Articles | Volume 16, issue 7
https://doi.org/10.5194/tc-16-2837-2022
https://doi.org/10.5194/tc-16-2837-2022
Research article
 | 
19 Jul 2022
Research article |  | 19 Jul 2022

Contrasted geomorphological and limnological properties of thermokarst lakes formed in buried glacier ice and ice-wedge polygon terrain

Stéphanie Coulombe, Daniel Fortier, Frédéric Bouchard, Michel Paquette, Simon Charbonneau, Denis Lacelle, Isabelle Laurion, and Reinhard Pienitz

Data sets

Morphometry of glacial lakes formed in front of glaciers C-93 and C-79, Bylot Island, Nunavut Daniel Fortier and Stephanie Coulombe https://www.cen.ulaval.ca/nordicanad/dpage.aspx?DOI=45765CE-0DBCF1FE81114010

Organic matter content and grain size distribution in a lake sediment core, Bylot Island, Nunavut, Canada Daniel Fortier, Frédéric Bouchard, Zhaoyi Zhang, and Stéphanie Coulombe https://doi.org/10.5885/45603CE-21852993EE434926

Radiocarbon (14C) dates in terrestrial and aquatic environments, Bylot Island, Nunavut”, Daniel Fortier, Frédéric Bouchard, Isabelle Laurion, Reinhard Pienitz, and Michel Allard https://doi.org/10.5885/45651CE-C6FD628F45E44578

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Short summary
Buried glacier ice is widespread in Arctic regions that were once covered by glaciers and ice sheets. In this study, we investigated the influence of buried glacier ice on the formation of Arctic tundra lakes on Bylot Island, Nunavut. Our results suggest that initiation of deeper lakes was triggered by the melting of buried glacier ice. Given future climate projections, the melting of glacier ice permafrost could create new aquatic ecosystems and strongly modify existing ones.