Transformation of an Agulhas eddy near the continental slope

The transformation of Agulhas eddies near the continental slope of southern Africa and their subsequent self-propagation are analyzed in both observational data and numerical simulations. Self-propagation results from a net dipole moment of a generalized heton structure consisting of a surface-inten...

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Main Authors: S. Baker-Yeboah, G. R. Flierl, G. G. Sutyrin, Y. Zhang
Format: Article
Language:English
Published: Copernicus Publications 2010-02-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/6/143/2010/os-6-143-2010.pdf
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author S. Baker-Yeboah
G. R. Flierl
G. G. Sutyrin
Y. Zhang
author_facet S. Baker-Yeboah
G. R. Flierl
G. G. Sutyrin
Y. Zhang
author_sort S. Baker-Yeboah
collection DOAJ
description The transformation of Agulhas eddies near the continental slope of southern Africa and their subsequent self-propagation are analyzed in both observational data and numerical simulations. Self-propagation results from a net dipole moment of a generalized heton structure consisting of a surface-intensified anticyclonic eddy and deep cyclonic pattern. Such Agulhas vortical structures can form near the retroflection region and further north along the western coast of southern Africa. We analyze nonlinear topographic wave generation, vortex deformations, and filament production as an important part in water mass exchange. Self-propagating structures provide a conduit for exchange between the deep ocean and shelf regions in the Benguela upwelling system.
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spelling doaj.art-8f05dfc7322a4073bec842ae7a223f7f2022-12-21T20:39:34ZengCopernicus PublicationsOcean Science1812-07841812-07922010-02-0161143159Transformation of an Agulhas eddy near the continental slopeS. Baker-YeboahG. R. FlierlG. G. SutyrinY. ZhangThe transformation of Agulhas eddies near the continental slope of southern Africa and their subsequent self-propagation are analyzed in both observational data and numerical simulations. Self-propagation results from a net dipole moment of a generalized heton structure consisting of a surface-intensified anticyclonic eddy and deep cyclonic pattern. Such Agulhas vortical structures can form near the retroflection region and further north along the western coast of southern Africa. We analyze nonlinear topographic wave generation, vortex deformations, and filament production as an important part in water mass exchange. Self-propagating structures provide a conduit for exchange between the deep ocean and shelf regions in the Benguela upwelling system.http://www.ocean-sci.net/6/143/2010/os-6-143-2010.pdf
spellingShingle S. Baker-Yeboah
G. R. Flierl
G. G. Sutyrin
Y. Zhang
Transformation of an Agulhas eddy near the continental slope
Ocean Science
title Transformation of an Agulhas eddy near the continental slope
title_full Transformation of an Agulhas eddy near the continental slope
title_fullStr Transformation of an Agulhas eddy near the continental slope
title_full_unstemmed Transformation of an Agulhas eddy near the continental slope
title_short Transformation of an Agulhas eddy near the continental slope
title_sort transformation of an agulhas eddy near the continental slope
url http://www.ocean-sci.net/6/143/2010/os-6-143-2010.pdf
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AT ggsutyrin transformationofanagulhaseddynearthecontinentalslope
AT yzhang transformationofanagulhaseddynearthecontinentalslope