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Size Distribution, Surface Coverage, Water, Carbon, and Metal Storage of Thermokarst Lakes in the Permafrost Zone of the Western Siberia Lowland

Ugra Research Institute of Information Technologies, Mira str., 151, Khanty-Mansiysk 628011, Russia
Institute of Petroleum Chemistry SB RAS, 4 Akademichesky av., Tomsk 634021, Russia
Institute of Monitoring of Climate and Ecological Systems SB RAS, 10/3 Akademichesky av., Tomsk 634021, Russia
Tomsk Polytechnic University, Lenina av., 30, Tomsk 634004, Russia
BIO-GEO-CLIM Laboratory, Tomsk State University, Lenina av., 36, Tomsk 634004, Russia
Federal Center for Integrated Arctic research, Institute of Ecological Problem of the North, 23 Nab Severnoi Dviny, Arkhangelsk 163000, Russia
GET UMR 5563 CNRS University of Toulouse (France), 14 Avenue Edouard Belin, 31400 Toulouse, France
Author to whom correspondence should be addressed.
Academic Editors: Frédéric Frappart and Luc Bourrel
Water 2017, 9(3), 228;
Received: 13 January 2017 / Revised: 12 March 2017 / Accepted: 14 March 2017 / Published: 21 March 2017
(This article belongs to the Special Issue The Use of Remote Sensing in Hydrology)
Despite the importance of thermokarst (thaw) lakes of the subarctic zone in regulating greenhouse gas exchange with the atmosphere and the flux of metal pollutants and micro-nutrients to the ocean, the inventory of lake distribution and stock of solutes for the permafrost-affected zone are not available. We quantified the abundance of thermokarst lakes in the continuous, discontinuous, and sporadic permafrost zones of the western Siberian Lowland (WSL) using Landsat-8 scenes collected over the summers of 2013 and 2014. In a territory of 105 million ha, the total number of lakes >0.5 ha is 727,700, with a total surface area of 5.97 million ha, yielding an average lake coverage of 5.69% of the territory. Small lakes (0.5–1.0 ha) constitute about one third of the total number of lakes in the permafrost-bearing zone of WSL, yet their surface area does not exceed 2.9% of the total area of lakes in WSL. The latitudinal pattern of lake number and surface coverage follows the local topography and dominant landscape zones. The role of thermokarst lakes in dissolved organic carbon (DOC) and most trace element storage in the territory of WSL is non-negligible compared to that of rivers. The annual lake storage across the WSL of DOC, Cd, Pb, Cr, and Al constitutes 16%, 34%, 37%, 57%, and 73%, respectively, of their annual delivery by WSL rivers to the Arctic Ocean from the same territory. However, given that the concentrations of DOC and metals in the smallest lakes (<0.5 ha) are much higher than those in the medium and large lakes, the contribution of small lakes to the overall carbon and metal budget may be comparable to, or greater than, their contribution to the water storage. As such, observations at high spatial resolution (<0.5 ha) are needed to constrain the reservoirs and the mobility of carbon and metals in aquatic systems. To upscale the DOC and metal storage in lakes of the whole subarctic, the remote sensing should be coupled with hydrochemical measurements in aquatic systems of boreal plains. View Full-Text
Keywords: remote sensing; size; surface; volume; thermokarst; carbon; metal remote sensing; size; surface; volume; thermokarst; carbon; metal
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Polishchuk, Y.M.; Bogdanov, A.N.; Polishchuk, V.Y.; Manasypov, R.M.; Shirokova, L.S.; Kirpotin, S.N.; Pokrovsky, O.S. Size Distribution, Surface Coverage, Water, Carbon, and Metal Storage of Thermokarst Lakes in the Permafrost Zone of the Western Siberia Lowland. Water 2017, 9, 228.

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