SPC AC 210728
Day 3 Convective Outlook
NWS Storm Prediction Center Norman OK
0228 AM CDT Thu May 21 2020
Valid 231200Z - 241200Z
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS SATURDAY AFTERNOON
AND EVENING ACROSS MUCH OF CENTRAL AND SOUTHERN SOUTH DAKOTA AND
NORTHERN AND CENTRAL NEBRASKA...
...SUMMARY...
An organized cluster of thunderstorms may develop to the east and
southeast of the Black Hills Saturday afternoon, before spreading
into adjacent portions of the Plains and middle Missouri Valley,
accompanied by a risk for large hail and strong wind gusts through
Saturday evening.
...Synopsis...
Models suggest a continued weakening of the westerlies across the
U.S. Saturday through Saturday night. Mid-level ridging is forecast
to build northeast of the southern mid-latitude eastern Pacific,
toward the U.S. Pacific coast. As this occurs, initially amplified
downstream cyclonic flow over the Intermountain West and Rockies may
begin to split. One embedded perturbation, including a vigorous
remnant cyclonic vorticity center, appears likely to accelerate
northeast of the northern Great Basin, into the higher northern
plains by late Saturday night. Another may evolve and dig across
the Four Corners states.
Downstream, ridging may continue to build across much of the lower
Mississippi Valley and Southeast, while a remnant mid-level closed
low digs off the Mid Atlantic coast. Weakening troughing may also
progress around the crest of the southern branch ridging, across
parts of the Upper Midwest and Great Lakes region.
In lower levels, boundary-layer moisture return into the vicinity of
surface troughing across much of the plains appears likely to
contribute to moderate to large CAPE, with daytime heating beneath
steep mid-level lapse rates associated with warm elevated
mixed-layer air. In the presence of modest vertical shear, aided by
veering of wind fields with height, this environment is expected to
become conducive to scattered strong to severe thunderstorm
development Saturday afternoon and evening.
...Plains...
Models continue to suggest that the strongest and most organized
convective development will become focused east and southeast of the
Black Hills, beneath a strongly difluent upper flow regime, and
perhaps aided by forcing associated with lower/mid tropospheric warm
advection. This is expected to be near the nose of the plume of
warmer elevated mixed-layer air, where mid-level cooling will weaken
inhibition. Surface dew points increasing into mid 60s+ F, are
forecast to contribute to mixed-layer CAPE in excess of 2000 J/kg,
which should support vigorous updrafts capable of producing large
hail.
Deep-layer vertical shear probably will become at least marginally
sufficient for supercells initially. Low-level hodographs may
become large enough to support a risk for tornadoes. However,
activity may tend to grow upscale fairly quickly, with strong wind
gusts becoming the prominent severe hazard. The evolution of an
increasingly organized convective system is possible, which may
persist through much of the evening, while propagating eastward and
southeastward.
..Kerr.. 05/21/2020
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