Non-stationary hydrological regimes due to climate change: the impact of future precipitation in the spillway design of a reservoir, case study: sube y baja dam, in Ecuador

dc.contributor.authorHerbozo Alvarado, Jorge Enriqu
dc.contributor.authorHaro Ruiz, Patricia Lorena
dc.contributor.authorMinaya, Verónica Graciela
dc.contributor.authorGuerra, María José
dc.contributor.authorMuñoz, Luis Eduardo
dc.contributor.authorCampozano Parra, Lenin Vladimir
dc.contributor.authorManciati Jaramillo, Carla Paola
dc.contributor.authorCarrillo Serrano, Verónica Margarita
dc.date.accessioned2023-01-25T17:32:32Z
dc.date.available2023-01-25T17:32:32Z
dc.date.issued2022
dc.description.abstractChanges in flood loads and reservoir levels, produced by climate change (CC), represent an increasing concern for dam safety managers and downstream populations, highlighting the need to define adaptation strategies based on the dam failure risk management framework. Currently, thousands of dams worldwide, varying in use, age, and maintenance, may represent a threat to downstream cities in the case of structural failure. Several studies relate the failure of dams to several issues in the spillway, which may be even more vulnerable in CC conditions. This study provides a review of dam safety threats due to CC and approaches for the design/redesign of the spillway to cope with CC. A general four-stage methodology is proposed: data gathering and hydro-climatic, hydrological, and hydraulic analyses. Afterward, this methodology is applied to the spillway design for the Sube y Baja dam in Ecuador. The Probable Maximum Precipitation (PMP) increases around 20% considering CC under the Representative Concentration Pathway 8.5. Such an increment derived a 25% increase in the spillway maximum flow. These results show that the non-stationary hydrological regimes related to CC require a revision of engineering design criteria for hydraulic structures in general, and call for a consensus on design variables under CC.
dc.identifier.doi10.3390/atmos13050828
dc.identifier.issn2073-4433
dc.identifier.urihttp://dspace.ucuenca.edu.ec/handle/123456789/40879
dc.identifier.urihttps://doi.org/10.3390/atmos13050828
dc.language.isoes_ES
dc.sourceAtmosphere
dc.subjectProbable maximum precipitation
dc.subjectSpillway
dc.subjectDam risks
dc.subjectClimate change
dc.titleNon-stationary hydrological regimes due to climate change: the impact of future precipitation in the spillway design of a reservoir, case study: sube y baja dam, in Ecuador
dc.typeARTÍCULO
dc.ucuenca.afiliacionHerbozo, J., Escuela Politécnica Nacional (EPN), Quito, Ecuador
dc.ucuenca.afiliacionLuis, M., Escuela Politécnica Nacional (EPN), Quito, Ecuador
dc.ucuenca.afiliacionGuerra, M., Escuela Politécnica Nacional (EPN), Quito, Ecuador
dc.ucuenca.afiliacionMinaya, V., Escuela Politécnica Nacional (EPN), Quito, Ecuador
dc.ucuenca.afiliacionHaro, P., Escuela Politécnica Nacional (EPN), Quito, Ecuador
dc.ucuenca.afiliacionCarrillo, V., Universidad de Cuenca, Facultad de Ingeniería, Cuenca, Ecuador
dc.ucuenca.afiliacionManciati, C., Escuela Politécnica Nacional (EPN), Quito, Ecuador
dc.ucuenca.afiliacionCampozano, L., Escuela Politécnica Nacional (EPN), Quito, Ecuador
dc.ucuenca.areaconocimientofrascatiamplio1. Ciencias Naturales y Exactas
dc.ucuenca.areaconocimientofrascatidetallado1.5.10 Recursos Hídricos
dc.ucuenca.areaconocimientofrascatiespecifico1.5 Ciencias de la Tierra y el Ambiente
dc.ucuenca.areaconocimientounescoamplio05 - Ciencias Físicas, Ciencias Naturales, Matemáticas y Estadísticas
dc.ucuenca.areaconocimientounescodetallado0521 - Ciencias Ambientales
dc.ucuenca.areaconocimientounescoespecifico052 - Medio Ambiente
dc.ucuenca.correspondenciaLuis Eduardo, Muñoz, luis.munoz01@epn.edu.ec
dc.ucuenca.cuartilQ2
dc.ucuenca.factorimpacto0.692
dc.ucuenca.idautor0000-0001-5612-3075
dc.ucuenca.idautor0904289055
dc.ucuenca.idautor0000-0003-1677-9816
dc.ucuenca.idautor57715508500
dc.ucuenca.idautor55653057700
dc.ucuenca.idautor0104040480
dc.ucuenca.idautor1713190104
dc.ucuenca.idautor0102677200
dc.ucuenca.indicebibliograficoSCOPUS
dc.ucuenca.numerocitaciones0
dc.ucuenca.urifuentehttps://www.mdpi.com/2073-4433/13/5
dc.ucuenca.versionVersión publicada
dc.ucuenca.volumenVolumen 13, número 5

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