Abstract
Hailstone size distributions have been determined from 41 time-resolved hailstone samples collected at the ground from seven storms that occurred in Alberta in the summer of 1980. Most size distributions were found to quite closely fit an exponential function of the form n(D) = noe-lambda D. In studying variations in no and lambda, it was found that a relationship exists between the two. -from Authors
Cite
CITATION STYLE
APA
Cheng, L., & English, M. (1983). A relationship between hailstone concentration and size ( Alberta). Journal of the Atmospheric Sciences, 40(1), 204–213. https://doi.org/10.1175/1520-0469(1983)040<0204:ARBHCA>2.0.CO;2
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