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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.
When no specific risk areas are shown, you might see one of these phrases:
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| Day 4 | Monday, May 25 | potential too low |
| Day 5 | Tuesday, May 26 | predictability too low |
| Day 6 | Wednesday, May 27 | predictability too low |
| Day 7 | Thursday, May 28 | predictability too low |
| Day 8 | Friday, May 29 | predictability too low |
ZCZC SPCSWOD48 ALL ACUS48 KWNS 220901 SPC AC 220901
Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0401 AM CDT Fri May 22 2026
Valid 251200Z - 301200Z
DISCUSSION
Severe potential will remain low D4/Monday. Height rises begin across the central US with a high amplitude ridge settling in from the west. Slow moisture return will be ongoing across much of the Plains into the Midwest with widely scattered areas of rainfall and thunderstorms. A few strong to marginally severe storms will be possible, but generally weak flow and subsidence will keep organized storm potential low.
A trough is progged to begin deepening across the Pacific Northwest D5/Tuesday into D6/Wednesday. As the upper low slowly shifts eastward, stronger flow will overspread the Intermountain West into the Northern Rockies, resulting in strengthening lee troughing across the central/northern Plains. Moisture advection will spread northward amid strengthening southerly flow across the central/northern Plains. There remains uncertainty in the northward and westward extent of moisture return and in progression of the western trough. Severe storms may occur each day across some portion of the northern and northern/central High Plains. For now, confidence in exact corridors remains low.
By D7/Thursday-D8/Friday, guidance suggests the western low becomes cut off and slowly wobbles towards the Great Basin before becoming absorbed back into the northern stream. This is likely due to continued high amplitude ridging across the central US. Some severe potential may extend into the eastern US as a cold front shifts southward as flow enhances in the trough across Quebec in the D7-D8 period.
..Thornton.. 05/22/2026
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