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    Crystallographic Orientation Distributions in Accreted Ice

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 003::page 849
    Author:
    Macklin, W. C.
    ,
    Rye, P. J.
    DOI: 10.1175/1520-0469(1974)031<0849:CODIAI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The c-axis orientation distributions of ice formed by the accretion of supercooled droplets have been determined for a wide range of air and deposit temperatures. There are peaks in the distributions which may be related to the air temperature. Consequently, quantitative information on the growth environment of a hailstone can be obtained from its crystallographic structure.
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      Crystallographic Orientation Distributions in Accreted Ice

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4152352
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    contributor authorMacklin, W. C.
    contributor authorRye, P. J.
    date accessioned2017-06-09T14:17:27Z
    date available2017-06-09T14:17:27Z
    date copyright1974/04/01
    date issued1974
    identifier issn0022-4928
    identifier otherams-16556.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152352
    description abstractThe c-axis orientation distributions of ice formed by the accretion of supercooled droplets have been determined for a wide range of air and deposit temperatures. There are peaks in the distributions which may be related to the air temperature. Consequently, quantitative information on the growth environment of a hailstone can be obtained from its crystallographic structure.
    publisherAmerican Meteorological Society
    titleCrystallographic Orientation Distributions in Accreted Ice
    typeJournal Paper
    journal volume31
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1974)031<0849:CODIAI>2.0.CO;2
    journal fristpage849
    journal lastpage852
    treeJournal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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