It is called a rain shadow, and is true. It can be wetter on the prevailing windward side and drier on the lee side of a mountain range.
a rain shadow is an area of a land that is on the leeward side of a mountain which does not receive enough amount of precipitation. IDK HOW IT AFFECTS INTERIOR REGIONS!!
The Himalayas stretches 1491 miles making it the longest mountain range in Asia.
In this type of land formation, a range is a group of mountains, a chain is a group of mountain ranges, and a belt is a group of mountain ranges and systems.
The term is Rain Shadow.
The leeward side of a dune is shorter and called the slip face. Dunes often serve an important purpose in protecting land from storm waves.
A rain shadow or rainshadow, or more accurately, precipitation shadow, is a dry region of land that is leeward of a mountain range or other geographic feature, with respect to prevailing wind direction. The mountains block the passage of rain-producing weather systems, casting a "shadow" of dryness behind them.
a rain shadow is an area of a land that is on the leeward side of a mountain which does not receive enough amount of precipitation. IDK HOW IT AFFECTS INTERIOR REGIONS!!
Death Valley is a rain shadow desert in the U.S. It is in the rain shadow effect of the Sierra Nevada mountain range.
Many deserts are the result of mountain ranges blocking the flow of moisture from an ocean. The moist air is forced upward on the leeward side where the water in the air condenses and falls as rain or snow. The air, now dry, passes to the leeward side of the mountain range and a rain shadow desert forms. See the image above.
Mountains can affect the climate of nearby lands. Clouds approaching a mountain are forced to rise, and rising clouds can't hold so much water, so they drop their rain, so the windward side of a mountain range may be rainy and the leeward side may be a desert.Much of airborne moisture falls as rain on the windward side of mountains. This often means that the land on the other side of the mountain (the leeward side) gets far less rain - an effect called a "rain shadow" - which often produces a desert.The higher the mountain, the more pronounced the rain shadow effect is and the less likely rain will fall on the leeward side.(The Windward is the side of a mountain that is facing into the direction that the wind is coming from.The Leeward side is the wind protected side of a mountain.)
On the windward side of a mountain range, air rises, cools, and drops its moisture. On the leeward side of a mountain range air descends, heats up, and dries the land. Deserts are common behind mountains. (493) Glencoe Texas Science, Grade 8 © 2002
The longest mountain range on land is the Andes. It stretches over 7,000 kilometers along the western coast of South America, passing through seven countries.
A rainshadow desert is an area of land that doesn't get a lot of rain due to tall mountain ranges. Therefore, the mountain is causing little rain to fall on the side of the mountain, which causes there to be a shadow behind the mountains. HA!!!
Caucasus mountain range.
The Trans-antarctic Mountain Ranges
Asgard Range
The mountain range that spreads from Victoria Land to Rockefeller Plateau is the Transantarctic Mountains. It is one of the longest mountain ranges in the world, stretching for about 3,500 kilometers across Antarctica, separating East Antarctica from West Antarctica.