Ocean Cooling Pattern at the Last Glacial Maximum
Ocean temperature and ocean heat content change are analyzed based on four PMIP3 model results at the Last Glacial Maximum relative to the prehistorical run. Ocean cooling mostly occurs in the upper 1000 m depth and varies spatially in the tropical and temperate zones. The Atlantic Ocean experiences...
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fthindawi:oai:hindawi.com:10.1155/2012/213743 2023-05-15T13:53:13+02:00 Ocean Cooling Pattern at the Last Glacial Maximum Kelin Zhuang John R. Giardino 2012 https://doi.org/10.1155/2012/213743 en eng Advances in Meteorology https://doi.org/10.1155/2012/213743 Copyright © 2012 Kelin Zhuang and John R. Giardino. Research Article 2012 fthindawi https://doi.org/10.1155/2012/213743 2019-05-25T23:29:55Z Ocean temperature and ocean heat content change are analyzed based on four PMIP3 model results at the Last Glacial Maximum relative to the prehistorical run. Ocean cooling mostly occurs in the upper 1000 m depth and varies spatially in the tropical and temperate zones. The Atlantic Ocean experiences greater cooling than the rest of the ocean basins. Ocean cooling is closely related to the weakening of meridional overturning circulation and enhanced intrusion of Antarctic Bottom Water into the North Atlantic. Article in Journal/Newspaper Antarc* Antarctic North Atlantic Hindawi Publishing Corporation Antarctic Advances in Meteorology 2012 1 8 |
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Open Polar |
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Hindawi Publishing Corporation |
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fthindawi |
language |
English |
description |
Ocean temperature and ocean heat content change are analyzed based on four PMIP3 model results at the Last Glacial Maximum relative to the prehistorical run. Ocean cooling mostly occurs in the upper 1000 m depth and varies spatially in the tropical and temperate zones. The Atlantic Ocean experiences greater cooling than the rest of the ocean basins. Ocean cooling is closely related to the weakening of meridional overturning circulation and enhanced intrusion of Antarctic Bottom Water into the North Atlantic. |
format |
Article in Journal/Newspaper |
author |
Kelin Zhuang John R. Giardino |
spellingShingle |
Kelin Zhuang John R. Giardino Ocean Cooling Pattern at the Last Glacial Maximum |
author_facet |
Kelin Zhuang John R. Giardino |
author_sort |
Kelin Zhuang |
title |
Ocean Cooling Pattern at the Last Glacial Maximum |
title_short |
Ocean Cooling Pattern at the Last Glacial Maximum |
title_full |
Ocean Cooling Pattern at the Last Glacial Maximum |
title_fullStr |
Ocean Cooling Pattern at the Last Glacial Maximum |
title_full_unstemmed |
Ocean Cooling Pattern at the Last Glacial Maximum |
title_sort |
ocean cooling pattern at the last glacial maximum |
publisher |
Advances in Meteorology |
publishDate |
2012 |
url |
https://doi.org/10.1155/2012/213743 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic North Atlantic |
genre_facet |
Antarc* Antarctic North Atlantic |
op_relation |
https://doi.org/10.1155/2012/213743 |
op_rights |
Copyright © 2012 Kelin Zhuang and John R. Giardino. |
op_doi |
https://doi.org/10.1155/2012/213743 |
container_title |
Advances in Meteorology |
container_volume |
2012 |
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1 |
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8 |
_version_ |
1766258183860387840 |