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        <datestamp>2023-07-11</datestamp>
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          <dc:date>2020-08-26T21:58:02Z</dc:date>
          <dc:contributor>Trapp, Robert</dc:contributor>
          <dc:creator>Chehak, Devin Andrew</dc:creator>
          <dc:date>2020-08-26T21:58:02Z</dc:date>
          <dc:date>2020-05-13</dc:date>
          <dc:date>2020-05</dc:date>
          <dc:description>The primary goal of this research was to quantify occurrence frequencies of the two main proposed mechanisms of tornadogenesis in quasi-linear convective systems (QLCSs), namely, tilting and stretching (T&amp;S) and HSI and stretching (H&amp;S). This research then sought to investigate differences and similarities between the characteristics of the T&amp;S- and H&amp;S- associated tornadoes and their supporting environments. A combined Doppler radar, tornado report, and environment dataset was compiled for this purpose. Lastly, this research aimed to quantify National Weather Service (NWS) warning performance for both mechanisms. 
From a strict consideration of only the first tornado generated by a QLCS during 2016-2018, 152 QLCS tornado cases were identified. Of these, 145 where determined to be the result of T&amp;S, and 7 where determined to be the result of H&amp;S, indicating that T&amp;S is far more likely to be the tornadogenesis mechanism of the first tornado in a QLCS. QLCS tornadoes tended to be focused in the southern U.S. during winter and spring and the northern U.S. during summer. Tornadogenesis through H&amp;S occurred relatively earlier in the year and earlier in the day, and resulted in relatively weaker tornadoes than did tornadogenesis through T&amp;S. Environmental analysis showed that H&amp;S environments had relatively lower values of CAPE and relatively higher values of low-level shear compared to T&amp;S. Analysis of NWS warnings showed that H&amp;S tornadoes had relatively lower tornado warning frequencies than did T&amp;S tornadoes, while having, on average, half the warning lead time. Finally, based on a consideration of pre-tornadic Doppler radar data, it was found that H&amp;S low-level circulations tended to form more rapidly than did T&amp;S low-level circulations, thus providing less potential lead time.</dc:description>
          <dc:description>Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2020-08-25 without embargo terms</dc:description>
          <dc:description>The student, Devin Chehak, accepted the attached license on 2020-05-11 at 13:46.</dc:description>
          <dc:description>The student, Devin Chehak, submitted this Thesis for approval on 2020-05-11 at 13:55.</dc:description>
          <dc:description>This Thesis was approved for publication on 2020-05-13 at 16:49.</dc:description>
          <dc:description>DSpace SAF Submission Ingestion Package generated from Vireo submission #15326 on 2020-08-25 at 17:13:57</dc:description>
          <dc:description>Made available in DSpace on 2020-08-26T21:58:02Z (GMT). No. of bitstreams: 2
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  Previous issue date: 2020-05-13</dc:description>
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          <dc:identifier>http://hdl.handle.net/2142/108035</dc:identifier>
          <dc:language>en</dc:language>
          <dc:rights>Copyright 2020 Devin Chehak</dc:rights>
          <dc:subject>Severe Weather, Tornado, QLCS, Squall Line, MCS</dc:subject>
          <dc:title>Analyses of quasi-linear convective system tornado characteristics, environments, and genesis mechanisms</dc:title>
          <dc:type>text</dc:type>
          <dc:type>Thesis</dc:type>
          <degree>
            <department>Atmospheric Sciences</department>
            <discipline>Atmospheric Sciences</discipline>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Thesis</level>
            <name>M.S.</name>
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