A deep cyclonic gyre in the Australian-Antarctic Basin
The traditional image of ocean circulation between Australia and Antarctica is of a dominant belt of eastward flow, the Antarctic Circumpolar Current, with comparatively weak adjacent westward flows that provide anticyclonic circulation north and cyclonic circulation south of the Antarctic Circumpol...
Published in: | Progress in Oceanography |
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Main Authors: | , |
Format: | Text |
Language: | unknown |
Published: |
DigitalCommons@URI
2007
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Subjects: | |
Online Access: | https://digitalcommons.uri.edu/gsofacpubs/1225 https://doi.org/10.1016/j.pocean.2007.02.008 |