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contributor authorLin, Ray Q.
contributor authorPerrie, Will
date accessioned2017-06-09T14:52:41Z
date available2017-06-09T14:52:41Z
date copyright1997/09/01
date issued1997
identifier issn0022-3670
identifier otherams-28755.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165906
description abstractResonant wave?wave interaction processes are studied with the nonlinear dispersion relationship for shallow water. The formulation was derived based on a Hamiltonian representation first reported by Zakharov. Results show that four waves are needed for resonant interactions at all depths. Furthermore, when the nonlinear dispersion relationship for waves in intermediate water is considered, two interaction modes can result depending on the water depth and the nonlinearity: (i) in deep water the classic Phillips interactions dominate, involving four waves of comparable wavelengths, whereas (ii) in shallow water the dominant interactions still consist of four waves, but with one component of vanishingly small wavenumber. As an approximate asymptotic limit, the latter become triadic shoaling wave interactions.
publisherAmerican Meteorological Society
titleA New Coastal Wave Model. Part III: Nonlinear Wave–Wave Interaction
typeJournal Paper
journal volume27
journal issue9
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1997)027<1813:ANCWMP>2.0.CO;2
journal fristpage1813
journal lastpage1826
treeJournal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 009
contenttypeFulltext


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