East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum
The variability of the Atlantic meridional overturning circulation (AMOC) and its governing processes during the Last Glacial Maximum (LGM) is investigated in the Kiel Climate Model. Under LGM conditions, multidecadal AMOC variability is mainly forced by the surface heat flux variability linked to t...
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ftdatacite:10.23689/fidgeo-4757 2023-05-15T17:31:11+02:00 East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum Song, Zhaoyang Latif, Mojib Park, Wonsun 2019 https://dx.doi.org/10.23689/fidgeo-4757 https://e-docs.geo-leo.de/handle/11858/9103 en eng FID GEO Text Article article-journal ScholarlyArticle 2019 ftdatacite https://doi.org/10.23689/fidgeo-4757 2021-11-05T12:55:41Z The variability of the Atlantic meridional overturning circulation (AMOC) and its governing processes during the Last Glacial Maximum (LGM) is investigated in the Kiel Climate Model. Under LGM conditions, multidecadal AMOC variability is mainly forced by the surface heat flux variability linked to the East Atlantic pattern (EAP). In contrast, the multidecadal AMOC variability under preindustrial conditions is mainly driven by the surface heat flux variability associated with the North Atlantic Oscillation. Stand-alone atmosphere model experiments show that relative to preindustrial conditions, the change in AMOC forcing under LGM conditions is tightly linked to the differences in topography. Text North Atlantic North Atlantic oscillation DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
language |
English |
description |
The variability of the Atlantic meridional overturning circulation (AMOC) and its governing processes during the Last Glacial Maximum (LGM) is investigated in the Kiel Climate Model. Under LGM conditions, multidecadal AMOC variability is mainly forced by the surface heat flux variability linked to the East Atlantic pattern (EAP). In contrast, the multidecadal AMOC variability under preindustrial conditions is mainly driven by the surface heat flux variability associated with the North Atlantic Oscillation. Stand-alone atmosphere model experiments show that relative to preindustrial conditions, the change in AMOC forcing under LGM conditions is tightly linked to the differences in topography. |
format |
Text |
author |
Song, Zhaoyang Latif, Mojib Park, Wonsun |
spellingShingle |
Song, Zhaoyang Latif, Mojib Park, Wonsun East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum |
author_facet |
Song, Zhaoyang Latif, Mojib Park, Wonsun |
author_sort |
Song, Zhaoyang |
title |
East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum |
title_short |
East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum |
title_full |
East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum |
title_fullStr |
East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum |
title_full_unstemmed |
East Atlantic Pattern Drives Multidecadal Atlantic Meridional Overturning Circulation Variability During the Last Glacial Maximum |
title_sort |
east atlantic pattern drives multidecadal atlantic meridional overturning circulation variability during the last glacial maximum |
publisher |
FID GEO |
publishDate |
2019 |
url |
https://dx.doi.org/10.23689/fidgeo-4757 https://e-docs.geo-leo.de/handle/11858/9103 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_doi |
https://doi.org/10.23689/fidgeo-4757 |
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1766128567831232512 |