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    LONG WAVES IN A TWO-FLUID SYSTEM

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 001::page 70
    Author:
    Long, Robert R.
    DOI: 10.1175/1520-0469(1956)013<0070:LWIATF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The differential equations governing the unsteady motion of a system of two superimposed liquids are integrated by use of the method of characteristics. The solution differs significantly from that obtained by assuming a very thin lower layer. If the basic shear across the interface is small, a wave breaks forward (as an ordinary water wave) only if the amplitude is fairly small and if the lower layer is thinner than the upper layer. If the upper fluid is thinner, the wave breaks backward. The speed of the various points of the wave does not vary monotonically with amplitude. If a shear exists, higher velocities in the upper layer in the direction of wave propagation favor the forward breaking of a wave. The opposite shear may cause a wave to break backward.
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      LONG WAVES IN A TWO-FLUID SYSTEM

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    contributor authorLong, Robert R.
    date accessioned2017-06-09T14:11:22Z
    date available2017-06-09T14:11:22Z
    date copyright1956/02/01
    date issued1956
    identifier issn0095-9634
    identifier otherams-14229.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149767
    description abstractThe differential equations governing the unsteady motion of a system of two superimposed liquids are integrated by use of the method of characteristics. The solution differs significantly from that obtained by assuming a very thin lower layer. If the basic shear across the interface is small, a wave breaks forward (as an ordinary water wave) only if the amplitude is fairly small and if the lower layer is thinner than the upper layer. If the upper fluid is thinner, the wave breaks backward. The speed of the various points of the wave does not vary monotonically with amplitude. If a shear exists, higher velocities in the upper layer in the direction of wave propagation favor the forward breaking of a wave. The opposite shear may cause a wave to break backward.
    publisherAmerican Meteorological Society
    titleLONG WAVES IN A TWO-FLUID SYSTEM
    typeJournal Paper
    journal volume13
    journal issue1
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1956)013<0070:LWIATF>2.0.CO;2
    journal fristpage70
    journal lastpage74
    treeJournal of Meteorology:;1956:;volume( 013 ):;issue: 001
    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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