SPC 1200Z Day 1 Outlook
Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
1258 AM CDT Thu May 01 2025
Valid 011200Z - 021200Z
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS THIS AFTERNOON
THROUGH TONIGHT ACROSS PARTS OF WRN NY...WRN PA...WRN WV...MUCH OF
OH...SERN IN...CNTRL AND ERN KY...MIDDLE TN...CNTRL/SRN
MS...NRN/CNTRL LA...SRN AR...SRN OK...NRN TX...
...SUMMARY...
Lines and/or clusters of strong to severe thunderstorms are likely
to impact parts of the Ohio Valley into lower Great Lakes, parts of
the lower Mississippi Valley, and the southern Great Plains this
afternoon through tonight.
...Discussion...
It appears that an amplifying mid/upper flow regime across the
northern mid-latitudes of the eastern Pacific into North America
will undergo further amplification while continuing to develop
inland through this period. This will include a prominent ridge
overspreading the Canadian Rockies and northern U.S. intermountain
region later today through tonight, perhaps with an embedded high
evolving to the east of the Cascades.
Downstream, a notable short wave trough is forecast to continue
digging to the lee of the northern U.S. Rockies, preceded by a short
wave trough which has recently emerged from the Southwest. Models
suggest that the lead perturbation will undergo shearing, but it may
still provide support for modest deepening of a surface low
northeast of the middle Mississippi Valley through lower Great Lakes
region by late tonight.
To the southwest of this low, conglomerate outflow from extensive
convective development of prior days will at least initially precede
and obscure any trailing surface front. By 12Z this morning, it
appears that the leading edge of this outflow will be in the process
of advancing eastward through the lower Ohio Valley, while stalling
and weakening across the lower Mississippi Valley through upper
Texas coastal plain. It remains a bit unclear the extent to which
the surface outflow, residual cloud cover and rain will impact
destabilization and convective potential later today. It is
possible that this could impact a sizable area centered across parts
of the Mid South.
...Ohio Valley into lower Great Lakes...
Uncertainty exists concerning the possible influence of convective
outflow and cloud cover on destabilization, and spread is evident
among the various model output concerning the synoptic evolution.
However, broad surface troughing overspreading the region during the
day may provide the focus for the highest probabilities of vigorous
thunderstorm development. Boundary-layer moistening (including mid
60s F surface dew points) and warming may become sufficient to
support mixed-layer CAPE on the order of 1000-2000+ J/kg, in the
presence of 30-50 kt south to southwesterly flow in the 850-500 mb
layer. This environment may become conducive to organizing lines or
clusters of storms, and perhaps a few supercell structures, posing a
risk of severe wind and hail, with at least some potential for
tornadoes, during the afternoon and evening.
...Lower Mississippi Valley vicinity...
Large-scale forcing for ascent to support convective development
remains unclear, on top of the possible lingering influence of
convective outflow, cloud cover and rain. However, the NAM and
Rapid Refresh suggest that a zone of strengthening differential
heating may develop across the Ark-La-Tex into lower Mississippi
Valley during the day, providing a focus for strong destabilization
beneath steep-lapse rates associated with remnant elevated
mixed-layer air. Aided by boundary-layer moisture characterized by
surface dew points near 70F, large CAPE on the order of 2000-3000+
J/kg is forecast beneath modest westerly mid-level flow. Perhaps
aided by lift associated with low-level warm advection, organizing
convection posing a risk for large hail and damaging wind gusts
appears possible. This may include supercell structures, at least
initially, and eventually an upscale growing, east-southeastward
propagating cluster.
...Raton Mesa into southern Great Plains Red River vicinity...
Models indicate another zone of potentially strong convective
development may evolve late this afternoon into tonight, as the
boundary layer moistens and heats beneath the northern periphery of
a plume of elevated mixed-layer air. It appears that this will
advect east/east-southeast of the southern Rockies, near the
southern periphery of the mid-level troughing digging to the lee of
the northern Rockies. Models suggest that a smaller-scale embedded
perturbation may be accompanied by increasing convective development
across and east-southeast of the Raton Mesa vicinity by early this
evening. Aided by updraft inflow of increasing instability across
the Texas Panhandle into areas near/north of the Red River, there
appears potential for the evolution of an upscale growing cluster.
The 01/00Z NAM, in particular, generates a convective perturbation
that would appear to include 70+ kt westerly rear inflow (in the
850-700 mb layer) across Oklahoma by late tonight. Based on other
output, this appears an outlier, but the evolution of a convective
cluster posing a risk for severe hail and wind appears possible.
..Kerr/Weinman.. 05/01/2025
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