Weather Evidence

Storm Reports · Oklahoma

Norman, OK hail storm history

Every day with large hail, damaging wind or a tornado within 10 miles of central Norman since 2021, with each storm's reports on a map. The largest hail was 3.00 inches (teacup size) on May 25, 2025.

Norman since 2021 · within 10 mi of the center

Storm days
58all types
Hail days
281 in or larger
Largest hail
3.00 inMay 25, 2025
Tornado days
8any rating

Storm near Norman

Saturday, May 24, 2025

Largest hail
1.25 inhalf dollar
Strongest wind
—no reading
Tornadoes
0none reported
Reports
3within 10 mi
Hail10 miles from central Norman

3 reports

  • 1.25 in hail (half dollar)3.7 mi W of central Norman2.7 mi SW of (Oun)Norman Westheimer Arpt · Cleveland County · Public
  • 0.75 in hail (penny)3.8 mi SSE of central Norman2.9 mi NW of Noble · Cleveland County · Public

    The report was relayed through mPING.

  • 1.00 in hail (quarter)2.0 mi N of central Norman1.3 mi E of (Oun)Norman Westheimer Arpt · Cleveland County · Public

Also hit that day: Oklahoma City, OK, Moore, OK

What the National Weather Service wrote

The approximately 36-hour period, beginning during the initial hours of the 24th, featured three unique severe convective episodes across the WFO Norman Forecast Area. The initial round, triggered by moist isentropic ascent, featured scattered organized thunderstorms, including a few supercell thunderstorms. This activity produced primarily reports of large hail. However, localized storm-scale interactions across Cleveland, Pottawatomie, and Pontotoc Counties resulted in concentrated corridor of thunderstorm wind damage, as well as a tornado near Vanoss, OK, in Pontotoc County. During the same general time frame, a separate organized line of thunderstorms moved from far southern Kansas into north-central Oklahoma producing a few observed severe-caliber wind gusts.

Read the full description

Following the morning activity, dry and pleasant conditions occurred for much of the day on the 24th. However, by near-sunset, a destabilizing boundary layer near and south of a warm front across western and southern Oklahoma fostered the development of a few briefly intense thunderstorms. Finally, a progressive and high-intensity wake low and heat burst event evolved from portions of western-north Texas into central Oklahoma during the late evening of the 24th into the 25th. This event, tied to decaying severe convection from across central Texas, featured strong and occasionally damaging wind gusts.

Nearby cities

Sources: NCEI Storm Events Database (reviewed) and NWS Local Storm Reports (archived by the Iowa Environmental Mesonet) (preliminary). Weather Evidence is independent and not affiliated with NOAA or the National Weather Service. Storm reports show what was reported at a place and time; they do not establish conditions at any one property.