wdc-climate.de:3878678 eng; USA collection RCM_CMIP6_SSP126-HR_r1i1p1f1 Martin Schupfner Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact Martin Schupfner Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact 2020-01-10T13:43:37 ISO 19115 ISO 19115-2:2009 CMIP6 ScenarioMIP DKRZ MPI-ESM1-2-HR ssp126_r1i1p1f1 - RCM-forcing data 2020-04-08 publication 1 RCM_CMIP6_SSP126-HR_r1i1p1f1 doi:10.26050/WDCC/RCM_CMIP6_SSP126-HR_r1i1p1f1 Martin Schupfner Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: schupfner@dkrz.de principalInvestigator Martin Schupfner Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: schupfner@dkrz.de author Karl-Hermann Wieners Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: Karl-Hermann.Wieners@mpimet.mpg.de author Fabian Wachsmann Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: wachsmann@dkrz.de author Christian Steger Deutscher Wetterdienst https://www.dwd.de/ Email: christian.steger@dwd.de author Matthias Bittner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: matthias.bittner@mpimet.mpg.de author Dr. Johann Jungclaus Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: johann.jungclaus@mpimet.mpg.de author Dr. Barbara Früh Deutscher Wetterdienst https://www.dwd.de/ Email: Barbara.Frueh@dwd.de author Klaus Pankatz Deutscher Wetterdienst https://www.dwd.de/ Email: Klaus.Pankatz@dwd.de author Dr. Marco Giorgetta Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: cordex-cclm@dkrz.de author Dr. Christian Reick Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: christian.reick@mpimet.mpg.de author Dr. Stephanie Legutke Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: legutke@dkrz.de author Monika Esch Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: monika.esch@mpimet.mpg.de author Veronika Gayler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: veronika.gayler@mpimet.mpg.de author Dr. Helmuth Haak Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: helmuth.haak@mpimet.mpg.de author Philipp de Vrese Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: philipp.de-vrese@mpimet.mpg.de author Dr. Thomas Raddatz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: thomas.raddatz@mpimet.mpg.de author Dr. Thorsten Mauritsen Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: thorsten.mauritsen@mpimet.mpg.de author Dr. Jin-Song von Storch Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: jin-song.von.storch@mpimet.mpg.de author Jörg Behrens Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: behrens@dkrz.de author Dr. Victor Brovkin Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: victor.brovkin@mpimet.mpg.de author Prof. Martin Claussen Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: martin.claussen@mpimet.mpg.de author Dr. Traute Crueger Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: traute.crueger@mpimet.mpg.de author Irina Fast Deutsches Klimarechenzentrum http://www.dkrz.de/ Email: fast@dkrz.de author Stephanie Fiedler Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: stephanie.fiedler@mpimet.mpg.de author Dr. Stefan Hagemann Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: stefan.hagemann@hereon.de author Cathy Hohenegger Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: cathy.hohenegger@mpimet.mpg.de author Thomas Jahns Deutsches Klimarechenzentrum http://www.dkrz.de/ author Silvia Kloster Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: silvia.kloster@mpimet.mpg.de author Dr. Stefan Kinne Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: stefan.kinne@mpimet.mpg.de author Gitta Lasslop Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: gitta.lasslop@senckenberg.de author Dr. Luis Kornblueh Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: luis.kornblueh@mpimet.mpg.de author Prof. Jochem Marotzke Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: jochem.marotzke@mpimet.mpg.de author Dr. Daniela Matei Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: daniela.matei@mpimet.mpg.de author Katharina Meraner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: katharina.meraner@mpimet.mpg.de author Dr. Uwe Mikolajewicz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: uwe.mikolajewicz@mpimet.mpg.de author Kameswarrao Modali Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: modali@dkrz.de author Dr. Wolfgang Müller Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: wolfgang.mueller@mpimet.mpg.de author Dr. Julia Nabel Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: julia.nabel@mpimet.mpg.de author Dr. Dirk Notz Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: dirk.notz@mpimet.mpg.de author Dr. Karsten Peters Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: karsten.peters@mpimet.mpg.de author Robert Pincus University of Colorado http://www.colorado.edu/ Email: Robert.Pincus@colorado.edu author Dr. Holger Pohlmann Max Planck Institute for Meteorology https://mpimet.mpg.de/ Email: holger.pohlmann@mpimet.mpg.de author Prof. Julia Pongratz Max Planck Institute for Meteorology http://www.mpimet.mpg.de Email: julia.pongratz@geographie.uni-muenchen.de author Dr. Sebastian Rast Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: sebastian.rast@mpimet.mpg.de author Dr. Hauke Schmidt Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: hauke.schmidt@mpimet.mpg.de author Dr. Reiner Schnur Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: reiner.schnur@mpimet.mpg.de author Uwe