Sutherland, NE Hail Storm – July 2026

A severe hail storm tracked through Sutherland, NE on July 4, 2026, producing stones up to 3.13 inches and multiple concentrated hail cores. The event developed in late afternoon and persisted into early evening, generating a long sequence of radar-detected hail alerts and spotter observations.

What Happened

NWS issued 15 hail alerts between 3:48 PM CDT and 7:57 PM CDT as the storm crossed the Sutherland metro. Dual-polarization radar repeatedly detected compact hail cores with size estimates reported in alerts from about 1.0 inch to 2.4 inches; spotter reports supplemented the radar picture. At 3:55 PM CDT an mPing submission recorded a 2.5-inch stone near Sutherland. Mid-afternoon observations around 4:41 PM CDT noted mostly dime- to nickel-sized hail with a few golf-ball sized pieces, and a late report at 7:05 PM CDT described primarily pea- to nickel-sized hail with occasional quarters.

The sequence shows a storm that produced discrete, intense hail cores rather than a single uniform swath. Radar detections and spotter-verified reports align in time, with the largest surface observations occurring early in the sequence and smaller stones appearing as the storm evolved toward evening. NWS alerts during the event were driven primarily by dual-polarization radar hail detection and supplemented by a spotter submission at 7:30 PM CDT.

Damage Assessment

Field reports indicate localized heavy impacts in the Sutherland vicinity. The 3:55 PM CDT mPing entry documenting a 2.5-inch stone signals a concentrated pocket capable of causing roof and vehicle impact where that core crossed populated streets. The 4:41 PM CDT observer account of golf-ball sized pieces identifies a separate area of elevated exposure for exterior glass, soft metal, and exposed equipment. The later 7:05 PM CDT report of pea- to nickel-sized hail documents the storm weakening as it moved away from the town core.

Radar-detected hail cores occurred intermittently across the NWS warning area rather than uniformly across the entire polygon. That produced a patchy impact pattern inside Sutherland city limits and adjacent rural sections. Ground-truth measurements and observer timing indicate at least two arrival pulses of damaging-size hail in the town footprint: an early, high-impact pulse near mid-afternoon and a secondary, smaller-pulse in the late afternoon to early evening window. Photographic or physical evidence from those specific streets and neighborhoods will be necessary to link observed losses to the early large-stone pulse.

What Contractors Should Know

Prioritize inspections in locations tied to timed observations. Start with the area nearest the 3:55 PM CDT mPing report and then sample properties near the 4:41 PM CDT golf-ball observation. Take representative roof, gutter, and vehicle photos with a timestamp. Note exact addresses and the report times on each file. Field teams should document hail diameter against a known scale in every photo.