The browser you are using is not supported by this website. All versions of Internet Explorer are no longer supported, either by us or Microsoft (read more here: https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Please use a modern browser to fully experience our website, such as the newest versions of Edge, Chrome, Firefox or Safari etc.

Default user image.

Mats Lindeskog

Postdoctoral fellow

Default user image.

Historical carbon dioxide emissions caused by land-use changes are possibly larger than assumed

Author

  • A. Arneth
  • S. Sitch
  • J. Pongratz
  • B. D. Stocker
  • P. Ciais
  • B. Poulter
  • A. D. Bayer
  • A. Bondeau
  • L. Calle
  • L. P. Chini
  • T. Gasser
  • M. Fader
  • P. Friedlingstein
  • E. Kato
  • W. Li
  • M. Lindeskog
  • J. E.M.S. Nabel
  • T. A.M. Pugh
  • E. Robertson
  • N. Viovy
  • C. Yue
  • S. Zaehle

Summary, in English

The terrestrial biosphere absorbs about 20% of fossil-fuel CO 2 emissions. The overall magnitude of this sink is constrained by the difference between emissions, the rate of increase in atmospheric CO 2 concentrations, and the ocean sink. However, the land sink is actually composed of two largely counteracting fluxes that are poorly quantified: fluxes from land-use change and CO 2 uptake by terrestrial ecosystems. Dynamic global vegetation model simulations suggest that CO 2 emissions from land-use change have been substantially underestimated because processes such as tree harvesting and land clearing from shifting cultivation have not been considered. As the overall terrestrial sink is constrained, a larger net flux as a result of land-use change implies that terrestrial uptake of CO 2 is also larger, and that terrestrial ecosystems might have greater potential to sequester carbon in the future. Consequently, reforestation projects and efforts to avoid further deforestation could represent important mitigation pathways, with co-benefits for biodiversity. It is unclear whether a larger land carbon sink can be reconciled with our current understanding of terrestrial carbon cycling. Our possible underestimation of the historical residual terrestrial carbon sink adds further uncertainty to our capacity to predict the future of terrestrial carbon uptake and losses.

Department/s

  • Dept of Physical Geography and Ecosystem Science
  • BECC: Biodiversity and Ecosystem services in a Changing Climate

Publishing year

2017-02-01

Language

English

Pages

79-84

Publication/Series

Nature Geoscience

Volume

10

Issue

2

Document type

Journal article review

Publisher

Nature Publishing Group

Topic

  • Environmental Sciences

Status

Published

ISBN/ISSN/Other

  • ISSN: 1752-0894