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dc.contributor.authorFernández-Novoa, Diego
dc.contributor.authorGarcía-Feal, Orlando
dc.contributor.authorGonzález-Cao, José
dc.contributor.authorDeCastro, Maite
dc.contributor.authorGómez-Gesteira, Moncho
dc.date.accessioned2023-03-17T17:25:20Z
dc.date.available2023-03-17T17:25:20Z
dc.date.issued2022
dc.identifier.citationFernández-Nóvoa, D., García-Feal, O., González-Cao, J., deCastro, M., and Gómez-Gesteira, M.: Multiscale flood risk assessment under climate change: the case of the Miño River in the city of Ourense, Spain, Nat. Hazards Earth Syst. Sci., 22, 3957–3972, https://doi.org/10.5194/nhess-22-3957-2022, 2022.es_ES
dc.identifier.urihttp://hdl.handle.net/2183/32715
dc.description.abstract[Abstract:] River floods, which are one of the most dangerous natural hazards worldwide, have increased in intensity and frequency in recent decades as a result of climate change, and the future scenario is expected to be even worse. Therefore, their knowledge, predictability, and mitigation represent a key challenge for the scientific community in the coming decades, especially in those local areas that are most vulnerable to these extreme events. In this sense, a multiscale analysis is essential to obtain detailed maps of the future evolution of floods. In the multiscale analysis, the historical and future precipitation data from the CORDEX (Coordinated Regional Downscaling Experiment) project are used as input in a hydrological model (HEC-HMS) which, in turn, feeds a 2D hydraulic model (Iber+). This integration allows knowing the projected future changes in the flow pattern of the river, as well as analyzing the impact of floods in vulnerable areas through the flood hazard maps obtained with hydraulic simulations. The multiscale analysis is applied to the case of the Miño-Sil basin (NW Spain), specifically to the city of Ourense. The results show a delay in the flood season and an increase in the frequency and intensity of extreme river flows in the Miño-Sil basin, which will cause more situations of flooding in many areas frequented by pedestrians and in important infrastructure of the city of Ourense. In addition, an increase in water depths associated with future floods was also detected, confirming the trend for future floods to be not only more frequent but also more intense. Detailed maps of the future evolution of floods also provide key information to decision-makers to take effective measures in advance in those areas most vulnerable to flooding in the coming decades. Although the methodology presented is applied to a particular area, its strength lies in the fact that its implementation in other basins and cities is simple, also taking into account that all the models used are freely accessible.es_ES
dc.description.sponsorshipXunta de Galicia; ED431C 2021/44es_ES
dc.description.sponsorshipFEDER; 0034_RISC_ML_6_Ees_ES
dc.description.sponsorshipXunta de Galicia; ED481B-2021-108es_ES
dc.language.isoenges_ES
dc.publisherEuropean Geosciences Uniones_ES
dc.relation.urihttps://doi.org/10.5194/nhess-22-3957-2022es_ES
dc.rightsAtribución 3.0 Españaes_ES
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/es/*
dc.subjectPrecipitation dataes_ES
dc.subjectCORDEX projectes_ES
dc.subjectCoordinated Regional Downscaling Experimentes_ES
dc.subjectHydrological modelses_ES
dc.subjectHEC-HMSes_ES
dc.subjectHydraulic modelses_ES
dc.subjectIber+es_ES
dc.subjectMiño-Sil basines_ES
dc.subjectFloodses_ES
dc.titleMultiscale flood risk assessment under climate change: the case of the Miño river in the city of Ourense, Spaines_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccesses_ES
UDC.journalTitleNatural Hazards and Earth System Scienceses_ES
UDC.volume22es_ES
UDC.issue12es_ES
UDC.startPage3957es_ES
UDC.endPage3972es_ES
dc.identifier.doi10.5194/nhess-22-3957-2022


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