Ice cover decay and heat balance in Lake Kilpisjärvi in Arctic tundra

Ice decay in Lake Kilpisjärvi

Abstract

To gain more understanding of lake ice melting process, field research was carried out in an arctic tundra lake, Kilpisjärvi (surface area 37.1 km2, maximum depth 57 m) in the melting periods of 2013 and 2014. The heat budget of the ice cover was dominated by the radiation balance; turbulent heat fluxes were large in 2013 due to warm air advection but small in 2014. Transmittance of solar radiation through ice was 0.25 in 2013 and 0.10 in 2014, snow-ice was absent in 2013 but in 2014 accounted for 50% of the ice cover. The melting rate was 4.4 cm    d-1 in 2013, 1.9 cm d-1 in 2014. The portions of surface, bottom and internal melting were, respectively, 2.9, 1.0 and 0.5 cm d-1 in 2013 and 0.8, 1.0 and 0.1 cm d-1 in 2014. Internal melting was realized in increase of ice porosity. In 2013 a rapid ice breakage event completed the ice breakup in short time when ice porosity had reached 40-50%. A lake ice melting model should include the thickness and porosity of ice, with porosity connected to an ice strength criterion.

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Author Biographies

Matti Leppäranta, University of Helsinki, Institute of Atmospheric and Earth Sciences

Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Region, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China

Lijuan Wen, Chinese Academy of Sciences, Northwest Institute of Eco-Environment and Resources

Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Region

Published
2019-02-21
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Section
Original Articles
Edited By
Franco Tassi, University of Florence, Italy
Keywords:
Lake ice, melting, solar radiation, heat budget, light transfer
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How to Cite
1.
Leppäranta M, Lindgren E, Wen L, Kirillin G. Ice cover decay and heat balance in Lake Kilpisjärvi in Arctic tundra: Ice decay in Lake Kilpisjärvi. J Limnol [Internet]. 2019Feb.21 [cited 2020May25];78(2). Available from: https://jlimnol.it/index.php/jlimnol/article/view/jlimnol.2019.1879