Summary / Conclusion
The tornado in Bradford county developed in a thermodynamic environment typical for mini-supercells (MLCAPE values near 1000 J/kg).
However, the large-scale pattern was not similar to the pattern described by Davies and Guyer (no nearby closed upper-level low).
Tornadogenesis occurred with a long-lived, minimally strong, mesocyclone.
Radar-detected rotational velocity was near the low-end of what is typically associated with a tornado (28 kts, although dealiased data was an issue at 2042z).
The tornado developed on a hill, and moved down along a valley.
Slide 26