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    A Laboratory Study of Atmospheric Ice Particles

    Source: Journal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 003::page 232
    Author:
    Hoffer, Thomas E.
    ,
    Braham, Roscoe R.
    DOI: 10.1175/1520-0469(1962)019<0232:ALSOAI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: As a means of studying ice nucleation, snow and ice pellets collected from the tops of clouds were melted and refrozen in order to determine their freezing temperatures. In all cases where a definite cloud top temperature could be assigned, the melted ice pellets froze at a temperature colder than that of the cloud top, indicating that these pellets did not originate through the heterogeneous freezing of cloud drops. Essentially no difference was indicated in the freezing temperatures of ice pellets collected on seeded and non-seeded days. A firm statement on this point could not be made as the number of observations is limited, and it is not certain that the seeding agent had been ingested into the cloud being studied.
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      A Laboratory Study of Atmospheric Ice Particles

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4150448
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    contributor authorHoffer, Thomas E.
    contributor authorBraham, Roscoe R.
    date accessioned2017-06-09T14:12:53Z
    date available2017-06-09T14:12:53Z
    date copyright1962/05/01
    date issued1962
    identifier issn0022-4928
    identifier otherams-14842.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150448
    description abstractAs a means of studying ice nucleation, snow and ice pellets collected from the tops of clouds were melted and refrozen in order to determine their freezing temperatures. In all cases where a definite cloud top temperature could be assigned, the melted ice pellets froze at a temperature colder than that of the cloud top, indicating that these pellets did not originate through the heterogeneous freezing of cloud drops. Essentially no difference was indicated in the freezing temperatures of ice pellets collected on seeded and non-seeded days. A firm statement on this point could not be made as the number of observations is limited, and it is not certain that the seeding agent had been ingested into the cloud being studied.
    publisherAmerican Meteorological Society
    titleA Laboratory Study of Atmospheric Ice Particles
    typeJournal Paper
    journal volume19
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1962)019<0232:ALSOAI>2.0.CO;2
    journal fristpage232
    journal lastpage235
    treeJournal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 003
    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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