The contribution of the Weddell Gyre to the lower limb of the global overturning circulation

The horizontal and vertical circulation of the Weddell Gyre is diagnosed using a box inverse model constructed with recent hydrographic sections and including mobile sea ice and eddy transports. The gyre is found to convey 42 ± 8 Sv (1 Sv = 106 m3 s-1) across the central Weddell Sea and to intensify...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Jullion, Loïc, Naveira Garabato, Alberto C., Bacon, Sheldon, Meredith, Michael P., Brown, Pete J., Torres-Valdés, Sinhué, Speer, Kevin G., Holland, Paul R., Dong, Jun, Bakker, Dorothée, Hoppema, Mario, Loose, Brice, Venables, Hugh J., Jenkins, William J., Messias, Marie-José, Fahrbach, Eberhard
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://eprints.soton.ac.uk/364845/
https://eprints.soton.ac.uk/364845/1/jgrc20685.pdf
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spelling ftsouthampton:oai:eprints.soton.ac.uk:364845 2023-08-27T04:04:27+02:00 The contribution of the Weddell Gyre to the lower limb of the global overturning circulation Jullion, Loïc Naveira Garabato, Alberto C. Bacon, Sheldon Meredith, Michael P. Brown, Pete J. Torres-Valdés, Sinhué Speer, Kevin G. Holland, Paul R. Dong, Jun Bakker, Dorothée Hoppema, Mario Loose, Brice Venables, Hugh J. Jenkins, William J. Messias, Marie-José Fahrbach, Eberhard 2014-06 text https://eprints.soton.ac.uk/364845/ https://eprints.soton.ac.uk/364845/1/jgrc20685.pdf en English eng https://eprints.soton.ac.uk/364845/1/jgrc20685.pdf Jullion, Loïc, Naveira Garabato, Alberto C., Bacon, Sheldon, Meredith, Michael P., Brown, Pete J., Torres-Valdés, Sinhué, Speer, Kevin G., Holland, Paul R., Dong, Jun, Bakker, Dorothée, Hoppema, Mario, Loose, Brice, Venables, Hugh J., Jenkins, William J., Messias, Marie-José and Fahrbach, Eberhard (2014) The contribution of the Weddell Gyre to the lower limb of the global overturning circulation. Journal of Geophysical Research: Oceans, 119 (6), 3357-3377. (doi:10.1002/2013JC009725 <http://dx.doi.org/10.1002/2013JC009725>). Article PeerReviewed 2014 ftsouthampton https://doi.org/10.1002/2013JC009725 2023-08-03T22:20:34Z The horizontal and vertical circulation of the Weddell Gyre is diagnosed using a box inverse model constructed with recent hydrographic sections and including mobile sea ice and eddy transports. The gyre is found to convey 42 ± 8 Sv (1 Sv = 106 m3 s-1) across the central Weddell Sea and to intensify to 54±15 Sv further offshore. This circulation injects 36±13 TW of heat from the Antarctic Circumpolar Current to the gyre, and exports 51 ± 23 mSv of freshwater, including 13 ± 1 mSv as sea ice to the mid-latitude Southern Ocean. The gyre's overturning circulation has an asymmetric double-cell structure, in which 13 ± 4 Sv of Circumpolar Deep Water (CDW) and relatively light Antarctic Bottom Water (AABW) are transformed into upper-ocean water masses by mid-gyre upwelling (at a rate of 2 ± 2 Sv) and into denser AABW by downwelling focussed at the western boundary (8 ± 2 Sv). The gyre circulation exhibits a substantial throughflow component, by which CDW and AABW enter the gyre from the Indian sector, undergo ventilation and densification within the gyre, and are exported to the South Atlantic across the gyre's northern rim. The relatively modest net production of AABW in the Weddell Gyre (6±2 Sv) suggests that the gyre's prominence in the closure of the lower limb of global oceanic overturning stems largely from the recycling and equatorward export of Indian-sourced AABW. Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean Weddell Sea University of Southampton: e-Prints Soton Antarctic Indian Southern Ocean The Antarctic Weddell Weddell Sea Journal of Geophysical Research: Oceans 119 6 3357 3377
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description The horizontal and vertical circulation of the Weddell Gyre is diagnosed using a box inverse model constructed with recent hydrographic sections and including mobile sea ice and eddy transports. The gyre is found to convey 42 ± 8 Sv (1 Sv = 106 m3 s-1) across the central Weddell Sea and to intensify to 54±15 Sv further offshore. This circulation injects 36±13 TW of heat from the Antarctic Circumpolar Current to the gyre, and exports 51 ± 23 mSv of freshwater, including 13 ± 1 mSv as sea ice to the mid-latitude Southern Ocean. The gyre's overturning circulation has an asymmetric double-cell structure, in which 13 ± 4 Sv of Circumpolar Deep Water (CDW) and relatively light Antarctic Bottom Water (AABW) are transformed into upper-ocean water masses by mid-gyre upwelling (at a rate of 2 ± 2 Sv) and into denser AABW by downwelling focussed at the western boundary (8 ± 2 Sv). The gyre circulation exhibits a substantial throughflow component, by which CDW and AABW enter the gyre from the Indian sector, undergo ventilation and densification within the gyre, and are exported to the South Atlantic across the gyre's northern rim. The relatively modest net production of AABW in the Weddell Gyre (6±2 Sv) suggests that the gyre's prominence in the closure of the lower limb of global oceanic overturning stems largely from the recycling and equatorward export of Indian-sourced AABW.
