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Improved Methods for Estimating Flood Depth Exceedances Within Storm Surge Protection Systems

机译:估计风暴潮保护系统中洪水深度超过的改进方法

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Contemporary studies conducted by the U.S. Army Corps of Engineers estimate probability distributions of flooding on the interior of ring levee systems by estimating surge exceedances at points along levee system boundaries, calculating overtopping volumes generated by this surface, then passing the resulting volumes of water through a drainage model to calculate interior flood depths. This approach may not accurately represent the exceedance probability of flood depths within the system interior; a storm producing 100-year surge at one point is unlikely to simultaneously produce 100-year surge levels everywhere around the system exterior. A conceptually preferred approach estimates surge and waves associated with a large set of storms. Each storm is run through the interior model separately, and the resulting flood depths are weighted by a parameterized likelihood of each synthetic storm. This results in an empirical distribution of flood depths accounting for geospatial variation in any individual storm's characteristics. This method can also better account for the probability of levee breaches or other system failures. The two methods can produce different estimates of flood depth exceedances and damage when applied to storm surge flooding in coastal Louisiana. Even differences in flood depth exceedances of less than 0.2 m can still produce large differences in projected damage. This article identifies and discusses differences in estimated flood depths and damage produced by each method within multiple Louisiana protection systems. The novel coupled dynamics approach represents a step toward enabling risk-based design standards.
机译:美国陆军工程兵团进行的当代研究通过估算沿堤防系统边界沿点的浪涌超出量,计算该表面产生的越过顶部的水量,然后将所得的水量通过水流,估算环形堤防系统内部洪水的概率分布。排水模型以计算内部洪水深度。这种方法可能无法准确地表示系统内部洪水泛滥的可能性。在某一时刻产生100年电涌的风暴不太可能同时在系统外部各处同时产生100年电涌水平。从概念上讲,首选方法可估算与大量风暴相关的浪涌和海浪。每个风暴单独通过内部模型运行,并且通过每个合成风暴的参数化可能性对所得的洪水深度进行加权。这导致了洪水深度的经验分布,这说明了任何单个风暴特征中的地理空间变化。此方法还可以更好地说明堤防违规或其他系统故障的可能性。当将两种方法应用于路易斯安那州沿海地区的风暴潮洪水时,可以得出不同的洪水深度超标和破坏估计。即使洪水深度的差异小于0.2 m,仍可能在预计破坏中产生较大差异。本文确定并讨论了在多个路易斯安那州保护系统中,每种方法产生的估计洪水深度和破坏的差异。新颖的耦合动力学方法代表了朝着基于风险的设计标准迈出的一步。

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