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Biogeosciences An interactive open-access journal of the European Geosciences Union
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BG | Volume 15, issue 22
Biogeosciences, 15, 6867–6884, 2018
https://doi.org/10.5194/bg-15-6867-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Biogeosciences, 15, 6867–6884, 2018
https://doi.org/10.5194/bg-15-6867-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

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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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (24 Aug 2018) by Nobuhito Ohte
AR by O.S. Pokrovsky on behalf of the Authors (26 Aug 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (11 Sep 2018) by Nobuhito Ohte
RR by Anonymous Referee #1 (24 Sep 2018)
ED: Publish subject to minor revisions (review by editor) (10 Oct 2018) by Nobuhito Ohte
AR by O.S. Pokrovsky on behalf of the Authors (12 Oct 2018)  Author's response    Manuscript
ED: Publish as is (29 Oct 2018) by Nobuhito Ohte
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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.
We tested the effect of climate, permafrost and physio-geographical landscape parameters on...
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