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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Bibliographic Details
Published inJournal of physical oceanography Vol. 40; no. 6; pp. 1263 - 1282
Main Authors HANLEY, Kirsty E, BELCHER, Stephen E, SULLIVAN, Peter P
Format Journal Article
LanguageEnglish
Published Boston, MA American Meteorological Society 01.06.2010
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