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dc.contributor.authorKochtubajda, B.
dc.contributor.authorLozowski, E. P.
dc.date.accessioned2017-06-09T14:00:39Z
dc.date.available2017-06-09T14:00:39Z
dc.date.copyright1985/06/01
dc.date.issued1985
dc.identifier.issn0733-3021
dc.identifier.otherams-10860.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146024
dc.description.abstractA numerical model has been developed to investigate the sublimation rate of cylindrical dry ice pellets in clear and cloudy air. Experiments conducted in the University of Alberta FROST icing-wind tunnel were used to make comparisons with the model predictions of the sublimation rate. These experiments were carried out in both cold and warm environments. Furthermore, some of the experiments were conducted with the sprays operating in order to determine the effect of a simulated ?cloudy? environment on the sublimation rate. The principal conclusions are: a) despite the use of several simplifying assumptions, the cylindrical model predict the sublimation rates of dry ice pellets to within 20%, when compared with wind tunnel observations, and b) cloudy and saturated conditions at warm temperatures enhance the sublimation rate of dry ice, but cloudy and saturated conditions at cold temperatures do not have an appreciable effect on the sublimation rate of dry ice.
dc.publisherAmerican Meteorological Society
dc.titleThe Sublimation of Dry Ice Pellets Used for Cloud Seeding
dc.typeJournal Paper
dc.journal.volume24
dc.journal.issue6
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1985)024<0597:TSODIP>2.0.CO;2
dc.journal.fristpage597
dc.journal.lastpage605
dc.treeJournal of Climate and Applied Meteorology:;1985:;Volume( 024 ):;Issue: 006
dc.contenttypeFulltext


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