A rain shadow is a dry area on the lee side of a mountainous area. The mountains block the passage of rain-producing weather systems casting a "shadow" of dryness behind them. As shown by the diagram to the right, the warm moist air is "pulled" by the prevailing winds over a mountain. Then it condenses and precipitates and the dry air moves forward leaving a rain shadow behind the mountain.
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.
The rain shadow equals rain
The rain shadow effect is associated with the leeward side of mountains where moist air rises, cools, and releases precipitation on the windward side. As the air descends on the leeward side, it warms and becomes drier, creating a rain shadow with reduced precipitation.
The rain shadow effect occurs when moist air is forced to rise over a mountain range, causing it to cool and release precipitation on the windward side of the mountain. As the air descends on the leeward side, it becomes warmer and drier, creating a rain shadow where little precipitation falls. This results in a contrast in vegetation and climate on either side of the mountain range.
The rain shadow effect occurs when moist air is pushed up over a mountain range, causing it to cool and release precipitation on the windward side. As the air descends down the other side of the mountain, it warms up and becomes more dry, leading to a rain shadow area with much less precipitation on the leeward side of the mountains.
The rain shadow equals rain
The rain shadow equals rain
Rain shadow effect is possible rarely in mountains, not in Bucharest.
Mountains cause rain shadow effect because they are tall. The mountains keep out the rain.
Mountains
Death Valley is a rain shadow desert in the U.S. It is in the rain shadow effect of the Sierra Nevada mountain range.
On the side of mountain ranges. :)
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.
The rain shadow equals rain
NO
A rain shadow is a natural phenomenon over which man has no control.
The rain shadow effect is associated with the leeward side of mountains where moist air rises, cools, and releases precipitation on the windward side. As the air descends on the leeward side, it warms and becomes drier, creating a rain shadow with reduced precipitation.