Derivation of Stokes drift for a deep-water random gravity wave field

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Abstract

A new method was used to derive the Stokes drift. Full non-linear terms were included in the equations which were transformed into integral equations by Fourier-Stieltjes representations. Solution was obtained by the method of successive approximations. To the second order, the result was similar to that of Kenyon (1969).

Original languageEnglish
Pages (from-to)255-259
Number of pages5
JournalDeep-Sea Research and Oceanographic Abstracts
Volume18
Issue number2
DOIs
StatePublished - Feb 1971

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