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    A Model of Katabatic Winds

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 004::page 619
    Author:
    Manins, P. C.
    ,
    Sawford, B. L.
    DOI: 10.1175/1520-0469(1979)036<0619:AMOKW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new model of katabatic winds is presented. A hydraulic approach is employed in which the detailed vertical structure of the flow is replaced by a quiescent stably stratified environment and an equivalent flowing layer which is subject to sustained layer cooling, surface stress and interfacial entrainment. A scaling which contains most of the parametric behavior is found. It shows that interfacial entrainment is the dominating retardation mechanism of the flow and that surface stress may be relatively unimportant. Steady solutions are presented to show that katabatic winds are essentially supercritical on all practical slopes (slope angles >0.1°), and are affected by ambient stratification only at large distances. The model is in satisfactory quantitative agreement with the limited field data available.
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      A Model of Katabatic Winds

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153599
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    • Journal of the Atmospheric Sciences

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    contributor authorManins, P. C.
    contributor authorSawford, B. L.
    date accessioned2017-06-09T14:20:43Z
    date available2017-06-09T14:20:43Z
    date copyright1979/04/01
    date issued1979
    identifier issn0022-4928
    identifier otherams-17679.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153599
    description abstractA new model of katabatic winds is presented. A hydraulic approach is employed in which the detailed vertical structure of the flow is replaced by a quiescent stably stratified environment and an equivalent flowing layer which is subject to sustained layer cooling, surface stress and interfacial entrainment. A scaling which contains most of the parametric behavior is found. It shows that interfacial entrainment is the dominating retardation mechanism of the flow and that surface stress may be relatively unimportant. Steady solutions are presented to show that katabatic winds are essentially supercritical on all practical slopes (slope angles >0.1°), and are affected by ambient stratification only at large distances. The model is in satisfactory quantitative agreement with the limited field data available.
    publisherAmerican Meteorological Society
    titleA Model of Katabatic Winds
    typeJournal Paper
    journal volume36
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1979)036<0619:AMOKW>2.0.CO;2
    journal fristpage619
    journal lastpage630
    treeJournal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 004
    contenttypeFulltext
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    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian