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wdc-climate.de:3943640 eng; USA collection C6DANCCNLHG Øyvind Seland Norwegian Meteorological Institute https://www.met.no pointOfContact 2019-11-08T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: NCC NorESM2-LM model output prepared for CMIP6 DAMIP hist-GHG 2023-08-16 publication 1 C6DANCCNLHG doi:10.26050/WDCC/AR6.C6DANCCNLHG Øyvind Seland Norwegian Meteorological Institute https://www.met.no Email: oyvind.seland@met.no author Mats Bentsen NORCE Norwegian Research Centre https://www.norceresearch.no Email: mben@norceresearch.no author Dirk Jan Leo Oliviè Norwegian Meteorological Institute https://www.met.no Email: dirk.j.l.olivie@met.no author Thomas Toniazzo NORCE Norwegian Research Centre https://www.norceresearch.no Email: thto@norceresearch.no author Ada Gjermundsen Norwegian Meteorological Institute https://www.met.no Email: ada.gjermundsen@met.no author Lise Seland Graff Norwegian Meteorological Institute https://www.met.no Email: lise.s.graff@met.no author Jens Boldingh Debernard Norwegian Meteorological Institute https://www.met.no Email: jens.debernard@met.no author Alok Kumar Gupta NORCE Norwegian Research Centre https://www.norceresearch.no Email: algu@norceresearch.no author Yanchun He Nansen Environmental and Remote Sensing Center https://www.nersc.no Email: yanchun.he@nersc.no author Alf Kirkevåg Norwegian Meteorological Institute https://www.met.no Email: alf.kirkevag@met.no author Jörg Schwinger NORCE Norwegian Research Centre https://www.norceresearch.no Email: jorg.schwinger@norceresearch.no author Jerry Tjiputra NORCE Norwegian Research Centre https://www.norceresearch.no Email: jerry.tjiputra@norceresearch.no author Kjetil Schanke Aas University of Oslo https://www.mn.uio.no/geo/ Email: k.s.aas@geo.uio.no author Ingo Bethke University of Bergen https://www.uib.no/en/gfi Email: ingo.bethke@uib.no author Yuanchao Fan NORCE Norwegian Research Centre https://www.norceresearch.no Email: ycfan@g.harvard.edu author Jan Griesfeller Norwegian Meteorological Institute https://www.met.no Email: jan.griesfeller@met.no author Alf Grini Norwegian Meteorological Institute https://www.met.no Email: alfg@met.no author Chuncheng Guo NORCE Norwegian Research Centre https://www.norceresearch.no Email: chgu@norceresearch.no author Mehmet Ilicak NORCE Norwegian Research Centre https://www.norceresearch.no Email: meil@norceresearch.no author Inger Helene Hafsahl Karset University of Oslo https://www.mn.uio.no/geo/ Email: i.h.h.karset@geo.uio.no author Oskar Andreas Landgren Norwegian Meteorological Institute https://www.met.no Email: oskar.a.landgren@met.no author Johan Liakka Nansen Environmental and Remote Sensing Center https://www.nersc.no Email: johan.liakka@nersc.no author Kine Onsum Moseid Norwegian Meteorological Institute https://www.met.no Email: kine.onsum.moseid@met.no author Aleksi Nummelin NORCE Norwegian Research Centre https://www.norceresearch.no Email: alnu@norceresearch.no author Clemens Spensberger University of Bergen https://www.uib.no/en/gfi Email: clemens.spensberger@uib.no author Hui Tang University of Oslo https://www.mn.uio.no/geo/ Email: hui.tang@geo.uio.no author Zhongshi Zhang NORCE Norwegian Research Centre https://www.norceresearch.no Email: zhzh@norceresearch.no author Christoph Heinze University of Bergen https://www.uib.no/en/gfi Email: christoph.heinze@uib.no author Trond Iversen Norwegian Meteorological Institute https://www.met.no Email: trond.iversen@met.no author Michael Schulz Norwegian Meteorological Institute https://www.met.no Email: michael.schulz@met.no 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.DAMIP.NCC.NorESM2-LM.hist-GHG' 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 NorESM2-LM (low atmosphere-medium ocean resolution, GHG concentration driven) climate model, released in 2017, includes the following components: aerosol: OsloAero, atmos: CAM-OSLO (2 degree resolution; 144 x 96; 32 levels; top level 3 mb), atmosChem: OsloChemSimp, land: CLM, landIce: CISM, ocean: MICOM (1 degree resolution; 360 x 384; 70 levels; top grid cell minimum 0-2.5 m [native model uses hybrid density and generic upper-layer coordinate interpolated to z-level for contributed data]), ocnBgchem: HAMOCC, seaIce: CICE. The model was run by the NorESM Climate modeling Consortium consisting of CICERO (Center for International Climate and Environmental Research, Oslo 0349), MET-Norway (Norwegian Meteorological Institute, Oslo 0313), NERSC (Nansen Environmental and Remote Sensing Center, Bergen 5006), NILU (Norwegian Institute for Air Research, Kjeller 2027), UiB (University of Bergen, Bergen 5007), UiO (University of Oslo, Oslo 0313) and UNI (Uni Research, Bergen 5008), Norway. Mailing address: NCC, c/o MET-Norway, Henrik Mohns plass 1, Oslo 0313, Norway (NCC) 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. Øyvind Seland Norwegian Meteorological Institute https://www.met.no pointOfContact NetCDF CMIP6 DAMIP IPCC IPCC-AR6 IPCC-DDC NCC NorESM2-LM climate change hist-GHG 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 1850-01-16 2020-12-16 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K ocean_volume Ocean Grid-Cell Volume [CF-Standard Name]; unit: m3 leaf_area_index "X_area" means the horizontal area occupied by X within the grid cell.[CF-Standard Name]; unit: 1 global_average_thermosteric_sea_level_change Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m 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 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 sea_water_potential_temperature sea_water_potential_temperature [CF-Standard Name]; unit: degC surface_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W m-2 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_downward_heat_flux_in_sea_water surface_downward_heat_flux_in_sea_water [CF-Standard Name]; unit: W m-2 surface_snow_amount surface_snow_amount [CF-Standard Name]; unit: kg 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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K surface_downwelling_longwave_flux_in_air surface_downwelling_longwave_flux_in_air [CF-Standard Name]; unit: W m-2 sea_water_salinity sea_water_salinity [CF-Standard Name]; unit: 0.001 toa_outgoing_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2 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 atmosphere_mass_content_of_water_vapor atmosphere_mass_content_of_water_vapor [CF-Standard Name]; unit: kg 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_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 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 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 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_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 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 sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 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 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_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 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 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 NetCDF 213756 https://www.wdc-climate.de/ui/entry?acronym=C6DANCCNLHG information collection