气候变化加剧了近期热带气旋造成的复合洪水

L. E. Grimley, K. E. Hollinger Beatty, A. Sebastian, S. Bunya, G. M. Lackmann
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引用次数: 0

摘要

热带气旋(TCs)造成了巨大的破坏,引起了人们对气候变化如何放大其影响的担忧。然而,将TC特征(风、降水)的变化与洪水灾害和暴露的变化联系起来,特别是由于多个驱动因素的相互作用,是具有挑战性的。在这项研究中,我们使用高分辨率的基于物理的模型来研究北卡罗来纳州和南卡罗来纳州最近三个tc的洪水在4摄氏度的变暖下会如何变化。径流过程是当前和未来总洪水范围的最大贡献者。然而,复合过程的相对贡献在未来会增加,扩大到上游和洪泛区以外,而径流过程以前是孤立发生的。复合洪水暴露总面积增加了65%,洪水深度增加了0.8 m,突出了模拟复合过程在TC洪水暴露评估中的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Climate change exacerbates compound flooding from recent tropical cyclones

Climate change exacerbates compound flooding from recent tropical cyclones
Tropical cyclones (TCs) generate substantial damage raising concerns about how climate change may amplify their impacts. However, linking changes in TC characteristics (wind, precipitation) to shifts in flood hazards and exposure, particularly due to the interaction of multiple drivers, is challenging. In this study, we use highly resolved physics-based models to investigate how flooding from three recent TCs in North and South Carolina would change under 4 degrees Celsius of warming. Runoff processes are the largest contributor to the total flood extent in both the present and future. However, the relative contribution of compound processes increases in the future, expanding upriver and beyond the floodplain where runoff processes previously occurred in isolation. The total area exposed to compound flooding increases by 65% and flood depths in these areas increase by 0.8 m highlighting the importance of simulating compound processes in TC flood exposure assessment.
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