As air moves from the windward side to the leeward side, it loses moisture.
Dry.
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.
A dry area on a mountain side. Rain shadow effect relates to leeward of mountain
The rain shadow equals rain
is the climate on the ocean side of a mountain dry
As air moves from the windward side to the leeward side, it loses moisture.
Dry.
Dry.
The leeward side of a mountain or anything else is warm and dry.
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
because the leeward side of a mountain doesn't get any rain like on the westward side, also air drops in horse latitudes, and when air drops it causes a dry climate
I assume you are referring to a rain shadow desert but your question makes little sense as written. A rain shadow desert forms when a mountain range blocks the flow of moisture from reaching the interior of a continent. It forces the ran to fall on the windward side of the mountains and little moisture is able to cross the mountains to the leeward side. See the diagram above.
The dry area on the side of a mountain is called the leeward side. This is normally the area where deserts and steppes begin to form.
rain shadow
The windward side of a mountain is typically the west side of the mountain, receiving the various weather as weather moves west to east. The leeward side of a mountain opposes the windward side, making it the east side of the mountain, receiving little weather, blocking weather (rain) and warming air rapidly as it moves down this side of the mountain. The leeward side of mountains causes deserts, dry places, little rain, etc., for it releases warm air unto these places, and blocks weather (rain) from moistening them (I.E. Las Vegas, etc. on the eastern side of the mountain ranges).
The windward side of the mountain has most of the precipitation. This happens because it gets colder the higher you go. As the air cools off, it reaches its dew point temperature,and the moisture in the air condenses to form clouds, and eventually rain, or snow.