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与全新世短期气候变率相关的反复洪水分布模式。

Recurring flood distribution patterns related to short-term Holocene climatic variability.

作者信息

Benito Gerardo, Macklin Mark G, Panin Andrei, Rossato Sandro, Fontana Alessandro, Jones Anna F, Machado Maria J, Matlakhova Ekaterina, Mozzi Paolo, Zielhofer Christoph

机构信息

Museo Nacional de Ciencias Naturales, CSIC, Serrano 115 bis, 28006 Madrid, Spain.

Centre for Catchment and Coastal Research and the River Basin Dynamics and Hydrology Research Group, Department of Geography and Earth Sciences, Aberystwyth University, Ceredigion SY23 3DB, UK.

出版信息

Sci Rep. 2015 Nov 9;5:16398. doi: 10.1038/srep16398.

Abstract

Millennial- and multi-centennial scale climate variability during the Holocene has been well documented, but its impact on the distribution and timing of extreme river floods has yet to be established. Here we present a meta-analysis of more than 2000 radiometrically dated flood units to reconstruct centennial-scale Holocene flood episodes in Europe and North Africa. Our data analysis shows a general increase in flood frequency after 5000 cal. yr BP consistent with a weakening in zonal circulation over the second half of the Holocene, and with an increase in winter insolation. Multi-centennial length phases of flooding in UK and central Europe correspond with periods of minimum solar irradiance, with a clear trend of increasing flood frequency over the last 1000 years. Western Mediterranean regions show synchrony of flood episodes associated with negative phases of the North Atlantic Oscillation that are out-of-phase with those evident within the eastern Mediterranean. This long-term flood record reveals complex but geographically highly interconnected climate-flood relationships, and provides a new framework to understand likely future spatial changes of flood frequency.

摘要

全新世期间千年和数百年尺度的气候变率已有充分记录,但其对极端河流洪水的分布和发生时间的影响尚未确定。在此,我们对2000多个经放射性测年的洪水单元进行了荟萃分析,以重建欧洲和北非百年尺度的全新世洪水事件。我们的数据分析表明,公元前5000年校准年之后洪水频率总体增加,这与全新世后半期纬向环流减弱以及冬季日照增加相一致。英国和中欧多百年长度的洪水期与太阳辐照度最低的时期相对应,在过去1000年里洪水频率有明显增加的趋势。西地中海地区洪水事件与北大西洋涛动的负相位同步,这与东地中海地区明显不同步。这一长期洪水记录揭示了复杂但在地理上高度相互关联的气候-洪水关系,并为理解未来洪水频率可能的空间变化提供了一个新框架。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6846/4637870/21c8259ac414/srep16398-f1.jpg

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