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    Unexpected Waves

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 010::page 2330
    Author:
    Gemmrich, Johannes
    ,
    Garrett, Chris
    DOI: 10.1175/2008JPO3960.1
    Publisher: American Meteorological Society
    Abstract: Extreme, or ?rogue,? waves are those in the tail of the probability distribution and are a matter of great concern and considerable research. They may be partly associated with non-Gaussian behavior caused by resonant nonlinear interactions. Here it is shown that even in a Gaussian sea, ?unexpected? waves, in the sense of, for example, waves twice as large as any in the preceding 30 periods, occur with sufficient frequency to be of interest and importance. The return period of unexpected waves is quantified as a function of the height multiplier and prior quiescent interval for various spectral shapes, and it is shown how the return period is modified if allowance is made for nonlinear changes in wave shape and/or a buildup of one or more waves prior to the unexpected wave. The return period of ?two-sided? unexpected waves, with subsequent as well as prior quiescence, is also evaluated.
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      Unexpected Waves

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    contributor authorGemmrich, Johannes
    contributor authorGarrett, Chris
    date accessioned2017-06-09T16:25:17Z
    date available2017-06-09T16:25:17Z
    date copyright2008/10/01
    date issued2008
    identifier issn0022-3670
    identifier otherams-67550.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209009
    description abstractExtreme, or ?rogue,? waves are those in the tail of the probability distribution and are a matter of great concern and considerable research. They may be partly associated with non-Gaussian behavior caused by resonant nonlinear interactions. Here it is shown that even in a Gaussian sea, ?unexpected? waves, in the sense of, for example, waves twice as large as any in the preceding 30 periods, occur with sufficient frequency to be of interest and importance. The return period of unexpected waves is quantified as a function of the height multiplier and prior quiescent interval for various spectral shapes, and it is shown how the return period is modified if allowance is made for nonlinear changes in wave shape and/or a buildup of one or more waves prior to the unexpected wave. The return period of ?two-sided? unexpected waves, with subsequent as well as prior quiescence, is also evaluated.
    publisherAmerican Meteorological Society
    titleUnexpected Waves
    typeJournal Paper
    journal volume38
    journal issue10
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/2008JPO3960.1
    journal fristpage2330
    journal lastpage2336
    treeJournal of Physical Oceanography:;2008:;Volume( 038 ):;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
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