Path of the North Atlantic Deep Water in the Brazil Basin
Recent hydrographic sections and high-quality historical data sets are used to determine geostrophic currents at subtropical latitudes in the western basin of the South Atlantic. Levels of no motion are determined from water mass information and a mass balance constraint to obtain the transport fiel...
Published in: | Journal of Geophysical Research: Oceans |
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Language: | English |
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AGU (American Geophysical Union)
1998
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Online Access: | https://oceanrep.geomar.de/id/eprint/6855/ https://oceanrep.geomar.de/id/eprint/6855/1/97JC03287.pdf https://doi.org/10.1029/97JC03287 |
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ftoceanrep:oai:oceanrep.geomar.de:6855 2023-05-15T17:13:49+02:00 Path of the North Atlantic Deep Water in the Brazil Basin Zangenberg, Norbert Siedler, Gerold 1998 text https://oceanrep.geomar.de/id/eprint/6855/ https://oceanrep.geomar.de/id/eprint/6855/1/97JC03287.pdf https://doi.org/10.1029/97JC03287 en eng AGU (American Geophysical Union) https://oceanrep.geomar.de/id/eprint/6855/1/97JC03287.pdf Zangenberg, N. and Siedler, G. (1998) Path of the North Atlantic Deep Water in the Brazil Basin. Open Access Journal of Geophysical Research: Oceans, 103 (C3). pp. 5419-5428. DOI 10.1029/97JC03287 <https://doi.org/10.1029/97JC03287>. doi:10.1029/97JC03287 info:eu-repo/semantics/openAccess Article PeerReviewed 1998 ftoceanrep https://doi.org/10.1029/97JC03287 2023-04-07T14:53:46Z Recent hydrographic sections and high-quality historical data sets are used to determine geostrophic currents at subtropical latitudes in the western basin of the South Atlantic. Levels of no motion are determined from water mass information and a mass balance constraint to obtain the transport field of North Atlantic Deep Water (NADW) in this region. The incoming NADW transport of about 20 Sv from the north at 19 degrees S appears to be balanced by only one third of this transport leaving in the south and two thirds leaving to the east or northeast at the Mid-Atlantic Ridge. A simple model is proposed to determine the cause of the NADW branching. It is shown that potential vorticity preservation in the presence of topographic changes leads to a similar flow pattern as observed, with branching near the Vitoria-Trindade-Ridge and also an eastward turning of the southward western boundary current at about 28 degrees S, the latitude where a balance of planetary vorticity change and stretching can be expected. Article in Journal/Newspaper NADW North Atlantic Deep Water North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Mid-Atlantic Ridge Western Basin Journal of Geophysical Research: Oceans 103 C3 5419 5428 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Recent hydrographic sections and high-quality historical data sets are used to determine geostrophic currents at subtropical latitudes in the western basin of the South Atlantic. Levels of no motion are determined from water mass information and a mass balance constraint to obtain the transport field of North Atlantic Deep Water (NADW) in this region. The incoming NADW transport of about 20 Sv from the north at 19 degrees S appears to be balanced by only one third of this transport leaving in the south and two thirds leaving to the east or northeast at the Mid-Atlantic Ridge. A simple model is proposed to determine the cause of the NADW branching. It is shown that potential vorticity preservation in the presence of topographic changes leads to a similar flow pattern as observed, with branching near the Vitoria-Trindade-Ridge and also an eastward turning of the southward western boundary current at about 28 degrees S, the latitude where a balance of planetary vorticity change and stretching can be expected. |
format |
Article in Journal/Newspaper |
author |
Zangenberg, Norbert Siedler, Gerold |
spellingShingle |
Zangenberg, Norbert Siedler, Gerold Path of the North Atlantic Deep Water in the Brazil Basin |
author_facet |
Zangenberg, Norbert Siedler, Gerold |
author_sort |
Zangenberg, Norbert |
title |
Path of the North Atlantic Deep Water in the Brazil Basin |
title_short |
Path of the North Atlantic Deep Water in the Brazil Basin |
title_full |
Path of the North Atlantic Deep Water in the Brazil Basin |
title_fullStr |
Path of the North Atlantic Deep Water in the Brazil Basin |
title_full_unstemmed |
Path of the North Atlantic Deep Water in the Brazil Basin |
title_sort |
path of the north atlantic deep water in the brazil basin |
publisher |
AGU (American Geophysical Union) |
publishDate |
1998 |
url |
https://oceanrep.geomar.de/id/eprint/6855/ https://oceanrep.geomar.de/id/eprint/6855/1/97JC03287.pdf https://doi.org/10.1029/97JC03287 |
geographic |
Mid-Atlantic Ridge Western Basin |
geographic_facet |
Mid-Atlantic Ridge Western Basin |
genre |
NADW North Atlantic Deep Water North Atlantic |
genre_facet |
NADW North Atlantic Deep Water North Atlantic |
op_relation |
https://oceanrep.geomar.de/id/eprint/6855/1/97JC03287.pdf Zangenberg, N. and Siedler, G. (1998) Path of the North Atlantic Deep Water in the Brazil Basin. Open Access Journal of Geophysical Research: Oceans, 103 (C3). pp. 5419-5428. DOI 10.1029/97JC03287 <https://doi.org/10.1029/97JC03287>. doi:10.1029/97JC03287 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/97JC03287 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
103 |
container_issue |
C3 |
container_start_page |
5419 |
op_container_end_page |
5428 |
_version_ |
1766071012999299072 |