The south – west monsoon season, or the advancing monsoon season, lasts from
June to September. The intense heat of summer causes the development of a
powerful low-pressure trough over the north – western parts of the Indian
subcontinent. Winds originating from a high – pressure area centered over the
southern Indian Ocean are drawn to the low-pressure trough in the north. Since
the winds originate over the sea, absorb the enormous amount of moisture as they blow over the sea. These moisture laden winds cross the equator and approach the
Indian landmass from the south-west.
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