Mesoscale eddies in the Subantarctic Front-Southwest Atlantic

Satellite and ship observations in the southern southwest Atlantic (SSWA) reveal an intense eddy field and highlight the potential for using continuous real-time satellite altimetry to detect and monitor mesoscale phenomena with a view to understanding the regional circulation. The examples presente...

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Main Authors: Pablo D. Glorioso, Alberto R. Piola, Robert R. Leben
Format: Article
Language:English
Published: Consejo Superior de Investigaciones Científicas 2005-12-01
Series:Scientia Marina
Subjects:
Online Access:http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/307
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spelling doaj-32843d96f41540c482141242670315812021-05-05T13:49:44ZengConsejo Superior de Investigaciones CientíficasScientia Marina0214-83581886-81342005-12-0169S271510.3989/scimar.2005.69s27303Mesoscale eddies in the Subantarctic Front-Southwest AtlanticPablo D. Glorioso0Alberto R. Piola1Robert R. Leben2British Antarctic SurveyDepto. Oceanografía, Servicio de Hidrografía Naval and Depto. Cs. de la Atmósfera y los Océanos, Universidad de Buenos AiresColorado Center for Astrodynamics Research, University of ColoradoSatellite and ship observations in the southern southwest Atlantic (SSWA) reveal an intense eddy field and highlight the potential for using continuous real-time satellite altimetry to detect and monitor mesoscale phenomena with a view to understanding the regional circulation. The examples presented suggest that mesoscale eddies are a dominant feature of the circulation and play a fundamental role in the transport of properties along and across the Antarctic Circumpolar Current (ACC). The main ocean current in the SSWA, the Falkland-Malvinas Current (FMC), exhibits numerous embedded eddies south of 50°S which may contribute to the patchiness, transport and mixing of passive scalars by this strong, turbulent current. Large eddies associated with meanders are observed in the ACC fronts, some of them remaining stationary for long periods. Two particular cases are examined using a satellite altimeter in combination with in situ observations, suggesting that cross-frontal eddy transport and strong meandering occur where the ACC flow intensifies along the sub-Antarctic Front (SAF) and the Southern ACC Front (SACCF).http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/307southwest atlanticmesoscaleeddiestransportfalkland-malvinas current
collection DOAJ
language English
format Article
sources DOAJ
author Pablo D. Glorioso
Alberto R. Piola
Robert R. Leben
spellingShingle Pablo D. Glorioso
Alberto R. Piola
Robert R. Leben
Mesoscale eddies in the Subantarctic Front-Southwest Atlantic
Scientia Marina
southwest atlantic
mesoscale
eddies
transport
falkland-malvinas current
author_facet Pablo D. Glorioso
Alberto R. Piola
Robert R. Leben
author_sort Pablo D. Glorioso
title Mesoscale eddies in the Subantarctic Front-Southwest Atlantic
title_short Mesoscale eddies in the Subantarctic Front-Southwest Atlantic
title_full Mesoscale eddies in the Subantarctic Front-Southwest Atlantic
title_fullStr Mesoscale eddies in the Subantarctic Front-Southwest Atlantic
title_full_unstemmed Mesoscale eddies in the Subantarctic Front-Southwest Atlantic
title_sort mesoscale eddies in the subantarctic front-southwest atlantic
publisher Consejo Superior de Investigaciones Científicas
series Scientia Marina
issn 0214-8358
1886-8134
publishDate 2005-12-01
description Satellite and ship observations in the southern southwest Atlantic (SSWA) reveal an intense eddy field and highlight the potential for using continuous real-time satellite altimetry to detect and monitor mesoscale phenomena with a view to understanding the regional circulation. The examples presented suggest that mesoscale eddies are a dominant feature of the circulation and play a fundamental role in the transport of properties along and across the Antarctic Circumpolar Current (ACC). The main ocean current in the SSWA, the Falkland-Malvinas Current (FMC), exhibits numerous embedded eddies south of 50°S which may contribute to the patchiness, transport and mixing of passive scalars by this strong, turbulent current. Large eddies associated with meanders are observed in the ACC fronts, some of them remaining stationary for long periods. Two particular cases are examined using a satellite altimeter in combination with in situ observations, suggesting that cross-frontal eddy transport and strong meandering occur where the ACC flow intensifies along the sub-Antarctic Front (SAF) and the Southern ACC Front (SACCF).
topic southwest atlantic
mesoscale
eddies
transport
falkland-malvinas current
url http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/307
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