StormProof → hail seasons → Toledo → 2011
Toledo hail season 2011
14 NWS-recorded hail reports ≥1″ within 25 miles, across 6 storm days, max 2.00". Every one of those reports is a dated, located, citable official record — the context behind this market's 2011 claim volume.
Biggest storm days (2011, final record)
| Date | ≥1″ reports | Max hail | Areas named in the record |
|---|---|---|---|
| August 18, 2011 | 7 | 2.00" | WOOD, LUCAS |
| November 14, 2011 | 2 | 1.50" | WOOD |
| August 1, 2011 | 2 | 1.75" | SANDUSKY, OTTAWA |
| June 9, 2011 | 1 | 1.00" | MONROE |
| May 25, 2011 | 1 | 1.50" | LUCAS |
“Hail as large as hen eggs fell on the Shoreland area for several minutes. Many vehicles were damaged by the hail.”
— NWS event narrative, August 18, 2011 (NCEI Storm Events)
When it fell
Mar 1 · May 1 · Jun 1 · Aug 9 · Nov 2
Wind context: the record also holds 65 thunderstorm-wind events ≥50 kt (≈58 mph, the NWS severe criterion) in this radius for 2011 — relevant where the dispute is wind vs hail causation.
Working a Toledo claim from 2011?
These are aggregates. A claim file needs the per-address record: every recorded event within 1, 3 and 10 miles of the property, distances, official narratives, and citations an adjuster can check line by line. That's the report — generated in seconds, hosted on HailEvidence (the neutral evidence surface), formatted as an insurance-appeal attachment.
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Provenance
Final counts: NCEI Storm Events Database, file vintage c20260527, hail events with recorded magnitude ≥1.00″ and point coordinates within 25 miles of the Toledo anchor. NWS records are point and path observations. The absence of a nearby report does NOT prove that no hail fell at this address — it means no observation was logged nearby. A report of nearby hail documents the event; it does not by itself prove damage to a specific structure. Spotted an error? Email the address on our terms page and we correct against the source.