Severe Storm Outlook Narrative (AC)
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337
ACUS01 KWNS 081256
SWODY1
SPC AC 081255

Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
0755 AM CDT Wed May 08 2024

Valid 081300Z - 091200Z

...THERE IS A MODERATE RISK OF SEVERE THUNDERSTORMS OVE PORTIONS OF
SOUTHERN/SOUTHEASTERN MISSOURI...EXTREME NORTHEASTERN AR...EXTREME
SOUTHERN ILLINOIS...WESTERN/SOUTH-CENTRAL KENTUCKY...AND
NORTHWESTERN TO MIDDLE TENNESSEE...

...SUMMARY...
Severe thunderstorms appear likely from parts of the mid
Mississippi, Ohio, and Tennessee Valleys into the southern Plains.
All severe hazards, including tornadoes, very large to giant hail,
and potentially significant damaging winds are possible.  Some
tornadoes may be strong.

...Synopsis...
In mid/upper levels, a temporarily blocky pattern has evolved around
a cutoff cyclone over the northern Great Plains.  The associated
500-mb low is expected to drift erratically southeastward and fill
slowly through the remainder of the period, while a series of
shortwaves amplify associated synoptic troughing extending
southwestward across the Intermountain West and Great Basin.
Meanwhile, a northern-stream perturbation over the Upper Great
Lakes, that peeled eastward off the cyclone`s influence, has a
compact cyclone aloft centered near ANJ.  This feature should
devolve into an open shortwave trough and accelerate eastward as it
enters the northern stream today, reaching eastern NY and western
New England around 00Z.

In the southern stream, broadly cyclonic flow will prevail over the
western CONUS.  A weak perturbation -- apparent in moisture-channel
imagery over the central Gulf of California -- should move
east-northeastward through the period, reaching northern Coahuila
and adjoining southwest TX around 00Z, then parts of LA/northern MS
by the end of the period.  Downstream perturbations over the
Southeast and central/southern Appalachians should be predominantly
convectively derived.

At 11Z, a surface lows were evident over southwestern ND and between
OFK-YKN, along an occluded front.  An occluded/cold front arched
from the NE low across northeastern KS to another weak low near CNU,
then southwestward over southwestern OK and the TX South Plains.
Today, the cold front will overtake the northern part of a dryline
now over northwest TX to the Big Bend region.  By 00Z, the front and
dryline together will act as a western limit of substantial
convective/severe potential, from eastern OK to
north-central/central TX.  A Gulf warm front over northeastern OK
and central/northeastern AR was moving northward and should cross
the Ozarks this morning, moving into southern MO.  A progressive
outflow boundary was apparent from northern VA across southern WV,
southeastern KY, to northern parts of middle/western TN and
southeastern MO.  The western part of this boundary is stalling, and
soon should retreat northward through the rest of the morning across
parts of western KY and southeastern MO, essentially linking with
the warm front to form a baroclinic zone focusing the greatest of
today`s severe risks.

...Ozarks to Mid Mississippi, lower Ohio and Tennessee Valleys...
A complicated, potentially dangerous severe-weather event is
possible today into this evening.  Multiple rounds of strong-severe
thunderstorms are expected today across this region, additively
contributing enough severe hazard for the "moderate" (level 4 of 5)
risk area.  A swath of damaging to severe gusts and at least a few
embedded tornadoes are likely to accompany a complex of
thunderstorms from southern MO across parts of the multi-state area
near the Ohio/Mississippi River junction, to at least northern parts
of the Tennessee Valley region.  The main MCS should move
east-southeastward to southeastward along and near the instability
gradient associated with the aforementioned outflow boundary.
Before and during that process, several supercells are expected,
offering tornadoes (a few potentially significant/EF2+), large to
very large hail, and localized severe gusts.

An ongoing area of strong-severe thunderstorms across portions of MO
should pose mainly a severe-hail threat for another couple hours,
though the gust potential will increase as it grows upscale.  See
severe thunderstorm watch 202 and related mesoscale discussions for
the near-term threat.  As the morning progresses, the wind threat
will ramp up further, with some tornado potential starting as well,
as this activity and/or additional convection developing later over
western MO interacts with 1) a northward-moving plume of
surface-based inflow air and 2) rich low-level moisture now found
south of the outflow boundary.  Meanwhile, diurnal destabilization
of an already richly moist airmass south of the boundary will grow
MLCAPE commonly into the 3000-4000 J/kg range, beneath favorable
(50-60 kt) deep shear.  Low-level shear/vorticity, SRH and hodograph
size will peak near the boundary, supporting a corridor of
relatively maximized tornado potential with any sustained/discrete
or semi-discrete supercells in the area, as well as a focus for MCS
forward propagation from the northwest.  MCS activity should merge
upscale further this evening and tonight, maintaining severe-wind
potential into parts of the Tennessee Valley region before moving
into gradually less instability late tonight.

