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The economic significance of the monsoon is aptly described by Pranab Mukherjee's remark that the monsoon is the "real finance minister of India". [ 4 ] [ 5 ] A good monsoon results in better agricultural yields, which brings down prices of essential food commodities and reduces imports, thus reducing food inflation overall. [ 49 ]
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.
It eventually separates from the coastline, turning to the right as it enters the Arabian Sea. The Summer Monsoon Current, located between 10 and 15 North latitude in the Arabian Sea, bends around India and Sri Lanka, and enters the Bay of Bengal. The Great Whirl is a gyre located around 10 N and 55 E, and is only present during the summer season.
MUMBAI/NEW DELHI (Reuters) -Monsoon rains hit the coast of India's southernmost state of Kerala on Thursday, two days sooner than expected, weather officials said, offering respite from a ...
India has received 19% less rainfall since June 1, IMD data showed, as the monsoon's progress had stalled, with almost the entire country except for a few southern states experiencing shortfalls ...
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 ...
The Tropical Easterly Jet is the meteorological term referring to an upper level easterly wind that starts in late June and continues until early September. This strong flow of air that develops in the upper atmosphere during the Asian monsoon is centred on 15°N, 50-80°E and extends from South-East Asia to Africa.
Winds round it circle counterclockwise, from May to September or October giving persistent southwest monsoon winds from over the north Indian Ocean and South China Sea, also south-south-west or south winds over the west Pacific Ocean. [3] Its counterpart during the winter is the Siberian High. [4]