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全球气候和人为变化导致暴洪径流极值的大幅增加。

Large increase in global storm runoff extremes driven by climate and anthropogenic changes.

机构信息

State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, 430072, China.

Department of Earth and Environmental Engineering, Columbia University, New York, NY, 10027, USA.

出版信息

Nat Commun. 2018 Oct 22;9(1):4389. doi: 10.1038/s41467-018-06765-2.

Abstract

Weather extremes have widespread harmful impacts on ecosystems and human communities with more deaths and economic losses from flash floods than any other severe weather-related hazards. Flash floods attributed to storm runoff extremes are projected to become more frequent and damaging globally due to a warming climate and anthropogenic changes, but previous studies have not examined the response of these storm runoff extremes to naturally and anthropogenically driven changes in surface temperature and atmospheric moisture content. Here we show that storm runoff extremes increase in most regions at rates higher than suggested by Clausius-Clapeyron scaling, which are systematically close to or exceed those of precipitation extremes over most regions of the globe, accompanied by large spatial and decadal variability. These results suggest that current projected response of storm runoff extremes to climate and anthropogenic changes may be underestimated, posing large threats for ecosystem and community resilience under future warming conditions.

摘要

极端天气对生态系统和人类社区造成了广泛的有害影响,其中由暴洪引发的死亡人数和经济损失比任何其他与恶劣天气相关的灾害都要多。由于气候变暖以及人为因素的改变,归因于风暴径流极端事件的暴洪在全球范围内预计将变得更加频繁和具有破坏性,但之前的研究尚未检验这些风暴径流极端事件对地表温度和大气水汽含量自然和人为驱动变化的响应。在这里,我们表明,在大多数地区,风暴径流极端事件的增加速度高于克劳修斯-克拉珀龙缩放所表明的速度,且在全球大多数地区,这些增加速度接近或超过降水极端事件的增加速度,同时还伴随着较大的空间和年代际可变性。这些结果表明,目前对气候和人为变化的风暴径流极端事件的响应可能被低估了,这对未来变暖条件下生态系统和社区的恢复力构成了巨大威胁。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6c9b/6197252/04c0846b3960/41467_2018_6765_Fig1_HTML.jpg

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