The variability of the sea level pressure in the North Atlantic sector is the most important driver of weather and climate in Europe. The main mode of this variability, the North Atlantic Oscillation (NAO), explains up to 50% of the total variance. Other modes, known as the Scandinavian index, East Atlantic, and East Atlantic/West Russian pattern, complement the variability of the sea level pressure, thereby influencing the European climate. It has been shown previously that a seasonal prediction system with enhanced winter NAO skill due to ensemble subsampling entails an improved prediction of the surface climate variables as well. Here, we show that a refined subselection procedure that accounts both for the NAO index and for the three additional modes of sea level pressure variability is able to further increase the prediction skill of wintertime mean sea level pressure, near-surface temperature, and precipitation across Europe.Plain Language Summary Atmospheric winter conditions in Europe are primarily controlled by the varying pressure field over the North Atlantic, influencing temperature and precipitation in Europe. Current seasonal forecasts of European winter climate, though highly desirable for society and economy, are as yet not fully reliable. There exist a number of autumn predictors, such as sea surface and stratospheric temperature, Eurasian snow depth, and Arctic sea ice, that impact on the upcoming pressure regimes in a predictable way. The present dynamical seasonal forecast systems respond still too weakly to these known seasonal predictors. But the relationship is reproduced quite well by means of statistics. In combination, statistical and dynamical forecasts have the potential to improve forecasts of the North Atlantic pressure conditions and thereby affected variables like temperature and precipitation in Europe considerably. We extend an existing hybrid seasonal forecast procedure by considering more modes of variability of the Atlantic pressure regimes than just the North Atlantic Oscillation. In this way, we are able to improve the forecasts for temperature and precipitation over wider regions in Europe. Cohen et al. (2019) argue that new statistical techniques can increase the accuracy of seasonal forecasts and advocate the development of hybrid dynamical-statistical forecasts to produce more robust seasonal predictions. Hybrid forecasts based on circulation specification were presented, for example, by Baker, Shaffrey, and Scaife (2018) and Dobrynin et al. (2018).In boreal winter, European weather and climate is dominated by the zonal propagation of planetary and synoptic-scale waves. This large-scale circulation is an extremely high-dimensional phenomenon in real RESEARCH LETTER