Show simple item record

contributor authorLin, Ray Q.
contributor authorPerrie, Will
date accessioned2017-06-09T14:52:44Z
date available2017-06-09T14:52:44Z
date copyright1997/10/01
date issued1997
identifier issn0022-3670
identifier otherams-28778.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165931
description abstractThe authors study the action flux associated with three-dimensional wave?wave interactions of ocean surface waves. Over deep water, two-dimensional wave?wave interactions are dominant: the three-dimensional five-wave interactions are two orders of magnitude smaller than the two-dimensional four-wave interactions. However, the five-wave interactions become increasingly important as the water depth decreases. Because of the effects of finite depth, three-dimensional five-wave interactions, involving steep finite-amplitude waves, dominate over two-dimensional four-wave interactions. Specifically, when the water depth h is less than 10 m, or nondimensionalizing with the spectral peak wavenumber Kp when Kph ≤ 3.6 and nonlinearity, ? = Ka(3 + tanh2Kh)/4 tanh3Kh ≥ 0.3, the five-wave interactions completely dominate. Results are consistent with the instability study by McLean.
publisherAmerican Meteorological Society
titleA New Coastal Wave Model. Part V: Five-Wave Interactions
typeJournal Paper
journal volume27
journal issue10
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1997)027<2169:ANCWMP>2.0.CO;2
journal fristpage2169
journal lastpage2186
treeJournal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 010
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record