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Concept
Rain Shadow Effect
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Summary
The
rain shadow effect
occurs when
moist air
ascends a
mountain range
, cools and loses moisture as precipitation on the
windward side
, leaving the
leeward side
dry as
descending air
warms and retains moisture. This phenomenon creates distinct
ecological zones
and influences
local climate
, often resulting in
arid regions
adjacent to
lush areas
.
Relevant Degrees
Meteorology 60%
Geomorphology 30%
External Geodynamics 10%
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