Abstract

In terms of flood hazard, the presence of large wood (logs, trees, branches and roots) in rivers may aggravate the consequences of flood events. This material may affect infrastructures such as bridges, weirs, etc., especially those intersecting forested mountain rivers. Until recently, a widely accepted practice was to systematically remove wood debris from river channels as a preventive measure. However, studies have shown that this practice may be useless as the material is transported and deposited after each flood and may even not benefit the long term natural balance of the river ecosystem. Therefore, the presence of this woody material in rivers must be managed and included in flood hazard and risk analysis. In this paper we present a comprehensive methodological approach to study the role of large wood in rivers, with a focus on flood hazard. First, to understand the dynamics of wood recruitment, the contributing areas delivering wood to the streams have to be delineated and the recruitment mechanisms studied. Thus, an estimate can be obtained of the potential volume of deliverable wood. To analyse wood transport we present a numerical model, which allows simulates the behaviour of individual pieces of wood together with hydrodynamics. Finally, we analyse the impact of wood on the magnitude of flood events (in terms of water level, flow velocity or flooded areas), using as an example a flood which occurred in December 1997 in the Sierra de Gredos. The results allowed us to reproduce the wood deposit patterns during the event and to reconstruct the bridge blockage. This caused the upstream water level to rise by up to 2 meters and reduced the flow velocity, which favoured debris and sediment deposits. Consequently, the effects of flooding were equivalent to those of a greater magnitude event. This increase in the flood hazard has been numerically quantified.

Highlights

  • The high potential risk associated with flash floods in mountain watercourses is a result of a rapid and complex hydrological catchment response

  • Large wood in rivers and its influence on flood hazard morphology during flood events and the reduction of cross-sectional areas that are blocked by transported materials such as large wood may increase associated flood risk

  • In order to analyse the influence of wood on the flood event the procedure applied to the 1997 event study is divided into 3 main stages: (1) estimation of the large wood recruited at a basin scale; (2) establishment of the inlet boundary conditions for the studied reach by means of scenarios; (3) and the modelling of the 1997 flood including large wood transport

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Summary

Introduction

The high potential risk associated with flash floods in mountain watercourses is a result of a rapid and complex hydrological catchment response. In order to analyse the influence of wood on the flood event the procedure applied to the 1997 event study is divided into 3 main stages: (1) estimation of the large wood recruited at a basin scale (analysing the recruitment areas caused by avulsion, fluvial transport and bank erosion occurring during the 1997 event); (2) establishment of the inlet boundary conditions for the studied reach (water and wood fluxes) by means of scenarios; (3) and the modelling of the 1997 flood including large wood transport This information allowed us to establish the scenario that best reproduces the 1997 event and analyse the linear patterns of predicted wood deposits. According to the previous data available for this event, Scenario 2 seems to more closely reproduce the bridge clogging and backwater elevation of the 1997 flood event

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