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        <identifier>oai:www.ideals.illinois.edu:2142/97383</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>Makela, Jonathan J.</dc:contributor>
          <dc:creator>Grawe, Matthew A.</dc:creator>
          <dc:date>2017-08-10T19:15:17Z</dc:date>
          <dc:date>2017-08-10T19:15:17Z</dc:date>
          <dc:date>2017-04-18</dc:date>
          <dc:date>2017-05</dc:date>
          <dc:description>Tsunamis generate internal gravity waves (IGWs) that propagate vertically into the atmosphere and can create detectable signatures in the ionosphere. These signatures have consistently been observed in the presence of a tsunami for over a decade in the total electron content and for over 5 years in the 630.0 nm airglow. Here, we provide a comprehensive overview on the utilization of airglow imaging systems for monitoring tsunamis. We develop the basic theory behind tsunami-ionospheric coupling from first principles and give special attention to the topic of tsunami-ionospheric coupling efficiency. This is followed by the presentation and analysis of a methodology for extracting wave parameters of tsunami-induced signatures appearing in airglow images. The methodology is applied to the 11 March 2011 Tohoku and 16 September 2015 Chile tsunamis as case studies. A previously developed geometric model that takes into account the assumed posture of tsunami-induced IGWs in the geomagnetic field and the observation geometry is shown to predict the region of the sky in which the observations were seen.</dc:description>
          <dc:description>Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2017-08-10 without embargo terms</dc:description>
          <dc:description>The student, Matthew Grawe, accepted the attached license on 2017-04-17 at 16:34.</dc:description>
          <dc:description>The student, Matthew Grawe, submitted this Thesis for approval on 2017-04-17 at 17:26.</dc:description>
          <dc:description>This Thesis was approved for publication on 2017-04-18 at 16:54.</dc:description>
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  Previous issue date: 2017-04-18</dc:description>
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          <dc:identifier>http://hdl.handle.net/2142/97383</dc:identifier>
          <dc:language>en</dc:language>
          <dc:rights>Copyright 2017 Matthew Grawe</dc:rights>
          <dc:subject>Airglow</dc:subject>
          <dc:subject>Ionosphere</dc:subject>
          <dc:subject>Tsunami</dc:subject>
          <dc:subject>Gabor filter</dc:subject>
          <dc:title>Tsunami monitoring using airglow imaging systems</dc:title>
          <dc:type>text</dc:type>
          <dc:type>text</dc:type>
          <degree>
            <department>Electrical &amp; Computer Eng</department>
            <discipline>Electrical &amp; Computer Engr</discipline>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Thesis</level>
            <name>M.S.</name>
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