Coupling a global hydrodynamic algorithm and a regional hydrological model for large-scale flood inundation simulations

被引:15
|
作者
Huang, Shaochun [1 ,2 ]
Hattermann, Fred F. [2 ]
机构
[1] Norwegian Water Resources & Energy Directorate NV, POB 5091, N-0301 Oslo, Norway
[2] Potsdam Inst Climate Impact Res, POB 601203, D-14412 Potsdam, Germany
来源
HYDROLOGY RESEARCH | 2018年 / 49卷 / 02期
关键词
CaMa-flood; flood inundation simulation; large scale; Mulde; SWIM; RISK;
D O I
10.2166/nh.2017.061
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
To bridge the gap between 1D and 2D hydraulic models for regional scale assessment and global river routing models, we coupled the CaMa-Flood (Catchment-based Macro -scale Floodplain) model and the regional hydrological model SWIM (Soil and Water Integrated Model) as a tool for large-scale flood risk assessments. As a proof-of-concept study, we tested the coupled models in a meso-scale catchment in Germany. The Mulde River has a catchment area of ca. 6,171 km(2) and is a sub-catchment of the Elbe River. The modified CaMa-Flood model routes the sub -basin -based daily runoff generated by SWIM along the river network and estimates the river discharge as well as flood inundation areas. The results show that the CaMa-Flood hydrodynamic algorithm can reproduce the daily discharges from 1991 to 2003 well. It outperforms the Muskingum flow routing method (the default routing method in the SWIM) for the 2002 extreme flood event. The simulated flood inundation area in August 2002 is comparable with the observations along the main river. However, problems may occur in upstream areas. The results presented here show the potential of the coupled models for flood risk assessments along large rivers.
引用
收藏
页码:438 / 449
页数:12
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