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    Ventilation Coefficients for Falling Ice Crystals in the Atmosphere at Low–Intermediate Reynolds Numbers

    Source: Journal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 006::page 829
    Author:
    Ji, Wusheng
    ,
    Wang, Pao K.
    DOI: 10.1175/1520-0469(1999)056<0829:VCFFIC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The ventilation coefficients for columnar, hexagonal plate, and broad branch ice crystals falling in air are computed by first solving numerically the convective diffusion equation for water vapor density to obtain its profile around these ice crystals and then determining the total vapor flux on the surface of the crystal. The ratio of this flux to the flux on a stationary crystal gives the ventilation coefficient. The local flow velocity profiles around the falling crystals necessary for specifying the convective term in the convective diffusion equation were obtained previously by numerically solving the unsteady Navier?Stokes equations subject to appropriate crystal-shaped boundary conditions. Ventilation coefficients obtained in this way are illustrated as a function of the Schmidt and Reynolds numbers and are also fitted by empirical expressions. Applications of these ventilation coefficients are discussed.
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      Ventilation Coefficients for Falling Ice Crystals in the Atmosphere at Low–Intermediate Reynolds Numbers

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4158720
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    contributor authorJi, Wusheng
    contributor authorWang, Pao K.
    date accessioned2017-06-09T14:35:19Z
    date available2017-06-09T14:35:19Z
    date copyright1999/03/01
    date issued1999
    identifier issn0022-4928
    identifier otherams-22287.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158720
    description abstractThe ventilation coefficients for columnar, hexagonal plate, and broad branch ice crystals falling in air are computed by first solving numerically the convective diffusion equation for water vapor density to obtain its profile around these ice crystals and then determining the total vapor flux on the surface of the crystal. The ratio of this flux to the flux on a stationary crystal gives the ventilation coefficient. The local flow velocity profiles around the falling crystals necessary for specifying the convective term in the convective diffusion equation were obtained previously by numerically solving the unsteady Navier?Stokes equations subject to appropriate crystal-shaped boundary conditions. Ventilation coefficients obtained in this way are illustrated as a function of the Schmidt and Reynolds numbers and are also fitted by empirical expressions. Applications of these ventilation coefficients are discussed.
    publisherAmerican Meteorological Society
    titleVentilation Coefficients for Falling Ice Crystals in the Atmosphere at Low–Intermediate Reynolds Numbers
    typeJournal Paper
    journal volume56
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1999)056<0829:VCFFIC>2.0.CO;2
    journal fristpage829
    journal lastpage836
    treeJournal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 006
    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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