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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%">Sous, D.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Chevalier, Cristèle</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Devenon, J. L.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Blanchot, Jean</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Pagano, Marc</style>
          </author>
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      <titles>
        <title>Circulation patterns in a channel reef-lagoon system, Ouano lagoon, New Caledonia</title>
        <secondary-title>Estuarine Coastal and Shelf Science</secondary-title>
      </titles>
      <pages>315-330</pages>
      <keywords>
        <keyword>NOUVELLE CALEDONIE</keyword>
        <keyword>PACIFIQUE</keyword>
        <keyword>OUANO LAGON</keyword>
      </keywords>
      <dates>
        <year>2017</year>
      </dates>
      <call-num>fdi:010071045</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Estuarine Coastal and Shelf Science</full-title>
      </periodical>
      <isbn>0272-7714</isbn>
      <accession-num>ISI:000411302000029</accession-num>
      <electronic-resource-num>10.1016/j.ecss.2017.07.015</electronic-resource-num>
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          <url>https://www.documentation.ird.fr/hor/fdi:010071045</url>
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          <url>https://www.documentation.ird.fr/intranet/publi/2017/10/010071045.pdf</url>
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      <volume>196</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>This paper reports on two three-months field experiments carried out in the Ouano lagoon, New Caledonia. This channel-type lagoon, exposed to meso-tides, south pacific swells and trade winds, has been monitored thanks to a network of currents profilers to understand the dynamics of the lagoon waters. Four typical circulation patterns have been identified, covering all together more than 90% of the survey period. These patterns are mainly driven by the waves and wind features. In particular, obliquely incident waves or strong winds blowing over a sufficient period are able to reverse the typical circulation pattern. The analysis of the vertical structure of the currents through passages shows the regular presence of a nearly linear vertical shear within the water column.</abstract>
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