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    Dual-Frequency Radar Observations of Precipitation

    Source: Journal of Applied Meteorology:;1964:;volume( 003 ):;issue: 004::page 430
    Author:
    Walker, B.
    ,
    Lamberth, L. S.
    ,
    Stephens, J. J.
    DOI: 10.1175/1520-0450(1964)003<0430:DFROOP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An equal volume, dual-frequency radar system is used to obtain a quantitative characterization of a precipitation volume. The power back-scattered is related to the rainfall rate through the use of an assumed exponential drop-size distribution and the Mie radar cross section. A method is given whereby the relative consistency of a dual-frequency radar system is aided by calibration in the Rayleigh scattering region of a light rainshower. Discrepancies that occur in the observed rainfall rate are attributed to: 1) errors in the form of the assumed drop-size distribution, and 2) local vertical velocity and velocity divergence. Simultaneous observations of precipitation by the dual-frequency radar and raingages are shown for two rain situations.
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      Dual-Frequency Radar Observations of Precipitation

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4212890
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    • Journal of Applied Meteorology

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    contributor authorWalker, B.
    contributor authorLamberth, L. S.
    contributor authorStephens, J. J.
    date accessioned2017-06-09T16:37:09Z
    date available2017-06-09T16:37:09Z
    date copyright1964/08/01
    date issued1964
    identifier issn0021-8952
    identifier otherams-7104.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212890
    description abstractAn equal volume, dual-frequency radar system is used to obtain a quantitative characterization of a precipitation volume. The power back-scattered is related to the rainfall rate through the use of an assumed exponential drop-size distribution and the Mie radar cross section. A method is given whereby the relative consistency of a dual-frequency radar system is aided by calibration in the Rayleigh scattering region of a light rainshower. Discrepancies that occur in the observed rainfall rate are attributed to: 1) errors in the form of the assumed drop-size distribution, and 2) local vertical velocity and velocity divergence. Simultaneous observations of precipitation by the dual-frequency radar and raingages are shown for two rain situations.
    publisherAmerican Meteorological Society
    titleDual-Frequency Radar Observations of Precipitation
    typeJournal Paper
    journal volume3
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1964)003<0430:DFROOP>2.0.CO;2
    journal fristpage430
    journal lastpage438
    treeJournal of Applied Meteorology:;1964:;volume( 003 ):;issue: 004
    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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