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The long-term average has been 899 millimeters of precipitation. [1] However, the monsoon varies over the Indian subcontinent within a ±20% range. Rains that exceed 10% typically lead to major floods, while a 10% shortfall is a significant drought. [2] The Monsoon of South Asia is among several geographically distributed global monsoons.
India, where nearly half of the country's farmland lacks irrigation, has so far received 7% above average rainfall since June 1, when the monsoon arrived on the southernmost Kerala coast, said ...
A monsoon (/ m ɒ n ˈ s uː n /) 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 annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator.
During the Triassic period of 251–199.6 Ma, the Indian subcontinent was the part of a vast supercontinent known as Pangaea.Despite its position within a high-latitude belt at 55–75° S—latitudes now occupied by parts of the Antarctic Peninsula, as opposed to India's current position between 8 and 37° N—India likely experienced a humid temperate climate with warm and frost-free weather ...
After months of flooding, deadly lightning strikes and numerous landslides, residents across India and the surrounding region may be eagerly awaiting the retreat of the Southwest monsoon. However ...
Retrieved from "https://en.wikipedia.org/w/index.php?title=Monsoon_of_India&oldid=566973231"This page was last edited on 3 August 2013, at 11:13
In Asia, rainfall is favored across its southern portion from India east and northeast across the Philippines and southern China into Japan due to the monsoon advecting moisture primarily from the Indian Ocean into the region. Similar, but weaker, monsoon circulations are present over North America and Australia.
The seasonally reversing open ocean currents that pass south of India are referred to as the Winter Monsoon Current and the Summer Monsoon Current (alternately, the Northeast Monsoon Current and the Southwest Monsoon Current). [1] The cold Somali Current, which is strongly linked to the Indian monsoon, is also discussed in this article.