A Global Climatology of Wind-Wave Interaction
Abstract Generally, ocean waves are thought to act as a drag on the surface wind so that momentum is transferred downward, from the atmosphere into the waves. Recent observations have suggested that when long wavelength waves—which are characteristic of remotely generated swell—propagate faster than...
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Published in | Journal of physical oceanography Vol. 40; no. 6; pp. 1263 - 1282 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Boston, MA
American Meteorological Society
01.06.2010
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Subjects | |
Online Access | Get full text |
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