Abstract

Flash-flood forecasting has emerged worldwide due to the catastrophic socio-economic impacts this hazard might cause and the expected increase of its frequency in the future. In mountain catchments, precipitation-runoff forecasts are limited by the intrinsic complexity of the processes involved, particularly its high rainfall variability. While process-based models are hard to implement, there is a potential to use the random forest algorithm due to its simplicity, robustness and capacity to deal with complex data structures. Here a step-wise methodology is proposed to derive parsimonious models accounting for both hydrological functioning of the catchment (e.g., input data, representation of antecedent moisture conditions) and random forest procedures (e.g., sensitivity analyses, dimension reduction, optimal input composition). The methodology was applied to develop short-term prediction models of varying time duration (4, 8, 12, 18 and 24 h) for a catchment representative of the Ecuadorian Andes. Results show that the derived parsimonious models can reach validation efficiencies (Nash-Sutcliffe coefficient) from 0.761 (4-h) to 0.384 (24-h) for optimal inputs composed only by features accounting for 80% of the model’s outcome variance. Improvement in the prediction of extreme peak flows was demonstrated (extreme value analysis) by including precipitation information in contrast to the use of pure autoregressive models.

Highlights

  • Flooding is nowadays the most common natural disaster worldwide [1]

  • The autocorrelation function (ACF) and the corresponding 95% confidence band was estimated from lag to lag 400 (h), and the highest autocorrelation occurred at the first lag

  • The partial autocorrelation function (PACF) and its 95% confidence levels were estimated from lag 1 to 25

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Summary

Introduction

Flooding is nowadays the most common natural disaster worldwide [1]. Its occurrence is expected to further intensify during coming years due to the increase in the frequency of extreme precipitation events [2]. As a result, during last decades, real-time flood forecasting has become an emerging field of research for water management and risk analysis [3]. Extreme flash flood events have the potential to cause serious damage to downstream infrastructure and produce large socio-economic impacts. In the Andean region of Ecuador, flash-flood events cause human losses and perturb the everyday life of people (e.g., interruption in the water supply service, damage in transportation network) [4]. According to a report of the Andean community for the period 1970–2007

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