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    Large Amplitude Lee Waves and Chinook Winds

    Source: Journal of Applied Meteorology:;1967:;volume( 006 ):;issue: 005::page 865
    Author:
    Beran, Donald W.
    DOI: 10.1175/1520-0450(1967)006<0865:LALWAC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Four types of chinook winds are described and features detectable in satellite pictures are shown. The hypothesis that large amplitude lee waves could be a possible driving mechanism for chinook winds is investigated for a case occurring in the Rocky Mountains during April 1963. It is shown that the stability of the surface inversion layer on the windward side of a mountain is related to the occurrence of chinook winds to the leeward side. This relationship leads to the speculation that chinook winds may undergo a quasi-diurnal fluctuation, in phase with the onset of the windward surface inversion.
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      Large Amplitude Lee Waves and Chinook Winds

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    contributor authorBeran, Donald W.
    date accessioned2017-06-09T16:52:14Z
    date available2017-06-09T16:52:14Z
    date copyright1967/10/01
    date issued1967
    identifier issn0021-8952
    identifier otherams-7564.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218000
    description abstractFour types of chinook winds are described and features detectable in satellite pictures are shown. The hypothesis that large amplitude lee waves could be a possible driving mechanism for chinook winds is investigated for a case occurring in the Rocky Mountains during April 1963. It is shown that the stability of the surface inversion layer on the windward side of a mountain is related to the occurrence of chinook winds to the leeward side. This relationship leads to the speculation that chinook winds may undergo a quasi-diurnal fluctuation, in phase with the onset of the windward surface inversion.
    publisherAmerican Meteorological Society
    titleLarge Amplitude Lee Waves and Chinook Winds
    typeJournal Paper
    journal volume6
    journal issue5
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1967)006<0865:LALWAC>2.0.CO;2
    journal fristpage865
    journal lastpage877
    treeJournal of Applied Meteorology:;1967:;volume( 006 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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