Data-driven estimates of global nitrous oxide emissions from croplands

被引:117
作者
Wang, Qihui [1 ]
Zhou, Feng [1 ]
Shang, Ziyin [1 ]
Ciais, Philippe [1 ,2 ]
Winiwarter, Wilfried [3 ,4 ]
Jackson, Robert B. [5 ]
Tubiello, Francesco N. [6 ]
Janssens-Maenhout, Greet [7 ]
Tian, Hanqin [8 ]
Cui, Xiaoqing [1 ]
Canadell, Josep G. [9 ]
Piao, Shilong [1 ]
Tao, Shu [1 ]
机构
[1] Peking Univ, Coll Urban & Environm Sci, Lab Earth Surface Proc, Sino France Inst Earth Syst Sci, Beijing 100871, Peoples R China
[2] CEA CNRS UVSQ, LSCE, F-91191 Gif Sur Yvette, France
[3] IIASA, A-2361 Laxenburg, Austria
[4] Univ Zielona Gora, Inst Environm Engn, PL-65417 Zielona Gora, Poland
[5] Stanford Univ, Dept Earth Syst Sci, Stanford, CA 94305 USA
[6] UN, Stat Div, Food & Agr Org, Via Terme Caracalla, I-00153 Rome, Italy
[7] European Commiss, Joint Res Ctr, I-21027 Ispra, Italy
[8] Auburn Univ, Sch Forestry & Wildlife Sci, Int Ctr Climate & Global Change Res, Auburn, AL 36849 USA
[9] CSIRO Oceans & Atmosphere, Global Carbon Project, Canberra, ACT 2601, Australia
基金
中国国家自然科学基金; 奥地利科学基金会;
关键词
nitrous oxide; agricultural soils; flux upscaling; emission factor; emission inventories; temporal trend; DIRECT N2O EMISSIONS; FERTILIZER; SOIL; MODEL; MITIGATION; NUTRIENT; NITRATE; FIELDS; FLUXES; TREND;
D O I
10.1093/nsr/nwz087
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
Croplands are the single largest anthropogenic source of nitrous oxide (N2O) globally, yet their estimates remain difficult to verify when using Tier 1 and 3 methods of the Intergovernmental Panel on Climate Change (IPCC). Here, we re-evaluate global cropland-N2O emissions in 1961-2014, using N-rate-dependent emission factors (EFs) upscaled from 1206 field observations in 180 global distributed sites and high-resolution N inputs disaggregated from sub-national surveys covering 15593 administrative units. Our results confirm IPCC Tier 1 default EFs for upland crops in 1990-2014, but give a similar to 15% lower EF in 1961-1989 and a similar to 67% larger EF for paddy rice over the full period. Associated emissions (0.82 +/- 0.34 Tg N yr(-1)) are probably one-quarter lower than IPCC Tier 1 global inventories but close to Tier 3 estimates. The use of survey-based gridded N-input data contributes 58% of this emission reduction, the rest being explained by the use of observation-based non-linear EFs. We conclude that upscaling N2O emissions from site-level observations to global croplands provides a new benchmark for constraining IPCC Tier 1 and 3 methods. The detailed spatial distribution of emission data is expected to inform advancement towards more realistic and effective mitigation pathways.
引用
收藏
页码:441 / 452
页数:12
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