Observing the local emergence of the Southern Ocean residual-mean circulation
The role of mesoscale turbulence in maintaining the mean buoyancy structure and overturning circulation of the Southern Ocean is investigated through a 2-year-long, single-mooring record of measurements in Drake Passage. The buoyancy budget of the area is successively assessed within the Eulerian an...
Published in: | Geophysical Research Letters |
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Language: | English |
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ftsouthampton:oai:eprints.soton.ac.uk:430530 2023-08-27T04:04:37+02:00 Observing the local emergence of the Southern Ocean residual-mean circulation Sévellec, F. Naveira Garabato, A.C. Vic, C. Ducousso, N. 2019-04-16 text https://eprints.soton.ac.uk/430530/ https://eprints.soton.ac.uk/430530/1/sevellec_et_al_grl19.pdf https://eprints.soton.ac.uk/430530/2/S_vellec_et_al_2019_Geophysical_Research_Letters.pdf en English eng https://eprints.soton.ac.uk/430530/1/sevellec_et_al_grl19.pdf https://eprints.soton.ac.uk/430530/2/S_vellec_et_al_2019_Geophysical_Research_Letters.pdf Sévellec, F., Naveira Garabato, A.C., Vic, C. and Ducousso, N. (2019) Observing the local emergence of the Southern Ocean residual-mean circulation. Geophysical Research Letters, 46 (7), 3862-3870. (doi:10.1029/2018GL081382 <http://dx.doi.org/10.1029/2018GL081382>). accepted_manuscript cc_by_4 Article PeerReviewed 2019 ftsouthampton https://doi.org/10.1029/2018GL081382 2023-08-03T22:23:52Z The role of mesoscale turbulence in maintaining the mean buoyancy structure and overturning circulation of the Southern Ocean is investigated through a 2-year-long, single-mooring record of measurements in Drake Passage. The buoyancy budget of the area is successively assessed within the Eulerian and the Temporal-Residual-Mean frameworks. We find that a regime change occurs on time scales of 1 to 100 days, characteristic of mesoscale dynamics, whereby the eddy-induced turbulent horizontal advection balances the vertical buoyancy advection by the mean flow. We use these diagnostics to reconstruct the region's overturning circulation, which is found to entail an equatorward downwelling of Antarctic Intermediate and Bottom Waters and a poleward upwelling of Circumpolar Deep Water. The estimated eddy-induced flow can be accurately parameterized via the Gent-McWilliams closure by adopting a diffusivity of ∼2,000 m 2 s −1 with a middepth increase to 2,500 m 2 s −1 at 2,100 m, immediately underneath the maximum interior stratification. Article in Journal/Newspaper Antarc* Antarctic Drake Passage Southern Ocean University of Southampton: e-Prints Soton Antarctic Drake Passage Southern Ocean Geophysical Research Letters 46 7 3862 3870 |
institution |
Open Polar |
collection |
University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
English |
description |
The role of mesoscale turbulence in maintaining the mean buoyancy structure and overturning circulation of the Southern Ocean is investigated through a 2-year-long, single-mooring record of measurements in Drake Passage. The buoyancy budget of the area is successively assessed within the Eulerian and the Temporal-Residual-Mean frameworks. We find that a regime change occurs on time scales of 1 to 100 days, characteristic of mesoscale dynamics, whereby the eddy-induced turbulent horizontal advection balances the vertical buoyancy advection by the mean flow. We use these diagnostics to reconstruct the region's overturning circulation, which is found to entail an equatorward downwelling of Antarctic Intermediate and Bottom Waters and a poleward upwelling of Circumpolar Deep Water. The estimated eddy-induced flow can be accurately parameterized via the Gent-McWilliams closure by adopting a diffusivity of ∼2,000 m 2 s −1 with a middepth increase to 2,500 m 2 s −1 at 2,100 m, immediately underneath the maximum interior stratification. |
format |
Article in Journal/Newspaper |
author |
Sévellec, F. Naveira Garabato, A.C. Vic, C. Ducousso, N. |
spellingShingle |
Sévellec, F. Naveira Garabato, A.C. Vic, C. Ducousso, N. Observing the local emergence of the Southern Ocean residual-mean circulation |
author_facet |
Sévellec, F. Naveira Garabato, A.C. Vic, C. Ducousso, N. |
author_sort |
Sévellec, F. |
title |
Observing the local emergence of the Southern Ocean residual-mean circulation |
title_short |
Observing the local emergence of the Southern Ocean residual-mean circulation |
title_full |
Observing the local emergence of the Southern Ocean residual-mean circulation |
title_fullStr |
Observing the local emergence of the Southern Ocean residual-mean circulation |
title_full_unstemmed |
Observing the local emergence of the Southern Ocean residual-mean circulation |
title_sort |
observing the local emergence of the southern ocean residual-mean circulation |
publishDate |
2019 |
url |
https://eprints.soton.ac.uk/430530/ https://eprints.soton.ac.uk/430530/1/sevellec_et_al_grl19.pdf https://eprints.soton.ac.uk/430530/2/S_vellec_et_al_2019_Geophysical_Research_Letters.pdf |
geographic |
Antarctic Drake Passage Southern Ocean |
geographic_facet |
Antarctic Drake Passage Southern Ocean |
genre |
Antarc* Antarctic Drake Passage Southern Ocean |
genre_facet |
Antarc* Antarctic Drake Passage Southern Ocean |
op_relation |
https://eprints.soton.ac.uk/430530/1/sevellec_et_al_grl19.pdf https://eprints.soton.ac.uk/430530/2/S_vellec_et_al_2019_Geophysical_Research_Letters.pdf Sévellec, F., Naveira Garabato, A.C., Vic, C. and Ducousso, N. (2019) Observing the local emergence of the Southern Ocean residual-mean circulation. Geophysical Research Letters, 46 (7), 3862-3870. (doi:10.1029/2018GL081382 <http://dx.doi.org/10.1029/2018GL081382>). |
op_rights |
accepted_manuscript cc_by_4 |
op_doi |
https://doi.org/10.1029/2018GL081382 |
container_title |
Geophysical Research Letters |
container_volume |
46 |
container_issue |
7 |
container_start_page |
3862 |
op_container_end_page |
3870 |
_version_ |
1775352467831128064 |