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Abstract:
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Rainfall is one of the most important hydrologic model inputs and is recognized as a random process in time and space. Rain gauges generally provide good quality data, however they are usually too sparse to capture the spatial variability. Radar estimates provide a better spatial representation of rainfall patterns, but they are subject to substantial biases. Our calibration of radar estimates using gauge data takes season, rainfall type, and rainfall amount into account, and is accomplished via a combination of threshold estimation, bias reduction, regression techniques, and geostatistical procedures. We employ the varying-coefficient model to adapt to the temporal variability of rainfall. The methods are illustrated using Texas rainfall data in 2003, which includes WSR-88D radar-reflectivity data and the corresponding rain gauge measurements.
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