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    An Analysis of Cloud Drop Growth by Collection: Part IV. A New Parameterization

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 008::page 2127
    Author:
    Berry, Edwin X.
    ,
    Reinhardt, Richard L.
    DOI: 10.1175/1520-0469(1974)031<2127:AAOCDG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new parameterization of cloud particle growth combines the effects of accretion and self-collection, and frees the large-hydrometeor water mass and spectral moments to grow independently. The large-hydrometeor water mass grows through accretion in proportion to the cloud water mass. The spectral moments grow through self-collection in proportion to the large-hydrometeor water content. Accretion is also dependent upon the magnitude of the spectral moments and thus an important feedback loop occurs. The spreading or narrowing of the drop spectrum is dependent upon the collection kernel and the relative magnitudes of accretion and self-collection in the region of interest. These effects are included in the parameterization. In order for the spectrum to spread there must exist both the stochastic mode and a sufficiently rapid increase in the collection kernel with drop size.
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      An Analysis of Cloud Drop Growth by Collection: Part IV. A New Parameterization

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4152499
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    contributor authorBerry, Edwin X.
    contributor authorReinhardt, Richard L.
    date accessioned2017-06-09T14:17:50Z
    date available2017-06-09T14:17:50Z
    date copyright1974/11/01
    date issued1974
    identifier issn0022-4928
    identifier otherams-16689.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152499
    description abstractA new parameterization of cloud particle growth combines the effects of accretion and self-collection, and frees the large-hydrometeor water mass and spectral moments to grow independently. The large-hydrometeor water mass grows through accretion in proportion to the cloud water mass. The spectral moments grow through self-collection in proportion to the large-hydrometeor water content. Accretion is also dependent upon the magnitude of the spectral moments and thus an important feedback loop occurs. The spreading or narrowing of the drop spectrum is dependent upon the collection kernel and the relative magnitudes of accretion and self-collection in the region of interest. These effects are included in the parameterization. In order for the spectrum to spread there must exist both the stochastic mode and a sufficiently rapid increase in the collection kernel with drop size.
    publisherAmerican Meteorological Society
    titleAn Analysis of Cloud Drop Growth by Collection: Part IV. A New Parameterization
    typeJournal Paper
    journal volume31
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1974)031<2127:AAOCDG>2.0.CO;2
    journal fristpage2127
    journal lastpage2135
    treeJournal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian