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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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