Articles | Volume 21, issue 11
Hydrol. Earth Syst. Sci., 21, 5725–5746, 2017
https://doi.org/10.5194/hess-21-5725-2017
Hydrol. Earth Syst. Sci., 21, 5725–5746, 2017
https://doi.org/10.5194/hess-21-5725-2017

Research article 17 Nov 2017

Research article | 17 Nov 2017

Impact of snow deposition on major and trace element concentrations and elementary fluxes in surface waters of the Western Siberian Lowland across a 1700 km latitudinal gradient

Vladimir P. Shevchenko et al.

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by Editor and Referees) (04 Jul 2017) by Laurent Pfister
AR by O.S. Pokrovsky on behalf of the Authors (04 Jul 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Jul 2017) by Laurent Pfister
RR by Anonymous Referee #1 (09 Aug 2017)
ED: Publish subject to minor revisions (further review by Editor) (11 Sep 2017) by Laurent Pfister
AR by O.S. Pokrovsky on behalf of the Authors (12 Sep 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (15 Oct 2017) by Laurent Pfister
AR by O.S. Pokrovsky on behalf of the Authors (16 Oct 2017)  Author's response    Manuscript
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Short summary
We used a coupled hydrological–hydrochemical approach to assess the impact of snow on river and lake water chemistry across a permafrost gradient in very poorly studied Western Siberia Lowland (WSL), encompassing > 1.5 million km2. The riverine springtime fluxes of major and trace element in WSL rivers might be strongly overestimated due to previously unknown input from the snow deposition.