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    Experimental Determination of the Radar Cross Sections of Artificial Hailstones Containing Water

    Source: Journal of Applied Meteorology:;1965:;volume( 004 ):;issue: 006::page 723
    Author:
    Joss, Jürg
    ,
    Aufdermaur, Armin N.
    DOI: 10.1175/1520-0450(1965)004<0723:EDOTRC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The radar cross sections of particles grown in a hail tunnel (ice spheres with a spongy ice shell) and snow spheres dipped in water (spongy ice throughout) were measured at wavelengths of 3.21 cm, 4.67 cm, and 10 cm. The results were comparable and did not show obvious systematic differences either for the three wavelengths or for the two kinds of particles. The average normalized cross section versus α(α = πd/?, where d is the particle diameter and ? the wave-length) is given in the range of 0.4 < α < for liquid water contents of 0 per cent (frozen particles), 5, 10, 20, and 30 per cent. For α > 1, a water content of more than 10 per cent was sufficient to produce a mean cross section equivalent to that of an all-water sphere.
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      Experimental Determination of the Radar Cross Sections of Artificial Hailstones Containing Water

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4214845
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    contributor authorJoss, Jürg
    contributor authorAufdermaur, Armin N.
    date accessioned2017-06-09T16:42:48Z
    date available2017-06-09T16:42:48Z
    date copyright1965/12/01
    date issued1965
    identifier issn0021-8952
    identifier otherams-7280.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214845
    description abstractThe radar cross sections of particles grown in a hail tunnel (ice spheres with a spongy ice shell) and snow spheres dipped in water (spongy ice throughout) were measured at wavelengths of 3.21 cm, 4.67 cm, and 10 cm. The results were comparable and did not show obvious systematic differences either for the three wavelengths or for the two kinds of particles. The average normalized cross section versus α(α = πd/?, where d is the particle diameter and ? the wave-length) is given in the range of 0.4 < α < for liquid water contents of 0 per cent (frozen particles), 5, 10, 20, and 30 per cent. For α > 1, a water content of more than 10 per cent was sufficient to produce a mean cross section equivalent to that of an all-water sphere.
    publisherAmerican Meteorological Society
    titleExperimental Determination of the Radar Cross Sections of Artificial Hailstones Containing Water
    typeJournal Paper
    journal volume4
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1965)004<0723:EDOTRC>2.0.CO;2
    journal fristpage723
    journal lastpage726
    treeJournal of Applied Meteorology:;1965:;volume( 004 ):;issue: 006
    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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