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从长期角度重新审视近期欧洲干旱。

Revisiting the recent European droughts from a long-term perspective.

机构信息

Czech University of Life Sciences, Faculty of Environmental Sciences, Prague, 169 00, Czech Republic.

UFZ-Helmholtz Centre for Environmental Research, Leipzig, 04318, Germany.

出版信息

Sci Rep. 2018 Jun 22;8(1):9499. doi: 10.1038/s41598-018-27464-4.

Abstract

Early 21st-century droughts in Europe have been broadly regarded as exceptionally severe, substantially affecting a wide range of socio-economic sectors. These extreme events were linked mainly to increases in temperature and record-breaking heatwaves that have been influencing Europe since 2000, in combination with a lack of precipitation during the summer months. Drought propagated through all respective compartments of the hydrological cycle, involving low runoff and prolonged soil moisture deficits. What if these recent droughts are not as extreme as previously thought? Using reconstructed droughts over the last 250 years, we show that although the 2003 and 2015 droughts may be regarded as the most extreme droughts driven by precipitation deficits during the vegetation period, their spatial extent and severity at a long-term European scale are less uncommon. This conclusion is evident in our concurrent investigation of three major drought types - meteorological (precipitation), agricultural (soil moisture) and hydrological (grid-scale runoff) droughts. Additionally, unprecedented drying trends for soil moisture and corresponding increases in the frequency of agricultural droughts are also observed, reflecting the recurring periods of high temperatures. Since intense and extended meteorological droughts may reemerge in the future, our study highlights concerns regarding the impacts of such extreme events when combined with persistent decrease in European soil moisture.

摘要

21 世纪早期的欧洲干旱被广泛认为异常严重,严重影响了广泛的社会经济部门。这些极端事件主要与自 2000 年以来欧洲不断上升的气温和破纪录的热浪有关,再加上夏季降水不足。干旱通过水文循环的各个环节传播,包括低径流量和长时间的土壤水分亏缺。如果这些最近的干旱并不像之前认为的那么极端呢?利用过去 250 年重建的干旱数据,我们表明,虽然 2003 年和 2015 年的干旱可能被认为是植被期降水亏缺驱动的最极端干旱,但它们在长期的欧洲范围内的空间范围和严重程度并不罕见。这一结论在我们对三种主要干旱类型——气象(降水)、农业(土壤水分)和水文(网格尺度径流)干旱的同时调查中显而易见。此外,还观察到土壤水分前所未有的干燥趋势和农业干旱频率的相应增加,反映出高温的反复出现。由于强烈和持久的气象干旱可能在未来再次出现,因此,我们的研究强调了在与欧洲土壤水分持续减少相结合的情况下,对这种极端事件的影响的担忧。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6b7f/6015036/d9ee019bf55f/41598_2018_27464_Fig1_HTML.jpg

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