Articles | Volume 20, issue 9
https://doi.org/10.5194/tc-20-5071-2026
https://doi.org/10.5194/tc-20-5071-2026
Research article
 | 
09 Sep 2026
Research article |  | 09 Sep 2026

Mélange, landfast sea ice, ice velocities: What controls seasonal calving rates in North West Greenland?

Sofie Hedetoft, Olivia Bang Brinck, Ruth Mottram, Andrea M. U. Gierisch, Steffen Malskær Olsen, Martin Olesen, Nicolaj Hansen, Anders Anker Bjørk, Erik Loebel, Anne Solgaard, and Peter Thejll

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Short summary
Iceberg mélange is the jumble of icebergs in front of some glaciers that calve into the sea. Some studies suggest mélange might help to control the retreat of glaciers. We studied 3 glaciers in NW Greenland where we used GPS sensors and satellites to track ice movement. We found that glaciers push forward and calve all year, including when mélange and landfast sea ice are present, suggesting mélange is not important in supporting glaciers, but may influence the seasonal calving cycle.
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