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contributor authorKobayashi, T.
contributor authorOhtake, T.
date accessioned2017-06-09T14:17:36Z
date available2017-06-09T14:17:36Z
date copyright1974/07/01
date issued1974
identifier issn0022-4928
identifier otherams-16603.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152405
description abstractMany prismatic ice crystals have been observed to have grooves which circle the prism faces at right angles to the c-axis. In both natural and artificial crystals the grooves appear when the crystal is evaporating and disappear when it is growing. A possible ice-twinning structure is proposed to explain these observations, analogous to zinc-blende rotation twins and implying a diamond-structured layer at the interface.
publisherAmerican Meteorological Society
titleHexagonal Twin Prisms of Ice
typeJournal Paper
journal volume31
journal issue5
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1974)031<1377:HTPOI>2.0.CO;2
journal fristpage1377
journal lastpage1383
treeJournal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 005
contenttypeFulltext


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