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 equals rain
The rain shadow effect is when there is an area of land that is blocked from precipitation by mountains.
The rain shadow effect produces dry climates in areas downwind from mountain ranges.
A dry area on a mountain side. Rain shadow effect relates to leeward of mountain
mountains
The rain shadow equals rain
The rain shadow equals rain
The rain shadow equals rain
The rain shadow effect is when there is an area of land that is blocked from precipitation by mountains.
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.
The rain shadow effect produces dry climates in areas downwind from mountain ranges.
A dry area on a mountain side. Rain shadow effect relates to leeward of mountain
mountains
Mountains
it has to do with the clouds, rain, and 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.