SPC 2000Z Day 1 Outlook
Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
0247 PM CDT Mon May 08 2023
Valid 082000Z - 091200Z
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS THE OZARKS INTO
THE OHIO RIVER VALLEY AND ACROSS PORTIONS OF SOUTH TEXAS...
...SUMMARY...
Scattered severe thunderstorms are most likely from the Ozark
Plateau to the Lower Ohio Valley, centered on 4 to 11 PM CDT. Large
hail and damaging winds should be the main severe risks. Severe
thunderstorms are also possible across areas such as South Texas.
...Ozarks to Lower Ohio Valley...
Convective initiation appears likely within the next 1-2 hours
across south-central MO per latest trends in visible imagery. A
residual outflow boundary is noted extending from the southern MO
cumulus field southeastward into southern Middle TN. This may be a
preferential corridor for storm clusters and/or a more organized MCS
to propagate into during the late evening hours. While most CAMs
appear to be too low with CI based on noted trends, several
solutions hint at the idea of convection maintaining intensity into
middle TN. Wind probabilities were nudged slightly southward to
address this potential. See MCD #729 for more details on near-term
trends.
...Texas Coastal Plains...
A cluster of strong thunderstorms has initiation northwest of the
Houston metro area. While radar trends suggest this convection is
slow to mature, GOES IR imagery has shown persistent cloud top
cooling consistent with intensifying storms. Consequently, this
activity may pose an isolated severe hail/damaging wind threat
through the late afternoon given favorable environmental buoyancy
and modest, but perhaps adequate, deep-layer shear. A storm or two
is plausible to the southwest of this activity along the TX coast,
but a diminishing cumulus field under approaching cirrus suggest
additional CI is unlikely in the near-term.
..Moore/Jewell.. 05/08/2023
.PREV DISCUSSION... /ISSUED 1147 AM CDT Mon May 08 2023/
...Ozarks to Lower Ohio Valley...
A linear cluster of storms across western/central Kentucky has
gradually trended downscale since early this morning but still
otherwise continues to persist southeastward. To its west/northwest,
the most confident scenario is for the front and lingering outflow
boundary to focus later afternoon convective development from
southern Missouri into southern Illinois, and eventually western
Kentucky.
Regional WSR-88D VWP data continues to sample a core of relatively
strong, potentially rear inflow/convectively enhanced, mid-level
winds in the wake of the MCS across southeast Missouri/western
Kentucky/southern Illinois vicinity. Resultant 40+ kt deep-layer
shear will tend to largely persist regionally and support organized
updrafts, including some supercells and sustained multicells as
storms redevelop later this afternoon. This should particularly be
the case within the greater instability reservoir across southern
portions of Missouri/Illinois. Significant severe hail will be
possible with initial supercells given the rather steep mid-level
lapse rates emanating east from the Great Plains. However,
convection should quickly tend to grow upscale into clusters where
the deep-layer shear vector is oriented more parallel to the front
from the Ozark Plateau to the Lower Ohio Valley. As such, a mix of
large hail and damaging wind should be the primary threats as
clusters/MCSs spread east-southeastward towards the Tennessee Valley
and central Appalachians tonight.
...Texas Rio Grande vicinity/Edwards Plateau/Low Rolling Plains...
The dryline from the Big Country to the Edwards Plateau should
support isolated thunderstorms from late afternoon to early evening.
Unlike previous days, winds should be weak through much of the large
buoyancy profile as stronger upper flow is displaced southeast of
the dryline due to a low-amplitude upper trough. While isolated
large hail/localized severe-caliber gusts are possible, the scenario
suggests that convection should tend to be rather disorganized
across the Low Rolling Plains into parts of the Edwards Plateau.
A somewhat higher probability of severe storms (Slight Risk),
nonetheless with a number of lingering uncertainties, appears to
exist from the middle Rio Grande vicinity northward into southern
parts of the Edwards Plateau, potentially aided by a weak mid-level
disturbance currently over northern Mexico. Near-dryline convective
development aside, this could also include the eastward propagation
of storms across the Rio Grande this evening. The northwestward
advection of a very moist air mass, as sampled by the 12z CRP
sounding with 1.80 PW value and 15.4 g/kg mean mixing ratio, will
support robust 4000+ J/kg MLCAPE across south-central Texas this
afternoon. Very steep mid-level lapse rates (12z DRT observed
sounding), ample buoyancy, and around 30 kt effective shear will
support large hail/severe-caliber wind gusts where storms do develop
later this afternoon into evening.
...South-Central Plains to ArkLaTex - Marginal Risk Areas...
Several mechanisms for sustaining deep convection are apparent this
afternoon and evening, offering a threat for generally isolated
large hail and severe wind gusts. The trailing portion of the
weak quasi-stationary front near the Oklahoma/Kansas border may be a
focus for later evening slow-moving thunderstorm development.
Additionally, a pair of MCVs, one drifting east from north-central
Texas and the other drifting northeast near the Upper TX Coast
should support downstream isolated to scattered thunderstorms,
peaking in intensity this afternoon to early evening. Modest
deep-layer shear coincident with the eastern fringe of the steep
mid-level lapse rate plume should yield sporadic multicell clusters
and foster a threat for lower-end intensities of severe hail/wind.
...Mid-Missouri Valley/Upper Midwest...
A belt of enhanced mid-level westerlies will be maintained to the
south of a low near the Minnesota/Ontario border drifting northwest
into southern Manitoba. Despite an ill-defined surface pattern,
robust boundary-layer heating from Kansas towards the Middle
Missouri Valley should overlap with the western periphery of a
lingering plume of 50s F surface dew points over Iowa. This may aid
in isolated late afternoon to early evening thunderstorms. With
light low-level winds, speed shear through the cloud-bearing layer
will foster a moderately elongated straight-line hodograph. This
will favor splitting discrete cells with mid-level rotation and
potential for isolated large hail, and perhaps even a brief tornado
risk across far southeast Minnesota/northeast Iowa near a residual
weak boundary.
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