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Monsoon is the rainy phase of a seasonally-changing pattern, although . It is because of seasonal changes in atmospheric circulation and precipitation associated with the asymmetric heating of land and sea. The major monsoon systems of the world consist of the West African and Asia-Australian monsoons. The term was first used in English in British India to refer to the big seasonal winds blowing from the Bay of Bengal and Arabian Sea in the southwest bringing rainfall to the area.
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