wdc-climate.de:5285957 eng; USA collection C6_5285957 Wolfgang Müller Deutscher Wetterdienst not filled pointOfContact Tatiana Ilyina Max Planck Institute for Meteorology https://mpimet.mpg.de/ pointOfContact Hongmei Li Max Planck Institute for Meteorology https://mpimet.mpg.de/ pointOfContact Dr. Claudia Timmreck Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Veronika Gayler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Karl-Hermann Wieners Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Michael Botzet Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Victor Brovkin 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 Dr. Stephanie Legutke Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Martin Schupfner Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Fabian Wachsmann Deutsches Klimarechenzentrum http://www.dkrz.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 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 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 2026-02-04T10:21:32 ISO 19115 ISO 19115-2:2009 MPI-M MPI-ESM1.2-LR model output prepared for CMIP6 DAMIP hist-nat 2025-09-09 publication 1 C6_5285957 doi:10.26050/WDCC/C6_5285957 Wolfgang Müller Deutscher Wetterdienst not filled Email: wolfgang.mueller@mpimet.mpg.de author Tatiana Ilyina Max Planck Institute for Meteorology https://mpimet.mpg.de/ Email: tatiana.ilyina@mpimet.mpg.de author Hongmei Li Max Planck Institute for Meteorology https://mpimet.mpg.de/ Email: hongmei.li@mpimet.mpg.de author Dr. Claudia Timmreck Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: claudia.timmreck@mpimet.mpg.de author Veronika Gayler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: veronika.gayler@mpimet.mpg.de author Karl-Hermann Wieners Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: Karl-Hermann.Wieners@mpimet.mpg.de author Michael Botzet Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: michael.botzet@mpimet.mpg.de author Dr. Victor Brovkin Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: victor.brovkin@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 Dr. Stephanie Legutke Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: legutke@dkrz.de author Martin Schupfner Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: schupfner@dkrz.de author Fabian Wachsmann Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: wachsmann@dkrz.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 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 www.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 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 WDCC publisher These data include all datasets published for 'CMIP6.DAMIP.MPI-M.MPI-ESM1-2-LR.hist-nat' 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. Individuals using the data must abide by terms of use for CMIP6 data (https://pcmdi.llnl.gov/CMIP6/TermsOfUse). The original license restrictions on these datasets were recorded as global attributes in the data files, but these may have been subsequently updated. Wolfgang Müller Deutscher Wetterdienst not filled pointOfContact Tatiana Ilyina Max Planck Institute for Meteorology https://mpimet.mpg.de/ pointOfContact Hongmei Li Max Planck Institute for Meteorology https://mpimet.mpg.de/ pointOfContact Dr. Claudia Timmreck Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Veronika Gayler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Karl-Hermann Wieners Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Michael Botzet Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ pointOfContact Dr. Victor Brovkin 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 Dr. Stephanie Legutke Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Martin Schupfner Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Fabian Wachsmann Deutsches Klimarechenzentrum http://www.dkrz.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 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 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 DAMIP MPI-ESM1-2-LR MPI-M hist-nat model-output 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 proleptic_gregorian 1850-01-01 2014-12-31 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 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 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 dew_point_temperature Dew point temperature is the temperature at which a parcel of air reaches saturation upon being cooled at constant pressure and specific humidity. [CF-Standard Name]; unit: K air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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 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 mole_concentration_of_dissolved_inorganic_carbon_in_sea_water mole_concentration_of_dissolved_inorganic_carbon_in_sea_water [CF-Standard Name]; unit: mol m-3 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_water_ph_reported_on_total_scale sea_water_ph_reported_on_total_scale [CF-Standard Name]; unit: 1 sea_ice_thickness sea_ice_thickness [CF-Standard Name]; unit: m atmosphere_optical_thickness_due_to_ambient_aerosol_particles Ambient Aerosol Optical Thickness at 440nm Comment: AOD from the ambient aerosols (i.e., includes aerosol water). Does not include AOD from stratospheric aerosols if these are prescribed but includes other possible background aerosol types. Needs a comment attribute 'wavelength: 440nm' Used for mip era 'CMIP6' in CMOR MIP table(s): Table AERmon, provided in frequency(s): mon, and for Realm(s): aerosol. 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: 1 soil_mass_content_of_carbon Carbon Mass in Model Soil Pool Comment: Carbon mass in the full depth of the soil model. