SPC write up for Friday included this....
...Synopsis and Discussion...
Deep upper trough extending along the MS Valley early Friday morning
is expected to continue eastward, maturing into a well-formed
mid-latitude cyclone centered over the southern Appalachians by the
end of the period. Very strong flow aloft will exist throughout the
base of the upper trough, with the strongest flow developing within
its eastern periphery Friday afternoon and continuing into Saturday
morning. 500-mb flow could exceed 100 kt, which is near record
values across the Carolinas and into the mid-Atlantic based on SPC
sounding climatology. In contrast to these impressive dynamics,
overall thermodynamic environment will be marginal. Given that ample
low-level moisture will be in place (i.e. dewpoints in the mid 60s
to low 70s and 100-mb mean mixing ratios over 12 g/kg), the modest
instability is largely a result of warm temperatures aloft and
consequent poor lapse rates.