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    Oscillatory Bottom Boundary Layers

    Source: Journal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 011::page 3075
    Author:
    Mellor, George
    DOI: 10.1175/1520-0485(2002)032<3075:OBBL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A turbulence closure model is applied to the case of an oscillating boundary layer; model calculations compare favorably with data. Wave-induced oscillations can be temporally resolved in a one-dimensional model but not in three-dimensional ocean models, and, indeed, statistical wave models, working in consort with ocean models, can only provide information on expected wave periods and amplitudes. Therefore, in this paper, a way has been found to parameterize the effects of bottom flow oscillations; it entails augmenting the turbulence shear production as a function of amplitude and period of the oscillation, the bottom shear stress of the mean current flow, and the angle between the directions of the oscillations and the mean flow. The more conventional method of solving for an apparent wall roughness is also investigated in an appendix.
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      Oscillatory Bottom Boundary Layers

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    contributor authorMellor, George
    date accessioned2017-06-09T14:55:30Z
    date available2017-06-09T14:55:30Z
    date copyright2002/11/01
    date issued2002
    identifier issn0022-3670
    identifier otherams-29774.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4167038
    description abstractA turbulence closure model is applied to the case of an oscillating boundary layer; model calculations compare favorably with data. Wave-induced oscillations can be temporally resolved in a one-dimensional model but not in three-dimensional ocean models, and, indeed, statistical wave models, working in consort with ocean models, can only provide information on expected wave periods and amplitudes. Therefore, in this paper, a way has been found to parameterize the effects of bottom flow oscillations; it entails augmenting the turbulence shear production as a function of amplitude and period of the oscillation, the bottom shear stress of the mean current flow, and the angle between the directions of the oscillations and the mean flow. The more conventional method of solving for an apparent wall roughness is also investigated in an appendix.
    publisherAmerican Meteorological Society
    titleOscillatory Bottom Boundary Layers
    typeJournal Paper
    journal volume32
    journal issue11
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(2002)032<3075:OBBL>2.0.CO;2
    journal fristpage3075
    journal lastpage3088
    treeJournal of Physical Oceanography:;2002:;Volume( 032 ):;issue: 011
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
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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