Controls on Wintertime Ventilation in Southern Drake Passage
Abstract Drake Passage is a key region for transport between the surface and interior ocean, but a mechanistic understanding of this exchange remains immature. Here, we present wintertime, submesoscale‐resolving hydrographic transects spanning the southern boundary of the Antarctic Circumpolar Curre...
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Online Access: | https://doi.org/10.1029/2022GL102550 https://doaj.org/article/bc0fa28033b94736a3eb0c7ca8128783 |
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ftdoajarticles:oai:doaj.org/article:bc0fa28033b94736a3eb0c7ca8128783 2024-09-15T17:44:14+00:00 Controls on Wintertime Ventilation in Southern Drake Passage Lilian A. Dove Giuliana A. Viglione Andrew F. Thompson M. Mar Flexas Taylor R. Cason Janet Sprintall 2023-03-01T00:00:00Z https://doi.org/10.1029/2022GL102550 https://doaj.org/article/bc0fa28033b94736a3eb0c7ca8128783 EN eng Wiley https://doi.org/10.1029/2022GL102550 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL102550 https://doaj.org/article/bc0fa28033b94736a3eb0c7ca8128783 Geophysical Research Letters, Vol 50, Iss 5, Pp n/a-n/a (2023) Drake Passage Polar Front eddy suppression submesoscale ventilation Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2022GL102550 2024-08-05T17:49:23Z Abstract Drake Passage is a key region for transport between the surface and interior ocean, but a mechanistic understanding of this exchange remains immature. Here, we present wintertime, submesoscale‐resolving hydrographic transects spanning the southern boundary of the Antarctic Circumpolar Current and the Polar Front (PF). Despite the strong surface wind and buoyancy forcing, a freshwater lens suppresses surface‐interior exchange south of the PF; ventilation is instead localized to the PF. Multiple lines of the analysis suggest submesoscale processes contribute to ventilation at the PF, including small‐scale, O(10 km), frontal structure in water mass properties below the mixed layer and modulation of a surface eddy diffusivity at sub‐50 km scales. These results show that ventilation is sensitive to both submesoscale properties near fronts and non‐local processes, for example, sea‐ice melt, that set stratification and mixed layer properties. This highlights the need for adaptive observing strategies to constrain Southern Ocean heat and carbon budgets. Article in Journal/Newspaper Antarc* Antarctic Drake Passage Sea ice Southern Ocean Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 5 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Drake Passage Polar Front eddy suppression submesoscale ventilation Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Drake Passage Polar Front eddy suppression submesoscale ventilation Geophysics. Cosmic physics QC801-809 Lilian A. Dove Giuliana A. Viglione Andrew F. Thompson M. Mar Flexas Taylor R. Cason Janet Sprintall Controls on Wintertime Ventilation in Southern Drake Passage |
topic_facet |
Drake Passage Polar Front eddy suppression submesoscale ventilation Geophysics. Cosmic physics QC801-809 |
description |
Abstract Drake Passage is a key region for transport between the surface and interior ocean, but a mechanistic understanding of this exchange remains immature. Here, we present wintertime, submesoscale‐resolving hydrographic transects spanning the southern boundary of the Antarctic Circumpolar Current and the Polar Front (PF). Despite the strong surface wind and buoyancy forcing, a freshwater lens suppresses surface‐interior exchange south of the PF; ventilation is instead localized to the PF. Multiple lines of the analysis suggest submesoscale processes contribute to ventilation at the PF, including small‐scale, O(10 km), frontal structure in water mass properties below the mixed layer and modulation of a surface eddy diffusivity at sub‐50 km scales. These results show that ventilation is sensitive to both submesoscale properties near fronts and non‐local processes, for example, sea‐ice melt, that set stratification and mixed layer properties. This highlights the need for adaptive observing strategies to constrain Southern Ocean heat and carbon budgets. |
format |
Article in Journal/Newspaper |
author |
Lilian A. Dove Giuliana A. Viglione Andrew F. Thompson M. Mar Flexas Taylor R. Cason Janet Sprintall |
author_facet |
Lilian A. Dove Giuliana A. Viglione Andrew F. Thompson M. Mar Flexas Taylor R. Cason Janet Sprintall |
author_sort |
Lilian A. Dove |
title |
Controls on Wintertime Ventilation in Southern Drake Passage |
title_short |
Controls on Wintertime Ventilation in Southern Drake Passage |
title_full |
Controls on Wintertime Ventilation in Southern Drake Passage |
title_fullStr |
Controls on Wintertime Ventilation in Southern Drake Passage |
title_full_unstemmed |
Controls on Wintertime Ventilation in Southern Drake Passage |
title_sort |
controls on wintertime ventilation in southern drake passage |
publisher |
Wiley |
publishDate |
2023 |
url |
https://doi.org/10.1029/2022GL102550 https://doaj.org/article/bc0fa28033b94736a3eb0c7ca8128783 |
genre |
Antarc* Antarctic Drake Passage Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Drake Passage Sea ice Southern Ocean |
op_source |
Geophysical Research Letters, Vol 50, Iss 5, Pp n/a-n/a (2023) |
op_relation |
https://doi.org/10.1029/2022GL102550 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL102550 https://doaj.org/article/bc0fa28033b94736a3eb0c7ca8128783 |
op_doi |
https://doi.org/10.1029/2022GL102550 |
container_title |
Geophysical Research Letters |
container_volume |
50 |
container_issue |
5 |
_version_ |
1810491650111176704 |