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    Influences of the Local Environment on Supercell Cloud-to-Ground Lightning, Radar Characteristics, and Severe Weather on 2 June 1995

    Source: Monthly Weather Review:;2002:;volume( 130 ):;issue: 010::page 2349
    Author:
    Gilmore, Matthew S.
    ,
    Wicker, Louis J.
    DOI: 10.1175/1520-0493(2002)130<2349:IOTLEO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Radar, cloud-to-ground (CG) lightning characteristics, and storm reports were documented for 20 long-lived supercell thunderstorms that occurred during a 6-h period in the west Texas Panhandle on 2?3 June 1995. These thunderstorms occurred in proximity to a preexisting mesoscale outflow boundary. Storms that remained on the warm side of the mesoscale outflow boundary and storms that formed directly on the boundary tended to produce weaker low-level rotation, lower maximum heights for the 40-dBZ echo top, and had the largest negative CG flash rates. The largest negative flash rate was produced as each storm was gradually weakening. In contrast, out of 11 boundary-crossing storms, several important radar-based measurands increased unambiguously after storms crossed the boundary: 40-dBZ echo-top height in 5 cases, radar reflectivity above the environmental freezing level in 6 cases, and low-level mesocyclone strength in 9 cases. Trends of the first two measurands were ambiguous for 4 of 11 cases affected by a ±15 min estimated boundary-position uncertainty. Five out of 11 storms dramatically increased their positive flash rate within 60 min after crossing the outflow boundary. These large positive flash rates were associated with descending reflectivity cores that were larger in magnitude and areal extent compared to other storms in this study. The local mesoscale environment and its horizontal variations of 0?3-km vertical wind profile, CAPE below the in-cloud freezing level, and boundary layer mixing ratio appeared to greatly influence storm structure and evolution. The observed environmental variations are hypothesized to support changes in charge structure that might lead to the observed changes in flash rate and polarity.
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      Influences of the Local Environment on Supercell Cloud-to-Ground Lightning, Radar Characteristics, and Severe Weather on 2 June 1995

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4205076
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    • Monthly Weather Review

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    contributor authorGilmore, Matthew S.
    contributor authorWicker, Louis J.
    date accessioned2017-06-09T16:14:36Z
    date available2017-06-09T16:14:36Z
    date copyright2002/10/01
    date issued2002
    identifier issn0027-0644
    identifier otherams-64009.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4205076
    description abstractRadar, cloud-to-ground (CG) lightning characteristics, and storm reports were documented for 20 long-lived supercell thunderstorms that occurred during a 6-h period in the west Texas Panhandle on 2?3 June 1995. These thunderstorms occurred in proximity to a preexisting mesoscale outflow boundary. Storms that remained on the warm side of the mesoscale outflow boundary and storms that formed directly on the boundary tended to produce weaker low-level rotation, lower maximum heights for the 40-dBZ echo top, and had the largest negative CG flash rates. The largest negative flash rate was produced as each storm was gradually weakening. In contrast, out of 11 boundary-crossing storms, several important radar-based measurands increased unambiguously after storms crossed the boundary: 40-dBZ echo-top height in 5 cases, radar reflectivity above the environmental freezing level in 6 cases, and low-level mesocyclone strength in 9 cases. Trends of the first two measurands were ambiguous for 4 of 11 cases affected by a ±15 min estimated boundary-position uncertainty. Five out of 11 storms dramatically increased their positive flash rate within 60 min after crossing the outflow boundary. These large positive flash rates were associated with descending reflectivity cores that were larger in magnitude and areal extent compared to other storms in this study. The local mesoscale environment and its horizontal variations of 0?3-km vertical wind profile, CAPE below the in-cloud freezing level, and boundary layer mixing ratio appeared to greatly influence storm structure and evolution. The observed environmental variations are hypothesized to support changes in charge structure that might lead to the observed changes in flash rate and polarity.
    publisherAmerican Meteorological Society
    titleInfluences of the Local Environment on Supercell Cloud-to-Ground Lightning, Radar Characteristics, and Severe Weather on 2 June 1995
    typeJournal Paper
    journal volume130
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(2002)130<2349:IOTLEO>2.0.CO;2
    journal fristpage2349
    journal lastpage2372
    treeMonthly Weather Review:;2002:;volume( 130 ):;issue: 010
    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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