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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- Seasonality of submarine groundwater discharge to an Arctic coastal lagoon E. Bullock et al. 10.1002/lno.12585
- In-situ temperatures and thermal properties of the East Siberian Arctic shelf sediments: Key input for understanding the dynamics of subsea permafrost E. Chuvilin et al. 10.1016/j.marpetgeo.2022.105550
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- Impact of winter freshwater from tidewater glaciers on fjords in Svalbard and Greenland; A review T. Vonnahme et al. 10.1016/j.pocean.2023.103144
- Subsea permafrost as a potential major source of dissolved organic matter to the East Siberian Arctic Shelf M. Chen et al. 10.1016/j.scitotenv.2021.146100
- The influence of sedimentation regime on natural radionuclide activity concentration in marine sediments of the East Siberian Arctic Shelf A. Charkin et al. 10.1016/j.jenvrad.2022.106988
- Change trends of mean ice thickness, water level, and surface salinity in the Laptev Sea in winter-spring period under further climate warming conditions S. Podporin & A. Kholoptsev 10.21821/2309-5180-2023-15-6-923-931
- Discharge of Meteoric Water in the Eastern Norwegian Sea since the Last Glacial Period W. Hong et al. 10.1029/2019GL084237
- Fluidogenic landforms on the Arctic shelves A. Kokhan et al. 10.55959/10.55959/MSU0579-9414.5.79.2.8
- Serpentine (Floating) Ice Channels and their Interaction with Riverbed Permafrost in the Lena River Delta, Russia B. Juhls et al. 10.3389/feart.2021.689941
- Evaluation of the Thermal Erosion of River Banks Based on Laboratory and Numerical Modeling E. Debolskaya et al. 10.1007/s10749-024-01777-z
- Vulnerability of Arctic-Boreal methane emissions to climate change F. Parmentier et al. 10.3389/fenvs.2024.1460155
- Hydrochemistry and isotopic signatures of subpermafrost groundwater discharge along the eastern slope of the Lena River Delta in the Laptev Sea A. Charkin et al. 10.1016/j.jhydrol.2020.125515
- Radium Isotopes Across the Arctic Ocean Show Time Scales of Water Mass Ventilation and Increasing Shelf Inputs M. Rutgers van der Loeff et al. 10.1029/2018JC013888
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- A unique warm–water oasis in the Siberian Arctic’s Chaun Bay sustained by hydrothermal groundwater discharge A. Charkin et al. 10.1038/s43247-024-01529-x
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- Recent advances (2010–2019) in the study of taliks H. O’Neill et al. 10.1002/ppp.2050
- Thermal properties of sediments in the East Siberian Arctic Seas: A case study in the Buor-Khaya Bay E. Chuvilin et al. 10.1016/j.marpetgeo.2020.104672
- Increased fluxes of shelf-derived materials to the central Arctic Ocean L. Kipp et al. 10.1126/sciadv.aao1302
- Heat and Salt Flow in Subsea Permafrost Modeled with CryoGRID2 M. Angelopoulos et al. 10.1029/2018JF004823
- Radioactivity of Surface Marine Sediments of Chaun Bay: Analysis of Natural and Anthropogenic Factors A. Ulyantsev et al. 10.3103/S0145875224700078
- Physical drivers of sediment-water interaction on the Beaufort Sea shelf J. Dabrowski et al. 10.1016/j.dsr.2022.103700
- Assessing the potential for non-turbulent methane escape from the East Siberian Arctic Shelf M. Puglini et al. 10.5194/bg-17-3247-2020
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1 citations as recorded by crossref.
Latest update: 23 Nov 2024
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