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    On the Evaluation of the Collection Kernel for the Coalescence of Water Droplets

    Source: Journal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 004::page 1053
    Author:
    Long, Alexis B.
    ,
    Manton, Michael J.
    DOI: 10.1175/1520-0469(1974)031<1053:OTEOTC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Two anomalies are described which arise in the kernel for stochastic droplet collection when it is specified by the formula of Scott and Chen for the linear collision efficiency y(R,r) and by the formula of Wobus et al. for the droplet terminal velocity V(R). It is pointed out that if accurate values for y(R,r) are to be obtained for a given droplet pair by interpolation using data for specific droplet pairs, then for large droplet radii (R<30 ?m) it is desirable that these data he tabulated for 2-?m intervals of R. It is shown that if the difference in terminal velocities of two droplets is computed from a formula approximating V(R) and composed of various functions V*(R) applicable over adjoining domains of R, then it is necessary that these functions be constructed so that the formula and its derivatives, at least up to second order, are everywhere continuous. An improved formula for V(R) satisfying this criterion is described.
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      On the Evaluation of the Collection Kernel for the Coalescence of Water Droplets

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4152369
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    contributor authorLong, Alexis B.
    contributor authorManton, Michael J.
    date accessioned2017-06-09T14:17:31Z
    date available2017-06-09T14:17:31Z
    date copyright1974/05/01
    date issued1974
    identifier issn0022-4928
    identifier otherams-16571.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152369
    description abstractTwo anomalies are described which arise in the kernel for stochastic droplet collection when it is specified by the formula of Scott and Chen for the linear collision efficiency y(R,r) and by the formula of Wobus et al. for the droplet terminal velocity V(R). It is pointed out that if accurate values for y(R,r) are to be obtained for a given droplet pair by interpolation using data for specific droplet pairs, then for large droplet radii (R<30 ?m) it is desirable that these data he tabulated for 2-?m intervals of R. It is shown that if the difference in terminal velocities of two droplets is computed from a formula approximating V(R) and composed of various functions V*(R) applicable over adjoining domains of R, then it is necessary that these functions be constructed so that the formula and its derivatives, at least up to second order, are everywhere continuous. An improved formula for V(R) satisfying this criterion is described.
    publisherAmerican Meteorological Society
    titleOn the Evaluation of the Collection Kernel for the Coalescence of Water Droplets
    typeJournal Paper
    journal volume31
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1974)031<1053:OTEOTC>2.0.CO;2
    journal fristpage1053
    journal lastpage1057
    treeJournal of the Atmospheric Sciences:;1974:;Volume( 031 ):;issue: 004
    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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