Xu Liang, Saatchi Sassan S, Yang Yan, Yu Yifan, Pongratz Julia, Bloom A Anthony, Bowman Kevin, Worden John, Liu Junjie, Yin Yi, Domke Grant, McRoberts Ronald E, Woodall Christopher, Nabuurs Gert-Jan, de-Miguel Sergio, Keller Michael, Harris Nancy, Maxwell Sean, Schimel David
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA.
Institute of Environment and Sustainability, University of California, Los Angeles, CA, USA.
Sci Adv. 2021 Jul 2;7(27). doi: 10.1126/sciadv.abe9829. Print 2021 Jul.
Live woody vegetation is the largest reservoir of biomass carbon, with its restoration considered one of the most effective natural climate solutions. However, terrestrial carbon fluxes remain the largest uncertainty in the global carbon cycle. Here, we develop spatially explicit estimates of carbon stock changes of live woody biomass from 2000 to 2019 using measurements from ground, air, and space. We show that live biomass has removed 4.9 to 5.5 PgC year from the atmosphere, offsetting 4.6 ± 0.1 PgC year of gross emissions from disturbances and adding substantially (0.23 to 0.88 PgC year) to the global carbon stocks. Gross emissions and removals in the tropics were four times larger than temperate and boreal ecosystems combined. Although live biomass is responsible for more than 80% of gross terrestrial fluxes, soil, dead organic matter, and lateral transport may play important roles in terrestrial carbon sink.
活木本植被是生物量碳的最大储存库,其恢复被视为最有效的自然气候解决方案之一。然而,陆地碳通量仍是全球碳循环中最大的不确定性因素。在此,我们利用地面、空中和空间测量数据,对2000年至2019年活木本生物量的碳储量变化进行了空间明确估计。我们发现,活生物量每年从大气中吸收4.9至5.5PgC,抵消了因干扰产生的4.6±0.1PgC的总排放量,并为全球碳储量大幅增加(每年0.23至0.88PgC)。热带地区的总排放量和吸收量比温带和北方生态系统的总和大四倍。尽管活生物量占陆地总通量的80%以上,但土壤、死有机物质和横向传输可能在陆地碳汇中发挥重要作用。