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    Laboratory Measurements of Axial Pressures in Two-Celled Tornado-like Vortices

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 021::page 3392
    Author:
    Pauley, Randal L.
    DOI: 10.1175/1520-0469(1989)046<3392:LMOAPI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An experimental study of two-celled vortex flows was conducted in a Ward-type tornado vortex chamber (TVC). Time-averaged, stream-static pressure measurements on the vortex axis and observations of the visualized flow in two-celled vortices are reported. The static pressure measured on the vortex axis increases with height downstream of the vortex breakdown, with the axial pressure gradient tending to zero only well aloft. Visualization indicates that the flow downstream of the breakdown in the TVC is everywhere two-celled, with the strongest axial downflow occurring at middle levels. Analysis of the vertical momentum equation strengthens the argument that the turbulent stresses can play an important role in the axial momentum balance of two-celled vortices by opposing the ?filling? of the vortex core with higher stagnation pressure fluid from aloft, therefore helping to maintain low pressure and high velocities near the surface.
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      Laboratory Measurements of Axial Pressures in Two-Celled Tornado-like Vortices

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4156423
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    contributor authorPauley, Randal L.
    date accessioned2017-06-09T14:29:22Z
    date available2017-06-09T14:29:22Z
    date copyright1989/11/01
    date issued1988
    identifier issn0022-4928
    identifier otherams-20219.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156423
    description abstractAn experimental study of two-celled vortex flows was conducted in a Ward-type tornado vortex chamber (TVC). Time-averaged, stream-static pressure measurements on the vortex axis and observations of the visualized flow in two-celled vortices are reported. The static pressure measured on the vortex axis increases with height downstream of the vortex breakdown, with the axial pressure gradient tending to zero only well aloft. Visualization indicates that the flow downstream of the breakdown in the TVC is everywhere two-celled, with the strongest axial downflow occurring at middle levels. Analysis of the vertical momentum equation strengthens the argument that the turbulent stresses can play an important role in the axial momentum balance of two-celled vortices by opposing the ?filling? of the vortex core with higher stagnation pressure fluid from aloft, therefore helping to maintain low pressure and high velocities near the surface.
    publisherAmerican Meteorological Society
    titleLaboratory Measurements of Axial Pressures in Two-Celled Tornado-like Vortices
    typeJournal Paper
    journal volume46
    journal issue21
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1989)046<3392:LMOAPI>2.0.CO;2
    journal fristpage3392
    journal lastpage3399
    treeJournal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 021
    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