Articles | Volume 20, issue 11
https://doi.org/10.5194/tc-20-6535-2026
https://doi.org/10.5194/tc-20-6535-2026
Research article
 | 
13 Nov 2026
Research article |  | 13 Nov 2026

Intra-annual grounding-line migration and retreat: insights from high-resolution satellite and in situ observations over Milne Glacier in the Canadian High Arctic

Yulia K. Antropova, Derek Mueller, Sergey V. Samsonov, Alexander S. Komarov, and Jérémie Bonneau

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Cited articles

Andersen, J. K., Millan, R., Rignot, E., Gimenes, L., Scheuchl, B., Barré, J. B., and Bjørk, A. A.: Brief communication: Updated grounding line mapping in the Amundsen Sea Embayment, Antarctica, from one day repeat Sentinel-1 SAR data, The Cryosphere, 20, 1589–1598, https://doi.org/10.5194/tc-20-1589-2026, 2026. 
Antropova, Y. K., Mueller, D., Samsonov, S. V., Komarov, A. S., Bonneau, J., and Crawford, A. J.: Grounding-line retreat of Milne Glacier, Ellesmere Island, Canada over 1966–2023 from satellite, airborne, and ground radar data, Remote Sens. Environ., 315, 114478, https://doi.org/10.1016/j.rse.2024.114478, 2024. 
Black, T. E. and Joughin, I.: Multi-decadal retreat of marine-terminating outlet glaciers in northwest and central-west Greenland, The Cryosphere, 16, 807–824, https://doi.org/10.5194/tc-16-807-2022, 2022. 
Bonneau, J., Laval, B. E., Mueller, D., Hamilton, A. K., and Crawford, A. J.: Heat fluxes in a glacial fjord: the role of buoyancy-driven circulation and offshore forcing, Geophys. Res. Lett., 51, e2024GL111242, https://doi.org/10.1029/2024GL111242, 2024a. 
Bonneau, J., Laval, B. E., Mueller, D., Hamilton, A. K., and Forrest, A. L.: Unsteady circulation in a glacial fjord: a multiyear modeling study of Milne Fiord, J. Geophys. Res.-Oceans, 129, e2023JC020140, https://doi.org/10.1029/2023JC020140, 2024b. 
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Short summary
Arctic glaciers that flow into the ocean are changing rapidly due to climate warming. The grounding line, where these glaciers transition from land to ocean, is critical to their stability. We examined Milne Glacier in the Canadian High Arctic using satellite, field, and modelled data. Our study shows how changes in ice flow and ice bending near the grounding line affect satellite-based mapping of this area and documents a newly discovered grounding-line retreat associated with subglacial ridges.
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