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

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...

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Main Authors: Julio Garrote, Miguel González-Jiménez, Carolina Guardiola-Albert, Andrés Díez-Herrero
Format: Article
Language:English
Published: MDPI AG 2021-10-01
Series:Applied Sciences
Subjects:
Online Access:https://www.mdpi.com/2076-3417/11/19/9267
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author Julio Garrote
Miguel González-Jiménez
Carolina Guardiola-Albert
Andrés Díez-Herrero
author_facet Julio Garrote
Miguel González-Jiménez
Carolina Guardiola-Albert
Andrés Díez-Herrero
author_sort Julio Garrote
collection DOAJ
description 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 <i>n</i> value inside the riverbed. The use of abnormally low Manning’s <i>n</i> 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 <i>n</i> values) to only about 10 cm (models without bathymetry and “calibrated” Manning’s <i>n</i> values), was propagated towards a reduction in the estimation of direct flood damage, which fell from 25–30% to about 5%.
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spelling doaj.art-e1069f8888074e5cbe8ce6af4de02e852023-11-22T15:50:12ZengMDPI AGApplied Sciences2076-34172021-10-011119926710.3390/app11199267The 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 SpainJulio Garrote0Miguel González-Jiménez1Carolina Guardiola-Albert2Andrés Díez-Herrero3Department of Geodynamics, Stratigraphy, and Paleontology, Faculty of Geology, Complutense University of Madrid, 28040 Madrid, SpainGeological Hazards Division, Geological Survey of Spain (IGME, CSIC), 28003 Madrid, SpainGeological Hazards Division, Geological Survey of Spain (IGME, CSIC), 28003 Madrid, SpainGeological Hazards Division, Geological Survey of Spain (IGME, CSIC), 28003 Madrid, SpainThe 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 <i>n</i> value inside the riverbed. The use of abnormally low Manning’s <i>n</i> 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 <i>n</i> values) to only about 10 cm (models without bathymetry and “calibrated” Manning’s <i>n</i> values), was propagated towards a reduction in the estimation of direct flood damage, which fell from 25–30% to about 5%.https://www.mdpi.com/2076-3417/11/19/9267flood riskcultural heritage sitesbathymetric datamanning’s roughness coefficienthydrodynamic modelling
spellingShingle Julio Garrote
Miguel González-Jiménez
Carolina Guardiola-Albert
Andrés Díez-Herrero
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
Applied Sciences
flood risk
cultural heritage sites
bathymetric data
manning’s roughness coefficient
hydrodynamic modelling
title 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
title_full 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
title_fullStr 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
title_full_unstemmed 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
title_short 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
title_sort 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
topic flood risk
cultural heritage sites
bathymetric data
manning’s roughness coefficient
hydrodynamic modelling
url https://www.mdpi.com/2076-3417/11/19/9267
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