Braided reaches of large rivers in alluvial plains show major morphological changes, particularly the external bank erosion, due to the flood events. This paper highlights the bank erosion and channel evolution induced by eleven different flood events in a 7-km long reach of the River Chenab, Pak...
Enlace original:
https://cgspace.cgiar.org/handle/10568/76275
Ashraf, M.
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Bhatti, Muhammad Tousif
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Shakir, A.S.
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[River bank erosion and channel evolution in sand-bed braided reach of River Chenab: role of floods during different flow regimes]
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River bank erosion and channel evolution in sand-bed braided reach of River Chenab: role of floods during different flow regimes
