotrophs ('producers') expressed as the mass of carbon which it contains. For example, photosynthesis in plants or phytoplankton. The producers also respire some of this biomass and the difference is referred to as the net primary production. Used for mip era 'CMIP6' in CMOR MIP table(s): Table E3hr; Table Lmon, provided in frequency(s): 3hr; mon, and for Realm(s): land. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: kg m-2 s-1 surface_snow_amount surface_snow_amount [CF-Standard Name]; unit: kg m-2 ocean_meridional_overturning_mass_streamfunction Ocean Meridional Overturning Mass Streamfunction [CF-Standard Name]; unit: kg s-1 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K NetCDF 261343 https://www.wdc-climate.de/ui/entry?acronym=C6SPMXML2s245 information collection