Pittsburgh to Salt Lake City Turbulence Forecast

PIT → SLC · 1,655 miles · ~3h 49m

What to Expect

Your flight from Pittsburgh to Salt Lake City crosses a diverse range of landscapes, each with its own potential for turbulence. The initial leg over the Ohio Valley may encounter frontal turbulence, where contrasting air masses meet. Crossing the Great Lakes, especially during cooler months, lake-effect turbulence can occur as cold air passes over warmer water. As you proceed over the Mississippi Valley, you might experience convective turbulence, caused by rising warm air, particularly in the warmer months. Further west, over the Great Plains, keep an eye out for clear-air turbulence (CAT), which is often found at higher altitudes and can be difficult to predict. Finally, approaching Salt Lake City, your plane will navigate the Central Rockies, where mountain wave turbulence can develop as air flows over the peaks. All these types are commonly dealt with by pilots every day, and they're well-versed in managing the flight for passenger comfort.

Between Pittsburgh 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

• Frontal Turbulence: The Ohio Valley is a preferred storm track where frontal boundaries and embedded convection create turbulence year-round.
• Lake-Effect Turbulence: The Great Lakes produce lake-effect convection and low-level wind shear from land-water temperature contrasts.
• Clear-Air Turbulence (CAT): The jet stream frequently meanders over the Great Plains, producing wind shear and 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 flight, aim for summer or early fall. During these months, the air tends to be more stable, reducing the likelihood of convective turbulence over the Mississippi Valley and lake-effect turbulence over the Great Lakes. Winter, spring, late fall, early winter, early spring, and early summer tend to be bumpier due to stronger frontal systems over the Ohio Valley and more pronounced mountain wave turbulence over the Central Rockies. Clear-air turbulence over the Great Plains can occur year-round but is often more frequent during periods of strong jet stream activity, which is more common outside of summer.

Tips for This Flight

Booking a morning flight often provides a smoother experience, as the atmosphere tends to be more stable earlier in the day, reducing the chance of convective turbulence over the Mississippi Valley. Any turbulence you might experience on this route is usually light to moderate; think of it like driving on a slightly bumpy road. To enhance your comfort, choose a seat over the wing for a more stable ride, stay well-hydrated, and practice deep, calming breaths. Remember, the pilots are highly skilled at navigating these conditions, and your safety and comfort are their top priorities.

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Forecasts based on NOAA HRRR and GFS atmospheric model data.