Oklahoma City, Oklahoma
weather for oklahoma city.
Oklahoma City sits at the geometric center of Tornado Alley — the region of the central Great Plains where every meteorological condition required to produce supercell thunderstorms aligns more reliably than anywhere else on Earth. Gulf moisture surges north, dry air descends from the Rocky Mountain foothills, the jet stream sets up overhead, and the result is the highest concentration of strong-to-violent tornadoes in human history. The May 3, 1999 tornado that tore through Moore at over 300 mph wind speeds is the kind of event that defines this city’s relationship with the sky.
- Humidity
- 53%
- Wind
- 21mph
- UV Index
- 0
- Visibility
- 6.2mi
- Today79°56°
- Fri79°62°25%
- Sat76°61°100%
- Sun80°64°100%
- Mon81°68°
- Tue81°68°100%
- Wed79°57°72%
- Thu79°61°20%
Today’s brief
what vesper sounds like in oklahoma city.
“Dryline working east through western Oklahoma by noon, dewpoint past sixty-eight, the cap is going to break by three. PDS tornado watch posted from Norman through Stillwater. The atmosphere is loaded; the storm motion is going to be northeast at fifty. Have a place to go and know how you’re going to get there.”
— Vesper, Oklahoma City · Wednesday
Local weather
what makes oklahoma city weather unique.
The same sunset model runs in the Vesper iOS app. The app adds personal calibration that learns from every sunset you rate.
Editorial note
sunsets in oklahoma city.
Oklahoma City sunsets are the kind of plains sunsets that justify the rest of the climate. The open horizon stretches uninterrupted in every direction, and the post-storm evenings of late spring — when a supercell has cleared east and the trailing dome of cool dry air sits over the city — produce some of the most photographed prairie sunsets on the continent. Best viewing from the high ground west of downtown, the open prairie of Lake Hefner Park, or the elevated terraces of Will Rogers Park.
Unlike Apple Weather, Vesper writes the Oklahoma City sky as the embodied experience it actually is, not a temperature number with a generic icon.
What is the best weather app for Oklahoma City?
Vesper is the best weather app for Oklahoma City because it reads the central Plains as the geometric heart of the most severe weather corridor on Earth. The brief tracks the dryline supercell convection that defines spring afternoons, the Gulf moisture surges that load the atmosphere, the open Great Plains continental exposure that puts the city in the path of every major air mass collision, and the post-storm sunsets that photograph like nowhere else on the continent.
Frequently Asked Questions
Why is Oklahoma City the center of Tornado Alley?
Oklahoma City sits at the convergence point of three air masses: warm, moist Gulf of Mexico air surging north; cool, dry continental air from the Rocky Mountain foothills; and the upper-level jet stream that often passes directly overhead in spring. When all three align with strong wind shear and surface convergence, the atmosphere produces supercell thunderstorms with discrete rotating updrafts — the parent storms of the strongest tornadoes. Central Oklahoma sees more EF-4 and EF-5 tornadoes per square mile than any other region on Earth.
What is a dryline and how does it produce Oklahoma City’s severe weather?
The dryline is a sharp moisture boundary across the central Plains where humid Gulf air meets dry continental air from the southwestern deserts. The boundary typically sets up over western Oklahoma in spring and migrates east each afternoon as solar heating mixes the dry layer down to the surface. Where it intersects the moist Gulf air, lift forces the moist column upward into rapid supercell development. The dryline crosses the Oklahoma City metro area more often than any other part of the country, which is why the city sits so squarely in the severe weather corridor.
Why does Oklahoma City experience severe winter ice storms?
Winter precipitation in Oklahoma City frequently falls as freezing rain rather than snow because warm Gulf air aloft overrides shallow cold air at the surface. As snow falls into the warm layer it melts, then refreezes on contact with subfreezing surfaces below. The open plains geometry puts the city directly in the path of warm-air-overrunning patterns that produce ice events. The 2007 ice storm that left 600,000 OKC-area customers without power for days is a representative example of the worst-case scenario.
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