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Why mountains are wetter?
Mountains are wetter because of orographic lifting, a process where moist air is forced to rise as it encounters the mountain slope. As the air rises, it cools and condenses into clouds and precipitation. This results in higher amounts of rainfall or snowfall on the windward side of the mountain.
Explain with the aid of a diagram how relief rainfall occurs?
Relief rainfall occurs when moist air is forced to rise over a mountain barrier. As the air rises, it cools and condenses to form clouds and eventually rain. The diagram would show warm, moist air approaching the mountain, rising, cooling, condensing, and then raining on the windward side of the mountain. The leeward side of the mountain would be in a rain shadow, receiving significantly less rainfall.
Why is precipitation more abundant on one side e of the mountain?
When moist air rises up a mountain, it cools and condenses, leading to precipitation on the windward side. As the air descends down the other side, it warms and dries out, creating a rain shadow effect. This creates a drier climate on the leeward side of the mountain.
Land that rises above the land around it?
hill
What is oragraphic rainfall?
Orographic rainfall occurs when moist air is forced upwards by a barrier, such as a mountain range, leading to the air cooling and condensing to form clouds and precipitation. As the air rises over the barrier, it cools and releases moisture, resulting in increased rainfall on the windward side of the mountain range.
What happens to warm moist air which rises up the western side of a mountain?
As warm, moist air rises up the western side of a mountain, it cools due to the decrease in atmospheric pressure at higher altitudes. This cooling causes the moisture in the air to condense, forming clouds and often resulting in precipitation. This process is known as orographic lift. Once the air descends on the eastern side of the mountain, it warms up and becomes drier, leading to a rain shadow effect.
What happens as warm, moist air rises in the atmosphere?
As warm, moist air rises in the atmosphere, it cools and condenses, forming clouds and eventually leading to the possibility of precipitation such as rain or snow.
Why condensations occurs when moist air rises?
Condensation may occur when moist air rises because of the different arrangement of water molecules.
What happens when moist air is lifted higher in the atmosphere?
When moist air rises this process is called evaporation.after this most air have rised it condense then rain falls.
What happens when domestic income rises?
What happens when domestic income rises?
What is the tallest mountain in the western hemisphere?
That would be Aconcagua located in western Argentina near the border with Chile whose height is 6,962 meters or 22,841 feet. Mt. Aconcagua
A tall landform that rises to a peak is called?
A tall landform that rises to a peak is called a mountain.
Why mountains are wetter?
Mountains are wetter because of orographic lifting, a process where moist air is forced to rise as it encounters the mountain slope. As the air rises, it cools and condenses into clouds and precipitation. This results in higher amounts of rainfall or snowfall on the windward side of the mountain.
When warm moist air rises to form thunderstorms what do you call that?
Evaporation.
What is the mountain the rises along the eastern board of the US?
I believe that would be the Aplelacian Mountains. maybe rockies The Rocky Montains run along the western seaboard.
What happens to air as it rises over a mountain range?
On the windward side of a mountain range, air rises, cools, and drops its moisture. On the leeward side of a mountain range air descends, heats up, and dries the land. Deserts are common behind mountains. (493) Glencoe Texas Science, Grade 8 © 2002
Explain with the aid of a diagram how relief rainfall occurs?
Relief rainfall occurs when moist air is forced to rise over a mountain barrier. As the air rises, it cools and condenses to form clouds and eventually rain. The diagram would show warm, moist air approaching the mountain, rising, cooling, condensing, and then raining on the windward side of the mountain. The leeward side of the mountain would be in a rain shadow, receiving significantly less rainfall.