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Emon; Table Eyr, provided in frequency(s): mon; yrPt, 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 sinking_mole_flux_of_particulate_silicon_in_sea_water cf:In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid. [CF-Standard Name]; unit: mol 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 ocean_meridional_overturning_mass_streamfunction Ocean Meridional Overturning Mass Streamfunction [CF-Standard Name]; unit: kg 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 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 ocean_meridional_overturning_mass_streamfunction_due_to_parameterized_mesoscale_eddy_advection Ocean Meridional Overturning Mass Streamfunction Due to Parameterized Mesoscale Advection Comment: CMIP5 called this 'due to Bolus Advection'. Name change respects the more general physics of the mesoscale parameterizations. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Omon, provided in frequency(s): mon, and for Realm(s): ocean; ocnBgchem. 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 s-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 sea_water_volume Sea Water Volume [CF-Standard Name]; unit: m3 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 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 surface_downwelling_longwave_flux_in_air surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2 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 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_downward_x_stress surface_downward_x_stress [CF-Standard Name]; unit: N 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 vegetation_carbon_content vegetation_carbon_content [CF-Standard Name]; unit: kg m-2 eastward_sea_water_velocity sea_water_x_velocity [CF-Standard Name]; unit: m s-1 northward_sea_water_velocity sea_water_y_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 square_of_sea_surface_height_above_geoid Square of Sea Surface Height Above Geoid [CF-Standard Name]; unit: m2 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 surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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 area_fraction "Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01 area_fraction "Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01 area_fraction "Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01 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 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 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 toa_outgoing_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2 sea_ice_y_velocity sea_ice_y_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 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 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 net_primary_productivity_of_biomass_expressed_as_carbon Carbon Mass Flux out of Atmosphere Due to Net Primary Production on Land Comment: 'Production of carbon' means the production of biomass expressed as the mass of carbon which it contains. Net primary production is the excess of gross primary production (rate of synthesis of biomass from inorganic precursors) by autotrophs ('producers'), for example, photosynthesis in plants or phytoplankton, over the rate at which the autotrophs themselves respire some of this biomass. 'Productivity' means production per unit area. The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Lmon, 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 s-1 surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_plant_respiration Carbon Mass Flux into Atmosphere Due to Autotrophic (Plant) Respiration on Land Comment: Carbon mass flux per unit area into atmosphere due to autotrophic respiration on land (respiration by producers) [see rh for heterotrophic 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 sea_ice_x_velocity sea_ice_x_velocity [CF-Standard Name]; unit: m s-1 mass_concentration_of_phytoplankton_expressed_as_chlorophyll_in_sea_water mass_concentration_of_phytoplankton_expressed_as_chlorophyll_in_sea_water [CF-Standard Name]; unit: kg m-3 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 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 area_fraction "Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01 area_fraction "Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [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 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 surface_snow_thickness surface_snow_thickness [CF-Standard Name]; unit: m northward_ocean_heat_transport Northward Ocean Heat Transport [CF-Standard Name]; unit: W 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 surface_downward_heat_flux_in_sea_water surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2 surface_net_downward_shortwave_flux The surface called "surface" means the lower boundary of the atmosphere. "shortwave" means shortwave radiation. "Downward" indicates a vector component which is positive when directed downward (negative upward). Net downward radiation is the difference between radiation from above (downwelling) and radiation from below (upwelling). 