Abstract
This study employs in situ measurements to examine cloud conditions in which hydrometeors develop in mature Oklahoma convective clouds and to develop hypotheses as to how they formed. The measurements were made from penetrations on six days using a T-28 aircraft. Particle growth calculations are used in conjunction with the measurements to infer the processes of formation of drops, graupel and hail, and secondary ice crystals. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 2811-2835 |
| Number of pages | 25 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 41 |
| Issue number | 19 |
| DOIs | |
| State | Published - 1984 |
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