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    The Stochastic Coalescence Model for Cloud Droplet Growth

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 008::page 1496
    Author:
    Gillespie, Daniel T.
    DOI: 10.1175/1520-0469(1972)029<1496:TSCMFC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The stochastic coalescence model for droplet growth in warm clouds is analyzed, with a view to clarifying the theoretical foundations and significance of the well-known stochastic coalescence equation. It is suggested that the analysis of the model is most logically carried out in terms of a function P (n, m; t which is defined as the probability that the number of cloud droplets consisting of m molecules at time t will be n. A time-evolution equation for P (n, m; t is derived, and under certain stated assumptions it is deduced that: 1) the mean value of P (n, m; t with respect to n satisfies the stochastic coalescence equation; and 2) regardless of the initial conditions, the graph of P (n, m; t vs n will approach the Poisson shape as t ?∞ to with an estimable ?relaxation tirne.? The implications of these results for the stochastic fluctuations in the number of cloud droplets are examined. It is found that a distinction must be made between fluctuations in droplet concentration arising from the assumed stochasticity of the coalescence process, and fluctuations in droplet concentration arising from the hypothesis that the droplets are randomly positioned in the cloud; the former fluctuations are normally very much smaller than the latter.
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      The Stochastic Coalescence Model for Cloud Droplet Growth

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4152050
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    contributor authorGillespie, Daniel T.
    date accessioned2017-06-09T14:16:43Z
    date available2017-06-09T14:16:43Z
    date copyright1972/11/01
    date issued1972
    identifier issn0022-4928
    identifier otherams-16284.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152050
    description abstractThe stochastic coalescence model for droplet growth in warm clouds is analyzed, with a view to clarifying the theoretical foundations and significance of the well-known stochastic coalescence equation. It is suggested that the analysis of the model is most logically carried out in terms of a function P (n, m; t which is defined as the probability that the number of cloud droplets consisting of m molecules at time t will be n. A time-evolution equation for P (n, m; t is derived, and under certain stated assumptions it is deduced that: 1) the mean value of P (n, m; t with respect to n satisfies the stochastic coalescence equation; and 2) regardless of the initial conditions, the graph of P (n, m; t vs n will approach the Poisson shape as t ?∞ to with an estimable ?relaxation tirne.? The implications of these results for the stochastic fluctuations in the number of cloud droplets are examined. It is found that a distinction must be made between fluctuations in droplet concentration arising from the assumed stochasticity of the coalescence process, and fluctuations in droplet concentration arising from the hypothesis that the droplets are randomly positioned in the cloud; the former fluctuations are normally very much smaller than the latter.
    publisherAmerican Meteorological Society
    titleThe Stochastic Coalescence Model for Cloud Droplet Growth
    typeJournal Paper
    journal volume29
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1972)029<1496:TSCMFC>2.0.CO;2
    journal fristpage1496
    journal lastpage1510
    treeJournal of the Atmospheric Sciences:;1972:;Volume( 029 ):;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
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