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Insects drift along with the prevailing wind, but the flight of birds is less dependent on it. Prevailing winds in mountain locations can lead to significant rainfall gradients, ranging from wet across windward-facing slopes to desert-like conditions along their lee slopes. Prevailing winds can vary due to the uneven heating of the Earth ...
The mountain ranges on the eastern side of Madagascar provide a rain shadow for the country's western portion. The windward side of the island of Madagascar, which sees easterly on-shore winds, is wet tropical, while the western and southern sides of the island lie in the rain shadow of the central highlands and are home to thorn forests and ...
This flow, trade winds, and cold air flowing south from North America contribute to winds flowing through several mountain valleys. Along Central America are three main wind jets through breaks in the American Cordillera , on the Pacific Ocean side due to prevailing winds.
Buran (a wind which blows across eastern Asia. It is also known as Purga when over the tundra); Karakaze (strong cold mountain wind from Gunma Prefecture in Japan); East Asian Monsoon, known in Korea as jangma (), and in Japan as tsuyu (梅雨) when advancing northwards in the spring and shurin (秋霖) when retreating southwards in autumn.
It is commonly observed near microbursts and downbursts caused by thunderstorms, [65] weather fronts, areas of locally higher low level winds referred to as low level jets, near mountains, [66] radiation inversions that occur because of clear skies and calm winds, buildings, [67] wind turbines, [68] and sailboats. [69]
Wind and moist air are drawn by the prevailing winds towards the top of the mountains, condensing and precipitating before it crosses the top. In an effect opposite that of orographic lift, the air, without much moisture left, advances behind the mountains, creating a drier side called the "rain shadow". [citation needed]
The westerlies, anti-trades, [2] or prevailing westerlies, are prevailing winds from the west toward the east in the middle latitudes between 30 and 60 degrees latitude. They originate from the high-pressure areas in the horse latitudes (about 30 degrees) and trend towards the poles and steer extratropical cyclones in this general manner. [ 3 ]
The mountain rises approximately 500 feet (150 m) above the plateaus to the west, and over 1,500 feet (460 m) above the lowlands to the east. The prevailing winds hit the mountain's slopes, accelerating up and over its bald summit. It is these conditions that can cause wind chill factors to dip below zero during the winter months.