Pathways of the Agulhas waters poleward of 29°S
Passive tracers are advected in a Southern Ocean State Estimate (SOSE) to map the pathways of Agulhas waters, with a focus on determining where the Agulhas waters intrude into the Antarctic Circumpolar Current (ACC). Results show that Agulhas waters spread into all three ocean basins within 3 years...
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ftcdlib:oai:escholarship.org/ark:/13030/qt88h1698w 2023-05-15T13:33:01+02:00 Pathways of the Agulhas waters poleward of 29°S Wang, J Mazloff, MR Gille, ST 4234 - 4250 2014-01-01 application/pdf https://escholarship.org/uc/item/88h1698w unknown eScholarship, University of California qt88h1698w https://escholarship.org/uc/item/88h1698w public Journal of Geophysical Research: Oceans, vol 119, iss 7 Geophysics Oceanography Physical Geography and Environmental Geoscience article 2014 ftcdlib 2021-02-18T15:14:38Z Passive tracers are advected in a Southern Ocean State Estimate (SOSE) to map the pathways of Agulhas waters, with a focus on determining where the Agulhas waters intrude into the Antarctic Circumpolar Current (ACC). Results show that Agulhas waters spread into all three ocean basins within 3 years of release. After leaving the African continent, the mean Agulhas water pathway tilts northwest toward the South Atlantic and southeast toward the ACC. The majority (from 60% to 100% depending on specific water mass) of the Agulhas waters stay in the South Indian Ocean north of the Sub-Antarctic Front. From 10 to 28% enters the South Atlantic Ocean through the boundary current along the southern tip of South Africa and via Agulhas rings in the retroflection region. Up to 12% of intermediate depth Agulhas waters enter the ACC. Most of the tracer transport into the ACC occurs just downstream of the Kerguelen Plateau, which clearly demonstrates the importance of topography in elevating cross-frontal exchange. Agulhas waters also contribute to Sub-Antarctic Mode Water formation in the Southeast Indian Ocean by lateral advection. The surface Agulhas waters are preconditioned by strong surface buoyancy loss before turning into mode water, while the intermediate Agulhas waters are advected to the mode water formation region along isopycnals before being drawn into the mixed layer. Key Points The pathways of Agulhas waters are mapped using passive tracer in SOSE Agulhas waters can be mixed into the SEISAMW and ACC Cross-ACC mixing is aggrandized by topography © 2014. American Geophysical Union. All Rights Reserved. Article in Journal/Newspaper Antarc* Antarctic South Atlantic Ocean Southern Ocean University of California: eScholarship Antarctic Southern Ocean The Antarctic Kerguelen Indian |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
unknown |
topic |
Geophysics Oceanography Physical Geography and Environmental Geoscience |
spellingShingle |
Geophysics Oceanography Physical Geography and Environmental Geoscience Wang, J Mazloff, MR Gille, ST Pathways of the Agulhas waters poleward of 29°S |
topic_facet |
Geophysics Oceanography Physical Geography and Environmental Geoscience |
description |
Passive tracers are advected in a Southern Ocean State Estimate (SOSE) to map the pathways of Agulhas waters, with a focus on determining where the Agulhas waters intrude into the Antarctic Circumpolar Current (ACC). Results show that Agulhas waters spread into all three ocean basins within 3 years of release. After leaving the African continent, the mean Agulhas water pathway tilts northwest toward the South Atlantic and southeast toward the ACC. The majority (from 60% to 100% depending on specific water mass) of the Agulhas waters stay in the South Indian Ocean north of the Sub-Antarctic Front. From 10 to 28% enters the South Atlantic Ocean through the boundary current along the southern tip of South Africa and via Agulhas rings in the retroflection region. Up to 12% of intermediate depth Agulhas waters enter the ACC. Most of the tracer transport into the ACC occurs just downstream of the Kerguelen Plateau, which clearly demonstrates the importance of topography in elevating cross-frontal exchange. Agulhas waters also contribute to Sub-Antarctic Mode Water formation in the Southeast Indian Ocean by lateral advection. The surface Agulhas waters are preconditioned by strong surface buoyancy loss before turning into mode water, while the intermediate Agulhas waters are advected to the mode water formation region along isopycnals before being drawn into the mixed layer. Key Points The pathways of Agulhas waters are mapped using passive tracer in SOSE Agulhas waters can be mixed into the SEISAMW and ACC Cross-ACC mixing is aggrandized by topography © 2014. American Geophysical Union. All Rights Reserved. |
format |
Article in Journal/Newspaper |
author |
Wang, J Mazloff, MR Gille, ST |
author_facet |
Wang, J Mazloff, MR Gille, ST |
author_sort |
Wang, J |
title |
Pathways of the Agulhas waters poleward of 29°S |
title_short |
Pathways of the Agulhas waters poleward of 29°S |
title_full |
Pathways of the Agulhas waters poleward of 29°S |
title_fullStr |
Pathways of the Agulhas waters poleward of 29°S |
title_full_unstemmed |
Pathways of the Agulhas waters poleward of 29°S |
title_sort |
pathways of the agulhas waters poleward of 29°s |
publisher |
eScholarship, University of California |
publishDate |
2014 |
url |
https://escholarship.org/uc/item/88h1698w |
op_coverage |
4234 - 4250 |
geographic |
Antarctic Southern Ocean The Antarctic Kerguelen Indian |
geographic_facet |
Antarctic Southern Ocean The Antarctic Kerguelen Indian |
genre |
Antarc* Antarctic South Atlantic Ocean Southern Ocean |
genre_facet |
Antarc* Antarctic South Atlantic Ocean Southern Ocean |
op_source |
Journal of Geophysical Research: Oceans, vol 119, iss 7 |
op_relation |
qt88h1698w https://escholarship.org/uc/item/88h1698w |
op_rights |
public |
_version_ |
1766037846955655168 |