Abstract
Wind energy input into the ocean is primarily produced through surface waves. The total rate of this energy source, integrated over the World Ocean, is estimated at 60 TW, based on empirical formulas and results from a numerical model of surface waves. Thus, surface wave energy input is about 50 times the energy input to the surface geostrophic current and 20 times the total tidal dissipation rate. Most of the energy input is concentrated within the Antarctic Circumpolar Current. © 2004 American Meteorological Society.
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CITATION STYLE
Wang, W., & Huang, R. X. (2004). Wind energy input to the surface waves. Journal of Physical Oceanography, 34(5), 1276–1280. https://doi.org/10.1175/1520-0485(2004)034<1276:WEITTS>2.0.CO;2
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