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    Vertically Pointing Airborne Doppler Radar Observations of Kelvin–Helmholtz Billows

    Source: Monthly Weather Review:;2009:;volume( 138 ):;issue: 003::page 982
    Author:
    Geerts, Bart
    ,
    Miao, Qun
    DOI: 10.1175/2009MWR3212.1
    Publisher: American Meteorological Society
    Abstract: A train of Kelvin?Helmholtz billows in a deep stratiform cloud over a mountain range is documented using data from a high-resolution vertically pointing airborne Doppler radar. The billows had a spacing of 2?2.5 km and a small aspect ratio. The formation and decay of the billows appear to be related to flow acceleration over a mountain.
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      Vertically Pointing Airborne Doppler Radar Observations of Kelvin–Helmholtz Billows

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4211389
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    contributor authorGeerts, Bart
    contributor authorMiao, Qun
    date accessioned2017-06-09T16:32:35Z
    date available2017-06-09T16:32:35Z
    date copyright2010/03/01
    date issued2009
    identifier issn0027-0644
    identifier otherams-69692.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211389
    description abstractA train of Kelvin?Helmholtz billows in a deep stratiform cloud over a mountain range is documented using data from a high-resolution vertically pointing airborne Doppler radar. The billows had a spacing of 2?2.5 km and a small aspect ratio. The formation and decay of the billows appear to be related to flow acceleration over a mountain.
    publisherAmerican Meteorological Society
    titleVertically Pointing Airborne Doppler Radar Observations of Kelvin–Helmholtz Billows
    typeJournal Paper
    journal volume138
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/2009MWR3212.1
    journal fristpage982
    journal lastpage986
    treeMonthly Weather Review:;2009:;volume( 138 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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