资源环境科技发展态势分析平台

The Northern European summer of 2018 was the driest for 35 years with resulting impacts on health, agriculture, energy, and water resources. Here we show that this rainfall anomaly was well predicted by a real-time seasonal forecast. An anticyclonic circulation anomaly was correctly forecast over the North Sea and Scandinavia in 2018 and also in the 1976 record dry summer. In both these exceptionally dry summers, a similar tripole anomaly pattern of North Atlantic sea surface temperatures was present. We perform perturbation experiments that reveal significant circulation, and European rainfall, responses due to changes in the Atlantic meridional temperature gradient. However, consistent with previous work, we find that the model dynamical response is weak relative to that observed and hence large ensembles are required to produce sufficiently skilful predictions. This case study illustrates the potential for the development of summer European climate services.