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 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 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 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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K surface_downward_y_stress surface_downward_y_stress [CF-Standard Name]; unit: N m-2 upward_transformed_eulerian_mean_air_velocity Transformed Eulerian Mean Upward Wind Comment: Transformed Eulerian Mean Diagnostics w*, meridional component of the residual meridional circulation (v*, w*) derived from 6 hr or higher frequency data fields (use instantaneous daily fields or 12 hr fields if the 6 hr data are not available). Scale height: 6950 m Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m 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 sea_ice_surface_temperature sea_ice_surface_temperature [CF-Standard Name]; unit: K ocean_mixed_layer_thickness_defined_by_sigma_t Ocean Mixed Layer Thickness Defined by Sigma T [CF-Standard Name]; unit: m sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 northward_eliassen_palm_flux_in_air Northward Component of the Eliassen-Palm Flux Comment: Transformed Eulerian Mean Diagnostics Meridional component Fy of Eliassen-Palm (EP) flux (Fy, Fz) derived from 6hr or higher frequency fields (use daily fields or 12 hr fields if the 6 hr are not available). Please use the definitions given by equation 3.5.3a of Andrews, Holton and Leovy text book, but scaled by density to have units m3 s-2. Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m3 s-2 depth_of_isosurface_of_sea_water_potential_temperature Depth of 20 degree Celsius Isotherm Comment: This quantity, sometimes called the 'isotherm depth', is the depth (if it exists) at which the sea water potential temperature equals some specified value. This value should be specified in a scalar coordinate variable. Depth is the vertical distance below the surface. Potential temperature is the temperature a parcel of air or sea water would have if moved adiabatically to sea level pressure. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Eday; Table Emon, provided in frequency(s): day; mon, and for Realm(s): land; ocean. 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: m sea_surface_height_above_geoid sea_surface_height_above_geoid [CF-Standard Name]; unit: m sea_water_potential_temperature sea_water_potential_temperature [CF-Standard Name]; unit: degC lagrangian_tendency_of_air_pressure "tendency_of_X" means derivative of X with respect to time. The Lagrangian tendency of a quantity is its rate of change following the motion of the fluid, also called the "material derivative" or "convective derivative". The Lagrangian tendency of air pressure, often called "omega", plays the role of the upward component of air velocity when air pressure is being used as the vertical coordinate. If the vertical air velocity is upwards, it is negative when expressed as a tendency of air pressure; downwards is positive.[CF-Standard Name]; unit: Pa s-1 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 mole_concentration_of_dissolved_inorganic_silicon_in_sea_water Total Dissolved Inorganic Silicon Concentration Comment: Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Dissolved inorganic silicon' means the sum of all inorganic silicon in solution (including silicic acid and its first dissociated anion SiO(OH)3-). Used for mip era 'CMIP6' in CMOR MIP table(s): Table Omon; Table Oyr, provided in frequency(s): mon; yr, and for Realm(s): ocnBgchem. 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: mol m-3 upward_eliassen_palm_flux_in_air Upward Component of the Eliassen-Palm Flux Comment: Transformed Eulerian Mean Diagnostics Meridional component Fz of the Eliassen-Palm (EP) flux (Fy, Fz) derived from 6hr or higher frequency fields (use daily fields or 12 hr fields if the 6 hr are not available). Please use the definitions given by equation 3.5.3b of Andrews, Holton and Leovy text book, but scaled by density to have units m3 s-2. Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m3 s-2 net_primary_mole_productivity_of_biomass_expressed_as_carbon_by_phytoplankton Primary Organic Carbon Production by All Types of Phytoplankton Comment: Vertically integrated total primary (organic carbon) production by phytoplankton. This should equal the sum of intpdiat+intpphymisc, but those individual components may be unavailable in some models. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Omon, provided in frequency(s): mon, and for Realm(s): ocnBgchem. 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: mol m-2 s-1 sea_water_potential_temperature sea_water_potential_temperature [CF-Standard Name]; unit: degC northward_transformed_eulerian_mean_air_velocity Transformed Eulerian Mean Northward Wind Comment: Transformed Eulerian Mean Diagnostics v*, meridional component of the residual meridional circulation (v*, w*) derived from 6 hr or higher frequency data fields (use instantaneous daily fields or 12 hr fields if the 6 hr data are not available). Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m s-1 sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 mole_concentration_of_phytoplankton_expressed_as_carbon_in_sea_water mole_concentration_of_phytoplankton_expressed_as_carbon_in_sea_water [CF-Standard Name]; unit: mol m-3 sea_water_potential_temperature sea_water_potential_temperature [CF-Standard Name]; unit: degC northward_transformed_eulerian_mean_air_velocity Transformed Eulerian Mean Northward Wind Comment: Transformed Eulerian Mean Diagnostics v*, meridional component of the residual meridional circulation (v*, w*) derived from 6 hr or higher frequency data fields (use instantaneous daily fields or 12 hr fields if the 6 hr data are not available). Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m 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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K mole_concentration_of_dissolved_molecular_oxygen_in_sea_water mole_concentration_of_dissolved_molecular_oxygen_in_sea_water [CF-Standard Name]; unit: mol m-3 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K mole_concentration_of_dissolved_iron_in_sea_water mole_concentration_of_dissolved_iron_in_sea_water [CF-Standard Name]; unit: mol m-3 surface_downwelling_longwave_flux_in_air surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2 surface_upward_mass_flux_of_carbon_dioxide_expressed_as_carbon_due_to_heterotrophic_respiration Carbon Mass Flux into Atmosphere Due to Heterotrophic Respiration on Land Comment: Carbon mass flux per unit area into atmosphere due to heterotrophic respiration on land (respiration by consumers) 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 tendency_of_mole_concentration_of_particulate_organic_matter_expressed_as_carbon_in_sea_water_due_to_net_primary_production tendency_of_mole_concentration_of_particulate_organic_matter_expressed_as_carbon_in_sea_water_due_to_net_primary_production [CF-Standard Name]; unit: mol m-3 s-1 carbon_mass_content_of_forestry_and_agricultural_products Carbon Mass in Products of Land-Use Change Comment: Carbon mass per unit area in that has been removed from the environment through land use change. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Eyr; Table Lmon, provided in frequency(s): mon; yrPt, 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 surface_partial_pressure_of_carbon_dioxide_in_sea_water surface_partial_pressure_of_carbon_dioxide_in_sea_water [CF-Standard Name]; unit: Pa sinking_mole_flux_of_particulate_organic_matter_expressed_as_carbon_in_sea_water cf:The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid. [CF-Standard Name]; unit: mol 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 litter_mass_content_of_carbon Carbon Mass in Litter Pool Comment: 'Litter' is dead plant material in or above the soil. It is distinct from coarse wood debris. The precise distinction between 'fine' and 'coarse' is model dependent. 'Content' indicates a quantity per unit area. The sum of the quantities with standard names surface_litter_mass_content_of_carbon and subsurface_litter_mass_content_of_carbon has the standard name litter_mass_content_of_carbon. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Eyr; Table Lmon, provided in frequency(s): mon; yrPt, 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 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 mole_concentration_of_dissolved_organic_carbon_in_sea_water "Mole concentration" means number of moles per unit volume, also called "molarity", and is used in the construction "mole_concentration_of_X_in_Y", where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as "nitrogen" or a phrase such as "nox_expressed_as_nitrogen". "Organic carbon" describes a family of chemical species and is the term used in standard names for all species belonging to the family that are represented within a given model. The list of individual species that are included in a quantity having a group chemical standard name can vary between models. Where possible, the data variable should be accompanied by a complete description of the species represented, for example, by using a comment attribute. [CF-Standard Name]; unit: mol m-3 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 sea_water_alkalinity_expressed_as_mole_equivalent sea_water_alkalinity_expressed_as_mole_equivalent [CF-Standard Name]; unit: mol m-3 area_fraction "Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01 area_fraction "Area fraction" means the fraction of horizontal area. To specify which area is quantified by a variable of "area_fraction", provide a coordinate variable or scalar coordinate variable of "area_type". Alternatively, if one is defined, use a more specific standard name of "X_area_fraction" for the fraction of horizontal area occupied by X. [CF-Standard Name]; unit: 0.01 ocean_mixed_layer_thickness_defined_by_sigma_t Ocean Mixed Layer Thickness Defined by Sigma T [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 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 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 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 upward_transformed_eulerian_mean_air_velocity Transformed Eulerian Mean Upward Wind Comment: Transformed Eulerian Mean Diagnostics w*, meridional component of the residual meridional circulation (v*, w*) derived from 6 hr or higher frequency data fields (use instantaneous daily fields or 12 hr fields if the 6 hr data are not available). Scale height: 6950 m Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m s-1 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 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 tendency_of_eastward_wind_due_to_eliassen_palm_flux_divergence Tendency of Eastward Wind Due to Eliassen-Palm Flux Divergence Comment: Tendency of the zonal mean zonal wind due to the divergence of the Eliassen-Palm flux. Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m s-2 sinking_mole_flux_of_calcite_expressed_as_carbon_in_sea_water cf:The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid. Calcite is a mineral that is a polymorph of calcium carbonate. The chemical formula of calcite is CaCO3. Standard names also exist for aragonite, another polymorph of calcium carbonate. [CF-Standard Name]; unit: mol m-2 s-1 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 northward_eliassen_palm_flux_in_air Northward Component of the Eliassen-Palm Flux Comment: Transformed Eulerian Mean Diagnostics Meridional component Fy of Eliassen-Palm (EP) flux (Fy, Fz) derived from 6hr or higher frequency fields (use daily fields or 12 hr fields if the 6 hr are not available). Please use the definitions given by equation 3.5.3a of Andrews, Holton and Leovy text book, but scaled by density to have units m3 s-2. Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m3 s-2 depth_of_isosurface_of_sea_water_potential_temperature Depth of 20 degree Celsius Isotherm Comment: This quantity, sometimes called the 'isotherm depth', is the depth (if it exists) at which the sea water potential temperature equals some specified value. This value should be specified in a scalar coordinate variable. Depth is the vertical distance below the surface. Potential temperature is the temperature a parcel of air or sea water would have if moved adiabatically to sea level pressure. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Eday; Table Emon, provided in frequency(s): day; mon, and for Realm(s): land; ocean. 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: m 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 surface_snow_thickness surface_snow_thickness [CF-Standard Name]; unit: m sinking_mole_flux_of_particulate_organic_matter_expressed_as_carbon_in_sea_water cf:The phrase 'expressed_as' is used in the construction A_expressed_as_B, where B is a chemical constituent of A. It means that the quantity indicated by the standard name is calculated solely with respect to the B contained in A, neglecting all other chemical constituents of A. In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. 'Sinking' is the gravitational settling of particulate matter suspended in a liquid. A sinking flux is positive downwards and is calculated relative to the movement of the surrounding fluid. [CF-Standard Name]; unit: mol m-2 s-1 northward_ocean_salt_transport Northward Ocean Salt Transport Comment: function of latitude, basin Used for mip era 'CMIP6' in CMOR MIP table(s): Table EmonZ, provided in frequency(s): mon, and for Realm(s): atmos; ocean. 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 s-1 tendency_of_eastward_wind_due_to_eliassen_palm_flux_divergence Tendency of Eastward Wind Due to Eliassen-Palm Flux Divergence Comment: Tendency of the zonal mean zonal wind due to the divergence of the Eliassen-Palm flux. Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m s-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 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 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 upward_eliassen_palm_flux_in_air Upward Component of the Eliassen-Palm Flux Comment: Transformed Eulerian Mean Diagnostics Meridional component Fz of the Eliassen-Palm (EP) flux (Fy, Fz) derived from 6hr or higher frequency fields (use daily fields or 12 hr fields if the 6 hr are not available). Please use the definitions given by equation 3.5.3b of Andrews, Holton and Leovy text book, but scaled by density to have units m3 s-2. Used for mip era 'CMIP6' in CMOR MIP table(s): Table EdayZ; Table EmonZ, provided in frequency(s): day; mon, and for Realm(s): atmos. 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: m3 s-2 surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 surface_air_pressure The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa upward_sea_water_velocity upward_sea_water_velocity [CF-Standard Name]; unit: m s-1 leaf_area_index "X_area" means the horizontal area occupied by X within the grid cell.[CF-Standard Name]; unit: 1 mole_concentration_of_dissolved_inorganic_phosphorus_in_sea_water Total Dissolved Inorganic Phosphorus Concentration Comment: Mole concentration means number of moles per unit volume, also called 'molarity', and is used in the construction 'mole_concentration_of_X_in_Y', where X is a material constituent of Y. A chemical or biological species denoted by X may be described by a single term such as 'nitrogen' or a phrase such as 'nox_expressed_as_nitrogen'. 'Dissolved inorganic phosphorus' means the sum of all inorganic phosphorus in solution (including phosphate, hydrogen phosphate, dihydrogen phosphate, and phosphoric acid). Used for mip era 'CMIP6' in CMOR MIP table(s): Table Omon; Table Oyr, provided in frequency(s): mon; yr, and for Realm(s): ocnBgchem. 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: mol m-3 surface_net_downward_longwave_flux The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. "Downward" indicates a vector component which is positive when directed downward (negative upward). Net downward radiation is the difference between radiation from above (downwelling) and radiation from below (upwelling). 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 dew_point_temperature Dew point temperature is the temperature at which a parcel of air reaches saturation upon being cooled at constant pressure and specific humidity. [CF-Standard Name]; unit: K 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 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 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 sea_water_potential_temperature sea_water_potential_temperature [CF-Standard Name]; unit: degC 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 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 global_average_thermosteric_sea_level_change Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m mole_concentration_of_nitrate_in_sea_water mole_concentration_of_nitrate_in_sea_water [CF-Standard Name]; unit: mol m-3 ocean_heat_y_transport Ocean Heat Y Transport [CF-Standard Name]; unit: W mole_concentration_of_zooplankton_expressed_as_carbon_in_sea_water mole_concentration_of_zooplankton_expressed_as_carbon_in_sea_water [CF-Standard Name]; unit: mol m-3 sea_water_salinity sea_water_salinity [CF-Standard Name]; unit: 0.001 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 sea_ice_surface_temperature sea_ice_surface_temperature [CF-Standard Name]; unit: K NetCDF 7927476 https://www.wdc-climate.de/ui/entry?acronym=C6_5285957 information collection n/a None