Norfolk to Salt Lake City Turbulence Forecast

ORF → SLC · 1,931 miles · ~4h 22m

What to Expect

Your flight from Norfolk (ORF) to Salt Lake City (SLC) crosses a wide variety of terrains, each presenting its own type of turbulence. Initially, as you leave the Atlantic Seaboard, expect the possibility of clear-air turbulence, or CAT, which can occur even in seemingly clear skies. As you move inland, the flight will cross the Southern Appalachians, where mechanical turbulence, caused by wind interacting with the mountains, can be present. Further along, over the Ohio and Mississippi Valleys, you might encounter frontal or convective turbulence, especially if there are weather systems active. The Great Plains can also bring clear-air turbulence. Finally, approaching Salt Lake City, you'll cross the Front Range and Central Rockies, where mountain wave turbulence is common. Remember, pilots are highly trained to anticipate and navigate these conditions every day.

Flights between Norfolk and Salt Lake City pass along the Front Range, where the abrupt rise of the Colorado Rockies generates some of the strongest mountain wave turbulence in the continental U.S. Downdrafts east of the ridgeline can be intense, and rotor turbulence near the surface sometimes extends to cruising altitude during high-wind events.

Turbulence Factors on This Route

• Clear-Air Turbulence (CAT): The Atlantic coast jet stream and land-sea temperature contrasts create frequent clear-air turbulence at cruising altitude.
• Mechanical Turbulence: The Southern Appalachians produce terrain-induced chop, especially during strong wind events and summer convection over the ridgeline.
• Frontal Turbulence: The Ohio Valley is a preferred storm track where frontal boundaries and embedded convection create turbulence year-round.
• Convective Turbulence: The Mississippi Valley is a breeding ground for squall lines and mesoscale convective systems that produce widespread turbulence.

When Is This Route Bumpiest?

The smoothest flights on this route tend to be in summer, early fall, and fall, as weather patterns are typically more stable. Winter, early spring, spring, and early summer can be bumpier. Winter brings stronger jet streams, increasing the likelihood of clear-air turbulence over the Atlantic Seaboard and Great Plains. Spring and early summer can see increased convective activity over the Mississippi Valley, leading to more turbulence from thunderstorms. Mountain wave turbulence near the Rockies is possible year-round, but can be more pronounced during periods of strong winds aloft.

Tips for This Flight

Choosing a morning flight can often lead to a smoother experience, as the atmosphere tends to be more stable earlier in the day. Any turbulence you do encounter on this route is most likely to feel like driving on a bumpy, unpaved road for a few minutes at a time. For added comfort, choose a seat over the wing, which is closest to the plane's center of gravity and experiences less motion. Remember to stay hydrated, and know that the flight crew is there to ensure your safety and comfort.

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Forecasts based on NOAA HRRR and GFS atmospheric model data.