Because the atmosphere gets denser as elevation increases.
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.
rain shadow
A rain shadow is a region on the leeward side of a mountain that receives significantly less precipitation than the windward side. As moist air rises over the mountain, it cools and releases most of its moisture, creating rainy conditions on one side of the mountain. The air that descends on the other side is dry and warms up, leading to drier conditions and creating the rain shadow effect.
When moist air rises up a mountain, it cools and condenses, leading to precipitation on the windward side. As the air descends down the other side, it warms and dries out, creating a rain shadow effect. This creates a drier climate on the leeward side of the mountain.
This is due to the orographic effect, where moist air is forced to rise over the mountain, cools, condenses and forms clouds, and then releases precipitation on the windward side. As the air descends on the leeward side, it warms and dries, leading to a rain shadow effect where this side receives less precipitation.
Which_of_these_areas_most_likely_has_the_least_precipitation_is_it_coastal_plain_mountain_top_leeward_side_of_a_mountain_or_winward_side_of_mountain
Which_of_these_areas_most_likely_has_the_least_precipitation_is_it_coastal_plain_mountain_top_leeward_side_of_a_mountain_or_winward_side_of_mountain
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.
One side receives significantly less precipitation due to a phenomenon known as the rain shadow effect. When moist air rises over a mountain range, it cools and loses moisture in the form of precipitation on the windward side. As the air descends on the leeward side, it warms and becomes drier, resulting in significantly less rainfall. This creates a stark contrast in climate between the two sides of the mountain.
Your mom fool!
rain shadow
A rain shadow is a region on the leeward side of a mountain that receives significantly less precipitation than the windward side. As moist air rises over the mountain, it cools and releases most of its moisture, creating rainy conditions on one side of the mountain. The air that descends on the other side is dry and warms up, leading to drier conditions and creating the rain shadow effect.
When moist air rises up a mountain, it cools and condenses, leading to precipitation on the windward side. As the air descends down the other side, it warms and dries out, creating a rain shadow effect. This creates a drier climate on the leeward side of the mountain.
pumas, bears, mountain lions, wolves, other large mountain animals, and sometimes humans
pumas, mountain lions, bears, other large mountain animals, wolves, and sometimes humans
pumas, bears, mountain lions, other large mountain animals, wolves, and sometimes humans
The tornado would go up one side of the mountain and down the other without being significantly affected.