From latest outlook
...Midwest...
Considered increasing tornado probabilities and adding significant
hail but low confidence exists in whether supercells can be
sustained in the warm sector across IL/IN.
A slowly decaying MCS is ongoing near the IL/WI border within a warm
advection regime. Morning CAM guidance has poorly handled with most
struggling to maintain any semblance of convection beyond
initialization. The stratiform region across Lake MI should have an
impact on downstream destabilization in Lower MI given that richer
boundary-layer moisture characterized by low to mid 60s surface dew
points is currently confined from IL west. It is possible that the
MCS may not entirely dissipate as warm advection persists through
the period. Renewed development on the upshear side would seemingly
be most likely along trailing convective outflow. Along the eastern
extent of the Great Plains elevated mixed layer at peak heating,
robust upstream diabatic heating should result in large buoyancy
with MLCAPE of 2000-3000 J/kg. Veering of the wind profile with
height on the periphery of moderate mid-level northwesterlies will
favor supercell structures. An evolution to another MCS with
wind/hail risks appears probable tonight towards the OH Valley.