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Stefan Olin

Postdoctoral fellow

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Global soil nitrous oxide emissions since the preindustrial era estimated by an ensemble of terrestrial biosphere models : Magnitude, attribution, and uncertainty


  • Hanqin Tian
  • Jia Yang
  • Rongting Xu
  • Chaoqun Lu
  • Josep G. Canadell
  • Eric A. Davidson
  • Robert B. Jackson
  • Almut Arneth
  • Jinfeng Chang
  • Philippe Ciais
  • Stefan Gerber
  • Akihiko Ito
  • Fortunat Joos
  • Sebastian Lienert
  • Palmira Messina
  • Stefan Olin
  • Shufen Pan
  • Changhui Peng
  • Eri Saikawa
  • Rona L. Thompson
  • Nicolas Vuichard
  • Wilfried Winiwarter
  • Sönke Zaehle
  • Bowen Zhang

Summary, in English

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/year in the preindustrial period (the 1860s) to 10.0 ± 2.0 Tg N2O-N/year in the recent decade (2007–2016). Cropland soil emissions increased from 0.3 Tg N2O-N/year to 3.3 Tg N2O-N/year over the same period, accounting for 82% of the total increase. 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 but showed only a relatively small increase of 0.7 ± 0.5 Tg N2O-N/year (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 total increase. 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 directed emissions from excreta of grazing livestock. To address uncertainties in estimating regional and global soil N2O emissions, this study recommends several critical strategies for improving the process-based simulations.


  • MERGE - ModElling the Regional and Global Earth system
  • eSSENCE: The e-Science Collaboration
  • Dept of Physical Geography and Ecosystem Science
  • BECC - Biodiversity and Ecosystem services in a Changing Climate

Publishing year







Global Change Biology





Document type

Journal article




  • Biological Sciences


  • global nitrogen cycle
  • greenhouse gas emission
  • nitrous oxide
  • process-based modeling
  • soil NO emission




  • ISSN: 1354-1013