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StormProofhail seasonsOrlando → 2015

Orlando hail season 2015

10 NWS-recorded hail reports ≥1″ within 30 miles, across 6 storm days, max 1.75". Every one of those reports is a dated, located, citable official record — the context behind this market's 2015 claim volume.

Biggest storm days (2015, final record)

Date≥1″ reportsMax hailAreas named in the record
June 1, 201551.75"ORANGE, SEMINOLE
August 20, 201511.00"OSCEOLA
July 5, 201511.00"SEMINOLE
July 3, 201511.00"LAKE
June 20, 201511.00"OSCEOLA

“Quarter sized hail was reported via social media near the intersection of Interstate 4 and State Road 46 in Sanford. Quarter sized hail was also reported by a trained spotter near Lake Emma Road and Lake Mary Boulevard and nickel sized hail was reported near Greenwood Boulevard, both in Sanford.”

— NWS event narrative, June 1, 2015 (NCEI Storm Events)

When it fell

May 1 · Jun 6 · Jul 2 · Aug 1

Wind context: the record also holds 7 thunderstorm-wind events ≥50 kt (≈58 mph, the NWS severe criterion) in this radius for 2015 — relevant where the dispute is wind vs hail causation.

Working a Orlando claim from 2015?

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 30 miles of the Orlando 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.