The Antarctic Circumpolar Wave is a coupled ocean/atmospherewave that circles the Southern Ocean in approximately eight years. Since it is a wave-2 phenomenon (there are two peaks and two troughs in a latitude circle) at each fixed point in space a signal with a period of four years is seen. The wave moves eastward with the prevailing currents.
Note that although the "wave" is seen in temperature, atmospheric pressure, sea ice and ocean height, the variations are hard to see in the raw data and need to be filtered to become visible. It is not a wave you can surf! Because the reliable record for the Southern Ocean is short (since the early 1980s) and signal processing is needed to reveal its existence, some climatologists doubt the existence of the wave. Others admit its existence but say that it varies in strength over decades.
The wave was discovered simultaneously by Warren White and R G Peterson; and Jacobs and Mitchell; in 1996. Since then, ideas about the wave structure and maintenance mechanisms have changed and grown: by some accounts it is now to be considered as part of a global ENSO wave.
White, W.B. and R.G. Peterson, 1996. An Antarctic circumpolar wave in surface pressure, temperature and sea-ice extent. Nature 380, 699-702.
Jacobs, G. A., and J. L. Mitchell, Ocean circulation variations associated with the Antarctic Circumpolar Wave. Geophys. Res. Let., Vol. 23, No. 21, pp. 2947-2950, 1996 [1] (http://www.pol.ac.uk/psmsl/gb/gb3/jacobs.html)
Connolley, W. M., 2002. Long-term variation of the Antarctic Circumpolar Wave, JGR. doi:10.1029/2000JC000380.
The AntarcticCircumpolarWave is a coupled ocean/atmosphere wave that circles the Southern Ocean in approximately eight years.
Note that although the "wave" is seen in temperature, atmospheric pressure, sea ice and ocean height, the variations are hard to see in the raw data and need to be filtered to become apparent.
The wave was discovered simultaneously by Warren White and R G Peterson; and Jacobs and Mitchell; in 1996.
The AntarcticCircumpolar Current (ACC) is an ocean current that flows from west to east around Antarctica.
There is general agreement that the large transport of the Circumpolar Current is linked to the strong westerly winds which are found in the Southern Ocean and that these winds blow over a band of open latitudes.
Evidence of this is the AntarcticCircumpolarWave, a periodic oscillation that affects the climate of much of the southern hemisphere.
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