Tornado, Damaging Wind Risk in Illinois and Indiana Today
- Andrew Pritchard

- Dec 28, 2025
- 3 min read
Classic clash of the air masses today as warm and humid air surges northward into the Midwest, with bitterly cold Arctic air blasting across the Dakotas. The result will be a dynamic, high impact storm system with blizzard and winter storm conditions across the Upper Midwest and Great Lakes, with a springlike severe weather setup in the warm sector across portions of Illinois and Indiana.


The severe risk across Illinois and Indiana comes in two distinct rounds. First, as the warm front lifts north a few intense storms may produce hail generally near I-80 across north-central Illinois, moving into northeast Illinois and eventually northern Indiana mid to late Sunday morning. These storms and their hail risk may even make it into southern Michigan by mid-day.

The potentially more robust and higher impact round of severe storms accompanies the area of low pressure and cold front as it moves east into eastern Illinois, approaching the Indiana border mid afternoon into the evening hours. If we were looking at a better aligned surface low with southerly surface winds, I think we'd be looking at a tornado outbreak across eastern Illinois into Indiana later today. You've got really anomalously high moisture with dew points in the low 60s, and a 110 knot jet stream at 500 mb screaming overhead. Show me just dew points and H5 winds today and I'm super concerned.

As it is, surface winds out of the south-southwest may still allow just enough of a "hump" in the low-level hodograph to allow for a couple of supercells with an associated tornado risk ahead of the cold front, that is unless they're right up against the Arctic cold front blasting in from the east.

Less than perfect surface winds and a strongly forced cold front might make this lean linear with a predominant wind damage risk, but there's just enough to make me go "hmmm" here and think either a kinky line with embedded tornadoes or at least one or two supercells ahead of the cold front might be possible.
Here's what the Storm Prediction Center has to say in their latest outlook which upgraded the Illinois/Indiana border to slight risk / level 2 out of 5:
WATER-VAPOR IMAGERY THIS MORNING SHOWS A MID-LEVEL LOW NEAR THE MT/ND BORDER WITH A TROUGH INTO THE CENTRAL ROCKIES/SANGRE DE CRISTOS. THIS MID-LEVEL LOW WILL MOVE INTO THE CENTRAL GREAT LAKES BY EARLY MONDAY MORNING. STRONG SOUTHWESTERLY 500-MB FLOW (80 KT) EXTENDING FROM THE BASE OF THE TROUGH THROUGH THE LOWER MO VALLEY AND OH VALLEY WILL FEATURE AN INTENSIFYING 110-KT JET REACHING THE MO-IL BORDER THIS EVENING BEFORE FURTHER STRENGTHENING TO 130 KT OVER OH BY THE END OF THE PERIOD. A SURFACE LOW OVER EASTERN KS WILL DEEPEN RAPIDLY THROUGH TONIGHT AS IT MOVES TO LAKE HURON. A FRONTAL ZONE EXTENDING EAST-NORTHEAST THROUGH THE SOUTHERN GREAT LAKES THIS MORNING WILL SERVE AS THE NORTHERN EDGE OF THE MOIST SECTOR. A COLD FRONT INITIALLY OVER KS-OK WILL SURGE SOUTH-EAST. SOUTHERLY LOW-LEVEL FLOW ACROSS THE MOIST SECTOR WILL MAINTAIN A FETCH OF SEASONABLY HIGH 58-62 DEG F DEWPOINTS IMMEDIATELY AHEAD OF THE FRONT/LOW. A RAIN SHIELD WITH EMBEDDED THUNDERSTORMS THIS MORNING FROM NORTHERN MO INTO THE SOUTHERN GREAT LAKES COULD FEATURE A STRONGER STORM OR TWO THROUGH MIDDAY, BUT THE PRIMARY SEVERE RISK WILL LIKELY FOCUS THIS AFTERNOON THROUGH TONIGHT. MODEL GUIDANCE INDICATES THE CAP WILL ERODE NEAR THE EVOLVING TRIPLE POINT AND COLD FRONT BY MID-LATE AFTERNOON. UPWARDS OF 500-1000 J/KG MLCAPE IS POSSIBLE ACROSS PARTS OF CENTRAL INTO EASTERN IL WITH BUOYANCY TAPERING WITH EAST EXTENT ACROSS THE OH VALLEY. A SOUTHWARD-DEVELOPING CONVECTIVE BAND IS FORECAST TO EVOLVE LATE THIS AFTERNOON THROUGH THE EARLY EVENING. LONG HODOGRAPHS AND STRONG 2-3 KM FLOW WILL FAVOR A RISK FOR SEVERE GUSTS WITH THE MORE INTENSE STORMS AND SURGES WITH THE MATURING BAND. MODELS INDICATE THE WIND-DAMAGE THREAT MAY PERSIST ACROSS THE OH VALLEY/SOUTHERN GREAT LAKES TONIGHT DESPITE MEAGER INSTABILITY. THE TORNADO RISK APPEARS HIGHEST WITH CELLS THAT CAN DEVELOP NEAR THE INSTABILITY AXIS AND MATURE BEFORE EITHER DESTRUCTIVE INTERFERENCE OF THE LARGER-SCALE COLD POOL OVERWHELMS CELLULAR MODE, AND/OR THIS ACTIVITY MOVES FARTHER EAST INTO LESSENING INSTABILITY. 