format Article in Journal/Newspaper
author Jullion, Loïc
Naveira Garabato, Alberto C.
Bacon, Sheldon
Meredith, Michael P.
Brown, Pete J.
Torres-Valdés, Sinhué
Speer, Kevin G.
Holland, Paul R.
Dong, Jun
Bakker, Dorothée
Hoppema, Mario
Loose, Brice
Venables, Hugh J.
Jenkins, William J.
Messias, Marie-José
Fahrbach, Eberhard
spellingShingle Jullion, Loïc
Naveira Garabato, Alberto C.
Bacon, Sheldon
Meredith, Michael P.
Brown, Pete J.
Torres-Valdés, Sinhué
Speer, Kevin G.
Holland, Paul R.
Dong, Jun
Bakker, Dorothée
Hoppema, Mario
Loose, Brice
Venables, Hugh J.
Jenkins, William J.
Messias, Marie-José
Fahrbach, Eberhard
The contribution of the Weddell Gyre to the lower limb of the global overturning circulation
author_facet Jullion, Loïc
Naveira Garabato, Alberto C.
Bacon, Sheldon
Meredith, Michael P.
Brown, Pete J.
Torres-Valdés, Sinhué
Speer, Kevin G.
Holland, Paul R.
Dong, Jun
Bakker, Dorothée
Hoppema, Mario
Loose, Brice
Venables, Hugh J.
Jenkins, William J.
Messias, Marie-José
Fahrbach, Eberhard
author_sort Jullion, Loïc
title The contribution of the Weddell Gyre to the lower limb of the global overturning circulation
title_short The contribution of the Weddell Gyre to the lower limb of the global overturning circulation
title_full The contribution of the Weddell Gyre to the lower limb of the global overturning circulation
title_fullStr The contribution of the Weddell Gyre to the lower limb of the global overturning circulation
title_full_unstemmed The contribution of the Weddell Gyre to the lower limb of the global overturning circulation
title_sort contribution of the weddell gyre to the lower limb of the global overturning circulation
publishDate 2014
url https://eprints.soton.ac.uk/364845/
https://eprints.soton.ac.uk/364845/1/jgrc20685.pdf
geographic Antarctic
Indian
Southern Ocean
The Antarctic
Weddell
Weddell Sea
geographic_facet Antarctic
Indian
Southern Ocean
The Antarctic
Weddell
Weddell Sea
genre Antarc*
Antarctic
Sea ice
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
Weddell Sea
op_relation https://eprints.soton.ac.uk/364845/1/jgrc20685.pdf
Jullion, Loïc, Naveira Garabato, Alberto C., Bacon, Sheldon, Meredith, Michael P., Brown, Pete J., Torres-Valdés, Sinhué, Speer, Kevin G., Holland, Paul R., Dong, Jun, Bakker, Dorothée, Hoppema, Mario, Loose, Brice, Venables, Hugh J., Jenkins, William J., Messias, Marie-José and Fahrbach, Eberhard (2014) The contribution of the Weddell Gyre to the lower limb of the global overturning circulation. Journal of Geophysical Research: Oceans, 119 (6), 3357-3377. (doi:10.1002/2013JC009725 <http://dx.doi.org/10.1002/2013JC009725>).
op_doi https://doi.org/10.1002/2013JC009725
container_title Journal of Geophysical Research: Oceans
container_volume 119
container_issue 6
container_start_page 3357
op_container_end_page 3377
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