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    Internal Waves at an Interface between Two Layers of Differing Stability

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 006::page 1845
    Author:
    McHugh, John
    DOI: 10.1175/2008JAS2881.1
    Publisher: American Meteorological Society
    Abstract: Internal waves in a two-layer fluid are considered. The layers have different values of the buoyancy frequency, assumed to be constant in each layer. The density profile is chosen to be continuous across the interface and the flow is Boussinesq. The solution is an expansion in the wave amplitude, similar to a Stokes expansion for free surface waves. The results show that the nonlinear terms in the interfacial boundary conditions require higher harmonics and result in nonlinear wave steepening at the interface. The first few harmonics are scattered by the interface, whereas the higher harmonics are evanescent in the vertical. The second-order correction to the wave speed is negative, similar to previous results with a rigid upper boundary.
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      Internal Waves at an Interface between Two Layers of Differing Stability

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    contributor authorMcHugh, John
    date accessioned2017-06-09T16:23:08Z
    date available2017-06-09T16:23:08Z
    date copyright2009/06/01
    date issued2009
    identifier issn0022-4928
    identifier otherams-66921.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208310
    description abstractInternal waves in a two-layer fluid are considered. The layers have different values of the buoyancy frequency, assumed to be constant in each layer. The density profile is chosen to be continuous across the interface and the flow is Boussinesq. The solution is an expansion in the wave amplitude, similar to a Stokes expansion for free surface waves. The results show that the nonlinear terms in the interfacial boundary conditions require higher harmonics and result in nonlinear wave steepening at the interface. The first few harmonics are scattered by the interface, whereas the higher harmonics are evanescent in the vertical. The second-order correction to the wave speed is negative, similar to previous results with a rigid upper boundary.
    publisherAmerican Meteorological Society
    titleInternal Waves at an Interface between Two Layers of Differing Stability
    typeJournal Paper
    journal volume66
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2008JAS2881.1
    journal fristpage1845
    journal lastpage1855
    treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;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
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