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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.
openaire +1 more source
Possible influence of ENSO on annual maximum streamflow of the Yangtze River, China
Journal of Hydrology, 2007Tong Jiang, Chong-Yu Xu, Yijin Wu
exaly
Sediment and runoff changes in the Yangtze River basin during past 50 years
Journal of Hydrology, 2006Tong Jiang +2 more
exaly
Interactions of the Yangtze river flow and hydrologic processes of the Poyang Lake, China
Journal of Hydrology, 2007Qi Hu, Tong Jiang
exaly
Provenance and time constraints on the formation of the first bend of the Yangtze River
Geochemistry, Geophysics, Geosystems, 2012Yong Zheng, Marc Caffee
exaly

