Abstract
On the afternoon of 3 June 1981 a severe thunderstorm spawned two tornadoes which moved across a portion of metropolitan Denver. The tornadoes were classified as strong F2 intensity, and caused damage totaling over $15 million. The synoptic-scale setting for this event was similar to that associated with many other occurrences of severe convection in eastern Colorado, with post-frontal southeasterly upslope flow at low levels and southwesterly flow aloft in advance of an approaching trough.-from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 790-808 |
| Number of pages | 19 |
| Journal | Monthly Weather Review |
| Volume | 112 |
| Issue number | 4 |
| DOIs | |
| State | Published - 1984 |
| Externally published | Yes |