What are the orographic clouds?

Orographic clouds form when moist air is forced to rise over mountains or elevated terrains. As the air ascends, it cools and condenses, leading to cloud formation typically on the windward side of the mountain. This process often results in increased precipitation in these regions, while the leeward side may experience drier conditions, a phenomenon known as the rain shadow effect. These clouds can vary in appearance, including stratus, cumulus, or even more complex formations depending on atmospheric conditions.