Articles | Volume 39
https://doi.org/10.5194/adgeo-39-15-2014
https://doi.org/10.5194/adgeo-39-15-2014
01 Apr 2014
 | 01 Apr 2014

Relative role of bed roughness change and bed erosion on peak discharge increase in hyperconcentrated floods

W. Li, Z. B. Wang, D. S. van Maren, H. J. de Vriend, and B. S. Wu

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Cited articles

Cao, Z. X., Pender, G., Wallis, S., and Carling, P.: Computational dam-break hydraulics over erodible sediment bed, J. Hydraul. Eng.-ASCE, 130, 689–703, 2004.
Cao, Z. X., Pender, G., and Carling, P.: Shallow water hydrodynamic models for hyperconcentrated sediment-laden floods over erodible bed, Adv. Water Res., 29, 546–557, 2006.
He, L., Duan, J. G., Wang, G. Q., and Fu, X. D.: Numerical simulation of unsteady hyperconcentrated sediment-laden flow in the Yellow River, J. Hydraul. Eng.-ASCE, 138, 958–969, 2012.
Jiang, E. H., Zhao, L. J., and Wei, Z. L.: Mechanism of flood peak increase along the Lower Yellow River and its verification, J. Hydraul. Eng., 37, 1454–1459, 2006 (in Chinese).
Li, G. Y.: Analysis on mechanism of peak discharge increasing during flood routing in lower reaches of Yellow River, J. Hydraul. Eng., 39, 511–517, 2008 (in Chinese).