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Rainfall on the windward and leeward sides of a mountain differ in the amount, whereby the windward side receives more rainfall.
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∙ 10y agoThe windward side of a mountain is typically wetter and receives more rainfall due to the moist air being forced to rise and cool, causing precipitation. In contrast, the leeward side experiences a rain shadow effect, receiving much less rainfall as the air descends and warms, leading to drier conditions.
The windward side of a mountain typically receives more rainfall because as moist air rises up the mountain, it cools and condenses, leading to precipitation. On the leeward side, the air is drier and descends, which causes it to warm and retain less moisture, resulting in a rain shadow effect and less rainfall.
The windward side of a mountain receives more rainfall due to moist air being forced to rise and cool, leading to precipitation. In contrast, the leeward side, also known as the rain shadow side, receives less rainfall because the descending air is warmed and unable to hold as much moisture, resulting in drier conditions.
The leeward side of a mountain is typically drier and experiences a rain shadow effect, where the air loses moisture as it rises and cools over the mountain, leading to less precipitation. In contrast, the windward side of a mountain is usually wetter due to orographic lifting, where air is forced to rise, cool, and condense, resulting in more rainfall or snowfall.
The windward side of a mountain receives more rainfall because as moist air rises up the mountain slope, it cools and condenses, leading to precipitation. In contrast, the leeward side, also known as the rain shadow side, receives significantly less rainfall as the air has already released much of its moisture on the windward side and descends, causing warming and drying.
The leeward side of a mountain is often drier and experiences a rain shadow effect because most of the moisture is already released on the windward side. This can lead to desert-like conditions and lower precipitation levels. In contrast, the windward side tends to be wetter due to orographic lifting, which cools the air and leads to condensation and precipitation.
rain shadows usually occur on the leeward side of the mountain ranges.
the wind left his all moisture on windward side.
The windward side of a mountain typically receives more rainfall because as moist air rises up the mountain, it cools and condenses, leading to precipitation. On the leeward side, the air is drier and descends, which causes it to warm and retain less moisture, resulting in a rain shadow effect and less rainfall.
The windward side of a mountain receives more rainfall due to moist air being forced to rise and cool, leading to precipitation. In contrast, the leeward side, also known as the rain shadow side, receives less rainfall because the descending air is warmed and unable to hold as much moisture, resulting in drier conditions.
The leeward side of a mountain is typically drier and experiences a rain shadow effect, where the air loses moisture as it rises and cools over the mountain, leading to less precipitation. In contrast, the windward side of a mountain is usually wetter due to orographic lifting, where air is forced to rise, cool, and condense, resulting in more rainfall or snowfall.
You may refer to the following link, which is self explanatory: http://en.wikipedia.org/wiki/Rain_shadow Answered on 26/06/2009 by: Jeril
The windward side of a mountain receives more rainfall because as moist air rises up the mountain slope, it cools and condenses, leading to precipitation. In contrast, the leeward side, also known as the rain shadow side, receives significantly less rainfall as the air has already released much of its moisture on the windward side and descends, causing warming and drying.
The leeward side of a mountain is often drier and experiences a rain shadow effect because most of the moisture is already released on the windward side. This can lead to desert-like conditions and lower precipitation levels. In contrast, the windward side tends to be wetter due to orographic lifting, which cools the air and leads to condensation and precipitation.
The wind forces the moist air mass to move upward, which reduces the pressure on the air mass. As a result, it is less able to support the moisture it is carrying and it dumps water on the windward side. Depending on the size of the mountain, this can result in a wind flow over the top that is low in moisture and higher in temperature. In Switzerland, there is an effect called a Foehn, which results in everyone taking the day off because of the pleasant climactic effect. Google Foehn.
Steppes get more rainfall
Turkey's coastal areas have a Mediterranean climate with hot, dry summers and mild, wet winters. In contrast, the steppes in Turkey experience a continental climate with hot summers and cold winters, characterized by low precipitation and temperature variations. The coastal areas have more moderate temperatures and higher levels of humidity compared to the steppes.
They are made up of different things and differ in size.