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Read Full Article (file size: 1087597 bytes) Cited by
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 113,
C10002,
doi:10.1029/2007JC004579,
2008
Stokes drift–induced and direct wind energy inputs into the Ekman layer within the Antarctic Circumpolar Current
Kejian Wu
Physical Oceanography Laboratory, Ocean University of China, Qingdao, China
Bin Liu
Physical Oceanography Laboratory, Ocean University of China, Qingdao, China
Abstract
Theoretical analysis of energetics of the Ekman layer by incorporating the Coriolis-Stokes forcing into the classical Ekman
model shows that the wind energy input to the Ekman layer has two components: the work done by the wind stress on the surface
Ekman current and that done by the Coriolis-Stokes forcing on the whole body of water in the mixed layer. Under the assumption
of constant vertical diffusivity, analytical forms of the direct wind energy input and the Stokes drift–induced energy input
are derived. Assessments of relative importance of surface waves are made by comparing the wind energy input into the Ekman
layer with and without wave-induced Stokes drift effects included. Using the European Centre for Medium-Range Weather Forecasts
40-year reanalysis wind stress and surface wave data sets, the total rate of wind energy input into the Ekman layer within
the Antarctic Circumpolar Current (ACC) is estimated to be 833 GW, in which the direct wind energy input is 650 GW (78%),
and the Stokes drift–induced energy input is 183 GW (22%). The total mechanical energy input into the ACC due to wave effects
is increased by approximately 4% (30 GW) compared to that into the classical Ekman layer. Long-term variability of direct
wind and Stokes drift–induced energy inputs to the ACC is also examined.
Received 6
October
2007;
accepted 17
July
2008;
published 4
October
2008.
Keywords: wind energy input;
Ekman-Stokes layer;
Antarctic Circumpolar Current.
Index Terms: 4532 Oceanography: Physical: General circulation (1218, 1222); 4207 Oceanography: General: Arctic and Antarctic oceanography (9310, 9315); 4560 Oceanography: Physical: Surface waves and tides (1222).
Read Full Article (file size: 1087597 bytes) Cited by
Citation: Wu, K., and B. Liu
(2008),
Stokes drift–induced and direct wind energy inputs into the Ekman layer within the Antarctic Circumpolar Current,
J. Geophys. Res.,
113,
C10002,
doi:10.1029/2007JC004579.
Copyright 2008 by the American Geophysical Union.
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