Minneapolis, MN...St. Paul, MN...Sioux Falls, SD...Rochester, MN...Duluth, 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 2 Wind Risk
Area (sq. mi.)
Area Pop.
Some Larger Population Centers in Risk Area
30 %
19,355
76,768
North Platte, NE...
15 %
199,956
5,341,097
Minneapolis, MN...St. Paul, MN...Sioux Falls, SD...Fargo, ND...Bloomington, MN...
5 %
348,233
66,016,808
New York, NY...Philadelphia, PA...Baltimore, MD...Boston, MA...Denver, 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.
Minneapolis, MN...St. Paul, MN...Sioux Falls, SD...Fargo, ND...Bloomington, MN...
5 %
244,936
12,332,842
Denver, CO...New Orleans, LA...Colorado Springs, CO...Aurora, CO...Lincoln, NE...
SPC AC 121736
Day 2 Convective Outlook
NWS Storm Prediction Center Norman OK
1236 PM CDT Sun Jul 12 2020
Valid 131200Z - 141200Z
...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS ACROSS WESTERN
NEBRASKA AND FAR NORTHEASTERN COLORADO...
...SUMMARY...
Severe storms are possible across portions of the central Plains
into the eastern Dakotas, western Minnesota and Iowa on Monday
afternoon into Monday night. Additional isolated strong storms are
possible near the Gulf Coast region and from the eastern Carolinas
into Southern New England Monday afternoon.
...Synopsis...
A longwave trough over western Canada/northwestern CONUS will
continue to amplify slightly, spreading height falls as south as
Utah and Colorado during the day. Meanwhile, a substantial
shortwave trough will migrate through the base of the broader trough
and impact the Dakotas and Minnesota through the latter half of the
forecast period. Meanwhile, a mid-level ridge centered over New
Mexico/west Texas will weaken slightly, while another long-wave
trough along the East Coast shifts slowly eastward throughout the
period.
At the surface, lee troughing will extend from the central Dakotas
southward through eastern New Mexico/Texas Panhandle initially and
gradually strengthen/deepen throughout the day. The northern
portion of this trough (across the Dakotas) will shift eastward
toward western Minnesota through the afternoon. Another weak
surface trough will extend from New England southwestward to the
Carolinas, with a trailing boundary extending westward toward south
Louisiana. The position of this boundary may be augmented by
ongoing convection during the D1 period, which may impact subsequent
afternoon development of thunderstorms in Louisiana during the
forecast period.
...Nebraska southward through northeastern New Mexico...
Models suggest that convective development will begin in earnest
across the higher terrain of the central Rockies during the early
afternoon within a deeply mixed boundary layer environment and weak
low-level shear. These storms will likely evolve into clusters and
loosely organized linear segments that propagate eastward into
gradually deeper boundary layer moisture through the afternoon and
early evening. The greatest concentration of storms is currently
expected from western through northeastern Nebraska, where enough of
a concentration of severe wind/hail producing convection will exist
to justify a categorical upgrade to Enhanced driven by 30% hail and
30% wind probabilities. Storms in this environment will tend to be
outflow dominant, although steep tropospheric lapse rates, upper 50s
to low 60s F dewpoints, and afternoon temperatures nearing 100 F
will maintain 3000 J/kg MUCAPE, while 40-45 kt deep shear will aid
in modest organization into linear segments. An isolated tornado
cannot be ruled out - especially in Nebraska. Farther south,
somewhat weaker deep shear will exist in eastern Colorado, New
Mexico, and vicinity, although enough flow aloft will exist to
encourage forward-propagating clusters and linear segments that
could reach western Kansas and the Texas/Oklahoma Panhandles late in
the day. Large hail and damaging wind gusts are possible with this
activity.
...Eastern Dakotas through western Wisconsin...
The aforementioned shortwave will advance upon western portions of
the warm sector in that area and encourage robust convective
development beginning in eastern North Dakota/northwestern Minnesota
during the afternoon. Initial development will likely be
supercellular - enough mid-level inhibition will exist to keep
storms isolated within an environment characterized by appreciable
low-level sear (200-300 m2/s2 SRH) and 2000-2500 J/kg MLCAPE.
Significant hail and a few tornadoes are possible - especially near
discrete updrafts.
Over time, models suggest that these storms will congeal into one or
two linear complexes that will migrate eastward across much of
northern and central Minnesota through the evening. All severe
hazards will be possible through the evening before storms gradually
become elevated due to nocturnal boundary layer cooling.
Nevertheless, steep lapse rates aloft and appreciable mid-level flow
will promote a hail/wind risk even after dark as far east as western
Wisconsin. Additional convection migrating northeastward from
Nebraska into eastern South Dakota will also be capable of hail and
damaging wind gusts.
...Louisiana, far southeast Texas, and coastal Mississippi...
Though forcing for ascent is modest at best, a weak surface
boundary/remnant outflow boundary will exist across the region and
may promote isolated thunderstorm development during the afternoon.
Dry air aloft, steep mid-level lapse rates, and near 80F
dewpoints/90s F surface temperatures will promote very strong
instability and downdraft potential within any convection that can
materialize. 5% hail/wind probabilities were address to address
this primarily diurnally driven threat.
...New England southward through the Carolinas...
Though mid-level lapse rates will generally be weaker compared to
areas west, the combination of surface heating and ascent with the
longwave trough over the region will foster scattered to numerous
band of convection throughout the entire region in the afternoon and
early evening. Enough mid-level flow will exist for loose
organization into clusters and linear segments, which will promote
potential for isolated damaging wind gusts in a few areas. This
threat will also be diurnally driven and wane after sunset.
..Cook.. 07/12/2020
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