Typically the lee side of a mountain is where the effect of a rain shadow occurs.
As a cloud moves over a mountain, it drops precipitation and rises. By the time that cloud gets over the mountain-top to the other side of the mountain, it has much less moisture to drop - thus leaving the lee side of the mountain much dryer.
There is no official name. The wet area is upwind. The dry area on the lee side is called the rain shadow. This effect is called the rain shadow effect.
You would find a Rain Shadow, or an area with very little rain. This area would be dry, and quite possibly have a miniature (Or not so miniature!) desert.
One reason is something called the rain shadow effect. When a moist air mass is forced up the face of a mountain range, it drops most of its moisture on the windward side, and so is rather dry going over the mountains. The storms that produce thunderstorms generally need an ample supply of moisture. Second, the highly uneven terrain might inhibit the organization of strong thunderstorms.
There are four general types of climate in the Philippines based on seasonal rainfall distribution. These are: * Type I - two pronounced seasons, dry and wet, with maximum rain period from June to September and a dry season which lasts from three to six months * Type II - no dry season with a very pronounced maximum rain period that occursin December and January * Type III - no very pronounced maximum rain period, with a short dry season lasting from one to three months * Type IV - rainfall more or less evenly distributed throughout the year.
[1] Dry farming's put into effect whenever the cultivator relies just on rain and snow fall, and on soil moisture. Geographically, it would be found in desert-like and drought-prone environments. [2] Successful examples in the United States would be the corn growing of the Hopi in the southwest, and the crop growing of pioneer Latter Day Saints communities in Utah.
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
The rain shadow equals rain
Death Valley is a rain shadow desert in the U.S. It is in the rain shadow effect of the Sierra Nevada mountain range.
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.
There is no official name. The wet area is upwind. The dry area on the lee side is called the rain shadow. This effect is called the rain shadow effect.
Yes it is. See diagram above to explain why.
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 climate in a rain shadow is often extremely dry and dessert-like.
A rain shadow is a dry area on the mountains facing away from the direction of the wind. The mountains block the passage of rain producing weather systems, casting a "shadow" of dryness behind them.
rain shadow
Your shadow.