It refers to the blocking of rain on one side of a mountain range. The Sierra Nevada mountains, for example, receive a lot of rain on their western slopes off the Pacific Ocean, but the clouds do not travel across their peaks as well, so little rain falls in the big desert east of this range.
Just a few million years ago, when the range was much lower in elevation, there were big lakes in Nevada which are now arid playa.
A rain shadow.
The rain shadow occurs on the leeward side of the mountain, which is the side facing away from the prevailing winds. As the air rises and cools on the windward side, it releases most of its moisture as precipitation. By the time the air descends on the leeward side, it is drier, creating a rain shadow effect.
False. A rain shadow is the dry area on the leeward side of a mountain caused by the blocking of moisture-laden air by the mountain, leading to little or no precipitation. The side of the mountain with clouds and rain is the windward side.
Arid or dry deserts.
The Atlas Mountains in North Africa can create a rain shadow effect. As moist air moves from the Mediterranean Sea towards the mountains, it is forced to rise, cool, and release moisture on the windward side. This can result in dry conditions on the leeward side of the mountains, leading to a rain shadow effect.
Rain shadow
The rain shadow of the Himalayas makes the Tibetan Plateau comparatively dry. The high mountains blocked the clouds, creating a rain shadow for the valleys to the east.
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A rain shadow is a term commonly used to describe the area on the back side of a mountainous area. A rain shadow is caused by mountains being high enough to block the passage of rain-producing weather which casts a "shadow of dryness" behind them.
The rain shadow equals rain
The rain shadow equals rain
Death Valley is a rain shadow desert in the U.S. It is in the rain shadow effect of the Sierra Nevada mountain range.
The term nimbus refers to a rain cloud. The prefix "nimbus" tells you the cloud is raining, or capable of producing rain.
The area in a rainshadow receives less rain than a similar area not in a rain shadow.
A rain shadow.
The rain shadow effect refers to a dry area on the leeward side of a mountain caused by the blocking of moisture from prevailing winds. As air rises over the windward side, it cools, expands, and releases precipitation. This leaves little moisture for the leeward side, resulting in a rain shadow desert.
easy, the rain shadow effects mountains