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    Evaporative and Radiative Cooling in POST Stratocumulus

    Source: Journal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 010::page 3877
    Author:
    Gerber, H.
    ,
    Malinowski, Szymon P.
    ,
    Jonsson, Haflidi
    DOI: 10.1175/JAS-D-16-0023.1
    Publisher: American Meteorological Society
    Abstract: uoyancy reversal by evaporative cooling in entrainment holes has a minimal influence on stratocumulus (Sc) observed during the Physics of Stratocumulus Top (POST) aircraft field study held off the California coast in 2008. High-resolution temperature and microphysics measurements show only small differences for Sc with and without buoyancy reversal predicted by mixing fraction analysis that relates mixtures of cloudy air and free-atmospheric air to buoyancies of the mixtures. The reduction of LWC due to evaporation in the holes is a small percentage (average ~12%) of liquid water diluted in the Sc by entrainment from the entrainment interface layer (EIL) located above unbroken cloud top where most mixing, evaporation, and reduction of the large buoyancy jump between the cloud and free atmosphere occur. Entrainment is dominated by radiative cooling at cloud top.
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      Evaporative and Radiative Cooling in POST Stratocumulus

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4220117
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    contributor authorGerber, H.
    contributor authorMalinowski, Szymon P.
    contributor authorJonsson, Haflidi
    date accessioned2017-06-09T16:59:31Z
    date available2017-06-09T16:59:31Z
    date copyright2016/10/01
    date issued2016
    identifier issn0022-4928
    identifier otherams-77547.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4220117
    description abstractuoyancy reversal by evaporative cooling in entrainment holes has a minimal influence on stratocumulus (Sc) observed during the Physics of Stratocumulus Top (POST) aircraft field study held off the California coast in 2008. High-resolution temperature and microphysics measurements show only small differences for Sc with and without buoyancy reversal predicted by mixing fraction analysis that relates mixtures of cloudy air and free-atmospheric air to buoyancies of the mixtures. The reduction of LWC due to evaporation in the holes is a small percentage (average ~12%) of liquid water diluted in the Sc by entrainment from the entrainment interface layer (EIL) located above unbroken cloud top where most mixing, evaporation, and reduction of the large buoyancy jump between the cloud and free atmosphere occur. Entrainment is dominated by radiative cooling at cloud top.
    publisherAmerican Meteorological Society
    titleEvaporative and Radiative Cooling in POST Stratocumulus
    typeJournal Paper
    journal volume73
    journal issue10
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-D-16-0023.1
    journal fristpage3877
    journal lastpage3884
    treeJournal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 010
    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