Articles | Volume 20, issue 5
https://doi.org/10.5194/tc-20-3025-2026
https://doi.org/10.5194/tc-20-3025-2026
Research article
 | 
22 May 2026
Research article |  | 22 May 2026

Mass changes of the Antarctic Peninsula ice sheet and peripheral glaciers, 2007–2021

Maud Bernat, Etienne Berthier, Amaury Dehecq, Romain Hugonnet, Joaquin M. C. Belart, Naomi Ochwat, Peter Kuipers Munneke, Elizabeth Case, Ted Scambos, Louis-Marie Gauer, and David Youssefi

Data sets

Mass changes of the Antarctic Peninsula ice sheet and peripheral glaciers, 2007–2021 M. Bernat et al. https://doi.org/10.5281/zenodo.19593987

Output from the Glacier Energy and Mass Balance (GEMB v1.0) forced with 3-hourly ERA5 fields and gridded to 10 km, Greenland and Antarctica 1979-2024 N.-J. Schlegel and A. Gardner https://doi.org/10.5281/zenodo.14714746

IMAU-FDM v1.2A variables over Antarctica (1979-2023) S. Veldhuijsen et al. https://doi.org/10.5281/zenodo.14634258

NASA GSFC Firn Densification Model version 1.2.1 (GSFC-FDMv1.2.1) for the Greenland and Antarctic Ice Sheets: 1980-2021 B. Medley et al. https://doi.org/10.5281/zenodo.7054574

Model code and software

NeoGeographyToolkit/StereoPipeline: ASP 3.3.0 O. Alexandrov et al. https://doi.org/10.5281/zenodo.8270270

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Short summary
The Antarctic Peninsula is a mountainous region containing an ice sheet and peripheral glaciers. Differences remain between the methods used to estimate its mass changes. We use thousands of digital elevation models derived from high resolution stereoscopic images to calculate a new estimate of mass changes. We find that between 2007 and 2021, the ice sheet lost -28±6Gt/a and its peripheral glaciers -14±3Gt/a. We highlight the importance of resolving fine-scale changes in complex coastal areas.
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