Abstract
A two-dimensional, time-dependent cloud model has been used to simulate a moderate intensity thunderstorm for the High Plains region. The simulations show that the inclusion of snow has improved the realism of the results compared to a model without snow. The formation of virga from cloud anvils is now modeled. Addition of the snow field has resulted in the inclusion of more diverse and physically sound mechanisms for initiating the hail field, yielding greater potential for distinguishing dominant embryo types characteristically different from warm- and cold-based clouds.-from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1065-1092 |
| Number of pages | 28 |
| Journal | Journal of Climate & Applied Meteorology |
| Volume | 22 |
| Issue number | 6 |
| DOIs | |
| State | Published - Jan 1 1983 |
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