MTSU Aerospace Practice Test

Turbulence is driven by how the air moves vertically and how the wind changes with height. When the atmosphere is unstable, parcels of air tend to rise and mix with the air around them. That vertical motion creates irregular, swirling air—turbulence. Wind shear adds another source: if different layers of air move at different speeds or directions, those layers slide past each other and form eddies, which also shake the flow and produce turbulence.

So turbulence tends to be higher when there is strong vertical air movement or significant wind shear. It’s not limited to the ground; turbulence can occur anywhere in the atmosphere where vertical motions or wind shear exist. And the idea that wind doesn’t affect turbulence isn’t correct, because wind shear and changes in wind with height are major causes of turbulent air. Turbulence can even occur with light surface winds if the atmosphere is very unstable (strong convection).