Alterra, Wageningen University and Research Centre, PO Box 47, 6700 AA Wageningen, The Netherlands.
Environ Pollut. 2011 Oct;159(10):2289-99. doi: 10.1016/j.envpol.2010.11.023. Epub 2010 Dec 16.
We modelled the combined effects of past and expected future changes in climate and nitrogen deposition on tree carbon sequestration by European forests for the period 1900-2050. Two scenarios for deposition (current legislation and maximum technically feasible reductions) and two climate scenarios (no change and SRES A1 scenario) were used. Furthermore, the possible limitation of forest growth by calcium, magnesium, potassium and phosphorus is investigated. The area and age structure of the forests was assumed to stay constant to observations during the period 1970-1990. Under these assumptions, the simulations show that the change in forest growth and carbon sequestration in the past is dominated by changes in nitrogen deposition, while climate change is the major driver for future carbon sequestration. However, its impact is reduced by nitrogen availability. Furthermore, limitations in base cations, especially magnesium, and in phosphorus may significantly affect predicted growth in the future.
我们模拟了过去和预期未来的气候和氮沉积变化对欧洲森林碳固存的综合影响,时间跨度为 1900-2050 年。我们使用了两种沉积情景(现行法规和最大技术可行减排)和两种气候情景(无变化和 SRES A1 情景)。此外,还研究了钙、镁、钾和磷可能对森林生长的限制。假设森林的面积和年龄结构保持与 1970-1990 年期间的观测结果一致。在这些假设下,模拟结果表明,过去森林生长和碳固存的变化主要受氮沉积变化的影响,而气候变化是未来碳固存的主要驱动因素。然而,氮的可利用性降低了其影响。此外,基础阳离子(特别是镁)和磷的限制可能会对未来的预测生长产生重大影响。