StormProof → hail seasons → Toledo → 2010
Toledo hail season 2010
20 NWS-recorded hail reports ≥1″ within 25 miles, across 4 storm days, max 1.75". Every one of those reports is a dated, located, citable official record — the context behind this market's 2010 claim volume.
Biggest storm days (2010, final record)
| Date | ≥1″ reports | Max hail | Areas named in the record |
|---|---|---|---|
| May 5, 2010 | 12 | 1.75" | LUCAS, OTTAWA, WOOD, FULTON |
| May 7, 2010 | 5 | 1.75" | WOOD, SANDUSKY, LUCAS |
| August 15, 2010 | 2 | 1.25" | OTTAWA |
| May 1, 2010 | 1 | 1.00" | MONROE |
“Golf ball size hail was reported. A few vehicles sustained minor damage from the hail.”
— NWS event narrative, May 5, 2010 (NCEI Storm Events)
When it fell
May 18 · Aug 2
Wind context: the record also holds 59 thunderstorm-wind events ≥50 kt (≈58 mph, the NWS severe criterion) in this radius for 2010 — relevant where the dispute is wind vs hail causation.
Working a Toledo claim from 2010?
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.
Unlimited reports — Pro $99/mo Single report $29
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.