<?xml version="1.0" encoding="UTF-8"?>
<xml>
  <records>
    <record>
      <source-app name="Horizon">Horizon</source-app>
      <rec-number>1</rec-number>
      <foreign-keys>
        <key app="Horizon" db-id="fdi:010075550">1</key>
      </foreign-keys>
      <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="bold" font="default" size="100%">Illig, Serena</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Bachelery, M. L.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Propagation of subseasonal equatorially-forced coastal trapped waves down to the Benguela upwelling system</title>
        <secondary-title>Scientific Reports - Nature</secondary-title>
      </titles>
      <pages>art. 5306 [10 ]</pages>
      <keywords>
        <keyword>ATLANTIQUE</keyword>
        <keyword>BENGUELA COURANT</keyword>
      </keywords>
      <dates>
        <year>2019</year>
      </dates>
      <call-num>fdi:010075550</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Scientific Reports - Nature</full-title>
      </periodical>
      <isbn>2045-2322</isbn>
      <accession-num>ISI:000462585600016</accession-num>
      <electronic-resource-num>10.1038/s41598-019-41847-1</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010075550</url>
        </related-urls>
        <pdf-urls>
          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers19-04/010075550.pdf</url>
        </pdf-urls>
      </urls>
      <volume>9</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The oceanic connection between the coastal variability along the southwestern African coasts and the linear equatorial dynamics at subseasonal time-scales (&lt;120 days) is examined using a variety of model outputs, ranging from linear to general circulation models. We focus on the equatorially-forced fast and weakly dissipative first-mode coastal trapped waves which are shown to propagate down to the southern tip of Africa. In the eastern equatorial Atlantic, the first-mode equatorial forcing is tangled with the higher-order Kelvin wave modes and is overshadowed by the dominant second baroclinic mode. The latter is slower and peaks 10 days after the concealed first-mode contribution. Within this time frame, the remotely-forced first-mode coastal trapped waves impinge on the variability of the Benguela upwelling ecosystem, almost in phase with the subseasonal sea level fluctuations in the Gulf of Guinea. Over 1993-2008, the equatorial forcing undergoes a substantial interannual modulation. Periods of energetic first-mode equatorial Kelvin waves coincide with a strong subseasonal coastal wind activity that breaks the stronger equatorial connection. This suggests the existence of a large-scale atmospheric connection between the equatorial wave forcing and the along-shore winds in the Benguela, modulating the maximum latitude at which the equatorial dynamics impacts the local marine resources.</abstract>
      <custom6>032</custom6>
      <custom1>UR065</custom1>
      <custom7>Afrique du Sud</custom7>
    </record>
  </records>
</xml>
