C/S algorithm based on properties of dual-polarization radar measurements derived from disdrometer data
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1. Natural Variations in the Analytical Form of the Raindrop Size Distribution
2. Comparison of different fittings of drop spectra for rainfall retrievals
3. Comparison of different fittings of experimental DSD
4. Evaluation of Gamma Raindrop Size Distribution Assumption through Comparison of Rain Rates of Measured and Radar-Equivalent Gamma DSD
5. Evidence from Tropical Raindrop Spectra of the Origin of Rain from Stratiform versus Convective Clouds
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