Articles | Volume 15, issue 22
Biogeosciences, 15, 6867–6884, 2018
https://doi.org/10.5194/bg-15-6867-2018
Biogeosciences, 15, 6867–6884, 2018
https://doi.org/10.5194/bg-15-6867-2018

Research article 19 Nov 2018

Research article | 19 Nov 2018

Riverine particulate C and N generated at the permafrost thaw front: case study of western Siberian rivers across a 1700 km latitudinal transect

Ivan V. Krickov et al.

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Cited articles

Ala-aho, P., Soulsby, C., Pokrovsky, O. S., Kirpotin, S. N., Karlsson, J., Serikova, S., Manasypov, R. M., Krickov, I., Lim, A., and Tetzlaff, D.: Permafrost and lakes control river isotope composition across a boreal-arctic transect in the western Siberia lowland, Environ. Res. Lett., 13, 034028, https://doi.org/10.1088/1748-9326/aaa4fe, 2018a. 
Ala-Aho, P., Soulsby, C., Pokrovsky, O. S., Kirpotin, S. N., Karlsson, J., Serikova, S., Vorobyev, S. N., Manasypov, R. M., Loiko, S., and Tetzlaff, D.: Using stable isotopes to assess surface water source dynamics and hydrological connectivity in a high-latitude wetland and permafrost influenced landscape, J. Hydrol., 556, 279–293, https://doi.org/10.1016/j.jhydrol.2017.11.024, 2018b. 
Anisimov, O. and Reneva, S.: Permafrost and Changing Climate: The Russian Perspective, AMBIO, 35, 169–175, 2006. 
Anisimov, O. A. and Sherstiukov, A. B.: Evaluating the effect of climatic and environmental factors on permafrost in Russia, Earth's Cryosphere, XX, 78–86, 2016. 
Anisimov, O. A., Zhiltsova, E. L., and Reneva, S. A.: Estimation of critical levels of climate change impact on natural land ecosystems of Russian territory, Meteorology and Hydrology, 11, 723–730, https://doi.org/10.3103/S1068373911110033, 2011. 
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Short summary
We tested the effect of climate, permafrost and physio-geographical landscape parameters on particulate C, N and P concentrations in small- and medium- sized rivers in the Western Siberian Lowland (WSL). We discovered a maximum of particulate C and N concentrations at the beginning of the permafrost appearance. A northward shift of permafrost boundaries may increase the particulate C and N export by WSL rivers to the Arctic Ocean by a factor of 2.
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