What is characteristic of the windward side of a mountain?

The windward side of a mountain is characterized by cool and moist conditions due to the process of orographic lift. As moist air approaches the mountain, it is forced to rise. As the air rises, it expands and cools, leading to condensation of moisture and the formation of clouds and precipitation. This is why areas on the windward side typically experience higher humidity and more rainfall. The cooling effect of this uplift also contributes to lower temperatures compared to the leeward side, which can be drier and warmer as it experiences descending, warming air. This distinction in climate is a fundamental concept in understanding how terrain influences local weather patterns.