Abstract
Using the special data set collected in Project SESAME (1979), we describe our analysis and modeling efforts to test the hypothesis that a unique combination of terrain, boundary layer processes, and synoptic-scale circulations result in a preferred region of latent instability that determines the location of severe thunderstorm outbreaks. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1018-1032 |
| Number of pages | 15 |
| Journal | Bulletin of the American Meteorological Society |
| Volume | 61 |
| Issue number | 9 |
| State | Published - 1980 |