The tornado formed approximately 2.4 km SSE of the Columbus, MS, WSR-88D radar (KGWX) and moved NNE, passing within 800 m of the radar site before moving northward and growing substantially in size and intensity. Due to the close passage to the east of KGWX and the sharp northward component of motion, the tornado moved nearly along a uniform azimuth relative to KGWX while it was at maximum intensity, enabling KGWX to sample nearly the maximum wind speed in Doppler velocity, despite a translational speed of 24-26 m/s. The maximum Doppler velocity sampled by KGWX was 81.5 m/s (182 MPH), observed at a range of 3.62 km and height of 56 m (183 ft.) ARL. Damage in this area of maximum radar-estimated intensity consisted of five large high-tension transmission towers collapsed and extreme forest damage, including near-100% tree fall of loblolly pine forests over a width of up to 400 m and >75% tree fall over a maximum width of approximately 700 m within the much larger tornado damage path.
This presentation gives an overview of the datasets collected on this major tornado event. Plans for the use of KGWX radar data to compare to the corresponding tree damage are highlighted. Implications of this case on the refinement of EF-scale damage indicators for tree damage are discussed.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner