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    Unusual Types of Single Ice Crystals Originating from Frozen Cloud Droplets

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 012::page 2495
    Author:
    Magono, Choji
    ,
    Fujita, Shin-Ichi
    ,
    Taniguchi, Takashi
    DOI: 10.1175/1520-0469(1979)036<2495:UTOSIC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Laboratory experiments were conducted to study the formation process of unusual types of ice crystals, using a cold chamber in the temperature range ?15 to ?25°C. Ice crystals of the bottle type seem to originate from frozen water droplets with spicules. Ice crystals of twin columns (or twin bullets) with plates were found. By observing the various stages of development of pyramidal faces of ice crystals with plates and ice crystals of ?single bullet? type?it was concluded that these pyramidal portions of ice crystals may originate from the spicule of frozen droplets or from hemispherical frozen droplets, and that the pyramidal faces can survive further growth at temperatures colder that ?25°C.
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      Unusual Types of Single Ice Crystals Originating from Frozen Cloud Droplets

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153754
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    contributor authorMagono, Choji
    contributor authorFujita, Shin-Ichi
    contributor authorTaniguchi, Takashi
    date accessioned2017-06-09T14:21:09Z
    date available2017-06-09T14:21:09Z
    date copyright1979/12/01
    date issued1979
    identifier issn0022-4928
    identifier otherams-17818.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153754
    description abstractLaboratory experiments were conducted to study the formation process of unusual types of ice crystals, using a cold chamber in the temperature range ?15 to ?25°C. Ice crystals of the bottle type seem to originate from frozen water droplets with spicules. Ice crystals of twin columns (or twin bullets) with plates were found. By observing the various stages of development of pyramidal faces of ice crystals with plates and ice crystals of ?single bullet? type?it was concluded that these pyramidal portions of ice crystals may originate from the spicule of frozen droplets or from hemispherical frozen droplets, and that the pyramidal faces can survive further growth at temperatures colder that ?25°C.
    publisherAmerican Meteorological Society
    titleUnusual Types of Single Ice Crystals Originating from Frozen Cloud Droplets
    typeJournal Paper
    journal volume36
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1979)036<2495:UTOSIC>2.0.CO;2
    journal fristpage2495
    journal lastpage2501
    treeJournal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 012
    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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