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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Cuypers, Y.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Bouruet-Aubertot, P.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Vialard, Jérôme</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">McPhaden, M. J.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Focusing of internal tides by near-inertial waves</title>
        <secondary-title>Geophysical Research Letters</secondary-title>
      </titles>
      <pages>2398-2406</pages>
      <keywords>
        <keyword>OCEAN INDIEN</keyword>
        <keyword>ZONE TROPICALE</keyword>
      </keywords>
      <dates>
        <year>2017</year>
      </dates>
      <call-num>fdi:010069421</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Geophysical Research Letters</full-title>
      </periodical>
      <isbn>0094-8276</isbn>
      <accession-num>ISI:000398183700040</accession-num>
      <number>5</number>
      <electronic-resource-num>10.1002/2017gl072625</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010069421</url>
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          <url>https://www.documentation.ird.fr/intranet/publi/2017/04/010069421.pdf</url>
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      <volume>44</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The refraction of internal waves by lower-frequency near-inertial waves has been predicted theoretically, but never observed before. Here, we report observations of semi-diurnal internal tides generated by the rough topography of the Central Indian Ridge, in the presence of a strong, lower-frequency near-inertial wave field generated by a tropical storm. The semi-diurnal internal tide energy is trapped within upward propagating bands with a periodicity close to the inertial period. A ray-tracing model suggests that this trapping results from the internal tide refraction by the shear associated with near-inertial waves. This yields a strong increase of the internal tide energy and shear in space-time regions where the background flow focuses the rays, leading to the formation of caustics. This mechanism may increase vertical mixing generated by baroclinic tides in the vicinity of mid-ocean ridges in tropical regions.</abstract>
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      <custom1>UR182</custom1>
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