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    Aging of Accreted Ice

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 006::page 1375
    Author:
    Prodi, F.
    ,
    Levi, L.
    DOI: 10.1175/1520-0469(1980)037<1375:AOAI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The effect of annealing in accreted ice has been investigated for artificially grown ice deposits after ?100 days of storage in a deep freeze unit. Cross sections of the cylindrical deposits have been cut and replicated soon after growth and after annealing to determine the average cross section σ?, the maximum length li, the maximum width wi, and the orientation of the c axis of the crystal grains. Significant grain growth has been observed even at the relatively low temperature of ?19°C. The average grain cross section increased for nearly all the deposits, and a decrease of the grain elongation was observed while the crystals tended to assume compact final shapes. The statistical distributions of the orientations of crystal grains was not modified substantially by annealing, thus indicating that information on hailstone growth may be contained more firmly in the orientation of crystals rather than in their size. The change of the crystal dimensions is interpreted in terms of a polycrystalline grain growth process. The consequences of annealing on the crystal size analysis in hailstones are examined.
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      Aging of Accreted Ice

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153891
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    contributor authorProdi, F.
    contributor authorLevi, L.
    date accessioned2017-06-09T14:21:35Z
    date available2017-06-09T14:21:35Z
    date copyright1980/06/01
    date issued1980
    identifier issn0022-4928
    identifier otherams-17941.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153891
    description abstractThe effect of annealing in accreted ice has been investigated for artificially grown ice deposits after ?100 days of storage in a deep freeze unit. Cross sections of the cylindrical deposits have been cut and replicated soon after growth and after annealing to determine the average cross section σ?, the maximum length li, the maximum width wi, and the orientation of the c axis of the crystal grains. Significant grain growth has been observed even at the relatively low temperature of ?19°C. The average grain cross section increased for nearly all the deposits, and a decrease of the grain elongation was observed while the crystals tended to assume compact final shapes. The statistical distributions of the orientations of crystal grains was not modified substantially by annealing, thus indicating that information on hailstone growth may be contained more firmly in the orientation of crystals rather than in their size. The change of the crystal dimensions is interpreted in terms of a polycrystalline grain growth process. The consequences of annealing on the crystal size analysis in hailstones are examined.
    publisherAmerican Meteorological Society
    titleAging of Accreted Ice
    typeJournal Paper
    journal volume37
    journal issue6
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1980)037<1375:AOAI>2.0.CO;2
    journal fristpage1375
    journal lastpage1384
    treeJournal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 006
    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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