I should have mentioned that - yea he’s writing for VA/MD specifically. We don’t have the prime atmospheric conditions VA will have. But that’s mostly for tornadic activity. The QLCS will mix down major winds. LWX mentions this in this afternoon’s write up which I have to say is much more in-depth than CTP’s. Granted however their entire coverage area is in the mod risk. CTP’s isn’t and they have a more dynamic atmosphere than we do. I don’t see tornadoes as much of a thing north of BWI.
Once any earlier low stratus are scoured out, expect ample
diurnal heating as temperatures rise into the upper 60s to low
70s. Prolonged south to southeasterly flow should also raise dew
points into the upper 50s to low 60s. The seasonably warm/moist
low-levels coupled by strong forcing aloft and cyclonic turning
of the winds with height will make for a very active convective
day. While the degree of vertical shear is impressive on its own
(0-6 km values around 55 to 65 knots), this comes with more than
sufficient buoyancy levels as surface-based CAPE values push
into the 500 to 750 J/kg range. The shear/instability
combination will be conducive to supercell development,
particularly for any discrete cells that form ahead of a likely
squall line. Additionally, the degree of deep-layer shear should
make this more of a quasi-linear convective system (QLCS) which
will be capable of tornadogenesis. Aside from any tornado risk,
the strong cloud-bearing level winds should easily mix down in
convective downdrafts. With 850-700 mb winds around 60-70 knots,
any of this higher momentum air being transferred to the surface
could yield surface wind gusts into the 65 to 75 mph range.
Thus, SPC has a broad area of significant damaging wind
potential (45-74%) advertised from I-81 eastward in their latest
outlook.