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Improvement of artificial neural networks to predict daily streamflow in a semi-arid area
Authors:Mahmoud Zemzami  Lahcen Benaabidate
Affiliation:1. Department of Earth Sciences, Sidi Mohammad Ben Abdellah University, Fez, Moroccomohmoud.zemzami@usmba.ac.ma;3. Department of Earth Sciences, Sidi Mohammad Ben Abdellah University, Fez, Morocco
Abstract:ABSTRACT

The application of artificial neural networks (ANNs) has been widely used recently in streamflow forecasting because of their ?exible mathematical structure. However, several researchers have indicated that using ANNs in streamflow forecasting often produces a timing lag between observed and simulated time series. In addition, ANNs under- or overestimate a number of peak flows. In this paper, we proposed three data-processing techniques to improve ANN prediction and deal with its weaknesses. The Wilson-Hilferty transformation (WH) and two methods of baseflow separation (one parameter digital filter, OPDF, and recursive digital filter, RDF) were coupled with ANNs to build three hybrid models: ANN-WH, ANN-OPDF and ANN-RDF. The network behaviour was quantitatively evaluated by examining the differences between model output and observed variables. The results show that even following the guidelines of the Wilson-Hilferty transformation, which significantly reduces the effect of local variations, it was found that the ANN-WH model has shown no significant improvement of peak flow estimation or of timing error. However, combining baseflow with streamflow and rainfall provides important information to ANN models concerning the flow process operating in the aquifer and the watershed systems. The model produced excellent performance in terms of various statistical indices where timing error was totally eradicated and peak flow estimation significantly improved.
Editor D. Koutsoyiannis; Associate editor Y. Gyasi-Agyei
Keywords:artificial neural networks  daily streamflow prediction  peak flow estimation  timing error  Wilson-Hilferty transformation  baseflow separation
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