The side of a mountain range that initially receives the precipitation is caused, or increased by a process called orthographic precipitation.
After the system, or pocket of air moves over the range, much of the moisture has been drained from the weather system or pocket of air.
The back side of a mountain range is called the rain shadow. Because much of the moisture has been drained from the air, it often creates a desert. The Gobi Desert is created by the Himalayn Range, and the Mojave Desert is created by the San Bernardino and San Gaberial mountains.
These deserts are called Rain Shadow Deserts.
A rain-shadow.
Because the atmosphere gets denser as elevation increases.
One side of a mountain range will have significantly less precipitation than the other side due to the height of the mountain. The clouds that carry the water for precipitation, may be blocked by the tall mountains.
eastern side receives less precipitation
rain shadow
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The coastal plain is most likely to have the least precipitation as it is located farthest from the ocean where most of the moisture comes from. The leeward side of a mountain typically receives less precipitation as it is in the rain shadow of the mountain.
A rain-shadow.
Because the atmosphere gets denser as elevation increases.
One side of a mountain range will have significantly less precipitation than the other side due to the height of the mountain. The clouds that carry the water for precipitation, may be blocked by the tall mountains.
eastern side receives less precipitation
does the leeward side of a mountain receive precipitation
west side of the mountain
rain shadow
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does the leeward side of a mountain receive precipitation
One example of a location that is dry due to the rain shadow effect is Death Valley in California, USA. The Sierra Nevada mountain range blocks moisture-laden air from reaching the valley, resulting in very dry conditions and minimal rainfall.