Raleigh-Durham to Burbank Turbulence Forecast

RDU → BUR · 2,226 miles · ~4h 57m

What to Expect

The Raleigh-Durham to Burbank route, heading west, presents a variety of turbulence possibilities given the diverse geography it crosses. Immediately after takeoff, you might encounter mechanical turbulence over the Southern Appalachians, caused by wind interacting with the mountains. As you progress westward, the flight path takes you over the Ohio and Mississippi Valleys, where frontal and convective turbulence, respectively, are common; these are weather-related disturbances. Further along, the Ozark Plateau and Tornado Alley might present convective turbulence, sometimes severe. Over the Great Plains, clear-air turbulence (CAT) is possible, often unexpected but usually short-lived. Finally, nearing Burbank, the Southern Rockies can generate mountain wave turbulence, and the Mojave and Sonoran Deserts might have thermal turbulence. Pilots are very familiar with these patterns and actively monitor and adjust course to minimize discomfort, using onboard radar and reports from other aircraft.

The Raleigh-Durham to Burbank 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

• Mechanical Turbulence: The Southern Appalachians produce terrain-induced chop, especially during strong wind events and summer convection over the ridgeline.
• Frontal Turbulence: The Ohio Valley is a preferred storm track where frontal boundaries and embedded convection create turbulence year-round.
• Convective Turbulence: The Mississippi Valley is a breeding ground for squall lines and mesoscale convective systems that produce widespread turbulence.
• Clear-Air Turbulence (CAT): The jet stream frequently meanders over the Great Plains, producing wind shear and clear-air turbulence at cruising altitudes.

When Is This Route Bumpiest?

For the smoothest possible ride on this route, aim to fly in the fall. Spring and summer can also be relatively calm. Winter, though, tends to be the bumpiest time, as storm systems are more frequent and intense, increasing frontal turbulence over the Ohio Valley. Early spring, early summer, and late winter can also see increased convective activity over the Mississippi Valley, the Ozark Plateau, and Tornado Alley, leading to more turbulence. Mountain wave turbulence near the Rockies is also more common when strong winds are present during the winter and spring months.

Tips for This Flight

If you're concerned about turbulence, consider booking a morning flight, as atmospheric conditions are often more stable earlier in the day; this can help minimize convective turbulence. Any bumps you experience will likely feel like driving on a road with potholes or hitting a few unexpected speed bumps, perfectly manageable. To stay comfortable, choose a seat over the wing; it tends to be the most stable part of the aircraft. Remember to stay hydrated and focus on slow, deep breaths, knowing that the pilots are expertly handling the flight and any weather conditions that arise.

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Forecasts based on NOAA HRRR and GFS atmospheric model data.