The Conrad Rise as an obstruction to the Antarctic Circumpolar Current
The Antarctic Circumpolar Current (ACC) carries water freely around the whole continent of Antarctica, but not without obstructions. Some, such as the Drake Passage, constrict its path, while others, such as mid-ocean ridges, may induce meandering in the current's cores and may cause the genesi...
Published in: | Geophysical Research Letters |
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Language: | English |
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AGU (American Geophysical Union)
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Online Access: | https://oceanrep.geomar.de/id/eprint/2486/ https://oceanrep.geomar.de/id/eprint/2486/1/Durgadoo_et_al-2008-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2008GL035382 |
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ftoceanrep:oai:oceanrep.geomar.de:2486 2024-09-30T14:26:38+00:00 The Conrad Rise as an obstruction to the Antarctic Circumpolar Current Durgadoo, Jonathan V. Lutjeharms, J. R. E. Biastoch, Arne Ansorge, I. J. 2008-10-28 text https://oceanrep.geomar.de/id/eprint/2486/ https://oceanrep.geomar.de/id/eprint/2486/1/Durgadoo_et_al-2008-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2008GL035382 en eng AGU (American Geophysical Union) https://oceanrep.geomar.de/id/eprint/2486/1/Durgadoo_et_al-2008-Geophysical_Research_Letters.pdf Durgadoo, J. V. , Lutjeharms, J. R. E., Biastoch, A. and Ansorge, I. J. (2008) The Conrad Rise as an obstruction to the Antarctic Circumpolar Current. Open Access Geophysical Research Letters, 35 (20). L20606. DOI 10.1029/2008GL035382 <https://doi.org/10.1029/2008GL035382>. doi:10.1029/2008GL035382 info:eu-repo/semantics/openAccess Article PeerReviewed 2008 ftoceanrep https://doi.org/10.1029/2008GL035382 2024-09-04T05:04:40Z The Antarctic Circumpolar Current (ACC) carries water freely around the whole continent of Antarctica, but not without obstructions. Some, such as the Drake Passage, constrict its path, while others, such as mid-ocean ridges, may induce meandering in the current's cores and may cause the genesis of mesoscale turbulence. It has recently been demonstrated that some regions that are only relatively shallow may also have a major effect on the flow patterns of the ACC. This is here shown to be particularly true for the Conrad Rise. Using the trajectories of surface drifters, altimetry and the simulated velocities from a numerical model, we show that the ACC bifurcates at the western side of this Rise. In this process it forms two intense jets at the two meridional extremities of the Rise with a relatively stagnant water body over the Rise itself. Preliminary results from a recent cruise provide compelling support for this portrayal. Article in Journal/Newspaper Antarc* Antarctic Antarctica Drake Passage OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Antarctic The Antarctic Drake Passage Conrad Rise ENVELOPE(41.000,41.000,-53.000,-53.000) Geophysical Research Letters 35 20 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
The Antarctic Circumpolar Current (ACC) carries water freely around the whole continent of Antarctica, but not without obstructions. Some, such as the Drake Passage, constrict its path, while others, such as mid-ocean ridges, may induce meandering in the current's cores and may cause the genesis of mesoscale turbulence. It has recently been demonstrated that some regions that are only relatively shallow may also have a major effect on the flow patterns of the ACC. This is here shown to be particularly true for the Conrad Rise. Using the trajectories of surface drifters, altimetry and the simulated velocities from a numerical model, we show that the ACC bifurcates at the western side of this Rise. In this process it forms two intense jets at the two meridional extremities of the Rise with a relatively stagnant water body over the Rise itself. Preliminary results from a recent cruise provide compelling support for this portrayal. |
format |
Article in Journal/Newspaper |
author |
Durgadoo, Jonathan V. Lutjeharms, J. R. E. Biastoch, Arne Ansorge, I. J. |
spellingShingle |
Durgadoo, Jonathan V. Lutjeharms, J. R. E. Biastoch, Arne Ansorge, I. J. The Conrad Rise as an obstruction to the Antarctic Circumpolar Current |
author_facet |
Durgadoo, Jonathan V. Lutjeharms, J. R. E. Biastoch, Arne Ansorge, I. J. |
author_sort |
Durgadoo, Jonathan V. |
title |
The Conrad Rise as an obstruction to the Antarctic Circumpolar Current |
title_short |
The Conrad Rise as an obstruction to the Antarctic Circumpolar Current |
title_full |
The Conrad Rise as an obstruction to the Antarctic Circumpolar Current |
title_fullStr |
The Conrad Rise as an obstruction to the Antarctic Circumpolar Current |
title_full_unstemmed |
The Conrad Rise as an obstruction to the Antarctic Circumpolar Current |
title_sort |
conrad rise as an obstruction to the antarctic circumpolar current |
publisher |
AGU (American Geophysical Union) |
publishDate |
2008 |
url |
https://oceanrep.geomar.de/id/eprint/2486/ https://oceanrep.geomar.de/id/eprint/2486/1/Durgadoo_et_al-2008-Geophysical_Research_Letters.pdf https://doi.org/10.1029/2008GL035382 |
long_lat |
ENVELOPE(41.000,41.000,-53.000,-53.000) |
geographic |
Antarctic The Antarctic Drake Passage Conrad Rise |
geographic_facet |
Antarctic The Antarctic Drake Passage Conrad Rise |
genre |
Antarc* Antarctic Antarctica Drake Passage |
genre_facet |
Antarc* Antarctic Antarctica Drake Passage |
op_relation |
https://oceanrep.geomar.de/id/eprint/2486/1/Durgadoo_et_al-2008-Geophysical_Research_Letters.pdf Durgadoo, J. V. , Lutjeharms, J. R. E., Biastoch, A. and Ansorge, I. J. (2008) The Conrad Rise as an obstruction to the Antarctic Circumpolar Current. Open Access Geophysical Research Letters, 35 (20). L20606. DOI 10.1029/2008GL035382 <https://doi.org/10.1029/2008GL035382>. doi:10.1029/2008GL035382 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1029/2008GL035382 |
container_title |
Geophysical Research Letters |
container_volume |
35 |
container_issue |
20 |
_version_ |
1811632776354463744 |