Prediction of Landslide Susceptibility in the Polroud Watershed Using Machine Learning Methods
Subject Areas : Natural disaster management
Marziyeh Heydari
1
,
Ali Fazlolahi
2
*
,
Seyed Pedram Nainiva
3
1 - M.Sc. Student, Department of Rang and Watershed Management, Faculty of Natural Resources, University of Guilan, Sowmehsara, Iran.
2 - Assistant Professor, Department of Rang and Watershed Management, Faculty of Natural Resources, University of Guilan, Sowmehsara, Iran.
3 - Ph.D. in Watershed Management, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran.
Keywords: Zonation, Random Forest, Geographic Information System (GIS), Natural Hazards, Slope Instability,
Abstract :
Landslides are among the most significant geomorphological hazards, posing a serious threat to natural resources, infrastructure, and human settlements. The aim of this study was to perform landslide susceptibility zonation in the Polrud Watershed using machine learning algorithms and to evaluate their performance comparatively. For this purpose, three machine learning algorithms—Random Forest (RF), Support Vector Machine (SVM), and Decision Tree (DT)—were employed, and 19 landslide conditioning factors, categorized into topographic, hydrological, and environmental–anthropogenic groups, were utilized in the modeling process. The landslide inventory data were randomly divided into training (70%) and testing (30%) datasets for model evaluation. The performance of the models was evaluated using metrics including the Area Under the Curve (AUC), overall accuracy, sensitivity, specificity, precision, correlation coefficient (R), F1-score, CV-ROC, and Cohen's kappa coefficient. The results showed that the RF algorithm outperformed the other models in identifying the spatial pattern of landslide susceptibility and, by providing a more realistic distribution of high-susceptibility zones, classified approximately 24% of the watershed area as high susceptibility. Accordingly, the AUC value of 0.75 and CV-ROC of 0.97 indicate appropriate model stability, although the overall accuracy of 0.62 reveals the impact of data imbalance. In contrast, the SVM model showed a greater tendency to classify areas as low susceptibility, whereas the DT model exhibited lower stability. Variable importance analysis confirmed the prominent role of the morphometric indices TRI and TPI, as well as the hydrological variables SPI and CN, in controlling slope instability. Overall, the research results confirm the superiority of the RF algorithm and its greater efficiency and reliability in landslide susceptibility zonation
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