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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%">Wongchuig, S.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Kitambo, B.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Papa, Fabrice</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Paris, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Fleischmann, A.S.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Gal, L.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Boucharel, Julien</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Paiva, R.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Juca Oliveira, Romulo Augusto</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Tshimanga, R.M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Calmant, Stéphane</style>
          </author>
        </authors>
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      <titles>
        <title>Improved modeling of Congo's hydrology for floods and droughts analysis and ENSO teleconnections</title>
        <secondary-title>Journal of Hydrology : Regional Studies</secondary-title>
      </titles>
      <pages>101563 [21 ]</pages>
      <keywords>
        <keyword>CENTRAFRIQUE</keyword>
        <keyword>CAMEROUN</keyword>
        <keyword>CONGO</keyword>
        <keyword>ANGOLA</keyword>
        <keyword>ZAMBIE</keyword>
        <keyword>TANZANIE</keyword>
        <keyword>RWANDA</keyword>
        <keyword>BURUNDI</keyword>
        <keyword>CONGO BASSIN</keyword>
      </keywords>
      <dates>
        <year>2023</year>
      </dates>
      <call-num>fdi:010089436</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Journal of Hydrology : Regional Studies</full-title>
      </periodical>
      <isbn>2214-5818</isbn>
      <accession-num>ISI:001149943800001</accession-num>
      <electronic-resource-num>10.1016/j.ejrh.2023.101563</electronic-resource-num>
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          <url>https://www.documentation.ird.fr/hor/fdi:010089436</url>
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          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/2024-02/010089436.pdf</url>
        </pdf-urls>
      </urls>
      <volume>50</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Study region : The Congo River basin (CRB), the world's second-largest river system, is subject to extreme hydrological events that strongly impact its ecosystems and population. Study focus : Here we present an improved 40-year (1981-2020) hydrological reanalysis of daily CRB discharge and analyze the spatiotemporal dynamics of recent major CRB floods and droughts, and their teleconnection with El Niño-Southern Oscillation (ENSO), the dominant driver of tropical precipitation. We employ a large-scale hydrologic-hydrodynamic model (MGB) with lake storage dynamics representation and a data assimilation (DA) technique using in-situ and remote sensing observations. New Hydrological Insights : The MGB model demonstrates satisfactory performance, with Kling-Gupta efficiency metric of 0.84 and 0.71 for calibration and validation, respectively. Incorporating lake representation substantially enhances simulations, increasing the Pearson correlation coefficient from 0.3 to 0.63. Additionally, DA yields a ?13% reduction in discharge errors via cross-validation. We find that the 1997-1998 flood impacting the south and central CRB is statistically linked to a major El Niño event during that period. However, no such association is found for the 2019-2020 flood. Severe droughts in 1983-1984 and 2011-2012, affecting northern and southern CRB respectively, exhibit strong correlation with preceding El Niño and La Niña events, with a ?10-12 months lag. This study advances understanding of the intricate interplay between spatiotemporal hydrological variability in CRB and large-scale climate phenomena like ENSO.</abstract>
      <custom6>126TELAPP04</custom6>
      <custom1>UR065</custom1>
      <custom7>Brésil / République démocratique du Congo</custom7>
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