Climate is the measure of average meteorological variables in a given region over long periods of time. A rain shadow could possibly effect the temperature, humidity, atmospheric pressure, or precipitation of a region.
A rain shadow is the relatively dry area on the side of a mountain that is away from the prevailing wind. The local winds that result tend to be very dry as the moisture is dropped on the other side of the mountain before the winds rise over the crest.
because it creates tropical cumulus sublimation
winds that flow down the eastern slopes of the rocky mountains are called chinook.
Mountain Ranges
Mountains
The rain shadow effect produces dry climates in areas downwind from mountain ranges.
The rain shadow effect happens by a mountain and on the leeward side (west side) has a warm and wet climate. The windward side (east side ) has a cool & dry climate.
The climate in a rain shadow is often extremely dry and dessert-like.
The rain shadow equals rain
The rain shadow equals rain
The rain shadow effect produces dry climates in areas downwind from mountain ranges.
The rain shadow effect happens by a mountain and on the leeward side (west side) has a warm and wet climate. The windward side (east side ) has a cool & dry climate.
The climate in a rain shadow is often extremely dry and dessert-like.
The rain shadow equals rain
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.
False, you big cheater.
A dry area on a mountain side. Rain shadow effect relates to leeward of mountain