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
2 %
113,201
1,318,495
Fargo, ND...Greeley, CO...Grand Forks, ND...Grand Island, NE...Moorhead, MN...
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
15 %
67,347
807,743
Fargo, ND...Grand Forks, ND...Grand Island, NE...Moorhead, MN...Kearney, NE...
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
SIG SEVERE
14,588
80,783
Garden City, KS...
15 %
67,224
824,716
Fargo, ND...Grand Forks, ND...Grand Island, NE...Moorhead, MN...Kearney, NE...
5 %
193,196
3,541,532
Lincoln, NE...Lubbock, TX...Amarillo, TX...Sioux Falls, SD...Greeley, CO...
SPC AC 081252
Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
0752 AM CDT Sat Jun 08 2019
Valid 081300Z - 091200Z
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS IN PORTIONS OF THE
CENTRAL PLAINS...AS WELL AS THE EASTERN NORTH DAKOTA/NORTHWESTERN
MINNESOTA AREA...
...SUMMARY...
The greatest potential for severe storms will be over parts of the
central Great Plains and Red River of the North area, with large
hail and severe gusts expected.
...Synopsis...
A split-flow pattern will persist in mid/upper levels, related to a
large but weak cyclone now centered over middle TN. This feature is
expected to remain generally near its current location through the
period, but with continued gradual filling, and perhaps transition
to a broad open-wave trough overnight. Associated mid/upper winds
accordingly are forecast to weaken through the period, though
several convectively induced/enhanced vorticity lobes will traverse
the cyclonic flow over the Southeast States.
Meanwhile, a synoptic-scale, northern-stream trough -- initially
evident in moisture-channel imagery from the AB/SK line across
northwestern MT, ID and northern NV -- will move eastward through
the period. By 12Z, this trough should reach the Dakotas, southern
WY and northern UT.
The 11Z surface analysis showed a low near the MB/ND/MN border
junction, with cold front to southwestern SD and south-central WY.
This front will move slowly eastward/southeastward through the day.
By 00Z, the front should extend from northwestern MN across eastern
SD and central NE, intersecting a dryline near the KS/CO border, to
a surface low over southeastern CO. The dryline will extend
southward through the TX/OK Panhandles to the lower Pecos Valley and
Big Bend regions.
...Northern/central Plains to southern High Plains...
Scattered thunderstorms are forecast to form near the cold front
from the eastern Dakotas to near the KS/CO border, offering severe
hail and gusts early in the convective cycle when cells are
relatively separated. As convection aggregates near the front, wind
will become the more predominant concern. Large hail, some
potentially above 2 inches in diameter, appears most probable where
supercell mode can be sustained the longest, which currently appears
to be in the area east and southeast of the front/dryline
intersection.
The most concentrated overall potential still appears to be over the
central High Plains, where lapse rates and buoyancy will be
greatest, and near the Red River of the North, in the zone of
greatest deep-layer forcing. Additional, isolated to widely
scattered convection -- potentially including a few supercells --
should form in the post-frontal/upslope flow regime of northeastern
CO where low-level shear is maximized (but CAPE is weaker than areas
along/ahead of the front), and near and south of the front/dryline
intersection into western KS.
Favorable diurnal heating and a corridor of 50s to low 60s F
prefrontal surface dew points will support weakening MLCINH and the
development of around 1500-2000 J/kg MLCAPE in the northern Plains,
and 2000-2500 J/kg across portions of KS/NE east of the front and
dryline. Forecast soundings suggest 40-45-kt effective-shear
magnitudes will exist near the front and the KS/CO portion of the
dryline, with vectors more orthogonal to the forcing boundaries
(favoring longer discrete character) over the central High Plains.
...Southern High Plains...
A conditional and very isolated severe hail/wind threat is evident
farther south across the TX/OK Panhandles to the Permian Basin and
lower Pecos Valley region, ahead of the dryline. Forcing for ascent
in this corridor will be very localized, related to strong surface
heating and the intensity of the vertical circulations in the
moisture gradient. Any mature storm(s) that develop will move atop
a well-mixed subcloud layer amidst steep midlevel lapse rates, and
MLCAPE in the 1000-2000 J/kg range. Uncertainties regarding
coverage/duration of convection preclude more than a marginal
unconditional risk at this time, though significant wind or hail
cannot be ruled out under any sustained cell that develops.
...Southeastern CONUS...
Widely scattered to scattered thunderstorms should develop from
midday through this evening across this region, preferentially
favoring outflow, differential-heating and sea-breeze boundaries.
The preconvective air mass again will be characterized by strong
heating in relatively cloud-free preconvective areas, rich low-level
moisture, with PW 1.75-2.25 inches, mean mixing ratios 16-18 g/kg,
and surface dew points commonly in the 70s F. Though a rogue
damaging or severe gust cannot be ruled out in the water-loaded core
of virtually any surface-based cell in the region, the most favored
area for marginally severe gusts should be southeast of the
mid/upper low, in and near the "marginal" outlook area, beneath a
belt of 25-35 flow atop the boundary layer that will enhance
low-level shear and storm-relative flow somewhat, in favor of
organized multicells or brief supercell characteristics.
..Edwards/Goss.. 06/08/2019
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