Transport and variability of the Antarctic Circumpolar Current in Drake Passage

1] The baroclinic transport of the Antarctic Circumpolar Current (ACC) above 3000 m through Drake Passage is 107.3 ± 10.4 Sv and has been steady between 1975 and 2000. For six hydrographic sections (1993–2000) along the World Ocean Circulation Experiment (WOCE) line SR1b, the baroclinic transport re...

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Published in:Journal of Geophysical Research
Main Authors: Cunningham, S., Alderson, S., King, B., Brandon, M.
Format: Book
Language:English
Published: 2003
Subjects:
Online Access:http://hdl.handle.net/1834/17234
https://doi.org/10.1029/2001JC001147
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spelling ftoceandocs:oai:aquadocs.org:1834/17234 2024-06-09T07:40:06+00:00 Transport and variability of the Antarctic Circumpolar Current in Drake Passage Cunningham, S. Alderson, S. King, B. Brandon, M. 2003 pp.80-84 http://hdl.handle.net/1834/17234 https://doi.org/10.1029/2001JC001147 en eng https://doi.org/10.1029/2001JC001147 http://hdl.handle.net/1834/17234 Journal Contribution Refereed 2003 ftoceandocs https://doi.org/10.1029/2001JC001147 2024-05-15T08:02:16Z 1] The baroclinic transport of the Antarctic Circumpolar Current (ACC) above 3000 m through Drake Passage is 107.3 ± 10.4 Sv and has been steady between 1975 and 2000. For six hydrographic sections (1993–2000) along the World Ocean Circulation Experiment (WOCE) line SR1b, the baroclinic transport relative to the deepest common level is 136.7 ± 7.8 Sv. The ACC transport is carried in two jets, the Subantarctic Front 53 ± 10 Sv and the Polar Front (PF) 57.5 ± 5.7 Sv. Southward of the ACC the Southern Antarctic Circumpolar Current transports 9.3 ± 2.4 Sv. We observe the PF at two latitudes separated by 90 km. This bimodal distribution is related to changes in the circulation and properties of Antarctic Bottom Water. Three realizations of the instantaneous velocity field were obtained with lowered ADCPs. From these observations we obtain near‐bottom reference velocities for transport calculations. Net transport due to these reference velocities ranges from −28 to 43 Sv, consistent with previous estimates of variability. The transport in density layers shows systematic variations due to seasonal heating in near‐surface layers. Volume transport‐weighted mean temperatures vary by 0.40°C from spring to summer; a seasonal variation in heat flux of about 0.22 PW. Finally, we review a series of papers from the International Southern Ocean Studies Program. The average yearlong absolute transport is 134 Sv, and the standard deviation of the average is 11.2 Sv; the error of the average transport is 15 to 27 Sv. We emphasize that baroclinic variability is an important contribution to net variability in the ACC. Published Book Antarc* Antarctic Drake Passage Southern Ocean IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications Antarctic Drake Passage Southern Ocean The Antarctic Journal of Geophysical Research 108 C5
institution Open Polar
collection IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications
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language English
description 1] The baroclinic transport of the Antarctic Circumpolar Current (ACC) above 3000 m through Drake Passage is 107.3 ± 10.4 Sv and has been steady between 1975 and 2000. For six hydrographic sections (1993–2000) along the World Ocean Circulation Experiment (WOCE) line SR1b, the baroclinic transport relative to the deepest common level is 136.7 ± 7.8 Sv. The ACC transport is carried in two jets, the Subantarctic Front 53 ± 10 Sv and the Polar Front (PF) 57.5 ± 5.7 Sv. Southward of the ACC the Southern Antarctic Circumpolar Current transports 9.3 ± 2.4 Sv. We observe the PF at two latitudes separated by 90 km. This bimodal distribution is related to changes in the circulation and properties of Antarctic Bottom Water. Three realizations of the instantaneous velocity field were obtained with lowered ADCPs. From these observations we obtain near‐bottom reference velocities for transport calculations. Net transport due to these reference velocities ranges from −28 to 43 Sv, consistent with previous estimates of variability. The transport in density layers shows systematic variations due to seasonal heating in near‐surface layers. Volume transport‐weighted mean temperatures vary by 0.40°C from spring to summer; a seasonal variation in heat flux of about 0.22 PW. Finally, we review a series of papers from the International Southern Ocean Studies Program. The average yearlong absolute transport is 134 Sv, and the standard deviation of the average is 11.2 Sv; the error of the average transport is 15 to 27 Sv. We emphasize that baroclinic variability is an important contribution to net variability in the ACC. Published
format Book
author Cunningham, S.
Alderson, S.
King, B.
Brandon, M.
spellingShingle Cunningham, S.
Alderson, S.
King, B.
Brandon, M.
Transport and variability of the Antarctic Circumpolar Current in Drake Passage
author_facet Cunningham, S.
Alderson, S.
King, B.
Brandon, M.
author_sort Cunningham, S.
title Transport and variability of the Antarctic Circumpolar Current in Drake Passage
title_short Transport and variability of the Antarctic Circumpolar Current in Drake Passage
title_full Transport and variability of the Antarctic Circumpolar Current in Drake Passage
title_fullStr Transport and variability of the Antarctic Circumpolar Current in Drake Passage
title_full_unstemmed Transport and variability of the Antarctic Circumpolar Current in Drake Passage
title_sort transport and variability of the antarctic circumpolar current in drake passage
publishDate 2003
url http://hdl.handle.net/1834/17234
https://doi.org/10.1029/2001JC001147
geographic Antarctic
Drake Passage
Southern Ocean
The Antarctic
geographic_facet Antarctic
Drake Passage
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Drake Passage
Southern Ocean
genre_facet Antarc*
Antarctic
Drake Passage
Southern Ocean
op_relation https://doi.org/10.1029/2001JC001147
http://hdl.handle.net/1834/17234
op_doi https://doi.org/10.1029/2001JC001147
container_title Journal of Geophysical Research
container_volume 108
container_issue C5
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