Turbulence triumphantly rar

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A turbulent flow can occur when the wind changes directions or a storm arrives at a locality. Stay informed: Sign up for our daily aviation news digest.

Mechanical Turbulence — where the terrain on the ground causes the wind to pool and form vertical eddies. A good example of this would be where the mountains meet the plains or oceans. The flat wind reaches the mountain range and has nowhere to go but up, hitting air traffic and changing direction as it cools.

The worse case is hot desert wind or the tropics hitting big mountains. Interestingly, human cities have started to get big enough for eddies to form over skyscrapers and other dense urban areas. Thermal Turbulence — Heat has a huge impact on turbulence.

When the sun heats the air, it starts to rise and cool. The hot air updrafts form pillars of turbulence that can affect aircraft coming to land and eventually form thunderstorms. However, this type of turbulence is rarely found above the cloud layer. If an aircraft is flying over a region, then it is generally unaffected. The eddies are formed laterally over the dome and can be very unstable. Once a plane traverses this barrier, then they are generally secure.

If there is a thunderstorm in this environment, then the turbulence may be extreme. Wind Shear Turbulence — The last type of turbulence is when the wind changes in the aircraft path.