The Manning's Roughness Coefficient Calibration Method to Improve Flood Hazard Analysis in the Absence of River Bathymetric Data: Application to the Urban Historical Zamora City Centre in Spain

被引:17
|
作者
Garrote, Julio [1 ]
Gonzalez-Jimenez, Miguel [2 ]
Guardiola-Albert, Carolina [2 ]
Diez-Herrero, Andres [2 ]
机构
[1] Univ Complutense Madrid, Fac Geol, Dept Geodynam Stratig & Paleontol, Madrid 28040, Spain
[2] CSIC, IGME, Geol Survey Spain, Geol Hazards Div, Madrid 28003, Spain
来源
APPLIED SCIENCES-BASEL | 2021年 / 11卷 / 19期
关键词
flood risk; cultural heritage sites; bathymetric data; manning's roughness coefficient; hydrodynamic modelling; CULTURAL-HERITAGE; DAMAGE FUNCTIONS; TOPOGRAPHIC DATA; MODEL; INUNDATION;
D O I
10.3390/app11199267
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Featured Application</p> The methodology proposed in this manuscript makes it possible to improve the estimation of flood zones and their flow depth values in situations where there are no available bathymetric data of the channel (or they are scarce and do not allow for its shape reconstruction). It could improve flood risk assessment too.</p> The accurate estimation of flood risk depends on, among other factors, a correct delineation of the floodable area and its associated hydrodynamic parameters. This characterization becomes fundamental in the flood hazard analyses that are carried out in urban areas. To achieve this objective, it is necessary to have a correct characterization of the topography, both inside the riverbed (bathymetry) and outside it. Outside the riverbed, the LiDAR data led to an important improvement, but not so inside the riverbed. To overcome these deficiencies, different models with simplified bathymetry or modified inflow hydrographs were used. Here, we present a model that is based upon the calibration of the Manning's n value inside the riverbed. The use of abnormally low Manning's n values made it possible to reproduce both the extent of the flooded area and the flow depth value within it (outside the riverbed) in an acceptable manner. The reduction in the average error in the flow depth value from 50-75 cm (models without bathymetry and "natural " Manning's n values) to only about 10 cm (models without bathymetry and "calibrated " Manning's n values), was propagated towards a reduction in the estimation of direct flood damage, which fell from 25-30% to about 5%.</p>
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页数:21
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