South of the warm front, the low-level CAPE became increasingly favorable during the evening (increased from around 50 to 130 J/kg).
South of the warm front, the mid-level storm relative winds were modest. (decreased from 10 m/s to 8 m/s). Shear was mostly in the lowest 1 km.
All and south of the warm front, LCL heights were around 1000 m.
North of the warm front, the thermodynamic environment was not favorable for tornadogenesis.
North of the warm front, strong shear profiles resulted in favorably strong mid-level storm relative winds.
North of the warm front, LCL heights were low.