Abstract

Landslide is one of the most important geomorphological hazards that cause significant ecological and economic losses and results in billions of dollars in financial losses and thousands of casualties per year. The occurrence of landslide in northern Iran (Alborz Mountain Belt) is often due to the geological and climatic conditions and tectonic and human activities. To reduce or control the damage caused by landslides, landslide susceptibility mapping (LSM) and landslide risk assessment are necessary. In this study, the efficiency and integration of frequency ratio (FR) and random forest (RF) in statistical- and artificial intelligence-based models and different digital elevation models (DEMs) with various spatial resolutions were assessed in the field of LSM. The experiment was performed in Sangtarashan watershed, Mazandran Province, Iran. The study area, which extends to 1072.28 km2, is severely affected by landslides, which cause severe economic and ecological losses. An inventory of 129 landslides that occurred in the study area was prepared using various resources, such as historical landslide records, the interpretation of aerial photos and Google Earth images, and extensive field surveys. The inventory was split into training and test sets, which include 70 and 30% of the landslide locations, respectively. Subsequently, 15 topographic, hydrologic, geologic, and environmental landslide conditioning factors were selected as predictor variables of landslide occurrence on the basis of literature review, field works and multicollinearity analysis. Phased array type L-band synthetic aperture radar (PALSAR), ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer), and SRTM (Shuttle Radar Topography Mission) DEMs were used to extract topographic and hydrologic attributes. The RF model showed that land use/land cover (16.95), normalised difference vegetation index (16.44), distance to road (15.32) and elevation (13.6) were the most important controlling variables. Assessment of model performance by calculating the area under the receiving operating characteristic curve parameter showed that FR–RF integrated model (0.917) achieved higher predictive accuracy than the individual FR (0.865) and RF (0.840) models. Comparison of PALSAR, ASTER, and SRTM DEMs with 12.5, 30 and 90 m spatial resolution, respectively, with the FR–RF integrated model showed that the prediction accuracy of FR–RF–PALSAR (0.917) was higher than FR–RF–ASTER (0.865) and FR–RF–SRTM (0.863). The results of this study could be used by local planners and decision makers for planning development projects and landslide hazard mitigation measures.

Highlights

  • Mass movements are influenced by natural and human factors [1]

  • stream power index (SPI) and topography wetness index (TWI) were excluded, and Landslide susceptibility (LS) modelling in the study area was based on the following variables, which were unaffected by collinearity problems: Elevation, slope degree, slope aspect, convergence index, SL, plan curvature, profile curvature, drainage density, distance to stream, distance to road, distance to fault, lithology, rainfall, land use/land cover (LU/LC), and normalised difference vegetation index (NDVI)

  • Two statistical- and artificial intelligence-based methods, namely frequency ratio (FR) and random forest (RF), and their integration were used for landslide susceptibility mapping (LSM) to promote their advantages and overcome their shortcomings

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Summary

Introduction

Mass movements are influenced by natural and human factors [1] These hazards, which occur in many parts of the world, cause considerable damage to people’s lives and property every year. The average annual economic loss is approximately $1.5 billion in the United States, $2 billion in Japan and $2 million in Italy [2] These hazards annually cause approximately 500 billion rial worth of damage in Iran, and this amount does not include the destruction of nonrenewable natural resources [3]. The rapid population growth, the expansion of human settlements in mountainous areas, the difficulty of predicting the occurrence of landslide and the multiple factors controlling this phenomenon indicate the need for landslide susceptibility assessment (LSA) [12]. LSM is the prediction of the spatial occurrence of landslide on the basis of geomorphological and geo-environmental conditioning factors [14,15]

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