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    Cloud Modification by Helicopter Wakes

    Source: Journal of Applied Meteorology:;1969:;volume( 008 ):;issue: 004::page 566
    Author:
    Plank, Vernon G.
    ,
    Spatola, Alfred A.
    DOI: 10.1175/1520-0450(1969)008<0566:CMBHW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Helicopter wake effects on stratus and stratocumulus clouds are described. Holes and troughs were created in such clouds with dimensions several hundred feet across. The velocities and penetration distances of the downwash flow beneath the HH-53B helicopter employed in the experiments were investigated by the release of a ?tracing agent? from the helicopter and by hovering at various altitudes above the water surface of a Florida bayou. The downwash velocities were as large as 100 ft sec?1, near the rotor, and the downwash extended some 1300 ft beneath the helicopter (under near dry adiabatic conditions). A suggestion is made that helicopters might be employed operationally to clear radiation-type ground fog from airfield runways. The cloud clearing capabilities of the HH-53B helicopter are discussed in support of this suggestion, by reference to observational data and to the theory of Hohler.
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      Cloud Modification by Helicopter Wakes

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4221400
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    contributor authorPlank, Vernon G.
    contributor authorSpatola, Alfred A.
    date accessioned2017-06-09T17:03:30Z
    date available2017-06-09T17:03:30Z
    date copyright1969/08/01
    date issued1969
    identifier issn0021-8952
    identifier otherams-7870.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221400
    description abstractHelicopter wake effects on stratus and stratocumulus clouds are described. Holes and troughs were created in such clouds with dimensions several hundred feet across. The velocities and penetration distances of the downwash flow beneath the HH-53B helicopter employed in the experiments were investigated by the release of a ?tracing agent? from the helicopter and by hovering at various altitudes above the water surface of a Florida bayou. The downwash velocities were as large as 100 ft sec?1, near the rotor, and the downwash extended some 1300 ft beneath the helicopter (under near dry adiabatic conditions). A suggestion is made that helicopters might be employed operationally to clear radiation-type ground fog from airfield runways. The cloud clearing capabilities of the HH-53B helicopter are discussed in support of this suggestion, by reference to observational data and to the theory of Hohler.
    publisherAmerican Meteorological Society
    titleCloud Modification by Helicopter Wakes
    typeJournal Paper
    journal volume8
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1969)008<0566:CMBHW>2.0.CO;2
    journal fristpage566
    journal lastpage578
    treeJournal of Applied Meteorology:;1969:;volume( 008 ):;issue: 004
    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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