First resolution of flow through the Hunter Channel in the South Atlantic
Dense Antarctic Bottom Water formed around the continent of Antarctica spreads northward in the Atlantic underneath North Atlantic Deep Water, gradually mixing and upwelling into it. This Antarctic Water forms a significant element of the meridional circulation in both directions: northward as botto...
Published in: | Earth and Planetary Science Letters |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Elsevier
1992
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Online Access: | https://oceanrep.geomar.de/id/eprint/15391/ https://oceanrep.geomar.de/id/eprint/15391/1/Speer.pdf https://doi.org/10.1016/0012-821X(92)90226-L |
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ftoceanrep:oai:oceanrep.geomar.de:15391 2023-05-15T13:37:49+02:00 First resolution of flow through the Hunter Channel in the South Atlantic Speer, Kevin Zenk, Walter Siedler, Gerold Pätzold, Jürgen Heidland, Clemens 1992 text https://oceanrep.geomar.de/id/eprint/15391/ https://oceanrep.geomar.de/id/eprint/15391/1/Speer.pdf https://doi.org/10.1016/0012-821X(92)90226-L en eng Elsevier https://oceanrep.geomar.de/id/eprint/15391/1/Speer.pdf Speer, K., Zenk, W., Siedler, G., Pätzold, J. and Heidland, C. (1992) First resolution of flow through the Hunter Channel in the South Atlantic. Open Access Earth and Planetary Science Letters, 113 (1-2). pp. 287-292. DOI 10.1016/0012-821X(92)90226-L <https://doi.org/10.1016/0012-821X%2892%2990226-L>. doi:10.1016/0012-821X(92)90226-L info:eu-repo/semantics/openAccess Article PeerReviewed 1992 ftoceanrep https://doi.org/10.1016/0012-821X(92)90226-L 2023-04-07T15:05:23Z Dense Antarctic Bottom Water formed around the continent of Antarctica spreads northward in the Atlantic underneath North Atlantic Deep Water, gradually mixing and upwelling into it. This Antarctic Water forms a significant element of the meridional circulation in both directions: northward as bottom water and southward as deep water. It is important to determine the strength of each component to assess its role in ocean circulation. Such measurements are useful when made in constricted pathways because any flow is more clearly defined. A new set of fine-resolution hydrograhic measurements in the Hunter Channel of the South Atlantic Ocean has been obtained, which allow the geostrophic bottom flow there to be estimated for the first time. The northward flow through the Hunter Channel of water cooler than 2-degrees-C is thus estimated to be 0.7 X 10(6) m3 s-1. Article in Journal/Newspaper Antarc* Antarctic Antarctica North Atlantic Deep Water North Atlantic South Atlantic Ocean OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Antarctic Earth and Planetary Science Letters 113 1-2 287 292 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Dense Antarctic Bottom Water formed around the continent of Antarctica spreads northward in the Atlantic underneath North Atlantic Deep Water, gradually mixing and upwelling into it. This Antarctic Water forms a significant element of the meridional circulation in both directions: northward as bottom water and southward as deep water. It is important to determine the strength of each component to assess its role in ocean circulation. Such measurements are useful when made in constricted pathways because any flow is more clearly defined. A new set of fine-resolution hydrograhic measurements in the Hunter Channel of the South Atlantic Ocean has been obtained, which allow the geostrophic bottom flow there to be estimated for the first time. The northward flow through the Hunter Channel of water cooler than 2-degrees-C is thus estimated to be 0.7 X 10(6) m3 s-1. |
format |
Article in Journal/Newspaper |
author |
Speer, Kevin Zenk, Walter Siedler, Gerold Pätzold, Jürgen Heidland, Clemens |
spellingShingle |
Speer, Kevin Zenk, Walter Siedler, Gerold Pätzold, Jürgen Heidland, Clemens First resolution of flow through the Hunter Channel in the South Atlantic |
author_facet |
Speer, Kevin Zenk, Walter Siedler, Gerold Pätzold, Jürgen Heidland, Clemens |
author_sort |
Speer, Kevin |
title |
First resolution of flow through the Hunter Channel in the South Atlantic |
title_short |
First resolution of flow through the Hunter Channel in the South Atlantic |
title_full |
First resolution of flow through the Hunter Channel in the South Atlantic |
title_fullStr |
First resolution of flow through the Hunter Channel in the South Atlantic |
title_full_unstemmed |
First resolution of flow through the Hunter Channel in the South Atlantic |
title_sort |
first resolution of flow through the hunter channel in the south atlantic |
publisher |
Elsevier |
publishDate |
1992 |
url |
https://oceanrep.geomar.de/id/eprint/15391/ https://oceanrep.geomar.de/id/eprint/15391/1/Speer.pdf https://doi.org/10.1016/0012-821X(92)90226-L |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctica North Atlantic Deep Water North Atlantic South Atlantic Ocean |
genre_facet |
Antarc* Antarctic Antarctica North Atlantic Deep Water North Atlantic South Atlantic Ocean |
op_relation |
https://oceanrep.geomar.de/id/eprint/15391/1/Speer.pdf Speer, K., Zenk, W., Siedler, G., Pätzold, J. and Heidland, C. (1992) First resolution of flow through the Hunter Channel in the South Atlantic. Open Access Earth and Planetary Science Letters, 113 (1-2). pp. 287-292. DOI 10.1016/0012-821X(92)90226-L <https://doi.org/10.1016/0012-821X%2892%2990226-L>. doi:10.1016/0012-821X(92)90226-L |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1016/0012-821X(92)90226-L |
container_title |
Earth and Planetary Science Letters |
container_volume |
113 |
container_issue |
1-2 |
container_start_page |
287 |
op_container_end_page |
292 |
_version_ |
1766097999257141248 |