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How was the winter rain different from the rain in the monsoon?
Answers
Explanation:
Monsoons are principally regular winds in the hotter areas of the world caused by substantial temperature contrasts between land masses and contiguous seas. In the winter, the course is from the cool land to the hotter ocean, while in the mid-year, the inverse is valid.
Answer:
A monsoon is a regular move in the predominant wind course, that as a rule carries with it an alternate sort of climate. It quite often alludes to the Asian storm, a substantial area stretching out from India to Southeast Asia where rainstorm conditions win.
A Western Disturbance is an extratropical storm starting in the Mediterranean district that conveys sudden winter rain toward the northwestern parts of the Indian subcontinent. It is a non-monsoonal precipitation design driven by the westerlies.
Where the mid-year monsoon ends, winter monsoon starts. The winds now originating from the upper east cause insignificant precipitation over whatever remains of the nation, yet the eastern shore of India gets a lot of precipitation. This is on the grounds that the winds disregard the Bay of Bengal, grabbing dampness all the while.
Explanation:
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