Abstract

Slope failure probabilistic models generated using random forest (RF) machine learning (ML), manually interpreted incident points, and light detection and ranging (LiDAR) digital terrain variables are assessed for predicting and generalizing to new geographic extents. Specifically, models for four Major Land Resource Areas (MLRAs) in the state of West Virginia in the United States (US) were created. All region-specific models were then used to predict withheld validation data within all four MLRAs. For all validation datasets, the model trained using data from the same MLRA provided the highest reported overall accuracy (OA), Kappa statistic, F1 Score, area under the receiver operating characteristic curve (AUC ROC), and area under the precision-recall curve (AUC PR). However, the model from the same MLRA as the validation dataset did not always provide the highest precision, recall, and/or specificity, suggesting that models extrapolated to new geographic extents tend to either overpredict or underpredict the land area of slope failure occurrence whereas they offer a better balance between omission and commission error within the region in which they were trained. This study highlights the value of developing region-specific inventories, models, and high resolution and detailed digital elevation data, since models may not generalize well to new geographic extents, potentially resulting from spatial heterogeneity in landscape and/or slope failure characteristics.

Highlights

  • Slope failures, such as landslides, are a geohazard of global concern that often result in damage to personal property and public infrastructure, exacerbation of social and economic issues impacting already strained communities and governments, and loss of life [1,2,3]

  • We focus on the production of probabilistic slope failure occurrence models using light detection and ranging (LiDAR)-derived terrain variables and manually digitized failure locations to explore the key issue of how well models trained in different landscapes, defined by Major Land Resource Areas (MLRAs), extrapolate to other MLRAs in the state of West Virginia in the United States (US)

  • The highest annual precipitation occurs on the western slopes of the high mountains within the Eastern Allegheny Plateau and Mountains (EAPM) MLRA, with totals as high as 1600 mm per year, while the lowest precipitation occurs in the Northern Appalachian Ridges and Valleys (NARV) MLRA, with totals around 635 mm

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Summary

Introduction

Slope failures, such as landslides, are a geohazard of global concern that often result in damage to personal property and public infrastructure, exacerbation of social and economic issues impacting already strained communities and governments, and loss of life [1,2,3]. High spatial resolution digital terrain data, such as those derived using light detection and ranging (LiDAR), have improved our ability to identify slope failures on the landscape surface, even when obscured by vegetative cover, and generate detailed terrain variables to aid in modeling [17,18,19,20,21,22] Such data are becoming more widely available; for example, the United States Geological Survey (USGS) is currently coordinating the collection of LiDAR data for the entire contiguous United States (US) via the 3D Elevation Program (3DEP) [23,24].

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