Zhang Ke, de Almeida Castanho Andrea D, Galbraith David R, Moghim Sanaz, Levine Naomi M, Bras Rafael L, Coe Michael T, Costa Marcos H, Malhi Yadvinder, Longo Marcos, Knox Ryan G, McKnight Shawna, Wang Jingfeng, Moorcroft Paul R
Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, USA.
Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, Norman, OK, USA.
Glob Chang Biol. 2015 Jul;21(7):2569-2587. doi: 10.1111/gcb.12903. Epub 2015 May 12.
There is considerable interest in understanding the fate of the Amazon over the coming century in the face of climate change, rising atmospheric CO levels, ongoing land transformation, and changing fire regimes within the region. In this analysis, we explore the fate of Amazonian ecosystems under the combined impact of these four environmental forcings using three terrestrial biosphere models (ED2, IBIS, and JULES) forced by three bias-corrected IPCC AR4 climate projections (PCM1, CCSM3, and HadCM3) under two land-use change scenarios. We assess the relative roles of climate change, CO fertilization, land-use change, and fire in driving the projected changes in Amazonian biomass and forest extent. Our results indicate that the impacts of climate change are primarily determined by the direction and severity of projected changes in regional precipitation: under the driest climate projection, climate change alone is predicted to reduce Amazonian forest cover by an average of 14%. However, the models predict that CO fertilization will enhance vegetation productivity and alleviate climate-induced increases in plant water stress, and, as a result, sustain high biomass forests, even under the driest climate scenario. Land-use change and climate-driven changes in fire frequency are predicted to cause additional aboveground biomass loss and reductions in forest extent. The relative impact of land use and fire dynamics compared to climate and CO impacts varies considerably, depending on both the climate and land-use scenario, and on the terrestrial biosphere model used, highlighting the importance of improved quantitative understanding of all four factors - climate change, CO fertilization effects, fire, and land use - to the fate of the Amazon over the coming century.
面对气候变化、大气中二氧化碳水平上升、持续的土地转变以及该地区不断变化的火灾状况,人们对了解未来一个世纪亚马逊地区的命运有着浓厚兴趣。在本分析中,我们使用三种陆地生物圈模型(ED2、IBIS和JULES),在两种土地利用变化情景下,由三种经偏差校正的IPCC AR4气候预测(PCM1、CCSM3和HadCM3)驱动,探讨这四种环境驱动力共同作用下亚马逊生态系统的命运。我们评估气候变化、二氧化碳施肥效应、土地利用变化和火灾在推动亚马逊生物量和森林范围预计变化中的相对作用。我们的结果表明,气候变化的影响主要由区域降水预计变化的方向和严重程度决定:在最干旱的气候预测下,仅气候变化预计就会使亚马逊森林覆盖率平均降低14%。然而,模型预测二氧化碳施肥效应将提高植被生产力并缓解气候引起的植物水分胁迫增加,因此,即使在最干旱的气候情景下也能维持高生物量森林。预计土地利用变化和气候驱动的火灾频率变化将导致额外的地上生物量损失和森林范围减少。与气候和二氧化碳影响相比,土地利用和火灾动态的相对影响差异很大,这取决于气候和土地利用情景以及所使用的陆地生物圈模型,凸显了更好地定量理解所有四个因素——气候变化、二氧化碳施肥效应、火灾和土地利用——对未来一个世纪亚马逊命运的重要性。