Here is a sounding for Berks later on.
Notice there is AMPLE deep layer shear and a huge amount of veering in the lower levels. 61 knots of EFF Shear is insane around here! Plenty of SRH too. The problem is the amount of SBCAPE for the storms to tap into. Lots of low level cloudiness this morning. It's still very early though, so if we're still socked in clouds by 11-12, then I'd say the storm chances dramatically diminish. However, Mount Holly mentions that even if we don't completely clear out, there will still be enough MLCAPE to tap into
As described
above, the forecast is for the morning showers and isolated
thunderstorms to slowly translate east. As this occurs a
fractured stratus deck will start to lift. The stalled front
currently near the fall line will also lift north as a warm
front with rich theta-e air surging northwards. This recycled
moisture regime will help to destabilize the region even if the
stratus doesn`t ever completely clear. Both the GFS and NAM are
indicating MLCAPE values of around 1000/1500 J/kg. Still though,
the amount of available instability is one of the potential
failure modes today (esp. if morning showers prove to be more
robust than initially forecast). Generally though, during late
July it doesn`t take much to destabilize the region.
Early this afternoon the MCV will be approaching from the west
with showers and thunderstorms across central PA. Ascent will
increase across the region as the MCV approaches. Across the
warm sector, effective bulk shear values of ~45 kts will be more
than sufficient to support rotating updrafts. Some upscale
growth is forecast as multiple cold pools start to be deposited
and merge. The primary threats with these storms will be
damaging winds, large hail, and an isolated tornado (thanks to
slightly back southeast flow and impressive directional shear).