El Paso, TX...Denver, CO...Albuquerque, NM...Colorado Springs, CO...Minneapolis, MN...
Probabilistic Tornado Graphic
Probability of a tornado within 25 miles of a point. Hatched Area: 10% or greater probability of EF2 - EF5 tornadoes within 25 miles of a point.
Day 1 Tornado Risk
Area (sq. mi.)
Area Pop.
Some Larger Population Centers in Risk Area
No Risk Areas Forecast
Probabilistic Damaging Wind Graphic
Probability of damaging thunderstorm winds or wind gusts of 50 knots or higher within 25 miles of a point. Hatched Area: 10% of greater probability of wind gusts 65 knots or greater within 25 miles of a point.
Day 1 Wind Risk
Area (sq. mi.)
Area Pop.
Some Larger Population Centers in Risk Area
5 %
249,691
9,653,841
El Paso, TX...Denver, CO...Albuquerque, NM...Colorado Springs, CO...Aurora, CO...
Probabilistic Large Hail Graphic
Probability of hail 1" or larger within 25 miles of a point. Hatched Area: 10% or greater probability of hail 2" or larger within 25 miles of a point.
Day 1 Hail Risk
Area (sq. mi.)
Area Pop.
Some Larger Population Centers in Risk Area
5 %
54,113
4,903,427
Minneapolis, MN...St. Paul, MN...Bloomington, MN...Plymouth, MN...Brooklyn Park, MN...
SPC AC 300557
Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
1257 AM CDT Sat Sep 30 2023
Valid 301200Z - 011200Z
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS FOR PORTIONS OF
THE UPPER MS VALLEY...CENTRAL AND SOUTHERN HIGH PLAINS...AND WESTERN
INTO CENTRAL UTAH...
...SUMMARY...
Isolated severe gusts may occur across portions of the
southern/central High Plains and western into central Utah this
afternoon. An instance or two of severe hail also cannot be ruled
out across portions of the Upper Mississippi Valley.
...Synopsis...
A broad, pronounced mid-level trough will continue to amplify over
the Interior West today as upper ridging builds over the CONUS east
of the Rockies. Beneath the mid-level trough, a large surface
cyclone should become established over the Great Basin, with the
surface cyclonic flow extending as far northeast as the northern
Plains, where the northward advection of low-level moisture will be
taking place. Strong tropospheric wind fields overspreading a deep,
mixed, but marginally buoyant boundary layer will support scattered
strong to isolated severe storms across portions of the Great Basin,
eastward to the central and southern High Plains. At the terminus of
a Great Plains low-level jet, warm-air advection may support
isolated strong to severe thunderstorms given the presence of
elevated buoyancy.
...Central and Southern High Plains...
A mid-level impulse embedded within the broader upper trough will
traverse the southern Rockies and approach the central High Plains
through the afternoon, providing locally stronger forcing for ascent
to support scattered thunderstorms. These storms will develop atop a
well-mixed, dry boundary layer extending up to 600 mb in spots.
Though hodographs are not overly long, modestly stronger flow aloft,
combined with downward momentum transport driven by rainwater
evaporation in the deep and dry sub-cloud layer, should support at
least isolated severe gusts with the stronger storms during the late
afternoon and evening hours.
...Western into central Utah...
A belt of 50-70 kt 500 mb south-southwest to north-northeasterly
flow will accompany the leading edge of the broad upper trough
during the afternoon, and is poised to overspread a dry, well-mixed
boundary layer. Through the afternoon, strong southerly flow
associated with the aforementioned surface cyclone may encourage
dewpoints to approach the 35-40 F range, resulting in marginal (i.e.
less than 500 J/kg) SBCAPE. Though buoyancy should be quite scant,
strong forcing along a surface cold front will foster a line of
low-topped thunderstorms immediately preceded by strong (albeit
meridional, unidirectional) speed shear and accompanying elongated
hodographs. When also considering the impacts of evaporative cooling
in a dry boundary layer with steep low-level lapse rates, organized
cells or small bows within the parent convective line may produce a
couple of severe gusts by late afternoon.
...Upper Mississippi Valley...
By mid to late afternoon, the gradual approach of an upper trough
will encourage the strengthening of a low-level jet over the Plains
states. A plume of low-level moisture (including low to mid 60s F
surface dewpoints) will continue to advect northward to a diffuse
surface-850 mb baroclinic zone draped across the northern Plains
into the Upper MS Valley. Isentropic ascent along this boundary will
be sufficient for scattered thunderstorm development by late
afternoon. By this point, 7-8 C/km mid-level lapse rates will
overspread the low-level moist axis, boosting MLCAPE to over 2000
J/kg. Forecast soundings depict short hodographs with appreciable
low-level curvature, suggesting that any storms that form will be
multicellular in nature, capable of producing a couple instances of
severe hail by late afternoon or early evening.
..Squitieri/Lyons.. 09/30/2023
NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 1300Z