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    A Model of Rocky Mountain Lee Cyclogenesis

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 016::page 1510
    Author:
    Bannon, Peter R.
    DOI: 10.1175/1520-0469(1992)049<1510:AMORML>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A quasi-geostrophic model of cyclogenesis in the lee of the Rocky Mountains treats the cyclogenesis as a forecasting problem and uses an initial value approach. The model consists of the interaction of a growing baroclinic wave with an infinitely long mountain ridge. This transient interaction simulates many of the observed features of the phenomena, including the formation of a lee trough concurrent with the poleward displacement of the incident low on the upstream side of the mountain and the development of a lee cyclone equatorward of the unperturbed storm track. Despite this development, the low is weakened by its interaction with the orography.These results are explained physically and compared with those using a normal-mode approach to lee cyclogenesis.
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      A Model of Rocky Mountain Lee Cyclogenesis

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4157000
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    contributor authorBannon, Peter R.
    date accessioned2017-06-09T14:30:58Z
    date available2017-06-09T14:30:58Z
    date copyright1992/08/01
    date issued1992
    identifier issn0022-4928
    identifier otherams-20739.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157000
    description abstractA quasi-geostrophic model of cyclogenesis in the lee of the Rocky Mountains treats the cyclogenesis as a forecasting problem and uses an initial value approach. The model consists of the interaction of a growing baroclinic wave with an infinitely long mountain ridge. This transient interaction simulates many of the observed features of the phenomena, including the formation of a lee trough concurrent with the poleward displacement of the incident low on the upstream side of the mountain and the development of a lee cyclone equatorward of the unperturbed storm track. Despite this development, the low is weakened by its interaction with the orography.These results are explained physically and compared with those using a normal-mode approach to lee cyclogenesis.
    publisherAmerican Meteorological Society
    titleA Model of Rocky Mountain Lee Cyclogenesis
    typeJournal Paper
    journal volume49
    journal issue16
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1992)049<1510:AMORML>2.0.CO;2
    journal fristpage1510
    journal lastpage1522
    treeJournal of the Atmospheric Sciences:;1992:;Volume( 049 ):;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