721
ACUS01 KWNS 022002
SWODY1
SPC AC 022000

Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
0300 PM CDT Tue Jun 02 2026

Valid 022000Z - 031200Z

...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS PART OF THE
NORTHERN PLAINS...

...SUMMARY...
Thunderstorms with large hail, severe wind gusts, and potentially a
couple of tornadoes are expected this afternoon and evening in parts
of the northern Plains. Strong wind gusts and marginal hail will
also be possible in parts of the southern and central High Plains. A
few severe wind gusts may also occur from southern Georgia into
northern and eastern Florida.

...20Z Update...
The forecast remains on track and only minor changes were made with
this update. The primary addition was a CIG1 wind area over parts of
western/central SD. Current thinking is that thunderstorms will
evolve off the Black Hills and grow upscale as they intercept a
diurnally destabilized air mass and gradually strengthening
low-level jet -- promoting some gusts upwards of 75 mph.

..Weinman.. 06/02/2026

.PREV DISCUSSION... /ISSUED 1130 AM CDT Tue Jun 02 2026/

...Northern Plains...
Morning surface analysis places a low over northwest ND, with a cold
front extending southward from this low across western ND and into
northwest SD before becoming oriented more southwestward through
northeast WY into south-central WY. Warm-air advection showers and
thunderstorms are already ongoing in the vicinity of this boundary
across ND. General expectation is for these showers to continue
while remaining predominantly subsevere. By this afternoon,
additional development is anticipated along the slow-moving front
from central ND into western SD and far eastern WY.

Environment preceding the front will be moist and unstable, with
upper 50s/low 60s dewpoints and MLCAPE around 2000 J/kg.
Boundary-parallel shear suggest the potential for both an anafrontal
character and quickly linear mode across much of ND. Even so, some
severe is possible, with large hail (isolated very large) and
damaging gusts as the primary risks. The shear orientation becomes a
bit less parallel to the boundary with southern extent, and there is
some potential for initial supercell structures from south-central
ND through western SD and into far eastern WY. Some low-level
southeasterly flow is expected near the surface low (which is
expected to redevelop southward), resulting in low-level hodographs
that indicate some tornado risk. This risk could be countered by
high LCLs and the likely quick transition to more linear structures.
Some undercutting or movement north of the outflow-augmented cold
front is likely with time, and the potential for development of a
strong to severe evening/overnight MCS appears limited.

...Central/Southern High Plains...
Scattered to numerous thunderstorms are anticipated across the
central and southern High Plains today amid moist low-level
easterlies/southeasterlies and modest southwesterlies aloft. There
is some indication one or two vorticity maxima may move into the
region along the northwestern periphery of the southern Plains
ridging. Shear is weak and a generally disorganized,
outflow-dominant storm structure is expected but some isolated hail
and/or damaging gusts are possible sporadically with the strongest
storms.

...Southeast into Central TX...
Surface analysis places an outflow boundary associated with
convective clusters over OK arcing from northwest TX south of the
Metroplex and into northeast TX. A hot and humid air mass over
central/southeast TX will be supportive of re-development of
afternoon thunderstorms along this outflow boundary. Storms will
likely track southward through the early evening, posing a risk of
locally damaging wind gusts.

...Southeast AL/southern GA into much of FL...
A deepening upper trough and associated large-scale ascent will
augment mesoscale factors (including surface moisture convergence
and sea-breeze boundaries) to support numerous thunderstorms across
the region. Strong buoyancy and modest deep-layer shear could
support occasional storm organization and robust updrafts capable of
producing damaging downbursts. Interactions between ongoing storms
and mesoscale boundaries could also augment updrafts, with the
resultant water loading also producing occasionally strong gusts.

$$