Enid hail storm history
Garfield County·NOAA NCEI Storm Events Database·~75-day publication lag
Enid, located in Garfield County in the Oklahoma Panhandle, sits at the convergence of Tornado Alley's most active severe weather corridor. The dryline, jet stream, and Gulf moisture interact over this region to produce intense supercell thunderstorms capable of generating large hail. Garfield County has a documented history of significant hail events in the National Weather Service record.
Check if your roof was damaged by recent hail
Hail season in Enid peaks from April through June, with May historically producing the most damaging large-hail events in Garfield County. Secondary activity occurs in March and July. These storms develop when warm, moist Gulf air collides with cold, dry air from the high plains, creating the atmospheric instability required for supercell development and severe hail.
Annual frequency — last 10 years
When hail hits — monthly pattern
Avg events per month · all years · NOAA data
All recorded hail events
Of 162 recorded events, 62 (38%) reached 1.5" or larger — the threshold for likely functional damage on standard asphalt shingles.
The location is approximate.
The report was relayed through mPING.
The location is approximate.
A social media image was relayed by broadcast media. The location is approximate.
The report was relayed by emergency management. The location is approximate.
The location is approximate.
The report was relayed through mPING.
The report was relayed through mPING.
An image was relayed by emergency management.
The report was relayed through mPING. Event time adjusted based on radar observations.
The report was relayed through mPING.
The report was relayed through mPING.
Emergency management relayed an image. Event time is estimated from radar observations.
Hail size increased from golf ball to near tennis ball between 1650-1655 LST. Report relayed by emer…
MPing report.
Report of golf ball size hail from two miles west towards the center of the community of Carrier. Re…
MPing report. Time adjusted from radar and additional nearby reports.
Image relayed through broadcast media. Time is radar estimated.
Relayed image.
Based on radar evidence, hailfall likely occurred prior (1640-1645 LST) to report time.
Size is estimated from a live video feed.
MPing report.
Time estimate from radar.
Time estimated from radar.
Report from Mping.
From the Vance Airforce base weather observer via the KEND METAR.
Time estimate from radar.
Time based on radar data.
Hail damage reported to roofs and cars. Time estimated by radar.
NOAA National Centers for Environmental Information Storm Events Database. Publication lag is approximately 75 days — current-year events may be incomplete.
NOAA Storm Events Database ↗