New research suggests that the capacity of the terrestrial biosphere to absorb carbon dioxide (CO2) may have been underestimated in past calculations due to certain land-use changes not being fully taken into account.
It is widely known that the terrestrial biosphere (the collective term for all the world’s land vegetation, soil, etc.) is an important factor in mitigating climate change, as it absorbs around 20% of all fossil fuel CO2 emissions. However, its role as a net carbon sink is affected by land-use changes such as deforestation and expanded agricultural practice.
A new study, conducted by an international collaboration of scientists and published in the journal Nature Geoscience, has analysed the extent to which these changing land-use practices affect carbon emissions – allowing the levels of CO2 uptake by the terrestrial biosphere to be more accurately predicted.
The results not only show that CO2 emissions from changing land-use practices are likely to be significantly higher than previously thought, but also imply that these emissions are compensated for by a higher rate of carbon uptake among terrestrial ecosystems.
Co-author of the study, Dr Tom Pugh from the University of Birmingham, says:
‘Our work shows that the terrestrial biosphere might have greater potential than previously thought to mitigate climate change by sequestering carbon emissions from fossil fuels. However, to fully realise this potential we will have to ensure that the significant emissions resulting from land-use changes are reduced as much as possible.’
Co-author Professor Stephen Sitch from the University of Exeter adds:
‘The results imply that reforestation projects and efforts to avoid further deforestation are of the utmost importance in our pursuit to limit global warming to below 2oC, as stated in the Paris climate agreement.’
For more information please contact Liz Bell in the University of Birmingham Press Office, on or call (+44) 0121 414 2772.
Arneth et al. (2017) 'Historical carbon dioxide emissions caused by land-use changes are possibly larger than assumed' Nature Geoscience DOI: 10.1038/ngeo2882
Link to paper (activated upon publication):http://dx.doi.org/10.1038/ngeo2882
In addition to the researchers from the Universities of Birmingham and Exeter, this paper is co-authored by researchers affiliated with the following institutions:
Department of Atmospheric Environmental Research (Germany), Max Planck Institute for Meteorology (Germany), Imperial College London (UK), ETH Zürich (Switzerland), LSCE (France), NASA Goddard Space Flight Center (US), Aix-Marseille Université (France), University of Maryland (US), German Federal Institute of Hydrology (Germany), The Institute of Applied Energy (Japan), Lund University (Sweden), Met Office Hadley Centre (UK), Max Planck Institute for Biogeochemistry (Germany).