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    Conversion of Water Vapor to Ice by Silver Iodide

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 003::page 464
    Author:
    Berg, T. G. Owe
    ,
    Clutter, Joyce E.
    ,
    Gaukler, Thomas A.
    ,
    McDonald, Robert L.
    DOI: 10.1175/1520-0469(1968)025<0464:COWVTI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Experiments 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.
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      Conversion of Water Vapor to Ice by Silver Iodide

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4151108
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    • Journal of the Atmospheric Sciences

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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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    DSpace software copyright © 2002-2015  DuraSpace
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