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    The Influence of Terrain on Rainfall Estimates from Radar Reflectivity and Specific Propagation Phase Observations

    Source: Journal of Atmospheric and Oceanic Technology:;1999:;volume( 016 ):;issue: 007::page 837
    Author:
    Vivekanandan, J.
    ,
    Yates, David N.
    ,
    Brandes, Edward A.
    DOI: 10.1175/1520-0426(1999)016<0837:TIOTOR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The effect of beam blockage on rainfall estimates derived from radar reflectivity and specific propagation phase was evaluated from measurements of a convective rainfall event from the National Center for Atmospheric Research?s S-band polarized (S-Pol) radar. This storm produced a flash flood in a mountainous watershed to the southwest of Denver, Colorado, and widespread rainfall over the plains. A beam blockage map of the region, based on a digital elevation model and characteristics of the S-Pol radiation pattern, was computed. Rain-rate estimates over both low and high beam-blockage areas were compared. Results supported the hypothesis that specific propagation phase?based quantitative precipitation estimates tend to be less influenced by terrain than reflectivity-based precipitation estimates are.
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      The Influence of Terrain on Rainfall Estimates from Radar Reflectivity and Specific Propagation Phase Observations

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4151179
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorVivekanandan, J.
    contributor authorYates, David N.
    contributor authorBrandes, Edward A.
    date accessioned2017-06-09T14:14:37Z
    date available2017-06-09T14:14:37Z
    date copyright1999/07/01
    date issued1999
    identifier issn0739-0572
    identifier otherams-1550.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151179
    description abstractThe effect of beam blockage on rainfall estimates derived from radar reflectivity and specific propagation phase was evaluated from measurements of a convective rainfall event from the National Center for Atmospheric Research?s S-band polarized (S-Pol) radar. This storm produced a flash flood in a mountainous watershed to the southwest of Denver, Colorado, and widespread rainfall over the plains. A beam blockage map of the region, based on a digital elevation model and characteristics of the S-Pol radiation pattern, was computed. Rain-rate estimates over both low and high beam-blockage areas were compared. Results supported the hypothesis that specific propagation phase?based quantitative precipitation estimates tend to be less influenced by terrain than reflectivity-based precipitation estimates are.
    publisherAmerican Meteorological Society
    titleThe Influence of Terrain on Rainfall Estimates from Radar Reflectivity and Specific Propagation Phase Observations
    typeJournal Paper
    journal volume16
    journal issue7
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1999)016<0837:TIOTOR>2.0.CO;2
    journal fristpage837
    journal lastpage845
    treeJournal of Atmospheric and Oceanic Technology:;1999:;volume( 016 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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