...Eastern OK to AR, Mid-South and central TX...
Thunderstorms should develop by late afternoon near the front and
dryline, as a combination of lift along those boundaries and strong
surface heating combine with very rich low-level moisture to erode
the EML cap sampled well by the 12Z FWD RAOB.  Large to giant hail,
occasional severe gusts, and a few tornadoes are possible as
activity shifts eastward to northeastward across central/east TX,
the Arklatex, and AR through the evening.  The northern part of this
convection may merge with or be overtaken by MCS activity moving out
of MO and into parts of the Mid-South.

The afternoon/preconvective environment should be characterized by
steep low/middle level lapse rates on either side of the weakening
cap, along with surface dewpoints commonly in the 70s F.  This will
contribute to strong buoyancy with the peak/preconvective MLCAPE
reaching 4500-5500 J/kg, and SBCAPE values topping 6000 J/kg.
Although near-surface flow generally will be 10 kt or less, limiting
lowest-km hodographs/shear, effective-shear magnitudes in the
40-55-kt range indicate supercells will be possible.  These will be
capable of very large/destructive hail exceeding 3 inches in
diameter.  Clusters or upscale mergers of convection also may offer
deep, precip-loaded, hail-cooled downdrafts with locally severe
gusts.  Cell mergers and interactions with boundaries will factor
into tornado potential on the storm scale, since the environmental
low-level shear appears on the margins.

...Southern Appalachians/Cumberland Plateau into Carolinas...
Thunderstorms are ongoing along and behind the outflow boundary near
the TN/KY border area, and may pose a severe threat through the
remainder of the morning while moving generally southeastward.  See
SPC mesoscale discussion 693 for near-term details.  Further
intensification and/or additional development is possible into the
afternoon over and east of the mountains, moving into an environment
of favorable moisture and diurnal destabilization.  MLCAPE in the
1500-2500 J/kg range appears attainable, amidst roughly 35-45-kt
effective-shear magnitudes.  A mix of supercell and multicell modes
is expected, with small bows possible, supporting localized threats
for damaging wind, large hail and at least marginal tornado
potential.

...Northeastern CONUS...
Widely scattered to scattered thunderstorms may develop as soon as
mid/late morning over parts of eastern NY and New England.  Activity
should form atop a diurnally destabilizing and weakly capped
boundary layer, along/ahead of a prefrontal surface trough and
behind a plume of non-severe thunderstorms and precip now crossing
parts of the region.  Thunderstorms should move generally eastward,
offering damaging to isolated severe gusts and isolated large hail.
A combination of low-level warm advection, spotty/irregular diurnal
surface heating, and cooling aloft related to the approaching Great
Lakes shortwave trough, will steepen low/middle-level lapse rates
substantially.  With favorable moisture (surface dewpoints generally
50s to low 60s F), a plume of 500-1000 J/kg MLCAPE should develop,
amidst effective-shear magnitudes that reach 40-50 kt, and despite
strongly veered/westerly surface wind components.  A mix of
multicell and modest supercell characteristics should be observed
before activity moves over more-stable air and/or offshore, and
weakens by early evening.

...Eastern SD to eastern IA and vicinity...
Widely scattered to scattered thunderstorms are possible from early
afternoon in western parts to evening closer to the Mississippi
River, with isolated damaging gusts, large hail and possibly a
tornado or two.  Activity should form in an area of deep-layer lift
(including low-level convergence/mass response) related to a
vorticity lobe in the southeastern part of the mid/upper-level
cyclone.  Associated cooling aloft will combine with residual
low-level moisture (dewpoints mid 40s to mid 50s F) to yield pockets
of around 500-1000 J/kg MLCAPE.  Backed low-level winds will aid
convergence and storm-relative low-level flow, and may contribute to
locally enlarged hodographs.

..Edwards.. 05/08/2024

$$