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Quantitative assessment of inundation risks from physical contributors associated with future storm surges: a case study of Typhoon Maemi (2003)

机译:与未来风暴飙升有关的物理贡献者的泛滥风险的定量评估 - 以台风MAEMI为例(2003)

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摘要

Future storm-induced inundation risks were assessed by performing storm surge modeling based on Typhoon Maemi (2003) under the generic climate change scenarios proposed by IPCC AR5. The three physical factors governing the projected aggravation of inundation damage in a coastal basin (i.e., sea-level rise (SLR), direct runoff (DR) and tropical cyclones (TCs)) were defined and considered in the modeling both individually and in combination. With the application of a coupled hydrodynamic-hydrologic model, the inundation extent during the storm event under both current and year 2100 climate conditions was evaluated, and the impact of each factor on the inundation risk was identified. The intercomparison among the results revealed that SLR was the most influential single flooding driver aggravating the future inundation risk, and TC intensification was two-thirds as influential as SLR. However, DR was predicted to make a nearly negligible contribution and to have a minimal impact despite its significant projected increase in the future. Apart from the contributions of these three factors to aggravating the inundation level, the ways in which they affected the inundation risk were quite distinct. Additionally, the result considering both SLR and TC intensification demonstrated that nonlinear interactions between these factors can occur and further amplify the inundation damage. Finally, it was revealed that, depending on the level of the climate change projection, future storms with intensified rainfall and TC properties are likely to cause the maximum projected inundation damage in the study area to increase by up to 28.7% in inundation extent and by 236.6% in inundation volume relative to the current conditions without altering the spatial pattern of the inundation depth distribution.
机译:根据IPCC AR5提出的通用气候变化情景,通过基于台风Maemi(2003)进行风暴浪涌建模来评估未来的风暴造型的洪水风险。在沿海盆地(即海平面上升(SLR),直接径流(DR)和热带气旋(TCS)中定义和考虑单独和组合地区。随着耦合流体动力学 - 水文模型的应用,评估了在当前和2100年气候条件下的暴风事件期间的淹没程度,并确定了每个因素对淹没风险的影响。结果的竞争结果显示,SLR是加剧未来泛滥风险的最具影响力的单洪水驱动因素,而TC强化是二分之二的二分之二,如SLR。然而,博士预计,尽管未来的重大预计增加,但仍有几乎可忽略的贡献并具有最小的影响。除了这三个因素的贡献之外,对惩罚级别加剧,他们影响淹没风险的方式都是如此。另外,考虑SLR和TC强化的结果表明,这些因素之间的非线性相互作用可能发生并进一步扩增淹没损伤。最后,据透露,根据气候变化投影的水平,降雨量和TC性能的未来风暴可能会导致研究区域的最大预测淹没损害,在泛滥范围内增加了28.7%。相对于当前条件的淹没体积236.6%而不改变淹没深度分布的空间模式。

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