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    Comments on “The Three-Dimensional Current and Surface Wave Equations”

    Source: Journal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 006::page 1340
    Author:
    Ardhuin, Fabrice
    ,
    Jenkins, Alastair D.
    ,
    Belibassakis, Konstadinos A.
    DOI: 10.1175/2007JPO3670.1
    Publisher: American Meteorological Society
    Abstract: The lowest order sigma-transformed momentum equation given by Mellor takes into account a phase-averaged wave forcing based on Airy wave theory. This equation is shown to be generally inconsistent because of inadequate approximations of the wave motion. Indeed the evaluation of the vertical flux of momentum requires an estimation of the pressure p and coordinate transformation function s to first order in parameters that define the large-scale evolution of the wave field, such as the bottom slope. Unfortunately, there is no analytical expression for p and s at that order. A numerical correction method is thus proposed and verified. Alternative coordinate transforms that allow a separation of wave and mean flow momenta do not suffer from this inconsistency nor do they require a numerical estimation of the wave forcing. Indeed, the problematic vertical flux is part of the wave momentum flux, thus distinct from the mean flow momentum flux, and not directly relevant to the mean flow evolution.
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      Comments on “The Three-Dimensional Current and Surface Wave Equations”

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    contributor authorArdhuin, Fabrice
    contributor authorJenkins, Alastair D.
    contributor authorBelibassakis, Konstadinos A.
    date accessioned2017-06-09T16:20:11Z
    date available2017-06-09T16:20:11Z
    date copyright2008/06/01
    date issued2008
    identifier issn0022-3670
    identifier otherams-65985.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4207270
    description abstractThe lowest order sigma-transformed momentum equation given by Mellor takes into account a phase-averaged wave forcing based on Airy wave theory. This equation is shown to be generally inconsistent because of inadequate approximations of the wave motion. Indeed the evaluation of the vertical flux of momentum requires an estimation of the pressure p and coordinate transformation function s to first order in parameters that define the large-scale evolution of the wave field, such as the bottom slope. Unfortunately, there is no analytical expression for p and s at that order. A numerical correction method is thus proposed and verified. Alternative coordinate transforms that allow a separation of wave and mean flow momenta do not suffer from this inconsistency nor do they require a numerical estimation of the wave forcing. Indeed, the problematic vertical flux is part of the wave momentum flux, thus distinct from the mean flow momentum flux, and not directly relevant to the mean flow evolution.
    publisherAmerican Meteorological Society
    titleComments on “The Three-Dimensional Current and Surface Wave Equations”
    typeJournal Paper
    journal volume38
    journal issue6
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/2007JPO3670.1
    journal fristpage1340
    journal lastpage1350
    treeJournal of Physical Oceanography:;2008:;Volume( 038 ):;issue: 006
    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