Abstract

Abstract. Probabilistic flood inundation mapping is performed and analysed at the ungauged Xerias stream reach, Volos, Greece. The study evaluates the uncertainty introduced by the roughness coefficient values on hydraulic models in flood inundation modelling and mapping. The well-established one-dimensional (1-D) hydraulic model, HEC-RAS is selected and linked to Monte-Carlo simulations of hydraulic roughness. Terrestrial Laser Scanner data have been used to produce a high quality DEM for input data uncertainty minimisation and to improve determination accuracy on stream channel topography required by the hydraulic model. Initial Manning's n roughness coefficient values are based on pebble count field surveys and empirical formulas. Various theoretical probability distributions are fitted and evaluated on their accuracy to represent the estimated roughness values. Finally, Latin Hypercube Sampling has been used for generation of different sets of Manning roughness values and flood inundation probability maps have been created with the use of Monte Carlo simulations. Historical flood extent data, from an extreme historical flash flood event, are used for validation of the method. The calibration process is based on a binary wet-dry reasoning with the use of Median Absolute Percentage Error evaluation metric. The results show that the proposed procedure supports probabilistic flood hazard mapping at ungauged rivers and provides water resources managers with valuable information for planning and implementing flood risk mitigation strategies.

Highlights

  • Natural hazards have caused significant damages to natural and manmade environments during the last few decades

  • The 1-D HECRAS model is applied for probabilistic flood inundation mapping based on roughness coefficient values

  • The estimation of the inflow flood hydrograph based on the implementation of the Clark Instantaneous Unit Hydrograph (CIUH) on the inlet of the study stream reach for the extreme observed rainfall hyetograph on that day gave the inflow flood hydrograph (Fig. 5)

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Summary

Introduction

Natural hazards have caused significant damages to natural and manmade environments during the last few decades. Floodplain mapping and flood risk assessment have been mainly assessed using one-dimensional (1-D) and two-dimensional (2-D) hydraulic models (e.g.; Aronica et al, 2002; Horritt et al, 2007; Costabile and Macchione, 2015; Papaioannou et al, 2016). These models are able to simulate floodplain inundation and river hydraulics as demonstrated in many studies Most of these studies have been carried out at gauged watersheds using information from hydrometric stations with discharge data and stage/discharge relationships which limit the application of these models in accurate

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