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    Structure and Evolution of Winter Cyclones in the Central United States and Their Effects on the Distribution of Precipitation. Part III: The Development of a Squall Line Associated with Weak Cold Frontogenesis Aloft

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 009::page 2641
    Author:
    Locatelli, John D.
    ,
    Martin, Jonathan E.
    ,
    Castle, Jeffrey A.
    ,
    Hobbs, Peter V.
    DOI: 10.1175/1520-0493(1995)123<2641:SAEOWC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: From 8 to 9 March 1992 cold frontogenesis aloft (CFA), which was associated with the development of a vigorous baroclinic wave, triggered a series of squall lines that produced large hail and several tornadoes as they moved across the central United States. The air lifted by the CFA, which produced the squall lines, was made potentially unstable as a result of the circulation associated with a surface drytrough. This study provides further support for the view that in winter and early spring CFA plays an important role in triggering severe weather in the central United States.
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      Structure and Evolution of Winter Cyclones in the Central United States and Their Effects on the Distribution of Precipitation. Part III: The Development of a Squall Line Associated with Weak Cold Frontogenesis Aloft

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4203496
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    • Monthly Weather Review

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    contributor authorLocatelli, John D.
    contributor authorMartin, Jonathan E.
    contributor authorCastle, Jeffrey A.
    contributor authorHobbs, Peter V.
    date accessioned2017-06-09T16:10:26Z
    date available2017-06-09T16:10:26Z
    date copyright1995/09/01
    date issued1995
    identifier issn0027-0644
    identifier otherams-62588.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203496
    description abstractFrom 8 to 9 March 1992 cold frontogenesis aloft (CFA), which was associated with the development of a vigorous baroclinic wave, triggered a series of squall lines that produced large hail and several tornadoes as they moved across the central United States. The air lifted by the CFA, which produced the squall lines, was made potentially unstable as a result of the circulation associated with a surface drytrough. This study provides further support for the view that in winter and early spring CFA plays an important role in triggering severe weather in the central United States.
    publisherAmerican Meteorological Society
    titleStructure and Evolution of Winter Cyclones in the Central United States and Their Effects on the Distribution of Precipitation. Part III: The Development of a Squall Line Associated with Weak Cold Frontogenesis Aloft
    typeJournal Paper
    journal volume123
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1995)123<2641:SAEOWC>2.0.CO;2
    journal fristpage2641
    journal lastpage2662
    treeMonthly Weather Review:;1995:;volume( 123 ):;issue: 009
    contenttypeFulltext
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