Title
Spatial variability of diurnal to seasonal cycles of precipitation from a high-altitude equatorial Andean valley to the Amazon Basin
Date Issued
01 December 2021
Access level
open access
Resource Type
journal article
Author(s)
Ruiz-Hernández J.C.
Condom T.
Ribstein P.
Le Moine N.
Villacís M.
Vera A.
Muñoz T.
Maisincho L.
Campozano L.
Rabatel A.
Sicart J.E.
Publisher(s)
Elsevier B.V.
Abstract
Study region: The upper part of the Guayllabamba and Napo basins (78.2 ° W, 0.3 °S; 18,500 km2) 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.
Volume
38
Language
English
OCDE Knowledge area
Investigación climática Meteorología y ciencias atmosféricas
Scopus EID
2-s2.0-85117710376
Source
Journal of Hydrology: Regional Studies
ISSN of the container
22145818
Source funding
Institut de Recherche pour le Développement
Sponsor(s)
This study was conducted as part of the International Joint Laboratory GREAT-ICE, a joint initiative of the IRD and universities and institutions in Bolivia, Peru, Ecuador and Colombia. We acknowledge the support of the LabEx OSUG@2020 (Investissement d'Avenir – ANR10 LABX56) with regards to the data provided by the Andean part of the French Service National d'Observation GLACIOCLIM (P.I. Antoine Rabatel, Univ. Grenoble Alpes, IRD, CNRS-INSU). JCR thanks to Secretaría Nacional de Educación Superior, Ciencia, Tecnología e Innovación, SENESCYT for financial support through a PhD scholarship. JCE received the support of the French AMANECER-MOPGA project funded by ANR and IRD (ref. ANR-18-MPGA-0008). We are also grateful to Instituto Nacional de Meteorología e Hidrología (INAMHI) and to EPMAPS-FONAG through the Estación Científica Agua y Páramos (ECAP) for providing the precipitation data. The support received from EPMAPS and FONAG during field work is also acknowledged. JCR is also grateful to Dr Hans Segura for valuable scientific discussions during quarantines and Dr Jai Beeman for revising the manuscript edition.
Sources of information: Directorio de Producción Científica Scopus