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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Main Authors: Song, Zhaoyang, Latif, Mojib, Park, Wonsun
Format: Text
Language:English
Published: FID GEO 2019
Subjects:
Online Access:https://dx.doi.org/10.23689/fidgeo-4757
https://e-docs.geo-leo.de/handle/11858/9103
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spelling 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)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id 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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