Sublimation of Ice CrystalsSource: Journal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 005::page 910Author:Nelson, Jon
DOI: 10.1175/1520-0469(1998)055<0910:SOIC>2.0.CO;2Publisher: American Meteorological Society
Abstract: Recent experiments on the sublimation of single crystals of ice in an atmosphere of air indicate that the sublimation rate is diffusion limited and initially solid prismatic crystals evolve into time-independent shapes similar to confocal ellipses rotated about their major or minor axis (prolate or oblate spheroids). Step formation at crystal edges and vapor diffusion easily explain these observations.
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| contributor author | Nelson, Jon | |
| date accessioned | 2017-06-09T14:34:56Z | |
| date available | 2017-06-09T14:34:56Z | |
| date copyright | 1998/03/01 | |
| date issued | 1998 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-22144.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4158562 | |
| description abstract | Recent experiments on the sublimation of single crystals of ice in an atmosphere of air indicate that the sublimation rate is diffusion limited and initially solid prismatic crystals evolve into time-independent shapes similar to confocal ellipses rotated about their major or minor axis (prolate or oblate spheroids). Step formation at crystal edges and vapor diffusion easily explain these observations. | |
| publisher | American Meteorological Society | |
| title | Sublimation of Ice Crystals | |
| type | Journal Paper | |
| journal volume | 55 | |
| journal issue | 5 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1998)055<0910:SOIC>2.0.CO;2 | |
| journal fristpage | 910 | |
| journal lastpage | 919 | |
| tree | Journal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 005 | |
| contenttype | Fulltext |