SPC 1300Z Day 1 Outlook
Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
0750 AM CDT Sun Mar 31 2024
Valid 311300Z - 011200Z
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FROM NORTHERN
MISSOURI INTO THE OHIO VALLEY...
...SUMMARY...
Scattered thunderstorms are expected today along a corridor from
northern Missouri into the Ohio Valley, with large hail expected.
Damaging gusts are possible, and a marginal tornado threat also
exists.
...Synopsis...
The major mid/upper-level influence on convective potential today,
and for the next few days, will be a high-amplitude, positively
tilted, synoptic-scale trough now extending from the northern
Rockies southwestward to offshore from southern CA. Two
accompanying, closed cyclones were noted in moisture-channel imagery
-- the largest centered about 150 nm west of LAX, the smaller one
over west-central NV. Both cyclones are forecast to devolve to open
shortwave troughs through the period, as an upstream perturbation --
now over the interior Northwest -- digs southward in the backside
cyclonic-flow field. Meanwhile, the synoptic trough itself will
shift eastward by 12Z to an axial position near DIK-LND-BCE-YUM,
then offshore from central/southern Baja. Ridging aloft will
amplify slightly and drift eastward across the central/southern
Plains.
At the surface, 11Z analysis showed a low over extreme western KS,
with quasistationary to slow-moving warm front extending across
central parts of KS/MO to near SDF and central WV. The eastern part
of this boundary may be shunted southward over the middle Ohio
Valley and WV today by precip. The KS low is expected to ripple
east-northeastward on the northward-drifting warm front toward MKC,
and weaken through the period, with the warm front reaching perhaps
80-120 nm north of its initial position in MO/IL/IN. Meanwhile, lee
cyclogenesis will occur over eastern CO, at or near a lee trough
intersection with the front. The resulting low should migrate along
the boundary tonight, across southwestern/central KS. A dryline was
analyzed from a frontal intersection near GBD across the TX South
Plains and Permian Basin to the Big Bend area. The dryline should
mix eastward this afternoon to western OK and west-central TX,
before retreating westward overnight, and is expected to remain
capped for deep convective potential this period.
...MO to central Appalachians...
An ongoing, broken swath of precip, with widely scattered
thunderstorms, was apparent in radar composites from southern IN
into portions of WV. This activity should shift east-southeastward
through the remainder of the morning and continue largely as
non-severe. However, isolated large hail or strong gusts may occur
from any sustained, relatively discrete activity near the southern
part of the precip plume.
The main convective episode should occur from around midafternoon
into this evening, as scattered thunderstorms develop near the
front. With a strongly front-parallel component to mean flow,
activity should move along or just north of the surface boundary,
offering large hail and sporadic damaging to marginally severe
gusts. Local boundary processes (e.g., interaction between storm
and vorticity-rich outflow boundary or front) may alter local
low-level shear favorably enough for some tornado potential, though
this threat appears isolated and conditional, given the lack of
greater boundary-layer moisture.
Although weak height rises are forecast across the region as the
synoptic ridge to the west amplifies, associated effects on
large-scale motion should be too small to impact convective
potential. Diurnal heating and moist advection will boost theta-e
enough to remove most or all MLCINH along and just south of the
front, with convergence on/near the front being the primary
convective forcing. Surface dewpoints commonly will reach the upper
50s to low 60s F in the warm sector. Modified forecast soundings
depict 1500-2000 J/kg MLCAPE over near-frontal parts of MO this
afternoon, decreasing to an eastward-narrowing corridor of 500-1200
J/kg peak MLCAPE over the Ohio Valley and into the WV/western VA
uplands where weaker low- and middle-level lapse rates will be
found. Though modest near-surface flow will limit lower boundary-
layer hodograph size, deep shear will be more than adequate for
supercells, with effective-shear magnitudes commonly 50-60 kt.
However, upscale clustering and mixed modes are also possible.
..Edwards/Leitman.. 03/31/2024
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