Grand Forks, ND...Dickinson, ND...Fergus Falls, MN...Pierre, SD...Bemidji, MN...
MARGINAL
118,238
2,641,286
Duluth, MN...Appleton, WI...Oshkosh, WI...Eau Claire, WI...Rapid City, SD...
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
SIG SEVERE
5,876
26,888
No Major Population Center in Risk Area
10 %
6,642
28,172
No Major Population Center in Risk Area
5 %
11,356
93,495
Minot, ND...
2 %
11,555
79,664
Williston, ND...Devils Lake, ND...Grafton, ND...
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.
Duluth, MN...Appleton, WI...Oshkosh, WI...Eau Claire, WI...Rapid City, SD...
SPC AC 141630
Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
1130 AM CDT Thu Jun 14 2018
Valid 141630Z - 151200Z
...THERE IS A MODERATE RISK OF SEVERE THUNDERSTORMS FAR NORTHERN
ND...
...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS PARTS OF THE
DAKOTAS...
...SUMMARY...
Scattered to numerous severe storms are expected during the late
afternoon and evening across parts of the Dakotas into northwest
Minnesota. A couple tornadic storms, very large hail, and intense
wind gusts are possible.
...Dakotas to MN/WI...
A shortwave trough over the northern Rockies will eject northeast
into the southern Prairie Provinces through early Friday. A surface
cyclone over southeast MT should develop into separate lows with one
tracking northeast into southwest Manitoba by evening and a
thermal-induced circulation near the Black Hills, along a cold front
that progresses east across the Dakotas tonight. Rich boundary-layer
moisture sampled by the 12Z OAX sounding and characterized by mid
60s to low 70s surface dew points will spread north from the Mid-MO
Valley beneath a stout elevated mixed layer as sampled by the 12Z
UNR sounding. With robust surface heating underway, this setup will
result in a plume of strong to extreme buoyancy across the Dakotas
by early evening with MLCAPE commonly reaching 2500-5000 J/kg.
Ongoing elevated storms across far northeast MT into northwest ND
may continue to produce isolated severe hail over the next few
hours. In the wake of this activity, two corridors of surface-based
storm development are anticipated during the late afternoon. One is
expected to be over far northwest ND into southeast Saskatchewan and
southwest Manitoba, in the zone of stronger large-scale forcing for
ascent along the northwest edge of the warm sector. These storms
will be supercells, a couple of which may be long-tracked. These
will be capable of producing very large hail and tornadoes given the
steep mid-level lapse rates/buoyancy and sufficient low-level
moisture with strong low-level shear/hodograph curvature. The areal
extent of this risk in northern ND should be rather confined as the
cap will probably inhibit storm development to its immediate south.
The second corridor of storm development is anticipated across
western SD in the zone of strongest surface heating and deep mixing.
Here, surface temperatures around 100 should weaken the cap
sufficiently for high-based storm development near the lee
trough/cyclone in vicinity of the Black Hills. Outflow generated by
this convection could help it persist as an MCS spreading northeast
through the evening. The very large MLCAPE plume and steep
low/mid-level lapse rates should result in severe wind being the
primary hazard, with isolated significant severe gusts possible.
Morning guidance does suggest that in spite of a strengthening
southwesterly low-level jet tonight, negative theta-e advection will
become increasingly common across the eastern Dakotas into
central/southern MN. This indicates a stout capping inversion will
overspread this region and likely result in weakening intensity of
this MCS overnight. However, a separate MCS should form as elevated
storms become widespread from northern MN southeast into WI in
association with strengthening low-level warm advection, on the
northeast edge of the elevated mixed-layer. While heavy rain should
be a comparatively greater hazard, the strongest cores could produce
isolated severe hail overnight.
..Grams/Nauslar.. 06/14/2018
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