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The Monsoon season typically begins from June and ends in September. The following is the annual monsoon rainfall for the last few years based on data from the Bangladesh Meteorological Department. [11] In 2000, a total of 5,220 millimetres (206 in) was recorded. In 2001, a total of 5,590 millimetres (220 in) was recorded.
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.
It is the first of the two months that comprise the wet season, locally known as "Barsha" (Bengali: বর্ষা Bôrsha, Nepali: वर्षा Barsha, Odia: ବର୍ଷା Barsā), when the monsoon winds blow. [3] [4] It is one of the first five months of the year that have 31 days, according to the Bangladeshi version of the Bengali ...
The death toll this year was more than five times that of 2022, when Bangladesh recorded 281 dengue-related deaths, and the deadliest si Rising temperatures, longer monsoon drive Bangladesh's ...
The second wave of the floods, which lasted from June 2022 to September 2022, due to "Monsoon season", caused the Brahmaputra, Barak and other major rivers in the state to overflow which eroded the river banks and also the houses present their. Around 1,100 houses got completely destroyed and 7,000 houses got partially damaged.
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.
The Bangladesh Ministry of Cultural Affairs has launched an ambitious anthology film project titled “Remembering Monsoon Revolution,” selecting eight accomplished directors to create works ...
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.