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、降雨与河道径流共同作用引发的复合型洪水对基础设施和社区构成重大威胁——艾萨克与哈维飓风已充分证明了这一点。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的模型虽能捕捉洪水驱动因子的共现性,却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石的联合概率方法(JPM),从未被正式扩展至涵盖水文驱动因子——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。本文通过将JPM理论扩展至水文过程,量化热带与非热带风暴中复合洪水深度的发生概率。该扩展方法整合了降雨场、前期土壤湿度、基流以及海岸风暴潮,实现了:(1)以洪水深度作为水文与海岸驱动因子联合分布响应的统计描述;(2)基于超越概率的CFTZ统计界定;(3)针对特定重现期洪水深度的设计风暴系统识别,突破了仅依赖驱动因子可能性的传统设计范式。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界定面积的两倍以上,且复合相互作用使洪水深度最大增加2.25英尺。这一扩展的JPM为复合洪水风险评估与规划提供了概率理论基础。