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    Time-Constant Variation in the Collision-Breakup Equation

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 012::page 2758
    Author:
    Brown, Philip S.
    DOI: 10.1175/1520-0469(1981)038<2758:TCVITC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Discretization of the collision-breakup equation results in a nonlinear system that can produce highly damped solution components. An analytic expression is derived for the smallest time constant τmin, a parameter used to describe the most rapid decay rate associated with the system. τmin is found to be a measure of the decay time for destruction of the largest drops considered in the model. For Marshall-Palmer distributions N0e?AD, τmin decreases with increasing N0 and with increasing rainfall rate R. τmin determines the maximum time step that can be used to insure computational stability in numerical solution of the breakup equation. For large N0 and R, time steps as small as 1 s may be required to prevent error growth.
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      Time-Constant Variation in the Collision-Breakup Equation

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    contributor authorBrown, Philip S.
    date accessioned2017-06-09T14:22:44Z
    date available2017-06-09T14:22:44Z
    date copyright1981/12/01
    date issued1981
    identifier issn0022-4928
    identifier otherams-18260.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154246
    description abstractDiscretization of the collision-breakup equation results in a nonlinear system that can produce highly damped solution components. An analytic expression is derived for the smallest time constant τmin, a parameter used to describe the most rapid decay rate associated with the system. τmin is found to be a measure of the decay time for destruction of the largest drops considered in the model. For Marshall-Palmer distributions N0e?AD, τmin decreases with increasing N0 and with increasing rainfall rate R. τmin determines the maximum time step that can be used to insure computational stability in numerical solution of the breakup equation. For large N0 and R, time steps as small as 1 s may be required to prevent error growth.
    publisherAmerican Meteorological Society
    titleTime-Constant Variation in the Collision-Breakup Equation
    typeJournal Paper
    journal volume38
    journal issue12
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1981)038<2758:TCVITC>2.0.CO;2
    journal fristpage2758
    journal lastpage2762
    treeJournal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 012
    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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