west side of the mountain
This is false most of the precipitation from moisture laden winds from the sea does not fall on the leeward side of mountains. Many deserts are located in the interior of continents, far from moisture- laden winds blowing from the ocean.
Windward
Mountains force the humid air from the sea to rise where the moisture condenses and falls as rain on the windward side of the mountains. The air passes to the leeward side but now lacks moisture forming a rain shadow desert. See the diagram above.
Rain Shadows form on the leeward side of some mountain ranges. The mountains block the flow of moist air and force it to condense and fall as rain on the windward side of the mountain. See the diagram above.
its the west side.The east is the dry side on the West Coast.
Southern California is very dry because there is very little rain fall. This is because the mountains block precipitation.
the windward slope is wetter. the leeward slope is drier. source: geosystems sixth edition by christopherson, page 213 by: josephine
the inland side, AKA leeward side
Mountains have two effects on precipitation. These are the rain shadow effect and the orographic effect. These both cause the type and amount of precipitation to change because the air is forced higher up.
Windward Side.
cuz they are on the windward side of mountains
One side of a mountain range will have significantly less precipitation than the other side due to the height of the mountain. The clouds that carry the water for precipitation, may be blocked by the tall mountains.
However, such effects do not occur frequently over low mountain ranges, .... This causes much spillover on the lee side of the mountains. .... 8); as a consequence, precipitation downstream of the mountains is ..... of long-term annual precipitation in a mountainous region from a diagnostic model. ...
falxsesfdsxbg
False, windward.
rain shadow
in the west side