Antarctic Circumpolar Current

E17552

The Antarctic Circumpolar Current is the powerful, continuous ocean current that flows eastward around Antarctica, connecting the Atlantic, Pacific, and Indian Oceans and playing a key role in global climate and ocean circulation.


Statements (47)
Predicate Object
instanceOf circumpolar current
ocean current
physical oceanographic feature
affectedBy Southern Annular Mode variability
climate change
alsoKnownAs ACC
West Wind Drift
associatedWith Antarctic Polar Front
Subantarctic Front
multiple oceanic fronts and jets
connects Atlantic Ocean
Indian Ocean
Pacific Ocean
contributesTo isolation of Antarctica from warmer subtropical waters
maintenance of Antarctic ice sheet by thermal isolation
drivenBy density gradients in the Southern Ocean
strong westerly winds
encircles Antarctica
flowsDirection eastward
hasApproximateLatitudeRange between about 40°S and 65°S
hasApproximateTransport 100 to 150 Sverdrups
about 100 million cubic meters per second or more
hasDepthExtent from surface to more than 3000 meters depth in places
hasHistoricalNameOrigin named for its circumpolar flow around Antarctica
hasKeyRegion Drake Passage
south of Africa
south of Australia
south of New Zealand
hasTypicalSurfaceSpeed up to several tens of centimeters per second
influences Antarctic climate
Southern Ocean ecosystems
global carbon cycle
interactsWith Antarctic Bottom Water formation
North Atlantic Deep Water inflow
isImportantFor global nutrient distribution
upwelling of deep waters in the Southern Ocean
isLargestCurrentBy volume transport
isOnlyCurrentThat flows completely around the globe without continental interruption
locatedIn Southern Ocean
monitoredBy Argo floats
satellite altimetry
ship-based hydrographic sections
playsRoleIn exchange of water masses between Atlantic, Pacific, and Indian Oceans
global climate regulation
global thermohaline circulation
heat redistribution between ocean basins
studiedInDiscipline physical oceanography


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