Antarctic Circumpolar Wave

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Oceans and seas (main)


March 29, 2010, 12:00 am
November 9, 2011, 9:07 am

The term Antarctic Circumpolar Wave (ACW) describes interannual variations in the following parameters: atmospheric pressure at sea level, wind stress, sea surface temperature and sea–ice extent that propagate eastwards around the Southern Ocean. These anomalies propagate with the circumpolar flow with a time period of four to five years and taking eight to ten years to circle the pole.

This article is written at a definitional level only. Authors wishing to expand this entry are inivited to expand the present treatment, which additions will be peer reviewed prior to publication of any expansion.

See Also

Further Reading

  • Physical Oceanography Index
  • W. B. White and R. Peterson. An Antarctic Circumpolar Wave in surface pressure, wind, temperature, and sea ice extent. Nature, 380:699–702, 1996.
  • Antarctic Circumpolar Wave, E. Linacre, (accessed March 8, 2010)

Citation

Baum, S. (2011). Antarctic Circumpolar Wave. Retrieved from http://editors.eol.org/eoearth/wiki/Antarctic_Circumpolar_Wave