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The Introduction of Monsoon Season : ウィキペディア英語版 | The Introduction of Monsoon Season
The introduction of Monsoon season: ( تعارف مون سون ) The Arabic language word for the season 'mawsin' is the root of the word 'monsoon' due to their annual presence. Although the exact cause of the monsoons are not fully clear, it is believed pressure of air is one of the primary factors. During the season of summer, Southern Asia, especially India, Pakistan, Bangladesh and Sri Lanka are soaked with heavy rains that come from air masses, the moist air that moves in from the Indian Ocean to the southern areas. These showers and the masses of air that bring them, are called monsoons ( مون سون یا مانسون ). This term was used first in English in British India. Now this term is also used in India, Bangladesh and Pakistan and other nearby countries. ==Development of Monsoon==
The high pressure over the ocean of air masses moves to the low pressure area over the Asian continent. It produces moisture-laden air to the south of Asia. During winter seasons in Asia, the process is a backtrack and low pressure lies over the Indian Ocean while high pressure sits over the Tibetan Plateau, so air flows directly down to the south ocean and the Himalayas. The migration of swap winds and wind from the west also provide to the monsoon seasons.
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