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Global soil nitrous oxide emissions since the pre-industrial era estimated by an ensemble of Terrestrial Biosphere Models: Magnitude, attribution and uncertainty

Authors: 
Tian H, J Yang, R Xu, C Lu, JG Canadell, EA Davidson, RB Jackson, A Arneth, J Chang, P Ciais, S Gerber, A Ito, F Joos, S Lienert, P Messina, S Olin, S Pan, C Peng, E Saikawa, RL Thompson, N Vuichard, W Winiwater, S Zaehle, B Zhang
Year: 
2019
Journal: 
Global Change Biology
Journal Volume/Pages: 
25:640-659

Our understanding and quantification of global soil nitrous oxide (N2O) emissions and the underlying processes remain largely uncertain. Here we assessed the effects of multiple anthropogenic and natural factors, including nitrogen fertilizer (N) application, atmospheric N deposition, manure N application, land cover change, climate change and rising atmospheric CO2 concentration, on global soil N2O emissions for the period 1861–2016 using a standard simulation protocol with seven process-based terrestrial biosphere models. Results suggest global soil N2O emissions have increased from 6.3 ± 1.1 Tg N2O-N yr-1 in the pre-industrial period (the 1860s) to 10.0 ± 2.0 Tg N2O-N yr-1 in the recent decade (2007-2016). Cropland soil emissions, in particular, increased from 0.3 Tg N2O-N yr-1 to 3.3 Tg N2O-N yr-1 over the same period, contributing 82% of the increased global soil N2O emissions. Regionally, China, South Asia and Southeast Asia underwent rapid increases in cropland N2O emissions since the 1970s. However, US cropland N2O emissions had been relatively flat in magnitude since the 1980s, and EU cropland N2O emissions appear to have decreased by 14%. Soil N2O emissions from predominantly natural ecosystems accounted for 67% of the global soil emissions in the recent decade and showed only a relatively small increase of 0.7 ± 0.5 Tg N2O-N yr-1 (11%) since the 1860s. In the recent decade, N fertilizer application, N deposition, manure N application and climate change contributed 54%, 26%, 15% and 24%, respectively, to the increased global soil N2O emissions. Rising atmospheric CO2 concentration reduced soil N2O emissions by 10% through the enhanced plant N uptake, while land cover change played a minor role. Our estimation here does not account for indirect emissions from soils and the direct emissions from the excreta of grazing livestock, which need to be quantified in future research. To address uncertainties in estimating regional and global soil N2O emissions, this study recommends several critical strategies for improving the process-based simulations.

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