Which type of precipitation results when warm, wet air is forced over mountains?

Orographic precipitation occurs when warm, moist air encounters a mountain range and is forced to rise. As the air ascends, it cools and condenses, leading to cloud formation and precipitation on the windward side of the mountains. This process is particularly significant because it can create lush, green landscapes on one side of the mountain while leaving the leeward side dry, often referred to as a rain shadow.

In contrast, convectional precipitation is a result of localized heating that causes warm air to rise, while frontal precipitation occurs when warm air meets cold air, leading to the rising of the warm air and subsequent cooling. Dorsal precipitation is not a recognized term in meteorology, further distinguishing orographic precipitation as the correct choice for this question.