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    Buoyant Forcing within the Marine Stratocumulus-topped Boundary Layer

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 016::page 2759
    Author:
    Moyer, Kerry A.
    ,
    Young, George S.
    DOI: 10.1175/1520-0469(1993)050<2759:BFWTMS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A marine stratocumulus experiment was conducted off the coast of southern California during June and July 1987 as part of the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE). This investigation addresses the FIRE goal of enhancing our understanding of the buoyant production/destruction of turbulent kinetic energy within the marine stratocumulus-topped boundary layer through an analysis of the vertical profiles of buoyancy flux collected by the NCAR Electra aircraft. The FIRE boundary layers were observed to span the range of buoyant forcing possibilities from nearly pure surface-forced convection through nearly pure cloud top-forced convection.
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      Buoyant Forcing within the Marine Stratocumulus-topped Boundary Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157299
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    • Journal of the Atmospheric Sciences

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    contributor authorMoyer, Kerry A.
    contributor authorYoung, George S.
    date accessioned2017-06-09T14:31:43Z
    date available2017-06-09T14:31:43Z
    date copyright1993/08/01
    date issued1993
    identifier issn0022-4928
    identifier otherams-21007.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157299
    description abstractA marine stratocumulus experiment was conducted off the coast of southern California during June and July 1987 as part of the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment (FIRE). This investigation addresses the FIRE goal of enhancing our understanding of the buoyant production/destruction of turbulent kinetic energy within the marine stratocumulus-topped boundary layer through an analysis of the vertical profiles of buoyancy flux collected by the NCAR Electra aircraft. The FIRE boundary layers were observed to span the range of buoyant forcing possibilities from nearly pure surface-forced convection through nearly pure cloud top-forced convection.
    publisherAmerican Meteorological Society
    titleBuoyant Forcing within the Marine Stratocumulus-topped Boundary Layer
    typeJournal Paper
    journal volume50
    journal issue16
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1993)050<2759:BFWTMS>2.0.CO;2
    journal fristpage2759
    journal lastpage2771
    treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 016
    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