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Mircea Grecu
Lin Tian
Gerald M. Heymsfield
Ali Tokay
William S. Olson
Andrew J. Heymsfield
, and
Aaron Bansemer

1. Introduction Estimates of precipitation derived from single-frequency radar observations are inherently uncertain. This is because to express accurately the distribution of the number of precipitation particles in an observation volume as a function of their sizes more than one variable is necessary, whereas single-frequency radars provide only one reflectivity observation per volume. Solid precipitation is characterized by an additional type of significant uncertainty stemming from the fact

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