A rain shadow.
The leeward side of a mountain is called the "rain shadow" side. It is a dry area that receives significantly less precipitation than the windward side of the mountain due to the barrier effect the mountain has on air masses.
The area of the mountain that receives high rainfall is called the windward side. This side of the mountain is typically lush and green due to the moist air being forced to rise and cool, leading to precipitation.
desert area because they can only had drought
A group of mountain slopes in one area is called a mountain range.
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.
Canyon
A plain
The area behind a mountain with little rain is called a rain shadow.
The area behind a mountain that receives little rain is known as a rain shadow. This phenomenon occurs when moist air rises over the mountain, cools, and loses moisture as precipitation on the windward side. As the air descends on the leeward side, it becomes drier and warmer, leading to significantly reduced rainfall in the rain shadow region. This can create arid or semi-arid conditions, often resulting in distinct vegetation and ecosystems.
That area is called a rain shadow. It occurs when moist air rises over a mountain, releases moisture on the windward side, and descends down the other side, resulting in a drier climate on the leeward side.
a plain
The portion of a mountain that receives little precipitation is typically the leeward side, also known as the rain shadow area. As moist air rises over the mountain, it cools and loses moisture in the form of precipitation on the windward side. By the time the air descends on the leeward side, it is drier, resulting in significantly less rainfall and often leading to arid conditions.
The desert is the term for a large land area that receives little rain. Almost every continent has a desert except for Antarctica.
A rain shadow is an area of land that receives reduced precipitation due to proximity to mountain ranges. The mountains block the passage of rain-producing weather systems, casting a "shadow" of dryness behind them.
The leeward side of a mountain is called the "rain shadow" side. It is a dry area that receives significantly less precipitation than the windward side of the mountain due to the barrier effect the mountain has on air masses.
The area of the mountain that receives high rainfall is called the windward side. This side of the mountain is typically lush and green due to the moist air being forced to rise and cool, leading to precipitation.
slimish