Buoyancy forcing and the subpolar Atlantic meridional overturning circulation

The North Atlantic meridional overturning circulation and its variability are examined in terms of the overturning in density space and diapycnal water mass transformation. The magnitude of the mean overturning is similar to the surface water mass transformation, but the density and properties of th...

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Published in:Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Authors: Buckley, Martha W., Lozier, M. Susan, Desbruyères, Damien, Evans, Dafydd Gwyn
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/536299/
https://nora.nerc.ac.uk/id/eprint/536299/1/buckley-et-al-2023-buoyancy-forcing-and-the-subpolar-atlantic-meridional-overturning-circulation.pdf
https://doi.org/10.1098/rsta.2022.0181
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spelling ftnerc:oai:nora.nerc.ac.uk:536299 2023-12-24T10:18:22+01:00 Buoyancy forcing and the subpolar Atlantic meridional overturning circulation Buckley, Martha W. Lozier, M. Susan Desbruyères, Damien Evans, Dafydd Gwyn 2023-12-11 text http://nora.nerc.ac.uk/id/eprint/536299/ https://nora.nerc.ac.uk/id/eprint/536299/1/buckley-et-al-2023-buoyancy-forcing-and-the-subpolar-atlantic-meridional-overturning-circulation.pdf https://doi.org/10.1098/rsta.2022.0181 en eng https://nora.nerc.ac.uk/id/eprint/536299/1/buckley-et-al-2023-buoyancy-forcing-and-the-subpolar-atlantic-meridional-overturning-circulation.pdf Buckley, Martha W.; Lozier, M. Susan; Desbruyères, Damien; Evans, Dafydd Gwyn orcid:0000-0002-6328-4093 . 2023 Buoyancy forcing and the subpolar Atlantic meridional overturning circulation. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 381 (2262). https://doi.org/10.1098/rsta.2022.0181 <https://doi.org/10.1098/rsta.2022.0181> cc_by_4 Publication - Article PeerReviewed 2023 ftnerc https://doi.org/10.1098/rsta.2022.0181 2023-11-24T00:03:12Z The North Atlantic meridional overturning circulation and its variability are examined in terms of the overturning in density space and diapycnal water mass transformation. The magnitude of the mean overturning is similar to the surface water mass transformation, but the density and properties of these waters are modified by diapycnal mixing. Surface waters are progressively densified while circulating cyclonically around the subpolar gyre, with the densest waters and deepest convection occurring in the Labrador Sea and Nordic Seas. The eddy-driven interaction between the convective interior and boundary currents is a key to the export of dense waters from marginal seas. Due to the multitude of pathways of dense waters within the subpolar gyre, as well as mixing with older waters, waters exiting the subpolar gyre have a wide range of ages, with a mean age on the order of a decade. As a result, interannual changes in water mass transformation are mostly balanced locally and do not result in changes in export to the subtropics. Only persistent changes in water mass transformation result in changes in export to the subtropics. The dilution of signals from upstream water mass transformation suggests that variability in export of dense waters to the subtropics may be controlled by other processes, including interaction of dense waters with the energetic upper ocean. This article is part of a discussion meeting issue ‘Atlantic overturning: new observations and challenges’. Article in Journal/Newspaper Labrador Sea Nordic Seas North Atlantic Natural Environment Research Council: NERC Open Research Archive Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 381 2262
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language English
description The North Atlantic meridional overturning circulation and its variability are examined in terms of the overturning in density space and diapycnal water mass transformation. The magnitude of the mean overturning is similar to the surface water mass transformation, but the density and properties of these waters are modified by diapycnal mixing. Surface waters are progressively densified while circulating cyclonically around the subpolar gyre, with the densest waters and deepest convection occurring in the Labrador Sea and Nordic Seas. The eddy-driven interaction between the convective interior and boundary currents is a key to the export of dense waters from marginal seas. Due to the multitude of pathways of dense waters within the subpolar gyre, as well as mixing with older waters, waters exiting the subpolar gyre have a wide range of ages, with a mean age on the order of a decade. As a result, interannual changes in water mass transformation are mostly balanced locally and do not result in changes in export to the subtropics. Only persistent changes in water mass transformation result in changes in export to the subtropics. The dilution of signals from upstream water mass transformation suggests that variability in export of dense waters to the subtropics may be controlled by other processes, including interaction of dense waters with the energetic upper ocean. This article is part of a discussion meeting issue ‘Atlantic overturning: new observations and challenges’.
format Article in Journal/Newspaper
author Buckley, Martha W.
Lozier, M. Susan
Desbruyères, Damien
Evans, Dafydd Gwyn
spellingShingle Buckley, Martha W.
Lozier, M. Susan
Desbruyères, Damien
Evans, Dafydd Gwyn
Buoyancy forcing and the subpolar Atlantic meridional overturning circulation
author_facet Buckley, Martha W.
Lozier, M. Susan
Desbruyères, Damien
Evans, Dafydd Gwyn
author_sort Buckley, Martha W.
title Buoyancy forcing and the subpolar Atlantic meridional overturning circulation
title_short Buoyancy forcing and the subpolar Atlantic meridional overturning circulation
title_full Buoyancy forcing and the subpolar Atlantic meridional overturning circulation
title_fullStr Buoyancy forcing and the subpolar Atlantic meridional overturning circulation
title_full_unstemmed Buoyancy forcing and the subpolar Atlantic meridional overturning circulation
title_sort buoyancy forcing and the subpolar atlantic meridional overturning circulation
publishDate 2023
url http://nora.nerc.ac.uk/id/eprint/536299/
https://nora.nerc.ac.uk/id/eprint/536299/1/buckley-et-al-2023-buoyancy-forcing-and-the-subpolar-atlantic-meridional-overturning-circulation.pdf
https://doi.org/10.1098/rsta.2022.0181
genre Labrador Sea
Nordic Seas
North Atlantic
genre_facet Labrador Sea
Nordic Seas
North Atlantic
op_relation https://nora.nerc.ac.uk/id/eprint/536299/1/buckley-et-al-2023-buoyancy-forcing-and-the-subpolar-atlantic-meridional-overturning-circulation.pdf
Buckley, Martha W.; Lozier, M. Susan; Desbruyères, Damien; Evans, Dafydd Gwyn orcid:0000-0002-6328-4093 . 2023 Buoyancy forcing and the subpolar Atlantic meridional overturning circulation. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 381 (2262). https://doi.org/10.1098/rsta.2022.0181 <https://doi.org/10.1098/rsta.2022.0181>
op_rights cc_by_4
op_doi https://doi.org/10.1098/rsta.2022.0181
container_title Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
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