Atmospheric circulation compounds anthropogenic warming and impacts of climate extremes in Europe

被引:36
|
作者
Faranda, Davide [1 ,2 ,3 ,4 ]
Messori, Gabriele [5 ,6 ,7 ]
Jezequel, Aglae [4 ,8 ]
Vrac, Mathieu [1 ,2 ]
Yiou, Pascal [1 ,2 ]
机构
[1] Univ Paris Saclay, Univ Versailles St Quentin En Yvelines, CNRS, Commissariat Energie Atom & Aux Energies Alternat, F-91191 Gif Sur Yvette, France
[2] Inst Pierre Simon Laplace, F-91191 Gif Sur Yvette, France
[3] London Math Lab, London W6 8RH, England
[4] Sorbonne Univ, Paris Sci & Lettres Res Univ, CNRS, Lab Meteorol Dynam IPSL,Ecole Normale Super,Ecole, F-75005 Paris, France
[5] Uppsala Univ, Ctr Nat Hazards & Disaster Sci, Dept Earth Sci, S-75236 Uppsala, Sweden
[6] Stockholm Univ, Dept Meteorol, S-10691 Stockholm, Sweden
[7] Stockholm Univ, Bolin Ctr Climate Res, S-10691 Stockholm, Sweden
[8] Ecole Ponts, F-77420 Marne La Vallee, France
基金
欧洲研究理事会;
关键词
climate change; atmospheric dynamics; European heatwaves; European windstorms; PATTERNS; ATTRIBUTION; GRADIENT; LOSSES; EVENTS;
D O I
10.1073/pnas.2214525120
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Diagnosing dynamical changes in the climate system, such as those in atmospheric circulation patterns, remains challenging. Here, we study 1950 to 2021 trends in the frequency of occurrence of atmospheric circulation patterns over the North Atlantic. Roughly 7% of atmospheric circulation patterns display significant occurrence trends, yet they have major impacts on surface climate. Increasingly frequent patterns drive heatwaves across Europe and enhanced wintertime storminess in the northern part of the continent. Over 91% of recent heatwave-related deaths and 33% of high-impact windstorms in Europe were concurrent with increasingly frequent atmospheric circulation patterns. While the trends identified are statistically significant, they are not necessarily anthropogenic. Atmospheric patterns which are becoming rarer correspond instead to wet, cool summer conditions over northern Europe and wet winter conditions over continental Europe. The combined effect of these circulation changes is that of a strong, dynamically driven year-round warming over most of the continent and large regional and seasonal changes in precipitation and surface wind.
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页数:8
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