Articles | Volume 11, issue 5
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, Michiel Rutgers van der Loeff, Natalia E. Shakhova, Örjan Gustafsson, Oleg V. Dudarev, Maxim S. Cherepnev, Anatoly N. Salyuk, Andrey V. Koshurnikov, Eduard A. Spivak, Alexey Y. Gunar, Alexey S. Ruban, and Igor P. Semiletov

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The spatial and interannual dynamics of the surface water carbonate system and air–sea CO2 fluxes in the outer shelf and slope of the Eurasian Arctic Ocean
Irina I. Pipko, Svetlana P. Pugach, Igor P. Semiletov, Leif G. Anderson, Natalia E. Shakhova, Örjan Gustafsson, Irina A. Repina, Eduard A. Spivak, Alexander N. Charkin, Anatoly N. Salyuk, Kseniia P. Shcherbakova, Elena V. Panova, and Oleg V. Dudarev
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Space–time dynamics of carbon and environmental parameters related to carbon dioxide emissions in the Buor-Khaya Bay and adjacent part of the Laptev Sea
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Cited articles

Anderson, B., Bryant, I., Lülig, M., Spies, B., and and Helbig, K.: Oilfield anisotropy: its origins and electrical characteristics, Oilfield Rev., 6, 48–56, 1994.
Antonov, V. S.: Mouth area of the Lena river (hydrological sketch), Hydrometizdat, Leningrad, 1–107, 1987.
Baker, G. C. and Osterkamp., T. E.: Salt distribution during freezing of saline sand columns at constant rates, Water Resour. Res., 25, 1825–1831, 1989.
Barry, R. G. and Serreze., M. C.: Atmospheric components of the arctic ocean freshwater balance and their interannual variability, in: The Freshwater Budget of the Arctic Ocean, edited by: Lewis, E. L., Jones, E. P., Lemke, P., Prowse, T. D., and Wadhams, P., Springer, New York, 45–56, 2000.
Bisson, R. A.: Space-age integrated exploration and treatment of renewable regional sources of pristine ground water in fractured rock megawatersheds, Desalination, 99, 257–273, 1994.
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.