Articles | Volume 27, issue 11
https://doi.org/10.5194/hess-27-2173-2023
https://doi.org/10.5194/hess-27-2173-2023
Research article
 | 
09 Jun 2023
Research article |  | 09 Jun 2023

Hydrological, meteorological, and watershed controls on the water balance of thermokarst lakes between Inuvik and Tuktoyaktuk, Northwest Territories, Canada

Evan J. Wilcox, Brent B. Wolfe, and Philip Marsh

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Cited articles

Andresen, C. G. and Lougheed, V. L.: Disappearing Arctic tundra ponds: Fine-scale analysis of surface hydrology in drained thaw lake basins over a 65 year period (1948–2013), J. Geophys. Res.-Biogeo., 120, 466–479, https://doi.org/10.1002/2014JG002778, 2015. a, b
Arp, C. D., Jones, B. M., Urban, F. E., and Grosse, G.: Hydrogeomorphic processes of thermokarst lakes with grounded-ice and floating-ice regimes on the Arctic coastal plain, Alaska, Hydrol. Process., 25, 2422–2438, https://doi.org/10.1002/hyp.8019, 2011. a, b
Arp, C. D., Jones, B. M., Liljedahl, A. K., Hinkel, K. M., and Welker, J. A.: Depth, ice thickness, and ice-out timing cause divergent hydrologic responses among Arctic lakes, Water Resour. Res., 51, 9379–9401, https://doi.org/10.1016/0022-1694(68)90080-2, 2015. a, b, c, d
Bartsch, A., Widhalm, B., Leibman, M., Ermokhina, K., Kumpula, T., Skarin, A., Wilcox, E. J., Jones, B. M., Frost, G. V., Höfler, A., and Pointner, G.: Feasibility of tundra vegetation height retrieval from Sentinel-1 and Sentinel-2 data, Remote Sens. Environ., 237, 111515, https://doi.org/10.1016/j.rse.2019.111515, 2020. a
Bergmann, M. A. and Welch, H. E.: Spring Meltwater Mixing in Small Arctic Lakes, Can. J. Fish. Aquat. Sci., 42, 1789–1798, https://doi.org/10.1139/f85-224, 1985. a, b
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Short summary
The Arctic is warming quickly and influencing lake water balances. We used water isotope concentrations taken from samples of 25 lakes in the Canadian Arctic and estimated the average ratio of evaporation to inflow (E / I) for each lake. The ratio of watershed area (the area that flows into the lake) to lake area (WA / LA) strongly predicted E / I, as lakes with relatively smaller watersheds received less inflow. The WA / LA could be used to predict the vulnerability of Arctic lakes to future change.
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