Articles | Volume 12, issue 21
https://doi.org/10.5194/bg-12-6301-2015
https://doi.org/10.5194/bg-12-6301-2015
Research article
 | 
05 Nov 2015
Research article |  | 05 Nov 2015

Permafrost coverage, watershed area and season control of dissolved carbon and major elements in western Siberian rivers

O. S. Pokrovsky, R. M. Manasypov, S. Loiko, L. S. Shirokova, I. A. Krickov, B. G. Pokrovsky, L. G. Kolesnichenko, S. G. Kopysov, V. A. Zemtzov, S. P. Kulizhsky, S. N. Vorobyev, and S. N. Kirpotin

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ED: Publish subject to minor revisions (Editor review) (14 Oct 2015) by Jorien Vonk
AR by O.S. Pokrovsky on behalf of the Authors (17 Oct 2015)  Author's response   Manuscript 
ED: Publish as is (20 Oct 2015) by Jorien Vonk
AR by O.S. Pokrovsky on behalf of the Authors (22 Oct 2015)
Short summary
The governing parameter of DOC and major element concentrations and fluxes in western Siberia is latitude. High fluxes in the continuous permafrost zone of frozen peat bogs stem from the fact that the underlining mineral layer is not reactive, protected by the permafrost so that the major part of the active layer is located within the organic (peat) matrix and not the mineral matrix. Possible changes in export fluxes of DOC and major river water components under permafrost thaw are quantified.
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