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The European Monsoon (more commonly known as the return of the westerlies) is the result of a resurgence of westerly winds from the Atlantic, where they become loaded with wind and rain. [60] These westerly winds are a common phenomenon during the European winter, but they ease as spring approaches in late March and through April and May.
The unique geographical features of the Indian subcontinent, along with associated atmospheric, oceanic, and geographical factors, influence the behavior of the monsoon. Because of its effect on agriculture, on flora and fauna, and on the climates of nations such as Bangladesh, Bhutan, India, Nepal, Pakistan, and Sri Lanka – among other ...
Wet season storm in Darwin. In northern Australia, the predominant wind is from the east or southeast in most occasions, which usually bring dry conditions. [4] Though during monsoon periods (between November and April), the winds change to northwesterly, where atmospheric pressure decreases over an area extending to Java, Sumatra, Timor Sea and eastward to Papua New Guinea.
August position of the ITCZ and monsoon trough in the Pacific Ocean, depicted by area of convergent streamlines in the northern Pacific. The monsoon trough is a portion of the Intertropical Convergence Zone in the Western Pacific, [1] [2] as depicted by a line on a weather map showing the locations of minimum sea level pressure, [1] and as such, is a convergence zone between the wind patterns ...
Monsoon storms typically form when an area of high pressure draws moisture up from the Baja Peninsula and other parts of Mexico and then the wind turns to blow from the south, pushing that ...
Onset dates and prevailing wind currents of the southwest summer monsoon. See also: Monsoon and Monsoon trough During the Northern Hemisphere summer season the MJO-related effects on the Indian and West African summer monsoon are well documented.
India's monsoon season is arguably the single most important weather phenomenon for the country, and a good monsoon can noticeably boost the nation's economy and the livelihoods of its 120 million ...
The ancient Sinhalese of Anuradhapura and in other cities around Sri Lanka used the monsoon winds to power furnaces as early as 300 BCE. The furnaces were constructed on the path of the monsoon winds to bring the temperatures inside up to 1,200 °C (2,190 °F). [94] A rudimentary windmill was used to power an organ in the first century CE. [95]