Over Western and Central Europe, the temperature has risen more sharply since 1980 than projected in the regional climate models that form the basis for CH2018. There are two main explanations for this: On the one hand, air quality - worldwide, but also in Europe - has improved significantly since the 1980s, meaning that the concentration of aerosols in the air has decreased. As a result, less sunlight is scattered back, causing the atmosphere to heat up more (brightening effect). This was not directly taken into account in previous models (e.g. Wild, 2012). On the other hand, natural fluctuations in the climate may play a significant role.
The Swiss climate scenarios CH2018 are currently being revised as part of the "Climate CH2025" project. In the new scenarios, the effects of circulation changes and aerosol emissions are also to be better taken into account so that the model projections better reflect the observations of the past and present.
According to the provisional results, the core statements of CH2018 will not change qualitatively: In Switzerland, we expect drier summers, an increase in extreme precipitation, more hot days and heatwaves and winters with less snow in the future. Quantitatively, the local changes expected in the future for given scenarios will probably be more pronounced.
The final quantifications will be published in the Climate CH2025 products at the end of the project (end of 2025).
References:
Schumacher, D.L., Singh, J., Hauser, M. et al. Exacerbated summer European warming not captured by climate models neglecting long-term aerosol changes. Commun Earth Environ 5, 182 (2024). https://doi.org/10.1038/s43247-024-01332-8
Wild, M. (2012). Enlightening global dimming and brightening. Bulletin of the American Meteorological Society, 93(1), 27-37.