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NASA's NPOL S-band Doppler radar collected nearly continuous data from April 11 to June 3, 2011, during the Midlatitude Continental Convective Clouds Experiment. The dataset provides high-resolution vertical structure sampling via Range Height Indicator scans every 40 seconds. Additional processing with the Colorado State University Hydrometeor Identification Algorithm classifies precipitation types like rain, hail, and graupel.
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