2021
DOI: 10.3389/feart.2021.609896
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A One-Class-Classifier-Based Negative Data Generation Method for Rapid Earthquake-Induced Landslide Susceptibility Mapping

Abstract: Machine learning with extensively labeled training samples (e.g., positive and negative data) has received much attention in terms of addressing earthquake-induced landslide susceptibility mapping (LSM). However, the extensive amount of labeled training data required by machine learning, particularly the precise negative data (i.e., non-landslide area), cannot be easily and efficiently collected. To address this issue, this study presents a one-class-classifier-based negative data generation method for rapid e… Show more

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Cited by 9 publications
(5 citation statements)
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“…When preparing susceptibility map of landslides triggered by earthquakes, Wang et al (2021) employed elevation, aspect, slope angle, terrain relief, distance to faults, distance to rivers and terrain wetness index as conditioning factors while considered elevation, slope, aspect, land cover, soil type, precipitation, distance to faults, distance to roads and distance to streams for investigating eartquakes on landslides susceptibility in a seismic prone area in Central Asia. Several studies (Chen et al 2021;Guo et al 2021;Liu et al 2021) considered similar conditioning and triggering parameters when producing susceptibility maps of landslides triggered by earthquakes. Consequently, different conditioning factors such as altitude, slope, aspect, plan and pro le curvature, lithology, topographic wetness index (TWI), stream power index (SPI), normalized difference vegetation index (NDVI), drainage density, distance to roads were used to produce LSM in the literature (Chen et al 2017b;de Oliveira et al 2019;Wang et al 2020;Adnan et al 2020;Bui et al 2020).…”
Section: Methodsmentioning
confidence: 99%
See 2 more Smart Citations
“…When preparing susceptibility map of landslides triggered by earthquakes, Wang et al (2021) employed elevation, aspect, slope angle, terrain relief, distance to faults, distance to rivers and terrain wetness index as conditioning factors while considered elevation, slope, aspect, land cover, soil type, precipitation, distance to faults, distance to roads and distance to streams for investigating eartquakes on landslides susceptibility in a seismic prone area in Central Asia. Several studies (Chen et al 2021;Guo et al 2021;Liu et al 2021) considered similar conditioning and triggering parameters when producing susceptibility maps of landslides triggered by earthquakes. Consequently, different conditioning factors such as altitude, slope, aspect, plan and pro le curvature, lithology, topographic wetness index (TWI), stream power index (SPI), normalized difference vegetation index (NDVI), drainage density, distance to roads were used to produce LSM in the literature (Chen et al 2017b;de Oliveira et al 2019;Wang et al 2020;Adnan et al 2020;Bui et al 2020).…”
Section: Methodsmentioning
confidence: 99%
“…In the recent literature, it is possible to nd studies on regional susceptibility assessments of landslides triggered by earthquakes (e.g. Xie et al 2018;Chen et al 2020 a, b, c;Chen et al 2021). However, if there is no landslide inventory prepared immediately after earthquake, it is still di cult to distinguish the landslides in a region that are triggered by earthquakes.…”
Section: Introductionmentioning
confidence: 99%
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“…The selection of reasonable negative samples has a significant impact on the prediction results. In previous studies, negative samples have often been selected using environmental similarity-based sampling (ESBS), buffer-controlled sampling (BCS) [39], target space exteriorization sampling (TSES) [40], etc. A-Xing Zhu [41] proposed a negative sample sampling similarity theory that quantifies negative samples based on the environmental similarity between alternative negative and positive samples, and compared it with two existing negative sample generation methods, BCS and TSES.…”
Section: Geospatial Databasementioning
confidence: 99%
“…, M}, x i ∈ R n . The OC-SVM maps the samples from low-dimensional to high-dimensional space through the Φ, establishing an optimal hyperplane between the zero point and the high-dimensional space (Chen et al, 2021). This hyperplane can be described by the n-dimensional vector W [w 1 , w 2 , .…”
Section: One-class Svmmentioning
confidence: 99%