Salt Lake City to Atlanta Turbulence Forecast

SLC → ATL · 1,587 miles · ~3h 40m

What to Expect

The Salt Lake City to Atlanta flight, heading east over 1587 miles, crosses a diverse range of geographic features that influence turbulence. Initially, you'll encounter the Central Rockies and Front Range, where mountain wave turbulence can occur as air flows over the peaks. As you cross the Great Plains, be aware that clear-air turbulence (CAT) is common, caused by shifting air currents at high altitudes. Moving into Tornado Alley, severe convective turbulence is possible, especially during storm seasons. The Ozark Plateau, Mississippi Valley, and Southeast Interior may present convective turbulence as well, thanks to rising warm air. Finally, approach to Atlanta can involve mechanical turbulence near the Southern Appalachians, caused by wind interacting with the mountains. Pilots are well-versed in monitoring and navigating these conditions to ensure a safe flight.

Between Salt Lake City and Atlanta, the flight path crosses the Central Rockies of Colorado and Utah. This area is one of the most turbulence-prone zones in the U.S., with mountain wave activity reported on more than half of winter days. Waves can propagate far downstream, meaning turbulence may begin well before or after the visible peaks.

Turbulence Factors on This Route

• Mountain Wave Turbulence: The Central Rockies produce frequent, sometimes severe, mountain waves that can extend 100+ miles downstream.
• Clear-Air Turbulence (CAT): The jet stream frequently meanders over the Great Plains, producing wind shear and clear-air turbulence at cruising altitudes.
• Severe Convective Turbulence: Tornado Alley supercells produce some of the most intense convective turbulence in North American aviation.
• Mechanical Turbulence: The Southern Appalachians produce terrain-induced chop, especially during strong wind events and summer convection over the ridgeline.

When Is This Route Bumpiest?

For the smoothest possible flight, aim to travel this route in the late fall. Summer and early fall also tend to be relatively calm. Winter, early spring, spring, early summer, and summer can be bumpier due to mountain wave turbulence off the Rockies, and convective turbulence arising from storms in Tornado Alley and the Southeast. This is because temperature differences create unstable air, which leads to increased turbulence. Spring storms tend to be stronger and more frequent, making for a potentially less comfortable flight.

Tips for This Flight

If possible, booking a morning flight often provides a smoother ride as the atmosphere is typically more stable early in the day. Any turbulence you experience on this route might feel like driving over a series of potholes, or perhaps a bumpy country road, rather than anything dramatic. For added comfort, choose a seat over the wing, as this area tends to experience less motion, and stay well-hydrated to minimize any potential discomfort. Remember that the crew is trained to handle all conditions, and they are there to assist you in any way they can.

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Forecasts based on NOAA HRRR and GFS atmospheric model data.