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    The Origin and Concentration of Ice Crystals in Clouds

    Source: Bulletin of the American Meteorological Society:;1985:;volume( 066 ):;issue: 003::page 264
    Author:
    Mossop, S. C.
    DOI: 10.1175/1520-0477(1985)066<0264:TOACOI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Ice crystals in supercooled clouds may form upon ice nuclei, or they may arise through secondary processes. Two of these secondary ice ?multiplication? mechanisms are discussed in some detail: the rime-splintering process and the mechanical fracture of ice particles. The nature of the water-drop size distribution has an important bearing on secondary ice production. Confident predictions of ice particle concentration can only be made in a few limited cloud situations. This is a serious handicap in assessing the feasibility of artificial rainmaking through the ice crystal process.
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      The Origin and Concentration of Ice Crystals in Clouds

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    contributor authorMossop, S. C.
    date accessioned2017-06-09T14:40:14Z
    date available2017-06-09T14:40:14Z
    date copyright1985/03/01
    date issued1985
    identifier issn0003-0007
    identifier otherams-24111.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160748
    description abstractIce crystals in supercooled clouds may form upon ice nuclei, or they may arise through secondary processes. Two of these secondary ice ?multiplication? mechanisms are discussed in some detail: the rime-splintering process and the mechanical fracture of ice particles. The nature of the water-drop size distribution has an important bearing on secondary ice production. Confident predictions of ice particle concentration can only be made in a few limited cloud situations. This is a serious handicap in assessing the feasibility of artificial rainmaking through the ice crystal process.
    publisherAmerican Meteorological Society
    titleThe Origin and Concentration of Ice Crystals in Clouds
    typeJournal Paper
    journal volume66
    journal issue3
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1985)066<0264:TOACOI>2.0.CO;2
    journal fristpage264
    journal lastpage273
    treeBulletin of the American Meteorological Society:;1985:;volume( 066 ):;issue: 003
    contenttypeFulltext
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