The leeward side of a mountain range is often warmer and drier than the windward side.

Question

Quizplus · Accepted Answer

The prevailing winds carry moist air towards the windward side of the mountain range, causing the air to rise and cool, resulting in precipitation. By the time the air reaches the leeward side, it has lost much of its moisture and has become warmer and drier due to the descending air motion. This is known as the rain shadow effect. Therefore, the leeward side of a mountain range is often warmer and drier than the windward side.

The Leeward Side of a Mountain Range Is Often Warmer