Luo Meng, Zhao Xin, Hao Dalei, Bond-Lamberty Ben, Daigneault Adam, Patel Pralit L, Kou-Giesbrecht Sian, Reyer Christopher P O, Dashti Hamid, Chen Min
Department of Forest and Wildlife Ecology, University of Wisconsin-Madison, Madison, Wisconsin, USA.
Joint Global Change Research Institute, Pacific Northwest National Laboratory, College Park, Maryland, USA.
Glob Chang Biol. 2025 May;31(5):e70219. doi: 10.1111/gcb.70219.
Global change, particularly the changes in atmospheric CO concentration, climatic variables, and nitrogen deposition, has been widely recognized and examined to have worldwide impacts on forest carbon. However, its influence on forest area required to meet the demand for timber and carbon storage and subsequent land use and land cover change (LULCC) is rarely studied. This study explores the role of global change-driven forest carbon change in shaping future global LULCC projections and investigates underlying drivers. We incorporated the global change impacts on forest carbon from the Canadian Land Surface Scheme Including Biogeochemical Cycles model simulations (driven by meteorological forcing projections from two Earth system models [ESMs]) into the Global Change Analysis Model, under three combinations of shared socioeconomic pathways and representative concentration pathways (SSP126, SSP370, and SSP585). Including forest carbon change decreases the projected expansion of managed forest and managed pasture, reduces the loss of unmanaged pastures and forests, and provides more cropland. The relative change in managed forest by 2100 is -4.0%, -21.7%, and -31.9%, under SSP126, SSP370, and SSP585, respectively, when forest carbon change is considered. CO fertilization is the dominant driver, increasing forest vegetation and soil carbon by 37% and 4.1%, and leading to 78.6% of the total area with a change in land use types by 2100 under SSP585. In comparison, climate change reduces forest vegetation and soil carbon by -3.5% and -0.8%, influencing 23.9% of the total area with a change in land use types by 2100 under SSP585, while nitrogen deposition has minor impacts. Using meteorological forcing data from two ESMs leads to similar impacts of forest carbon change on LULCC in terms of sign and trend but different magnitudes. This study highlights the large impact of forest carbon change on shaping future LULCC dynamics and the critical role of CO fertilization.
全球变化,尤其是大气中二氧化碳浓度、气候变量和氮沉降的变化,已被广泛认识并研究其对全球森林碳的影响。然而,其对满足木材需求和碳储存所需森林面积以及随后土地利用和土地覆盖变化(LULCC)的影响却鲜有研究。本研究探讨了全球变化驱动的森林碳变化在塑造未来全球LULCC预测中的作用,并调查了潜在驱动因素。我们将加拿大包括生物地球化学循环的陆面模式模拟(由两个地球系统模型[ESMs]的气象强迫预测驱动)对森林碳的全球变化影响纳入全球变化分析模型,采用共享社会经济路径和代表性浓度路径的三种组合(SSP126、SSP370和SSP585)。纳入森林碳变化会减少人工林和人工牧场的预计扩张,减少天然牧场和森林的损失,并提供更多农田。考虑森林碳变化时,到2100年,在SSP126、SSP370和SSP585情景下,人工林的相对变化分别为-4.0%、-21.7%和-31.9%。二氧化碳施肥是主要驱动因素,使森林植被和土壤碳分别增加37%和4.1%,并导致在SSP585情景下到2100年78.6%的总面积土地利用类型发生变化。相比之下,气候变化使森林植被和土壤碳分别减少-3.5%和-0.8%,在SSP585情景下到2100年影响23.9%的总面积土地利用类型发生变化,而氮沉降影响较小。使用来自两个ESM的气象强迫数据,森林碳变化对LULCC的影响在符号和趋势方面相似,但幅度不同。本研究强调了森林碳变化对塑造未来LULCC动态的重大影响以及二氧化碳施肥的关键作用。