Here is the RAP reanalysis proximity sounding of the Robinson tornado. I’ve noticed these reanalysis skew Ts can really undercount thermodynamics and instability, so take those measurements with a grain of salt. However, this tornado took place well after dark so instability was decreasing with time.
Definitely high end kinematics, but not even in the ballpark of that thermal boundary area on 4/27/11 where 0-1 KM SRH was reaching up into the 800s,
0-3 SRH a little over 1000, and almost 2000 ML CAPE.
View attachment 46602