Abstract
The airborne NCAR Electra Doppler Radar (ELDORA) was repeatedly flown across the lake during intensive operations periods of the Lake-Induced Convection Experiment (Lake-ICE). Data were obtained on the spatial and temporal evolution of the boundary layer across the lake for a number of lake-effect cases. The obtained data were analysed using methods similar to those described by Hildebrand et al. 1996.
Original language | English (US) |
---|---|
Pages | 545-548 |
Number of pages | 4 |
State | Published - 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 |
ASJC Scopus subject areas
- Atmospheric Science
- Electrical and Electronic Engineering