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    Severe Thunderstorm and Tornado Warnings at Raleigh, North Carolina

    Source: Bulletin of the American Meteorological Society:;1997:;volume( 078 ):;issue: 011::page 2559
    Author:
    Hoium, Debra K.
    ,
    Riordan, Allen J.
    ,
    Monahan, John
    ,
    Keeter, Kermit K.
    DOI: 10.1175/1520-0477(1997)078<2559:STATWA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The National Weather Service issues public warnings for severe thunderstorms and tornadoes when these storms appear imminent. A study of the warning process was conducted at the National Weather Service Forecast Office at Raleigh, North Carolina, from 1994 through 1996. The purpose of the study was to examine the decision process by documenting the types of information leading to decisions to warn or not to warn and by describing the sequence and timing of events in the development of warnings. It was found that the evolution of warnings followed a logical sequence beginning with storm monitoring and proceeding with increasingly focused activity. For simplicity, information input to the process was categorized as one of three types: ground truth, radar reflectivity, or radar velocity. Reflectivity, velocity, and ground truth were all equally likely to initiate the investigation process. This investigation took an average of 7 min, after which either a decision was made not to warn or new information triggered the warning. Decisions not to issue warnings were based more on ground truth and reflectivity than radar velocity products. Warnings with investigations of more than 2 min were more likely to be triggered by radar reflectivity, than by velocity or ground truth. Warnings with a shorter investigation time, defined here as ?immediate trigger warnings,? were less frequently based on velocity products and more on ground truth information. Once the decision was made to warn, it took an average of 2.1 min to prepare the warning text. In 85% of cases when warnings were issued, at least one contact was made to emergency management officials or storm spotters in the warned county. Reports of severe weather were usually received soon after the warning was transmitted?almost half of these within 30 min after issue. A total of 68% were received during the severe weather episode, but some of these storm reports later proved false according to Storm Data. Even though the WSR-88D is a sophisticated tool, ground truth information was found to be a vital part of the warning process. However, the data did not indicate that population density was statistically correlated either with the number of warnings issued or the verification rate.
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      Severe Thunderstorm and Tornado Warnings at Raleigh, North Carolina

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    contributor authorHoium, Debra K.
    contributor authorRiordan, Allen J.
    contributor authorMonahan, John
    contributor authorKeeter, Kermit K.
    date accessioned2017-06-09T14:42:01Z
    date available2017-06-09T14:42:01Z
    date copyright1997/11/01
    date issued1997
    identifier issn0003-0007
    identifier otherams-24765.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161473
    description abstractThe National Weather Service issues public warnings for severe thunderstorms and tornadoes when these storms appear imminent. A study of the warning process was conducted at the National Weather Service Forecast Office at Raleigh, North Carolina, from 1994 through 1996. The purpose of the study was to examine the decision process by documenting the types of information leading to decisions to warn or not to warn and by describing the sequence and timing of events in the development of warnings. It was found that the evolution of warnings followed a logical sequence beginning with storm monitoring and proceeding with increasingly focused activity. For simplicity, information input to the process was categorized as one of three types: ground truth, radar reflectivity, or radar velocity. Reflectivity, velocity, and ground truth were all equally likely to initiate the investigation process. This investigation took an average of 7 min, after which either a decision was made not to warn or new information triggered the warning. Decisions not to issue warnings were based more on ground truth and reflectivity than radar velocity products. Warnings with investigations of more than 2 min were more likely to be triggered by radar reflectivity, than by velocity or ground truth. Warnings with a shorter investigation time, defined here as ?immediate trigger warnings,? were less frequently based on velocity products and more on ground truth information. Once the decision was made to warn, it took an average of 2.1 min to prepare the warning text. In 85% of cases when warnings were issued, at least one contact was made to emergency management officials or storm spotters in the warned county. Reports of severe weather were usually received soon after the warning was transmitted?almost half of these within 30 min after issue. A total of 68% were received during the severe weather episode, but some of these storm reports later proved false according to Storm Data. Even though the WSR-88D is a sophisticated tool, ground truth information was found to be a vital part of the warning process. However, the data did not indicate that population density was statistically correlated either with the number of warnings issued or the verification rate.
    publisherAmerican Meteorological Society
    titleSevere Thunderstorm and Tornado Warnings at Raleigh, North Carolina
    typeJournal Paper
    journal volume78
    journal issue11
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1997)078<2559:STATWA>2.0.CO;2
    journal fristpage2559
    journal lastpage2575
    treeBulletin of the American Meteorological Society:;1997:;volume( 078 ):;issue: 011
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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