1. The definition of the hooks becomes less defined past BREF2. The cells 
become more blobs.

2. The storm looks weaker on tilt 4 than on tilt 1 because there's less 
precip higher up and the radar beam isn't looking at the same part of the 
storm as the others at the same tilt due to earth curvature.

3. zero velocity couplets
   no high inbounds next to high outbounds

4. Possibly. Given that these echoes are at the far edge of the radar, the 
radar's beam is high up due to the earth's curvature so more than likely a 
40kt outbound velocity is accurate.

5. The max gate-to-gate shear for the Caddo Co. storm is 50kts. The Grady 
Co. storm has issues w/ purple haze (range folding).

6. +36kt

7. I can make out 1 velocity couplet (Caddo Co.)

8. The max gate-to-gate shear on the Caddo Co. storm using storm-relative 
velocity is 60kts. Storm-relative velocity is easier to use to determine 
mesocyclone strength b/c I could make out couplets much better w/ 
storm-relative velocity than w/ base velocity.

9. The storm-relative velocity associated w/ the RFD is 10kts.
An observer on the ground in the path of the RFD would expect to encounter 
wind speed associated w/ base velocity.