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A comprehensive quantification of global nitrous oxide sources and sinks
Nature ( IF 64.8 ) Pub Date : 2020-10-07 , DOI: 10.1038/s41586-020-2780-0
Hanqin Tian 1 , Rongting Xu 1 , Josep G Canadell 2 , Rona L Thompson 3 , Wilfried Winiwarter 4, 5 , Parvadha Suntharalingam 6 , Eric A Davidson 7 , Philippe Ciais 8 , Robert B Jackson 9, 10, 11 , Greet Janssens-Maenhout 12, 13 , Michael J Prather 14 , Pierre Regnier 15 , Naiqing Pan 1, 16 , Shufen Pan 1 , Glen P Peters 17 , Hao Shi 1 , Francesco N Tubiello 18 , Sönke Zaehle 19 , Feng Zhou 20 , Almut Arneth 21 , Gianna Battaglia 22 , Sarah Berthet 23 , Laurent Bopp 24 , Alexander F Bouwman 25, 26, 27 , Erik T Buitenhuis 6, 28 , Jinfeng Chang 8, 29 , Martyn P Chipperfield 30, 31 , Shree R S Dangal 32 , Edward Dlugokencky 33 , James W Elkins 33 , Bradley D Eyre 34 , Bojie Fu 16, 35 , Bradley Hall 33 , Akihiko Ito 36 , Fortunat Joos 22 , Paul B Krummel 37 , Angela Landolfi 38, 39 , Goulven G Laruelle 15 , Ronny Lauerwald 8, 15, 40 , Wei Li 8, 41 , Sebastian Lienert 22 , Taylor Maavara 42 , Michael MacLeod 43 , Dylan B Millet 44 , Stefan Olin 45 , Prabir K Patra 46, 47 , Ronald G Prinn 48 , Peter A Raymond 42 , Daniel J Ruiz 14 , Guido R van der Werf 49 , Nicolas Vuichard 8 , Junjie Wang 27 , Ray F Weiss 50 , Kelley C Wells 44 , Chris Wilson 30, 31 , Jia Yang 51 , Yuanzhi Yao 1
Affiliation  

Nitrous oxide (N2O), like carbon dioxide, is a long-lived greenhouse gas that accumulates in the atmosphere. Over the past 150 years, increasing atmospheric N2O concentrations have contributed to stratospheric ozone depletion1 and climate change2, with the current rate of increase estimated at 2 per cent per decade. Existing national inventories do not provide a full picture of N2O emissions, owing to their omission of natural sources and limitations in methodology for attributing anthropogenic sources. Here we present a global N2O inventory that incorporates both natural and anthropogenic sources and accounts for the interaction between nitrogen additions and the biochemical processes that control N2O emissions. We use bottom-up (inventory, statistical extrapolation of flux measurements, process-based land and ocean modelling) and top-down (atmospheric inversion) approaches to provide a comprehensive quantification of global N2O sources and sinks resulting from 21 natural and human sectors between 1980 and 2016. Global N2O emissions were 17.0 (minimum-maximum estimates: 12.2-23.5) teragrams of nitrogen per year (bottom-up) and 16.9 (15.9-17.7) teragrams of nitrogen per year (top-down) between 2007 and 2016. Global human-induced emissions, which are dominated by nitrogen additions to croplands, increased by 30% over the past four decades to 7.3 (4.2-11.4) teragrams of nitrogen per year. This increase was mainly responsible for the growth in the atmospheric burden. Our findings point to growing N2O emissions in emerging economies-particularly Brazil, China and India. Analysis of process-based model estimates reveals an emerging N2O-climate feedback resulting from interactions between nitrogen additions and climate change. The recent growth in N2O emissions exceeds some of the highest projected emission scenarios3,4, underscoring the urgency to mitigate N2O emissions.
更新日期:2020-10-07
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