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    Imbalance in a Mesoscale Vortex within a Midlatitude, Continental Mesoscale Convective System

    Source: Journal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 014::page 1827
    Author:
    Knievel, Jason C.
    ,
    Nolan, David S.
    ,
    Kossin, James P.
    DOI: 10.1175/1520-0469(2004)061<1827:IIAMVW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The authors examine the degree of hydrostatic and gradient balances in a mesoscale convective vortex (MCV) in the stratiform region of a mesoscale convective system (MCS) that crossed Oklahoma on 1 August 1996. Results indicate that the MCV was partially unbalanced because the cool layer at the base of its core was too cool and too shallow to balance the tangential winds about the MCV's axis. The apparent imbalance may have been due to strong, unsteady forcing on the vortex; insufficient or unrepresentative data; approximations used in the analysis; or reasons that are unknown.
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      Imbalance in a Mesoscale Vortex within a Midlatitude, Continental Mesoscale Convective System

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4160089
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    • Journal of the Atmospheric Sciences

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    contributor authorKnievel, Jason C.
    contributor authorNolan, David S.
    contributor authorKossin, James P.
    date accessioned2017-06-09T14:38:51Z
    date available2017-06-09T14:38:51Z
    date copyright2004/07/01
    date issued2004
    identifier issn0022-4928
    identifier otherams-23519.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160089
    description abstractThe authors examine the degree of hydrostatic and gradient balances in a mesoscale convective vortex (MCV) in the stratiform region of a mesoscale convective system (MCS) that crossed Oklahoma on 1 August 1996. Results indicate that the MCV was partially unbalanced because the cool layer at the base of its core was too cool and too shallow to balance the tangential winds about the MCV's axis. The apparent imbalance may have been due to strong, unsteady forcing on the vortex; insufficient or unrepresentative data; approximations used in the analysis; or reasons that are unknown.
    publisherAmerican Meteorological Society
    titleImbalance in a Mesoscale Vortex within a Midlatitude, Continental Mesoscale Convective System
    typeJournal Paper
    journal volume61
    journal issue14
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2004)061<1827:IIAMVW>2.0.CO;2
    journal fristpage1827
    journal lastpage1832
    treeJournal of the Atmospheric Sciences:;2004:;Volume( 061 ):;issue: 014
    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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