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大气二氧化碳数据估算的中国大规模陆地碳汇。

Large Chinese land carbon sink estimated from atmospheric carbon dioxide data.

机构信息

Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China.

University of Chinese Academy of Sciences, Beijing, China.

出版信息

Nature. 2020 Oct;586(7831):720-723. doi: 10.1038/s41586-020-2849-9. Epub 2020 Oct 28.

DOI:10.1038/s41586-020-2849-9
PMID:33116288
Abstract

Limiting the rise in global mean temperatures relies on reducing carbon dioxide (CO) emissions and on the removal of CO by land carbon sinks. China is currently the single largest emitter of CO, responsible for approximately 27 per cent (2.67 petagrams of carbon per year) of global fossil fuel emissions in 2017. Understanding of Chinese land biosphere fluxes has been hampered by sparse data coverage, which has resulted in a wide range of a posteriori estimates of flux. Here we present recently available data on the atmospheric mole fraction of CO, measured from six sites across China during 2009 to 2016. Using these data, we estimate a mean Chinese land biosphere sink of -1.11 ± 0.38 petagrams of carbon per year during 2010 to 2016, equivalent to about 45 per cent of our estimate of annual Chinese anthropogenic emissions over that period. Our estimate reflects a previously underestimated land carbon sink over southwest China (Yunnan, Guizhou and Guangxi provinces) throughout the year, and over northeast China (especially Heilongjiang and Jilin provinces) during summer months. These provinces have established a pattern of rapid afforestation of progressively larger regions, with provincial forest areas increasing by between 0.04 million and 0.44 million hectares per year over the past 10 to 15 years. These large-scale changes reflect the expansion of fast-growing plantation forests that contribute to timber exports and the domestic production of paper. Space-borne observations of vegetation greenness show a large increase with time over this study period, supporting the timing and increase in the land carbon sink over these afforestation regions.

摘要

限制全球平均气温上升依赖于减少二氧化碳(CO)排放和通过陆地碳汇去除 CO。中国目前是 CO 的最大单一排放国,约占 2017 年全球化石燃料排放量的 27%(每年 2.67 太吨碳)。由于数据覆盖范围稀疏,对中国陆地生物圈通量的理解受到阻碍,这导致了通量的后验估计范围很广。在这里,我们展示了最近获得的关于大气 CO 摩尔分数的数据,这些数据是在 2009 年至 2016 年期间在中国六个地点测量的。利用这些数据,我们估计 2010 年至 2016 年期间中国陆地生物圈的平均碳汇为-1.11±0.38 太吨碳/年,相当于同期中国人为排放的碳年排放量的 45%左右。我们的估计反映了中国西南地区(云南、贵州和广西)全年以及中国东北地区(特别是黑龙江和吉林省)夏季对碳汇的低估。这些省份形成了一个快速造林的模式,造林面积逐年增加,过去 10 到 15 年,各省的森林面积每年增加 4 万至 44 万公顷。这些大规模的变化反映了速生人工林的扩张,这有助于木材出口和国内纸张生产。植被绿色度的天基观测显示,在本研究期间随时间呈大幅增加,支持了这些造林地区陆地碳汇的时间和增加。

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