Title
Evaluation of precipitation products over complex mountainous terrain: A water resources perspective
Date Issued
01 October 2011
Access level
metadata only access
Resource Type
journal article
Author(s)
Imperial College of Science
Abstract
The availability of in situ measurements of precipitation in remote locations is limited. As a result, the use of satellite measurements of precipitation is attractive for water resources management. Combined precipitation products that rely partially or entirely on satellite measurements are becoming increasingly available. However, these products have several weaknesses, for example their failure to capture certain types of precipitation, limited accuracy and limited spatial and temporal resolution. This paper evaluates the usefulness of several commonly used precipitation products over data scarce, complex mountainous terrain from a water resources perspective. Spatially averaged precipitation time series were generated or obtained for 16 sub-basins of the Paute river basin in the Ecuadorian Andes and 13 sub-basins of the Baker river basin in Chilean Patagonia. Precipitation time series were generated using the European Centre for Medium Weather Range Forecasting (ECMWF) 40year reanalysis (ERA-40) and the subsequent ERA-interim products, and the National Centers for Environmental Prediction/National Center for Atmospheric Research reanalysis dataset 1 (NCEP R1) hindcast products, as well as precipitation estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN). The Tropical Rainfall Measurement Mission (TRMM) 3B42 is also used for the Ecuadorian Andes. These datasets were compared to both spatially averaged gauged precipitation and river discharge. In general, the time series of the remotely sensed and hindcast products show a low correlation with locally observed precipitation data. Large biases are also observed between the different products. Hydrological verification based on river flows reveals that water balance errors can be extremely high for all evaluated products, including interpolated local data, in basins smaller than 1000km2. The observations are consistent over the two study regions despite very different climatic settings and hydrological processes, which is encouraging for extrapolation to other mountainous regions. © 2011 Elsevier Ltd.
Start page
1222
End page
1231
Volume
34
Issue
10
Language
English
OCDE Knowledge area
Meteorología y ciencias atmosféricas
Oceanografía, Hidrología, Recursos hídricos
Subjects
Scopus EID
2-s2.0-80052851867
Source
Advances in Water Resources
ISSN of the container
03091708
Sponsor(s)
EW and LP were funded by NERC studentships. WB acknowledges funding from project MECESUP UCO0308 at UdeC-DIC during his 2008 stay at U. Concepción, Chile, and a RGS-IBG Small Research Grant. The authors would also like to thank Florian Pappenberger of ECMWF of Reading, UK and Alejandro Dussaillant of the University of Greenwich, UK for the provision of data used during this study. The authors would also like to thank four anonymous reviewers for their comments, which have helped to improve the quality of the paper.
Sources of information:
Directorio de Producción Científica
Scopus