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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Main Authors: Wang, J, Mazloff, MR, Gille, ST
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2014
Subjects:
Online Access:https://escholarship.org/uc/item/88h1698w
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spelling 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
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