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wdc-climate.de:3907182 eng; USA collection C6CMCSIACCam Dr. Chloe Mackallah Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au pointOfContact Martin Dix Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au pointOfContact 2020-08-17T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: CSIRO-ARCCSS ACCESS-CM2 model output prepared for CMIP6 CMIP amip 2023-07-25 publication 1 C6CMCSIACCam doi:10.26050/WDCC/AR6.C6CMCSIACCam Martin Dix Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: martin.dix@csiro.au author Daohua Bi Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: dave.bi@csiro.au author Peter Dobrohotoff Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: peter.dobrohotoff@csiro.au author Russell Fiedler Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: russ.fiedler@csiro.au author Ian Harman Commonwealth Scientific & Industrial Research Organisation http://www.csiro.au Email: ian.harman@csiro.au author Rachel Law Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: rachel.law@csiro.au author Dr. Chloe Mackallah Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: Chloe.Mackallah@csiro.au author Simon Marsland Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: simon.marsland@csiro.au author Siobhan O'Farrell Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: siobhan.o'farrell@csiro.au author Harun Rashid Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: harun.rashid@csiro.au author Jhan Srbinovsky Commonwealth Scientific & Industrial Research Organisation http://www.csiro.au Email: jhan.srbinovsky@csiro.au author Arnold Sullivan Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: arnold.sullivan@csiro.au author Claire Trenham Commonwealth Scientific & Industrial Research Organisation http://www.csiro.au Email: Claire.Trenham@csiro.au author Peter Vohralik Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: peter.vohralik@csiro.au author Ian Watterson Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: ian.watterson@csiro.au author Gareth Williams Commonwealth Scientific & Industrial Research Organisation http://www.csiro.au Email: gareth.williams@csiro.au author Matthew Woodhouse Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au Email: matthew.woodhouse@csiro.au author Roger Bodman Commonwealth Scientific & Industrial Research Organisation http://www.csiro.au Email: roger.bodman@csiro.au author Fabio Boeira Dias University of Tasmania http://www.imas.utas.edu.au/ Email: fabio.dias@utas.edu.au author Catia M. Domingues University of Tasmania http://www.imas.utas.edu.au/ Email: catiad@utas.edu.au author Nicholas Hannah ARC Centre of Excellence for Climate System Science http://www.climatescience.org.au/tags/arccss Email: nchlshnnh@gmail.com author Aidan Heerdegen Australian National University not filled Email: aidan.heerdegen@anu.edu.au author Abhishek Savita University of Tasmania http://www.imas.utas.edu.au/ Email: asavita@geomar.de author Scott Wales University of Melbourne not filled Email: scott.wales@unimelb.edu.au author Chris Allen National Computational Infrastructure http://nci.org.au Email: chris.allen@anu.edu.au author Dr. Kelsey Druken National Computational Infrastructure http://nci.org.au Email: kelsey.druken@anu.edu.au author Dr. Ben Evans National Computational Infrastructure http://nci.org.au Email: Ben.Evans@anu.edu.au author Clare Richards National Computational Infrastructure http://nci.org.au Email: clare.richards@anu.edu.au author Syazwan Mohamed Ridzwan National Computational Infrastructure http://nci.org.au Email: Syazwan.MohamedRidzwan@anu.edu.au author Dale Roberts National Computational Infrastructure http://nci.org.au Email: ds.roberts@anu.edu.au author Jon Smillie National Computational Infrastructure http://nci.org.au Email: jon.smillie@anu.edu.au author Kate Snow National Computational Infrastructure http://nci.org.au Email: kate.snow@anu.edu.au author Marshall Ward National Computational Infrastructure http://nci.org.au Email: marshall.ward@anu.edu.au author Rui Yang National Computational Infrastructure http://nci.org.au Email: rui.yang@anu.edu.au 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.CSIRO-ARCCSS.ACCESS-CM2.amip' 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 Australian Community Climate and Earth System Simulator Climate Model Version 2 climate model, released in 2019, includes the following components: aerosol: UKCA-GLOMAP-mode, atmos: MetUM-HadGEM3-GA7.1 (N96; 192 x 144 longitude/latitude; 85 levels; top level 85 km), land: CABLE2.5, ocean: ACCESS-OM2 (GFDL-MOM5, tripolar primarily 1deg; 360 x 300 longitude/latitude; 50 levels; top grid cell 0-10 m), seaIce: CICE5.1.2 (same grid as ocean). The model was run by the CSIRO (Commonwealth Scientific and Industrial Research Organisation, Aspendale, Victoria 3195, Australia), ARCCSS (Australian Research Council Centre of Excellence for Climate System Science). Mailing address: CSIRO, c/o Simon J. Marsland, 107-121 Station Street, Aspendale, Victoria 3195, Australia (CSIRO-ARCCSS) in native nominal resolutions: aerosol: 250 km, atmos: 250 km, land: 250 km, ocean: 100 km, seaIce: 100 km. Dr. Chloe Mackallah Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au pointOfContact Martin Dix Commonwealth Scientific & Industrial Research Organisation http://www.cmar.csiro.au pointOfContact NetCDF ACCESS-CM2 CMIP CMIP6 CSIRO-ARCCSS IPCC IPCC-AR6 IPCC-DDC amip climate change 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 1979-01-16 2014-12-16 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 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 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_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2 atmosphere_mass_content_of_water_vapor atmosphere_mass_content_of_water_vapor [CF-Standard Name]; unit: kg 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 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 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 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 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 soil_temperature Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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 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 surface_downwelling_longwave_flux_in_air surface_downwelling_longwave_flux_in_air [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 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 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 NetCDF 7038 https://www.wdc-climate.de/ui/entry?acronym=C6CMCSIACCam information collection