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dc.contributor.authorDerin, Y.
dc.contributor.authorAnagnostou, E.
dc.contributor.authorBerne, A.
dc.contributor.authorBorga, M.
dc.contributor.authorBoudevillain, Brice
dc.contributor.authorBuytaert, W.
dc.contributor.authorChang, Che-Hao
dc.contributor.authorDelrieu, Guy
dc.contributor.authorHong, Yang
dc.contributor.authorChia Hsu, Yung
dc.contributor.authorLavado-Casimiro, W.
dc.contributor.authorManz, Bastian
dc.contributor.authorMoges, Semu
dc.contributor.authorNikolopoulos, Efthymios I.
dc.contributor.authorSahlu, Dejene
dc.contributor.authorSalerno, Franco
dc.contributor.authorRodríguez-Sánchez, Juan-Pablo
dc.contributor.authorVergara, Humberto J.
dc.contributor.authorYilmaz, Koray K..
dc.date.accessioned2020-03-23T23:35:34Z
dc.date.available2020-03-23T23:35:34Z
dc.date.issued2016-06
dc.identifier.urihttps://hdl.handle.net/20.500.12542/298
dc.description.abstractAn extensive evaluation of nine global-scale high-resolution satellite-based rainfall (SBR) products is performed using a minimum of 6 years (within the period of 2000-13) of reference rainfall data derived from rain gauge networks in nine mountainous regions across the globe. The SBR products are compared to a recently released global reanalysis dataset from the European Centre for Medium-Range Weather Forecasts (ECMWF). The study areas include the eastern Italian Alps, the Swiss Alps, the western Black Sea of Turkey, the French Cévennes, the Peruvian Andes, the Colombian Andes, the Himalayas over Nepal, the Blue Nile in East Africa, Taiwan, and the U.S. Rocky Mountains. Evaluation is performed at annual, monthly, and daily time scales and 0.25° spatial resolution. The SBR datasets are based on the following retrieval algorithms: Tropical Rainfall Measuring Mission Multisatellite Precipitation Analysis (TMPA), the NOAA/Climate Prediction Center morphing technique (CMORPH), Precipitation Estimation from Remotely Sensed Information Using Artificial Neural Networks (PERSIANN), and Global Satellite Mapping of Precipitation (GSMaP). SBR products are categorized into those that include gauge adjustment versus unadjusted. Results show that performance of SBR is highly dependent on the rainfall variability. Many SBR products usually underestimate wet season and overestimate dry season precipitation. The performance of gauge adjustment to the SBR products varies by region and depends greatly on the representativeness of the rain gauge network.en_US
dc.formatapplication/pdf
dc.language.isoengen_US
dc.publisherAmerican Meteorological Societyen_US
dc.relation.ispartofurn:issn:1525-7541
dc.rightsinfo:eu-repo/semantics/openAccessen_US
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 - SENAMHIen_US
dc.sourceServicio Nacional de Meteorología e Hidrología del Perúen_US
dc.subjectSatéliteen_US
dc.subjectPrecipitaciónen_US
dc.subjectLluviaen_US
dc.subjectClimatología
dc.subjectHidrometeorología
dc.titleMultiregional satellite precipitation products evaluation over complex terrainen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.identifier.isni0000 0001 0746 0446
dc.description.peerreviewPor pares
dc.identifier.doihttps://doi.org/10.1175/JHM-D-15-0197.1
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.10


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