Floodplain Terrain Analysis for Coarse Resolution 2D Flood Modeling

Hydraulic modeling is a fundamental tool for managing and mitigating flood risk. Developing low resolution hydraulic models, providing consistent inundation simulations with shorter running time, as compared to high-resolution modeling, has a variety of potential applications. Rapid coarse resolutio...

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Main Authors: Francisco Peña, Fernando Nardi
Format: Article
Language:English
Published: MDPI AG 2018-09-01
Series:Hydrology
Subjects:
Online Access:http://www.mdpi.com/2306-5338/5/4/52
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author Francisco Peña
Fernando Nardi
author_facet Francisco Peña
Fernando Nardi
author_sort Francisco Peña
collection DOAJ
description Hydraulic modeling is a fundamental tool for managing and mitigating flood risk. Developing low resolution hydraulic models, providing consistent inundation simulations with shorter running time, as compared to high-resolution modeling, has a variety of potential applications. Rapid coarse resolution flood models can support emergency management operations as well as the coupling of hydrodynamic modeling with climate, landscape and environmental models running at the continental scale. This work sought to investigate the uncertainties of input parameters and bidimensional (2D) flood wave routing simulation results when simplifying the terrain mesh size. A procedure for fluvial channel bathymetry interpolation and floodplain terrain data resampling was investigated for developing upscaled 2D inundation models. The proposed terrain processing methodology was tested on the Tiber River basin evaluating coarse (150 m) to very coarse (up to 700 m) flood hazard modeling results. The use of synthetic rectangular cross sections, replacing surveyed fluvial channel sections, was also tested with the goal of evaluating the potential use of geomorphic laws providing channel depth, top width and flow area when surveyed data are not available. Findings from this research demonstrate that fluvial bathymetry simplification and DTM resampling is feasible when the terrain data resampling and fluvial cross section interpolation are constrained to provide consistent representation of floodplain morphology, river thalweg profile and channel flow area. Results show the performances of low-resolution inundation simulations running in seconds while maintaining a consistent representation of inundation extents and depths.
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spelling doaj.art-81564568de434a7e9c37b62bb11203ab2022-12-22T02:53:06ZengMDPI AGHydrology2306-53382018-09-01545210.3390/hydrology5040052hydrology5040052Floodplain Terrain Analysis for Coarse Resolution 2D Flood ModelingFrancisco Peña0Fernando Nardi1Water Resources Research and Documentation Center (WARREDOC), University for Foreigners of Perugia, 06123 Perugia, ItalyDepartment of Civil and Environmental Engineering (DICEA), University of Florence, 50139 Florence, ItalyHydraulic modeling is a fundamental tool for managing and mitigating flood risk. Developing low resolution hydraulic models, providing consistent inundation simulations with shorter running time, as compared to high-resolution modeling, has a variety of potential applications. Rapid coarse resolution flood models can support emergency management operations as well as the coupling of hydrodynamic modeling with climate, landscape and environmental models running at the continental scale. This work sought to investigate the uncertainties of input parameters and bidimensional (2D) flood wave routing simulation results when simplifying the terrain mesh size. A procedure for fluvial channel bathymetry interpolation and floodplain terrain data resampling was investigated for developing upscaled 2D inundation models. The proposed terrain processing methodology was tested on the Tiber River basin evaluating coarse (150 m) to very coarse (up to 700 m) flood hazard modeling results. The use of synthetic rectangular cross sections, replacing surveyed fluvial channel sections, was also tested with the goal of evaluating the potential use of geomorphic laws providing channel depth, top width and flow area when surveyed data are not available. Findings from this research demonstrate that fluvial bathymetry simplification and DTM resampling is feasible when the terrain data resampling and fluvial cross section interpolation are constrained to provide consistent representation of floodplain morphology, river thalweg profile and channel flow area. Results show the performances of low-resolution inundation simulations running in seconds while maintaining a consistent representation of inundation extents and depths.http://www.mdpi.com/2306-5338/5/4/52DTMterrain analysishydraulic geometrylarge scale2D hydraulic modelingscaling in hydrology
spellingShingle Francisco Peña
Fernando Nardi
Floodplain Terrain Analysis for Coarse Resolution 2D Flood Modeling
Hydrology
DTM
terrain analysis
hydraulic geometry
large scale
2D hydraulic modeling
scaling in hydrology
title Floodplain Terrain Analysis for Coarse Resolution 2D Flood Modeling
title_full Floodplain Terrain Analysis for Coarse Resolution 2D Flood Modeling
title_fullStr Floodplain Terrain Analysis for Coarse Resolution 2D Flood Modeling
title_full_unstemmed Floodplain Terrain Analysis for Coarse Resolution 2D Flood Modeling
title_short Floodplain Terrain Analysis for Coarse Resolution 2D Flood Modeling
title_sort floodplain terrain analysis for coarse resolution 2d flood modeling
topic DTM
terrain analysis
hydraulic geometry
large scale
2D hydraulic modeling
scaling in hydrology
url http://www.mdpi.com/2306-5338/5/4/52
work_keys_str_mv AT franciscopena floodplainterrainanalysisforcoarseresolution2dfloodmodeling
AT fernandonardi floodplainterrainanalysisforcoarseresolution2dfloodmodeling