期刊
CLIMATE DYNAMICS
卷 50, 期 9-10, 页码 3537-3555出版社
SPRINGER
DOI: 10.1007/s00382-017-3822-7
关键词
Attribution; Precipitation; Drought
资金
- European Union's Seventh Framework Programme for research, technological development, and demonstration under the EUCLEIA project [607085]
- European Research Council under the European Union's FP7/ERC Grant [338965-A2C2]
- US Department of Energy, Office of Science Innovative and Novel Computational Impact on Theory and Experiment (DOE INCITE) program
- Office of Biological and Environmental Research (BER)
- National Oceanic and Atmospheric Administration Climate Program Office
- NERC [ncas10008, NE/M005127/1, NE/M005909/1, ncas10005] Funding Source: UKRI
- Natural Environment Research Council [NE/M005909/1, ncas10005, ncas10009, NE/M005127/1, ncas10008, NE/N018001/1] Funding Source: researchfish
Summer 2012 was very wet in northern Europe, and unusually dry and hot in southern Europe. We use multiple approaches to determine whether anthropogenic forcing made the extreme European summer of 2012 more likely. Using a number of observation- and model-based methods, we find that there was an anthropogenic contribution to the extremes in southern Europe, with a qualitative consensus across all methodologies. There was a consensus across the methodologies that there has been a significant increase in the risk of hot summers in southern Europe with climate change. Most approaches also suggested a slight drying, but none of the results were statistically significant. The unusually wet summer in northern Europe was made more likely by the observed atmospheric circulation pattern in 2012, but no evidence was found for a long-term trend in circulation.
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