Abstract

Abstract. In southern France, flash flood episodes frequently cause fatalities and severe damage. In order to inform and warn populations, the French flood forecasting service (SCHAPI, Service Central d'Hydrométéorologie et d'Appui à la Prévision des Inondations) initiated the BVNE (Bassin Versant Numérique Expérimental, or Experimental Digital Basin) project in an effort to enhance flash flood predictability. The target area for this study is the Gardon d'Anduze basin, located in the heart of the Cévennes range. In this Mediterranean mountainous setting, rainfall intensity can be very high, resulting in flash flooding. Discharge and rainfall gauges are often exposed to extreme weather conditions, which undermines measurement accuracy and continuity. Moreover, the processes governing rainfall-discharge relations are not well understood for these steeply-sloped and heterogeneous basins. In this context of inadequate information on both the forcing variables and process knowledge, neural networks are investigated due to their universal approximation and parsimony properties. We demonstrate herein that thanks to a rigorous variable and complexity selection, efficient forecasting of up to two-hour durations, without requiring rainfall forecasting as input, can be derived using the measured discharges available from a feedforward model. In the case of discharge gauge malfunction, in degraded mode, forecasting may result using a recurrent neural network model. We also observe that neural network models exhibit low sensitivity to uncertainty in rainfall measurements since producing ensemble forecasting does not significantly affect forecasting quality. In providing good results, this study suggests close consideration of our main purpose: generating forecasting on ungauged basins.

Highlights

  • In Mediterranean regions, flash floods due to heavy rainfall events frequently occur, causing a large number of fatalities and costly damage

  • Population growth, especially in these attractive areas, and a sustainable land management policy imply the need to enhance prevention measures and early warning alerts transmitted to authorities and local populations. Aware of this issue, the French Flood Forecasting Center (SCHAPI, Service Central d’Hydrometeorologie et d’Appui ala Prevision des Inondations) initiated in 2006 the Experimental Digital Basin project (BVNE, Bassin Versant Numerique Experimental) as a mean of improving flash flood forecasting by providing input to the flood warning map in the form of high-water alarm levels, through the use of new models, which are more efficient than previous ones relative to rapid hydrological responses

  • In the present study, that for a simple basin, a linear part combined to a nonlinear one in the model brings a significant enhancing to a multilayer perceptron (MLP) feedforward model

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Summary

Introduction

In Mediterranean regions, flash floods due to heavy rainfall events frequently occur, causing a large number of fatalities and costly damage. Population growth, especially in these attractive areas, and a sustainable land management policy imply the need to enhance prevention measures and early warning alerts transmitted to authorities and local populations Aware of this issue, the French Flood Forecasting Center (SCHAPI, Service Central d’Hydrometeorologie et d’Appui ala Prevision des Inondations) initiated in 2006 the Experimental Digital Basin project (BVNE, Bassin Versant Numerique Experimental) as a mean of improving flash flood forecasting by providing input to the flood warning map in the form of high-water alarm levels (known as “vigicrues”, www.vigicrues.gouv.fr), through the use of new models, which are more efficient than previous ones relative to rapid hydrological responses. Its distance to the Mediterranean Sea varies from 50 km in the Herault to more than 100 km in the Ardeche The elevations of this range can be as low as 100–200 m in the foothills area and rise to 1700 m, e.g., on Mont-Lozere crests. This aspect is responsible for the high spatial variability (Fig. 1)

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