4.8 Article

Acceleration of global N2O emissions seen from two decades of atmospheric inversion

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NATURE CLIMATE CHANGE
卷 9, 期 12, 页码 993-+

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NATURE PUBLISHING GROUP
DOI: 10.1038/s41558-019-0613-7

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资金

  1. NASA (USA)
  2. BEIS (UK)
  3. NOAA (USA)
  4. BoM (Australia)
  5. NILU (Norway), SNU (Korea), CMA (China), NIES (Japan)
  6. Urbino University (Italy)
  7. MINEC-Spain
  8. European Commission ERDF Ramon y Cajal grant [RYC-201620269]
  9. Programa Propio from UPM
  10. Comunidad de Madrid (Spain) [AGRISOST-CM S2018/BAA-4330, 76810]
  11. European Commission
  12. Environment Research and Technology Development Fund [2-1802]
  13. Ministry of the Environment, Japan
  14. Food and Agriculture Organization of the United Nations
  15. NERC [nceo020004, nceo020005] Funding Source: UKRI

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Nitrous oxide (N2O) is the third most important long-lived GHG and an important stratospheric ozone depleting substance. Agricultural practices and the use of N-fertilizers have greatly enhanced emissions of N2O. Here, we present estimates of N2O emissions determined from three global atmospheric inversion frameworks during the period 1998-2016. We find that global N2O emissions increased substantially from 2009 and at a faster rate than estimated by the IPCC emission factor approach. The regions of East Asia and South America made the largest contributions to the global increase. From the inversion-based emissions, we estimate a global emission factor of 2.3 +/- 0.6%, which is significantly larger than the IPCC Tier-1 default for combined direct and indirect emissions of 1.375%. The larger emission factor and accelerating emission increase found from the inversions suggest that N2O emission may have a nonlinear response at global and regional scales with high levels of N-input.

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