A thermal gradient or effective front will develop as a result of
the morning convection and will be critical in determining the
northward extent of the afternoon and evening severe weather threat.
The most likely placement for this boundary at noon is somewhere
near Montgomery in a NW/SE orientation. A late morning to early
afternoon convective minimum appears likely which should give the
atmosphere a chance to become quite unstable. The most plausible
scenario is for a cluster of thunderstorms to form by early
afternoon in eastern MS and move eastward with the warm front
beginning to advance northeastward. The cluster of storms is likely
to grow upscale across our southwestern counties. Supercells may
also form ahead of the cluster along the advancing warm front in
response to warm advection with a strengthening low-level jet.
Dewpoints around 70 F in the warm sector and relatively cold
temperatures aloft could result in SBCAPE of 2000-3500 J/kg. 500 mb
flow of 50-60 kts and a strengthening low-level jet will be
supportive of supercells, bowing segments, and mesovortices mainly
across the southern half of our area. Large hail, damaging winds,
and tornadoes appear possible if this scenario unfolds. However,
there is still uncertainty regarding how the mesoscale details
will play out. Along and north of the warm front, training storms
could lead to flash flooding in an east to west corridor.