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Climate change exacerbates hurricane flood hazards along US Atlantic and Gulf Coasts in spatially varying patterns

机译:气候变化以空间变化的方式加剧了美国大西洋沿岸和墨西哥湾沿岸的飓风洪水灾害

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摘要

One of the most destructive natural hazards, tropical cyclone (TC)–induced coastal flooding, will worsen under climate change. Here we conduct climatology–hydrodynamic modeling to quantify the effects of sea level rise (SLR) and TC climatology change (under RCP 8.5) on late 21st century flood hazards at the county level along the US Atlantic and Gulf Coasts. We find that, under the compound effects of SLR and TC climatology change, the historical 100-year flood level would occur annually in New England and mid-Atlantic regions and every 1–30 years in southeast Atlantic and Gulf of Mexico regions in the late 21st century. The relative effect of TC climatology change increases continuously from New England, mid-Atlantic, southeast Atlantic, to the Gulf of Mexico, and the effect of TC climatology change is likely to be larger than the effect of SLR for over 40% of coastal counties in the Gulf of Mexico.
机译:热带气旋(TC)引起的沿海洪灾是最具破坏力的自然灾害之一,在气候变化下会恶化。在这里,我们进行气候-流体动力学建模,以量化海平面上升(SLR)和TC气候变化(根据RCP 8.5)对21世纪末美国大西洋沿岸和墨西哥湾沿岸县级洪水灾害的影响。我们发现,在SLR和TC气候变化的复合影响下,历史上100年的洪水位将在新英格兰和大西洋中部地区每年发生一次,而在东南大西洋和墨西哥湾地区的后期将每1–30年发生一次21世纪。从新英格兰,大西洋中部,东南大西洋到墨西哥湾,TC气候变化的相对影响持续增加,并且在超过40%的沿海县中,TC气候变化的影响可能大于SLR的影响在墨西哥湾。

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