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    WIND SPEED AND AIR FLOW PATTERNS IN THE DALLAS TORNADO OF APRIL 2, 1957

    Source: Monthly Weather Review:;1960:;volume( 088 ):;issue: 005::page 167
    Author:
    HOECKER, WALTER H.
    DOI: 10.1175/1520-0493(1960)088<0167:WSAAFP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A composite distribution of tangential and upward components of air flow is determined by tracing particles of debris and cloud tag movements in scaled movies of a tornado. The greatest tangential speed measured is 170 m.p.h. and the greatest upward speed derived is 150 m.p.h. A distribution of the convergent radial component of motion in the lower 600 ft. of the vortex is synthesized and used t o generate a vertical speed distribution which nearly duplicates the observed vertical speed distribution. The observed radial distribution of the vertical component of relative vorticity at three levels is shown and convergence at the 500-ft. radius is computed using the synthesized radial speed distribution. Three-dimensional trajectories of air parcels in the lower portion of the vortex are also shown.
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      WIND SPEED AND AIR FLOW PATTERNS IN THE DALLAS TORNADO OF APRIL 2, 1957

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4197440
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    contributor authorHOECKER, WALTER H.
    date accessioned2017-06-09T15:56:38Z
    date available2017-06-09T15:56:38Z
    date copyright1960/05/01
    date issued1960
    identifier issn0027-0644
    identifier otherams-57137.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4197440
    description abstractA composite distribution of tangential and upward components of air flow is determined by tracing particles of debris and cloud tag movements in scaled movies of a tornado. The greatest tangential speed measured is 170 m.p.h. and the greatest upward speed derived is 150 m.p.h. A distribution of the convergent radial component of motion in the lower 600 ft. of the vortex is synthesized and used t o generate a vertical speed distribution which nearly duplicates the observed vertical speed distribution. The observed radial distribution of the vertical component of relative vorticity at three levels is shown and convergence at the 500-ft. radius is computed using the synthesized radial speed distribution. Three-dimensional trajectories of air parcels in the lower portion of the vortex are also shown.
    publisherAmerican Meteorological Society
    titleWIND SPEED AND AIR FLOW PATTERNS IN THE DALLAS TORNADO OF APRIL 2, 1957
    typeJournal Paper
    journal volume88
    journal issue5
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1960)088<0167:WSAAFP>2.0.CO;2
    journal fristpage167
    journal lastpage180
    treeMonthly Weather Review:;1960:;volume( 088 ):;issue: 005
    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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