Maui to Savannah Turbulence Forecast

OGG → SAV · 4,626 miles · ~9h 45m

What to Expect

Flying from Maui (OGG) to Savannah (SAV) means traversing 4626 miles northeast across a wide range of geographic features, each with its own potential for turbulence. Initially, you'll be over the open Pacific, which can bring oceanic clear-air turbulence and convection, where air masses of different temperatures meet. As you approach the mainland, expect possible thermal turbulence over the Mojave and Sonoran Deserts, caused by rising warm air. The Southern Rockies could present mountain wave turbulence, as wind flows over the peaks. Further along, Tornado Alley and the Mississippi Valley are known for severe convective turbulence and convective turbulence, respectively, arising from unstable air and thunderstorms. Finally, the Southeast Interior may have convective turbulence. Remember, pilots are trained to navigate these conditions; these are typical weather patterns for this route.

The Maui to Savannah 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

• Oceanic Clear-Air Turbulence: Transoceanic jet stream crossings produce extended stretches of clear-air turbulence over the open Pacific.
• Oceanic Convection: Isolated thunderstorms over warm Pacific waters can develop away from radar coverage, catching flights off guard.
• 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.

When Is This Route Bumpiest?

Spring and early summer tend to offer the smoothest rides on this Maui to Savannah route, with calmer air masses over the deserts and less convective activity in Tornado Alley and the Southeast Interior. Winter, late summer, summer, late winter, spring, and early summer are generally bumpier. Winter can bring stronger jet streams contributing to clear-air turbulence over the Pacific. Late summer and summer sees increased convective activity, with more thunderstorms brewing over Tornado Alley and the Southeast Interior, while the deserts heat up and cause thermal turbulence.

Tips for This Flight

For the calmest flight, consider booking a morning departure, as daytime heating increases thermal and convective turbulence. Any turbulence you experience is likely to feel like driving over a bumpy road or encountering strong wind gusts while sailing. To enhance your comfort, choose a seat over the wing; this area experiences less motion. Staying hydrated can also help you feel more relaxed; remember that the crew are there to support you and ensure a safe flight, so don't hesitate to ask any questions or express any concerns.

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Forecasts based on NOAA HRRR and GFS atmospheric model data.