Abstract
An account is given on the retrieval of vertical velocity fields to study the characteristics of lake-effect clouds. In particular, results are discussed from 10 January 1998 study, when weather conditions were favorable for intense boundary layer convection.
| Original language | English (US) |
|---|---|
| Pages | 490-493 |
| Number of pages | 4 |
| State | Published - Jan 1 1999 |
| Event | Proceedings of the 1999 29th International Conference on Radar Meteorology - Montreal, Que., Can Duration: Jul 12 1999 → Jul 16 1999 |
Conference
| Conference | Proceedings of the 1999 29th International Conference on Radar Meteorology |
|---|---|
| City | Montreal, Que., Can |
| Period | 7/12/99 → 7/16/99 |
All Science Journal Classification (ASJC) codes
- Atmospheric Science
- Electrical and Electronic Engineering