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. (2010) proposed a methodology for combining the radar reflectivity profile from CloudSat ( Marchand et al. 2008 ) and the cloud properties (optical thickness and effective radius) from MODIS ( Platnick et al. 2003 ; Nakajima et al. 2010 ) to probe how the warm rain process occurs within clouds. The methodology composites the radar reflectivity profiles in the form of the probability density function normalized at each in-cloud optical depth, which is determined by vertically slicing the cloud
. (2010) proposed a methodology for combining the radar reflectivity profile from CloudSat ( Marchand et al. 2008 ) and the cloud properties (optical thickness and effective radius) from MODIS ( Platnick et al. 2003 ; Nakajima et al. 2010 ) to probe how the warm rain process occurs within clouds. The methodology composites the radar reflectivity profiles in the form of the probability density function normalized at each in-cloud optical depth, which is determined by vertically slicing the cloud
