Erossion.
The leeward side of a mountain is warm because as air moves up and over the mountain, it loses moisture and heat, resulting in warmer and drier air on the leeward side. This process is known as the rain shadow effect and contributes to the warmer temperatures experienced on the leeward side of the mountain.
As moist air is pushed up the windward side of a mountain, it cools and condenses, leading to cloud formation and precipitation. This process, known as orographic lift, causes wetter conditions on the windward side of a mountain.
The leeward side of a mountain is termed as the drier side, as it is the side of the mountain that faces away from the prevailing winds and therefore receives less moisture. This process, known as the rain shadow effect, results in the leeward side being arid or semi-arid compared to the windward side that receives more precipitation.
As winds move up the side of a mountain, they are forced to rise due to the slope. As they rise, the air cools and expands, leading to the formation of clouds and precipitation on the windward side of the mountain. This process is known as orographic lifting.
The warm moist air rises along the western side of the mountain, cools as it gains altitude, and condenses, forming clouds and precipitation. This process is known as orographic lifting, and it leads to increased rainfall on the windward side of the mountain.
The wet side of the mountain is called the windward side. The dry side of the mountain is called the leeward side.
My Side of the Mountain was created in 1959.
A group of mountain ranges that run side by side is called a cordillera.
As the air is forced to rise over the mountain range, it undergoes adiabatic cooling, leading to the condensation of water vapor and the formation of clouds and precipitation on the windward side of the mountain. This process is known as orographic lifting and can result in enhanced rainfall on the windward side and a rain shadow effect on the leeward side of the mountain.
Clouds form on the windward side of a mountain due to orographic lift, where moist air is forced to rise as it encounters the mountain's elevation. As the air ascends, it cools and expands, leading to condensation and cloud formation. This process often results in increased precipitation on the windward side, while the leeward side, or rain shadow, tends to be drier.
One side for back breaks and one side for front breaks
The first book is My Side of the Mountain, followed by On the Far Side of the Mountain, Frightful's Mountain, Frightful's Daughter, and Frightful's Daughter Meets the Baron Weasel.