Abstract
The evolution and fine scale structure of the squall line segment and its accompanied mesocyclone were documented using the dual-Doppler radar analyses from the NCAR Electra Doppler radar (ELDORA) data. ELDORA's 300 m along track resolution is able to resolve features with wavelength of 2 km. The Doppler radar data were edited in the NCAR SOLO package and were interpolated using Barnes scheme with grid spacing of 500 m in all three dimensions. The wind fields were deduced using a three dimensional variational Doppler analysis technique to resolve the circulation in the upper half of the storm including the anvil region.
| Original language | English |
|---|---|
| Pages | 520-521 |
| Number of pages | 2 |
| State | Published - 1997 |
| Event | Proceedings of the 1997 28th Conference on Radar Meteorology - Austin, TX, USA Duration: Sep 7 1997 → Sep 12 1997 |
Conference
| Conference | Proceedings of the 1997 28th Conference on Radar Meteorology |
|---|---|
| City | Austin, TX, USA |
| Period | 09/7/97 → 09/12/97 |