Validation of the CloudSat precipitation occurrence algorithm using the Canadian C band radar network

Abstract

The ability of CloudSat to detect precipitation in cold season cloud systems is examined using data from the Environment Canada C band weather radar at King City, Ontario. The factors complicating the comparison are the time mismatch, the differences in sensitivity, and the changes to the geometry of cross section with range from the ground radar, W band radar attenuation, and the effect of ground clutter. A total of 40 overpasses with precipitation were observed over the King City radar from September 2006 to April 2007. In about 14% of the precipitation profiles, time mismatches were diagnosed. When these cases were removed, the skill scores of the CloudSat precipitation occurrence product were excellent. The most frequent cause of a false detection was an incorrect precipitation threshold in the algorithm. The most frequent cause of a miss in detection was ground clutter removal of valid echoes by the algorithm. Overall, the CloudSat algorithm handled the effect of attenuation very well. Improvement to the algorithm would arise from a better tuning of the precipitation threshold, a threshold of −10 dBZ instead of −18 dBZ being more appropriate for winter storms in the Great Lakes area, and more effective ground clutter filtering in the lowest four range bins of the CloudSat data. The methodology employed here and the 1456 verified precipitation profiles from CloudSat can serve as a framework for a test bed to evaluate precipitation products from CloudSat.