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dc.contributor.authorFernández Palomino, Carlos
dc.contributor.authorHattermann, Fred
dc.contributor.authorKrysanova, Valentina
dc.contributor.authorLobanova, Anastasia
dc.contributor.authorVega Jácome, Fiorella
dc.contributor.authorLavado-Casimiro, W.
dc.contributor.authorSantini, William
dc.contributor.authorAybar Camacho, Cesar Luis
dc.contributor.authorBronstert, Axel
dc.date.accessioned2022-04-29T14:37:20Z
dc.date.available2022-04-29T14:37:20Z
dc.date.issued2022-03
dc.identifier.urihttps://hdl.handle.net/20.500.12542/2006
dc.description.abstractA novel approach for estimating precipitation patterns is developed here and applied to generate a new hydrologically corrected daily precipitation dataset, called RAIN4PE (Rain for Peru and Ecuador), at 0.18 spatial resolution for the period 1981–2015 covering Peru and Ecuador. It is based on the application of 1) the random forest method to merge multisource precipitation estimates (gauge, satellite, and reanalysis) with terrain elevation, and 2) observed and modeled streamflow data to first detect biases and second further adjust gridded precipitation by inversely applying the simulated results of the ecohydrological model SWAT (Soil and Water Assessment Tool). Hydrological results using RAIN4PE as input for the Peruvian and Ecuadorian catchments were compared against the ones when feeding other uncorrected (CHIRP and ERA5) and gaugecorrected (CHIRPS, MSWEP, and PISCO) precipitation datasets into the model. For that, SWAT was calibrated and validated at 72 river sections for each dataset using a range of performance metrics, including hydrograph goodness of fit andflow duration curve signatures. Results showed that gauge-corrected precipitation datasets outperformed uncorrected ones for streamflow simulation. However, CHIRPS, MSWEP, and PISCO showed limitations for streamflow simulation in several catchments draining into the Pacific Ocean and the Amazon River. RAIN4PE provided the best overall performance for streamflow simulation, including flow variability (low, high, and peak flows) and water budget closure. The overall good performance of RAIN4PE as input for hydrological modeling provides a valuable criterion of its applicability for robust countrywide hydrometeorological applications, including hydroclimatic extremes such as droughts and floods. © 2022 American Meteorological Society.es_PE
dc.formatapplication/pdfes_PE
dc.language.isospaes_PE
dc.publisherAmerican Meteorological Societyes_PE
dc.relation.urihttps://journals.ametsoc.org/view/journals/hydr/23/3/JHM-D-20-0285.1.xmles_PE
dc.rightsinfo:eu-repo/semantics/openAccesses_PE
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.sourceRepositorio Institucional - SENAMHIes_PE
dc.sourceServicio Nacional de Meteorología e Hidrología del Perúes_PE
dc.subjectPrecipitaciónes_PE
dc.subjectSouth Americaes_PE
dc.subjectAmazon Regiones_PE
dc.subjectMountain Meteorologyes_PE
dc.titleA Novel High-Resolution Gridded Precipitation Dataset for Peruvian and Ecuadorian Watersheds: Development and Hydrological Evaluationes_PE
dc.typeinfo:eu-repo/semantics/articlees_PE
dc.identifier.doihttps://doi.org/10.1175/JHM-D-20-0285.1
dc.identifier.journalJournal of Hydrometeorology
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.11es_PE
dc.subject.siniaprecipitacion - Clima y Eventos Naturales
dc.type.siniatext/publicacion cientifica
dc.identifier.urlhttps://hdl.handle.net/20.500.12542/2006


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