COSMOS simulated basic surface ocean characteristics for comparison with palynological data
Here we provide simulated seasonal (DJF and JJA) sea surface temperature (THO), sea surface salinity (SAO) as well as surface zonal (UKO) and meridional (VKE) ocean currents velocities. THO and SAO are provided on the regular grid in 360x180 resolution while UKO and VKE on the curvilinear grid in 12...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.917488 2023-05-15T14:58:46+02:00 COSMOS simulated basic surface ocean characteristics for comparison with palynological data Radmacher, Wiesława Niezgodzki, Igor Tyszka, Jaroslaw Mangerud, Gunn Pearce, Martin A 2020-05-18 text/tab-separated-values, 24 data points https://doi.pangaea.de/10.1594/PANGAEA.917488 https://doi.org/10.1594/PANGAEA.917488 en eng PANGAEA Radmacher, Wiesława; Niezgodzki, Igor; Tyszka, Jaroslaw; Mangerud, Gunn; Pearce, Martin A (2019): Palynology vs. model simulation: oceanographic reconstruction of incomplete data from the Cretaceous Greenland–Norwegian Seaway. Newsletters on Stratigraphy, 53(1), 93-120, https://doi.org/10.1127/nos/2019/0527 https://doi.pangaea.de/10.1594/PANGAEA.917488 https://doi.org/10.1594/PANGAEA.917488 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY File format File name File size Uniform resource locator/link to file Dataset 2020 ftpangaea https://doi.org/10.1594/PANGAEA.917488 https://doi.org/10.1127/nos/2019/0527 2023-01-20T09:13:34Z Here we provide simulated seasonal (DJF and JJA) sea surface temperature (THO), sea surface salinity (SAO) as well as surface zonal (UKO) and meridional (VKE) ocean currents velocities. THO and SAO are provided on the regular grid in 360x180 resolution while UKO and VKE on the curvilinear grid in 122x101 resolution (which is the resolution of the ocean component MPIOM). The simulations were produced with COSMOS in a coupled atmosphere-ocean configuration. All of the simulations were run with 4 x pre-industrial (PI) CO2 level (1120 ppm). The experiments differ by alterations in gateway configurations between the Arctic Ocean and North proto-Atlantic Basin. Our spin-up experiment (C-1120) employs Maastrichtian (~70 Ma) paleogeography of Markwick and Valdes [2004, doi:10.1016/j.palaeo.2004.06.015]. The experiment was run to the model year 10 600. Two other experiments were branched off from C-1120 from the model year 9200. One of them differs from C-1120 by the closure of Hudson Seaway (HUD-0) and was run for the next 1400 years. The other one (GNS-47) has each gateway between the Arctic Ocean and North proto-Atlantic basin closed apart Greenland-Norwegian Sea and was run for the next 2100 years. More information about the geological background and COSMOS configuration can be found in Radmacher et al. [2020, doi:10.1127/nos/2019/0527]. Dataset Arctic Arctic Ocean Greenland Norwegian Sea PANGAEA - Data Publisher for Earth & Environmental Science Arctic Arctic Ocean Norwegian Sea Greenland Hudson |
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Open Polar |
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PANGAEA - Data Publisher for Earth & Environmental Science |
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ftpangaea |
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English |
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File format File name File size Uniform resource locator/link to file |
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File format File name File size Uniform resource locator/link to file Radmacher, Wiesława Niezgodzki, Igor Tyszka, Jaroslaw Mangerud, Gunn Pearce, Martin A COSMOS simulated basic surface ocean characteristics for comparison with palynological data |
topic_facet |
File format File name File size Uniform resource locator/link to file |
description |
Here we provide simulated seasonal (DJF and JJA) sea surface temperature (THO), sea surface salinity (SAO) as well as surface zonal (UKO) and meridional (VKE) ocean currents velocities. THO and SAO are provided on the regular grid in 360x180 resolution while UKO and VKE on the curvilinear grid in 122x101 resolution (which is the resolution of the ocean component MPIOM). The simulations were produced with COSMOS in a coupled atmosphere-ocean configuration. All of the simulations were run with 4 x pre-industrial (PI) CO2 level (1120 ppm). The experiments differ by alterations in gateway configurations between the Arctic Ocean and North proto-Atlantic Basin. Our spin-up experiment (C-1120) employs Maastrichtian (~70 Ma) paleogeography of Markwick and Valdes [2004, doi:10.1016/j.palaeo.2004.06.015]. The experiment was run to the model year 10 600. Two other experiments were branched off from C-1120 from the model year 9200. One of them differs from C-1120 by the closure of Hudson Seaway (HUD-0) and was run for the next 1400 years. The other one (GNS-47) has each gateway between the Arctic Ocean and North proto-Atlantic basin closed apart Greenland-Norwegian Sea and was run for the next 2100 years. More information about the geological background and COSMOS configuration can be found in Radmacher et al. [2020, doi:10.1127/nos/2019/0527]. |
format |
Dataset |
author |
Radmacher, Wiesława Niezgodzki, Igor Tyszka, Jaroslaw Mangerud, Gunn Pearce, Martin A |
author_facet |
Radmacher, Wiesława Niezgodzki, Igor Tyszka, Jaroslaw Mangerud, Gunn Pearce, Martin A |
author_sort |
Radmacher, Wiesława |
title |
COSMOS simulated basic surface ocean characteristics for comparison with palynological data |
title_short |
COSMOS simulated basic surface ocean characteristics for comparison with palynological data |
title_full |
COSMOS simulated basic surface ocean characteristics for comparison with palynological data |
title_fullStr |
COSMOS simulated basic surface ocean characteristics for comparison with palynological data |
title_full_unstemmed |
COSMOS simulated basic surface ocean characteristics for comparison with palynological data |
title_sort |
cosmos simulated basic surface ocean characteristics for comparison with palynological data |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.917488 https://doi.org/10.1594/PANGAEA.917488 |
geographic |
Arctic Arctic Ocean Norwegian Sea Greenland Hudson |
geographic_facet |
Arctic Arctic Ocean Norwegian Sea Greenland Hudson |
genre |
Arctic Arctic Ocean Greenland Norwegian Sea |
genre_facet |
Arctic Arctic Ocean Greenland Norwegian Sea |
op_relation |
Radmacher, Wiesława; Niezgodzki, Igor; Tyszka, Jaroslaw; Mangerud, Gunn; Pearce, Martin A (2019): Palynology vs. model simulation: oceanographic reconstruction of incomplete data from the Cretaceous Greenland–Norwegian Seaway. Newsletters on Stratigraphy, 53(1), 93-120, https://doi.org/10.1127/nos/2019/0527 https://doi.pangaea.de/10.1594/PANGAEA.917488 https://doi.org/10.1594/PANGAEA.917488 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.917488 https://doi.org/10.1127/nos/2019/0527 |
_version_ |
1766330898404343808 |