I take it tomorrow is a stretch. Not looking very probable -
...Mid-MS/OH Valleys to the Mid-Atlantic...
Uncertainty remains this forecast cycle, particularly from around
central PA eastward to the northern Mid-Atlantic Coast/Chesapeake
Bay vicinity. Severe thunderstorm probabilities have been focused
along and just ahead of a southward sagging cold front and
instability gradient from central OH to the NJ coast. Rich
boundary-layer moisture (dewpoints in the upper 60s to mid 70s F)
will contribute to a corridor of MLCAPE around 2000-4000 J/kg from
the Mid-MS Valley eastward to the NJ coast. Warm midlevel
temperatures may lead to lingering inhibition, particularly across
eastern portions of the Slight and Marginal risk areas. Height falls
associated with troughing over eastern Canada will remain well north
of the region, and resulting in somewhat nebulous large-scale ascent
amid very modest vertical shear (effective shear magnitudes
generally less than 25 kt).
Convection from the Day 1/Tue period may be ongoing Wednesday
morning across parts of the Great Lakes vicinity and shift east
along the instability gradient/southward-sagging surface front
through the afternoon. Vertical shear may be locally enhanced with
any MCV that may be present with this activity, and damaging winds
are possible as the downstream boundary layer destabilizes.
Additional isolated thunderstorm development is possible from
central PA/northern VA eastward to the coast. This activity could
produce locally damaging gusts and perhaps small hail if capping can
be overcome and longer-lived updrafts develop.
Weak shear further west toward the Mid-MS Valley vicinity will
likely preclude a more organized severe risk. However, strong
heating amid the very moist/unstable airmass will support isolated
strong/locally damaging gusts during the afternoon.