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    A Three-Dimensional Cloud Chemistry Model

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 005::page 652
    Author:
    Tremblay, Andre
    ,
    Leighton, Henry
    DOI: 10.1175/1520-0450(1986)025<0652:ATDCCM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A cloud chemistry model is formulated in term of continuity equations for chemical species in the aqueous and aqueous phases within the cloud. The model includes scavenging of SO2, HNO3, HN3, H2O3, and sulphate aerosol particles. Calculations have been performed within the framework of a three-dimensional convective cloud model. The results are compared with aircraft measurements of cloud water chemistry.
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      A Three-Dimensional Cloud Chemistry Model

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4146175
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    contributor authorTremblay, Andre
    contributor authorLeighton, Henry
    date accessioned2017-06-09T14:01:07Z
    date available2017-06-09T14:01:07Z
    date copyright1986/05/01
    date issued1986
    identifier issn0733-3021
    identifier otherams-10997.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146175
    description abstractA cloud chemistry model is formulated in term of continuity equations for chemical species in the aqueous and aqueous phases within the cloud. The model includes scavenging of SO2, HNO3, HN3, H2O3, and sulphate aerosol particles. Calculations have been performed within the framework of a three-dimensional convective cloud model. The results are compared with aircraft measurements of cloud water chemistry.
    publisherAmerican Meteorological Society
    titleA Three-Dimensional Cloud Chemistry Model
    typeJournal Paper
    journal volume25
    journal issue5
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1986)025<0652:ATDCCM>2.0.CO;2
    journal fristpage652
    journal lastpage671
    treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 005
    contenttypeFulltext
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