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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Bibliographic Details
Published in:Geophysical Research Letters
Main Author: Marius Årthun
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Nordic Seas
overturning circulation
overflow waters
surface forcing
multidecadal variability
Geophysics. Cosmic physics
QC801-809
Greenland
Greenland-Scotland Ridge
Iceland
Online Access:https://doi.org/10.1029/2023GL104158
https://doaj.org/article/85806a01e7c949c7ad0b0939709e6274
Description
Summary: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.

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