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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Published in:Science
Main Authors: Fu, Lee-Lueng, Chelton, Dudley B.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1984
Subjects:
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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spelling 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
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