EF1 tornado in Montgomery County, Iowa

At approximately 5:08 AM CST, a tornado developed east of Stanton, Iowa, near 230th Street and Q Avenue, and moved northeast. The tornado produced tree damage on the west side of Viking Lake, including large broken limbs and uprooted trees, with estimated winds of 70 to 85 mph. The tornado then crossed to the east side

of Viking Lake, where it uprooted two trees, brought down numerous large limbs, caused minor siding and roof damage to a home near 230th Street and Raspberry Drive, and snapped approximately 10 pine tree trunks near S Avenue and Aldersgate Drive. Based on this damage, winds were estimated at 90 mph. The tornado then continued northeast, collapsing the walls of an outbuilding, snapping a tree trunk, and bringing down power lines near U.S. Highway 24 and T Avenue. Based on this damage, peak winds were estimated around 105 mph. The tornado then lofted grain bins from over a mile away into the interchange of Highway 71 and Highway 34. The tornado dissipated at approximately 5:16 AM CST.

On the morning of June 11, 2026, severe thunderstorms pushing across southeast Nebraska into southwest Iowa produced tornadoes, large hail, damaging wind gusts, and flash flooding. The synoptic setup for the event featured broad upper-level troughing over the Northern High Plains, with a strong shortwave trough pushing into eastern Nebraska early in the day. This feature provided upper-level dynamic support for the amplification of the low-level jet (LLJ) alongside subsequent low-level warm air and moisture advection. This ultimately generated the forcing necessary for storm development, which began around 1:00 AM to 2:00 AM local time over central Nebraska.

As the LLJ strengthened overnight, a surface frontal boundary began to advance northward into southeast Nebraska. Isentropic upglide to the north of the surface front led to destabilization above the boundary layer. This elevated instability, combined with 40 to 55 knots of 1-3 km bulk shear along the nose of the LLJ, led to the organization of a strong mesoscale convective system (MCS) that tracked across eastern Nebraska and into southwest Iowa.

As the storms initally pushed into eastern Nebraska, the first report of large hail'measuring up to 1.25 inches in diameter'surfacing was reported in Seward County at 2:19 AM CST. By 3:00 AM CST, the system intensified and progressed eastward into Lancaster County, producing an initial 74 mph wind gust near Valparaiso and dropping hail up to 2.50 inches in diameter. As the storms tracked directly through Lancaster County between 3:11 AM and 4:01 AM CST, they generated widespread wind damage, snapping trees and downing powerlines. One notable incident occurred at 3:46 AM CST when an estimated 10-inch diameter tree limb fell onto a home, resulting in an injury. The system then continued east toward the Missouri River, pushing into Cass County around 4:04 AM CST where it immediately began causing structural damage and dropped its first reported tornadoes shortly after 4:10 AM CST.

Crossing into southwest Iowa around 4:30 AM CST, the system's focus shifted heavily toward pockets of damaging wind gusts, brief tornadoes and flash flooding. Tornadoes were reported consecutively across Fremont, Mills, Page, and Montgomery counties between 4:29 AM CST and 5:11 AM CST. As the morning progressed, intense straight-line winds up to 90 mph continued in a swatch across eastern Page and Montgomery counties in Iowa, particularly between Coburg and Villisca, IA. By 5:26 AM CST, the severe wind and hail threats began to transition into a significant flash flood event. Heavy downpours'including a staggering 6 inches of rain reported in Sidney, Iowa by 6:00 AM CST'led to flooded creeks, residential yards, and submerged roadways across Page and Fremont counties as the storms finally pushed out of the area.