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Migrating Pools in Yangtze River
2002The severity and location of bank erosion and bed scour changes with the variation of water level. At low flows, the main flow thread tends to follow the concave bank. As the discharge increases, the flow tends to cut across the convex bar, to concentrate against concave bank only downstream the bend apex.
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Possible Influence of ENSO on Annual Maximum Streamflow of the Yangtze River, China
Journal of Hydrology, 2007Tong Jiang, Chong-Yu Xu, Yijin Wu
exaly
A New Era of Flood Control Strategies From the Perspective of Managing the 2020 Yangtze River Flood
Science China Earth Sciences, 2021exaly

