Performance assessment of two-dimensional hydraulic models for generation of flood inundation maps in mountain river basins

dc.contributor.authorTimbe Castro, Luis Manuel
dc.date.accessioned2020-05-06T22:42:54Z
dc.date.available2020-05-06T22:42:54Z
dc.date.issued2019
dc.descriptionHydraulic models for the generation of flood inundation maps are not commonly applied in mountain river basins because of the difficulty in modeling the hydraulic behavior and the complex topography. This paper presents a comparative analysis of the performance of four two-dimensional hydraulic models (HEC-RAS 2D, Iber 2D, Flood Modeller 2D, and PCSWMM 2D) with respect to the generation of flood inundation maps. The study area covers a 5-km reach of the Santa Barbara River located in the Ecuadorian Andes, at 2330 masl, in Gualaceo. The model's performance was evaluated based on the water surface elevation and flood extent, in terms of the mean absolute difference and measure of fit. The analysis revealed that, for a given case, Iber 2D has the best performance in simulating the water level and inundation for flood events with 20- and 50-year return periods, respectively, followed by Flood Modeller 2D, HEC-RAS 2D, and PCSWMM 2D in terms of their performance. Grid resolution, the way in which hydraulic structures are mimicked, the model code, and the default value of the parameters are considered the main sources of prediction uncertainty.
dc.description.abstractAbstract Hydraulic models for the generation of flood inundation maps are not commonly applied in mountain river basins because of the difficulty in modeling the hydraulic behavior and the complex topography. This paper presents a comparative analysis of the performance of four two-dimensional hydraulic models (HEC-RAS 2D, Iber 2D, Flood Modeller 2D, and PCSWMM 2D) with respect to the generation of flood inundation maps. The study area covers a 5-km reach of the Santa Barbara River located in the Ecuadorian Andes, at 2330 masl, in Gualaceo. The model's performance was evaluated based on the water surface elevation and flood extent, in terms of the mean absolute difference and measure of fit. The analysis revealed that, for a given case, Iber 2D has the best performance in simulating the water level and inundation for flood events with 20- and 50-year return periods, respectively, followed by Flood Modeller 2D, HEC-RAS 2D, and PCSWMM 2D in terms of their performance. Grid resolution, the way in which hydraulic structures are mimicked, the model code, and the default value of the parameters are considered the main sources of prediction uncertainty.
dc.identifier.doi10.1016/j.wse.2019.03.001
dc.identifier.issn1674-2370
dc.identifier.urihttp://dspace.ucuenca.edu.ec/handle/123456789/34234
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85064252627&origin=inward
dc.language.isoes_ES
dc.sourceWater Science and Engineering
dc.subjectFlood extent
dc.titlePerformance assessment of two-dimensional hydraulic models for generation of flood inundation maps in mountain river basins
dc.typeARTÍCULO
dc.ucuenca.afiliacionTimbe, L., Universidad de Cuenca, Departamento de Recursos Hídricos y Ciencias Ambientales, Cuenca, Ecuador
dc.ucuenca.areaconocimientofrascatiamplio2. Ingeniería y Tecnología
dc.ucuenca.areaconocimientofrascatidetallado2.1.1 Ingeniería Civil
dc.ucuenca.areaconocimientofrascatiespecifico2.1 Ingeniería Civil
dc.ucuenca.areaconocimientounescoamplio07 - Ingeniería, Industria y Construcción
dc.ucuenca.areaconocimientounescodetallado0732 - Construcción e Ingeniería Civil
dc.ucuenca.areaconocimientounescoespecifico073 - Arquitectura y Construcción
dc.ucuenca.correspondenciaPinos Flores, Juan Andres, juan.pinosf@ucuenca.edu.ec
dc.ucuenca.cuartilQ2
dc.ucuenca.embargoend2050-12-31
dc.ucuenca.embargointerno2050-12-31
dc.ucuenca.factorimpacto0.39
dc.ucuenca.idautor0104915558
dc.ucuenca.indicebibliograficoSCOPUS
dc.ucuenca.numerocitaciones0
dc.ucuenca.urifuentehttps://www.sciencedirect.com/journal/water-science-and-engineering/vol/12/issue/1
dc.ucuenca.versionVersión publicada
dc.ucuenca.volumenVolumen 12, número 1

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