wdc-climate.de:3953699 eng; USA collection C6ACGIGE1 Susanne Bauer NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ pointOfContact Kostas Tsigaridis 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 AerChemMIP 2023-08-08 publication 1 C6ACGIGE1 doi:10.26050/WDCC/AR6.C6ACGIGE1 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.AerChemMIP.NASA-GISS.GISS-E2-1-G' 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 Kostas Tsigaridis NASA Goddard Institute for Space Studies http://www.giss.nasa.gov/ pointOfContact NetCDF AerChemMIP CMIP6 GISS-E2-1-G 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 2100-12-16 mass_fraction_of_sea_salt_dry_aerosol_particles_in_air sea-salt aerosol Mass Mixing Ratio Comment: Mass fraction in the atmosphere of sea salt aerosol (dry mass). 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: kg kg-1 mass_fraction_of_pm2p5_dry_aerosol_particles_in_air PM2.5 Mass Mixing Ratio Comment: Mass fraction atmospheric particulate compounds with an aerodynamic diameter of less than or equal to 2.5 micrometers 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: kg kg-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 mass_fraction_of_pm2p5_dry_aerosol_particles_in_air PM2.5 Mass Mixing Ratio Comment: Mass fraction atmospheric particulate compounds with an aerodynamic diameter of less than or equal to 2.5 micrometers 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: kg kg-1 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 mole_fraction_of_ozone_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 mass_fraction_of_sulfate_dry_aerosol_particles_in_air Aerosol Sulfate Mass Mixing Ratio Comment: Dry mass of sulfate (SO4) in aerosol particles as a fraction of air mass. 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: kg kg-1 mass_fraction_of_elemental_carbon_dry_aerosol_particles_in_air Elemental Carbon Mass Mixing Ratio Comment: Dry mass fraction of black carbon aerosol particles in air. 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: kg kg-1 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 mole_fraction_of_ozone_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 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 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 mass_fraction_of_dust_dry_aerosol_particles_in_air Dust Aerosol Mass Mixing Ratio Comment: Dry mass fraction of dust aerosol particles in air. 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: kg kg-1 mass_fraction_of_particulate_organic_matter_dry_aerosol_particles_in_air Total Organic Aerosol Mass Mixing Ratio Comment: We recommend a scale factor of POM=1.4*OC, unless your model has more detailed info available. 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: kg kg-1 NetCDF 73544 https://www.wdc-climate.de/ui/entry?acronym=C6ACGIGE1 information collection