2026-04-06T10:01:57Z
http://dmoai.cloud.dkrz.de/oai/provider
oai:wdcc.dkrz.de:iso_3892019
2026-04-05T23:08:12Z
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wdc-climate.de:3892019
eng; USA
collection
RCM_CMIP6_SSP585-LR
Martin Schupfner
Deutsches Klimarechenzentrum
http://www.dkrz.de/
pointOfContact
Martin Schupfner
Deutsches Klimarechenzentrum
http://www.dkrz.de/
pointOfContact
2026-02-04T10:21:32
ISO 19115
ISO 19115-2:2009
CMIP6 ScenarioMIP MPI-ESM1-2-LR ssp585 - RCM-forcing data
2022-12-21
publication
1
RCM_CMIP6_SSP585-LR
doi:10.26050/WDCC/RCM_CMIP6_SSP585-LR
Martin Schupfner
Deutsches Klimarechenzentrum
http://www.dkrz.de/
Email: schupfner@dkrz.de
principalInvestigator
Sebastian Brune
Institut für Meereskunde
not filled
Email: sebastian.brune@uni-hamburg.de
author
Dr. Dirk Olonscheck
Max Planck Institute for Meteorology
https://mpimet.mpg.de/
Email: dirk.olonscheck@mpimet.mpg.de
author
Dr. Laura Suárez-Gutiérrez
Max Planck Institute for Meteorology
https://mpimet.mpg.de/
Email: laura.suarez@mpimet.mpg.de
author
Martin Schupfner
Deutsches Klimarechenzentrum
http://www.dkrz.de/
Email: schupfner@dkrz.de
author
Fabian Wachsmann
Deutsches Klimarechenzentrum
http://www.dkrz.de/
Email: wachsmann@dkrz.de
author
Karl-Hermann Wieners
Max Planck Institute for Meteorology
http://www.mpimet.mpg.de/
Email: Karl-Hermann.Wieners@mpimet.mpg.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
Senckenberg Biodiversity and Climate Research Institue (BiK-F)
not filled
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
Karsten Peters-von Gehlen
Deutsches Klimarechenzentrum
http://www.dkrz.de/
Email: peters@dkrz.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
Ludwig-Maximilian-University Munich
http://www.meteo.physik.uni-muenchen.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 20 realisations (r11i1p1f1-r30i1p1f1) of the
CMIP6/ScenarioMIP experiment ssp585, conducted with the MPI-ESM1-2-LR 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 ssp585:
SSP-based RCP scenario with high radiative forcing by the end of the century. Following approximately RCP8.5 global forcing pathway with SSP5 socioeconomic conditions. Radiative forcing reaches a level of 8.5 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-LR
RCM-forcing
ssp585
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
land_ice_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. "Land ice" means glaciers, ice-caps and ice-sheets resting on bedrock. [CF-Standard Name]; unit: 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
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_ice_area_fraction
sea_ice_area_fraction [CF-Standard Name]; unit: 0-1
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
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
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
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
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
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
soil_temperature
Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K
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
land_binary_mask
X_binary_mask has 1 where condition X is met, 0 elsewhere. 1 = land, 0 = sea. [CF-Standard Name]; unit: 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/s2
GRIB1 zipped; recs separated
8483811
https://www.wdc-climate.de/ui/entry?acronym=RCM_CMIP6_SSP585-LR
information
collection
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