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    The Structure, Energetics and Propagation of Rotating Convective Storms. Part I: Energy Exchange with the Mean Flow

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 002::page 113
    Author:
    Lilly, Douglas K.
    DOI: 10.1175/1520-0469(1986)043<0113:TSEAPO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A three-dimensional buoyant convective element responds to the existence of mean vertical shear by developing rotation about a vertical axis, with the rotational kinetic energy abstracted from that of the mean flow. This process is illustrated with the aid of linear analysis. From consideration of nonlinear processes it is concluded that a portion of the rotational energy is transformed into that of the overturning velocity field, thus enhancing further buoyant energy release. The storm structure which is optimal for energy transfer from the mean flow to rotational disturbances is a single updraft propagating with the mean flow and with counter-rotating vortices on both sides. The transfer of energy from rotational to overturning modes is, however, optimized by laterally propagating updrafts with coincident vortices.
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      The Structure, Energetics and Propagation of Rotating Convective Storms. Part I: Energy Exchange with the Mean Flow

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4155304
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    contributor authorLilly, Douglas K.
    date accessioned2017-06-09T14:26:10Z
    date available2017-06-09T14:26:10Z
    date copyright1986/01/01
    date issued1986
    identifier issn0022-4928
    identifier otherams-19212.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155304
    description abstractA three-dimensional buoyant convective element responds to the existence of mean vertical shear by developing rotation about a vertical axis, with the rotational kinetic energy abstracted from that of the mean flow. This process is illustrated with the aid of linear analysis. From consideration of nonlinear processes it is concluded that a portion of the rotational energy is transformed into that of the overturning velocity field, thus enhancing further buoyant energy release. The storm structure which is optimal for energy transfer from the mean flow to rotational disturbances is a single updraft propagating with the mean flow and with counter-rotating vortices on both sides. The transfer of energy from rotational to overturning modes is, however, optimized by laterally propagating updrafts with coincident vortices.
    publisherAmerican Meteorological Society
    titleThe Structure, Energetics and Propagation of Rotating Convective Storms. Part I: Energy Exchange with the Mean Flow
    typeJournal Paper
    journal volume43
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1986)043<0113:TSEAPO>2.0.CO;2
    journal fristpage113
    journal lastpage125
    treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 002
    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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