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    ELECTRIC FIELD INTENSITY AT THE GROUND UNDER ACTIVE THUNDERSTORMS AND TORNADOES

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 003::page 269
    Author:
    Gunn, Ross
    DOI: 10.1175/1520-0469(1956)013<0269:EFIATG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Electric field intensity-measurements were made at eight stations near the 25 May 1955 tornado which devastated Udall, Kansas. Simultaneous records are reproduced, showing the electrical activity throughout the near passage of this tornado funnel. This storm systematically transferred or induced positive electrical charges on the ground which were neutralized in part or over-neutralized by lightning discharges. The records show that the storm was very active, and wide excursions in the magnitude and sign of the electric field were observed. At the time of passage of the funnel near one observing station, the surface electric-field fluctuations became relatively quite small and the electric field intensity approximated +40 volts/cm. There is little evidence suggesting that the electrical effects near the funnel differ basically from ordinary thunderstorm electrification.
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      ELECTRIC FIELD INTENSITY AT THE GROUND UNDER ACTIVE THUNDERSTORMS AND TORNADOES

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4149803
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    contributor authorGunn, Ross
    date accessioned2017-06-09T14:11:28Z
    date available2017-06-09T14:11:28Z
    date copyright1956/06/01
    date issued1956
    identifier issn0095-9634
    identifier otherams-14261.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149803
    description abstractElectric field intensity-measurements were made at eight stations near the 25 May 1955 tornado which devastated Udall, Kansas. Simultaneous records are reproduced, showing the electrical activity throughout the near passage of this tornado funnel. This storm systematically transferred or induced positive electrical charges on the ground which were neutralized in part or over-neutralized by lightning discharges. The records show that the storm was very active, and wide excursions in the magnitude and sign of the electric field were observed. At the time of passage of the funnel near one observing station, the surface electric-field fluctuations became relatively quite small and the electric field intensity approximated +40 volts/cm. There is little evidence suggesting that the electrical effects near the funnel differ basically from ordinary thunderstorm electrification.
    publisherAmerican Meteorological Society
    titleELECTRIC FIELD INTENSITY AT THE GROUND UNDER ACTIVE THUNDERSTORMS AND TORNADOES
    typeJournal Paper
    journal volume13
    journal issue3
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1956)013<0269:EFIATG>2.0.CO;2
    journal fristpage269
    journal lastpage273
    treeJournal of Meteorology:;1956:;volume( 013 ):;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
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