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Answer:

1:Windward side. The windward side is the side of the mountain that has the lower temperatures. This is due to the much higher precipitation that the windward side experiences, and that it has much more cloudy days, while the leeward side is much drier and has much more sunny days.

2:The side of the mountain that experiences the high temperature is the leeward side because the side that experiences low temperature is the windward side.

3:Rain shadow is the answer to what dry region forms at the back of the mountain. This dry region is a land that has become a desert in the long run because there is no amount of water or rainwater for the matter.

4:Water vapor or moist air rising over a mountain will cool and precipitate as rainfall. As water vapor, or moist air approaches a mountain, it will rise because the mountains are in the way. ... The moisture in that air then condenses into clouds and eventually, rain.

5:As the air becomes warmer and drier while it moves down the leeward side of the mountain, the orographic effect takes place. ... When air becomes warmer and drier as it moves down the leeward side, it rises up the atmosphere.

6:The topography of an area can influence the weather and climate. Topography is the relief of an area. If an area is close to a body of water it tends to make milder climates. Mountainous areas tend to have more extreme weather because it acts as a barrier to air movements and moisture.

Explanation:

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