Looking into tomorrow is when the real questions arrive, along
with a noted
MLCAPE axis of 3000+
J/kg as temps and dewpoints
reach the 80s and 60s respectively: possibly the most warm/humid
day of the season thus far. With 0-6km
shear values jumping to
50+
kts, the
atmosphere will certainly be primed for severe
convection and discrete, all-mode supercells. The question will
be when, or if, initiation occurs however either due to CINH or
a lack of a sufficient forcing mechanism. While there will be
some weak
synoptic scale lift across eastern IA from MO into the
MS Valley, and models do suggest some weaker elevated
convection there, the main question will be whether deep convective
initiation can occur along a noted
dry line over western IA,
which doesn`t occur too often in the state. Low level mass
convergence will be weak with
flow fairly parallel to the
dryline, and the surface low and associated strong
QG forcing
moving from MN toward the Great Lakes. Extended range
hi res
models at this time yesterday, such as cSHiELD and the
NCAR
MPAS
ensemble, where noting nearly all healthy
convection and
updraft helicity streaks farther north closer to the triple
point and associated warm
front, close to the typical conceptual
model for
tornado outbreaks. Recent HRRR runs now entering the
applicable window reflect this evolution as well, as do various
MPAS and RRFS runs. However, some 12z HREF members across three
different cores (NamNest,
NSSL WRF, HRW FV3) are now depicting
isolated weak to moderate
updraft helicity swaths across
northern IA. While the Day 2
SPC outlook has scaled back
probabilities south to north, a Moderate Risk (4/5) is still in
place encompassing locations where some 12Z HREF members are
initiating
convection. Any healthy
convection that develops
could realize a somewhat alarming near storm environment.
Examination of 00z RAP soundings east of the dryline note
parameter space quite conductive for strong tornadoes in sub
1000m LCLs: 0-500m
shear and
SRH 30
kts and 326
m2/s2, and
streamwise
vorticity at 0.033 (96% of total
vorticity). So,
unfortunately, the primary message here needs to be that
possible outcomes range from little to no development this far
south, to
isolated, but strong supercells with large
hail and
longer track tornadoes. To compound those hazards, any storm
that develops would be moving rapidly,
likely in excess of 50
mph with conditions potentially changing quite rapidly,
straining
warning and reaction times. Needless to say, it would
be best to continue to monitor for updates into tomorrow. The
severe potential will mainly be in the early evening but
additional storms linger late evening with more development
possible east as
convergence increases with the merger of the
approaching cold
front and lingering dryline.