Data from Climate Model Simulations for Triassic-Jurassic Orbital Climate Cycles
Data from Climate Model Simulations for Triassic-Jurassic Orbital Climate Cycles
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.,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.
Geoforschungszentrum Potsdam
Sames, Benjamin
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Whiteside, Jessica H.
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Feulner, Georg
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Petri, Stefan
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Willeit, Matteo
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Wagreich, Michael
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Olsen, Paul E.
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Landwehrs, Jan Philip
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Sames, Benjamin
8a8a966b-96cb-422a-ac81-b36478706e9e
Whiteside, Jessica H.
5d9ad7aa-eba3-4ad9-9f6f-81be71b6829b
Feulner, Georg
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Petri, Stefan
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Willeit, Matteo
300db874-42a6-4323-ae3f-0a264a38d2e0
Wagreich, Michael
844d8db2-67cc-4820-8eff-9570e42047ee
Olsen, Paul E.
bdbec40b-82ed-41ac-8028-b6c333206f16
Landwehrs, Jan Philip
f2a54ea8-c475-4c44-a668-930dec6e3541
(2022)
Data from Climate Model Simulations for Triassic-Jurassic Orbital Climate Cycles.
Geoforschungszentrum Potsdam
doi:10.5880/pik.2022.001
[Dataset]
Abstract
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.,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.
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Published date: 1 January 2022
Identifiers
Local EPrints ID: 472226
URI: http://eprints.soton.ac.uk/id/eprint/472226
PURE UUID: 936cb12f-6949-49b5-a131-d609d724b89d
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Date deposited: 29 Nov 2022 17:55
Last modified: 01 Aug 2023 16:53
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Contributors
Contributor:
Benjamin Sames
Contributor:
Georg Feulner
Contributor:
Stefan Petri
Contributor:
Matteo Willeit
Contributor:
Michael Wagreich
Contributor:
Paul E. Olsen
Contributor:
Jan Philip Landwehrs
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