Severe turbulence is the level where aircraft briefly lose control, passengers feel strong upward and downward forces, and walking is impossible. Here's everything you need to know — which routes get it, when it's worst, and how to prepare.
Severe turbulence (EDR 0.4–0.7 m²/³s⁻¹) is caused by three main phenomena: (1) Jet stream wind shear — violent boundary between fast-moving jet stream air and calmer air below creates severe CAT with no visual warning, (2) Mountain wave turbulence — extreme waves extending to cruise altitude downwind of mountain ranges like the Andes, Rockies, and Alps, (3) Convective turbulence — cumulonimbus storm cells generating extreme up- and downdrafts. The first two are most relevant to commercial flights; pilots route around thunderstorms when possible.
Northern Hemisphere winter (December–March): jet stream is at its strongest (150–200 mph), producing the most severe CAT over the Atlantic and Pacific. Spring (March–May): transition season with strong frontal systems. Southern Hemisphere winter (June–August): severe Andes crossing turbulence peaks. Typhoon season (June–November) brings severe convective turbulence in the western Pacific. Summer over the North Atlantic is generally the calmest.
Ranked by historical turbulence score — click any route for details