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Morphodynamic Changes of Lohit River, NE India:GIS-Based Study


Affiliations
1 Department of Earth Sciences, Indian Institute of Technology Roorkee, Roorkee 247 667, India
2 Department of Earthquake Engineering, Indian Institute of Technology Roorkee, Roorkee 247 667, India
 

The Lohit River is a south bank tributary of the Brahmaputra River. Till 1987, the Lohit River used to meet the Brahmaputra at a place near Bairagi Chapari (27.77°N, 95.44°E). By 1995, the confluence point had shifted about 20 km downstream. One small channel of the Lohit River captured the Dangori River during the 1988 flood. Gradually the Lohit River started flowing along the captured channel. By 1995, it became the trunk channel of the Lohit River and Dibru Saikhowa region became an island. Banklines of Brahmaputra and Lohit rivers have undergone significant changes near their confluence point within the last few decades. By 1987, the south bank of the Brahmaputra near Rohmoria (27.55°N, 95.15°E) shifted about 1.6 km southward from its position in 1973. Interestingly, within the period 1988-90 the south bank shifted about 4.1 km south. This major shifting was the result of capturing of the Dangori River by the Lohit River. However, migration of the rivers towards the south has stopped after 1995. Analysis of SRTM DEM reveals that topographic elevation has played a major role in changing the course of the Lohit River.

Keywords

Banklines, Confluence Point, Morphodynamic Changes, Topographic Elevation, Trunk Channel.
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  • Morphodynamic Changes of Lohit River, NE India:GIS-Based Study

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Authors

S. Borgohain
Department of Earth Sciences, Indian Institute of Technology Roorkee, Roorkee 247 667, India
J. Das
Department of Earthquake Engineering, Indian Institute of Technology Roorkee, Roorkee 247 667, India
A. K. Saraf
Department of Earth Sciences, Indian Institute of Technology Roorkee, Roorkee 247 667, India
G. Singh
Department of Earth Sciences, Indian Institute of Technology Roorkee, Roorkee 247 667, India
S. Baral
Department of Earth Sciences, Indian Institute of Technology Roorkee, Roorkee 247 667, India

Abstract


The Lohit River is a south bank tributary of the Brahmaputra River. Till 1987, the Lohit River used to meet the Brahmaputra at a place near Bairagi Chapari (27.77°N, 95.44°E). By 1995, the confluence point had shifted about 20 km downstream. One small channel of the Lohit River captured the Dangori River during the 1988 flood. Gradually the Lohit River started flowing along the captured channel. By 1995, it became the trunk channel of the Lohit River and Dibru Saikhowa region became an island. Banklines of Brahmaputra and Lohit rivers have undergone significant changes near their confluence point within the last few decades. By 1987, the south bank of the Brahmaputra near Rohmoria (27.55°N, 95.15°E) shifted about 1.6 km southward from its position in 1973. Interestingly, within the period 1988-90 the south bank shifted about 4.1 km south. This major shifting was the result of capturing of the Dangori River by the Lohit River. However, migration of the rivers towards the south has stopped after 1995. Analysis of SRTM DEM reveals that topographic elevation has played a major role in changing the course of the Lohit River.

Keywords


Banklines, Confluence Point, Morphodynamic Changes, Topographic Elevation, Trunk Channel.

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DOI: https://doi.org/10.18520/cs%2Fv110%2Fi9%2F1810-1816