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None whatsoever. The terrain has an effect on the weather but it can't be resumed as precipitation per altitude because what works one way with the wind from one direction, may work the other way with the wind from another direction.

The effect of the terrain on the weather is called the orographic effect, from oro-, that means 'mountain' in Greek. As the air rises, being pushed up over a mountain range, the air cools down by adiabatic effect and moisture condenses into clouds and, perhaps, precipitations. On the lee side of the mountain, the air sinks and if it has lost much of its moisture in precipitation, it does it at the dry adiabatic lapse rate, which is twice that of moist air. It means that it is warmer at the lee side of the mountain. This is called a Foehn wind, in Europe, and a Chinook wind in Canada and the US.

Depending of the altitude of the land and how steep the rise is, it may rain on the weather side, or on a plateau, on the top. Sometimes it is not enough to produce precipitations, only what is called orographic fog. For example, I visited Sao Antonio on the Cape Verde islands and while the islands are extremely dry, they manage to grow some vegetables on the top of the volcanic mountains because there is a constant fog and plants absorb the dew on their leaves.

Not too sure if this is correct. Research more before writing this down. fanks babes.

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11y ago
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11y ago

find it your self dum boo

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12y ago

BHS?

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Q: What is the relationship between elevation and orographic precipitation?
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