Observations have been made on the size and concentration of graupel and hail occurring in untreated convective cloud systems over the High Plains of the United States. From these data, an average graupel and hail distribution has been generated. The comparison of this .,ize spectrum with data from other studies, along with the implications to hail detection and hail suppression, is also discussed.
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August H. Auer (1972) studied this question.
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