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    Numerical Modeling of Ice Deposition

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 002::page 226
    Author:
    Koenig, L. R.
    DOI: 10.1175/1520-0469(1971)028<0226:NMOID>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A method of computing the rate of growth of ice crystals by deposition is described. Predictions of growth characteristics over the temperature range of ?1 through ?35C are shown and compared with meager experimental data available within this temperature range. The growth rate equations are based on Fick's law of diffusion. In applying this law to nonspherical ice crystals, the analogy between an electrostatic potential field surrounding a charged body and the vapor-density field surrounding a similarly shaped ice crystal is utilized. Allowances are made for effects of forced convection caused by the movement of the crystal through the air and the change in shape and bulk density of the ice crystal; these effects are predicted to be of significant importance. A simple, empirical equation using two temperature-dependent parameters was found to describe the crystal growth rate as a, function of mass. For many cases where only the rate of mass conversion from vapor to solid is required, the simple equation is believed satisfactory.
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      Numerical Modeling of Ice Deposition

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4151649
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    contributor authorKoenig, L. R.
    date accessioned2017-06-09T14:15:45Z
    date available2017-06-09T14:15:45Z
    date copyright1971/03/01
    date issued1971
    identifier issn0022-4928
    identifier otherams-15923.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151649
    description abstractA method of computing the rate of growth of ice crystals by deposition is described. Predictions of growth characteristics over the temperature range of ?1 through ?35C are shown and compared with meager experimental data available within this temperature range. The growth rate equations are based on Fick's law of diffusion. In applying this law to nonspherical ice crystals, the analogy between an electrostatic potential field surrounding a charged body and the vapor-density field surrounding a similarly shaped ice crystal is utilized. Allowances are made for effects of forced convection caused by the movement of the crystal through the air and the change in shape and bulk density of the ice crystal; these effects are predicted to be of significant importance. A simple, empirical equation using two temperature-dependent parameters was found to describe the crystal growth rate as a, function of mass. For many cases where only the rate of mass conversion from vapor to solid is required, the simple equation is believed satisfactory.
    publisherAmerican Meteorological Society
    titleNumerical Modeling of Ice Deposition
    typeJournal Paper
    journal volume28
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1971)028<0226:NMOID>2.0.CO;2
    journal fristpage226
    journal lastpage237
    treeJournal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 002
    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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