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Joseph P. Zagrodnik, Lynn A. McMurdie, Robert A. Houze Jr., and Simone Tanelli

; Yuter and Houze 1995 ) and gridded maps of reflectivity height and coverage. The CFADs were constructed by binning the quality-controlled Ku reflectivity data into two-dimensional histograms of reflectivity from 0 to 50 dB Z in 1-dB intervals between heights above sea level of 1.5 and 8.0 km in 0.25-km intervals. Each CFAD is normalized by the maximum bin at any level after correcting the sample size for terrain obstruction at lower levels. The terrain correction primarily affects the four lowest

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