Palm Springs to Albany Turbulence Forecast

PSP → ALB · 2,369 miles · ~5h 14m

What to Expect

The Palm Springs to Albany route is a long one, taking you across a wide variety of terrain and weather patterns, so expect some variation in smoothness. Departing Palm Springs, you'll first cross the Mojave and Sonoran Deserts, where thermal turbulence, caused by rising warm air, is common. As you head northeast, you'll encounter the Southern, Central, and Front Range of the Rockies, all of which can create mountain wave turbulence as air flows over them. Further east, over the Great Plains, you might experience clear-air turbulence, or even, in Tornado Alley, severe convective turbulence. Approaching Albany, the flight path crosses the Great Lakes, Mississippi Valley, and Ohio Valley, where lake-effect, convective, and frontal turbulence respectively can all be factors. Finally, the plane will pass the Northern Appalachians, which can create mechanical turbulence, and the Atlantic Seaboard, which can cause clear-air turbulence.

The Palm Springs to Albany 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 early fall offers the calmest flights on this route. Winter and summer are generally smoother than other times of year, too. The bumpiest seasons are late winter, spring, early spring, early summer, late fall, and early winter. This is because those periods see more significant weather pattern transitions over the Great Plains and Tornado Alley, and more intense thermal activity over the deserts. Mountain wave turbulence is generally consistent, but severe convective turbulence is most common in the spring and summer.

Tips for This Flight

Booking a morning flight is your best bet for a smoother ride, as daytime heating hasn't yet fully kicked in to create bumps over the deserts. Any turbulence you do encounter on this route will likely feel like driving over a bumpy road or the sensation of quick, small dips. To help stay comfortable, choose a seat over the wing; this area tends to experience less motion. Remember to stay hydrated and breathe deeply; you'll be in Albany before you know it, with the pilots and crew capably navigating the skies.

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Forecasts based on NOAA HRRR and GFS atmospheric model data.