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    Glaciation of a Cumulus at Approximately −4C

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 005::page 889
    Author:
    Mossop, S. C.
    ,
    Ruskin, R. E.
    ,
    Heffernan, K. J.
    DOI: 10.1175/1520-0469(1968)025<0889:GOACAA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A long-lived cumulus cloud off the southern coast of Australia was found to contain ice crystals, even though the coldest temperature in it was about ?4C. Two instrumented aircraft made successive passes through the cloud and continuous samplers were used to replicate cloud particles. It was found that columnar crystals were present in concentrations up to 100 liter?1. This was at least three orders of magnitude greater than the expected concentration of active ice nuclei as determined by cloud chamber measurements made under the base of the same cloud. It appears that some ice crystal multiplication mechanism was at work, though the exact nature of the process cannot be decided on available evidence.
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      Glaciation of a Cumulus at Approximately −4C

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    contributor authorMossop, S. C.
    contributor authorRuskin, R. E.
    contributor authorHeffernan, K. J.
    date accessioned2017-06-09T14:14:37Z
    date available2017-06-09T14:14:37Z
    date copyright1968/09/01
    date issued1968
    identifier issn0022-4928
    identifier otherams-15502.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151182
    description abstractA long-lived cumulus cloud off the southern coast of Australia was found to contain ice crystals, even though the coldest temperature in it was about ?4C. Two instrumented aircraft made successive passes through the cloud and continuous samplers were used to replicate cloud particles. It was found that columnar crystals were present in concentrations up to 100 liter?1. This was at least three orders of magnitude greater than the expected concentration of active ice nuclei as determined by cloud chamber measurements made under the base of the same cloud. It appears that some ice crystal multiplication mechanism was at work, though the exact nature of the process cannot be decided on available evidence.
    publisherAmerican Meteorological Society
    titleGlaciation of a Cumulus at Approximately −4C
    typeJournal Paper
    journal volume25
    journal issue5
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1968)025<0889:GOACAA>2.0.CO;2
    journal fristpage889
    journal lastpage899
    treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 005
    contenttypeFulltext
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