Articles | Volume 20, issue 5
https://doi.org/10.5194/tc-20-2999-2026
https://doi.org/10.5194/tc-20-2999-2026
Research article
 | 
22 May 2026
Research article |  | 22 May 2026

Future Retreat of Great Aletsch Glacier and Hintereisferner – application of a full-Stokes model to two valley glaciers in the European Alps

Martin Rückamp, Gong Cheng, Karlheinz Gutjahr, Marco Möller, Petri K. E. Pellikka, and Christoph Mayer

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (24 Feb 2026) by Nicholas Barrand
AR by Martin Rückamp on behalf of the Authors (01 Apr 2026)  Author's response   Author's tracked changes   Manuscript 
EF by Mario Ebel (07 Apr 2026)  Supplement 
ED: Publish subject to minor revisions (review by editor) (15 Apr 2026) by Nicholas Barrand
ED: Publish as is (24 Apr 2026) by Nicholas Barrand
AR by Martin Rückamp on behalf of the Authors (03 May 2026)  Author's response   Manuscript 

Post-review adjustments

AA – Author's adjustment | EA – Editor approval
AA by Martin Rückamp on behalf of the Authors (15 May 2026)   Author's adjustment   Manuscript
EA: Adjustments approved (15 May 2026) by Nicholas Barrand
Download
Short summary
The study simulates the 21st-century evolution of Great Aletsch Glacier and Hintereisferner using full-Stokes ice dynamics and surface mass balance under different emission scenarios. Results show significant ice loss, with Hintereisferner expected to disappear by mid-century. Great Aletsch Glacier vanish by the end of the century under high-emission scenarios, but persist under lower-emission scenarios. These trends agree with large-scale models except some variability.
Share