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...
Published in: | Scientia Marina |
---|---|
Main Authors: | , , |
Format: | Book |
Language: | English |
Published: |
2005
|
Subjects: | |
Online Access: | http://hdl.handle.net/1834/17131 https://doi.org/10.3989/scimar.2005.69s27 |
id |
ftoceandocs:oai:aquadocs.org:1834/17131 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1801369348281991168 |