Temporal Variability of the Antarctic Circumpolar Current Observed from Satellite Altimetry
Sea level measurements by the Seasat altimeter were used to study the temporal variability of the Antarctic Circumpolar Current between July and October 1978. Large-scale zonal coherence in the cross-stream sea level difference was observed, indicating a general increase in the surface geostrophic v...
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American Association for the Advancement of Science (AAAS)
1984
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Online Access: | http://dx.doi.org/10.1126/science.226.4672.343 https://www.science.org/doi/pdf/10.1126/science.226.4672.343 |
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craaas:10.1126/science.226.4672.343 2024-06-23T07:46:55+00:00 Temporal Variability of the Antarctic Circumpolar Current Observed from Satellite Altimetry Fu, Lee-Lueng Chelton, Dudley B. 1984 http://dx.doi.org/10.1126/science.226.4672.343 https://www.science.org/doi/pdf/10.1126/science.226.4672.343 en eng American Association for the Advancement of Science (AAAS) Science volume 226, issue 4672, page 343-346 ISSN 0036-8075 1095-9203 journal-article 1984 craaas https://doi.org/10.1126/science.226.4672.343 2024-06-13T04:00:57Z Sea level measurements by the Seasat altimeter were used to study the temporal variability of the Antarctic Circumpolar Current between July and October 1978. Large-scale zonal coherence in the cross-stream sea level difference was observed, indicating a general increase in the surface geostrophic velocity of the current around the Southern Ocean. The result demonstrates the power of satellite altimetry to monitor the variability of large-scale ocean currents. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean AAAS Resource Center (American Association for the Advancement of Science) Antarctic Southern Ocean The Antarctic Science 226 4672 343 346 |
institution |
Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
Sea level measurements by the Seasat altimeter were used to study the temporal variability of the Antarctic Circumpolar Current between July and October 1978. Large-scale zonal coherence in the cross-stream sea level difference was observed, indicating a general increase in the surface geostrophic velocity of the current around the Southern Ocean. The result demonstrates the power of satellite altimetry to monitor the variability of large-scale ocean currents. |
format |
Article in Journal/Newspaper |
author |
Fu, Lee-Lueng Chelton, Dudley B. |
spellingShingle |
Fu, Lee-Lueng Chelton, Dudley B. Temporal Variability of the Antarctic Circumpolar Current Observed from Satellite Altimetry |
author_facet |
Fu, Lee-Lueng Chelton, Dudley B. |
author_sort |
Fu, Lee-Lueng |
title |
Temporal Variability of the Antarctic Circumpolar Current Observed from Satellite Altimetry |
title_short |
Temporal Variability of the Antarctic Circumpolar Current Observed from Satellite Altimetry |
title_full |
Temporal Variability of the Antarctic Circumpolar Current Observed from Satellite Altimetry |
title_fullStr |
Temporal Variability of the Antarctic Circumpolar Current Observed from Satellite Altimetry |
title_full_unstemmed |
Temporal Variability of the Antarctic Circumpolar Current Observed from Satellite Altimetry |
title_sort |
temporal variability of the antarctic circumpolar current observed from satellite altimetry |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1984 |
url |
http://dx.doi.org/10.1126/science.226.4672.343 https://www.science.org/doi/pdf/10.1126/science.226.4672.343 |
geographic |
Antarctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_source |
Science volume 226, issue 4672, page 343-346 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.226.4672.343 |
container_title |
Science |
container_volume |
226 |
container_issue |
4672 |
container_start_page |
343 |
op_container_end_page |
346 |
_version_ |
1802649354570301440 |