12Z ILN sounding is out now and you can go here to see it for yourself. Convective temp is 75 degrees today which of course isn't going to be a problem exceeding that temp.
https://www.spc.noaa.gov/exper/soundings/24050712_OBS/
No changes to the Day 1 Outlook from the SPC that was just issued. Below is the discussion for the Ohio Valley:
...Ohio Valley and vicinity...
A complex and multi-episode severe threat exists today over the
region. First, an ongoing band of strong/isolated severe
thunderstorms was apparent across portions of IL, southwestward over
southeastern MO and northeastern AR. Though favorable moisture and
buoyancy exists in the foregoing warm sector (along and south of the
warm front), height falls aloft and deep-layer lift will be greatest
over the middle and northern parts, near and just south of the warm
front and mainly north of the Ohio Rover. What does not overtake
too much of the warm frontal zone and dissipate in the next few
hours may reintensify as it encounters diurnally destabilizing low
levels, related both to low-level theta-e advection and cloudiness-
restrained surface diabatic heating. At least isolated severe gusts
would be the main concern with any such convection, which should
diminish as it moves over/past eastern IN/western OH while
outrunning already marginally favorable inflow-layer buoyancy.
The more-substantial severe concern exists for thunderstorms forming
this afternoon along/ahead of the cold front, then impinging on a
corridor of favorable heating and warm/moist advection behind the
morning activity. Surface dewpoints should recover into the mid-
upper 60s F, beneath a plume of steepening midlevel lapse rates that
is part of a remnant, somewhat modified EML spreading over the area
of low-level destabilization. Superposition of these processes
should yield peak MLCAPE in the 2000-3000 J/kg range over the
"enhanced" area, narrowing and weakening northward into Lower MI.
Favorable wind profiles are forecast, with effective-shear
magnitudes in the 55-65-kt range and large-enough hodographs to
support 200-400 J/kg effective SRH. To the extent an supercells
that develop can remain relatively discrete, hodographs in the
lowest couple km appear favorable for tornadoes (some possibly
strong). Damaging, large to very large hail also is a concern with
any such supercells. Buoyancy should be even greater with
southwestward extent into steeper midlevel lapse rates and greater
boundary-layer moisture of the Mid-South, and also southward over
the Tennessee Valley into AL, but with weaker overall forcing and/or
vertical shear otherwise, coverage and organization of strong-severe
convection are likely to be less.