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Bangladesh & Seas
River Erosion and Accretion
Rivers in Bangladesh are morphologically highly dynamic. The main rivers are braided, and form islands or char in between the braiding channels. These chars, of which  any are inhabited, "move with the flows" and are extremely sensitive to changes in the river conditions. Erosion processes are highly unpredictable, and not compensated by accretion. These processes also have dramatic consequences in the lives of people living in those areas. A four year study concluded in 1991 reported that: out of the 462 administrative units in the country, 100 were subject to some form of riverbank erosion, of which 35 were serious, and affected about 1 million people on a yearly basis (REIS, 1991).

A study by EGIS (1997), analyzing remote sensing images from 1973 to 1996 of the 240 km long Brahmaputra-Jamuna River between the Indian border, and the confluence with the Ganges concluded that the river has been widening at an average rate of about 130 m per year. This corresponded to a loss of about 70,000 ha in 23 years, while only 11,000 ha had been accreted. The same EGIS study concluded that the observed erosion during the flood years 1987 and 1988 was 8,000 ha per year against an average of 3,000 ha per during the mentioned 23 year period - this gives some indication of how sensitive these processes are. Changes in the river flows and sediment transport due to multi- dimensional impacts of climate change are expected to increase the dynamics of these rivers even more. While the consequences are highly uncertain, they give rise to major concern especially given the related loss of land and property.


 

 

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