The Aneto glacier's (Central Pyrenees) evolution from 1981 to 2022: ice lossobserved from historic aerial image photogrammetry and remote sensingtechniques

The Aneto glacier, although it may be considered a very small glacier (<0.5 km2), is the largest glacier in the Pyrenees. Its surface and thickness loss have been continuous in recent decades, and there have been signs of accelerated melting in recent years. In this study, thickness and surface losses of the Aneto glacier from 1981 to 2022 are investigated using historical aerial imagery, airborne lidar point clouds and unoccupied aerial vehicle (UAV) imagery. A ground-penetrating radar (GPR) survey conducted in 2020, combined with data from photogrammetric analyses, allowed us to reconstruct the current ice thickness and also the existing ice distribution in 1981 and 2011. Over the last 41 years, the total glacierised area has decreased by 64.7 %, and the ice thickness has decreased, on average, by 30.5 m. The mean remaining ice thickness in autumn 2022 was 11.9 m, as against the mean thickness of 32.9, 19.2 and 15.0 m reconstructed for 1981 and 2011 and observed in 2020, respectively. The results demonstrate the critical situation of the glacier, with an imminent segmentation into two smaller ice bodies and no evidence of an accumulation zone. We also found that the occurrence of an extremely hot and dry year, as observed in the 2021-2022 season, leads to a drastic degradation of the glacier, posing a high risk to the persistence of the Aneto glacier, a situation that could extend to the rest of the Pyrenean glaciers in a relatively short time.

Automated summary

The Aneto glacier, the largest in the Pyrenees, has been continuously melting in recent decades, with signs of accelerated melting in recent years. From 1981 to 2022, the glacier's surface and thickness have decreased, with a 64.7% reduction in glacierized area and an average thickness loss of 30.5 meters. The current average remaining thickness is 11.9 meters, indicating the critical situation of the glacier and the potential segmentation into two smaller ice bodies.