TY - JOUR
T1 - A minimal machine-learning glacier mass balance model
AU - Meer, Marijn van der
AU - Zekollari, Harry
AU - Huss, Matthias
AU - Bolibar, Jordi
AU - Sjursen, Kamilla Hauknes
AU - Farinotti, Daniel
N1 - Funding Information:
Harry Zekollari received financial support from the Research Foundation \u2013 Flanders (FWO) through an Odysseus Type II project (grant no. G0DCA23N; \u201CGlaciersMD\u201D project) and from the European Research Council (ERC) under the Horizon Framework research and innovation programme of the European Union (grant no. 101115565; \u201CICE3\u201D project).
Funding Information:
This paper resulted from the doctoral research by Marijn van der Meer at ETH Z\u00FCrich, supervised by Daniel Farinotti and Harry Zekollari. Harry Zekollari received financial support from the Research Foundation - Flanders (FWO) through an Odysseus Type II project (grant no. G0DCA23N; \"GlaciersMD\"project) and from the European Research Council (ERC) under the Horizon Framework research and innovation programme of the European Union (grant no. 101115565; \"ICE3\"project).
Publisher Copyright:
© Author(s) 2025.
PY - 2025/2/21
Y1 - 2025/2/21
N2 - 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.
AB - 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.
UR - http://dx.doi.org/10.5194/tc-19-805-2025
UR - http://www.scopus.com/inward/record.url?scp=85219041148&partnerID=8YFLogxK
U2 - 10.5194/tc-19-805-2025
DO - 10.5194/tc-19-805-2025
M3 - Article
SN - 1994-0416
VL - 19
SP - 805
EP - 826
JO - The Cryosphere
JF - The Cryosphere
IS - 2
ER -