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    Hydrodynamic Instability of Small Eddies in a Tornado Vortex

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 003::page 422
    Author:
    Staley, D. O.
    ,
    Gall, R. L.
    DOI: 10.1175/1520-0469(1984)041<0422:HIOSEI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A numerical method is shown for solving problems of nonaxisymmetric perturbations in incompressible, inviscid, swirling flow for arbitrary undisturbed azimuthal and axial flows. Exclusive attention is given to the hydrodynamic stability at large azimuthal and axial wavenumbers for a flow with a zone of constant and coinciding vertical and azimuthal vorticities. An infinite sequence of unstable modes is found having very large amplitude within the verticity zone. Analysis of a 3-level model confirms the instability in the 46-level numerical model and shows the instability criterion to be kr?z + n?? < 0, where k (>0) and n (≥0) are axial and azimuthal wavenumbers, respectively, ?z (>0) and ?? (≥0) are the corresponding vorticities, and r is radius. Maximum instability occurs approximately where k and n are related by 2kr?z + n?? = 0, provided ?? is small compared to ?z. Growth rates, for a tornado vortex of typical dimensions and vorticities, are significant fractions of a second.
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      Hydrodynamic Instability of Small Eddies in a Tornado Vortex

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4154777
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    • Journal of the Atmospheric Sciences

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    contributor authorStaley, D. O.
    contributor authorGall, R. L.
    date accessioned2017-06-09T14:24:30Z
    date available2017-06-09T14:24:30Z
    date copyright1984/02/01
    date issued1984
    identifier issn0022-4928
    identifier otherams-18739.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154777
    description abstractA numerical method is shown for solving problems of nonaxisymmetric perturbations in incompressible, inviscid, swirling flow for arbitrary undisturbed azimuthal and axial flows. Exclusive attention is given to the hydrodynamic stability at large azimuthal and axial wavenumbers for a flow with a zone of constant and coinciding vertical and azimuthal vorticities. An infinite sequence of unstable modes is found having very large amplitude within the verticity zone. Analysis of a 3-level model confirms the instability in the 46-level numerical model and shows the instability criterion to be kr?z + n?? < 0, where k (>0) and n (≥0) are axial and azimuthal wavenumbers, respectively, ?z (>0) and ?? (≥0) are the corresponding vorticities, and r is radius. Maximum instability occurs approximately where k and n are related by 2kr?z + n?? = 0, provided ?? is small compared to ?z. Growth rates, for a tornado vortex of typical dimensions and vorticities, are significant fractions of a second.
    publisherAmerican Meteorological Society
    titleHydrodynamic Instability of Small Eddies in a Tornado Vortex
    typeJournal Paper
    journal volume41
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1984)041<0422:HIOSEI>2.0.CO;2
    journal fristpage422
    journal lastpage429
    treeJournal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 003
    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