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dc.contributor.authorMuñoz Pauta, Paul Andres-
dc.contributor.authorOrellana Alvear, Johanna Marlene-
dc.contributor.authorWillems, Patrick-
dc.contributor.authorCelleri Alvear, Rolando Enrique-
dc.date.accessioned2019-07-31T15:51:51Z-
dc.date.available2019-07-31T15:51:51Z-
dc.date.issued2018-
dc.identifier.issn20734441-
dc.identifier.urihttp://dspace.ucuenca.edu.ec/handle/123456789/33168-
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85055719343&origin=inward-
dc.descriptionFlash-flood forecasting has emerged worldwide due to the catastrophic socio-economic impacts this hazard might cause and the expected increase of its frequency in the future. In mountain catchments, precipitation-runoff forecasts are limited by the intrinsic complexity of the processes involved, particularly its high rainfall variability. While process-based models are hard to implement, there is a potential to use the random forest algorithm due to its simplicity, robustness and capacity to deal with complex data structures. Here a step-wise methodology is proposed to derive parsimonious models accounting for both hydrological functioning of the catchment (eg, input data, representation of antecedent moisture conditions) and random forest procedures (eg, sensitivity analyses, dimension reduction, optimal input composition). The methodology was applied to develop short-term prediction models of varying time duration (4, 8, 12, 18 and 24 h) for a catchment representative of the Ecuadorian Andes. Results show that the derived parsimonious models can reach validation efficiencies (Nash-Sutcliffe coefficient) from 0.761 (4-h) to 0.384 (24-h) for optimal inputs composed only by features accounting for 80% of the model’s outcome variance. Improvement in the prediction of extreme peak flows was demonstrated (extreme value analysis) by including precipitation information in contrast to the use of pure autoregressive models. View Full-Text-
dc.description.abstractFlash-flood forecasting has emerged worldwide due to the catastrophic socio-economic impacts this hazard might cause and the expected increase of its frequency in the future. In mountain catchments, precipitation-runoff forecasts are limited by the intrinsic complexity of the processes involved, particularly its high rainfall variability. While process-based models are hard to implement, there is a potential to use the random forest algorithm due to its simplicity, robustness and capacity to deal with complex data structures. Here a step-wise methodology is proposed to derive parsimonious models accounting for both hydrological functioning of the catchment (eg, input data, representation of antecedent moisture conditions) and random forest procedures (eg, sensitivity analyses, dimension reduction, optimal input composition). The methodology was applied to develop short-term prediction models of varying time duration (4, 8, 12, 18 and 24 h) for a catchment representative of the Ecuadorian Andes. Results show that the derived parsimonious models can reach validation efficiencies (Nash-Sutcliffe coefficient) from 0.761 (4-h) to 0.384 (24-h) for optimal inputs composed only by features accounting for 80% of the model’s outcome variance. Improvement in the prediction of extreme peak flows was demonstrated (extreme value analysis) by including precipitation information in contrast to the use of pure autoregressive models. View Full-Text-
dc.language.isoes_ES-
dc.sourceWater (Switzerland)-
dc.subjectFlash-Flood-
dc.subjectForecasting-
dc.subjectLag Analysis-
dc.subjectMachine Learning-
dc.subjectPrecipitation-Runoff-
dc.subjectRandom Forest-
dc.titleFlash-flood forecasting in an andean mountain catchment-development of a step-wise methodology based on the random forest algorithm-
dc.typeARTÍCULO-
dc.ucuenca.idautor0104645619-
dc.ucuenca.idautor0104162268-
dc.ucuenca.idautorSgrp-1371-3-
dc.ucuenca.idautor0602794406-
dc.identifier.doi10.3390/w10111519-
dc.ucuenca.versionVersión publicada-
dc.ucuenca.areaconocimientounescoamplio05 - Ciencias Físicas, Ciencias Naturales, Matemáticas y Estadísticas-
dc.ucuenca.afiliacionMuñoz, P., Universidad de Cuenca, Departamento de Recursos Hídricos y Ciencias Ambientales, Cuenca, Ecuador; Muñoz, P., Universidad de Lovaina, Heverlee, Belgica-
dc.ucuenca.afiliacionOrellana, J., Universidad de Cuenca, Departamento de Recursos Hídricos y Ciencias Ambientales, Cuenca, Ecuador; Orellana, J., University of Marburg, Marburg, Alemania-
dc.ucuenca.afiliacionWillems, P., Universidad de Lovaina, Heverlee, Belgica-
dc.ucuenca.afiliacionCelleri, R., Universidad de Cuenca, Departamento de Recursos Hídricos y Ciencias Ambientales, Cuenca, Ecuador; Celleri, R., Universidad de Cuenca, Facultad de Ingeniería, Cuenca, Ecuador-
dc.ucuenca.correspondenciaMuñoz Pauta, Paul Andres, paul.andres.munoz@gmail.com-
dc.ucuenca.volumenvolumen 10, número 11-
dc.ucuenca.indicebibliograficoSCOPUS-
dc.ucuenca.factorimpacto0.67-
dc.ucuenca.cuartilQ2-
dc.ucuenca.numerocitaciones2-
dc.ucuenca.areaconocimientofrascatiamplio1. Ciencias Naturales y Exactas-
dc.ucuenca.areaconocimientofrascatiespecifico1.5 Ciencias de la Tierra y el Ambiente-
dc.ucuenca.areaconocimientofrascatidetallado1.5.10 Recursos Hídricos-
dc.ucuenca.areaconocimientounescoespecifico052 - Medio Ambiente-
dc.ucuenca.areaconocimientounescodetallado0522 - Medio Ambiente y Vida Silvestre-
dc.ucuenca.urifuentehttps://www.scimagojr.com/journalsearch.php?q=21100255400&tip=sid&clean=0-
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