Articles | Volume 11, issue 23
Biogeosciences, 11, 6573–6593, 2014
https://doi.org/10.5194/bg-11-6573-2014
Biogeosciences, 11, 6573–6593, 2014
https://doi.org/10.5194/bg-11-6573-2014
Research article
 | Highlight paper
01 Dec 2014
Research article  | Highlight paper | 01 Dec 2014

Estimated stocks of circumpolar permafrost carbon with quantified uncertainty ranges and identified data gaps

G. Hugelius et al.

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Cited articles

Aylsworth, J., Burgess, M., Desrochers, D., Duk-Rodkin, A., Robertson, T., and Traynor, J.: Surficial geology, subsurface materials, and thaw sensitivity of sediments, in: The physical environment of the Mackenzie valley, Northwest territories: A base line for the assessment of environmental change, edited by: Dyke, L. D. and Brooks, G. R., Geological Survey of Canada, Ottawa, 31–39, 2000.
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Burke, E. J., Hartley, I. P., and Jones, C. D.: Uncertainties in the global temperature change caused by carbon release from permafrost thawing, The Cryosphere, 6, 1063–1076, https://doi.org/10.5194/tc-6-1063-2012, 2012a.
Burke, E. J., Jones, C. D., and Koven, C. D.: Estimating the permafrost-carbon climate response in the CMIP5 climate models using a simplified approach, J. Climate, 26, 4897–4909, https://doi.org/10.1175/jcli-d-12-00550.1, 2012b.
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Short summary
This study provides an updated estimate of organic carbon stored in the northern permafrost region. The study includes estimates for carbon in soils (0 to 3 m depth) and deeper sediments in river deltas and the Yedoma region. We find that field data is still scarce from many regions. Total estimated carbon storage is ~1300 Pg with an uncertainty range of between 1100 and 1500 Pg. Around 800 Pg carbon is perennially frozen, equivalent to all carbon dioxide currently in the Earth's atmosphere.
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