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wdc-climate.de:3953295 eng; USA collection C6CMNGGFEpc GFDL Climate Model Info contact Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov pointOfContact John P. Krasting Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov pointOfContact 2018-07-01T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: NOAA-GFDL GFDL-ESM4 model output prepared for CMIP6 CMIP piControl 2023-08-01 publication 1 C6CMNGGFEpc doi:10.26050/WDCC/AR6.C6CMNGGFEpc John P. Krasting Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: John.Krasting@noaa.gov author Jasmin G John Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Jasmin.John@noaa.gov author Chris Blanton Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: chris.blanton@noaa.gov author Colleen McHugh Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: colleen.mchugh@noaa.gov author Serguei Nikonov Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: serguei.nikonov@noaa.gov author Aparna Radhakrishnan Princeton University not filled Email: aparna.radhakrishnan@noaa.gov author Kristopher Rand Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: kristopher.rand@noaa.gov author Niki T. Zadeh Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Niki.Zadeh@noaa.gov author V Balaji Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: v.balaji@noaa.gov author Jeff Durachta Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: jeff.durachta@noaa.gov author Christopher Dupuis Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: christopher.dupuis@noaa.gov author Raymond Menzel Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: raymond.menzel@noaa.gov author Thomas Robinson Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: thomas.robinson@noaa.gov author Seth Underwood Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: seth.underwood@noaa.gov author Hans Vahlenkamp Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: hans.vahlenkamp@noaa.gov author Krista A. Dunne Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: kadunne@usgs.gov author Paul PG Gauthier Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: paul.gauthier@noaa.gov author Dr. Paul Ginoux Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Paul.Ginoux@noaa.gov author Stephen M. Griffies Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Stephen.Griffies@noaa.gov author Robert Hallberg Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Robert.Hallberg@noaa.gov author Matthew Harrison Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Matthew.Harrison@noaa.gov author William Hurlin Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: bill.hurlin@noaa.gov author Sergey Malyshev Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Sergey.Malyshev@noaa.gov author Vaishali Naik Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Vaishali.Naik@noaa.gov author Fabien Paulot Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: fabien.paulot@noaa.gov author David J Paynter Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: david.paynter@noaa.gov author Jeffrey Ploshay Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: jeff.ploshay@noaa.gov author Brandon G Reichl Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: brandon.reichl@noaa.gov author Daniel M Schwarzkopf Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Dan.Schwarzkopf@noaa.gov author Charles J Seman Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: charles.seman@noaa.gov author Levi Silvers Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: levi.silvers@noaa.gov author Bruce Wyman Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Bruce.Wyman@noaa.gov author Yujin Zeng Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: yujin.zeng@noaa.gov author Alistair Adcroft Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Alistair.Adcroft@noaa.gov author Dr. John P. Dunne Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: john.dunne@noaa.gov author Raphael Dussin Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Raphael.Dussin@noaa.gov author Huan Guo Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: huan.guo@noaa.gov author Jian He Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: jian.he@noaa.gov author Dr. Isaac M Held Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Isaac.Held@noaa.gov author Dr. Larry W. Horowitz Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: larry.horowitz@noaa.gov author Pu Lin Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: pu.lin@noaa.gov author P.C.D Milly Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: cmilly@usgs.gov author Elena Shevliakova Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Elena.Shevliakova@noaa.gov author Charles Stock Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: charles.stock@noaa.gov author Michael Winton Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: michael.winton@noaa.gov author Dr. Andrew T. Wittenberg Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Wittenberg@noaa.gov author Yuanyu Xie Princeton University not filled Email: yuanyu.xie@noaa.gov author Dr. Ming Zhao Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: ming.zhao@noaa.gov 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.CMIP.NOAA-GFDL.GFDL-ESM4.piControl' 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 GFDL-ESM4 climate model, released in 2018, includes the following components: aerosol: interactive, atmos: GFDL-AM4.1 (Cubed-sphere (c96) - 1 degree nominal horizontal resolution; 360 x 180 longitude/latitude; 49 levels; top level 1 Pa), atmosChem: GFDL-ATMCHEM4.1 (full atmospheric chemistry), land: GFDL-LM4.1, landIce: GFDL-LM4.1, ocean: GFDL-OM4p5 (GFDL-MOM6, tripolar - nominal 0.5 deg; 720 x 576 longitude/latitude; 75 levels; top grid cell 0-2 m), ocnBgchem: GFDL-COBALTv2, seaIce: GFDL-SIM4p5 (GFDL-SIS2.0, tripolar - nominal 0.5 deg; 720 x 576 longitude/latitude; 5 layers; 5 thickness categories). The model was run by the National Oceanic and Atmospheric Administration, Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA (NOAA-GFDL) in native nominal resolutions: aerosol: 100 km, atmos: 100 km, atmosChem: 100 km, land: 100 km, landIce: 100 km, ocean: 50 km, ocnBgchem: 50 km, seaIce: 50 km. GFDL Climate Model Info contact Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov pointOfContact John P. Krasting Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov pointOfContact NetCDF CMIP CMIP6 GFDL-ESM4 IPCC IPCC-AR6 IPCC-DDC NOAA-GFDL climate change model-output piControl 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 0001-01-16 0500-12-16 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 sea_water_salinity sea_water_salinity [CF-Standard Name]; unit: 0.001 sea_water_potential_temperature sea_water_potential_temperature [CF-Standard Name]; unit: degC 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 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 mole_fraction_of_carbon_dioxide_in_air Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: mol mol-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 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 toa_outgoing_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [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 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_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 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 atmosphere_mass_content_of_water_vapor atmosphere_mass_content_of_water_vapor [CF-Standard Name]; unit: kg m-2 relative_humidity relative_humidity [CF-Standard Name]; unit: 0.01 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_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 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 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 ocean_volume Ocean Grid-Cell Volume [CF-Standard Name]; unit: m3 surface_downwelling_longwave_flux_in_air surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2 global_average_thermosteric_sea_level_change Global Average Thermosteric Sea Level Change [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_snow_amount surface_snow_amount [CF-Standard Name]; unit: kg m-2 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 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 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_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 cell_area Model Grid-Cell Area [CF-Standard Name]; unit: m2 sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 leaf_area_index "X_area" means the horizontal area occupied by X within the grid cell.[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 mole_fraction_of_carbon_dioxide_in_air Mole fraction is used in the construction mole_fraction_of_X_in_Y, where X is a material constituent of Y. [CF-Standard Name]; unit: mol mol-1 surface_downward_heat_flux_in_sea_water surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2 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 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 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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [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_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 NetCDF 557059 https://www.wdc-climate.de/ui/entry?acronym=C6CMNGGFEpc information collection