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    The Meteorological Parameterization of Specific Attenuation in Rain Viewed at Nadir

    Source: Journal of Applied Meteorology:;1994:;volume( 033 ):;issue: 008::page 1026
    Author:
    Jameson, A. R.
    DOI: 10.1175/1520-0450(1994)033<1026:TMPOSA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Polynomial expressions are presented for the parameterization of the specific attenuation in rain from 9 to 38 GHz that are applicable to a wide range of naturally occurring drop size distributions and for viewing angles close to nadir. Because the temperature T affects the specific attenuation at some frequencies, expressions for the polynomial coefficients as functions of T are also provided for ?10;deg;≤T≤30°C. The advantage of this parameterization is that even without a detailed specification of the drop size distribution, useful estimates of the specific attenuation are often possible given only two out of three parameters, namely, the rainfall rate R, the rainwater content W, or Dm (the mass-weighted mean drop diameter), particularly if the temperature is also specified.
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      The Meteorological Parameterization of Specific Attenuation in Rain Viewed at Nadir

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4147374
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    contributor authorJameson, A. R.
    date accessioned2017-06-09T14:04:59Z
    date available2017-06-09T14:04:59Z
    date copyright1994/08/01
    date issued1994
    identifier issn0894-8763
    identifier otherams-12075.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147374
    description abstractPolynomial expressions are presented for the parameterization of the specific attenuation in rain from 9 to 38 GHz that are applicable to a wide range of naturally occurring drop size distributions and for viewing angles close to nadir. Because the temperature T affects the specific attenuation at some frequencies, expressions for the polynomial coefficients as functions of T are also provided for ?10;deg;≤T≤30°C. The advantage of this parameterization is that even without a detailed specification of the drop size distribution, useful estimates of the specific attenuation are often possible given only two out of three parameters, namely, the rainfall rate R, the rainwater content W, or Dm (the mass-weighted mean drop diameter), particularly if the temperature is also specified.
    publisherAmerican Meteorological Society
    titleThe Meteorological Parameterization of Specific Attenuation in Rain Viewed at Nadir
    typeJournal Paper
    journal volume33
    journal issue8
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1994)033<1026:TMPOSA>2.0.CO;2
    journal fristpage1026
    journal lastpage1033
    treeJournal of Applied Meteorology:;1994:;volume( 033 ):;issue: 008
    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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