Phanerozoic global climatic fields simulated using the mixed-layer general circulation model FOAM
These files contain the output of Phanerozoic global climate simulations conducted using the “slab” mixed-layer ocean-atmosphere general circulation model FOAM. They are available every 20 Myrs between 540 Ma and 0 Ma, both included. Boundary conditions were adapted to best match each time slice. Co...
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ftzenodo:oai:zenodo.org:7220854 2023-05-15T18:40:31+02:00 Phanerozoic global climatic fields simulated using the mixed-layer general circulation model FOAM Pohl, Alexandre 2022-10-18 https://zenodo.org/record/7220854 https://doi.org/10.5281/zenodo.7220854 unknown doi:10.5281/zenodo.7220853 https://zenodo.org/record/7220854 https://doi.org/10.5281/zenodo.7220854 oai:zenodo.org:7220854 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Phanerozoic General circulation model climate Paleozoic Mesozoic Cenozoic info:eu-repo/semantics/other dataset 2022 ftzenodo https://doi.org/10.5281/zenodo.722085410.5281/zenodo.7220853 2023-03-10T23:53:18Z These files contain the output of Phanerozoic global climate simulations conducted using the “slab” mixed-layer ocean-atmosphere general circulation model FOAM. They are available every 20 Myrs between 540 Ma and 0 Ma, both included. Boundary conditions were adapted to best match each time slice. Continental reconstructions were taken from Scotese and Wright (https://www.earthbyte.org/paleodem-resource-scotese-and-wright-2018/). We defined pCO2 after the proxy data compilation of Foster et al. (doi:10.1038/ncomms14845) when available and Krause et al. (dot:10.1038/s41467-018-06383-y) for older time slices. Solar luminosity followed Gough et al. (doi:10.1007/BF00151270). Continental vegetation was set to Modern-like latitudinal bands between 0 Ma and 100 Ma (included), tropical evergreen, broad-leaved forest between 120 Ma and 360 Ma (included), tundra between 380 Ma and 440 Ma (included) and rocky desert afterwards. The orbital configuration was set to null eccentricity and minimum obliquity. The reader is referred to the associated paper for a full description of the model and boundary conditions. All model output file names use the following pattern: « [age]ebP2_solCgough1981_EccN_pCO2FosterKr_[model_component] _slab.nc", with [age], the age expressed in million years ago, and [model_component] being 'atmos' or 'coupl' (atmospheric component or coupler). For each time slice, the topography-bathymetry data used in FOAM is also provided (« Topobathy_[age]eb_postslarti_cor.nc »). Dataset Tundra Zenodo Gough ENVELOPE(159.367,159.367,-81.633,-81.633) |
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Open Polar |
collection |
Zenodo |
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ftzenodo |
language |
unknown |
topic |
Phanerozoic General circulation model climate Paleozoic Mesozoic Cenozoic |
spellingShingle |
Phanerozoic General circulation model climate Paleozoic Mesozoic Cenozoic Pohl, Alexandre Phanerozoic global climatic fields simulated using the mixed-layer general circulation model FOAM |
topic_facet |
Phanerozoic General circulation model climate Paleozoic Mesozoic Cenozoic |
description |
These files contain the output of Phanerozoic global climate simulations conducted using the “slab” mixed-layer ocean-atmosphere general circulation model FOAM. They are available every 20 Myrs between 540 Ma and 0 Ma, both included. Boundary conditions were adapted to best match each time slice. Continental reconstructions were taken from Scotese and Wright (https://www.earthbyte.org/paleodem-resource-scotese-and-wright-2018/). We defined pCO2 after the proxy data compilation of Foster et al. (doi:10.1038/ncomms14845) when available and Krause et al. (dot:10.1038/s41467-018-06383-y) for older time slices. Solar luminosity followed Gough et al. (doi:10.1007/BF00151270). Continental vegetation was set to Modern-like latitudinal bands between 0 Ma and 100 Ma (included), tropical evergreen, broad-leaved forest between 120 Ma and 360 Ma (included), tundra between 380 Ma and 440 Ma (included) and rocky desert afterwards. The orbital configuration was set to null eccentricity and minimum obliquity. The reader is referred to the associated paper for a full description of the model and boundary conditions. All model output file names use the following pattern: « [age]ebP2_solCgough1981_EccN_pCO2FosterKr_[model_component] _slab.nc", with [age], the age expressed in million years ago, and [model_component] being 'atmos' or 'coupl' (atmospheric component or coupler). For each time slice, the topography-bathymetry data used in FOAM is also provided (« Topobathy_[age]eb_postslarti_cor.nc »). |
format |
Dataset |
author |
Pohl, Alexandre |
author_facet |
Pohl, Alexandre |
author_sort |
Pohl, Alexandre |
title |
Phanerozoic global climatic fields simulated using the mixed-layer general circulation model FOAM |
title_short |
Phanerozoic global climatic fields simulated using the mixed-layer general circulation model FOAM |
title_full |
Phanerozoic global climatic fields simulated using the mixed-layer general circulation model FOAM |
title_fullStr |
Phanerozoic global climatic fields simulated using the mixed-layer general circulation model FOAM |
title_full_unstemmed |
Phanerozoic global climatic fields simulated using the mixed-layer general circulation model FOAM |
title_sort |
phanerozoic global climatic fields simulated using the mixed-layer general circulation model foam |
publishDate |
2022 |
url |
https://zenodo.org/record/7220854 https://doi.org/10.5281/zenodo.7220854 |
long_lat |
ENVELOPE(159.367,159.367,-81.633,-81.633) |
geographic |
Gough |
geographic_facet |
Gough |
genre |
Tundra |
genre_facet |
Tundra |
op_relation |
doi:10.5281/zenodo.7220853 https://zenodo.org/record/7220854 https://doi.org/10.5281/zenodo.7220854 oai:zenodo.org:7220854 |
op_rights |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.722085410.5281/zenodo.7220853 |
_version_ |
1766229903383986176 |