The Flow of Antarctic Bottom Water into the Brazil Basin
The total transport of Antarctic Bottom Water across the Rio Grande Rise, including the western boundary, the Vema Channel, and the Hunter Channel is estimated from hydrographic measurements across these pathways. The contribution of the Vema Channel is greatest at 3.9 X 10(6) m(3) s(-1), which is v...
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American Meteorological Society
1993
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ftarchimer:oai:archimer.ifremer.fr:30354 2023-05-15T13:50:49+02:00 The Flow of Antarctic Bottom Water into the Brazil Basin Speer, Kevin G Zenk, Walter 1993-12 application/pdf https://archimer.ifremer.fr/doc/00192/30354/29112.pdf https://doi.org/10.1175/1520-0485(1993)023<2667:TFOABW>2.0.CO;2 https://archimer.ifremer.fr/doc/00192/30354/ eng eng American Meteorological Society https://archimer.ifremer.fr/doc/00192/30354/29112.pdf doi:10.1175/1520-0485(1993)023<2667:TFOABW>2.0.CO;2 https://archimer.ifremer.fr/doc/00192/30354/ 1993 American Meteorological Society info:eu-repo/semantics/openAccess restricted use Journal of Physical Oceanography (0022-3670) (American Meteorological Society), 1993-12 , Vol. 23 , N. 12 , P. 2667-2682 text Publication info:eu-repo/semantics/article 1993 ftarchimer https://doi.org/10.1175/1520-0485(1993)023<2667:TFOABW>2.0.CO;2 2021-09-23T20:24:29Z The total transport of Antarctic Bottom Water across the Rio Grande Rise, including the western boundary, the Vema Channel, and the Hunter Channel is estimated from hydrographic measurements across these pathways. The contribution of the Vema Channel is greatest at 3.9 X 10(6) m(3) s(-1), which is very close to earlier estimates. The western boundary current contribution is 2.0 X 10(6) m(3) s(-1) and that of the Hunter Channel 0.7 X 10(6) m(3) s(-1). The lower values outside the Vema Channel are offset by the important source of mass they form to the lower density classes of bottom water. About 40% of the now is concentrated in the highest density class representing the source of Weddell Sea Deep Water to the Brazil Basin. The flow structure is characterized by horizontal and vertical recirculation. Article in Journal/Newspaper Antarc* Antarctic Weddell Sea Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Antarctic Weddell Weddell Sea |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
description |
The total transport of Antarctic Bottom Water across the Rio Grande Rise, including the western boundary, the Vema Channel, and the Hunter Channel is estimated from hydrographic measurements across these pathways. The contribution of the Vema Channel is greatest at 3.9 X 10(6) m(3) s(-1), which is very close to earlier estimates. The western boundary current contribution is 2.0 X 10(6) m(3) s(-1) and that of the Hunter Channel 0.7 X 10(6) m(3) s(-1). The lower values outside the Vema Channel are offset by the important source of mass they form to the lower density classes of bottom water. About 40% of the now is concentrated in the highest density class representing the source of Weddell Sea Deep Water to the Brazil Basin. The flow structure is characterized by horizontal and vertical recirculation. |
format |
Article in Journal/Newspaper |
author |
Speer, Kevin G Zenk, Walter |
spellingShingle |
Speer, Kevin G Zenk, Walter The Flow of Antarctic Bottom Water into the Brazil Basin |
author_facet |
Speer, Kevin G Zenk, Walter |
author_sort |
Speer, Kevin G |
title |
The Flow of Antarctic Bottom Water into the Brazil Basin |
title_short |
The Flow of Antarctic Bottom Water into the Brazil Basin |
title_full |
The Flow of Antarctic Bottom Water into the Brazil Basin |
title_fullStr |
The Flow of Antarctic Bottom Water into the Brazil Basin |
title_full_unstemmed |
The Flow of Antarctic Bottom Water into the Brazil Basin |
title_sort |
flow of antarctic bottom water into the brazil basin |
publisher |
American Meteorological Society |
publishDate |
1993 |
url |
https://archimer.ifremer.fr/doc/00192/30354/29112.pdf https://doi.org/10.1175/1520-0485(1993)023<2667:TFOABW>2.0.CO;2 https://archimer.ifremer.fr/doc/00192/30354/ |
geographic |
Antarctic Weddell Weddell Sea |
geographic_facet |
Antarctic Weddell Weddell Sea |
genre |
Antarc* Antarctic Weddell Sea |
genre_facet |
Antarc* Antarctic Weddell Sea |
op_source |
Journal of Physical Oceanography (0022-3670) (American Meteorological Society), 1993-12 , Vol. 23 , N. 12 , P. 2667-2682 |
op_relation |
https://archimer.ifremer.fr/doc/00192/30354/29112.pdf doi:10.1175/1520-0485(1993)023<2667:TFOABW>2.0.CO;2 https://archimer.ifremer.fr/doc/00192/30354/ |
op_rights |
1993 American Meteorological Society info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1175/1520-0485(1993)023<2667:TFOABW>2.0.CO;2 |
_version_ |
1766254115976904704 |