How does the tibet plateau influence the monsoon system of the indian subcontinent?
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↪▶Monsoon is traditionally defined as a seasonal reversing wind accompanied by corresponding changes in precipitation, but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with the asymmetric heating of land and sea.
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It influences in such a way that both the tibetan plateau as well as the indian subcontinent are benefitted.
Monsoon (commonly known as rainy season in many countries) is genuinely defined as a seasonal reversing wind accompanied by certain corresponding changes in precipitation but now is used to describe particular seasonal changes in the atmospheric circulation as well as precipitation associated with the asymmetric heating of land and/or sea.
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