Projecting atmospheric N2O rise until the end of the 21st century: an Earth System Model study
Nitrous Oxide (N _2 O) is a potent greenhouse gas with a centennial-scale lifetime that contributes significantly to global warming. It is emitted from natural and anthropogenic sources. In nature, N _2 O is released mainly from nitrification and denitrification from the ocean and terrestrial system...
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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
IOP Publishing
2024-01-01
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| Series: | Environmental Research Letters |
| Subjects: | |
| Online Access: | https://doi.org/10.1088/1748-9326/ad8c6c |
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| Summary: | Nitrous Oxide (N _2 O) is a potent greenhouse gas with a centennial-scale lifetime that contributes significantly to global warming. It is emitted from natural and anthropogenic sources. In nature, N _2 O is released mainly from nitrification and denitrification from the ocean and terrestrial systems. The use of agricultural fertilizers has significantly increased the emission of N _2 O in the past century. Here we present, to our knowledge, the first coupled ocean and terrestrial N _2 O modules within an Earth System Model. The coupled modules were used to simulate the six Shared Socioeconomic Pathways (SSPs) scenarios with available nitrogen fertilizer inputs. Our results are compared to projections of atmospheric N _2 O concentrations used for SSPs scenario experiments. Additionally, an extra set of simulations were prescribed with emulated N _2 O concentrations available as input in Shared Socioeconomic Pathways scenarios. We report four main drivers for terrestrial N _2 O uncertainties: atmospheric temperature, agricultural fertilizer input, soil denitrification and agricultural model dynamics. We project an atmospheric N _2 O concentration range from 401 to 418 ppb in six SSPs simulations with a robust lack of sensitivity to equilibrium climate sensitivity. We found a large difference between our low emission scenarios N _2 O concentrations by 2100 compared to the concentration provided for SSPs experiments. This divergence is likely explained by strong mitigation assumptions that were not accounted for in this study, which would require a substantial decrease of agricultural N _2 O emissions. The coupled model and the simulations prescribed with N _2 O concentrations showed a difference between −0.02 and 0.09 ^∘ C by 2100. Our model simulation shows a lack of sensitivity to climate mitigation efforts projecting similar N _2 O concentration in low and high mitigation scenarios, that could indicate the need of further development of agricultural model dynamics. Further improvements in Earth system models should focus on the impact of oxygen decline on N _2 O dynamics in the ocean and the representation of anaerobic soils and agricultural dynamics on land, including mitigation methods on nitrogen fertilizers. |
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| ISSN: | 1748-9326 |