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wdc-climate.de:3956656 eng; USA collection C6CMEEEVEpc Lars Nieradzik Lund University not filled pointOfContact 2020-02-26T00:00:00 ISO 19115 ISO 19115-2:2009 IPCC DDC: EC-Earth-Consortium EC-Earth3-Veg model output prepared for CMIP6 CMIP piControl 2023-07-27 publication 1 C6CMEEEVEpc doi:10.26050/WDCC/AR6.C6CMEEEVEpc Jose Antonio Parodi-Perdomo Agencia Estatal de Meteorología not filled Email: jparodip@aemet.es author Jose María Rodríguez González Agencia Estatal de Meteorología not filled Email: jrodriguezg@aemet.es author Ernesto Rodríguez Camino Agencia Estatal de Meteorología not filled Email: erodriguezc@aemet.es author Mario Acosta Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: mario.acosta@bsc.es author Thomas Arsouze Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: thomas.arsouze@bsc.es) author Raffaele Bernardello Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: raffaele.bernardello@bsc.es author Louis-Philippe Caron Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: louis-philippe.caron@bsc.es author Roberto Bilbao Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: roberto.bilbao@bsc.es author Pierre-Antoine Bretonnière Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: pierre-antoine.bretonniere@bsc.es author Miguel Castrillo Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: miguel.castrillo@bsc.es author Francisco J. Doblas-Reyes Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: francisco.doblas-reyes@bsc.es author Pablo Echevarria Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: pablo.echevarria@bsc.es author Martin Ménégoz Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: martin.menegoz@bsc.es author Eduardo Moreno-Chamarro Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: eduardo.moreno@bsc.es author Arthur Ramos Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: arthur.amaral@bsc.es author Yohan Ruprich-Robert Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: yohan.ruprich@bsc.es author Étienne Tourigny Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: etienne.tourigny@bsc.es author Simon Wild Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: simon.wild@bsc.es author Jost von Hardenberg Consiglio Nazionale delle Ricerche not filled Email: j.vonhardenberg@isac.cnr.it author Paolo Davini Consiglio Nazionale delle Ricerche not filled Email: p.davini@isac.cnr.it author Dr. Shuting Yang Danish Meteorological Institute http://research.dmi.dk/ Email: shuting@dmi.dk author Marianne Sloth Madsen Danish Meteorological Institute http://research.dmi.dk/ Email: msm@dmi.dk author Tian Tian Danish Meteorological Institute http://research.dmi.dk/ Email: tian@dmi.dk author Paul Nolan Irish Centre for High-End Computing not filled Email: paul.nolan@ichec.ie author Alastair McKinstry Irish Centre for High-End Computing http://www.ichec.ie Email: alastair.mckinstry@ichec.ie author Twan van Noije Royal Netherlands Meteorological Institute not filled Email: noije@knmi.nl author Philippe Le Sager Royal Netherlands Meteorological Institute not filled Email: sager@knmi.nl author Tommi Bergman Finnish Meteorological Institute http://en.ilmatieteenlaitos.fi/ Email: Tommi.Bergman@fmi.fi author Thomas Reerink Royal Netherlands Meteorological Institute not filled Email: reerink@knmi.nl author Gijs van den Oord Royal Netherlands Meteorological Institute not filled Email: g.vandenoord@esciencecenter.nl author Frank Selten Royal Netherlands Meteorological Institute not filled Email: selten@knmi.nl author Michiel van Weele Royal Netherlands Meteorological Institute not filled Email: weelevm@knmi.nl author Bart van den Hurk Royal Netherlands Meteorological Institute not filled Email: hurkvd@knmi.nl author Richard Bintanja Royal Netherlands Meteorological Institute not filled Email: bintanja@knmi.nl author Camiel Severijns Royal Netherlands Meteorological Institute not filled Email: camiel.severijns@knmi.nl author Andreas Sterl Royal Netherlands Meteorological Institute not filled Email: andreas.sterl@knmi.nl author Rein Haarsma Royal Netherlands Meteorological Institute not filled Email: haarsma@knmi.nl author Andrea Alessandri Institute of Atmospheric Sciences and Climate not filled Email: a.alessandri@isac.cnr.it author Torben Schmith Danish Meteorological Institute http://research.dmi.dk/ Email: ts@dmi.dk author Paul Miller Lund University not filled Email: paul.miller@nateko.lu.se author Lars Nieradzik Lund University not filled Email: lars.nieradzik@nateko.lu.se author Ben Smith Lund University not filled Email: ben.smith.lu@gmail.com author Stefan Olin Lund University not filled Email: stefan.olin@nateko.lu.se author Mats Lindeskog Lund University not filled Email: mats.lindeskog@nateko.lu.se author Johan Nord Lund University not filled Email: johan.nord@nateko.lu.se author Jan Julin Lund University not filled Email: jan.julin@protonmail.com author Jonathan McGovern Met Eireann not filled Email: jonathan.mcgovern@met.ie author Qiang Li Department of Physical Geography, Stockholm University not filled Email: qiang.li@natgeo.su.se author Jenson Zhang Department of Physical Geography, Stockholm University not filled Email: jenson.zhang@natgeo.su.se author Ralf Döscher Swedish Meteorological and Hydrological Institute not filled Email: ralf.doescher@smhi.se author Uwe Fladrich Swedish Meteorological and Hydrological Institute not filled Email: uwe.fladrich@smhi.se author Torben Koenigk Swedish Meteorological and Hydrological Institute not filled Email: torben.koenigk@smhi.se author Klaus Zimmermann Swedish