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        <datestamp>2023-07-11</datestamp>
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          <dc:contributor>Robert Wilhelmson</dc:contributor>
          <dc:creator>Romine, Glen Scott</dc:creator>
          <dc:date>2015-09-28T14:52:23Z</dc:date>
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          <dc:date>10000-01-01</dc:date>
          <dc:date>2008</dc:date>
          <dc:date>2008</dc:date>
          <dc:description>A detailed examination of the case study led to new insight into polarimetric field evolution associated with a significantly tornadic supercell thunderstorm. This included the identification of a specific differential phase foot and differential reflectivity shield as well as the first documentation focused on the relationship between polarimetric field evolution relative to surface gust front behavior. A strong but compact cold pool was found on the upshear side of the storm. However, an intriguing discovery was the lack of significant cooling at the surface within the forward flank downdraft region of the storm. Instead, there was an elevated cold pool along the forward storm flank that rested on a capping inversion layer. Comparison of the retrieved atmospheric state variables between the simple and advanced microphysical representation showed significant differences in spatial and temporal evolution, yet retrieved cold pool characteristics were qualitatively quite similar to one another and observations. This is related to the similar treatment of evaporation between the two microphysical schemes along the upshear side of the storm.</dc:description>
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  Previous issue date: 2008</dc:description>
          <dc:description>Embargo set by: Seth Robbins for item 87256
Lift date: Forever
Reason: Restricted to the U of I community idenfinitely during batch ingest of legacy ETDs</dc:description>
          <dc:description>Restricted to the U of I community idenfinitely during batch ingest of legacy ETDs</dc:description>
          <dc:description>U of I Only</dc:description>
          <dc:description>250 p.</dc:description>
          <dc:description>Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 2008.</dc:description>
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          <dc:identifier>(MiAaPQ)AAI3314874</dc:identifier>
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          <dc:subject>Atmospheric Sciences</dc:subject>
          <dc:title>Improving Storm-Scale Analyses of Convection via Assimilation of Polarimetric Radar Observations</dc:title>
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            <grantor>University of Illinois at Urbana-Champaign</grantor>
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