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    Calculations of Ice Crystal Growth

    Source: Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 005::page 728
    Author:
    Jayaweera, K. O. L. F.
    DOI: 10.1175/1520-0469(1971)028<0728:COICG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The growth rates, and the masses to which the crystals grow at different times, are calculated for various temperatures using the electrostatic analogy and assuming that the crystals follow the experimentally observed growth modes. The additional contribution to growth due to ventilation of the falling crystal is calculated. For small plate-like crystals and for all sizes of columns it is comparable with the growth by diffusion alone, while for larger plate-like crystals ventilation predominates. Peaks in the growth rate occur at temperatures of about ?5 and ?15C as a consequence of the high axial ratio of the crystals characteristic of these temperatures (needles and dendrites, respectively). At other temperatures, calculated growth rates do not differ widely from those obtained by assuming a spherical ice particle.
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      Calculations of Ice Crystal Growth

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    contributor authorJayaweera, K. O. L. F.
    date accessioned2017-06-09T14:15:53Z
    date available2017-06-09T14:15:53Z
    date copyright1971/07/01
    date issued1971
    identifier issn0022-4928
    identifier otherams-15981.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151713
    description abstractThe growth rates, and the masses to which the crystals grow at different times, are calculated for various temperatures using the electrostatic analogy and assuming that the crystals follow the experimentally observed growth modes. The additional contribution to growth due to ventilation of the falling crystal is calculated. For small plate-like crystals and for all sizes of columns it is comparable with the growth by diffusion alone, while for larger plate-like crystals ventilation predominates. Peaks in the growth rate occur at temperatures of about ?5 and ?15C as a consequence of the high axial ratio of the crystals characteristic of these temperatures (needles and dendrites, respectively). At other temperatures, calculated growth rates do not differ widely from those obtained by assuming a spherical ice particle.
    publisherAmerican Meteorological Society
    titleCalculations of Ice Crystal Growth
    typeJournal Paper
    journal volume28
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1971)028<0728:COICG>2.0.CO;2
    journal fristpage728
    journal lastpage736
    treeJournal of the Atmospheric Sciences:;1971:;Volume( 028 ):;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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