Abstract
Hail growth mechanisms in a Colorado multicellular hailstorm were investigated through use of dual-wavelength radar data, three-dimensional wind field data, in situ aircraft measurements and trajectory calculations. Peak hail production resulted when graupel particles and hailstones which grew within the updraft region of a feeder cell were advected in the wind field and fell into the main updraft region where they continued to grow. -from Authors
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CITATION STYLE
Heymsfield, A. J., Jameson, A. R., & Frank, H. W. (1980). Hail growth mechanisms in a Colorado storm. Part II: hail formation processes. Journal of the Atmospheric Sciences, 37(8), 1779–1807. https://doi.org/10.1175/1520-0469(1980)037<1779:HGMIAC>2.0.CO;2
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