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) |
|---|---|
| Pages (from-to) | 542-544 |
| Number of pages | 3 |
| Journal | Conference on Radar Meteorology |
| State | Published - 1999 |
ASJC Scopus subject areas
- Atmospheric Science
- Electrical and Electronic Engineering