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Simulation of Flood Propagation on Channel of the Yellow River by Convection-Diffusion Equation

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Taming the Yellow River: Silt and Floods

Part of the book series: The GeoJournal Library ((GEJL,volume 13))

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Abstract

The lower Yellow River bed is higher than the ground surface on both banks. It is known as the famous suspended river. Because of this, every breach during flooding causes more disasters than any other river in China. Flood threats to the lower Yellow River come from storms in the middle reaches. The main storm regions are located between Shanxi Province and Shaanxi Province in the basins of its major tributaries of Jin, Wei, Lou, and around the main course from Sannmenxia and Huayuankou, including the Yi, Lou, and Qin tributaries.

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References

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  2. Liang Jiyang, System analysis of flood wave, in Channel Yellow River, 1985, 5.

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© 1989 Kluwer Academic Publishers

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Jiyang, L., Changming, L. (1989). Simulation of Flood Propagation on Channel of the Yellow River by Convection-Diffusion Equation. In: Brush, L.M., Wolman, M.G., Bing-Wei, H. (eds) Taming the Yellow River: Silt and Floods. The GeoJournal Library, vol 13. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-2450-5_15

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  • DOI: https://doi.org/10.1007/978-94-009-2450-5_15

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-94-010-7605-0

  • Online ISBN: 978-94-009-2450-5

  • eBook Packages: Springer Book Archive

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