What type of cloud is a "Lenticular Cloud"?

A Lenticular Cloud is a specific type of cloud that typically forms on the upwind side of mountains. This phenomenon occurs when stable air flows over a mountain range, resulting in lift as the air rises to cross the peak. As the air rises, it cools and condenses, leading to the formation of the cloud. The characteristic lens-shaped appearance of Lenticular Clouds is due to this airflow pattern, which stabilizes and creates distinct cloud formations at higher elevations.

Lenticular Clouds are often mistaken for UFOs because of their unique shape, but they serve as indicators of the airflow patterns in mountainous regions. While they may be associated with turbulent air, they primarily form due to the lifting mechanisms present in mountainous terrains. Understanding the formation of Lenticular Clouds is integral to flight planning and weather assessment for aviation purposes.