基于贝叶斯推断的长江口复合洪水潜在风险

Compound flooding potential in the Yangtze Estuary based on Bayesian inference

  • 摘要: 在全球持续变暖背景下,河口复合洪水事件频发。台风、强降雨、河道洪水和风暴潮等灾害因子的影响相互叠加,严重威胁沿海城市的防洪安全。基于观测资料和数值模拟重构了1959—2020年复合洪水灾害因子数据集,采用基于贝叶斯推断的Copula方法,分析了长江口风暴潮“二碰头”“三碰头”事件的风险性及其不确定性。结果表明:1988—2020年长江口徐六泾站年极值高水位呈明显下降趋势,主要原因是风暴潮强度的减弱;长江口地区极端风暴潮高潮位与强降雨的遭遇风险较高,重现期为89 a,而大通径流与台风及其伴生事件在统计上近似独立;忽视变量间的相关性会显著低估复合洪水灾害的风险,且随着灾害因子重现期的延长低估愈加明显;长江口风暴潮“二碰头”事件风险低估幅度高达77.7%;自然变化导致的风暴潮“二碰头”重现期不确定性为− 12.6%, 16.3%;相较于风暴潮和依赖性,降雨是长江口复合洪水风险不确定性的主要来源。

     

    Abstract: In the context of escalating global warming, the compound effects of typhoons, intense rainfall, riverine flooding, and storm surges have led to a heightened frequency of compound flood events, posing considerable threats to the flood control security of coastal cities. Using observational data and numerical simulations, a comprehensive dataset encompassing compound flood hazard factors from 1959 to 2020 has been reconstructed. A Bayesian inference-based Copula approach is employed to evaluate the risks and uncertainties associated with double and triple compound events of storm surge in the Yangtze Estuary. The results indicate that, from 1988 to 2020, the annual extreme high water level at the Xuliujing station in the Yangtze Estuary exhibited a significant downward trend, primarily due to the weakening intensity of storm surges. The coincidence risk between extreme storm tide levels and heavy rainfall in the Yangtze Estuary is relatively high, with a return period of 89 years. Conversely, the Datong runoff is statistically independent of typhoons and their associated events. Neglecting the dependency between variables would lead to an underestimation of compound flood disaster risks, which will become more pronounced as the return period of hazard factors increases. For instance, the risk underestimation of double compound events of storm surge reaches up to 77.7%. The uncertainty in the return period of double compound events of storm surge due to natural variability ranges from − 12.6% to 16.3%. Compared to extreme storm tide levels and dependence, precipitation is the major contributor to the uncertainty of compound flooding.

     

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