Modelling the impact of nitrogen deposition, climate change and nutrient limitations on tree carbon sequestration in Europe for the period 1900-2050

► European tree C sequestration 1900-2050 has been modelled as function of N deposition and climate. ► N deposition drove tree C sequestration in the past, climate will do it in the future. ► The impact of climate change will be limited by N, but also base cation and P availability.