Authors: P. J. Roldán-Gómez, M. G. Donat, G. Marcet-Carbonell, D. M. Smith
First published: 30 June 2026
Abstract
Compared to observations, climate models underestimate the recent increase of European summer temperatures, due to an underestimation of Quasi-stationary Rossby Wave (QSW) trends over Europe. This is partially due to unpredictable internal variability and partially due to an underestimation of the predictable signal in response to external forcings. The analysis of a large ensemble of historical simulations shows that forcing factors generate changes in QSW and European summer temperatures consistent with those from observations but with a lower magnitude, making most of the observed changes predictable by the models through a signal adjustment. The analysis of single forcing experiments shows a major contribution of aerosols starting from 1980, when the reduction of sulfate aerosol emissions over Europe is associated with a longitudinal temperature asymmetry, which alters the atmospheric circulation. These results further demonstrate the need to account for model errors to best estimate past and future changes in climate.
Plain Language Summary
In the last decades, summer temperatures over Europe increased more than over other regions, associated with a reduction of particle emissions. In particular, the reduction of sulfate emissions over Europe starting from 1980 is associated with changes in the atmospheric circulation and an additional warming over Europe. Climate models reproduce this behavior, but with a magnitude much smaller than that of observations. If the outputs of the models are corrected to compensate for this underestimation, the increase in European summer temperatures becomes largely predictable. Our results highlight the need to take model error into account to estimate past and future climate change.
Source: AGU