Abstract
Our analysis suggests that snow boundaries on this day over the northeast Plains of Colorado may have acted through the development of a weak solenoidal field to enhance low-level inflow into a snow-free area within this region, thereby assisting with cloud development over the snow-free ground. Analogous to the sea breeze, this phenomenon might be termed a 'snow breeze'. Very-short-range forecasting of weather associated with phenomena such as this can be greatly improved with data from surface mesonetworks.-from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 69-74 |
| Number of pages | 6 |
| Journal | Unknown Journal |
| State | Published - 1984 |
All Science Journal Classification (ASJC) codes
- General Environmental Science
- General Earth and Planetary Sciences