Abstract

Flood risk is changing over time. Beside climatic changes, key drivers for changing flood risks are the modification of the river courses by flood defence structures and the increase in properties exposed to floods due to economic development. In this study, both effects – the modification of the river courses and the increase of economic assets – on the long-term evolution of flood risk were isolated and confronted. To this aim, two states of the river network were compared, one representing the river courses of today and another representing the river courses of the early 19th century before the river corrections took place. Selected observed and well documented flood events of the last decades were modelled on the historic states of the river reaches. The documented flood events were compared with the simulations in terms of inundated area and exposed buildings. Without river corrections, the flooded areas and the number of exposed residential housings would be remarkably higher than observed in recent flood events. The examples show that the effects of the main river corrections are remarkable for today’s economic activities in the floodplains. Therefore, the maintenance of the former river correction works is an important part of today’s risk management practice.

Highlights

  • Flood risk in terms of the probability of damages to persons, houses and infrastructure due to floodings is changing over time

  • A third group is analysing the alteration of hydrologic regimes by reconstructing or “retromodelling” historic states of the river channels and comparing them with the today’s river channels (e.g. [12], [13])

  • The results enable a first attempt to assess and quantify the effects of the river corrections of the 19th century for today’s flood exposure

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Summary

Introduction

Flood risk in terms of the probability of damages to persons, houses and infrastructure due to floodings is changing over time. For analysis of long-term changes in river systems, their historic states have to be reconstructed. The consideration of former extreme flood events can extent the time periods of discharge measurements and improve flood frequency estimation An overview of quantitative historical hydrology in Europe is given by [8]. Another use of reconstructed historical floods is the analysis of changes of the meteorological causes of floods A third group is analysing the alteration of hydrologic regimes by reconstructing or “retromodelling” historic states of the river channels and comparing them with the today’s river channels (e.g. [12], [13])

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