Rapid attribution analysis of the extraordinary heat wave on the Pacific coast of the US and Canada in June 2021

S. Philip, S. Kew, G. J. van Oldenborgh, F. Anslow, S. Seneviratne, R. Vautard, D. Coumou, K. Ebi, J. Arrighi, Roop K. Singh, M. V. van Aalst, Carolina Pereira Marghidan, M. Wehner, Wenchang Yang, Sihan Li, D. Schumacher, M. Hauser, R. Bonnet, Linh N. Luu, F. Lehner, N. Gillett, Jordis S. Tradowsky, G. Vecchi, Christopher E. Rodell, R. Stull, Rosie Howard, F. Otto
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引用次数: 21

Abstract

Abstract. Towards the end of June 2021, temperature records were broken by several degrees Celsius in several cities in the Pacific Northwest areas of the US and Canada, leading to spikes in sudden deaths and sharp increases in emergency calls and hospital visits for heat-related illnesses. Here we present a multi-model, multi-method attribution analysis to investigate the extent to which human-induced climate change has influenced the probability and intensity of extreme heat waves in this region. Based on observations, modelling and a classical statistical approach, the occurrence of a heat wave defined as the maximum daily temperature (TXx) observed in the area 45–52∘ N, 119–123∘ W, was found to be virtually impossible without human-caused climate change. The observed temperatures were so extreme that they lay far outside the range of historical temperature observations. This makes it hard to state with confidence how rare the event was. Using a statistical analysis that assumes that the heat wave is part of the same distribution as previous heat waves in this region led to a first-order estimation of the event frequency of the order of once in 1000 years under current climate conditions. Using this assumption and combining the results from the analysis of climate models and weather observations, we found that such a heat wave event would be at least 150 times less common without human-induced climate change. Also, this heat wave was about 2 ∘C hotter than a 1-in-1000-year heat wave would have been in 1850–1900, when global mean temperatures were 1.2 ∘C cooler than today. Looking into the future, in a world with 2 ∘C of global warming (0.8 ∘C warmer than today), a 1000-year event would be another degree hotter. Our results provide a strong warning: our rapidly warming climate is bringing us into uncharted territory with significant consequences for health, well-being and livelihoods. Adaptation and mitigation are urgently needed to prepare societies for a very different future.
2021年6月美国和加拿大太平洋沿岸异常热浪的快速归因分析
摘要2021年6月底,美国和加拿大太平洋西北部地区的几个城市的气温记录被打破了几摄氏度,导致猝死人数激增,与高温相关的疾病的紧急电话和医院就诊人数急剧增加。在这里,我们提出了一个多模型、多方法的归因分析,以调查人类引发的气候变化对该地区极端热浪发生的概率和强度的影响程度。根据观测、建模和经典统计方法,热浪的发生被定义为在45-52∘地区观测到的最高日温度(TXx) N、 119–123∘ W、 如果没有人为造成的气候变化,几乎是不可能的。观测到的温度非常极端,远远超出了历史温度观测的范围。这使得人们很难自信地说出这一事件是多么罕见。通过使用统计分析,假设热浪与该地区以前的热浪具有相同的分布,得出了在当前气候条件下1000年一次的事件频率的一阶估计。利用这一假设,并结合气候模型分析和天气观测的结果,我们发现,如果没有人类引起的气候变化,这种热浪事件的发生率将至少降低150倍。此外,这股热浪约为2 ∘1850年至1900年,全球平均气温为1.2摄氏度,比千年一遇的热浪还要热 ∘C比今天凉爽。展望未来,在一个有2 ∘全球变暖的C(0.8 ∘比今天高出摄氏度),一个1000年的事件将再热一度。我们的研究结果提供了一个强有力的警告:我们迅速变暖的气候正在将我们带入一个未知的领域,对健康、福祉和生计产生重大影响。迫切需要适应和缓解气候变化,使社会为一个截然不同的未来做好准备。
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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