.LONG TERM /SUNDAY THROUGH WEDNESDAY/...
As of 255 AM EST Thursday: As deep upper troughing slides into
the eastern
CONUS, rapid
height falls will be accompanied by
impressive channeled DPVA and enhanced upper-level
divergence in
the right
entrance region of an upper
jet. This potent synoptic
forcing will intersect an advancing surface
front which, based
on all the deterministic guidance at this point, will cross the
forecast area through the afternoon and evening, an opportune
time for a severe weather threat. The
GFS remains the fastest
among the
GFS/
ECMWF/GDPS trio, but all three depict a plume of
75-300
J/kg sbCAPE developing east of I-26 during the early
afternoon Sunday. With a 500mb speed max crossing the area
at this time, the environment will be ripe with speed
shear.
Sample forecast soundings depict some 55-70kts of deep layer
shear and excellent 0- 1km
shear of 30kts or more. As noted
by the previous forecaster, hodographs are straight, but being
that they`re oriented out of the
WSW and solely by virtue of
the
shear magnitude, the environment should surely be able to
support embedded mesovortices (and in fact, the kind of "ripples"
in mid-level
moisture associated with rear inflow development as
a precursor to mesovortex development are hinted at in both the
18z and 00z
GFS). As a further sanity check...a quick cluster
analysis of global
ensembles was done...revealing that of three
forecast modes - one supportive of early/mid afternoon
convection
like what`s depicted in most of the deterministic guidance, one
supportive of later afternoon
convection, and one supportive of
no
convection at all - only 10% of all
ensemble members now favor
a forecast solution with no severe threat
GSP's take on severe for Sunday.