Zheng Bo, Ciais Philippe, Chevallier Frederic, Chuvieco Emilio, Chen Yang, Yang Hui
Institute of Environment and Ecology, Tsinghua Shenzhen International Graduate School, Tsinghua University, Shenzhen 518055, China.
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France.
Sci Adv. 2021 Sep 24;7(39):eabh2646. doi: 10.1126/sciadv.abh2646.
Satellites have detected a global decline in burned area of grassland, coincident with a small increase in burned forest area. These contrasting trends have been reported in earlier literature; however, less is known of their impacts on global fire emission trends due to the scarcity of direct observations. We use an atmospheric inversion system to show that global fire emissions have been stable or slightly decreasing despite the substantial decline in global burned area over the past two decades caused by the carbon dioxide emission increase from forest fires offsetting the decreasing emissions from grass and shrubland fires. Forest fires are larger carbon dioxide sources per unit area burned than grassland fires, with a slow or incomplete follow-up recovery—sometimes no recovery due to degradation and deforestation. With fires expanding over forest areas, the slow recovery of carbon dioxide uptake over burned forest lands weakens land sink capacity, implying positive feedback on climate change.
卫星探测到全球草地火烧面积呈下降趋势,与此同时森林火烧面积略有增加。这些相反的趋势在早期文献中已有报道;然而,由于缺乏直接观测数据,人们对它们对全球火灾排放趋势的影响了解较少。我们使用一种大气反演系统表明,尽管过去二十年全球火烧面积大幅下降,但全球火灾排放一直保持稳定或略有下降,这是因为森林火灾产生的二氧化碳排放增加抵消了草地和灌木地火灾排放的减少。森林火灾每单位燃烧面积产生的二氧化碳源比草地火灾大,且后续恢复缓慢或不完全——有时由于退化和森林砍伐而无法恢复。随着火灾在森林地区蔓延,火烧森林土地上二氧化碳吸收的缓慢恢复削弱了陆地碳汇能力,这意味着对气候变化有正反馈作用。