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    A Remote Sensing Method of Measuring Atmospheric Vapor Fluxes: Application to Winter Mountain Storms

    Source: Journal of Applied Meteorology:;1990:;volume( 029 ):;issue: 001::page 22
    Author:
    Uttal, T.
    ,
    Snider, J. B.
    ,
    Kropfli, R. A.
    ,
    Orr, B. W.
    DOI: 10.1175/1520-0450(1990)029<0022:ARSMOM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Vapor fluxes are calculated across a mountain barrier during two wintertime storms using a passive microwave radiometer and a Doppler radar. The vapor flux fields are shown to have complicated structures that are not detectable by conventional rawinsonde techniques. The vapor-flux fields show several major pulses which are compared to episodes of supercooled liquid water, riming, precipitation and synoptic weather patterns. It appears from this data that the presence of an enhanced vapor in the flux field is a necessary condition for precipitation, but not a sufficient condition. It is suggested that detailed measurements of the vapor flux field are imperative to the improved local forecasting of precipitation.
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      A Remote Sensing Method of Measuring Atmospheric Vapor Fluxes: Application to Winter Mountain Storms

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4146762
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    contributor authorUttal, T.
    contributor authorSnider, J. B.
    contributor authorKropfli, R. A.
    contributor authorOrr, B. W.
    date accessioned2017-06-09T14:02:58Z
    date available2017-06-09T14:02:58Z
    date copyright1990/01/01
    date issued1990
    identifier issn0894-8763
    identifier otherams-11524.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146762
    description abstractVapor fluxes are calculated across a mountain barrier during two wintertime storms using a passive microwave radiometer and a Doppler radar. The vapor flux fields are shown to have complicated structures that are not detectable by conventional rawinsonde techniques. The vapor-flux fields show several major pulses which are compared to episodes of supercooled liquid water, riming, precipitation and synoptic weather patterns. It appears from this data that the presence of an enhanced vapor in the flux field is a necessary condition for precipitation, but not a sufficient condition. It is suggested that detailed measurements of the vapor flux field are imperative to the improved local forecasting of precipitation.
    publisherAmerican Meteorological Society
    titleA Remote Sensing Method of Measuring Atmospheric Vapor Fluxes: Application to Winter Mountain Storms
    typeJournal Paper
    journal volume29
    journal issue1
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1990)029<0022:ARSMOM>2.0.CO;2
    journal fristpage22
    journal lastpage34
    treeJournal of Applied Meteorology:;1990:;volume( 029 ):;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
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