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    The Influence of the Earth's Rotation on Mountain Wave Drag

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 001::page 177
    Author:
    Smith, Ron
    DOI: 10.1175/1520-0469(1979)036<0177:TIOTER>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The two-dimensional flow of a stratified rotating fluid over a ridge is considered using the linear theory model of Queney (1947). A general expression for the wave drag, or alternatively the vertical flux of angular momentum, is derived. As progressively wider mountains are considered, the wave drag decreases and the flow becomes more nearly geostrophic. With typical wind speeds, many mountain ranges, for example, the Alps, Andes and the Scandinavian mountains, have a drag between 0.1 and 0.9 of their f = 0 drag value and thus fall into the mesoscale category where the Coriolis force is important but not dominant.
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      The Influence of the Earth's Rotation on Mountain Wave Drag

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4153553
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    contributor authorSmith, Ron
    date accessioned2017-06-09T14:20:35Z
    date available2017-06-09T14:20:35Z
    date copyright1979/01/01
    date issued1979
    identifier issn0022-4928
    identifier otherams-17637.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153553
    description abstractThe two-dimensional flow of a stratified rotating fluid over a ridge is considered using the linear theory model of Queney (1947). A general expression for the wave drag, or alternatively the vertical flux of angular momentum, is derived. As progressively wider mountains are considered, the wave drag decreases and the flow becomes more nearly geostrophic. With typical wind speeds, many mountain ranges, for example, the Alps, Andes and the Scandinavian mountains, have a drag between 0.1 and 0.9 of their f = 0 drag value and thus fall into the mesoscale category where the Coriolis force is important but not dominant.
    publisherAmerican Meteorological Society
    titleThe Influence of the Earth's Rotation on Mountain Wave Drag
    typeJournal Paper
    journal volume36
    journal issue1
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1979)036<0177:TIOTER>2.0.CO;2
    journal fristpage177
    journal lastpage180
    treeJournal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 001
    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