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contributor authorBerg, T. G. Owe
contributor authorClutter, Joyce E.
contributor authorGaukler, Thomas A.
contributor authorMcDonald, Robert L.
date accessioned2017-06-09T14:14:26Z
date available2017-06-09T14:14:26Z
date copyright1968/05/01
date issued1968
identifier issn0022-4928
identifier otherams-15436.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151108
description abstractExperiments were conducted with sublimate AgI or AgI smoke in an expansion chamber at various temperatures. A condensate cloud of liquid droplets was formed at all temperatures. Below ?5C ice crystals appeared in the cloud a few seconds after its formation. Photographs were taken of liquid droplets and of partially frozen droplets. The droplet diameter was 7 ? above 0C, but at lower temperatures it was larger, reaching 15 ? at ?7C. The results show that the water vapor is converted to ice by condensation followed by freezing of the liquid droplets under these conditions. Impurities in the AgI and the air had no effect upon these observations.
publisherAmerican Meteorological Society
titleConversion of Water Vapor to Ice by Silver Iodide
typeJournal Paper
journal volume25
journal issue3
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1968)025<0464:COWVTI>2.0.CO;2
journal fristpage464
journal lastpage469
treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 003
contenttypeFulltext


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