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Antarctic Circumpolar Current

File:Antarctic_Circumpolar_Current.png · Wikimedia Commons · See Wikimedia Commons

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Antarctic Circumpolar Current

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Also known as ACC

ocean current that flows clockwise from west to east around Antarctica

~13 min read

Encyclopedic overview

Antarctic Circumpolar Current, showing branches connecting to the larger thermohaline circulation Animation of the thermohaline circulation. The later part of this animation shows the Antarctic Circumpolar Current.

The Antarctic Circumpolar Current (ACC) is an ocean current that flows clockwise (as seen from the South Pole) from west to east around Antarctica. An alternative name for the ACC is the West Wind Drift. The ACC is the dominant circulation feature of the Southern Ocean and has a mean transport estimated at 137 ± 7 sverdrups (Sv, million m/s), or possibly even higher, making it the largest ocean current. The current is circumpolar due to the lack of any landmass connecting with Antarctica and this keeps warm ocean waters away from Antarctica, enabling that continent to maintain its huge ice sheet.

Excerpted from Wikipedia’s “Antarctic Circumpolar Current” article, available under the CC BY-SA 4.0 licence.

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