Articles | Volume 20, issue 4
https://doi.org/10.5194/tc-20-2257-2026
https://doi.org/10.5194/tc-20-2257-2026
Research article
 | 
21 Apr 2026
Research article |  | 21 Apr 2026

Glacial decline next to stable permafrost in the Dry Andes? Vertical glacier surface changes and rock glacier kinematics based on Pléiades imagery (Rodeo basin, 2019–2025)

Melanie Stammler, Jan Blöthe, Diego Cusicanqui, Simon Ebert, Rainer Bell, Xavier Bodin, and Lothar Schrott

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Short summary
Dry Andean (debris-covered) glaciers and rock glaciers are essential to river runoff by contributing meltwaters in this extremely arid area. We quantify surface lowering for 19 glaciers and 3 debris-covered glaciers, and unchanged velocities for 47 rock glaciers in a ground-truthed and Pléiades satellite imagery based integrative glacier-permafrost study on catchment-scale for 2019-2025. For this period, our findings indicate glacial decline next to permafrost stability.
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