StormProof → hail seasons → Columbia (SC) → 2012
Columbia (SC) hail season 2012
33 NWS-recorded hail reports ≥1″ within 25 miles, across 9 storm days, max 2.00". Every one of those reports is a dated, located, citable official record — the context behind this market's 2012 claim volume.
Biggest storm days (2012, final record)
| Date | ≥1″ reports | Max hail | Areas named in the record |
|---|---|---|---|
| July 1, 2012 | 15 | 2.00" | LEXINGTON, RICHLAND, FAIRFIELD |
| March 24, 2012 | 5 | 1.25" | RICHLAND, SUMTER, LEXINGTON |
| August 2, 2012 | 4 | 1.00" | LEXINGTON, RICHLAND |
| May 15, 2012 | 4 | 1.75" | CALHOUN, LEXINGTON |
| November 4, 2012 | 1 | 1.00" | LEXINGTON |
“Numerous reports of 1 inch hail on Roland Drive, Emmanual Church Road, Longs Pond Road near I-20, and Lexington Hills Subdivision.”
— NWS event narrative, July 1, 2012 (NCEI Storm Events)
When it fell
Feb 1 · Mar 6 · May 5 · Jun 1 · Jul 15 · Aug 4 · Nov 1
Wind context: the record also holds 65 thunderstorm-wind events ≥50 kt (≈58 mph, the NWS severe criterion) in this radius for 2012 — relevant where the dispute is wind vs hail causation.
Working a Columbia (SC) claim from 2012?
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 Columbia (SC) 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.