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    The Environment of Fast- and Slow-Moving Tropical Mesoscale Convective Cloud Lines

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 009::page 1782
    Author:
    Barnes, G. M.
    ,
    Sieckman, K.
    DOI: 10.1175/1520-0493(1984)112<1782:TEOFAS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Rawinsonde data from GATE are composited to examine the environmental similarities and differences between fast-moving (line speed VL > 7 m s?1) and slow-moving VL < 3 m s?1) mesoscale convective cloud lines. Thermodynamic structures for the two types of line are similar with respect to the mixed-layer values of ?e and convective available potential energy, but the fast-moving lines have a more pronounced minimum in ?e at ?700 mb. Kinematic structure shows that the vertical shows of the horizontal wind is normal to the leading edge of convention in the fast-moving convective lines but parallel to the leading edge of the slow-moving cloud lines. The results suggest that the type of line (fast versus slow) which forms may be affected by the initial environmental conditions.
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      The Environment of Fast- and Slow-Moving Tropical Mesoscale Convective Cloud Lines

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4201189
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    contributor authorBarnes, G. M.
    contributor authorSieckman, K.
    date accessioned2017-06-09T16:05:00Z
    date available2017-06-09T16:05:00Z
    date copyright1984/09/01
    date issued1984
    identifier issn0027-0644
    identifier otherams-60511.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201189
    description abstractRawinsonde data from GATE are composited to examine the environmental similarities and differences between fast-moving (line speed VL > 7 m s?1) and slow-moving VL < 3 m s?1) mesoscale convective cloud lines. Thermodynamic structures for the two types of line are similar with respect to the mixed-layer values of ?e and convective available potential energy, but the fast-moving lines have a more pronounced minimum in ?e at ?700 mb. Kinematic structure shows that the vertical shows of the horizontal wind is normal to the leading edge of convention in the fast-moving convective lines but parallel to the leading edge of the slow-moving cloud lines. The results suggest that the type of line (fast versus slow) which forms may be affected by the initial environmental conditions.
    publisherAmerican Meteorological Society
    titleThe Environment of Fast- and Slow-Moving Tropical Mesoscale Convective Cloud Lines
    typeJournal Paper
    journal volume112
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1984)112<1782:TEOFAS>2.0.CO;2
    journal fristpage1782
    journal lastpage1794
    treeMonthly Weather Review:;1984:;volume( 112 ):;issue: 009
    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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