Abstract
This paper proposes a novel method to incorporate unfavorable orientations of discontinuities into machine learning (ML) landslide prediction by using GIS-based kinematic analysis. Discontinuities, detected from photogrammetric and aerial LiDAR surveys, were included in the assessment of potential rock slope instability through GIS-based kinematic analysis. Results from the kinematic analysis, coupled with several commonly used landslide influencing factors, were adopted as input variables in ML models to predict landslides. In this paper, various ML models, such as random forest (RF), support vector machine (SVM), multilayer perceptron (MLP) and deep learning neural network (DLNN) models were evaluated. Results of two validation methods (confusion matrix and ROC curve) show that the involvement of discontinuity-related variables significantly improved the landslide predictive capability of these four models. Their addition demonstrated a minimum of 6% and 4% increase in the overall prediction accuracy and the area under curve (AUC), respectively. In addition, frequency ratio (FR) analysis showed good consistency between landslide probability that was characterized by FR values and discontinuity-related variables, indicating a high correlation. Both results of model validation and FR analysis highlight that inclusion of discontinuities into ML models can improve landslide prediction accuracy.
Highlights
Landslides have drawn world-wide attention due to their potentially devastating impact on human safety and infrastructure
Frequency Ratio Analysis In frequency ratio (FR) analysis, the analyzed variables related to kinematic analysis were categorized into three different classes in accordance with their density values
This paper proposes a novel application of unfavorably orientated discontinuities in machine learning (ML) landslide analysis
Summary
Landslides have drawn world-wide attention due to their potentially devastating impact on human safety and infrastructure. It has been reported that the total land area over the world subjected to landslides is about 3.7 million square kilometers, affecting a population of nearly 300 million [1]. The relatively high-risk areas (top three deciles) cover about 820,000 square kilometers with an estimated population of 66 million. Examples of catastrophic landslide events have been recorded in different regions globally. In 2014, the Gold Basin landslide occurred in the USA, damaging 49 houses down the slope and causing 43 fatalities [3]. A catastrophic high-elevation and long-runout landslide occurred in China, causing the death of 51 people and the destruction and burial of 21 houses in 2019 [4]
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