Surface‐Forced Variability in the Nordic Seas Overturning Circulation and Overflows

Abstract Water mass transformation in the Nordic Seas and the associated overflow of dense waters across the Greenland‐Scotland Ridge (GSR) acts to maintain the lower limb of the Atlantic meridional overturning circulation. Here, we use ocean and atmospheric reanalysis to assess the temporal variabi...

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Published in:Geophysical Research Letters
Main Author: Marius Årthun
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL104158
https://doaj.org/article/85806a01e7c949c7ad0b0939709e6274
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spelling ftdoajarticles:oai:doaj.org/article:85806a01e7c949c7ad0b0939709e6274 2024-09-15T18:09:14+00:00 Surface‐Forced Variability in the Nordic Seas Overturning Circulation and Overflows Marius Årthun 2023-08-01T00:00:00Z https://doi.org/10.1029/2023GL104158 https://doaj.org/article/85806a01e7c949c7ad0b0939709e6274 EN eng Wiley https://doi.org/10.1029/2023GL104158 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL104158 https://doaj.org/article/85806a01e7c949c7ad0b0939709e6274 Geophysical Research Letters, Vol 50, Iss 15, Pp n/a-n/a (2023) Nordic Seas overturning circulation overflow waters surface forcing multidecadal variability Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL104158 2024-08-05T17:49:23Z Abstract Water mass transformation in the Nordic Seas and the associated overflow of dense waters across the Greenland‐Scotland Ridge (GSR) acts to maintain the lower limb of the Atlantic meridional overturning circulation. Here, we use ocean and atmospheric reanalysis to assess the temporal variability in the Nordic Seas overturning circulation between 1950 and 2020 and its relation to surface buoyancy forcing. We find that variable surface‐forced transformation of Atlantic waters in the eastern Nordic Seas can explain variations in overflow transport across the GSR. The production of dense water masses in the Greenland and Iceland Seas is of minor importance to overflow variability. The Nordic Seas overturning circulation shows pronounced multidecadal variability that is in phase with the Atlantic Multidecadal Variability (AMV) index, but no long‐term trend. As the AMV is currently transitioning into its negative phase, the next decades could see a decreased overflow from the Nordic Seas. Article in Journal/Newspaper Greenland Greenland-Scotland Ridge Iceland Nordic Seas Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 15
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Nordic Seas
overturning circulation
overflow waters
surface forcing
multidecadal variability
Geophysics. Cosmic physics
QC801-809
spellingShingle Nordic Seas
overturning circulation
overflow waters
surface forcing
multidecadal variability
Geophysics. Cosmic physics
QC801-809
Marius Årthun
Surface‐Forced Variability in the Nordic Seas Overturning Circulation and Overflows
topic_facet Nordic Seas
overturning circulation
overflow waters
surface forcing
multidecadal variability
Geophysics. Cosmic physics
QC801-809
description Abstract Water mass transformation in the Nordic Seas and the associated overflow of dense waters across the Greenland‐Scotland Ridge (GSR) acts to maintain the lower limb of the Atlantic meridional overturning circulation. Here, we use ocean and atmospheric reanalysis to assess the temporal variability in the Nordic Seas overturning circulation between 1950 and 2020 and its relation to surface buoyancy forcing. We find that variable surface‐forced transformation of Atlantic waters in the eastern Nordic Seas can explain variations in overflow transport across the GSR. The production of dense water masses in the Greenland and Iceland Seas is of minor importance to overflow variability. The Nordic Seas overturning circulation shows pronounced multidecadal variability that is in phase with the Atlantic Multidecadal Variability (AMV) index, but no long‐term trend. As the AMV is currently transitioning into its negative phase, the next decades could see a decreased overflow from the Nordic Seas.
format Article in Journal/Newspaper
author Marius Årthun
author_facet Marius Årthun
author_sort Marius Årthun
title Surface‐Forced Variability in the Nordic Seas Overturning Circulation and Overflows
title_short Surface‐Forced Variability in the Nordic Seas Overturning Circulation and Overflows
title_full Surface‐Forced Variability in the Nordic Seas Overturning Circulation and Overflows
title_fullStr Surface‐Forced Variability in the Nordic Seas Overturning Circulation and Overflows
title_full_unstemmed Surface‐Forced Variability in the Nordic Seas Overturning Circulation and Overflows
title_sort surface‐forced variability in the nordic seas overturning circulation and overflows
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2023GL104158
https://doaj.org/article/85806a01e7c949c7ad0b0939709e6274
genre Greenland
Greenland-Scotland Ridge
Iceland
Nordic Seas
genre_facet Greenland
Greenland-Scotland Ridge
Iceland
Nordic Seas
op_source Geophysical Research Letters, Vol 50, Iss 15, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2023GL104158
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2023GL104158
https://doaj.org/article/85806a01e7c949c7ad0b0939709e6274
op_doi https://doi.org/10.1029/2023GL104158
container_title Geophysical Research Letters
container_volume 50
container_issue 15
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