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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%">Espinoza, J. C.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Marengo, J. A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ronchail, J.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Carpio, J. M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Flores, L. N.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Guyot, Jean-Loup</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>The extreme 2014 flood in south-western Amazon basin : the role of tropical-subtropical South Atlantic SST gradient</title>
        <secondary-title>Environmental Research Letters</secondary-title>
      </titles>
      <pages>art. 124007 [9 ]</pages>
      <keywords>
        <keyword>extreme flood</keyword>
        <keyword>Amazon basin</keyword>
        <keyword>Madeira river</keyword>
        <keyword>Bolivian Amazon</keyword>
        <keyword>Brazilian Amazon</keyword>
        <keyword>AMAZONE BASSIN</keyword>
        <keyword>BOLIVIE</keyword>
        <keyword>BRESIL</keyword>
        <keyword>ATLANTIQUE</keyword>
        <keyword>ZONE TROPICALE</keyword>
      </keywords>
      <dates>
        <year>2014</year>
      </dates>
      <call-num>fdi:010063643</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Environmental Research Letters</full-title>
      </periodical>
      <isbn>1748-9326</isbn>
      <accession-num>ISI:000347454800008</accession-num>
      <number>12</number>
      <electronic-resource-num>10.1088/1748-9326/9/12/124007</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010063643</url>
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          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers17-08/010063643.pdf</url>
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      <volume>9</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Unprecedented wet conditions are reported in the 2014 summer (December-March) in Southwestern Amazon, with rainfall about 100% above normal. Discharge in the Madeira River (the main southern Amazon tributary) has been 74% higher than normal (58 000 m(3) s(-1)) at Porto Velho and 380% (25 000 m(3) s(-1)) at Rurrenabaque, at the exit of the Andes in summer, while levels of the Rio Negro at Manaus were 29.47 m in June 2014, corresponding to the fifth highest record during the 113 years record of the Rio Negro. While previous floods in Amazonia have been related to La Nina and/or warmer than normal tropical South Atlantic, the 2014 rainfall and flood anomalies are associated with warm condition in the western Pacific-Indian Ocean and with an exceptionally warm Subtropical South Atlantic. Our results suggest that the tropical and subtropical South Atlantic SST gradient is a main driver for moisture transport from the Atlantic toward south-western Amazon, and this became exceptionally intense during summer of 2014.</abstract>
      <custom6>062 ; 032</custom6>
      <custom1>UR182</custom1>
      <custom7>Bolivie / Brésil / Pérou</custom7>
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