<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Spatial variability of diurnal to seasonal cycles of precipitation from a high-altitude equatorial Andean valley to the Amazon Basin</dc:title>
  <dc:creator>Ruiz-Hernandez, J. C.</dc:creator>
  <dc:creator>/Condom, Thomas</dc:creator>
  <dc:creator>Ribstein, P.</dc:creator>
  <dc:creator>Le Moine, N.</dc:creator>
  <dc:creator>Espinoza, J. C.</dc:creator>
  <dc:creator>/Junquas, Cl&#xE9;mentine</dc:creator>
  <dc:creator>Villacis, M.</dc:creator>
  <dc:creator>Vera, A.</dc:creator>
  <dc:creator>Munoz, T.</dc:creator>
  <dc:creator>Maisincho, L.</dc:creator>
  <dc:creator>Campozano, L.</dc:creator>
  <dc:creator>Rabatel, A.</dc:creator>
  <dc:creator>/Sicart, Jean-Emmanuel</dc:creator>
  <dc:subject>Precipitation variability</dc:subject>
  <dc:subject>Diurnal and seasonal cycles</dc:subject>
  <dc:subject>Equatorial Andes</dc:subject>
  <dc:description>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.</dc:description>
  <dc:date>2021</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010083318</dc:identifier>
  <dc:identifier>fdi:010083318</dc:identifier>
  <dc:identifier>Ruiz-Hernandez J. C., Condom Thomas, Ribstein P., Le Moine N., Espinoza J. C., Junquas Cl&#xE9;mentine, Villacis M., Vera A., Munoz T., Maisincho L., Campozano L., Rabatel A., Sicart Jean-Emmanuel. Spatial variability of diurnal to seasonal cycles of precipitation from a high-altitude equatorial Andean valley to the Amazon Basin. 2021, 38, 100924 [16 ]</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>EQUATEUR</dc:coverage>
  <dc:coverage>ANDES</dc:coverage>
</oai_dc:dc>
