As moisture carrying air rises to go over a mountain, it cools. When the air cools sufficiently, it can no longer carry along as much moisture, and this moisture will then fall as rain. If the mountain is still higher, the air cools even further as it goes higher to get 'over the mountain'. If the air cools sufficiently, even more moisture is removed due to the decreased carrying capacity of cold air over warm air, and this leads to snow!
The following is an example of how the tallest mountains in the world 'The Himalayas ', influence rainfall and snowfall
The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan plateau. They prevent frigid, dry Arctic winds blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents. It also forms a barrier for the monsoon winds, keeping them from traveling northwards, and causing heavy rainfall in the Terai region. The Himalayas are also believed to play an important part in the formation of Central Asian deserts, such as the Taklamakan and Gobi.
Mountains influence the distribution of rainfall by causing air to rise and cool, leading to condensation and precipitation on the windward side. This results in more rainfall on the windward side of the mountain and a rain shadow effect on the leeward side, where less rainfall occurs.
The cambrian mountains get a lot of rainfall because they are near the coast of England so the water evaporates when it is warm and as it gets closer to the mountains it condenses and turn into clouds the rain mostly falls on one side of the mountain and less on the other this type of rainfall is called relief rainfall
Mountains can influence precipitation in Georgia by creating orographic lift. When moist air is forced to rise over the mountains, it cools and condenses, leading to increased precipitation on the windward side of the mountains. This can result in higher rainfall amounts in areas near the mountains compared to regions further away.
No, the Adirondack Mountains do not meet the criteria to be classified as a temperate rainforest. A temperate rainforest typically has high levels of rainfall and humidity, which are not characteristics of the Adirondack region in New York.
The Blue Ridge region tends to have a temperate climate with mild winters and warm summers. It experiences high humidity levels and can receive significant rainfall throughout the year. The elevation of the Blue Ridge Mountains can also influence local climate variations.
Mountains influence the distribution of rainfall by causing air to rise and cool, leading to condensation and precipitation on the windward side. This results in more rainfall on the windward side of the mountain and a rain shadow effect on the leeward side, where less rainfall occurs.
because, often receive a large amount of rainfall
In Scotland you get the most rainfall because of all the high mountains.
The cambrian mountains get a lot of rainfall because they are near the coast of England so the water evaporates when it is warm and as it gets closer to the mountains it condenses and turn into clouds the rain mostly falls on one side of the mountain and less on the other this type of rainfall is called relief rainfall
The Ethiopian highlands experience predominantly orographic rainfall. This occurs when moist air is forced to rise over the high mountains, leading to cooling and condensation of the water vapor, resulting in rainfall. This type of rainfall is important for supporting agriculture in the region.
Mountains can influence precipitation in Georgia by creating orographic lift. When moist air is forced to rise over the mountains, it cools and condenses, leading to increased precipitation on the windward side of the mountains. This can result in higher rainfall amounts in areas near the mountains compared to regions further away.
Rainfall in mountain areas is called: Orographic rainfall.
Mumbai receives a lot of rainfall due to its coastal location and the influence of the Western Ghats, which trap moisture-laden winds from the Arabian Sea. As these winds ascend the mountains, they cool and condense, resulting in heavy rainfall. In contrast, Pune, located further inland and at a higher elevation, experiences a rain shadow effect, where the mountains block the moist air, leading to significantly less rainfall. This geographical difference is the primary reason for the disparity in rainfall between the two cities.
No, the Adirondack Mountains do not meet the criteria to be classified as a temperate rainforest. A temperate rainforest typically has high levels of rainfall and humidity, which are not characteristics of the Adirondack region in New York.
According to a Forks, Wa. real estate web page the annual average rainfall is 121 inches.
When rainfall increases erosion increases, wearing away the mountains and cliffs and filling in the canyons with the products of erosion.
Mountains are very useful in agriculture because they bring relief rainfall on the windward side.