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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Volume 13, issue 6
The Cryosphere, 13, 1635–1659, 2019
https://doi.org/10.5194/tc-13-1635-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 13, 1635–1659, 2019
https://doi.org/10.5194/tc-13-1635-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 14 Jun 2019

Research article | 14 Jun 2019

Warming temperatures are impacting the hydrometeorological regime of Russian rivers in the zone of continuous permafrost

Olga Makarieva et al.
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Status: closed
Status: closed
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
AR by Olga Makarieva on behalf of the Authors (14 Feb 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (27 Feb 2019) by Valentina Radic
RR by Anonymous Referee #1 (05 Mar 2019)
ED: Publish subject to minor revisions (review by editor) (24 Mar 2019) by Valentina Radic
AR by Olga Makarieva on behalf of the Authors (03 Apr 2019)  Author's response    Manuscript
ED: Publish subject to technical corrections (19 Apr 2019) by Valentina Radic
AR by Olga Makarieva on behalf of the Authors (29 Apr 2019)  Author's response    Manuscript
Publications Copernicus
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Short summary
The streamflow of Arctic rivers is changing. We analyzed available data (22 gauges, 1936–2015) in the basins of the Yana and Indigirka rivers completely located within the continuous permafrost zone. The results show that the main factor of increasing low flows is the shift from snow to rain due to warming. Other factors related to the release of water from permafrost, glaciers, or aufeis may fractionally contribute to streamflow increase but cannot be quantified based on available data.
The streamflow of Arctic rivers is changing. We analyzed available data (22 gauges, 1936–2015)...
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