Abstract
During the Lake-Induced Convection Experiment (Lake-ICE), a mesoscale vortex developed along the eastern shore of Lake Michigan. The location of the vortex and its propagation speed and direction allowed the Grand Rapids, MI WSR-88D (KGRR) to observe the well-defined mesoscale vortex in both the radial velocity and reflectivity fields for nearly five hours. This article discusses the performance of the synthetic dual-Doppler analysis technique for this case and the structure and evolution of the mesoscale vortex as determined from the KGRR radar measurements.
| Original language | English (US) |
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| Pages | 542-544 |
| Number of pages | 3 |
| 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