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Spatial downscaling of TRMM precipitation data based on the orographical effect and meteorological conditions in a mountainous area
Institution:1. Centro de Investigaciones del Mar y la Atmósfera, CONICET-UBA, Buenos Aires, Argentina;2. Departamento de Ciencias de la Atmósfera y los Océanos, FCEN-UBA, Buenos Aires, Argentina;3. Instituto Franco-Argentino sobre Estudios de Clima y sus Impactos UMI 3351 CNRS–CONICET–UBA, Argentina;4. Servicio Meteorológico Nacional, Buenos Aires, Argentina;5. Consejo Nacional de Investigaciones Científicas y Técnicas, Argentina;6. Divisão de Satélites e Sistemas Ambientais, CPTEC-INPE, Brazil;1. Institute for Sustainability and Innovation, College of Engineering and Science, Victoria University, P.O. Box 14428, Melbourne, Victoria 8001, Australia;2. Faculty of Water Resources Management, Water and Marine Sciences, Lasbela University of Agriculture, Uthal, Balochistan, Pakistan;3. Civil, Environmental, and Construction Engineering Department, University of Central Florida, Orlando, Florida 32816-2450, USA;4. Faculty of Civil Engineering, Universiti Teknologi Malaysia, Johor Bahru 81310, Malaysia
Abstract:The lack of high resolution precipitation data has posed great challenges to the study and management of extreme rainfall events. Satellite-based rainfall products with large areal coverage provide a potential alternative source of data where in situ measurements are not available. However, the mismatch in scale between these products and model requirements has limited their application and demonstrates that satellite data must be downscaled before being used. This study developed a statistical spatial downscaling scheme based on the relationships between precipitation and related environmental factors such as local topography and pre-storm meteorological conditions. The method was applied to disaggregate the Tropical Rainfall Measuring Mission (TRMM) 3B42 products, which have a resolution of 0.25° × 0.25°, to 1 × 1 km gridded rainfall fields. The TRMM datasets in accord with six rainstorm events in the Xiao River basin were used to validate the effectiveness of this approach. The downscaled precipitation data were compared with ground observations and exhibited good agreement with r2 values ranging from 0.612 to 0.838. In addition, the proposed approach provided better results than the conventional spline and kriging interpolation methods, indicating its promise in the management of extreme rainfall events. The uncertainties in the final results and the implications for further study were discussed, and the needs for additional rigorous investigations of the rainfall physical process prior to institutionalizing the use of satellite data were highlighted.
Keywords:Spatial downscaling  TRMM  Extreme rainfall events  Orographical effect  Pre-storm conditions
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