Model Assesses Flood Risks in Lower Yellow River

Higher Education Press

A new study published in Engineering presents an integrated model that evaluates flood risks to people's life and property in the lower Yellow River (LYR) under various floodplain management modes. With climate change increasing flood frequency and the LYR floodplains being densely populated, accurate flood risk assessment is crucial for effective management.

River flooding causes significant losses globally, and the LYR is no exception. Its complex channel–floodplain system and high sediment load pose challenges for flood risk quantification. Existing 2D morphodynamic models have limitations in simulating highly sediment-laden floods like those in the LYR, and previous flood risk evaluation methods lack comprehensiveness for this region.

The integrated model developed by the research team consists of two modules. The 2D morphodynamic module uses modified hydrodynamic governing equations to account for sediment-laden flows and bed deformation. It is solved using the finite volume method on unstructured meshes. The flood risk evaluation module calculates the hazard degrees of people, buildings, and crops on the floodplains. For example, the flood hazard degree of people is calculated based on an improved formula considering body buoyancy and flow velocity, while that of buildings and crops is determined through mechanical analysis and field surveys.

The model was validated using two real-world flood events in the LYR: the 2004 hyperconcentrated flood and the 2003 dike-breach induced flood. In the 2004 flood simulation, the model showed good accuracy in predicting sediment concentration, with a maximum underestimation of 9%. The 2003 dike-breach flood simulation also matched well with the field record in terms of inundation depth.

The researchers then applied the model to assess flood risks under three common floodplain management modes: the original mode (Scheme I), the construction of protection embankment mode (Scheme II), and the floodplain partition harnessing mode (Scheme III). They identified the vulnerable reach between Jiahetan (JHT) and Gaocun (GC) under a 1000-year return period extreme flood.

The results indicate that under Scheme I, most of the floodplains would be in medium and heavy inundation degrees. Scheme II alleviates the inundation extent, with more areas in slight inundation. Scheme III leads to most areas being in medium inundation. The high-risk area for people's life and property reduces by 21%–49% under Scheme II and 35%–93% under Scheme III compared to Scheme I.

This study provides a valuable tool for flood risk assessment in the LYR. While it doesn't consider all socio-economic factors like infrastructure support and exact costs, it offers a starting point for further research and decision-making in floodplain management.

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