A wetland scene   Picture: Shutterstock

Wetlands are sensitive to climate change  Picture: Shutterstock

Global fossil fuel emissions would have to be reduced by as much as 20% more than previous estimates to achieve the Paris Agreement targets, because of natural greenhouse gas emissions from wetlands and permafrost, new research has found.

The additional reductions are equivalent to 5-6 years of carbon emissions from human activities at current rates, according to a new paper led by the UK’s Centre for Ecology & Hydrology.

The 2015 Paris Climate Agreement aims to keep “the global average temperature increase to well below 2 °C above pre-industrial levels and to pursue efforts to limit the temperature increase to 1.5 °C above pre-industrial levels”.

The research for the paper Carbon budgets for 1.5 and 2 °C targets lowered by natural wetland and permafrost feedbacks, which is published in the journal Nature Geoscience today [9th July], uses a novel form of climate model where a specified temperature target is used to calculate the compatible fossil fuel emissions.

The model simulations estimate the natural wetland and permafrost response to climate change, including their greenhouse gas emissions, and the implications for human fossil-fuel emissions.

Natural wetlands are very wet regions where the soils emit methane, which is also a greenhouse gas. The methane emissions are larger in warmer soils, so they will increase in a warmer climate.

Permafrost regions are those which are permanently frozen. Under a warming climate permafrost regions begin to thaw and as a result the soils begin to emit carbon dioxide, and in some cases methane, into the atmosphere.

The greenhouse gas emissions from natural wetland and permafrost increase with global temperature increases, this in turn adds further to global warming creating a “positive feedback” loop.

"Greenhouse gas emissions from natural wetlands and permafrost regions are sensitive to climate change, primarily via changes in soil temperature" - Dr Edward Comyn-Platt 

The results show the “positive feedback” process are disproportionately more important for the emission reductions needed to achieve the 1.5 °C target rather than the 2 °C target. This is because we model the impact of the additional processes for the time-period 2015-2100, which are broadly similar for the two temperature targets. However, as the emissions budgets to achieve the 1.5 °C target are half of what is required to meet the 2 °C target, the proportional impact of natural wetlands and permafrost thaw is much larger.

Lead author Dr Edward Comyn-Platt, a biogeochemist at the UK Centre for Ecology & Hydrology said: “Greenhouse gas emissions from natural wetlands and permafrost regions are sensitive to climate change, primarily via changes in soil temperature.

"Changes in these emissions will alter the amount of greenhouse gases in the atmosphere and must be considered when estimating the human emissions compatible with the Paris Climate Agreement.”

Co-author Prof Chris Huntingford, of the Centre for Ecology & Hydrology, said: “We were surprised at how large these permafrost and wetland feedbacks can be for the low warming target of just 1.5 °C”

The other institutions involved in the research were the University of Exeter, the Met Office Hadley Centre, Exeter, the University of Reading and the Joint Centre for Hydrometeorological Research, Wallingford.

Funding for the work was received under a Natural Environment Research Council programme, the Joint UK BEIS/Defra Met Office Hadley Centre Climate Programme, the EU-funded CRESCENDO project, the EPSRC Fellowship and Centre for Ecology & Hydrology National Capability Funding.

Links

Carbon budgets for 1.5 and 2 °C targets lowered by natural wetland and permafrost feedbacks is published in Nature Geoscience. Comyn-Platt, E.; Hayman, G.; Huntingford, C.; Chadburn, S. E.; Burke, E. J.; Harper, A. B.; Collins, W. J.; Webber, C. P.; Powell, T.; Cox, P. M.; Gedney, N.; Sitch, S. (2018) Carbon budgets for 1.5 and 2C targets lowered by natural wetland and permafrost feedbacks.

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