Impact of the Indonesian Throughflow on Agulhas leakage

Using ocean models of different complexity we show that opening the Indonesian Passage between the Pacific and the Indian oceans increases the input of Indian Ocean water into the South Atlantic via the Agulhas leakage. In a strongly eddying global ocean model this response results from an increased...

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Main Authors: D. Le Bars, H. A. Dijkstra, W. P. M. De Ruijter
Format: Article
Language:English
Published: Copernicus Publications 2013-09-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/9/773/2013/os-9-773-2013.pdf
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author D. Le Bars
H. A. Dijkstra
W. P. M. De Ruijter
author_facet D. Le Bars
H. A. Dijkstra
W. P. M. De Ruijter
author_sort D. Le Bars
collection DOAJ
description Using ocean models of different complexity we show that opening the Indonesian Passage between the Pacific and the Indian oceans increases the input of Indian Ocean water into the South Atlantic via the Agulhas leakage. In a strongly eddying global ocean model this response results from an increased Agulhas Current transport and a constant proportion of Agulhas retroflection south of Africa. The leakage increases through an increased frequency of ring shedding events. In an idealized two-layer and flat-bottom eddy resolving model, the proportion of the Agulhas Current transport that retroflects is (for a wide range of wind stress forcing) not affected by an opening of the Indonesian Passage. Using a comparison with a linear model and previous work on the retroflection problem, the result is explained as a balance between two mechanisms: decrease retroflection due to large-scale momentum balance and increase due to local barotropic/baroclinic instabilities.
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spelling doaj.art-390c918bed0d4c2e957f08e1e98201d72022-12-21T19:28:26ZengCopernicus PublicationsOcean Science1812-07841812-07922013-09-019577378510.5194/os-9-773-2013Impact of the Indonesian Throughflow on Agulhas leakageD. Le BarsH. A. DijkstraW. P. M. De RuijterUsing ocean models of different complexity we show that opening the Indonesian Passage between the Pacific and the Indian oceans increases the input of Indian Ocean water into the South Atlantic via the Agulhas leakage. In a strongly eddying global ocean model this response results from an increased Agulhas Current transport and a constant proportion of Agulhas retroflection south of Africa. The leakage increases through an increased frequency of ring shedding events. In an idealized two-layer and flat-bottom eddy resolving model, the proportion of the Agulhas Current transport that retroflects is (for a wide range of wind stress forcing) not affected by an opening of the Indonesian Passage. Using a comparison with a linear model and previous work on the retroflection problem, the result is explained as a balance between two mechanisms: decrease retroflection due to large-scale momentum balance and increase due to local barotropic/baroclinic instabilities.http://www.ocean-sci.net/9/773/2013/os-9-773-2013.pdf
spellingShingle D. Le Bars
H. A. Dijkstra
W. P. M. De Ruijter
Impact of the Indonesian Throughflow on Agulhas leakage
Ocean Science
title Impact of the Indonesian Throughflow on Agulhas leakage
title_full Impact of the Indonesian Throughflow on Agulhas leakage
title_fullStr Impact of the Indonesian Throughflow on Agulhas leakage
title_full_unstemmed Impact of the Indonesian Throughflow on Agulhas leakage
title_short Impact of the Indonesian Throughflow on Agulhas leakage
title_sort impact of the indonesian throughflow on agulhas leakage
url http://www.ocean-sci.net/9/773/2013/os-9-773-2013.pdf
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