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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Published in:Scientia Marina
Main Authors: Glorioso, P., Piola, A., Leben, R.
Format: Book
Language:English
Published: 2005
Subjects:
Online Access:http://hdl.handle.net/1834/17131
https://doi.org/10.3989/scimar.2005.69s27
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spelling ftoceandocs:oai:aquadocs.org:1834/17131 2024-06-09T07:40:56+00:00 Mesoscale eddies in the Subantarctic Front - Southwest Atlantic Glorioso, P. Piola, A. Leben, R. 2005 pp.7-15 http://hdl.handle.net/1834/17131 https://doi.org/10.3989/scimar.2005.69s27 en eng https://doi.org/10.3989/scimar.2005.69s27 http://hdl.handle.net/1834/17131 Journal Contribution Refereed 2005 ftoceandocs https://doi.org/10.3989/scimar.2005.69s27 2024-05-15T08:02:16Z 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 fea- ture 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 50S which may contribute to the patchiness, transport and mixing of passive scalars by this strong, turbu- lent 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, sug- gesting that cross-frontal eddy transport and strong meandering occur where the ACC flow intensifies along the sub-Antarc- tic Front (SAF) and the Southern ACC Front (SACCF). Published Book Antarc* Antarctic IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications Antarctic Lent ENVELOPE(-66.783,-66.783,-66.867,-66.867) The Antarctic Scientia Marina 69 S2 7 15
institution Open Polar
collection IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications
op_collection_id ftoceandocs
language English
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 fea- ture 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 50S which may contribute to the patchiness, transport and mixing of passive scalars by this strong, turbu- lent 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, sug- gesting that cross-frontal eddy transport and strong meandering occur where the ACC flow intensifies along the sub-Antarc- tic Front (SAF) and the Southern ACC Front (SACCF). Published
format Book
author Glorioso, P.
Piola, A.
Leben, R.
spellingShingle Glorioso, P.
Piola, A.
Leben, R.
Mesoscale eddies in the Subantarctic Front - Southwest Atlantic
author_facet Glorioso, P.
Piola, A.
Leben, R.
author_sort Glorioso, P.
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
publishDate 2005
url http://hdl.handle.net/1834/17131
https://doi.org/10.3989/scimar.2005.69s27
long_lat ENVELOPE(-66.783,-66.783,-66.867,-66.867)
geographic Antarctic
Lent
The Antarctic
geographic_facet Antarctic
Lent
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation https://doi.org/10.3989/scimar.2005.69s27
http://hdl.handle.net/1834/17131
op_doi https://doi.org/10.3989/scimar.2005.69s27
container_title Scientia Marina
container_volume 69
container_issue S2
container_start_page 7
op_container_end_page 15
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