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    Along-Valley Structure of Daytime Thermally Driven Flows in the Wipp Valley

    Source: Journal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 003::page 733
    Author:
    Rucker, Magdalena
    ,
    Banta, Robert M.
    ,
    Steyn, Douw G.
    DOI: 10.1175/2007JAMC1319.1
    Publisher: American Meteorological Society
    Abstract: High-resolution Doppler lidar observations obtained during the Mesoscale Alpine Program (MAP) 1999 field campaign are used to investigate the along-valley structure of daytime valley flows in the Wipp Valley, Austria. The observations show that under varying ambient conditions the valley flow increases in speed through a narrow section of the valley. Furthermore, the along-valley volume flux diverges along the valley segment under investigation, which suggests that the observed along-valley acceleration of the valley flow cannot be explained by the horizontal constriction of the valley sidewalls. It is hypothesized that the along-valley acceleration of the flow is caused by an intravalley change in the horizontal pressure gradient induced by differential heating rates of the valley atmosphere.
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      Along-Valley Structure of Daytime Thermally Driven Flows in the Wipp Valley

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4206477
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    contributor authorRucker, Magdalena
    contributor authorBanta, Robert M.
    contributor authorSteyn, Douw G.
    date accessioned2017-06-09T16:17:54Z
    date available2017-06-09T16:17:54Z
    date copyright2008/03/01
    date issued2008
    identifier issn1558-8424
    identifier otherams-65271.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206477
    description abstractHigh-resolution Doppler lidar observations obtained during the Mesoscale Alpine Program (MAP) 1999 field campaign are used to investigate the along-valley structure of daytime valley flows in the Wipp Valley, Austria. The observations show that under varying ambient conditions the valley flow increases in speed through a narrow section of the valley. Furthermore, the along-valley volume flux diverges along the valley segment under investigation, which suggests that the observed along-valley acceleration of the valley flow cannot be explained by the horizontal constriction of the valley sidewalls. It is hypothesized that the along-valley acceleration of the flow is caused by an intravalley change in the horizontal pressure gradient induced by differential heating rates of the valley atmosphere.
    publisherAmerican Meteorological Society
    titleAlong-Valley Structure of Daytime Thermally Driven Flows in the Wipp Valley
    typeJournal Paper
    journal volume47
    journal issue3
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/2007JAMC1319.1
    journal fristpage733
    journal lastpage751
    treeJournal of Applied Meteorology and Climatology:;2008:;volume( 047 ):;issue: 003
    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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