SPC 1200Z Day 1 Outlook
Day 1 Convective Outlook
NWS Storm Prediction Center Norman OK
0100 AM CDT Sat Aug 16 2025
Valid 161200Z - 171200Z
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS LATE THIS
AFTERNOON INTO TONIGHT ACROSS SOUTH DAKOTA AND PERHAPS ADJACENT
PORTIONS OF NORTHERN NEBRASKA...NORTHEASTERN WYOMING...SOUTHEASTERN
MONTANA...AND SOUTHWESTERN NORTH DAKOTA...
...SUMMARY...
Scattered strong thunderstorm development, including a couple of
evolving clusters posing a risk for strong to severe wind gusts, are
possible today into tonight across parts of the northern Great
Plains into Midwest and Great Lakes region.
...Discussion...
Stronger westerlies in the northern mid-latitudes are forecast to
generally remain confined to the north of the Canadian/U.S. border.
Within this regime, mid-level ridging, now building across and
northeast of the Canadian and adjacent northern U.S. Rockies, is
likely to undergo further amplification across and east of the
Canadian Prairies later today through tonight, downstream of an
initially vigorous short wave trough pivoting northeastward inland
of the British Columbia coast.
Models indicate that larger-scale troughing across the northeastern
Pacific will be maintained, as another vigorous short wave trough
digs southeast of the Gulf of Alaska. Downstream of the building
ridge, large-scale eastern Canadian mid-level troughing is forecast
to undergo amplification, as another notable short wave trough digs
across and southeast/east of the northern Ontario/southern Hudson
and James Bay vicinities. Even as this occurs, it appears that
modest mid-level height rises will develop across eastern portions
of the northern U.S. Great Plains through the Upper Midwest and
adjacent Great Lakes region later today through tonight, downstream
of mid-level troughing within weak, broadly confluent mid-level flow
across the Wyoming/Colorado Rockies into the western Dakotas. The
remnants of an initially notable convectively generated or enhanced
perturbation may dig southeastward within the northeastern periphery
of the building ridging, across the Midwest/adjacent Great Lakes
vicinity into Ohio Valley. However, there is considerably greater
spread evident in model output concerning this feature.
...Northern Great Plains into Great Lakes/Ohio Valley...
South of the westerlies, convective potential may depend largely on
sub-synoptic developments with still relatively low predictability.
The NAM and Rapid Refresh, among other model output, continue to
suggest a notable perturbation evolving with a consolidating cluster
of storms now across parts of central South Dakota into north
central Nebraska. By 12Z this morning, it appears that this may be
in the process of spreading east of the mid Missouri through upper
Mississippi Valleys, above a boundary-layer stabilized by preceding
convective activity.
A conglomerate surface outflow boundary currently extends from parts
of central Illinois through central Iowa and Minnesota. It seems
probable that the southern flank of this boundary will undergo at
least some modification/northward return into and beyond daybreak,
but the extent remains unclear. Outflow impacted air across eastern
Minnesota and northeastern Iowa into Wisconsin will probably be
reinforced by the approaching cluster, which probably will tend to
weaken while overspreading the Upper Midwest into Great Lakes
region. However, depending on how quickly the boundary-layer is
able to modify on the trailing flank of the reinforced outflow, it
appears possible that renewed thunderstorm development and
intensification could occur, and eventually grow upscale into
another organizing cluster with a tendency to propagate
southeastward toward the Ohio Valley.
HREF output suggests that a corridor across southern Wisconsin
toward areas near and south of southern Lake Michigan may need to be
considered for higher severe probabilities in later outlooks for
this period. However, given uncertain boundary-layer
destabilization, coupled with a tendency for warming aloft/rising
mid-level heights, in the presence of generally weak ambient mean
flow, there seems a reasonable possibility that the corridor of
higher convective potential evident in the HREF may be displaced, if
not overdone.
Otherwise, there remains a signal in model output that the
approaching mid-level troughing could contribute to another upscale
growing cluster of storms with potential to produce strong to severe
wind gusts across parts of South Dakota this evening. However, this
signal is more tempered than prior days.
..Kerr/Lyons.. 08/16/2025
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