Areas near mountains on the side away from the wind, known as the leeward side, typically experience a drier climate compared to the windward side. This phenomenon, called rain shadow effect, occurs because moist air rises over the mountain, cools, and loses moisture as precipitation. As the air descends on the leeward side, it becomes warmer and drier, leading to reduced vegetation and arid conditions. Consequently, these regions often have lower humidity and less rainfall.
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