Bank erosion under the impacts of fluvial erosion, frost heaving/freeze-thaw process of rivers in seasonal frozen regions
J Yang, D Jia, B Zhai, X Chen, J Wang - Heliyon, 2024 - cell.com
Bank erosion is a key feature of channel evolution in alluvial rivers, and will occur under the
combined effect of hydraulic erosion and frost heave/freeze-thaw process of rivers in …
combined effect of hydraulic erosion and frost heave/freeze-thaw process of rivers in …
Reach scale channel planform dynamics of transboundary River Jaldhaka within Himalayan Foreland Basin
The slopes of Himalayan piedmont and foothill plain are being modified by the Himalayan
origin river systems. In this study, spatiotemporal dynamics of channel planform of braided …
origin river systems. In this study, spatiotemporal dynamics of channel planform of braided …
Fluvio-hydrological drivers largely control the morphology and stability of channel bars in the transboundary Himalayan River Jaldhaka
This present study focused on the spatiotemporal morphological dynamics and stability of
channel bars of a tropical braided River Jaldhaka. Eleven sub-reaches, ten randomly …
channel bars of a tropical braided River Jaldhaka. Eleven sub-reaches, ten randomly …