Abstract

With the unique rainfall patterns of typhoons, plum rains, and short-term heavy rainfalls, the frequent landslide and debris flow disasters have caused severe loss to people in Taiwan. In the studies of landslide susceptibility, the information of factors used for analysis was usually annual-based content, and it was assumed that the same elements from different years were independent between each year. However, the occurrence of landslides was usually not simply due to the changes within a year. Instead, landslides were triggered because the factors that affected the potential of landslides reached critical conditions after a cumulative change with time. Therefore, this study had well evaluated the influence of temporal characteristics and the ratios of antecedent landslide areas in the past five years in the landslide potential evaluation model. The analysis was conducted through the random forest (RF) algorithm. Additional rainfall events of 2017 were used to test the proposed model’s performance to understand its practicality. The analysis results show that in the study area, the RF model had considerably acceptable performance. The results have also demonstrated that the antecedent landslide ratios in the past five years were essential to describe the significance of cumulative change with time when conducting potential landslide evaluation.

Highlights

  • The ratios related to landslide areas, i.e., the proportions of No 1, No 2, No 3, No.4, and No 5 in Figure 5 were calculated for each slope unit after satellite image processing and interpretation

  • The performance of the proposed random forest (RF) model was highlighted by conducting annual validation from 2011 to 2016

  • According to the analysis results, adding temporal characteristics had significantly improved the performance of landslide potential prediction by the proposed random forest model

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Summary

Introduction

Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. Rainfall data over the study areas and landslide cases were obtained and analyzed by constructing a fragility curve to describe the exceeding probability of landslide for given environmental conditions. The critical hazard potential and critical fragility potential were determined to express the probability of exceeding a damage state of landslides under certain conditions of rainfall intensity and accumulated rainfall [2] Both LSA and LRA models use factors to describe the potential of landslides. Among the rainfall-induced researches, the rainfall thresholds are usually the main factor when evaluating the landslide susceptibility [18], and the temporal resolution of rainfall affects the thresholds significantly [19] In these studies, the rainfall factors were included in the evaluation procedure by yearly-based input, not considering the consecutive influence from previous years. The insights from the newly developed RF model were included in this paper

Study Areas
Slope Units
Environmental Database and Model Factors
Development of Landslide Potential Evaluation Model
Model Performance Evaluation for Individual Rainfall Events
Conclusions
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