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    Charging of Ice Spheres Due to Collisions with Ice Crystals and the Electrification of Thunderstorms

    Source: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 003::page 560
    Author:
    Burrows, D. A.
    ,
    Hobbs, P. V.
    DOI: 10.1175/1520-0469(1969)026<0560:COISDT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The sources of the electrical charges acquired by ice spheres rotated through natural cloud or precipitation particles are considered. In general, the steady charge that a sphere receives in such experiments derives from collisions with particles in the air and from the electrical coupling of the sphere with the ground. The results of a number of experimental measurements on the charging of ice spheres whirled through natural snowfalls are described and analyzed. The average charge acquired by the ice sphere per ice particle collision was always negative over the range of temperatures investigated (?2 to ?8C) and reached a maximum negative value of about 1.5?10?4 esu at ?7C. It is pointed out that if natural hailstones falling through cumulonimbus clouds receive charges due to collisions with ice crystals which are similar in magnitude to those measured in these experiments, this mechanism would readily explain the electrification of thunderstorms.
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      Charging of Ice Spheres Due to Collisions with Ice Crystals and the Electrification of Thunderstorms

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4151308
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    contributor authorBurrows, D. A.
    contributor authorHobbs, P. V.
    date accessioned2017-06-09T14:14:57Z
    date available2017-06-09T14:14:57Z
    date copyright1969/05/01
    date issued1969
    identifier issn0022-4928
    identifier otherams-15616.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151308
    description abstractThe sources of the electrical charges acquired by ice spheres rotated through natural cloud or precipitation particles are considered. In general, the steady charge that a sphere receives in such experiments derives from collisions with particles in the air and from the electrical coupling of the sphere with the ground. The results of a number of experimental measurements on the charging of ice spheres whirled through natural snowfalls are described and analyzed. The average charge acquired by the ice sphere per ice particle collision was always negative over the range of temperatures investigated (?2 to ?8C) and reached a maximum negative value of about 1.5?10?4 esu at ?7C. It is pointed out that if natural hailstones falling through cumulonimbus clouds receive charges due to collisions with ice crystals which are similar in magnitude to those measured in these experiments, this mechanism would readily explain the electrification of thunderstorms.
    publisherAmerican Meteorological Society
    titleCharging of Ice Spheres Due to Collisions with Ice Crystals and the Electrification of Thunderstorms
    typeJournal Paper
    journal volume26
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1969)026<0560:COISDT>2.0.CO;2
    journal fristpage560
    journal lastpage565
    treeJournal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 003
    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