Monsoon winds of the Arabian Sea- Interesting Facts

Let us learn some important points about this topic –

1. In contrast to the trade winds, the monsoon has a throbbing nature that is influenced by various air conditions experienced on its excursion across the warm tropical seas.
2. At the point when the Southwest monsoon winds show up in India in June, the nation encounters its Southwest Rainstorm season, which goes on until mid-September.
3. At the southernmost mark of the Indian landmass, the storm frequently shows up during the first week of June.
4. The Arabian Sea branch and the Bay of Bengal branch are the two divisions that follow.
5. The Arabian Sea branch lands in Mumbai on June 10, about ten days later. This process happens rather quickly.
6. Over the Arabian Sea, monsoon winds originate in the northeast and shift to the southwest with the changing of the seasons.
7. In the winter, winds originate in Southwest Asia and blow toward the sea.
8. While the majority of the wind from the Bay of Bengal flows towards India, the remainder flows towards Myanmar, Thailand, and Malaysia. The entire wind from the Arabian Sea flows towards India.
9. There are three additional branches to the monsoon winds that emerge over the Arabian Sea:
10. One of its branches is blocked by the Western Ghats. These winds climb the 900-1200 m slopes of the Western Ghats.
11. They cool swiftly, resulting in very substantial rainfall (250–400 cm) on the windward side of the Sahyadris and Western Coastal Plain.
12. After passing over the Western Ghats, these winds descend and become warmer. This results in a decrease in the humidity in the breezes.
13. Because of strong winds, the Western Ghats receive very little rainfall. There is not much rain in the rain-shadow area.
14. North of Mumbai, the shoreline is hit by another branch of the Arabian Sea monsoon.
15. In much of central India, these winds, which pass across the basins of the Narmada and Tapi Rivers, produce rain. The Chotanagpur plateau receives 15 cm of rain from this part of the branch.
16. After that, they merge with the Bay of Bengal branch when they enter the Ganga plains.
17. This monsoon wind’s third branch strikes the Kachchh and the Saurashtra Peninsula.
18. After that, it passes into the Aravallis and western Rajasthan, bringing with it barely a little rain.
19. Additionally, it links to the Punjab and Haryana branches of the Bay of Bengal. These two branches, which reinforce one another, are what cause the rains in the western Himalayas.

The cold breezes that carry showers with them when they move from the ocean’s surface to the land are known as monsoon winds. India’s environment is fundamentally affected by monsoon winds. The branch monsoon winds over the Arabian Sea are the source of the rainstorm winds. Over the North Eastern Ocean, rainstorm winds begin in the northeast and shift toward the southwest with the changing of the seasons. In the colder time of year, winds begin in Southwest Asia and move toward the ocean.

You will find out about the Arabian Sea monsoon winds from this article, which will assist you with getting ready for the UPSC civil service test in geography.