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    A New Coastal Wave Model. Part V: Five-Wave Interactions

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 010::page 2169
    Author:
    Lin, Ray Q.
    ,
    Perrie, Will
    DOI: 10.1175/1520-0485(1997)027<2169:ANCWMP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The 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.
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      A New Coastal Wave Model. Part V: Five-Wave Interactions

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4165931
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    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
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian