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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%">Penhoat, Yves du</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Treguier, A.M.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>The seasonal linear response of the Tropical Atlantic ocean</title>
        <secondary-title>Journal of Physical Oceanography</secondary-title>
      </titles>
      <pages>316-328</pages>
      <keywords>
        <keyword>CIRCULATION OCEANIQUE</keyword>
        <keyword>COURANT</keyword>
        <keyword>TOPOGRAPHIE DYNAMIQUE</keyword>
        <keyword>MODELE</keyword>
        <keyword>ATLANTIQUE TROPICAL</keyword>
      </keywords>
      <dates>
        <year>1985</year>
      </dates>
      <call-num>fdi:010006333</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Journal of Physical Oceanography</full-title>
      </periodical>
      <isbn>0022-3670</isbn>
      <number>3</number>
      <electronic-resource-num>10.1175/1520-0485(1985)015&lt;0316:TSLROT&gt;2.0.CO;2</electronic-resource-num>
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          <url>https://www.documentation.ird.fr/hor/fdi:010006333</url>
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          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/pleins_textes_6/b_fdi_45-46/010006333.pdf</url>
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      <volume>15</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The linear response of the Tropical Atlantic ocean to climatological winds iscalculated in a continuously stratified model and compared with observations. All the characteristic features of the dynamic topography are reproduced at the proper locations including the series of zonally oriented ridges and thoughs, the Equatorial "pivot" zone and the seasonal variations of slope along the equator. Linear theory fails to explains seasonal variations of the South Equatorial current and of the Equatorial Undercurrent, but it compares favorably for the major zonal currents off the equator (The North Equatorial Countercurrent, the Guinea current and undercurrent). (Résumé d'auteur)</abstract>
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