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dc.contributor.authorManz, B.
dc.contributor.authorBuytaert, W.
dc.contributor.authorZulkafli, Z.
dc.contributor.authorLavado-Casimiro, W.
dc.contributor.authorWillems, B.
dc.contributor.authorRobles, L.A.
dc.contributor.authorRodríguez-Sánchez, Juan-Pablo
dc.coverage.spatialAndes
dc.date.accessioned2020-03-24T01:37:19Z
dc.date.available2020-03-24T01:37:19Z
dc.date.issued2016-02-09
dc.identifier.citation"Manz, B., W. Buytaert, Z. Zulkafli, W. Lavado, B. Willems, L. A. Robles, and J.-P. Rodríguez-Sánchez (2016), High-resolution satellite-gauge merged precipitation climatologies of the Tropical Andes, J. Geophys. Res. Atmos., 121, 1190–1207, doi:10.1002/2015JD023788."en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12542/300
dc.description.abstractSatellite precipitation products are becoming increasingly useful to complement rain gauge networks in regions where these are too sparse to capture spatial precipitation patterns, such as in the Tropical Andes. The Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (TPR) was active for 17 years (1998–2014) and has generated one of the longest single-sensor, high-resolution, and high accuracy rainfall records. In this study, high-resolution (5 km) gridded mean monthly climatological precipitation is derived from the raw orbital TPR data (TRMM 2A25) and merged with 723 rain gauges using multiple satellite-gauge (S-G) merging approaches. The resulting precipitation products are evaluated by cross validation and catchment water balances (runoff ratios) for 50 catchments across the Tropical Andes. Results show that the TPR captures major synoptic and seasonal precipitation patterns and also accurately defines orographic gradients but underestimates absolute monthly rainfall rates. The S-G merged products presented in this study constitute an improved source of climatological rainfall data, outperforming the gridded TPR product as well as a rain gauge-only product based on ordinary Kriging. Among the S-G merging methods, performance of inverse distance interpolation of satellite-gauge residuals was similar to that of geostatistical methods, which were more sensitive to gauge network density. High uncertainty and low performance of the merged precipitation products predominantly affected regions with low and intermittent precipitation regimes (e.g., Peruvian Pacific coast) and is likely linked to the low TPR sampling frequency. All S-G merged products presented in this study are available in the public domain.en_US
dc.formatapplication/pdf
dc.language.isoengen_US
dc.publisherWiley-Blackwellen_US
dc.relation.ispartofurn:issn:2156-2202
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.subjectPrecipitationen_US
dc.subjectCalibraciónes_PE
dc.subjectClima Tropicales_PE
dc.subjectMétodo de Evaluaciónes_PE
dc.subjectSatélitees_PE
dc.subjectRadares_PE
dc.titleHigh-resolution satellite-gauge merged precipitation climatologies of the tropical Andesen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.identifier.isni0000 0001 0746 0446
dc.description.peerreviewPor pares
dc.identifier.doihttps://doi.org/10.1002/2015JD023788.
dc.identifier.journalJournal of Geophysical Research
dc.source.volume121
dc.source.initialpage1190
dc.source.endpage1207
dc.subject.ocdeClimatologíaes_PE
dc.subject.ocdehttps://purl.org/pe-repo/ocde/ford#1.05.10


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