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    Measurement of Rainfall Rates by Lidar

    Source: Journal of Applied Meteorology:;1974:;volume( 013 ):;issue: 007::page 800
    Author:
    Shipley, S. T.
    ,
    Eloranta, E. W.
    ,
    Weinman, J. A.
    DOI: 10.1175/1520-0450(1974)013<0800:MORRBL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Monostatic lidar is explored as a means for determining the rainfall rate over an extended atmospheric path with a spatial resolution comparable to that of rain gages. An empirical relationship is established between the optical extinction coefficient of rain ?r (km?1) and the rainfall rate R (mm hr?1). Correlation of lidar-derived rainfall extinction and gage rainfall rates at Madison gives ?r = 0.16 R0.74. The ?r-R relations obtained from the work of other authors compare well with this relationship. A lidar equation which accounts for the multiple scattering of light in rain is presented. A numerical procedure which derives estimates of ?r as a function of range from lidar returns is developed. Examples of lidar-derived rainfall rate range profiles in spatially inhomogeneous thunderstorms are given.
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      Measurement of Rainfall Rates by Lidar

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4231677
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    contributor authorShipley, S. T.
    contributor authorEloranta, E. W.
    contributor authorWeinman, J. A.
    date accessioned2017-06-09T17:36:20Z
    date available2017-06-09T17:36:20Z
    date copyright1974/10/01
    date issued1974
    identifier issn0021-8952
    identifier otherams-8795.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4231677
    description abstractMonostatic lidar is explored as a means for determining the rainfall rate over an extended atmospheric path with a spatial resolution comparable to that of rain gages. An empirical relationship is established between the optical extinction coefficient of rain ?r (km?1) and the rainfall rate R (mm hr?1). Correlation of lidar-derived rainfall extinction and gage rainfall rates at Madison gives ?r = 0.16 R0.74. The ?r-R relations obtained from the work of other authors compare well with this relationship. A lidar equation which accounts for the multiple scattering of light in rain is presented. A numerical procedure which derives estimates of ?r as a function of range from lidar returns is developed. Examples of lidar-derived rainfall rate range profiles in spatially inhomogeneous thunderstorms are given.
    publisherAmerican Meteorological Society
    titleMeasurement of Rainfall Rates by Lidar
    typeJournal Paper
    journal volume13
    journal issue7
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1974)013<0800:MORRBL>2.0.CO;2
    journal fristpage800
    journal lastpage807
    treeJournal of Applied Meteorology:;1974:;volume( 013 ):;issue: 007
    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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