Orographic effect
first water evaporates mostly from oceans, then the wind carries the moist air inland, then the moist air cools as the wind pushes it up the mountain, then as it condense causing rain on the windward side of the mountain, then as the air reaches the leeward side of the mountain it warms and falls and then last but not least the warmer air produces a rain shadow on the opposite side of the mountain
The warm moist air rises along the western side of the mountain, cools as it gains altitude, and condenses, forming clouds and precipitation. This process is known as orographic lifting, and it leads to increased rainfall on the windward side of the mountain.
Orographic effect
Nothing
You hiccup.
Rainshadow
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.
If I Am Not Mistaken Cooler And Cooler.
Decreases
Air evaporates
it decreases
Created when warm, moist air is forces to rise over a barrier. (mountain).