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        <identifier>oai:www.ideals.illinois.edu:2142/69231</identifier>
        <datestamp>2023-07-11</datestamp>
        <setSpec>col_2142_5131</setSpec>
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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:creator>Weiland, Richard Mark</dc:creator>
          <dc:date>2014-12-15T19:04:18Z</dc:date>
          <dc:date>2014-12-15T19:04:18Z</dc:date>
          <dc:date>10000-01-01</dc:date>
          <dc:date>1982</dc:date>
          <dc:date>1982</dc:date>
          <dc:description>The development and first observations of the partial-reflection drifts experiment at Urbana, Illinois (40(DEGREES)N) are described. The winds data from the drifts experiment are compared with electron concentration data obtained by the differential-absorption technique to study the possible meteorological causes of the winter anomaly in the mesosphere at midlatitudes. Winds data obtained by the meteor-radar experiment at Urbana are also compared with electron concentration data measured at Urbana. A significant correlation is shown in both cases between southward winds and increasing electron concentration measured at the same location during winter.</dc:description>
          <dc:description>The possibility of stratospheric/mesospheric coupling is investigated by comparing satellite-measured 0.4 mbar geopotential data with mesospheric electron concentration data. No significant coupling was observed.</dc:description>
          <dc:description>The winds measured at Saskatoon, Saskatchewan (52(DEGREES)N) are compared with the electron concentrations measured at Urbana in an effort to establish a transport path from the auroral zone to Urbana. No constant fixed relationship is shown, but significant correlations are shown for short segments of the winter. A significant coherence is observed at discrete frequencies during segments of the winter.</dc:description>
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8209642.pdf: 7065063 bytes, checksum: 6196729f0661d09b441dc78c113e4361 (MD5)
  Previous issue date: 1982</dc:description>
          <dc:description>Embargo set by: Seth Robbins for item 69397
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>240 p.</dc:description>
          <dc:description>Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1982.</dc:description>
          <dc:identifier>http://hdl.handle.net/2142/69231</dc:identifier>
          <dc:identifier>(UMI)AAI8209642</dc:identifier>
          <dc:subject>Physics, Atmospheric Science</dc:subject>
          <dc:title>Investigation of the Winds and Electron Concentration Variability in the D Region of the Ionosphere by the Partial-Reflection Radar Technique</dc:title>
          <dc:type>text</dc:type>
          <degree>
            <department>Electrical Engineering</department>
            <discipline>Electrical Engineering</discipline>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Dissertation</level>
            <name>Ph.D.</name>
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