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        <identifier>oai:www.ideals.illinois.edu:2142/44134</identifier>
        <datestamp>2023-07-11</datestamp>
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        <thesis xmlns="http://www.ndltd.org/standards/metadata/etdms/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/" xsi:schemaLocation="http://www.ndltd.org/standards/metadata/etdms/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdms11.xsd http://purl.org/dc/elements/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdmsdc.xsd">
          <dc:contributor>Wilhelmson, Robert B.</dc:contributor>
          <dc:contributor>Jewett, Brian F.</dc:contributor>
          <dc:creator>Van Leer, Kevin</dc:creator>
          <dc:date>2013-05-24T21:51:48Z</dc:date>
          <dc:date>2013-05-24T21:51:48Z</dc:date>
          <dc:date>2013-05</dc:date>
          <dc:date>2013-05-24T21:51:48Z</dc:date>
          <dc:date>2013-05</dc:date>
          <dc:description>The relationship between storm mergers and tornado formation can result in local
conditions more favorable for rapid intensification of vertical vorticity at the surface than found
in the surrounding environment. Following the work of Lemon (1976) and Lee et al. (2006), this
study uses high-resolution WRF simulations to simulate and understand the significance of storm
mergers in subsequent intensification of the parent rotating updraft (mesocyclone) and tornadic
vortex in the 22 May 2011 Joplin, MO case. This case was noted for the rapid evolution of the
storm from tornado formation (tornadogenesis) to peak intensity in relation to the merging of
cells in the rear-flank region of the parent storm.
In an effort to identify the importance of the mergers in the tornadogenesis process, casestudy
WRF simulations are used to reproduce behavior observed in the event. An in-depth
qualitative and quantitative analysis of the relationships between internal storm dynamical
processes, such as precipitation loading and increased surface convergence, is performed. Three-dimensional
visualization is utilized to identify spatial and temporal relationships between stormscale
processes. Sensitivity tests, including the artificial removal or alteration of the merging
cells in the model, modify the storm evolution and allow the quantification of the mergers’
effects. This study pursued a goal of identifying storm scale processes resulting from storm
mergers that enhance, weaken or otherwise modulate tornado development in supercell storms.</dc:description>
          <dc:description>Item withdrawn by Mark Zulauf (zulauf@illinois.edu) on 2013-04-23T12:51:19Z
Item was in collections:
University of Illinois Theses &amp; Dissertations (ID: 1)
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          <dc:identifier>http://hdl.handle.net/2142/44134</dc:identifier>
          <dc:language>en</dc:language>
          <dc:rights>Copyright 2013 Kevin Van Leer</dc:rights>
          <dc:subject>Tornadoes</dc:subject>
          <dc:subject>Supercells</dc:subject>
          <dc:subject>Joplin</dc:subject>
          <dc:subject>Tornado Genesis</dc:subject>
          <dc:subject>Storm Mergers</dc:subject>
          <dc:subject>Severe Weather</dc:subject>
          <dc:title>Storm mergers and their role in tornado genesis during the 2011 Joplin storm</dc:title>
          <dc:type>text</dc:type>
          <degree>
            <department>Atmospheric Sciences</department>
            <departmentCode>1253</departmentCode>
            <discipline>Atmospheric Sciences</discipline>
            <disciplineCode>0334</disciplineCode>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Thesis</level>
            <name>M.S.</name>
            <program>MS:Atmospheric Sciences -UIUC</program>
            <programCode>10KS0334MS</programCode>
          </degree>
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