Influence of dike breaches on flood frequency estimation

被引:69
作者
Apel, H. [1 ]
Merz, B. [1 ]
Thieken, A. H. [1 ]
机构
[1] GeoForschungsZentrum Potsdam GFZ, D-14473 Potsdam, Germany
关键词
Flood frequency; Dike breach; Floodplain retention; Probabilistic dynamic modelling; CHANGING CLIMATE; RHINE; RISK; UNCERTAINTY; INUNDATION; SIMULATION; IMPACT; RIVER;
D O I
10.1016/j.cageo.2007.11.003
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Many river floodplains and their assets are protected by dikes. In case of extreme flood events, dikes may breach and floodwater may spill over into the dike hinterland. Depending on the specific situation, e.g. time and location of breach, and the capacity of the hinterland to contain the floodwater, dike breaches may lead to significant reductions of flood peaks downstream of breach locations. However, the influence of dike breaches on flood frequency distributions along rivers has not been systematically analysed. In order to quantify this influence, a dynamic-probabilistic model is developed. This model combines simplified flood process modules in a Monte Carlo framework. The simplifications allow for the simulation of a large number of different scenarios, taking into account the main physical processes. By using a Monte Carlo approach, frequency distributions can be derived from the simulations. In this way, process understanding and the characteristics of the river-dike-floodplain system are included in the derivation of flood frequency statements. The dynamic-probabilistic model is applied to the Lower Rhine in Germany and compared to the usually used flood frequency analysis. For extreme floods, the model simulates significant retention effects due to dike breaches, which lead to significant modifications of the flood frequency curve downstream of breach locations. The resulting probabilistic statements are much more realistic than those of the flood frequency approach, since the dynamic-probabilistic model incorporates all important flood process, i.e. dike breaching, that only occurs when a certain threshold is reached. Beyond this point, the behaviour of the flood frequency curve is dominated by this process. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:907 / 923
页数:17
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