River bank erosion and channel evolution in sand-bed braided reach of River Chenab: role of floods during different flow regimes
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, Pakist...
| Main Authors: | , , |
|---|---|
| Format: | Journal Article |
| Language: | Inglés |
| Published: |
Springer
2016
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| Subjects: | |
| Online Access: | https://hdl.handle.net/10568/76275 |
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