Articles | Volume 11, issue 5
https://doi.org/10.5194/tc-11-2305-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/tc-11-2305-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue editorial
| 
05 Oct 2017
Special issue editorial |
| 05 Oct 2017
Discovery and characterization of submarine groundwater discharge in the Siberian Arctic seas: a case study in the Buor-Khaya Gulf, Laptev Sea
Alexander N. Charkin
CORRESPONDING AUTHOR
Pacific Oceanological Institute (POI), Far Eastern Branch of
Russian Academy of Sciences Russian Academy of Sciences (FEBRAS),
Vladivostok, Russia
Department of Geology and Minerals Prospecting, National Research Tomsk Polytechnic
University, Tomsk,
Russia
Michiel Rutgers van der Loeff
Department of Geochemistry, Alfred-Wegener Institute, Helmholtz Center for Polar and
Marine Research, Bremerhaven, Germany
Natalia E. Shakhova
Department of Geology and Minerals Prospecting, National Research Tomsk Polytechnic
University, Tomsk,
Russia
International Arctic Research Center (IARC), University of
Alaska, Fairbanks, USA
Örjan Gustafsson
Dept. of Environmental Science and Analytical Chemistry, and
the Bolin Centre for Climate Research, Stockholm University,
Stockholm, Sweden
Oleg V. Dudarev
Pacific Oceanological Institute (POI), Far Eastern Branch of
Russian Academy of Sciences Russian Academy of Sciences (FEBRAS),
Vladivostok, Russia
Department of Geology and Minerals Prospecting, National Research Tomsk Polytechnic
University, Tomsk,
Russia
Maxim S. Cherepnev
Department of Geology and Minerals Prospecting, National Research Tomsk Polytechnic
University, Tomsk,
Russia
Anatoly N. Salyuk
Pacific Oceanological Institute (POI), Far Eastern Branch of
Russian Academy of Sciences Russian Academy of Sciences (FEBRAS),
Vladivostok, Russia
Andrey V. Koshurnikov
Department of Geocryology, Moscow State University, Moscow, Russia
Eduard A. Spivak
Pacific Oceanological Institute (POI), Far Eastern Branch of
Russian Academy of Sciences Russian Academy of Sciences (FEBRAS),
Vladivostok, Russia
Alexey Y. Gunar
Department of Geocryology, Moscow State University, Moscow, Russia
Alexey S. Ruban
Department of Geology and Minerals Prospecting, National Research Tomsk Polytechnic
University, Tomsk,
Russia
Igor P. Semiletov
Pacific Oceanological Institute (POI), Far Eastern Branch of
Russian Academy of Sciences Russian Academy of Sciences (FEBRAS),
Vladivostok, Russia
Department of Geology and Minerals Prospecting, National Research Tomsk Polytechnic
University, Tomsk,
Russia
International Arctic Research Center (IARC), University of
Alaska, Fairbanks, USA
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Latest update: 30 May 2025
Short summary
This study tests the hypothesis that SGD exists in the Siberian Arctic shelf seas, but its dynamics may be largely controlled by complicated geocryological conditions such as permafrost. The permafrost cements rocks, forms a confining bed, and as a result makes it difficult for the groundwater escape to the shelf surface. However, the discovery of subterranean outcrops of groundwater springs in the Buor-Khaya Gulf are clear evidence that a groundwater flow system exists in the environment.
This study tests the hypothesis that SGD exists in the Siberian Arctic shelf seas, but its...
Special issue