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    Improvements of an Ice-Phase Microphysics Parameterization for Use in Numerical Simulations of Tropical Convection

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 001::page 281
    Author:
    Krueger, Steven K.
    ,
    Fu, Qiang
    ,
    Liou, K. N.
    ,
    Chin, Hung-Neng S.
    DOI: 10.1175/1520-0450-34.1.281
    Publisher: American Meteorological Society
    Abstract: It is important to properly simulate the extent and ice water content of tropical anvil clouds in numerical models that explicitly include cloud formation because of the significant effects that these clouds have on the radiation budget. For this reason, a commonly used bulk ice-phase microphysics parameterization was modified to more realistically simulate some of the microphysical processes that occur in tropical anvil clouds. Cloud ice growth by the Bergeron process and the associated formation of snow were revised. The characteristics of graupel were also modified in accord with a previous study. Numerical simulations of a tropical squall line demonstrate that the amount of cloud ice and the extent of anvil clouds are increased to more realistic values by the first two changes.
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      Improvements of an Ice-Phase Microphysics Parameterization for Use in Numerical Simulations of Tropical Convection

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4148900
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    • Journal of Applied Meteorology

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    contributor authorKrueger, Steven K.
    contributor authorFu, Qiang
    contributor authorLiou, K. N.
    contributor authorChin, Hung-Neng S.
    date accessioned2017-06-09T14:09:23Z
    date available2017-06-09T14:09:23Z
    date copyright1995/01/01
    date issued1995
    identifier issn0894-8763
    identifier otherams-13449.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148900
    description abstractIt is important to properly simulate the extent and ice water content of tropical anvil clouds in numerical models that explicitly include cloud formation because of the significant effects that these clouds have on the radiation budget. For this reason, a commonly used bulk ice-phase microphysics parameterization was modified to more realistically simulate some of the microphysical processes that occur in tropical anvil clouds. Cloud ice growth by the Bergeron process and the associated formation of snow were revised. The characteristics of graupel were also modified in accord with a previous study. Numerical simulations of a tropical squall line demonstrate that the amount of cloud ice and the extent of anvil clouds are increased to more realistic values by the first two changes.
    publisherAmerican Meteorological Society
    titleImprovements of an Ice-Phase Microphysics Parameterization for Use in Numerical Simulations of Tropical Convection
    typeJournal Paper
    journal volume34
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450-34.1.281
    journal fristpage281
    journal lastpage287
    treeJournal of Applied Meteorology:;1995:;volume( 034 ):;issue: 001
    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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