Physical oceanography in the Scotia Sea during the CCAMLR 2000 survey, austral summer 2000

In January and February 2000, four ships conducted an extensive hydrographic survey of the Scotia Sea as part of the CCAMLR 2000 Survey. There were 169 CTD stations to at least 1000 m depth, making this the largest synoptic dataset since 1981. A hydrographic section at Drake Passage was used to defi...

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Published in:Deep Sea Research Part II: Topical Studies in Oceanography
Main Authors: Brandon, M., Naganobu, M., Demer, D., Chernyshkov, P., Trathan, P., Thorpe, S., Kameda, T., Berezhinskiy, O., Hawker, E., Grant, S.
Format: Book
Language:English
Published: 2004
Subjects:
Online Access:http://hdl.handle.net/1834/17176
https://doi.org/10.1016/j.dsr2.2004.06.006
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spelling ftoceandocs:oai:aquadocs.org:1834/17176 2024-06-09T07:38:58+00:00 Physical oceanography in the Scotia Sea during the CCAMLR 2000 survey, austral summer 2000 Brandon, M. Naganobu, M. Demer, D. Chernyshkov, P. Trathan, P. Thorpe, S. Kameda, T. Berezhinskiy, O. Hawker, E. Grant, S. 2004 pp.1301-1321 http://hdl.handle.net/1834/17176 https://doi.org/10.1016/j.dsr2.2004.06.006 en eng https://doi.org/10.1016/j.dsr2.2004.06.006 http://hdl.handle.net/1834/17176 Journal Contribution Refereed 2004 ftoceandocs https://doi.org/10.1016/j.dsr2.2004.06.006 2024-05-15T08:02:16Z In January and February 2000, four ships conducted an extensive hydrographic survey of the Scotia Sea as part of the CCAMLR 2000 Survey. There were 169 CTD stations to at least 1000 m depth, making this the largest synoptic dataset since 1981. A hydrographic section at Drake Passage was used to define water masses and ocean fronts. In 2000, the Subantarctic Front and the Polar Front were unusually close, and the entire survey occurred to the south of the Polar Front. The survey area was bisected by the Subantarctic Circumpolar Current Front and the Southern Boundary of the Antarctic Circumpolar Current. In Drake Passage, these fronts were widely spaced. A further two hydrographic sections to the east of Drake Passage show that the relative location of these fronts changes east of Drake Passage. Horizontal maps across the survey area show that close to Drake Passage, properties are aligned in a southwest to northeast direction. At approximately 35°W, properties become orientated in a north–south direction. A map of geopotential anomaly shows the flow field across the survey area and allows identification of oceanic fronts. In months previous to the survey, the giant icebergs A22B and B10A crossed the Scotia Sea and closely followed the geopotential field from the CCAMLR 2000 dataset. The SACCF is not the only important front for transporting biological matter from the Antarctic Peninsula to South Georgia; an interaction between the SBACC and the SACCF is also likely to be important. Published Book Antarc* Antarctic Antarctic Peninsula Drake Passage Iceberg* Scotia Sea IODE-UNESCO: OceanDocs - E-Repository of Ocean Publications Antarctic Antarctic Peninsula Austral Drake Passage Scotia Sea The Antarctic Deep Sea Research Part II: Topical Studies in Oceanography 51 12-13 1301 1321
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language English
description In January and February 2000, four ships conducted an extensive hydrographic survey of the Scotia Sea as part of the CCAMLR 2000 Survey. There were 169 CTD stations to at least 1000 m depth, making this the largest synoptic dataset since 1981. A hydrographic section at Drake Passage was used to define water masses and ocean fronts. In 2000, the Subantarctic Front and the Polar Front were unusually close, and the entire survey occurred to the south of the Polar Front. The survey area was bisected by the Subantarctic Circumpolar Current Front and the Southern Boundary of the Antarctic Circumpolar Current. In Drake Passage, these fronts were widely spaced. A further two hydrographic sections to the east of Drake Passage show that the relative location of these fronts changes east of Drake Passage. Horizontal maps across the survey area show that close to Drake Passage, properties are aligned in a southwest to northeast direction. At approximately 35°W, properties become orientated in a north–south direction. A map of geopotential anomaly shows the flow field across the survey area and allows identification of oceanic fronts. In months previous to the survey, the giant icebergs A22B and B10A crossed the Scotia Sea and closely followed the geopotential field from the CCAMLR 2000 dataset. The SACCF is not the only important front for transporting biological matter from the Antarctic Peninsula to South Georgia; an interaction between the SBACC and the SACCF is also likely to be important. Published
format Book
author Brandon, M.
Naganobu, M.
Demer, D.
Chernyshkov, P.
Trathan, P.
Thorpe, S.
Kameda, T.
Berezhinskiy, O.
Hawker, E.
Grant, S.
spellingShingle Brandon, M.
Naganobu, M.
Demer, D.
Chernyshkov, P.
Trathan, P.
Thorpe, S.
Kameda, T.
Berezhinskiy, O.
Hawker, E.
Grant, S.
Physical oceanography in the Scotia Sea during the CCAMLR 2000 survey, austral summer 2000
author_facet Brandon, M.
Naganobu, M.
Demer, D.
Chernyshkov, P.
Trathan, P.
Thorpe, S.
Kameda, T.
Berezhinskiy, O.
Hawker, E.
Grant, S.
author_sort Brandon, M.
title Physical oceanography in the Scotia Sea during the CCAMLR 2000 survey, austral summer 2000
title_short Physical oceanography in the Scotia Sea during the CCAMLR 2000 survey, austral summer 2000
title_full Physical oceanography in the Scotia Sea during the CCAMLR 2000 survey, austral summer 2000
title_fullStr Physical oceanography in the Scotia Sea during the CCAMLR 2000 survey, austral summer 2000
title_full_unstemmed Physical oceanography in the Scotia Sea during the CCAMLR 2000 survey, austral summer 2000
title_sort physical oceanography in the scotia sea during the ccamlr 2000 survey, austral summer 2000
publishDate 2004
url http://hdl.handle.net/1834/17176
https://doi.org/10.1016/j.dsr2.2004.06.006
geographic Antarctic
Antarctic Peninsula
Austral
Drake Passage
Scotia Sea
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
Austral
Drake Passage
Scotia Sea
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Drake Passage
Iceberg*
Scotia Sea
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Drake Passage
Iceberg*
Scotia Sea
op_relation https://doi.org/10.1016/j.dsr2.2004.06.006
http://hdl.handle.net/1834/17176
op_doi https://doi.org/10.1016/j.dsr2.2004.06.006
container_title Deep Sea Research Part II: Topical Studies in Oceanography
container_volume 51
container_issue 12-13
container_start_page 1301
op_container_end_page 1321
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