Los Angeles to Wichita Turbulence Forecast

LAX → ICT · 1,200 miles · ~2h 54m

What to Expect

The Los Angeles to Wichita route, heading east for about 1200 miles, crosses some interesting geography that can contribute to turbulence. Right after takeoff, you'll be flying over the Mojave and Sonoran Deserts, where warm air rising off the hot ground can cause what's called thermal turbulence, a bit like driving over small speed bumps. Next, the flight path crosses the Southern Rockies, which can generate mountain wave turbulence as air flows over the peaks; pilots are very familiar with this. Further along, over the Great Plains, you might encounter clear-air turbulence (CAT), which can happen even in seemingly clear skies. Finally, you'll be entering Tornado Alley where severe convective turbulence from storm clouds is possible. Pilots are skilled at using onboard radar and reports from other aircraft to avoid the worst of it, always prioritizing a smooth, safe flight.

The Los Angeles to Wichita 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

• Thermal Turbulence: Extreme desert heating generates strong thermal updrafts that cause low-to-mid-level turbulence, especially in summer afternoons.
• 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.

When Is This Route Bumpiest?

The smoothest flights between Los Angeles and Wichita are generally in the fall and winter months. In winter, the air is typically more stable, leading to fewer thermal updrafts over the deserts. Summer, late winter, spring, early summer are often bumpier. The summer heat intensifies thermal turbulence over the deserts, while late winter, spring, and early spring bring increased chances of mountain wave activity over the Rockies and convective turbulence in the Great Plains, especially as Tornado Alley storms develop.

Tips for This Flight

If possible, booking a morning flight often provides a smoother ride since the ground hasn't had all day to heat up and cause thermal turbulence. Any bumps you do encounter will likely feel like going over a few potholes in a car, maybe a bit more pronounced at times, but generally manageable. For extra comfort, consider choosing a seat over the wing, which tends to experience less motion; staying well-hydrated can also help you feel more relaxed. Remember, the pilots are highly trained to navigate these conditions and ensure a safe, comfortable flight.

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Forecasts based on NOAA HRRR and GFS atmospheric model data.