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The eastern side lies in a rain shadow getting much less rain than the western side. It is found in areas of rain shadow in the tropical marine climate.
rain shadow effect. the low-rainfall region that exists on the leeward (downwind) side of a mountain range; the result of the mountain range's causing precipitation on the windward side. windward side. the side of the mountain that is cool and moist, has lots of vegetation.
\ud835\uddea\ud835\uddf5\ud835\uddee\ud835\ude01 \ud835\uddf6\ud835\ude00 \ud835\ude01\ud835\uddf5\ud835\uddf2 \ud835\uddff\ud835\uddee\ud835\uddf6\ud835\uddfb \ud835\ude00\ud835\uddf5\ud835\uddee\ud835\uddf1\ud835\uddfc\ud835\ude04 \ud835\uddf2\ud835\uddf3\ud835\uddf3\ud835\uddf2\ud835\uddf0\ud835\ude01? An area having relatively little precipitation due to the effect of a topographic barrier, especially a mountain range, that causes the prevailing winds to lose their moisture on the windward side, causing the leeward side to be dry.
A rain shadow area is an area of dry land that lies on the leeward(or downwind) side of a mountain. High mountains act as barriers for cold or hot winds; they may also cause precipitation if they are high enough and lie in the path of rain-bearing winds. The leeward side of the mountains remains dry.
A rain shadow is a patch of land that has been forced to become a desert because mountain ranges blocked all plant-growing, rainy weather. On one side of the mountain, wet weather systems drop rain and snow. On the other side of the mountain\u2014the rain shadow side\u2014all that precipitation is blocked.
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Glossary Term. Rain shadow effect. The region on the lee (sheltered) side of a mountain or mountain range where the precipitation is noticeably less than on the windward side, because the moisture-bearing air mass loses most of its moisture on the windward side before reaching the lee side.
As moist air moves over land and encounters mountains it rises, expands, and cools because of the declining pressure and temperature.
Rain shadow deserts are created when mountain ranges lie parallel to moist, coastal areas. Prevailing winds moving inland cool as air is forced to rise over the mountains. Carried moisture falls on slopes facing the winds. When the winds move over the crest and down the far side, they are very dry.
One such example of a rain shadow region is Death valley. Rainshadow areas: Northern Karnataka, Osmanabad, Beed(Maharashtra), Solapur, Gilgit and Chitral, the Vidarbha plateau, and the eastern side of Kerala, Pakistan are all rainshadow areas.
A rain shadow area is an area of dry land that lies on the leeward(or downwind) side of a mountain. High mountains act as barriers for cold or hot winds; they may also cause precipitation if they are high enough and lie in the path of rain-bearing winds. The leeward side of the mountains remains dry.

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