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DOI | 10.1002/2017GB005671 |
Marine N2O Emissions From Nitrification and Denitrification Constrained by Modern Observations and Projected in Multimillennial Global Warming Simulations | |
Battaglia G.; Joos F. | |
发表日期 | 2018 |
ISSN | 0886-6236 |
EISSN | 1944-9224 |
起始页码 | 92 |
结束页码 | 121 |
卷号 | 32期号:1 |
英文摘要 | Nitrous oxide (N2O) is a potent greenhouse gas (GHG) and ozone destructing agent; yet global estimates of N2O emissions are uncertain. Marine N2O stems from nitrification and denitrification processes which depend on organic matter cycling and dissolved oxygen (O2). We introduce N2O as an obligate intermediate product of denitrification and as an O2-dependent by-product from nitrification in the Bern3D ocean model. A large model ensemble is used to probabilistically constrain modern and to project marine N2O production for a low (Representative Concentration Pathway (RCP)2.6) and high GHG (RCP8.5) scenario extended to A.D. 10,000. Water column N2O and surface ocean partial pressure N2O data serve as constraints in this Bayesian framework. The constrained median for modern N2O production is 4.5 (±1σ range: 3.0 to 6.1) Tg N yr−1, where 4.5% stems from denitrification. Modeled denitrification is 65.1 (40.9 to 91.6) Tg N yr−1, well within current estimates. For high GHG forcing, N2O production decreases by 7.7% over this century due to decreasing organic matter export and remineralization. Thereafter, production increases slowly by 21% due to widespread deoxygenation and high remineralization. Deoxygenation peaks in two millennia, and the global O2 inventory is reduced by a factor of 2 compared to today. Net denitrification is responsible for 7.8% of the long-term increase in N2O production. On millennial timescales, marine N2O emissions constitute a small, positive feedback to climate change. Our simulations reveal tight coupling between the marine carbon cycle, O2, N2O, and climate. ©2017. American Geophysical Union. All Rights Reserved. |
英文关键词 | denitrification; deoxygenation; long-term Earth System projections; marine N2O emissions; nitrification |
语种 | 英语 |
scopus关键词 | denitrification; dissolved oxygen; emission; ensemble forecasting; global warming; long-term change; marine atmosphere; model; nitrification; nitrogen dioxide; organic matter; oxygenation; partial pressure; remineralization; simulation; water column |
来源期刊 | Global Biogeochemical Cycles
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/129867 |
作者单位 | Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland; Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland |
推荐引用方式 GB/T 7714 | Battaglia G.,Joos F.. Marine N2O Emissions From Nitrification and Denitrification Constrained by Modern Observations and Projected in Multimillennial Global Warming Simulations[J],2018,32(1). |
APA | Battaglia G.,&Joos F..(2018).Marine N2O Emissions From Nitrification and Denitrification Constrained by Modern Observations and Projected in Multimillennial Global Warming Simulations.Global Biogeochemical Cycles,32(1). |
MLA | Battaglia G.,et al."Marine N2O Emissions From Nitrification and Denitrification Constrained by Modern Observations and Projected in Multimillennial Global Warming Simulations".Global Biogeochemical Cycles 32.1(2018). |
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