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    Simulation of Diurnal Variation in a Stratocumulus-capped Marine Boundary Layer during FIRE

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 012::page 3291
    Author:
    Duynkerke, Peter G.
    ,
    Hignett, Phillip
    DOI: 10.1175/1520-0493(1993)121<3291:SODVIA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A model simulation is presented of the diurnal cycle of a marine stratocumulus-capped boundary layer. The model results are compared with observations obtained during the 1987 First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment marine stratocumulus project, made from San Nicolas Island, off the coast of California. Both the simulation and the observations show a marked diurnal variation in cloud properties, as a result of the decoupling of the boundary layer into a separate cloud and a subcloud layer. In the model simulation the decoupling is caused by the absorption of the solar radiation in the cloud layer.
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      Simulation of Diurnal Variation in a Stratocumulus-capped Marine Boundary Layer during FIRE

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4203185
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    • Monthly Weather Review

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    contributor authorDuynkerke, Peter G.
    contributor authorHignett, Phillip
    date accessioned2017-06-09T16:09:42Z
    date available2017-06-09T16:09:42Z
    date copyright1993/12/01
    date issued1993
    identifier issn0027-0644
    identifier otherams-62307.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203185
    description abstractA model simulation is presented of the diurnal cycle of a marine stratocumulus-capped boundary layer. The model results are compared with observations obtained during the 1987 First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment marine stratocumulus project, made from San Nicolas Island, off the coast of California. Both the simulation and the observations show a marked diurnal variation in cloud properties, as a result of the decoupling of the boundary layer into a separate cloud and a subcloud layer. In the model simulation the decoupling is caused by the absorption of the solar radiation in the cloud layer.
    publisherAmerican Meteorological Society
    titleSimulation of Diurnal Variation in a Stratocumulus-capped Marine Boundary Layer during FIRE
    typeJournal Paper
    journal volume121
    journal issue12
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1993)121<3291:SODVIA>2.0.CO;2
    journal fristpage3291
    journal lastpage3300
    treeMonthly Weather Review:;1993:;volume( 121 ):;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
    yabeshDSpacePersian