Schulzweida Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: uwe.schulzweida@mpimet.mpg.de author Dr. Katharina Six Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: katharina.six@mpimet.mpg.de author Prof. Bjorn Stevens Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: bjorn.stevens@mpimet.mpg.de author Aiko Voigt Karlsruhe Institute of Technology not filled Email: aiko.voigt@kit.edu author Dr. Erich Roeckner Max Planck Institute for Meteorology http://www.mpimet.mpg.de/ Email: erich.roeckner@mpimet.mpg.de author WDC Climate at DKRZ publisher RCM forcing data from the 1st realisation (r1i1p1f1) of the CMIP6/ScenarioMIP experiment ssp126, conducted with the MPI-ESM1-2-HR on the Mistral supercomputer of the DKRZ. The experiment covers the years 2015 to 2100 and branches from realisations of the CMIP6/CMIP historical experiment. The file format is gzip-compressed GRIB (*.grb.gz). ScenarioMIP website: https://cmip.ucar.edu/scenario-mip ScenarioMIP paper: https://doi.org/10.5194/gmd-9-3461-2016 Experiment description ssp126: SSP-based RCP scenario with low radiative forcing by the end of the century. Following approximately RCP2.6 global forcing pathway with SSP1 socioeconomic conditions. Radiative forcing reaches a level of 2.6 W/m2 in 2100. Concentration-driven. Martin Schupfner Deutsches Klimarechenzentrum http://www.dkrz.de/ pointOfContact GRIB1 zipped; recs separated CMIP6 CORDEX ECHAM6 MPI-ESM MPI-ESM1-2-HR RCM-forcing rcp26 ssp126 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 proleptic_gregorian 2015-01-01 2100-12-31 mass_fraction_of_cloud_ice_in_air Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: kg kg-1 sea_ice_thickness sea_ice_thickness [CF-Standard Name]; unit: m soil_moisture_content_at_field_capacity "moisture" means water in all phases contained in soil. "Content" indicates a quantity per unit area. The "soil content" of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used. The field capacity of soil is the maximum content of water it can retain against gravitational drainage. [CF-Standard Name]; unit: m surface_snow_thickness-where_land The surface called "surface" means the lower boundary of the atmosphere. Unless indicated, a quantity is assumed to apply to the whole area of each horizontal grid box. The qualifier where_type specifies instead that the quantity applies only to the part of the grid box of the named type.[CF-Standard Name where cell method]; unit: m sea_land_mask sea_land_mask; unit: 0,1 divergence_of_wind "[horizontal_]divergence_of_X" means [horizontal] divergence of a vector X; if X does not have a vertical component then "horizontal" should be omitted. 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: s-1 atmosphere_relative_vorticity Relative vorticity is the upward component of the vorticity vector i.e. the component which arises from horizontal velocity. [CF-Standard Name]; unit: s-1 surface_temperature-where_land_or_land_ice surface_temperature where land or land ice [CF-Standard Name-where cell method]; unit: K lwe_thickness_of_canopy_water_amount "lwe" means liquid water equivalent. "Amount" means mass per unit area. The construction lwe_thickness_of_X_amount or _content means the vertical extent of a layer of liquid water having the same mass per unit area. "Water" means water in all phases, including frozen i.e. ice and snow. "Canopy" means the plant or vegetation canopy. The canopy water is the water on the canopy.[CF-Standard Name]; unit: m specific_humidity "specific" means per unit mass. Specific humidity is the mass fraction of water vapor in (moist) air.[CF-Standard Name]; unit: kg kg-1 surface_geopotential The surface called "surface" means the lower boundary of the atmosphere. Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. [CF-Standard Name]; unit: m2 s-2 mass_fraction_of_cloud_liquid_water_in_air Mass fraction is used in the construction mass_fraction_of_X_in_Y, where X is a material constituent of Y. It means the ratio of the mass of Y to the mass of X (including Y). [CF-Standard Name]; unit: kg kg-1 surface_temperature_of_sea_ice When computing the time-mean here, the time-samples, weighted by the area of sea ice in the grid cell, are accumulated and then divided by the sum of the weights. Reported as "missing" in regions free of sea ice. Note this will be the surface snow temperature in regions where snow covers the sea ice.; unit: K sea_ice_area_fraction sea_ice_area_fraction [CF-Standard Name]; unit: 1 glacier mask glacier mask, 0:no; 1:yes; unit: 0,1 soil_moisture_content-where_roots "moisture" means water in all phases contained in soil. "Content" indicates a quantity per unit area. The "soil content" of a quantity refers to the vertical integral from the surface down to the bottom of the soil model. For the content between specified levels in the soil, standard names including content_of_soil_layer are used. [CF-Standard Name where cell method]; unit: m liquid_water_content_of_snow_layer-where_sea_ice liquid_water_content_of_snow_layer-where_sea_ice [CF-Standard Name-where cell method]; unit: m surface_air_pressure The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K soil_temperature Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K 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: K GRIB1 zipped; recs separated 2972032 https://www.wdc-climate.de/ui/entry?acronym=RCM_CMIP6_SSP126-HR_r1i1p1f1 information collection n/a None