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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%">Hubert, P.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Bader, Jean-Claude</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Bendjoudi, H.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Un siècle de débits annuels du fleuve Sénégal</title>
        <secondary-title>Hydrological Sciences Journal. Journal des Sciences Hydrologiques</secondary-title>
      </titles>
      <pages>68-73</pages>
      <keywords>
        <keyword>Senegal</keyword>
        <keyword>West Africa</keyword>
        <keyword>time series analysis</keyword>
        <keyword>Hubert segmentation</keyword>
        <keyword>drought</keyword>
        <keyword>discharge</keyword>
        <keyword>nonstationarity</keyword>
        <keyword>singularity</keyword>
        <keyword>abrupt change</keyword>
        <keyword>FLEUVE SENEGAL VALLEE</keyword>
        <keyword>SENEGAL</keyword>
        <keyword>MALI</keyword>
      </keywords>
      <dates>
        <year>2007</year>
      </dates>
      <call-num>fdi:010069198</call-num>
      <language>FRE</language>
      <periodical>
        <full-title>Hydrological Sciences Journal. Journal des Sciences Hydrologiques</full-title>
      </periodical>
      <isbn>0262-6667</isbn>
      <accession-num>ISI:000244180100005</accession-num>
      <number>1</number>
      <electronic-resource-num>10.1623/hysj.52.1.68</electronic-resource-num>
      <urls>
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          <url>https://www.documentation.ird.fr/hor/fdi:010069198</url>
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      <volume>52</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The discharges of the Senegal River, the catchment area of which is 218 000 km(2) at the Bakel gauging station located on the Malian-Senegalese border, integrating the climatological conditions of a wide West African region, have been measured since the beginning of the 20th century. Thus, we now have a century-long time series, partially reconstituted as the river discharges have been influenced since 1987 by the Manantali Dam operation. The segmentation procedure-previously applied to a shorter time series-was applied to the 1904-2003 time series. Originating from the study of the pluviometric abrupt change observed in West Africa at the end of the 1960s, the segmentation procedure can be seen as a stationarity test enabling one to determine whether or not a time series is homogeneous (stationary) and, if not, whether it can be cut into stationary segments. This procedure has been applied in an original way, by investigating all sub-series beginning in 1904 and all sub-series finishing in 2003. This analysis, which studies the neighbourhood of the two extremities of the series, shows the pluviometric jumps already observed in the previous studies, but also shows a new positive jump between 1993 and 1994 which appears, at least for the Senegal River catchment, as the end of the drought which began at the end of the 1960s.</abstract>
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