Supplementary material from "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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Main Authors: Buckley, Martha W., Susan Lozier, M., Desbruyéres, Damien, Gwyn Evans, Dafydd
Format: Article in Journal/Newspaper
Language:unknown
Published: The Royal Society 2023
Subjects:
Online Access:https://dx.doi.org/10.6084/m9.figshare.c.6823321.v1
https://rs.figshare.com/collections/Supplementary_material_from_Buoyancy_forcing_and_the_subpolar_Atlantic_meridional_overturning_circulation_/6823321/1
id ftdatacite:10.6084/m9.figshare.c.6823321.v1
record_format openpolar
spelling ftdatacite:10.6084/m9.figshare.c.6823321.v1 2023-11-05T03:43:17+01:00 Supplementary material from "Buoyancy forcing and the subpolar Atlantic meridional overturning circulation" ... Buckley, Martha W. Susan Lozier, M. Desbruyéres, Damien Gwyn Evans, Dafydd 2023 https://dx.doi.org/10.6084/m9.figshare.c.6823321.v1 https://rs.figshare.com/collections/Supplementary_material_from_Buoyancy_forcing_and_the_subpolar_Atlantic_meridional_overturning_circulation_/6823321/1 unknown The Royal Society https://dx.doi.org/10.6084/m9.figshare.c.6823321 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Oceanography FOS Earth and related environmental sciences article Collection 2023 ftdatacite https://doi.org/10.6084/m9.figshare.c.6823321.v110.6084/m9.figshare.c.6823321 2023-10-09T10:24:37Z 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 ... Article in Journal/Newspaper Labrador Sea Nordic Seas North Atlantic 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 unknown
topic Oceanography
FOS Earth and related environmental sciences
spellingShingle Oceanography
FOS Earth and related environmental sciences
Buckley, Martha W.
Susan Lozier, M.
Desbruyéres, Damien
Gwyn Evans, Dafydd
Supplementary material from "Buoyancy forcing and the subpolar Atlantic meridional overturning circulation" ...
topic_facet Oceanography
FOS Earth and related environmental sciences
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 ...
format Article in Journal/Newspaper
author Buckley, Martha W.
Susan Lozier, M.
Desbruyéres, Damien
Gwyn Evans, Dafydd
author_facet Buckley, Martha W.
Susan Lozier, M.
Desbruyéres, Damien
Gwyn Evans, Dafydd
author_sort Buckley, Martha W.
title Supplementary material from "Buoyancy forcing and the subpolar Atlantic meridional overturning circulation" ...
title_short Supplementary material from "Buoyancy forcing and the subpolar Atlantic meridional overturning circulation" ...
title_full Supplementary material from "Buoyancy forcing and the subpolar Atlantic meridional overturning circulation" ...
title_fullStr Supplementary material from "Buoyancy forcing and the subpolar Atlantic meridional overturning circulation" ...
title_full_unstemmed Supplementary material from "Buoyancy forcing and the subpolar Atlantic meridional overturning circulation" ...
title_sort supplementary material from "buoyancy forcing and the subpolar atlantic meridional overturning circulation" ...
publisher The Royal Society
publishDate 2023
url https://dx.doi.org/10.6084/m9.figshare.c.6823321.v1
https://rs.figshare.com/collections/Supplementary_material_from_Buoyancy_forcing_and_the_subpolar_Atlantic_meridional_overturning_circulation_/6823321/1
genre Labrador Sea
Nordic Seas
North Atlantic
genre_facet Labrador Sea
Nordic Seas
North Atlantic
op_relation https://dx.doi.org/10.6084/m9.figshare.c.6823321
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.6084/m9.figshare.c.6823321.v110.6084/m9.figshare.c.6823321
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