Flooding in Bangladesh

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Flooding in Bangladesh

Bangladesh is a low lying country and almost all of Bangladesh lies on the largest delta in the world.  It is situated between the Himalayas and the Indian Ocean with a vast river basin made up of the Ganges, the Brahamaputra, the Meghna and their tributaries. It also has the highest population density in the world with 847 inhabitants per square kilometer.

Bangladesh is one of the world's least developed countries and prone to natural disasters, such as cyclones, floods and droughts. Half of it is less than five meters above sea level. Therefore any change in the earth’s temperature that causes the level of the oceans to rise would seriously affect the flooding of the delta area of Bangladesh.

A fifth to a third of the country is annually flooded by the river Ganges and there are many factors both human and physical which encourage the river Ganges and Brahmaputra to overflow its river banks. The obvious physical cause of flooding in Bangladesh is that about 90% of the land is below sea level, therefore any changes in the sea level would cause serious problems for Bangladesh.

Another physical cause includes the snow melting in the Himalayas, caused by global warming. The Himalayas are one of the few places in the world that retain permanent glaciers. In the warmer summer season however glacial ice goes through a period of melting. The source of the Brahmaputra starts in the Himalayas and an increase in melted-water flowing through its drainage basin will increase channel flow, saturate soils and cause massive overland flow – a major cause of flooding.

Another major cause is the cyclonic storms that frequent the Bay of Bengal. Storm surges which are rapid rises in sea-level caused by intense areas of low pressure i.e. depressions and tropical cyclones, precede cyclonic storms and are often as high as seven to ten meters.

The heavy wet summer monsoons also contribute to the flooding, it brings rain that adds to the flow of water in rivers. The summer monsoon was responsible for the excessive rainfall of 1987 and 1988 in Bangladesh.

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An increased amount of precipitation can also cause flooding. An above normal monsoon downpour in the Ganges-Brahmaputra-Megna drainage system is thought to be the primary cause of the 1988 flood in Bangladesh. It is not known, however, if the heavy precipitation is actually an effect of other processes such as the greenhouse effect or destruction of forests in the upstream region.

Another physical cause of flooding in Bangladesh is tectonic activity. The Indian Plate is moving towards the Eurasian Plate. The land where they meet (Himalayas) is getting higher and steeper every year (fold mountains). As a ...

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