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wdc-climate.de:3949225 eng; USA collection C6HRNGGFDH1 GFDL Climate Model Info contact 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-CM4C192 model output prepared for CMIP6 HighResMIP hist-1950 2023-08-21 publication 1 C6HRNGGFDH1 doi:10.26050/WDCC/AR6.C6HRNGGFDH1 Dr. Ming Zhao Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: ming.zhao@noaa.gov author Chris Blanton Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: chris.blanton@noaa.gov author Jasmin G John Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Jasmin.John@noaa.gov author Aparna Radhakrishnan Princeton University not filled Email: aparna.radhakrishnan@noaa.gov author Niki T. Zadeh Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Niki.Zadeh@noaa.gov author Colleen McHugh Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: colleen.mchugh@noaa.gov author Kristopher Rand Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: kristopher.rand@noaa.gov author Hans Vahlenkamp Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: hans.vahlenkamp@noaa.gov author Chandin Wilson Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Chandin.Wilson@noaa.gov author Dr. Paul Ginoux Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Paul.Ginoux@noaa.gov author Sergey Malyshev Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Sergey.Malyshev@noaa.gov author Bruce Wyman Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Bruce.Wyman@noaa.gov author Huan Guo Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: huan.guo@noaa.gov author V Balaji Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: v.balaji@noaa.gov author Dr. Isaac M Held Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Isaac.Held@noaa.gov author Dr. John P. Dunne Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: john.dunne@noaa.gov author Michael Winton Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: michael.winton@noaa.gov author Alistair Adcroft Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: Alistair.Adcroft@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 Thomas Knutson Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: tom.knutson@noaa.gov author Jeffrey Ploshay Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: jeff.ploshay@noaa.gov author Yujin Zeng Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov Email: yujin.zeng@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.HighResMIP.NOAA-GFDL.GFDL-CM4C192.hist-1950' 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-CM4C192 climate model, released in 2018, includes the following components: aerosol: interactive, atmos: GFDL-AM4C192 (Cubed-sphere (c192) - 0.5 degree nominal horizontal resolution; 720 x 360 longitude/latitude; 33 levels; top level 1 hPa), atmosChem: fast chemistry, aerosol only, land: GFDL-LM4.0.1, landIce: GFDL-LM4.0.1, ocean: GFDL-OM4p25 (GFDL-MOM6, tripolar - nominal 0.25 deg; 1440 x 1080 longitude/latitude; 75 levels; top grid cell 0-2 m), seaIce: GFDL-SIM4p25 (GFDL-SIS2.0, tripolar - nominal 0.25 deg; 1440 x 1080 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: 50 km, atmos: 50 km, atmosChem: 50 km, land: 50 km, landIce: 50 km, ocean: 25 km, seaIce: 25 km. GFDL Climate Model Info contact Geophysical Fluid Dynamics Laboratory/NOAA http://www.gfdl.noaa.gov pointOfContact NetCDF CMIP6 GFDL-CM4C192 HighResMIP IPCC IPCC-AR6 IPCC-DDC NOAA-GFDL climate change hist-1950 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 gregorian 1950-01-16 2014-12-16 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_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 air_temperature Air temperature is the bulk temperature of the air, 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 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 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_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 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_downwelling_longwave_flux_in_air surface_downwelling_longwave_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 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 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 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_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 toa_outgoing_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2 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 surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 NetCDF 38854 https://www.wdc-climate.de/ui/entry?acronym=C6HRNGGFDH1 information collection