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        <identifier>oai:www.ideals.illinois.edu:2142/85983</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>Walter Robinson</dc:contributor>
          <dc:creator>Werth, David William</dc:creator>
          <dc:date>2015-09-28T14:52:26Z</dc:date>
          <dc:date>2015-09-28T14:52:26Z</dc:date>
          <dc:date>10000-01-01</dc:date>
          <dc:date>1997</dc:date>
          <dc:date>1997</dc:date>
          <dc:description>"We have run a dry, nonlinear, primitive equation spectral model with no externally forced variability and with a realistic time mean state, and we have observed low frequency variability (LFV) in the stratosphere with timescales on the order of hundreds of days. Time lagged correlations have revealed that this variability is linked to LFV in the emission of longwaves from the troposphere. A set of linear model experiments is performed to determine the source of the stratospheric LFV. One set of runs reveal the lowest levels of the model troposphere as the source of most of the relevant forcing. A second set of runs forced with nonlinear terms has shown that the nonlinear interaction among shortwave, high-frequency eddy thermal anomalies in the troposphere has a ""beating"" effect which emits vertically propagating low-frequency longwaves. We also see that the eddies act in such a way as to offset the effects of linear temperature advection, allowing the thermal eddies to persist for long periods."</dc:description>
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  Previous issue date: 1997</dc:description>
          <dc:description>Embargo set by: Seth Robbins for item 87264
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>166 p.</dc:description>
          <dc:description>Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1997.</dc:description>
          <dc:identifier>http://hdl.handle.net/2142/85983</dc:identifier>
          <dc:identifier>(MiAaPQ)AAI9812806</dc:identifier>
          <dc:language>eng</dc:language>
          <dc:subject>Physics, Atmospheric Science</dc:subject>
          <dc:title>Low-Frequency Variability in the Stratosphere</dc:title>
          <dc:type>text</dc:type>
          <degree>
            <department>Atmospheric Sciences</department>
            <discipline>Atmospheric Sciences</discipline>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Dissertation</level>
            <name>Ph.D.</name>
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