4.7 Article

Response of the Sundarbans coastline to sea level rise and decreased sediment flow: A remote sensing assessment

期刊

REMOTE SENSING OF ENVIRONMENT
卷 115, 期 12, 页码 3121-3128

出版社

ELSEVIER SCIENCE INC
DOI: 10.1016/j.rse.2011.06.019

关键词

Sundarbans; Bengal delta; Coastline dynamics; Satellite imagery; Erosion; Accretion

资金

  1. NASA [NNX11AF50G]
  2. NASA [146008, NNX11AF50G] Funding Source: Federal RePORTER

向作者/读者索取更多资源

The Sundarbans is the world's largest remaining single block of mangrove forest, covering approximately 1 million ha (similar to 1,000 km(2)) of the Ganges-Brahmaputra delta along the coastal areas of India and Bangladesh. Sea level rise and alteration of water flows of the Himalayan headwaters are among the major disturbances threatening these coastal areas. But very few studies exist on the dynamics or current status of the Sundarbans coastline. We used Landsat images spanning from 1973 to 2010, and an algorithm that we developed, to consistently estimate the spatiotemporal dynamics of erosion and accretion for four different time intervals and the whole study period. Our results show that the direction and extent of erosion and accretion rates varied throughout the different periods. Erosion was the highest in the 1973-1979 interval, with 23.2 km(2) year(-1) of land loss. However, that rate substantially declined in the following periods, reaching a rate of 7-10 km(2) year(-1). Accretion showed a rate of 10 km(2) year(-1) between 1973 and 1989, but substantially declined to similar to 4 km(2) year(-1) between 1989 and 2010. Accretion rate has declined in the recent years but erosion rate has remained relatively high. As a result the delta front has undergone a net erosion of similar to 170 km(2) of coastal land in the 37 years of our study period. These numbers are significantly higher than the previously reported rates and magnitudes of erosion in this area. The methods and maps developed in this study may be helpful in management planning of this vulnerable coastline. (C) 2011 Elsevier Inc. All rights reserved.

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