Abstract
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reaches from the equator to about 50°S, and south of 40°S two cyclonic turns from the Circumpolar Current and Weddell Sea, west and east of the anticyclonic gyre. This figure has been changed very slightly between 40°S and 50°S from the figure shown in Reid (1994)...
Recommended Citation
Reid, Joseph L.. 2012. "Deep circulation within the Argentine Basin." Journal of Marine Research 70, (1). https://elischolar.library.yale.edu/journal_of_marine_research/338
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