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You are looking at an outlook that is part of the medium range forecast (the outlook for days 4-8). The most important thing to note is that lack of a risk does not mean zero risk. Generally speaking, confidence has to be pretty high for the Storm Prediction Center to have an outlook area this far into the future.
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| Day 4 | Saturday, August 29 | predictability too low |
| Day 5 | Sunday, August 30 | predictability too low |
| Day 6 | Monday, August 31 | predictability too low |
| Day 7 | Tuesday, September 1 | predictability too low |
| Day 8 | Wednesday, September 2 | predictability too low |
ZCZC SPCSWOD48 ALL ACUS48 KWNS 260842 SPC AC 260842
Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0342 AM CDT Wed Aug 26 2026
Valid 291200Z - 031200Z
DISCUSSION
D4/Saturday - Northern Plains to Upper Midwest
A mid-level ridge will move slowly east across the Plains with slight suppression through the day. A lee trough will consolidate into a surface low across the northern Plains through the day Saturday. Ahead of this surface low, strong instability is forecast across South Dakota and vicinity. Despite the favorable environment across this region, primary forcing will be focused on the nose of the low-level jet across Iowa and into Wisconsin, well east of the greatest instability and near the Canadian border. Therefore, limited storm coverage precludes severe weather probabilities at this time, but given the favorable environment, it will need to be monitored closely.
D5/Sunday - North Dakota and Vicinity
A mid-level shortwave trough will move from the Pacific Northwest to the northern Plains Saturday/D4 and Sunday/D5. 00Z guidance has come into fairly consistent agreement with the location and amplitude of this trough across eastern Montana at 00Z Sunday evening. However, there is considerable disagreement with the degree of destabilization across North Dakota, where forcing will be greatest. The GFS dry bias across most of the Plains has severely lessened the instability. However, despite this challenge, it is apparent that most of the instability significantly southeast of the upper-level forcing. The GFS-Para seems to have a more realistic handle on low-level moisture/instability magnitude but it also shows a significant disconnect between where this instability is located and the deeper forcing.
The deterministic ECMWF forecast shows a potentially significant severe weather event across North Dakota with strong instability and shear ahead of a robust convective QPF signal. This is supported by the AI-ECMWF which shows a similar evolution. However, the EC-ensemble mean of instability shows at least some trend toward the GEFS with primary instability southeast of the best forcing.
It is also worth noting that the wave is forecast to eject across North Dakota relatively late (~06Z) which may be a somewhat limiting factor to a greater threat. This potential timing disconnect, combined with some hint of limited overlap between the greatest instability and the primary upper forcing, cast enough uncertainty to preclude severe weather probabilities at this time. However, it is worth noting that if a solution similar to the ECMWF materializes, a significant severe weather event is possible.
D6 and Beyond
By early next week, the primary mid-level ridge appears to center around the southern Appalachians with broad southwesterly flow from the Southwest to the Great Lakes. Within this area of southwesterly flow, multiple embedded mid-level shortwave troughs are forecast. Predictability of these smaller scale features is relatively low at this range, but some continued severe weather threat will likely persist around the periphery of the ridge from the Plains to the Great Lakes and potentially into the Northeast.
..Bentley.. 08/26/2026
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