Answer:
When the air moves from the windward to the leeward side, that is when the air moves downward, it becomes warm very rapidly and loses all of its moisture content, and thereby becomes dry. This results in the formation of a very high kind of wind which is commonly known as Chinook (or Foehn) winds. This type of wind has a higher temperature and occurs when high mountain ranges are oriented perpendicular to the direction of prevailing winds. For example, the Sierra Nevadas occurring in North America.
When the air moves from the windward to the leeward , what happens is that its becomes warm very rapidly and loses all of its moisture content, and thereby becomes dry.
In geography, the leeward side means the side distant from the lee of the prevailing wind that are typically the drier.
Hence, when air moves from the windward to the leeward , what happens is that its becomes warm very rapidly and loses all of its moisture content, and thereby becomes dry
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