It gets cool beacause the air is thinner and cant hold as much heat.
According to Blackbody radiation, the darker the object the more light it will absorb. A perfect example is a radiometer, in a light bulb container, there is a thin pin pointing upwards in the middle of the bulb. Then, a little tube with the pin through it has four surfaces. Each surface has a white side and a dark side. If you put something that radiates heat, then it will spin. Since, one side absorb more radiation then the other side, on side is more denser. As a result, it spins.
Frictional energy is converted to heat.
it becomes a mixture of a warm and cold water :)))
Mostly they expand as they warm, contract as they cool.
it will pop
The water vapor melts and it goes into the mountain
The warm air cools as it is blown up the side of the mountain, causing rain. (info from prentice hall science explorer weather and climate book.)
The leeward side is the downwind side, the sheltered side
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.
The dry side of a mountain is called the leeward side. This is the side away from the wind. The dry area is known as a rain shadow.
The leeward side of a mountain or anything else is warm and dry.
Orographic lift.
The pie graph gets warm when the sunlight hits it.
When a cold front hits, usually the warm air rises.
When a hurricane hits the Gulf Stream is strengthens because the water in that current is warm.
The warm dry winds that blow down the side of the mountain (leeward side) are known as Foehn Winds.
Warm air expands and rises from the base on one side of the mountain. It cools and contracts in the clouds above the mountain and sinks back down but on the desert side of the mountains. This way both sides of the mountain are heated properly.