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    The Relationships between Network Lightning Surface and Hourly Observations of Thunderstorms

    Source: Monthly Weather Review:;1990:;volume( 118 ):;issue: 001::page 94
    Author:
    Reap, Ronald M.
    ,
    Orville, Richard E.
    DOI: 10.1175/1520-0493(1990)118<0094:TRBNLS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Relationships were established between lightning location data and surface hourly observations of thunderstorms for 132 stations in the northeastern United States. The relationships are based on statistics derived from 2 ? 2 contingency tables that were constructed for each station from a two-year sample of data for the 1985?86 warm seasons. To construct the tables, ground strike totals for the valid period of the hourly observations were accumulated for circular regions of varying radius (8?80 km) centered at each station. Separate contingency tables were constructed for each radius. For the entire sample, the fraction of observer reported thunderstorms that were also recorded by the lightning network was found to increase rapidly from 0.44 within a 16 km radius to 0.82 at 50 km, beyond which the rate of increase was much smaller with a maximum of 0.89 at 80 km. Values over 0.9 at 50 km were, however, typical for stations located well within the interior of the network. The continuing improvement in the relationships beyond the audible range of thunder (20 km) was most likely related to the errors biases, and uncertainty inherent in both sets of observations. The agreement between the network reports and station observations was slightly degraded by the possible reporting of intracloud flashes or weak ground strikes that were detected by the observer but not the network, especially at night. A significant increase was found in the ratio of the number of thunderstorms reported by observers at night to the number detected by the network, reflecting the improved ability of the observer to see lightning at night. In general, the lightning network was able to detect more thunderstorms than the observer beyond 17 and 26 km, respectively, for the daytime and nighttime samples. The improved detection capability for expanded regions about the station should have a significant impact on operational forecasts and warnings, especially with regard to aviation-related activities both en route and near airport terminals. Finally, improvements in the observer's ability to see lightning and hear thunder were found to be related to corresponding increases in flash density and peak signal strength.
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      The Relationships between Network Lightning Surface and Hourly Observations of Thunderstorms

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4202338
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    • Monthly Weather Review

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    contributor authorReap, Ronald M.
    contributor authorOrville, Richard E.
    date accessioned2017-06-09T16:07:38Z
    date available2017-06-09T16:07:38Z
    date copyright1990/01/01
    date issued1990
    identifier issn0027-0644
    identifier otherams-61545.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4202338
    description abstractRelationships were established between lightning location data and surface hourly observations of thunderstorms for 132 stations in the northeastern United States. The relationships are based on statistics derived from 2 ? 2 contingency tables that were constructed for each station from a two-year sample of data for the 1985?86 warm seasons. To construct the tables, ground strike totals for the valid period of the hourly observations were accumulated for circular regions of varying radius (8?80 km) centered at each station. Separate contingency tables were constructed for each radius. For the entire sample, the fraction of observer reported thunderstorms that were also recorded by the lightning network was found to increase rapidly from 0.44 within a 16 km radius to 0.82 at 50 km, beyond which the rate of increase was much smaller with a maximum of 0.89 at 80 km. Values over 0.9 at 50 km were, however, typical for stations located well within the interior of the network. The continuing improvement in the relationships beyond the audible range of thunder (20 km) was most likely related to the errors biases, and uncertainty inherent in both sets of observations. The agreement between the network reports and station observations was slightly degraded by the possible reporting of intracloud flashes or weak ground strikes that were detected by the observer but not the network, especially at night. A significant increase was found in the ratio of the number of thunderstorms reported by observers at night to the number detected by the network, reflecting the improved ability of the observer to see lightning at night. In general, the lightning network was able to detect more thunderstorms than the observer beyond 17 and 26 km, respectively, for the daytime and nighttime samples. The improved detection capability for expanded regions about the station should have a significant impact on operational forecasts and warnings, especially with regard to aviation-related activities both en route and near airport terminals. Finally, improvements in the observer's ability to see lightning and hear thunder were found to be related to corresponding increases in flash density and peak signal strength.
    publisherAmerican Meteorological Society
    titleThe Relationships between Network Lightning Surface and Hourly Observations of Thunderstorms
    typeJournal Paper
    journal volume118
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1990)118<0094:TRBNLS>2.0.CO;2
    journal fristpage94
    journal lastpage108
    treeMonthly Weather Review:;1990:;volume( 118 ):;issue: 001
    contenttypeFulltext
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