Abstract
The rates of development of graupel and hail in High Plains storms are calculated based on mechanisms for the growth of particles of various types. In the first part of this study, planar crystals, aggregates, graupel particles and frozen drops grow in a region of updraft specified by a one-dimensional parcel model. The processes of hail production are deduced by calculating the times required for each of the above embryo types to develop into hail from the time of nucleation over the range of typically observed liquid water contents. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 2867-2897 |
| Number of pages | 31 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 39 |
| Issue number | 12 |
| DOIs | |
| State | Published - 1982 |