Articles | Volume 20, issue 3
https://doi.org/10.5194/tc-20-1699-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-20-1699-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Active subglacial lakes in the Canadian Arctic identified by multi-annual ice elevation changes
Center for Space and Remote Sensing Research, National Central University, Taoyuan City 320317, Taiwan
Taiwan Polar Institute, National Central University, Taoyuan City 320317, Taiwan
Wesley Van Wychen
Department of Geography and Environmental Management, University of Waterloo, Waterloo N2L 3G1, Ontario, Canada
Bristol Glaciology Centre, University of Bristol, Bristol BS8 1SS, United Kingdom
Tsutomu Yamanokuchi
Remote Sensing Technology Center of Japan, Tokyo 105-0001, Japan
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We design and propose a method that can evaluate the quality of glacier velocity maps. The method includes two numbers that we can calculate for each velocity map. Based on statistics and ice flow physics, velocity maps with numbers close to the recommended values are considered to have good quality. We test the method using the data from Kaskawulsh Glacier, Canada, and release an open-sourced software tool called GLAcier Feature Tracking testkit (GLAFT) to help users assess their velocity maps.
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Whyjay Zheng
The Cryosphere, 16, 1431–1445, https://doi.org/10.5194/tc-16-1431-2022, https://doi.org/10.5194/tc-16-1431-2022, 2022
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A glacier can speed up when surface water reaches the glacier's bottom via crevasses and reduces sliding friction. This paper builds up a physical model and finds that thick and fast-flowing glaciers are sensitive to this friction disruption. The data from Greenland and Austfonna (Svalbard) glaciers over 20 years support the model prediction. To estimate the projected sea-level rise better, these sensitive glaciers should be frequently monitored for potential future instabilities.
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Short summary
We identify lakes beneath the glaciers in the Canadian Arctic using satellite measurements over a decade, increasing the number of known subglacial lakes in this area from 2 to 37. These lakes are recharged by billions of cubic meters of water, and the draining of these lakes can lower the ice elevation by more than 100 m. We find three types of subglacial lakes, two of which are primarily located in the Canadian Arctic. When glaciers lose their ice quickly, these lakes become active.
We identify lakes beneath the glaciers in the Canadian Arctic using satellite measurements over...