Compound flooding from the combined effects of extreme storm surge, rainfall, and river flows poses significant risks to infrastructure and communities -- as demonstrated by hurricanes Isaac and Harvey. Yet, existing methods to quantify compound flood risk lack a unified probabilistic basis. Copula-based models capture the co-occurrence of flood drivers but not the likelihood of the flood response, while coupled hydrodynamic models simulate interactions but lack a probabilistic characterization of compound flood extremes. The Joint Probability Method (JPM), the foundation of coastal surge risk analysis, has never been formally extended to incorporate hydrologic drivers -- leaving a critical gap in quantifying compound flood risk and the statistical structure of compound flood transition zones (CFTZs). Here, we extend the JPM theory to hydrologic processes for quantifying the likelihood of compound flood depths across both tropical and non-tropical storms. This extended methodology incorporates rainfall fields, antecedent soil moisture, and baseflow alongside coastal storm surge, enabling: (1) a statistical description of the flood depth as the response to the joint distribution of hydrologic and coastal drivers, (2) a statistical delineation of the CFTZ based on exceedance probabilities, and (3) a systematic identification of design storms for specified return period flood depths, moving beyond design based solely on driver likelihoods. We demonstrate this method around Lake Maurepas, Louisiana. Results show a CFTZ more than double the area of prior event-specific delineations, with compound interactions increasing flood depths by up to 2.25 feet. This extended JPM provides a probabilistic foundation for compound flood risk assessment and planning.
翻译:极端风暴潮、降雨与河道流量的共同作用引发的复合洪水对基础设施和社区构成重大风险——如艾萨克飓风和哈维飓风所证明。然而,现有量化复合洪水风险的方法缺乏统一的概率基础。基于Copula的模型能捕捉洪水驱动因子的共现性,但无法表征洪水响应的可能性;而耦合水动力模型虽能模拟相互作用,却缺乏对复合洪水极值的概率化描述。作为海岸风暴潮风险分析基础的联合概率方法(JPM),从未被正式扩展以纳入水文驱动因子——这导致在量化复合洪水风险及复合洪水过渡带(CFTZ)统计结构方面存在关键空白。本文扩展JPM理论至水文过程,用于量化热带与非热带风暴中复合洪水深度的发生概率。该扩展方法将降雨场、前期土壤湿度和基流与海岸风暴潮相结合,实现了:(1)将洪水深度作为水文与海岸驱动因子联合分布的响应进行统计描述;(2)基于超越概率对CFTZ进行统计划定;(3)系统识别特定重现期洪水深度的设计风暴,超越仅基于驱动因子可能性的传统设计方法。我们在路易斯安那州莫雷帕斯湖区域验证了该方法。结果表明,CFTZ范围超过以往事件特定划定面积的两倍,且复合相互作用使洪水深度最高增加2.25英尺。该扩展JPM为复合洪水风险评估与规划提供了概率理论基础。