A Lee wave, also known as a mountain wave, is a type of gravity wave that occurs in the atmosphere when stable air flows over a mountain range or a hill. When the airflow is disrupted by the terrain, it creates oscillations in the atmosphere on the leeward side (downwind) of the obstacle. The key features of Lee waves include: 1. **Formation**: When stable air encounters a mountain, it is forced upward, leading to an increase in altitude.
New to topics? Read the docs here!