A minimal machine-learning glacier mass balance model

• Main Authors: van der Meer, Marijn, id_orcid:0 000-0002-7604-4494, Zekollari, Harry, id_orcid:0 000-0002-7443-4034, Huss, Matthias, id_orcid:0 000-0002-2377-6923, Bolibar, Jordi, Hauknes Sjursen, Kamilla, Farinotti, Daniel, id_orcid:0 000-0003-3417-4570
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus 2025
• Subjects: The Cryosphere
• Online Access: https://hdl.handle.net/20.500.11850/724724; https://doi.org/10.3929/ethz-b-000724724

Glacier retreat presents significant environmental and social challenges. Understanding the local impacts of climatic drivers on glacier evolution is crucial, with mass balance being a central concept. This study introduces miniML-MB, a new minimal machine-learning model designed to estimate annual point surface mass balance (PMB) for very small datasets. Based on an eXtreme Gradient Boosting (XGBoost) architecture, miniML-MB is applied to model PMB at individual sites in the Swiss Alps, emphasising the need for an appropriate training framework and dimensionality reduction techniques. A substantial added value of miniML-MB is its data-driven identification of key climatic drivers of local mass balance. The best PMB prediction performance was achieved with two predictors: mean air temperature (May–August) and total precipitation (October–February). miniML-MB models PMB accurately from 1961 to 2021, with a mean absolute error (MAE) of 0.417 m w.e. across all sites. Notably, miniML-MB demonstrates similar and, in most cases, superior predictive capabilities compared to a simple positive degree-day (PDD) model (MAE of 0.541 m w.e.). Compared to the PDD model, miniML-MB is less effective at reproducing extreme mass balance values (e.g. 2022) that fall outside its training range. As such, miniML-MB shows promise as a gap-filling tool for sites with incomplete PMB measurements as long as the missing year's climate conditions are within the training range. This study underscores potential means for further refinement and broader applications of data-driven approaches in glaciology. ISSN:1994-0416 ISSN:1994-0424