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Robert Conrick, Joseph P. Zagrodnik, and Clifford F. Mass

estimate rain rate R at the surface using a power-law relation, known as a Z – R relationship. A number of such Z – R retrievals have since been developed for a variety of meteorological situations and locations, and they continue to be used by the U.S. National Weather Service to produce operational quantitative precipitation estimates ( Kuligowski 1997 ; Fulton 2002 ; Apffel et al. 2015 ). With the introduction of dual-polarization radars for research and operational applications ( Kumjian

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