EGU26-14578, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-14578
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Machine Learning and Remote Sensing Projections for Peruvian Glaciers (2016–2100)
Hugo Lepage1, Darina Andriychenko Leonenko1,2, Nina Elliott1, and Crispin Barnes1
Hugo Lepage et al.
  • 1Department of Physics, University of Cambridge, United Kingdom
  • 2Department of Physics, University of Oxford, United Kingdom

The Peruvian Andes contain over 70% of the world's tropical glaciers, which are vital for regional water security and are rapidly destabilising due to climate change. Current large-scale projections often lack the spatial resolution required for localised glacial melt modelling or rely on climate reanalysis products that are too coarse in rugged terrain. This study introduces a unified framework that combines high-resolution remote sensing (Sentinel-2, Landsat-8) with machine learning to characterise, monitor, and forecast glacial evolution across Peru from 2016 to 2100.

We propose a machine-learning modelling approach that addresses both the where and when of glacial retreat. We developed a spatial Random Forest classifier to generate country-wide melt vulnerability maps. Ensemble analysis of driving parameters reveals that "distance-to-edge" and topographic factors (elevation, slope) are significantly stronger predictors of melt spatiality than available coarse-resolution temperature and precipitation datasets. Our spatial model achieves a 74.9% overlap accuracy between simulated and observed melt (2016–2023), nearly doubling the performance of benchmark Multi-Criteria Decision Analysis methods (39.3%).

Complementing this spatial analysis, we developed a temporal, area-based melt model from annual inventories of over 2,000 individual glacier polygons. Using a Huber regression to fit negative power laws to ablation rates, we identified a clear acceleration in retreat for smaller ice bodies, consistent with albedo-ice feedback mechanisms. Between 2016 and 2023, we observed a relative area loss of 15 ± 4% (180 ± 70 km2).

Integrating these models to forecast future scenarios, we project that only ~30% (26–43%) of the 2020 glacial surface area will remain by 2100, with several cordilleras facing near-total extinction. This workflow establishes a new standard for observation-based, scalable glacial modelling, providing the high-resolution spatial and temporal insights necessary for effective water resource management and adaptation strategies in the tropical Andes.

How to cite: Lepage, H., Andriychenko Leonenko, D., Elliott, N., and Barnes, C.: Machine Learning and Remote Sensing Projections for Peruvian Glaciers (2016–2100), EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-14578, https://doi.org/10.5194/egusphere-egu26-14578, 2026.