Moisture-laden air is rich with water vapor, and its journey around mountain ranges plays a crucial role in the distribution of rain and snow.
Let’s see how it works:
- The source of this air is usually from large bodies of water, like oceans, where the sun's heat causes evaporation.
- As this moist air travels inland, it encounters mountain ranges, which act as barriers.
- When forced to rise over the mountains, the air cools and loses its moisture, typically raining down on the windward side.
This cycle is fundamental in shaping local weather patterns and water availability, which can influence agriculture, drinking water supply, and natural habitats.