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
| Original language | English |
|---|---|
| Pages (from-to) | 1779-1807 |
| Number of pages | 29 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 37 |
| Issue number | 8 |
| DOIs | |
| State | Published - 1980 |
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