Carbon budgets for 1.5 and 2 °C targets lowered by natural wetland and permafrost feedbacks
Autor: | Peter M. Cox, Sarah Chadburn, Garry Hayman, Christopher P. Webber, William J. Collins, Stephen Sitch, Tom Powell, Edward Comyn-Platt, Anna B. Harper, Eleanor J. Burke, Chris Huntingford, Nicola Gedney |
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Rok vydání: | 2018 |
Předmět: |
010504 meteorology & atmospheric sciences
business.industry Global warming Fossil fuel 15. Life on land 010501 environmental sciences Permafrost Atmospheric sciences 01 natural sciences Methane Carbon cycle chemistry.chemical_compound Meteorology and Climatology Climate change mitigation chemistry 13. Climate action General Earth and Planetary Sciences Environmental science Climate model business 0105 earth and related environmental sciences Positive feedback |
Zdroj: | Nature Geoscience |
ISSN: | 1752-0894 |
DOI: | 10.1038/s41561-018-0174-9 |
Popis: | Global methane emissions from natural wetlands and carbon release from permafrost thaw have a positive feedback on climate, yet are not represented in most state-of-the-art climate models. Furthermore, a fraction of the thawed permafrost carbon is released as methane, enhancing the combined feedback strength. We present simulations with an inverted intermediate complexity climate model, which follows prescribed global warming pathways to stabilization at 1.5 or 2.0 °C above pre-industrial levels by the year 2100, and which incorporates a state-of-the-art global land surface model with updated descriptions of wetland and permafrost carbon release. We demonstrate that the climate feedbacks from those two processes are substantial. Specifically, permissible anthropogenic fossil fuel CO2 emission budgets are reduced by 17–23% (47–56 GtC) for stabilization at 1.5 °C, and 9–13% (52–57 GtC) for 2.0 °C stabilization. In our simulations these feedback processes respond more quickly at temperatures below 1.5 °C, and the differences between the 1.5 and 2 °C targets are disproportionately small. This key finding holds for transient emission pathways to 2100 and does not account for longer-term implications of these feedback processes. We conclude that natural feedback processes from wetlands and permafrost must be considered in assessments of transient emission pathways to limit global warming. |
Databáze: | OpenAIRE |
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