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The Monsoon of South Asia is among several geographically distributed global monsoons. It affects the Indian subcontinent , where it is one of the oldest and most anticipated weather phenomena and an economically important pattern every year from June through September, but it is only partly understood and notoriously difficult to predict.
Cyclone Mocha destroyed 2,522 houses and damaged 10,469 others in May. [2] Three people died of indirect causes [3] and 12 others were injured. [4]Flooding in August killed 57 people, left several missing, displaced around 45,000 residents and affected 1.2 million others, as well as damaging over 2,700 shelters.
The Malaysian Meteorological Department projected between five and seven major rainfall events during the 2024 annual monsoon season in Malaysia, which typically spans from November through March. Government officials anticipated that the 2024 floods could surpass the severity of the 2014-15 monsoon season , which resulted in twenty-one ...
A food stall was washed away as monsoon floods submerged a street market in the Philippines. Footage shows the wooden stand floating on rubbish-filled waters swamping the road in Quezon City on 17 ...
Taiwan shuttered offices, schools and tourist sites across the island on Wednesday ahead of a powerful typhoon that already worsened seasonal rains in the Philippines, killed at least 13 people ...
In December 2022, a series of floods began to severely affect the provinces of Misamis Occidental and Misamis Oriental, and some parts of the southern island of Mindanao in the Philippines. The floods were caused by intense rain, which poured down on the central and southern parts of the country. [4] [5] [6] [7]
From January to October 2022, excessive rainfall and widespread monsoon flooding occurred in the South Asian countries of Afghanistan, Bangladesh, India, Nepal, Pakistan, and Sri Lanka. It has become the region's deadliest floods since 2020, with over 4,700 people dead.
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.