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wdc-climate.de:3923764 eng; USA collection C6SPGIGEGs434 Susanne Bauer NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ pointOfContact 2020-01-15T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: NASA-GISS GISS-E2.1G model output prepared for CMIP6 ScenarioMIP ssp434 2023-08-07 publication 1 C6SPGIGEGs434 doi:10.26050/WDCC/AR6.C6SPGIGEGs434 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.ScenarioMIP.NASA-GISS.GISS-E2-1-G.ssp434' 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-E2.1G 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 (2.5x2 degree; 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, ocean: GISS Ocean (GO1, 1 degree; 360 x 180 longitude/latitude; 40 levels; top grid cell 0-10 m), seaIce: GISS SI. 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, ocean: 100 km, seaIce: 250 km. Susanne Bauer NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ pointOfContact NetCDF CMIP6 GISS-E2-1-G IPCC IPCC-AR6 IPCC-DDC NASA-GISS ScenarioMIP climate change model-output ssp434 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 2015-01-16 2100-12-16 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 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_air_pressure The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa 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_downward_eastward_stress The surface called "surface" means the lower boundary of the atmosphere. "Eastward" indicates a vector component which is positive when directed eastward (negative westward). "Downward" indicates a vector component which is positive when directed downward (negative upward). "Downward eastward" indicates the ZX component of a tensor. A downward eastward stress is a downward flux of eastward momentum, which accelerates the lower medium eastward and the upper medium westward. The surface downward stress is the windstress on the surface. [CF-Standard Name]; unit: Pa sea_surface_salinity The unit of salinity is PSU, which is dimensionless. The units attribute should be given as 1e-3 or 0.001 i.e. parts per thousand if salinity is in PSU. Sea surface salinity is often abbreviated as "SSS". For the salinity of sea water at a particular depth or layer, a data variable of sea_water_salinity with a vertical coordinate axis should be used. [CF-Standard Name]; unit: 0.001 surface_upwelling_longwave_flux_in_air The surface called "surface" means the lower boundary of the atmosphere. "longwave" means longwave radiation. Upwelling radiation is radiation from below. It does not mean "net upward". When thought of as being incident on a surface, a radiative flux is sometimes called "irradiance". In addition, it is identical with the quantity measured by a cosine-collector light-meter and sometimes called "vector irradiance". In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: W m-2 wind_speed Speed is the magnitude of velocity. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1 surface_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 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 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_surface_height_above_geoid sea_surface_height_above_geoid [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 northward_wind "Northward" indicates a vector component which is positive when directed northward (negative southward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1 eastward_wind "Eastward" indicates a vector component which is positive when directed eastward (negative westward). Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.) [CF-Standard Name]; unit: m s-1 surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 geopotential_height Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. It is numerically similar to the altitude (or geometric height) and not to the quantity with standard name height, which is relative to the surface. [CF-Standard Name]; unit: m 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 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 surface_snow_thickness surface_snow_thickness [CF-Standard Name]; unit: m 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 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 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_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 relative_humidity relative_humidity [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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K cloud_area_fraction "X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 0.01 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K surface_snow_amount surface_snow_amount [CF-Standard Name]; unit: kg m-2 NetCDF 5834 https://www.wdc-climate.de/ui/entry?acronym=C6SPGIGEGs434 information collection