Kansas City, MO...Tulsa, OK...Overland Park, KS...Springfield, MO...Kansas City, KS...
MARGINAL
186,694
12,274,194
St. Louis, MO...Des Moines, IA...Little Rock, AR...Cedar Rapids, IA...Topeka, KS...
Probabilistic Graphic
Probability of severe weather within 25 miles of a point. Hatched Area: 10% or greater probability of significant severe within 25 miles of a point.
Day 2 Prob. Risk
Area (sq. mi.)
Area Pop.
Some Larger Population Centers in Risk Area
15 %
72,583
6,089,536
Kansas City, MO...Tulsa, OK...Overland Park, KS...Springfield, MO...Kansas City, KS...
5 %
189,387
12,539,275
St. Louis, MO...Des Moines, IA...Little Rock, AR...Cedar Rapids, IA...Topeka, KS...
SPC AC 050637
Day 2 Convective Outlook
NWS Storm Prediction Center Norman OK
1237 AM CST Sun Mar 05 2017
Valid 061200Z - 071200Z
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS THE OZARKS
AND VICINITY...
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS FROM PARTS OF
THE UPPER AND MIDDLE MISSISSIPPI VALLEY TO SOUTHEAST OKLAHOMA AND
EXTREME NORTHEAST TEXAS...
...SUMMARY...
A few severe storms will be possible from Monday evening through
early Tuesday morning from parts of the upper and middle Mississippi
Valley southwestward to the Ozarks.
...Synopsis...
General synoptic evolution remains consistent in model forecasts, as
a deep/cold midlevel trough just off the Pacific Northwest coast
progresses inland to the central/northern Plains by Monday evening,
and the upper MS Valley and upper Great Lakes by early Tuesday.
Associated surface cyclogenesis is expected from the northern Plains
to western Ontario, and a trailing cold front will move
southeastward across the central/southern Plains and MS Valley by
the end of the period. The primary focus for strong/severe storm
development will be along and immediately in advance of the cold
front.
...Upper/mid MS Valley to the Ozarks Monday evening/overnight...
Some minor differences persist with the eastward movement of the
cold front, related to the translation of the ejecting speed max
aloft, with the GFS still a bit faster (as is somewhat typical), and
the ECMWF/NAM a bit slower. The more important differences center
on the magnitude of low-level moistening and surface heating within
the moist sector Monday, with the NAM remaining more aggressive with
destabilization compared to other model forecasts. However, the
general scenario remains consistent with storm development expected
along the cold front late Monday from southern MN/IA into northwest
MO and northeast KS, where ascent will be focused northeast of the
dryline-cold front triple point.
Given more marginal moisture/buoyancy with northward extent, the
initial storms along the cold front should evolve into a line with a
marginal damaging wind risk per strong low-midlevel winds/shear and
relatively straight hodographs. The risk for strong/severe storms
should be a little greater and persist longer to the south, in
proximity to richer low-level moisture. While the convective mode
will trend toward linear organization, deep-layer and low-level
shear will be favorable for some embedded supercell risk from parts
of MO southwestward. Convection will develop southward overnight as
the cold front overtakes the remnant dryline across KS/OK. Storm
initiation still seems questionable at best along the dryline in OK.
The stronger forcing for ascent will pass well to the north,
somewhat veered low-level flow will not favor long residence times
in the zone of ascent along the dryline, and high clouds could limit
surface heating somewhat.
..Thompson.. 03/05/2017
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