10.5880/pik.2022.001 eng dataset GFZ German Research Centre for Geosciences datapub@gfz-potsdam.de http://www.gfz-potsdam.de Helmholtz-Centre Potsdam - GFZ German Research Centre for Geosciences Helmholtz-Centre Potsdam - GFZ German Research Centre for Geosciences pointOfContact 2022-10-19 urn:ogc:def:crs:EPSG:4326 Data from Climate Model Simulations for Triassic-Jurassic Orbital Climate Cycles 2022-10-19 revision doi:10.5880/pik.2022.001 Landwehrs, Jan Philip University of Vienna, Department of Geology, Vienna, Austria author Feulner, Georg Earth System Analysis, Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany author Willeit, Matteo Earth System Analysis, Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany author Petri, Stefan Earth System Analysis, Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany author Sames, Benjamin University of Vienna, Department of Geology, Vienna, Austria author Wagreich, Michael University of Vienna, Department of Geology, Vienna, Austria author Whiteside, Jessica H. Ocean and Earth Science, National Oceanography Centre, University of Southampton, United Kingdom author Olsen, Paul E. Lamont-Doherty Earth Observatory of Columbia University, New York, United States of America author GFZ Data Services publisher In "Astronomical Forcing, Continental Drift and CO2 Paced Pangaean Lake Level Cycles" we study the effect of cyclic orbital parameter changes on Late Triassic to Early Jurassic paleoclimates. For this, in total 36 transient climate simulations are performed with reconstructed paleogeographies for 9 time slices in 5 Myr steps (230 to 190 million years ago) at 3 different atmospheric pCO2 values, each driven by a simplified orbital forcing over a 250,000 yr period. The data presented here is the model output on which the results of the main article are based. (The majority of further output data is not included due to its large size, but it can be made available upon request.) Also included are different model configuration files and the scripts to generate the included figures (using the Python programming language in a Jupyter Notebook). The model output data is provided in different NetCDF files, see README for detailed description. Landwehrs, Jan Philip University of Vienna, Department of Geology, Vienna, Austria jan.landwehrs@univie.ac.at pointOfContact Feulner, Georg Earth System Analysis, Potsdam Institute for Climate Impact Research, Member of the Leibniz Association, Potsdam, Germany Georg.Feulner@pik-potsdam.de https://www.pik-potsdam.de/members/feulner informtion pointOfContact Mesozoic Triassic Jurassic Pangaea Newark Basin Paleoclimate Orbital Cycles climate > climatic change experiment > simulation > modelling > model > global model GEMET - INSPIRE themes, version 1.0 publication EARTH SCIENCE > PALEOCLIMATE > PALEOCLIMATE RECONSTRUCTIONS > DROUGHT/PRECIPITATION RECONSTRUCTION EARTH SCIENCE > PALEOCLIMATE > PALEOCLIMATE RECONSTRUCTIONS > LAKE LEVEL RECONSTRUCTION EARTH SCIENCE > SOLID EARTH > TECTONICS > PLATE TECTONICS EARTH SCIENCE SERVICES > MODELS > COUPLED CLIMATE MODELS NASA/GCMD Earth Science Keywords publication Models/Analyses > CLIMATE MODELS GCMD Platforms publication Phanerozoic > Mesozoic Phanerozoic > Mesozoic > Jurassic > Early/Lower Jurassic Phanerozoic > Mesozoic > Triassic > Late/Upper Triassic International Chronostratigraphic Chart (2014) publication CC BY 4.0 CC BY 4.0 10.1086/321493 DOI IsDerivedFrom 10.5194/bg-14-5425-2017 DOI IsDerivedFrom 10.1038/ncomms14845 DOI IsDerivedFrom 10.1029/2010GL045777 DOI IsDerivedFrom 10.1016/j.gr.2021.05.016 DOI IsDerivedFrom 10.1130/B31107.1 DOI IsDerivedFrom 10.5194/gmd-9-3817-2016 DOI IsDerivedFrom 10.1073/pnas.2203818119 DOI IsSupplementTo eng geoscientificInformation 230 to 190 Ma (Late Triassic to Early Jurassic) in 5 Myr timesteps -180 180 -90 90 http://doi.org/10.5880/pik.2022.001 WWW:LINK-1.0-http--link Data Access - DOI Data Access - DOI information The data is generated using the Earth System Model CLIMBER-X which simulates climate globally on a 5°x5° horizontal grid. Its coupled atmosphere, ocean, sea-ice and land surface have been used in this study.