2026-04-06T08:22:53Z http://dmoai.cloud.dkrz.de/oai/provider

oai:wdcc.dkrz.de:iso_3957026 2026-04-05T23:08:42Z iso-wdcc-doi

wdc-climate.de:3957026 eng; USA collection C6CMGIGE1 Dr. Gavin A. Schmidt NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ pointOfContact 2019-08-15T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: NASA-GISS GISS-E2-1-G-CC model output prepared for CMIP6 CMIP 2023-08-22 publication 1 C6CMGIGE1 doi:10.26050/WDCC/AR6.C6CMGIGE1 Dr. Gavin A. Schmidt NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: Gavin.A.Schmidt@nasa.gov author Max Kelley NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: mkelley@giss.nasa.gov author Larissa Nazarenko NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: larissa.s.nazarenko@nasa.gov author Ron Miller NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: ron.l.miller@nasa.gov author Gary L. Russell NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: Gary.L.Russell@nasa.gov author Susanne Bauer NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: susanne.e.bauer@nasa.gov author Rainer Bleck NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: rainer.bleck@nasa.gov author Michael Bauer NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: mpb20@columbia.edu author Shan Sun n/a n/a Email: shan.sun@noaa.gov author Vittorio Canuto NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: vittorio.canuto@nasa.gov author Ye Cheng NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: ye.cheng@nasa.gov author Thomas Clone NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: thomas.l.clune@nasa.gov author Anthony Del Genio NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: anthony.d.delgenio@nasa.gov author Greg Faluvegi NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: gregory.s.faluvegi@nasa.gov author Nancy Kiang NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: nancy.y.kiang@nasa.gov author Daehyun Kim University of Washington not filled Email: daehyun@uw.edu author Andrew Lacis NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: andrew.a.lacis@nasa.gov author Anthony Leboissetier NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: anthony.leboissetier@nasa.gov author Allegra LeGrande NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: allegra.n.legrande@nasa.gov author Ken Lo NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: kwok-wai.lo@nasa.gov author Elaine Matthews NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: elaine.matthews@nasa.gov author Lee Murray University of Rochester not filled Email: lee.murray@rochester.edu author Valdar Oinas NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: valdar.oinas@nasa.gov author Clara Orbe NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: clara.orbe@nasa.gov author Jan Perlwitz NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: jan.p.perlwitz@nasa.gov author Michael Puma NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: michael.j.puma@nasa.gov author David Rind NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: david.h.rind@nasa.gov author Anastasia Romanou NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: anastasia.romanou@nasa.gov author Drew Shindell Duke University not filled Email: drew.shindell@duke.edu author Nick Tausnev NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: nikolai.l.tausnev@nasa.gov author Kostas Tsigaridis NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: kostas.tsigaridis@nasa.gov author Ensheng Weng NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: ensheng.weng@nasa.gov author Jingbo Wu NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: jingbo.wu@nasa.gov author Mao-Sung Yao NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: mao-sung.yao@nasa.gov author Andrew Ackerman NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: andrew.ackerman@nasa.gov author Ann Fridlind NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ Email: ann.fridlind@nasa.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.NASA-GISS.GISS-E2-1-G-CC' 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 GISS-E2-1-G-CC climate model, released in 2019, includes the following components: aerosol: varies with physics-version (p==1 none, p==3 OMA, p==4 TOMAS, p==5 MATRIX), atmos: GISS-E2.1 (2 x 2.5 degrees; 144 x 90 longitude/latitude; 40 levels; top level 0.1 hPa), atmosChem: varies with physics-version (p==1 Non-interactive, p>1 GPUCCINI), land: GISS LSM, landIce: Fixed, ocean: GISS Ocean (1 deg; 360 x 180 longitude/latitude; 40 levels; top grid cell 0-10m), ocnBgchem: NOBM (NASA Ocean Biogeochemistry Model; same grid as ocean), seaIce: GISS SI (same grid as ocean). The model was run by the Goddard Institute for Space Studies, New York, NY 10025, USA (NASA-GISS) in native nominal resolutions: aerosol: 250 km, atmos: 250 km, atmosChem: 250 km, land: 250 km, landIce: 250 km, ocean: 100 km, ocnBgchem: 100 km, seaIce: 100 km. Dr. Gavin A. Schmidt NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ pointOfContact NetCDF CMIP CMIP6 GISS-E2-1-G-CC IPCC IPCC-AR6 IPCC-DDC NASA-GISS climate change model-output CC0-1.0: Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/ eng; USA 0.0 360.0 -90.0 90.0 gregorian 1850-01-16 2014-12-16 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_pressure_at_mean_sea_level Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL. Air pressure is the force per unit area which would be exerted when the moving gas molecules of which the air is composed strike a theoretical surface of any orientation. "Mean sea level" means the time mean of sea surface elevation at a given location over an arbitrary period sufficient to eliminate the tidal signals. [CF-Standard Name]; unit: Pa sea_water_salinity sea_water_salinity [CF-Standard Name]; unit: 0.001 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 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_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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K global_average_thermosteric_sea_level_change Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m 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 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 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_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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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 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_water_potential_temperature sea_water_potential_temperature [CF-Standard Name]; unit: degC air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K gross_primary_productivity_of_biomass_expressed_as_carbon Carbon Mass Flux out of Atmosphere Due to Gross Primary Production on Land Comment: The rate of synthesis of biomass from inorganic precursors by autotrophs ('producers') expressed as the mass of carbon which it contains. For example, photosynthesis in plants or phytoplankton. The producers also respire some of this biomass and the difference is referred to as the net primary production. Used for mip era 'CMIP6' in CMOR MIP table(s): Table E3hr; Table Lmon, provided in frequency(s): 3hr; mon, and for Realm(s): land. Codelist created on 2019-02-01 from https://github.com/PCMDI/cmip6-cmor-tables (CMOR Version=3.4; table_date(s):14 December 2018) [CF-Standard Name]; unit: kg m-2 s-1 atmosphere_mass_content_of_water_vapor atmosphere_mass_content_of_water_vapor [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 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 sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 toa_outgoing_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [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 ocean_meridional_overturning_mass_streamfunction Ocean Meridional Overturning Mass Streamfunction [CF-Standard Name]; unit: kg s-1 surface_snow_amount surface_snow_amount [CF-Standard Name]; unit: kg m-2 surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 surface_downwelling_longwave_flux_in_air surface_downwelling_longwave_flux_in_air [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 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 leaf_area_index "X_area" means the horizontal area occupied by X within the grid cell.[CF-Standard Name]; unit: 1 NetCDF 47188 https://www.wdc-climate.de/ui/entry?acronym=C6CMGIGE1 information collection