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Assessing Climate and Watershed Controls on Rain-on-Snow Runoff Using XGBoost-SHAP Explainable AI (XAI)

Assessing Climate and Watershed Controls on Rain-on-Snow Runoff Using XGBoost-SHAP Explainable AI (XAI)

This is a Preprint and has not been peer reviewed. This is version 2 of this Preprint.

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Authors

Yog Aryal 

Abstract

Rain-on-snow (ROS) events significantly impact hydrological processes in snowy regions, yet their seasonal drivers remain poorly understood, particularly in low-elevation and low-gradient catchments. This study uses an XGBoost-SHAP explainable artificial intelligence (XAI) model to analyze meteorological and watershed controls on ROS runoff in the Great Lakes Basin.  We used daily discharge, precipitation, temperature, and snow depth data from 2000 to 2023, available from HYSETS, to identify ROS runoff. The models demonstrated acceptable predictive accuracy for ROS runoff, with winter achieving higher performance (R² = 0.65, Nash-Sutcliffe = 0.59) than spring (R² = 0.56, Nash-Sutcliffe = 0.49), indicating greater predictability during colder months. The results reveal that Winter runoff is predominantly governed by climatic factors—rainfall, air temperature, and their interactions—with soil permeability and slope orientation playing secondary roles. In contrast, spring runoff shows increased sensitivity to land cover characteristics, particularly agricultural and shrub cover, as vegetation-driven processes become more influential. Snow depth effects shift from predominantly negative in winter, where snow acts as storage, to positive contributions in spring at shallow to moderate depths. ROS runoff responded positively to air temperatures exceeding approximately 2.5°C in both winter and spring. Land cover influences on ROS runoff differ by vegetation type and season. Agricultural areas consistently increase runoff in both seasons due to limited infiltration, whereas shrub-dominated regions exhibit stronger runoff enhancement in spring. The seasonal shift in dominant controls underscores the importance of accounting for land–climate interactions in predicting ROS runoff under future climate scenarios. These insights are essential for improving flood forecasting, managing water resources, and developing adaptive strategies. 

DOI

https://doi.org/10.31223/X5HT70

Subjects

Climate, Fresh Water Studies, Hydrology, Meteorology, Water Resource Management

Keywords

Rain-on-Snow, interpretable machine learning, XGBoost, SHAP

Dates

Published: 2025-06-27 11:47

Last Updated: 2025-06-28 06:08

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License

CC-BY Attribution-NonCommercial 4.0 International