Carbon emissions from the Arctic tundra could increase drastically as global warming thaws permafrost. Clues now obtained about the long-term effects of such thawing on carbon dioxide emissions highlight the need for more data.
Notes
References
Liljedahl, A. K. et al. Nature Geosci. 9, 312–318 (2016).
Kwon, M. J. et al. Biogeosciences 13, 4219–4235 (2016).
Merbold, L. et al. Glob. Change Biol. 15, 2599–2614 (2009).
Zona, D. et al. Glob. Biogeochem. Cycles 26, GB2004 (2012).
Stow, D. A. et al. Remote Sens. Environ. 89, 281–308 (2004).
Naito, A. T. & Cairns, D. M. Prog. Phys. Geogr. 35, 423–442 (2011).
Mastepanov, M. et al. Biogeosci. Discuss. 9, 15853–15900 (2012).
Oechel, W. C., Laskowski, C. A., Burba, G., Gioli, B. & Kalhori, A. A. M. J. Geophys. Res. Biogeosci. 119, 323–339 (2014).
Zona, D. et al. Proc. Natl Acad. Sci. USA 113, 40–45 (2016).
Author information
Authors and Affiliations
Corresponding author
Related links
Rights and permissions
About this article
Cite this article
Zona, D. Long-term effects of permafrost thaw. Nature 537, 625–626 (2016). https://doi.org/10.1038/537625a
Published:
Issue Date:
DOI: https://doi.org/10.1038/537625a
- Springer Nature Limited
This article is cited by
-
Global cooling induced by biophysical effects of bioenergy crop cultivation
Nature Communications (2021)