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    Parameterization of Ice Growth for Numerical Calculations of Cloud Dynamics

    Source: Monthly Weather Review:;1972:;volume( 100 ):;issue: 006::page 417
    Author:
    KOENIG, L. RANDALL
    DOI: 10.1175/1520-0493(1972)100<0417:POIGFN>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: Parametric equations describing the growth of ice particles in the range 10?11?1 g are presented. Three subranges (10?11?5 ? 10?8, 5 ? 10?8?10?4, and 10?4?1 g) are used. The parametric equations were developed with the aid of a complex method of calculating ice-particle growth. Two approaches to using the parametric equations in a simulation resembling a natural cloud situation are described. One method breaks the ice-particle spectrum into three components, the sizes of each being monitored. The other assumes a size distribution that can be characterized by a ?growth-median? size, so that only one size need be monitored to describe the rate of growth. The parametric method is compared with more complicated methods in a simulated cloud environment, and the results are regarded as satisfactory.
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      Parameterization of Ice Growth for Numerical Calculations of Cloud Dynamics

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4198897
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    contributor authorKOENIG, L. RANDALL
    date accessioned2017-06-09T16:00:01Z
    date available2017-06-09T16:00:01Z
    date copyright1972/06/01
    date issued1972
    identifier issn0027-0644
    identifier otherams-58449.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198897
    description abstractParametric equations describing the growth of ice particles in the range 10?11?1 g are presented. Three subranges (10?11?5 ? 10?8, 5 ? 10?8?10?4, and 10?4?1 g) are used. The parametric equations were developed with the aid of a complex method of calculating ice-particle growth. Two approaches to using the parametric equations in a simulation resembling a natural cloud situation are described. One method breaks the ice-particle spectrum into three components, the sizes of each being monitored. The other assumes a size distribution that can be characterized by a ?growth-median? size, so that only one size need be monitored to describe the rate of growth. The parametric method is compared with more complicated methods in a simulated cloud environment, and the results are regarded as satisfactory.
    publisherAmerican Meteorological Society
    titleParameterization of Ice Growth for Numerical Calculations of Cloud Dynamics
    typeJournal Paper
    journal volume100
    journal issue6
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1972)100<0417:POIGFN>2.3.CO;2
    journal fristpage417
    journal lastpage423
    treeMonthly Weather Review:;1972:;volume( 100 ):;issue: 006
    contenttypeFulltext
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