Explain monsoon winds in three points
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A monsoon (/mɒnˈsuːn/) is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation,[1] but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with the asymmetric heating of land and sea.[2][3] Usually, the term monsoon is used to refer to the rainy phase of a seasonally changing pattern, although technically there is also a dry phase. The term is sometimes incorrectly used for locally heavy but short-term rains.
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- Monsoons are basically seasonal winds that reverse their direction according to the change in season.
- They are hence, periodic winds.
- The monsoons travel from the sea to the land in summers and from land to the sea during winters, hence, are a double system of seasonal winds.
- The monsoons have been very important because these winds were used by traders and seafarers to move from place to place. Though there is monsoon in the Indian subcontinent, central-western Africa, Southeast Asia and a few other places, the winds are most pronounced in the Indian subcontinent.
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