Albuquerque to Chicago Midway Turbulence Forecast

ABQ → MDW · 1,119 miles · ~2h 44m

What to Expect

The Albuquerque to Chicago Midway route, stretching 1119 miles northeast, certainly crosses a variety of terrains known for turbulence. Immediately after takeoff, you might encounter Mountain Wave Turbulence as you fly over the Southern Rockies. As you cross the Great Plains, Clear-Air Turbulence (CAT) can sometimes occur, a phenomenon caused by shifting air currents at high altitudes. Further along, you'll be traversing Tornado Alley and the Mississippi Valley, where Severe Convective Turbulence and Convective Turbulence are possibilities, especially if there are thunderstorms. Near the end of your journey over the Great Lakes, Lake-Effect Turbulence can crop up from the lake-generated weather systems, and finally, Frontal Turbulence in the Ohio Valley from weather fronts. These are common atmospheric disturbances, and pilots are highly trained to navigate them safely, using weather forecasts and onboard radar to choose the smoothest possible path.

The Albuquerque to Chicago Midway route passes over the Southern Rockies in New Mexico and southern Colorado. While somewhat lower than the peaks to the north, these mountains still produce notable mountain wave turbulence, particularly when strong southwesterly winds aloft align perpendicular to the ridgeline.

Turbulence Factors on This Route

• Mountain Wave Turbulence: The Southern Rockies produce lee waves when southwesterly upper-level winds flow across the terrain.
• 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.
• 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?

For the smoothest possible flight, aim for summer or fall. During these seasons, the atmospheric conditions over the Great Plains and Tornado Alley tend to be more stable, reducing the likelihood of strong convective activity. Winter and early spring tend to be bumpier because of the stronger jet stream aloft, which stirs up Clear-Air Turbulence (CAT) over the plains and enhances mountain waves near the Rockies. Late winter, spring, early summer, late fall, and early winter can also experience more turbulence due to increased frontal activity and the potential for severe weather systems crossing the Mississippi Valley and Ohio Valley.

Tips for This Flight

Consider booking a morning flight; the atmosphere tends to be more stable earlier in the day, potentially leading to a smoother ride. Any turbulence you do experience on this route is likely to feel like driving over a bumpy road for a few minutes, not unlike hitting potholes. For added comfort, choose a seat over the wing; it's generally the most stable part of the aircraft. Stay hydrated and practice deep, steady breathing to help manage any anxiety; remember, your pilots are skilled professionals prepared for all types of weather.

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Forecasts based on NOAA HRRR and GFS atmospheric model data.