September 19, 2026 hail storm near Chadron, NE. Radar-confirmed hail track and contractor lead lists available.
NWS WARNING AREA · Chadron Metro · Sep 19, 2026
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Pro coverage in California, Vermont, and Oregon includes the confirmed hail track and Strike Map only — no address lists. State data-privacy law treats compiled address lists differently in those three states, so we exclude their addresses from extraction and delivery.
This storm generated 3 NWS alert zones. Pro access covers the complete storm track and all addresses across every zone.
Chadron, NE
33 addresses in warning area
Alert issued Sat, Sep 19 · 10:15 PM UTC
Hay Springs, NE
26 addresses in warning area
Alert issued Sat, Sep 19 · 10:49 PM UTC
Chadron, NE
46 addresses in warning area
Alert issued Sat, Sep 19 · 10:57 PM UTC
A strong late-afternoon hail storm moved through the Chadron, Nebraska metro on September 19, 2026, producing stones up to 1.85 inches and radar-detected hail cores during the early evening.
Dual-polarization radar first detected a hail-producing cell near the Chadron metro at 5:15 PM CDT. The initial radar-derived estimate registered 1.67-inch hail. Subsequent radar updates showed a weakening and reintensifying core with 1.38-inch estimates at 5:49 PM CDT and a 1.69-inch pulse at 5:57 PM CDT. The local storm report feed included a trained spotter observation at 5:59 PM CDT who reported half-dollar sized hail, estimating 1.25 inches, and gusts around 40–50 mph at his location. The radar sequence and the spotter observation align in time and location, indicating the hail-producing core crossed the Chadron metro in the late afternoon to early evening period.
Field reports for this event are limited to the trained spotter’s observation of half-dollar hail and 40–50 mph gusts near the Chadron metro at 5:59 PM CDT. Radar-detected hail echoes overlapped that report window, indicating the strongest returns passed through the same sector of the metro between 5:15 PM and 5:57 PM CDT. Where the spotter observed 1.25-inch stones and strong gusts, outdoor assets exposed at the time were at highest risk.
Inspectors should note that impacts tied to this event will be most concentrated in the immediate vicinity of the spotter location and along the radar-derived hail swath that crossed the metro in the late-afternoon window. Any photographic or physical evidence gathered should reference the 5:59 PM CDT spotter time and the radar alert times. Reports of isolated surface impacts are more consistent with localized 1–2 inch hail pulses than with a broad, continuous damage corridor across the entire county.
Begin inspections by targeting the addresses closest to the spotter location and the centerline of the radar-detected hail swath. Prioritize vehicles that were parked outdoors, exposed soft signage, and single-layer or aged asphalt shingle roofs in those areas. Stones in the 1.25–1.85 inch range commonly dent aluminum panels, damage HVAC fins, and accelerate loss of shingle granules where shingles are already weathered. Document sample locations with date-stamped photos and include the 5:59 PM CDT spotter observation in the claim notes.
For roofing crews, focus initial roof walks on visible hail impact patterns near ridges, valleys, and on north-facing slopes where ice melt patterns and granule displacement are easier to differentiate from preexisting wear. For vehicle inspections, look for round dents on sheet metal, chipped paint on exposed edges, and broken plastic trim. For exterior siding and skylights, inspect for pitting and radial fractures that align with the late-afternoon impact window. Record wind-related issues separately from hail where possible, since the spotter reported 40–50 mph gusts concurrent with the hail.
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Try the Free Demo →Schedule follow-up inspections during daylight and clear weather to ensure reliable photographic documentation. When filing estimates, reference the spotter-verified hail size, the radar-derived alert times, and the specific streets or addresses inspected in the Chadron metro. Closed-loop communication between field crews and adjusters will reduce re-inspection needs.
For a radar-confirmed hail swath and the paid damage zone overlay, see the Strike Map.
Address data is sourced from the US National Address Database (NOAA/USDOT). Inclusion of an address does not guarantee physical damage occurred. Confidence scores are radar-derived estimates. Data Accuracy Disclaimer