Foehn Effect

The Foehn Effect refers to a weather phenomenon that occurs when moist air rises over mountains, cools down, and loses moisture as precipitation on the windward side. When the now drier air descends on the leeward side, it warms up, often resulting in dry, warm conditions. This effect can significantly raise temperatures and lower humidity on the side of the mountain that is sheltered from the wind. It’s commonly observed in various mountain ranges around the world, creating distinct weather patterns and influencing local climates.