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      <source-app name="Horizon">Horizon</source-app>
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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%">Penven, Pierrick</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Lutjeharms, J.R.E.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Marchesiello, P.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Roy, Claude</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Weeks, S.J.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Generation of cyclonic eddies by the Agulhas current in the lee of the Agulhas bank</title>
        <secondary-title>Geophysical Research Letters</secondary-title>
      </titles>
      <pages>1055-1058</pages>
      <keywords>
        <keyword>INTERACTION OCEAN ATMOSPHERE</keyword>
        <keyword>TOURBILLON</keyword>
        <keyword>CYCLONE TROPICAL</keyword>
        <keyword>CIRCULATION OCEANIQUE</keyword>
        <keyword>COURANT MARIN</keyword>
        <keyword>SURFACE MARINE</keyword>
        <keyword>ALTIMETRIE</keyword>
        <keyword>TEMPERATURE DE SURFACE</keyword>
        <keyword>MODELISATION</keyword>
        <keyword>SIMULATION</keyword>
        <keyword>AFRIQUE DU SUD</keyword>
        <keyword>AGULHAS</keyword>
        <keyword>ATLANTIQUE SUD</keyword>
      </keywords>
      <dates>
        <year>2001</year>
      </dates>
      <call-num>fdi:010025372</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Geophysical Research Letters</full-title>
      </periodical>
      <isbn>0094-8276</isbn>
      <number>6</number>
      <electronic-resource-num>10.1029/2000GL011760</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010025372</url>
        </related-urls>
        <pdf-urls>
          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/pleins_textes_7/b_fdi_57-58/010025372.pdf</url>
        </pdf-urls>
      </urls>
      <volume>27</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Anti-cyclonic rings are shed from the Agulhas Current at its retroflection. They subsequently drift off into the South Atlantic. Smaller, cyclonic eddies have also been observed in this region. The origin of these latter eddies has remained unknown. We present model results that indicate that the configuration of the southern Agulhas Current and the poleward termination of the continental shelf of Africa allows shedding of cyclonic lee eddies by a flow detachment process. Hydrographic data, thermal infrared satellite images and altimetric observations are furnished that show that this model simulation is consistent with the characteristics and the behaviour of cyclonic eddies in the region. (Résumé d'auteur)</abstract>
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