Channel bar development, braiding and bankline migration of the Brahmaputra-Jamuna river, Bangladesh through RS and GIS techniques

• Published in: International journal of river basin management Vol. 22; no. 2; pp. 203 - 215
• Main Authors: Rashid, Md. Bazlar, Habib, Md. Ahosan
• Format: Journal Article
• Language: English
• Published: Abingdon Taylor & Francis 02-04-2024; Taylor & Francis Ltd
• Subjects: Bank erosion; bankline migration; Braided river; Braided rivers; Braiding; braiding and sinuosity index; Erosion rates; Geographic information systems; Geographical information systems; Geological hazards; Information systems; Landsat; Landsat satellites; Remote sensing; River erosion; River flow; river shifting; Rivers; Satellite imagery; Sediment; Sediment transport; Sinuosity; Bangladesh
• ISSN: 1571-5124; 1814-2060
• DOI: 10.1080/15715124.2022.2118281

Erosion of banks and channel migrations are usually common phenomenon and recurring geo-hazardous problem in the Brahmaputra-Jamuna river system of Bangladesh. The present study intensively analysed multi-temporal Landsat satellite imageries (Landsat MSS, Landsat TM, Landsat ETM+, Landsat OLI TIRS), historical documents (Hunter maps), and literature information employing Remote Sensing and Geographic Information System techniques, and estimation of braiding and sinuosity indices especially emphasizing channel bar development, braiding, and bank-line migration of the river. The computed braiding indices of the river were 1.5, 10.3, 13.4, 11.0, 10.6 and 14.6 for the year of 1853-1857, 1977, 1989, 2000, 2014 and 2018, respectively (overall deciphering increasing trend). Similar to the braiding indices, the sinuosity indices (2.58, 7.02, 9.92, 8.31, 7.42 and 11.25 for the same selected years) of the river have also been changed over time. During 1853-1857 to 2018, 766.7 and 1624.2 km
2
of lands extensively eroded on the east and west bank, respectively at a rate of 4.8 and 10.1 km
2
yr
−1
. However, from 1977 to 2018, the erosion rates were 14.4 and 12.5 km
2
yr
−1
, respectively. High discharges, sediment transport associated with random bars formation related braiding expansion, and weak bank materials are presumably the governing factors for causing such simultaneous severe bank erosion and remarkable bank-line migration phenomenon. Although, from 1853-1857 to 1977 the erosion of the river followed the river flow direction. It is expected that the outcomes of this research can contribute further research on morphodynamic characteristics of the braided river for better understanding the river characteristics, the river hydromorphology, water and sediment transport, its bank erosion, and formulating protective measurement plan for their sustainable current flow path maintenance.