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dc.contributor.authorÁvila, Leandropt_BR
dc.contributor.authorSilveira, Reinaldo Bomfim dapt_BR
dc.contributor.authorCampos, Andrépt_BR
dc.contributor.authorSilva, Nathalli Rogiski dapt_BR
dc.contributor.authorGonçalves, José Eduardopt_BR
dc.contributor.authorAlmeida, Arlan Scortegagnapt_BR
dc.contributor.authorFreitas, Camilapt_BR
dc.contributor.authorAver, Cássia Silmarapt_BR
dc.contributor.authorFan, Fernando Mainardipt_BR
dc.date.accessioned2023-01-02T05:09:06Zpt_BR
dc.date.issued2022pt_BR
dc.identifier.issn2073-4441pt_BR
dc.identifier.urihttp://hdl.handle.net/10183/253326pt_BR
dc.description.abstractHydrological modeling is an important tool for water resources management, providing a feasible solution to represent the main hydrological processes and predict future streamflow regimes. The literature presents a set of hydrological models commonly used to represent the rainfallrunoff process in watersheds with different meteorological and geomorphological characteristics. The response of such models could differ significantly for a single precipitation event, given the uncertainties associated with the input data, parameters, and model structure. In this way, a correct hydrological representation of a watershed should include the evaluation of different hydrological models. This study explores the use and performance of five hydrological models to represent daily streamflow regimes at six hydropower plants located in the Tocantins river basin (Brazil). The adopted models include the GR4J, HYMOD, HBV, SMAP, and MGB-IPH. The evaluation of each model was elaborated considering the calibration (2014–2019) and validation period (2005–2010) using observed data of precipitation and climatological variables. Deterministic metrics and statistical tests were used to measure the performance of each model. For the calibration stage, results show that all models achieved a satisfactory performance with NSE values greater than 0.6. For the validation stage, only the MGB-IPH model present a good performance with NSE values greater than 0.7. A bias correction procedure were applied to correct the simulated data of conceptual models. However, the statistical tests exposed that only the MGB-IPH model could preserve the main statistical properties of the observed data. Thus, this study discusses and presents some limitations of the lumped model to represent daily streamflows in large-scale river basins (>50,000 km²).en
dc.format.mimetypeapplication/pdfpt_BR
dc.language.isoengpt_BR
dc.relation.ispartofWater. Basel. Vol. 14, n. 19 (Oct. 2022), [Article] 3013, 21 p.pt_BR
dc.rightsOpen Accessen
dc.subjectHydrological modelen
dc.subjectGestão de recursos hídricospt_BR
dc.subjectWater balanceen
dc.subjectVazões : Simulaçãopt_BR
dc.subjectHydropower planten
dc.subjectModelos hidrológicospt_BR
dc.subjectWater resourcesen
dc.subjectGrandes baciaspt_BR
dc.subjectUsinas hidrelétricaspt_BR
dc.subjectTocantins, Rio, Baciapt_BR
dc.titleComparative evaluation of five hydrological models in a large-scale and tropical river basinpt_BR
dc.typeArtigo de periódicopt_BR
dc.identifier.nrb001154152pt_BR
dc.type.originEstrangeiropt_BR


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