Large Chinese land carbon sink estimated from atmospheric carbon dioxide data

被引:571
作者
Wang, Jing [1 ,2 ,3 ,4 ]
Feng, Liang [3 ,4 ]
Palmer, Paul I. [3 ,4 ]
Liu, Yi [1 ,2 ]
Fang, Shuangxi [5 ,6 ]
Bosch, Hartmut [7 ]
O'Dell, Christopher W. [8 ]
Tang, Xiaoping [9 ]
Yang, Dongxu [1 ,2 ]
Liu, Lixin [6 ]
Xia, ChaoZong [9 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
[2] Univ Chinese Acad Sci, Beijing, Peoples R China
[3] Univ Edinburgh, Natl Ctr Earth Observat, Edinburgh, Midlothian, Scotland
[4] Univ Edinburgh, Sch GeoSci, Edinburgh, Midlothian, Scotland
[5] Zhejiang Univ Technol, Coll Environm, Hangzhou, Peoples R China
[6] China Meteorol Adm, Meteorol Observat Ctr, Beijing, Peoples R China
[7] Univ Leicester, Natl Ctr Earth Observat, Leicester, Leics, England
[8] Colorado State Univ, Ft Collins, CO 80523 USA
[9] State Forestry Adm, Acad Forest Inventory & Planning, Beijing, Peoples R China
关键词
TERRESTRIAL ECOSYSTEMS; CO2; EMISSIONS; TOP-DOWN; FOREST; INVENTORY; ENSEMBLE; STORAGE; BUDGET; 1ST; VARIABILITY;
D O I
10.1038/s41586-020-2849-9
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Limiting the rise in global mean temperatures relies on reducing carbon dioxide (CO2) emissions and on the removal of CO2 by land carbon sinks. China is currently the single largest emitter of CO2, responsible for approximately 27 per cent (2.67 petagrams of carbon per year) of global fossil fuel emissions in 20171. Understanding of Chinese land biosphere fluxes has been hampered by sparse data coverage(2-4), 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 CO2, 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(5,6), 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(7). 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.
引用
收藏
页码:720 / +
页数:16
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