The Cryosphere
The Cryosphere
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Articles | Volume 13, issue 6
Articles | Volume 13, issue 6
https://doi.org/10.5194/tc-13-1635-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-1635-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 13, issue 6
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, Nataliia Nesterova, David Andrew Post, Artem Sherstyukov, and Lyudmila Lebedeva

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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.
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