Salt Lake City to Cleveland Turbulence Forecast

SLC → CLE · 1,561 miles · ~3h 37m

What to Expect

The Salt Lake City to Cleveland route, heading east, is interesting because it crosses so many different geographical areas, each potentially contributing to turbulence. Initially, you'll be flying over the Central Rockies, where mountain wave turbulence is common, caused by wind flowing over the mountains. As you continue east, the flight path takes you over the Great Plains and the Upper Midwest, regions known for clear-air turbulence (CAT), which can occur even in seemingly clear skies. Then, you'll cross the Great Lakes, where lake-effect turbulence can happen, particularly if there's cold air moving over the warmer lake waters. Further along, the Mississippi Valley can experience convective turbulence, created by rising warm air. Finally, as you approach Cleveland over the Ohio Valley, frontal turbulence is possible due to weather fronts colliding. Pilots are very familiar with these patterns and use weather forecasting to plan routes that minimize discomfort.

Between Salt Lake City and Cleveland, 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.
• Lake-Effect Turbulence: The Great Lakes produce lake-effect convection and low-level wind shear from land-water temperature contrasts.
• Frontal Turbulence: The Ohio Valley is a preferred storm track where frontal boundaries and embedded convection create turbulence year-round.

When Is This Route Bumpiest?

The summer and early fall months generally offer the smoothest flights along this route. Stable atmospheric conditions mean less turbulence over the Rockies, plains, and lakes. Winter, early spring, late fall, early winter, spring, and early summer can be more turbulent. In the colder months, mountain wave turbulence is more pronounced over the Rockies, and lake-effect turbulence becomes more common over the Great Lakes. Spring and early summer can bring increased convective activity over the Mississippi Valley and frontal systems over the Ohio Valley, all of which can contribute to bumpier flights.

Tips for This Flight

If possible, booking a morning flight is often your best bet for a smoother ride because the atmosphere tends to be more stable earlier in the day. Any turbulence you might experience on this route will likely feel like driving over a bumpy road for a few minutes at a time; it's usually more of a nuisance than anything else. For extra comfort, choose a seat over the wing, which tends to experience less motion, and remember to stay hydrated to help manage any anxiety. You've got this.

Get Your Forecast

Related Routes

See all routes from Salt Lake City or to Cleveland.

More from Salt Lake City

More to Cleveland

Forecasts based on NOAA HRRR and GFS atmospheric model data.