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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACLN : Articles dans des revues avec comité de lecture non répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="bold" font="default" size="100%">Delcroix, Thierry</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Hénin, Christian</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Mechanisms of subsurface thermal structure and sea surface thermohaline variabilities in the southwestern tropical Pacific during 1975-85</title>
        <secondary-title>Journal of Marine Research</secondary-title>
      </titles>
      <pages>777-812</pages>
      <keywords>
        <keyword>EL NINO</keyword>
        <keyword>VARIATION SAISONNIERE</keyword>
        <keyword>TEMPERATURE DE SURFACE</keyword>
        <keyword>THERMOCLINE</keyword>
        <keyword>STRUCTURE THERMIQUE</keyword>
        <keyword>PACIFIQUE TROPICAL SUD OUEST</keyword>
      </keywords>
      <dates>
        <year>1989</year>
      </dates>
      <call-num>fdi:30116</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Journal of Marine Research</full-title>
      </periodical>
      <isbn>0022-2402</isbn>
      <number>47</number>
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        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:30116</url>
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        <pdf-urls>
          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/pleins_textes_5/b_fdi_23-25/30116.pdf</url>
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      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Major features of the southwestern tropical Pacific (SWTP), defined between 160E-140W and 24S-10S, are brought to light through analysis of surface water samples (23000) and temperature/depth observations (8500), both collected by ship opportunity programs during the 1979-85 period. The mean vertical thermal structure (and its related parameters), mean sea surface temperature (SST) and salinity (SSS) are first portrayed, to further quantify the 1979-85 variability. It is demonstrated that the observed seasonal and interannual variabilities, the latter being associated with the strong 1982-83 El Nino Southern Oscillation (ENSO) event, are mostly governed by specific mechanisms involving varying wind field and rainfall regimes.</abstract>
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