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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 | Wednesday, July 22 | 15% |
| Day 5 | Thursday, July 23 | predictability too low |
| Day 6 | Friday, July 24 | predictability too low |
| Day 7 | Saturday, July 25 | predictability too low |
| Day 8 | Sunday, July 26 | predictability too low |
ZCZC SPCSWOD48 ALL ACUS48 KWNS 190746 SPC AC 190746
Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0246 AM CDT Sun Jul 19 2026
Valid 221200Z - 271200Z
DISCUSSION
Day 4/Wed - Mid-Atlantic/Carolinas
An upper trough will lift northeast across the region on Wednesday. At the surface, a cold front will be oriented from roughly the Hudson Valley to the central Appalachians at the beginning of the period. Within a zone of strong warm advection ahead of the surface front, widespread showers and thunderstorm may be ongoing across parts of the Mid-Atlantic and Northeast, resulting in uncertainty regarding northward extent of severe potential. For now, the 15 percent severe probability has been confined to portions of the southern Mid-Atlantic and Carolinas ahead of the surface trough/cold front. A very moist airmass will be in place across the region, and 25-35 kt effective shear magnitudes are forecast. Thunderstorm clusters or linear bands are expected to move across the region through evening, posing mainly a risk for damaging winds.
Days 5-8/Thu-Sun
Severe potential is expected to be lower late in the week into the weekend. An upper trough will persist over the eastern U.S., but deep-layer flow will be weak. Further west, the subtropical high will intensify over the Plains and into the Four Corners vicinity while the associated amplified upper ridge persists northward into the Canadian Prairies. As boundary layer moisture spreads northward beneath the upper ridge, some severe potential could develop each day across parts of the High Plains. However, this will largely be driven by mesoscale processes not well resolved at longer lead times. Overall, the intense upper ridge should largely suppress greater severe potential.
..Leitman.. 07/19/2026
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