What characterizes a rain shadow?

A rain shadow is characterized by a dry climate on the far side of a mountain range due to the effects of orographic lift. When moist air approaches the mountain, it is forced to rise over the peak. As the air rises, it cools and condenses, resulting in precipitation on the windward side of the mountain. By the time the air descends on the leeward side, it has lost much of its moisture, creating a dry environment, commonly referred to as a rain shadow. This phenomenon highlights the relationship between topography and climate, illustrating how geographical features can significantly influence local weather patterns.