High riverine CO2 emissions at the permafrost boundary of Western Siberia

S. Serikova* (Corresponding Author), O. S. Pokrovsky, P. Ala-Aho, V. Kazantsev, S. N. Kirpotin, S. G. Kopysov, I. V. Krickov, H. Laudon, R. M. Manasypov, L. S. Shirokova, C. Soulsby, D. Tetzlaff, J. Karlsson (Corresponding Author)

*Corresponding author for this work

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Abstract

The fate of the vast stocks of organic carbon stored in permafrost of the Western Siberian Lowland, the world’s largest peatland, is uncertain. Specifically, the amount of greenhouse gas emissions from rivers in the region is unknown. Here we present estimates of annual CO2 emissions from 58 rivers across all permafrost zones of the Western Siberian Lowland, between 56 and 67° N. We find that emissions peak at the permafrost boundary, and decrease where permafrost is more prevalent and in colder climatic conditions. River CO2 emissions were high, and on average two times greater than downstream carbon export. We suggest that high emissions and emission/export ratios are a result of warm temperatures and the long transit times of river water. We show that rivers in the Western Siberian Lowland play an important role in the carbon cycle by degassing terrestrial carbon before its transport to the Arctic Ocean, and suggest that changes in both temperature and precipitation are important for understanding and predicting high-latitude river CO2 emissions in a changing climate.

Original languageEnglish
Pages (from-to)825-829
Number of pages5
JournalNature Geoscience
Volume11
Early online date3 Sep 2018
DOIs
Publication statusPublished - 3 Sep 2018

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permafrost
river
carbon
degassing
peatland
carbon cycle
river water
greenhouse gas
temperature
organic carbon
climate

Keywords

  • carbon cycle
  • climate-change impacts
  • limnology

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)

Cite this

Serikova, S., Pokrovsky, O. S., Ala-Aho, P., Kazantsev, V., Kirpotin, S. N., Kopysov, S. G., ... Karlsson, J. (2018). High riverine CO2 emissions at the permafrost boundary of Western Siberia. Nature Geoscience, 11, 825-829. https://doi.org/10.1038/s41561-018-0218-1

High riverine CO2 emissions at the permafrost boundary of Western Siberia. / Serikova, S. (Corresponding Author); Pokrovsky, O. S.; Ala-Aho, P.; Kazantsev, V.; Kirpotin, S. N.; Kopysov, S. G.; Krickov, I. V.; Laudon, H.; Manasypov, R. M.; Shirokova, L. S.; Soulsby, C.; Tetzlaff, D.; Karlsson, J. (Corresponding Author).

In: Nature Geoscience, Vol. 11, 03.09.2018, p. 825-829.

Research output: Contribution to journalArticle

Serikova, S, Pokrovsky, OS, Ala-Aho, P, Kazantsev, V, Kirpotin, SN, Kopysov, SG, Krickov, IV, Laudon, H, Manasypov, RM, Shirokova, LS, Soulsby, C, Tetzlaff, D & Karlsson, J 2018, 'High riverine CO2 emissions at the permafrost boundary of Western Siberia', Nature Geoscience, vol. 11, pp. 825-829. https://doi.org/10.1038/s41561-018-0218-1
Serikova S, Pokrovsky OS, Ala-Aho P, Kazantsev V, Kirpotin SN, Kopysov SG et al. High riverine CO2 emissions at the permafrost boundary of Western Siberia. Nature Geoscience. 2018 Sep 3;11:825-829. https://doi.org/10.1038/s41561-018-0218-1
Serikova, S. ; Pokrovsky, O. S. ; Ala-Aho, P. ; Kazantsev, V. ; Kirpotin, S. N. ; Kopysov, S. G. ; Krickov, I. V. ; Laudon, H. ; Manasypov, R. M. ; Shirokova, L. S. ; Soulsby, C. ; Tetzlaff, D. ; Karlsson, J. / High riverine CO2 emissions at the permafrost boundary of Western Siberia. In: Nature Geoscience. 2018 ; Vol. 11. pp. 825-829.
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abstract = "The fate of the vast stocks of organic carbon stored in permafrost of the Western Siberian Lowland, the world’s largest peatland, is uncertain. Specifically, the amount of greenhouse gas emissions from rivers in the region is unknown. Here we present estimates of annual CO2 emissions from 58 rivers across all permafrost zones of the Western Siberian Lowland, between 56 and 67° N. We find that emissions peak at the permafrost boundary, and decrease where permafrost is more prevalent and in colder climatic conditions. River CO2 emissions were high, and on average two times greater than downstream carbon export. We suggest that high emissions and emission/export ratios are a result of warm temperatures and the long transit times of river water. We show that rivers in the Western Siberian Lowland play an important role in the carbon cycle by degassing terrestrial carbon before its transport to the Arctic Ocean, and suggest that changes in both temperature and precipitation are important for understanding and predicting high-latitude river CO2 emissions in a changing climate.",
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N1 - Acknowledgements: The study was part of the JPI Climate initiative, financially supported by VR (the Swedish Research Council) grant no. 325-2014-6898 to J.K. Additional funding from RNF (RSCF) grant no. 18-17-00237, RFBR grant no. 17-55-16008 and RF Federal Target Program RFMEFI58717X0036 ‘Kolmogorov’ to O.S.P. and S.N.K. as well as NERC grant no. NE/M019896/1 to C.S. is acknowledged. The authors thank A. Sorochinskiy and A. Lim for assistance in the field, as well as M. Myrstener, M. Klaus and S. Monteux for advice on data analysis. L. Kovaleva is acknowledged for artwork.

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