FOUS30 KWBC 190728
QPFERD
Excessive Rainfall Discussion
NWS Weather Prediction Center College Park MD
328 AM EDT Fri Jun 19 2026
Day 3
Valid 12Z Sun Jun 21 2026 - 12Z Mon Jun 22 2026
...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM EASTERN
OKLAHOMA AND THE OZARKS THROUGH MUCH OF THE MIDWEST AND OHIO VALLEY...
...Midwest...
By the start of the day 3 forecast period a potent shortwave and
related surface low are expected to eject eastward out of the
central Plains into the Midwest. There remains some uncertainty
regarding the speed and latitude of these features, but PWs above
the 90th climatological percentile (per the 00z GEFS) overlapping
with soils likely still recovering from recent heavy rain in the
Midwest will lead to at least scattered flash flooding concerns.
NBM probabilities for at least 2" are very high (between 60-80%)
and cover much of the northern SLGT risk area from MO/IA to OH.
Locally higher totals are likely given the convective environment.
The progressive nature of these storms may end up limiting the
severity of flash flood impacts, but a MDT risk upgrade is possible
should training/back- building elements become more obvious in the
short range updates, particularly along the leading warm front
ahead of the primary surface low.
...Southern Plains, Ozarks, and Lower Ohio Valley...
The setup on Sunday could lead to a southern secondary axis of
heaviest QPF and flash flooding impacts. The southern end of the
Saturday night thunderstorm complex/MCS is likely to sink
southeastward near a trailing cold front and impact areas near the
Ozarks early Sunday. Then, the expectation is for reforming
scattered convection during peak daytime heating and reorganization
of thunderstorms overnight Sunday associated with the LLJ to span
from OK to the Lower Ohio Valley, including northern AR, southern
MO, and western TN/KY. This combines for guidance to currently
depict current QPF amounts of 2-4" and an average localized max of
6". There remains obvious mesoscale uncertainties at this stage,
but with Pws near the 90th climatological percentile and a
favorably oriented west- east frontal boundary, it's possible a MDT
risk upgrade may be needed once CAMs come into forecast range. For
the Lower Ohio Valley in particular, some guidance also highlights thunderstorms associated with the initial warm front lifting
northward, which could add yet another potential for slow-moving
repeating thunderstorms.
Snell
Day 4 and Day 5
Valid 12Z Mon Jun 22 2026 - 12Z Wed Jun 24 2026
...THERE IS A SLIGHT RISK OF EXCESSIVE RAINFALL FROM PORTIONS OF
THE SOUTHERN PLAINS, LOWER MISSISSIPPI AND TENNESSEE VALLEYS, AND
CENTRAL APPALACHIANS ON DAY 4...
Day 4 continues to an active pattern through a good portion of the
CONUS, east of the Mississippi with a progressive trough axis
pushing through the Great Lakes and Northeast leading to periods of
moderate to heavy rainfall from the Ohio Valley into the Mid
Atlantic and Northeast. Areas of the Northeast are subject to
thunderstorm prospects with the best chance for flash flooding
likely to occur in the urban footprint from Philadelphia up to
Boston with an expansion inland to the Hudson Valley down through
eastern PA. Current probs off the latest ensembles and National
Blend indicate a large zone of 50-80% probs for >1" across the
aforementioned area above with deterministic outputs closer to
2-2.5" into parts of Southern New England. MRGL risk inherited
remains in effect, but there's potential here for an upgrade as we
move closer to the D4 window, but want to see more of the CAMs to
make that decision.
Across the Southern U.S., heavy precipitation will preclude another
round of convection forming along a quasi-stationary front draped
from the Southern High Plains to the Southeastern CONUS. Probs for
1" are highest in-of the areas of Eastern OK into the Lower
Mississippi and southwestern Tennessee Valleys. Elevated theta_E's
and PWAT anomalies +2 dev. or greater indicate a formidable
environment capable of continued heavy rain potential that will
likely produce rainfall of 2-4", at least in some of the
thunderstorm activity that develops. The focal point along the
front will likely be where the heaviest rain will occur, or at
least be a low-level convergence mechanism that can enhance
regional convection. There's high enough confidence in the location
of convection for the D4 period to overlap with areas that will
have seen several inches the periods prior which led to an upgrade
to a SLGT risk positioned over portions of the Southern Plains
through parts of the Lower Mississippi and neighboring Tennessee
Valleys. The risk extends through the Smokey Mountains up into
parts of the Central Appalachians in eastern KY up into WV as the
convergence regime follows the frontal positioning over these areas.
Day 5 is a transition period into a more typical summer time regime
for the CONUS with a longwave trough over the Northern U.S. and a
dome of mid and upper ridging positioning itself across the
Southwest. This will cause a persistent northwesterly flow pattern
across the Central and Southern High Plains over into the Lower
Mississippi Valley as progressive shortwave pulses eject out of the
Rockies and ride the prevailing northwesteries in place between the
ridge and trough. This highlights potential for MCS development and
flash flooding scenarios from the Front Range and points southeast
as the steering flow orients between the base of the trough and the northeastern flank of the ridge. This is historically projecting a
case of thunderstorm maturation and upscale growth over the area
between CO/KS down through OK/TX with potentially the Red River
Basin as a focus for thunderstorm activity. Eventually this ends up
migrating into the ArkLaTex and/or Lower Mississippi area which is
showing up in the QPF footprint on ensembles. With this becoming a
more stable signal in the global ensembles and aligning with the
NBM QPF output, a MRGL risk was added to the new D5 to account for
this potential evolution.
Kleebauer
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* Origin: Capitol City Online (618:250/10)