Abstract

A landslide susceptibility map (LSM) is the basis of hazard and risk assessment, guiding land planning and utilization, early warning of disaster, etc. Researchers are often overly keen on hybridizing state-of-the-art models or exploring new mathematical susceptibility models to improve the accuracy of the susceptibility map in terms of a receiver operator characteristic curve. Correlation analysis of the causal factors is a necessary routine process before susceptibility modeling to ensure that the overall correlation among all factors is low. However, this overall correlation analysis is insufficient to detect a high local correlation among the causal factor classes. The objective of this study is to answer three questions: 1) Is there a high correlation between causal factors in some parts locally? 2) Does it affect the accuracy of landslide susceptibility assessment? and 3) How can this influence be eliminated? To this aim, Wanzhou County was taken as the test site, where landslide susceptibility assessment based on 12 causal factors has been previously performed using the frequency ratio (FR) model and random forest (RF) model. In this work, we conducted a local spatial correlation analysis of the “altitude” and “rivers” factors and found a sizeable spatial overlap between altitude-class-1 and rivers-class-1. The “altitude” and “rivers” factors were reclassified, and then the FR model and RF model were used to reevaluate the susceptibility and analyze the accuracy loss caused by the local spatial correlation of the two factors. The results demonstrated that the accuracy of LSMs was markedly enhanced after reclassification of “altitude” and “rivers,” especially for the RF model–based LSM. This research shed new light on the local correlation of causal factors arising from a particular geomorphology and their impact on susceptibility.

Highlights

  • The landslide susceptibility map represents the spatial probability of landslide occurrence, is the basis for landslide hazard and risk assessment (Fell et al, 2008; Pellicani et al, 2017), and is used in practice for land planning (Cascini 2008; Chen et al, 2019), quantitative risk analysis (Chen et al, 2016; Yan et al, 2020), early warning systems (Segoni et al, 2018; Rosi et al, 2021), etc

  • The results show that the high local correlation of altitude and rivers factors does exist and truly affects the accuracy of landslide susceptibility map (LSM)

  • This study shows that the local correlation of causal factors could exist and reduce the accuracy of susceptibility assessment

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Summary

Introduction

The landslide susceptibility map represents the spatial probability of landslide occurrence, is the basis for landslide hazard and risk assessment (Fell et al, 2008; Pellicani et al, 2017), and is used in practice for land planning (Cascini 2008; Chen et al, 2019), quantitative risk analysis (Chen et al, 2016; Yan et al, 2020), early warning systems (Segoni et al, 2018; Rosi et al, 2021), etc. Researchers are overly keen on hybridizing state-of-the-art models (Schicker and Moon, 2012; Kornejady et al, 2018; Luo and Liu, 2018) or exploring new mathematical susceptibility models (Chen et al, 2017; Yang Y. et al, 2019; Paryani et al, 2020; Wu et al, 2020), often ignoring the interrelationships between causal factors. It is a well-known fact that each study area has its specific geomorphological features. Several issues need to be discussed: Is there a high correlation between causal factors in some parts locally? Does it affect the accuracy of landslide susceptibility assessment? How can this influence be eliminated?

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