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Dutta, Subashisa
- Study of Channel Instability in the Braided Brahmaputra River Using Satellite Imagery
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Authors
Affiliations
1 Department of Civil Engineering, Thapar University, Patiala 147 004, IN
2 Department of Civil Engineering, Indian Institute of Technology Kanpur, Kanpur 208 016, IN
3 Department of Civil Engineering, Indian Institute of Technology Guwahati, Guwahati 781 039, IN
1 Department of Civil Engineering, Thapar University, Patiala 147 004, IN
2 Department of Civil Engineering, Indian Institute of Technology Kanpur, Kanpur 208 016, IN
3 Department of Civil Engineering, Indian Institute of Technology Guwahati, Guwahati 781 039, IN
Source
Current Science, Vol 112, No 07 (2017), Pagination: 1533-1543Abstract
In the present study, instability of the river reach of Brahmaputra was analysed for braided belt width changes, braiding index and bar area. The river reach of the Brahmaputra from its confluence of Lohit, Dibang and Dihang to its confluence with the Tista river was studied from 1973 to 2009. The study was carried out using remotely sensed data from Landsat satellites at different dates. Discharge data synchronized with satellite data was collected by maintaining near-similar water level or discharge. Wavelet of the braided belt change was analysed to get the wavelet power and spatial extent of the changes. Finally, stream power was analysed from the average discharge data during the monsoon period to determine its effect on the instability of parameters considered. Results indicate that stream power does not directly relate to local changes in the braided belt or braiding index. However, with decrease in stream power, an increasing trend of bar area was found. Maximum wavelet power within a period showed a threshold behaviour at stream power of 5 W/km, beyond which the wavelet power raised sharply to a high value with increase in stream power. River response to the stream power was found at a global level rather than local level. Finally, a gradual decrease in stream power over time indicates the stable river reach. However, changes due to local bank erosion cannot be predicted using this analysis.Keywords
Braiding Index, Braided Belt, Plan Form, Stream Power.Full Text
References
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