Orographic effect
Orographic effect
A rain shadow desert forms at the back of a mountain range. As moist air is pushed up over the mountains, it cools, condenses, and releases precipitation on the windward side. By the time the air descends on the other side, it is drier, leading to arid conditions and the formation of a desert.
When the air in your eyelids is pushed out through the moist surface, the sound is made.
it becomes moist
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
Created when warm, moist air is forces to rise over a barrier. (mountain).
The higher you go, the colder it gets. The colder it gets, the less water vapor can remain in the air. That's the reason it rains on the windward side of mountain ranges. Warm, moist air gets pushed up and the rain condenses.
Amniotic fluid
It produces lift which if in a moist enough airmass will produce thunderstorms
You are referring to a "rain shadow".
Rainshadow
The southern Appalachians. They are a deep woods species, found in moist mountain woodlands.