Flooding in Bangladesh.

Formal Name: People's Republic of Bangladesh.

Capital: Dhaka.

Size: Total 144,000 square kilometres, land area 133,910 square kilometres.

Topography: Broad deltaic plain. Chittagong Hills in southeast, Low Hills in northeast and modest-elevation highlands in north and northwest.

Climate: Subtropical monsoon climate, wide seasonal variations in rainfall, moderately warm temperatures, high humidity. Climate generally uniform throughout entire country. Subject to severe natural disasters, such as floods, tropical cyclones, tornadoes, and tidal bores.

Population: Officially given at 109,963,551 in July 1988.

Bangladesh is trapped between two sets of floods: one caused by tidal surges and a rising sea level, and the other by rivers.
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> Silt, deposited at the mouth of the Ganges and Brahmaputra, has formed a large delta. This eventually created many flat islands. They attracted large numbers of farmers for rice growing. Further deposition of silt blocks the main channels and increases the flood risk by raising the beds of the rivers. Flooding is most likely to occur in late summer following the seasonal monsoon rains.

> Water is pushed northwards by tropical cyclones up the Bay of Bengal. Silt deposits cause the Bay of Bengal to become narrower and the sea shallower. The water builds up to ...

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