From the last mesoscale discussion:
"In the presence of 20-30 kt west-southwesterly mean ambient flow, moderately strong easterly updraft inflow of seasonably moist air characterized by CAPE in excess of 1500 J/kg seems likely to maintain current convective intensities at least to the the southwestern shores of Lake Michigan. As long as this continues, westerly rear inflow probably will remain sufficiently strong to contribute to strong to severe surface gusts in downdrafts."
Guess we'll see about that lmao