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    Mixing in Thermals with and without Buoyancy Reversal

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 016::page 1412
    Author:
    Johari, Hamid
    DOI: 10.1175/1520-0469(1992)049<1412:MITWAW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The mixing characteristics of turbulent thermals were investigated in a water tank via laser-induced fluorescence techniques. The concentration of mixed fluid in the far field of a ?classical? thermal is approximately uniform, whereas the near field is dominated by a moderately diluted toroidal core. The effects of atmospheric evaporative cooling on thermals were simulated by using chemicals with nonlinear buoyancy-reversing behavior. Even though the trajectory of an ?evaporating? thermal depends strongly on a buoyancy-reversal parameter, the minimum mixing rate is not greatly modified. A simple derivation, based on the self-similar properties of thermals, provides the minimum molecular-scale mixing rate, which agrees with the measurements. These observations may enhance the understanding of cumulus clouds in weakly stratified environments.
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      Mixing in Thermals with and without Buoyancy Reversal

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    contributor authorJohari, Hamid
    date accessioned2017-06-09T14:30:57Z
    date available2017-06-09T14:30:57Z
    date copyright1992/08/01
    date issued1992
    identifier issn0022-4928
    identifier otherams-20732.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156993
    description abstractThe mixing characteristics of turbulent thermals were investigated in a water tank via laser-induced fluorescence techniques. The concentration of mixed fluid in the far field of a ?classical? thermal is approximately uniform, whereas the near field is dominated by a moderately diluted toroidal core. The effects of atmospheric evaporative cooling on thermals were simulated by using chemicals with nonlinear buoyancy-reversing behavior. Even though the trajectory of an ?evaporating? thermal depends strongly on a buoyancy-reversal parameter, the minimum mixing rate is not greatly modified. A simple derivation, based on the self-similar properties of thermals, provides the minimum molecular-scale mixing rate, which agrees with the measurements. These observations may enhance the understanding of cumulus clouds in weakly stratified environments.
    publisherAmerican Meteorological Society
    titleMixing in Thermals with and without Buoyancy Reversal
    typeJournal Paper
    journal volume49
    journal issue16
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1992)049<1412:MITWAW>2.0.CO;2
    journal fristpage1412
    journal lastpage1426
    treeJournal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 016
    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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