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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%">Ruiz-Hernandez, J. C.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Condom, Thomas</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Ribstein, P.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Le Moine, N.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Espinoza, J. C.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Junquas, Clémentine</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Villacis, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Vera, A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Munoz, T.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Maisincho, L.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Campozano, L.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Rabatel, A.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Sicart, Jean-Emmanuel</style>
          </author>
        </authors>
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      <titles>
        <title>Spatial variability of diurnal to seasonal cycles of precipitation from a high-altitude equatorial Andean valley to the Amazon Basin</title>
        <secondary-title>Journal of Hydrology : Regional Studies</secondary-title>
      </titles>
      <pages>100924 [16 ]</pages>
      <keywords>
        <keyword>Precipitation variability</keyword>
        <keyword>Diurnal and seasonal cycles</keyword>
        <keyword>Equatorial Andes</keyword>
        <keyword>EQUATEUR</keyword>
        <keyword>ANDES</keyword>
        <keyword>AMAZONE BASSIN</keyword>
        <keyword>GUAYLLABAMBA BASSIN</keyword>
        <keyword>NAPO BASSIN</keyword>
      </keywords>
      <dates>
        <year>2021</year>
      </dates>
      <call-num>fdi:010083318</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Journal of Hydrology : Regional Studies</full-title>
      </periodical>
      <accession-num>ISI:000712249000002</accession-num>
      <electronic-resource-num>10.1016/j.ejrh.2021.100924</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010083318</url>
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        <pdf-urls>
          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/2021-12/010083318.pdf</url>
        </pdf-urls>
      </urls>
      <volume>38</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Study region: The upper part of the Guayllabamba and Napo basins (78.2 degrees W, 0.3 degrees S; 18,500 km(2)) in the equatorial Andes, which are vulnerable to stress on the ecosystem services. Study focus: This paper analyses the diurnal cycle of precipitation over a transect from the Andes to the Amazon. The diurnal cycle is estimated as the diurnal distribution of precipitation for 2014-2019 using records from 80 stations. Cluster analysis performed on the diurnal cycle estimates depicts the spatial association between the diurnal and seasonal cycles of precipitation. New hydrological insights: A northwest-southeast spatial variation in the diurnal and seasonal cycles is identified with four groups of stations. In the western part, the seasonal cycles of Groups 1 and 2 are bimodal with precipitation maxima in the March-April and October-November seasons and a short drier season in July-August. In the eastern part, Group 3 also presents bimodality, but a weaker seasonal cycle. Conversely, Group 4 is unimodal with a peak in June. Distinct diurnal cycles are observed in both drier and wetter seasons of Groups 1-3; no marked diurnal cycle is observed in Group 4. Groups 3 and 4 are the most spatially heterogeneous, with an exceptional horizontal variation of 330 mm/yr/km. The analysis of these variations provides insight into the atmospheric dynamics driving precipitation in this zone, and may help to better optimize the water supply system.</abstract>
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      <custom1>UR252</custom1>
      <custom7>Équateur</custom7>
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