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    Measurement of Raindrop Size Distributions Using a Small Doppler Radar

    Source: Journal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 002::page 255
    Author:
    Sheppard, Brian E.
    DOI: 10.1175/1520-0426(1990)007<0255:MORSDU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A small X-band bistatic Doppler radar originally developed for use in automated weather stations as a Precipitation Occurrence Sensor System (POSS) can also measure real time raindrop size distributions. In contrast to large-scale pulsed Doppler radars this system is continuous wave and the measurement volume is relatively small. The drop size distribution is retrieved from the Doppler power spectrum by using an iterative inversion method. The sampling requirements for a representative average power spectrum are estimated. The effect of winds on the measurement is discussed. The POSS measures rates that are consistent with conventional gauges assuming a 6 dB transmission loss due to water on the radomes. Average drop size distributions measured in stratiform rain are typically negative exponential for diameters greater than 0.7 mm. One-minute averages in rain showers show the multimodal character of the distribution.
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      Measurement of Raindrop Size Distributions Using a Small Doppler Radar

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4196955
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    contributor authorSheppard, Brian E.
    date accessioned2017-06-09T15:55:09Z
    date available2017-06-09T15:55:09Z
    date copyright1990/04/01
    date issued1990
    identifier issn0739-0572
    identifier otherams-567.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4196955
    description abstractA small X-band bistatic Doppler radar originally developed for use in automated weather stations as a Precipitation Occurrence Sensor System (POSS) can also measure real time raindrop size distributions. In contrast to large-scale pulsed Doppler radars this system is continuous wave and the measurement volume is relatively small. The drop size distribution is retrieved from the Doppler power spectrum by using an iterative inversion method. The sampling requirements for a representative average power spectrum are estimated. The effect of winds on the measurement is discussed. The POSS measures rates that are consistent with conventional gauges assuming a 6 dB transmission loss due to water on the radomes. Average drop size distributions measured in stratiform rain are typically negative exponential for diameters greater than 0.7 mm. One-minute averages in rain showers show the multimodal character of the distribution.
    publisherAmerican Meteorological Society
    titleMeasurement of Raindrop Size Distributions Using a Small Doppler Radar
    typeJournal Paper
    journal volume7
    journal issue2
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1990)007<0255:MORSDU>2.0.CO;2
    journal fristpage255
    journal lastpage268
    treeJournal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 002
    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
    yabeshDSpacePersian