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    A Measurement of the Velocity Field of a Cumulus Cloud

    Source: Journal of Applied Meteorology:;1973:;volume( 012 ):;issue: 005::page 841
    Author:
    Levine, J.
    ,
    Garstang, M.
    ,
    LaSeur, N. E.
    DOI: 10.1175/1520-0450(1973)012<0841:AMOTVF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A 3-hr flight of a constant-volume balloon which is entrained into a cumulus congestus cloud and lifted to an altitude of nearly 3 km provides an opportunity to determine the trajectory and vertical velocity of the balloon and, in turn, relate these to the circulation of the cloud. Simultaneous supplementary observations by radar, cameras, satellite, and other ground based instruments provide the meteorological context for the event. Computations show that the vertical velocities of the cloud may approach 10 m sec?1, and sustained upward velocities of 3?5 m sec?1 are maintained for considerable periods of time and height. Comparison with a ?jet? model shows remarkable agreement, while the ?bubble? model would require unreasonably large values of the radius to generate the observed vertical velocities.
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      A Measurement of the Velocity Field of a Cumulus Cloud

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4229411
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    contributor authorLevine, J.
    contributor authorGarstang, M.
    contributor authorLaSeur, N. E.
    date accessioned2017-06-09T17:28:26Z
    date available2017-06-09T17:28:26Z
    date copyright1973/08/01
    date issued1973
    identifier issn0021-8952
    identifier otherams-8591.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229411
    description abstractA 3-hr flight of a constant-volume balloon which is entrained into a cumulus congestus cloud and lifted to an altitude of nearly 3 km provides an opportunity to determine the trajectory and vertical velocity of the balloon and, in turn, relate these to the circulation of the cloud. Simultaneous supplementary observations by radar, cameras, satellite, and other ground based instruments provide the meteorological context for the event. Computations show that the vertical velocities of the cloud may approach 10 m sec?1, and sustained upward velocities of 3?5 m sec?1 are maintained for considerable periods of time and height. Comparison with a ?jet? model shows remarkable agreement, while the ?bubble? model would require unreasonably large values of the radius to generate the observed vertical velocities.
    publisherAmerican Meteorological Society
    titleA Measurement of the Velocity Field of a Cumulus Cloud
    typeJournal Paper
    journal volume12
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1973)012<0841:AMOTVF>2.0.CO;2
    journal fristpage841
    journal lastpage846
    treeJournal of Applied Meteorology:;1973:;volume( 012 ):;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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