section_path: Physical oceanography/Antarctic Circumpolar Current and Antarctic Convergence
section_name: Antarctic Circumpolar Current and Antarctic Convergence
paragraph_text: Antarctic Circumpolar Current and Antarctic Convergence
  
  While the Southern is the second smallest ocean it contains the unique and highly energetic Antarctic Circumpolar Current which moves perpetually eastward – chasing and joining itself, and at 21,000 km (13,000 mi) in length – it comprises the world's longest ocean current, transporting 130 million cubic metres per second (4.6 × 10 cu ft/s) of water – 100 times the flow of all the world's rivers.
  
  Several processes operate along the coast of Antarctica to produce, in the Southern Ocean, types of water masses not produced elsewhere in the oceans of the Southern Hemisphere. One of these is the Antarctic Bottom Water, a very cold, highly saline, dense water that forms under sea ice. Another is Circumpolar Deep Water, a mixture of Antarctic Bottom Water and North Atlantic Deep Water.
  
  Associated with the Circumpolar Current is the Antarctic Convergence encircling Antarctica, where cold northward-flowing Antarctic waters meet the relatively warmer waters of the subantarctic, Antarctic waters predominantly sink beneath subantarctic waters, while associated zones of mixing and upwelling create a zone very high in nutrients. These nurture high levels of phytoplankton with associated copepods and Antarctic krill, and resultant foodchains supporting fish, whales, seals, penguins, albatrosses and a wealth of other species.
  
  The Antarctic Convergence is considered to be the best natural definition of the northern extent of the Southern Ocean.