Carbon assimilation and wood production are influenced by environmental conditions and endogenous factors, such as species auto-ecology, age, and hierarchical position within the forest structure. Disentangling the intricate relationships between those factors is more pressing than ever due to climate change's pressure. Yet, our understanding of how future climate will interact with forests of different ages is particularly limited, and only a few studies have explored this relationship under changing climate conditions. We employed a validated process-based forest model for simulating undisturbed forests of different ages under five climate change scenarios coming from five Earth System Models. In this context, carbon stocks and increment were simulated via total carbon woody stocks (MgC ha-1) and the mean annual increment (m3 ha-1year-1), which depend mainly on age and long-term processes, such as climate trends. We find greater differences among different age cohorts under the same scenario than in different climate scenarios under the same age class. We found different C-accumulation patterns under climate change between coniferous stands and broadleaves. Increasing temperature and changes in precipitation patterns led to a decline in above-ground biomass in spruce stands, especially in the older age classes. On the contrary, the results show that beech forests at DK-Sor will maintain and even increase C-storage rates under most RCP scenarios. Scots pine forests show an intermediate behavior with a stable stock capacity over time and in different scenarios but with decreasing mean volume annual increment. These results confirm current observations worldwide that indicate a stronger climate-related decline in conifers forests than in broadleaves. We, therefore, advocate for a better understanding of the interaction between forests and climate to better inform forest management strategies, ultimately dampening the impacts of climate change on forest ecosystems