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    Anomalous Cloud-to-Ground Lightning in an F5-Tornado-Producing Supercell Thunderstorm on 28 August 1990

    Source: Bulletin of the American Meteorological Society:;1993:;volume( 074 ):;issue: 002::page 189
    Author:
    Seimon, Anton
    DOI: 10.1175/1520-0477(1993)074<0189:ACTGLI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: An F5 tornado that devastated Plainfield, Illinois, and environs on 28 August 1990, killing 29 people, is shown to be preduced by a thunderstorm characterized by highly anomalous could-to-ground (CG) lightning activity. Unlike typical summertime convective in which the majority of CG flashes lower negative charge to ground, the Plainfield storm produced predominantly positive-polarity CG flashes during development. Changes in storm structure revealed by radar imagery appear tied to distinct patterns in the CG flash parameters of polarity, flash frequency, first stroke peak current, flash multiplicity, and flash location relative to the parent cumulonimbus. The primary findings are 1) the anomalous predominance (91%) of positive-polarity CG flashes during development; 2) positive CG flashes anomalously occurring mainly within the region of the storm's radar reflectivity core; 3) the onset of a major downburst coinciding with a sudden increase in CG flash rate, from 4 to 17 flashes min?1, and positive percentage, from 91% to 100%; 4) a reduction in flash rate from 17 to 3 flashes min?1 in 3 min, coinciding with the rapid development of a front-flank mesocyclone; 5) a 20-min span of reduced CG activity (1?2 flashes min?1) coinciding with tornado formation and intensification; 6) the reversal in dominant CG flash polarity from positive to negative over the entire thunderstorm domain at the time of tornado touchdown, an occurrence previously undocumented in any other tornadic thunderstorm; 7) steadily weakening mean peak current values (from +100 to +38 kA) leading to the reversal, and steadily strengthening values (from ?20 to ?40 kA) following the reversal; and 8) the temporary clustering of all CG flashes within 10 km of the tornadic mesocyclone at maximum (F5) tornadic intensity. These findings suggest the possibility of a relationship between this tornadic thunderstorm's dynamics and electrical activity.
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      Anomalous Cloud-to-Ground Lightning in an F5-Tornado-Producing Supercell Thunderstorm on 28 August 1990

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4161117
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    contributor authorSeimon, Anton
    date accessioned2017-06-09T14:41:09Z
    date available2017-06-09T14:41:09Z
    date copyright1993/02/01
    date issued1993
    identifier issn0003-0007
    identifier otherams-24444.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161117
    description abstractAn F5 tornado that devastated Plainfield, Illinois, and environs on 28 August 1990, killing 29 people, is shown to be preduced by a thunderstorm characterized by highly anomalous could-to-ground (CG) lightning activity. Unlike typical summertime convective in which the majority of CG flashes lower negative charge to ground, the Plainfield storm produced predominantly positive-polarity CG flashes during development. Changes in storm structure revealed by radar imagery appear tied to distinct patterns in the CG flash parameters of polarity, flash frequency, first stroke peak current, flash multiplicity, and flash location relative to the parent cumulonimbus. The primary findings are 1) the anomalous predominance (91%) of positive-polarity CG flashes during development; 2) positive CG flashes anomalously occurring mainly within the region of the storm's radar reflectivity core; 3) the onset of a major downburst coinciding with a sudden increase in CG flash rate, from 4 to 17 flashes min?1, and positive percentage, from 91% to 100%; 4) a reduction in flash rate from 17 to 3 flashes min?1 in 3 min, coinciding with the rapid development of a front-flank mesocyclone; 5) a 20-min span of reduced CG activity (1?2 flashes min?1) coinciding with tornado formation and intensification; 6) the reversal in dominant CG flash polarity from positive to negative over the entire thunderstorm domain at the time of tornado touchdown, an occurrence previously undocumented in any other tornadic thunderstorm; 7) steadily weakening mean peak current values (from +100 to +38 kA) leading to the reversal, and steadily strengthening values (from ?20 to ?40 kA) following the reversal; and 8) the temporary clustering of all CG flashes within 10 km of the tornadic mesocyclone at maximum (F5) tornadic intensity. These findings suggest the possibility of a relationship between this tornadic thunderstorm's dynamics and electrical activity.
    publisherAmerican Meteorological Society
    titleAnomalous Cloud-to-Ground Lightning in an F5-Tornado-Producing Supercell Thunderstorm on 28 August 1990
    typeJournal Paper
    journal volume74
    journal issue2
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1993)074<0189:ACTGLI>2.0.CO;2
    journal fristpage189
    journal lastpage203
    treeBulletin of the American Meteorological Society:;1993:;volume( 074 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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