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Rain shadow - Wikipedia A rain shadow is an area of significantly reduced rainfall behind a mountainous region, on the side facing away from prevailing winds, known as its leeward side Evaporated moisture from bodies of water (such as oceans and large lakes) is carried by the prevailing onshore breezes towards the drier and hotter inland areas
Rain Shadow - Education On one side of the mountain, wet weather systems drop rain and snow On the other side of the mountain—the rain shadow side—all that precipitation is blocked In a rain shadow, it’s warm and dry On the other side of the mountain, it’s wet and cool Why is there a difference?
What Is a Rain Shadow? - Treehugger Rain shadows form when air moves from west to east across mountain ranges, which act as barriers to the flow of air When winds blow against a mountain, they have nowhere to go except be forced to
Explained: What is a Rain Shadow, and Why is it important? - Ground Report It's because of something called a "rain shadow " This happens when big mountains block rain clouds, and it can change the weather, ecosystems, and even how people live in those areas A rain shadow is always present on the opposite side just as a shadow is
What Causes A Rain Shadow? - Sciencing Rain shadows, or dry regions on the protected side of some mountain ranges, can be some of the driest places on Earth; the Atacama desert in the rain shadow of the Andes Mountains can go decades without receiving any rainfall
What Is A Rain Shadow Effect? - TRVST What Is A Rain Shadow Effect? The rain shadow effect is a weather phenomenon that occurs near mountain ranges Wet weather systems prevail on one side of a mountain, and it enjoys much rainfall and even snow, but the other side gets little or no precipitation and becomes a desert
Rain shadow | meteorology | Britannica Rain shadow, lee side of an orographic (mountainous) barrier, which receives considerably less precipitation than the windward side See orographic
All About the Rain Shadow Effect – Decoding Biosphere What is the Rain Shadow Effect? The rain shadow effect occurs when moist air rises over a mountain range, cools, and loses its moisture as precipitation (rain, snow, or other forms of water) As the air descends on the other side of the mountain, it warms up and dries out, creating a dry area known as a “rain shadow ”
rain shadow - Glossary of Meteorology Slopes facing windward with respect to prevailing or seasonal moisture-bearing flows typically experience heavy orographic precipitation To the lee of the barrier, however, the sinking air warms, dries, and becomes more stable, suppressing precipitation