Meteorological and Hydrological Institute not filled Email: klaus.zimmermann@smhi.se author Pasha Karami Swedish Meteorological and Hydrological Institute not filled Email: pasha.karami@smhi.se author Ramon Fuentes Franco Swedish Meteorological and Hydrological Institute not filled Email: ramon.fuentesfranco@smhi.se author Shiyu Wang Swedish Meteorological and Hydrological Institute not filled Email: shiyu.wang@smhi.se author Ulrika Willén Swedish Meteorological and Hydrological Institute not filled Email: ulrika.willen@smhi.se author Klaus Wyser Swedish Meteorological and Hydrological Institute not filled Email: klaus.wyser@smhi.se author Jukka-Pekka Keskinen University of Helsinki https://tuhat.halvi.helsinki.fi Email: jukka-pekka.keskinen@helsinki.fi author Valentina Sicardi Barcelona Supercomputing Center - Centro Nacional de Supercomputación not filled Email: valentina.sicardi@bsc.es author Qiong Zhang Department of Physical Geography, Stockholm University not filled Email: qiong.zhang@natgeo.su.se author Mariana Adam Joint Research Centre not filled Email: mariana.adam@inoe.ro author Emanuel Dutra Instituto Português do Mar e Atmosfera not filled Email: emanuel.dutra@ipma.pt author Ricardo Tomé Instituto Dom Luiz not filled Email: rftome@fc.ul.pt 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.EC-Earth-Consortium.EC-Earth3-Veg.piControl' 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 EC-Earth3-Veg climate model, released in 2019, includes the following components: atmos: IFS cy36r4 (TL255, linearly reduced Gaussian grid equivalent to 512 x 256 longitude/latitude; 91 levels; top level 0.01 hPa), land: HTESSEL (land surface scheme built in IFS) and LPJ-GUESS v4, ocean: NEMO3.6 (ORCA1 tripolar primarily 1 degree with meridional refinement down to 1/3 degree in the tropics; 362 x 292 longitude/latitude; 75 levels; top grid cell 0-1 m), seaIce: LIM3. The model was run by the AEMET, Spain; BSC, Spain; CNR-ISAC, Italy; DMI, Denmark; ENEA, Italy; FMI, Finland; Geomar, Germany; ICHEC, Ireland; ICTP, Italy; IDL, Portugal; IMAU, The Netherlands; IPMA, Portugal; KIT, Karlsruhe, Germany; KNMI, The Netherlands; Lund University, Sweden; Met Eireann, Ireland; NLeSC, The Netherlands; NTNU, Norway; Oxford University, UK; surfSARA, The Netherlands; SMHI, Sweden; Stockholm University, Sweden; Unite ASTR, Belgium; University College Dublin, Ireland; University of Bergen, Norway; University of Copenhagen, Denmark; University of Helsinki, Finland; University of Santiago de Compostela, Spain; Uppsala University, Sweden; Utrecht University, The Netherlands; Vrije Universiteit Amsterdam, the Netherlands; Wageningen University, The Netherlands. Mailing address: EC-Earth consortium, Rossby Center, Swedish Meteorological and Hydrological Institute/SMHI, SE-601 76 Norrkoping, Sweden (EC-Earth-Consortium) in native nominal resolutions: atmos: 100 km, land: 100 km, ocean: 100 km, seaIce: 100 km. Individuals using the data must abide by terms of use for CMIP6 data (https://pcmdi.llnl.gov/CMIP6/TermsOfUse). The original license restrictions on these datasets were recorded as global attributes in the data files, but these may have been subsequently updated. Lars Nieradzik Lund University not filled pointOfContact NetCDF CMIP CMIP6 EC-Earth-Consortium EC-Earth3-Veg IPCC IPCC-AR6 IPCC-DDC climate change model-output piControl 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 2349-12-16 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 water_evapotranspiration_flux Snow Evaporation Comment: Water here means water in all phases. Evaporation is the conversion of liquid or solid into vapor. (The conversion of solid alone into vapor is called 'sublimation'.) In accordance with common usage in geophysical disciplines, 'flux' implies per unit area, called 'flux density' in physics. Unless indicated in the cell_methods attribute, a quantity is assumed to apply to the whole area of each horizontal grid box. Previously, the qualifier where_type was used to specify that the quantity applies only to the part of the grid box of the named type. Names containing the where_type qualifier are deprecated and newly created data should use the cell_methods attribute to indicate the horizontal area to which the quantity applies. Used for mip era 'CMIP6' in CMOR MIP table(s): Table Eday, provided in frequency(s): day, 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 toa_outgoing_shortwave_flux_assuming_clear_sky toa_outgoing_shortwave_flux_assuming_clear_sky [CF-Standard Name]; unit: W m-2 sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 0.01 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_downwelling_shortwave_flux_in_air surface_downwelling_shortwave_flux_in_air [CF-Standard Name]; unit: W 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 global_average_thermosteric_sea_level_change Global Average Thermosteric Sea Level Change [CF-Standard Name]; unit: m leaf_area_index "X_area" means the horizontal area occupied by X within the grid cell.[CF-Standard Name]; unit: 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 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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 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_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 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 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 relative_humidity relative_humidity [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 NetCDF 35851 https://www.wdc-climate.de/ui/entry?acronym=C6CMEEEVEpc information collection