Cleveland to Salt Lake City Turbulence Forecast

CLE → SLC · 1,561 miles · ~3h 37m

What to Expect

The Cleveland to Salt Lake City route, covering 1561 miles westward, presents a variety of potential turbulence factors, something pilots are prepared for. Departing Cleveland, you might encounter Lake-Effect Turbulence, common near the Great Lakes. As you cross the Ohio Valley, Frontal Turbulence can occur due to weather fronts. Over the Mississippi Valley, Convective Turbulence, caused by rising warm air, is possible, especially in warmer months. Progressing into the Upper Midwest and Great Plains, Clear-Air Turbulence (CAT) can arise even in seemingly clear skies. Finally, approaching Salt Lake City, Mountain Wave Turbulence near the Central Rockies is a consideration; this happens when air flows over the mountains, creating waves. Pilots constantly monitor and adjust to these conditions, ensuring a safe and, as much as possible, comfortable flight.

Between Cleveland and Salt Lake City, 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

• 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.
• Clear-Air Turbulence (CAT): The Upper Midwest sits beneath frequent polar jet stream intrusions, producing clear-air turbulence at cruising altitudes.
• Mountain Wave Turbulence: The Central Rockies produce frequent, sometimes severe, mountain waves that can extend 100+ miles downstream.

When Is This Route Bumpiest?

For the smoothest experience, aim to fly this route during the summer, early fall, or fall. During these seasons, the atmospheric conditions are generally more stable, reducing the likelihood of convective activity and strong frontal systems. Late fall, early winter, winter, spring, early summer, and early spring tend to be bumpier. Lake-Effect Turbulence from the Great Lakes can intensify in late fall and winter. Spring and early summer can bring increased Convective Turbulence over the Mississippi Valley. Mountain Wave Turbulence is a year-round possibility near the Rockies, but can be more pronounced during certain wind patterns prevalent in winter and spring.

Tips for This Flight

If you're anxious about turbulence, consider booking a morning flight; the air is often calmer earlier in the day, reducing the chance of convective turbulence. Any turbulence you might experience on this route often feels like driving on a bumpy road or a series of gentle jolts. Choosing a seat over the wing tends to offer a slightly more stable ride. Remember to stay hydrated and practice deep, slow breathing; focusing on your breath can help manage any anxiety, and remember that the pilots are highly skilled at navigating these conditions, prioritizing your safety and comfort.

Get Your Forecast

Related Routes

See all routes from Cleveland or to Salt Lake City.

More from Cleveland

More to Salt Lake City

Forecasts based on NOAA HRRR and GFS atmospheric model data.