The extremely warm summer of 2018 in Sweden – set in a historical context

R. Wilcke, E. Kjellström, Changgui Lin, D. Matei, A. Moberg, E. Tyrlis
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引用次数: 27

Abstract

Abstract. Two long-lasting high pressure systems in summer 2018 lead to long lasting heat waves over Scandinavia and other parts of Europe and an extended summer period with devastating impacts on agriculture, infrastructure and human life. We use five climate model ensembles and the unique 263 year long Stockholm temperature time series along with a composite 150 year long time series for whole Sweden to set the latest heat-wave in summer 2018 in historical perspective. With 263 years we are able to grasp the pre-industrial time well and see a clear upward trend in temperature itself as well as heat wave indicators. With five climate model ensembles providing 20 580 simulated summers representing the latest 70 years, we analyse the likelihood of such a heat event and how unusual the 2018 Swedish summer actually was. We find that conditions as those observed in summer 2018 show up in all climate model ensembles. An exception is the monthly mean temperature for May for which 2018 was warmer than any member in one of the five climate model ensembles. However, even if the ensembles generally hold individual years like 2018, the comparison shows that such conditions are rare. For the indices assessed here, anomalies such as observed in 2018 occur maximally in 5 % of the ensemble members, sometimes even in less than 1 %. For all indices evaluated we find that probabilities of a summer like in 2018 have increased from relatively low values for the one ensemble extending back to 1861–90 and for all five ensembles including 1951–80 to the most recent decades (1989–2018). An implication is that anthropogenic climate change has strongly increased the probability of a warm summer such as the one observed 2018 to occur in Sweden. Despite this, we still find such summers also in the pre-industrial climate, however, with a lower probability.
2018年瑞典极端温暖的夏天——以历史背景为背景
摘要2018年夏季的两个持久高压系统导致斯堪的纳维亚半岛和欧洲其他地区持续的热浪,并延长了夏季,对农业、基础设施和人类生活造成了破坏性影响。我们使用五个气候模型组合和独特的263年斯德哥尔摩温度时间序列,以及整个瑞典150年的复合时间序列,从历史角度设定了2018年夏季最新的热浪。263年,我们能够很好地掌握工业化前的时间,并看到温度本身以及热浪指标的明显上升趋势。通过五个气候模型集合,提供了代表最近70年的20580个模拟夏季,我们分析了这种高温事件的可能性,以及2018年瑞典夏季的实际不寻常程度。我们发现,2018年夏季观测到的情况出现在所有气候模型集合中。一个例外是,2018年5月的月平均温度比五个气候模型组合中的任何一个成员都要高。然而,即使整体通常会出现像2018年这样的个别年份,比较也表明这种情况很少见。对于这里评估的指数,2018年观测到的异常最多发生在5%的整体成员中,有时甚至不到1%。对于评估的所有指数,我们发现2018年类似夏季的概率从1861-90年的一个整体的相对低值,以及包括1951-80年在内的所有五个整体到最近几十年(1989-2018年)的相对低值有所增加。这意味着,人为气候变化大大增加了瑞典出现2018年这样一个温暖夏季的可能性。尽管如此,我们仍然在工业化前的气候中发现这样的夏天,只是概率较低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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