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Landslide susceptibility mapping using GIS-based multi-criteria decision analysis, support vector machines, and logistic regression

机译:使用基于GIS的多准则决策分析,支持向量机和Logistic回归的滑坡敏感性地图

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摘要

Identification of landslides and production of landslide susceptibility maps are crucial steps that can help planners, local administrations, and decision makers in disaster planning. Accuracy of the landslide susceptibility maps is important for reducing the losses of life and property. Models used for landslide susceptibility mapping require a combination of various factors describing features of the terrain and meteorological conditions. Many algorithms have been developed and applied in the literature to increase the accuracy of landslide susceptibility maps. In recent years, geographic information system-based multi-criteria decision analyses (MCDA) and support vector regression (SVR) have been successfully applied in the production of landslide susceptibility maps. In this study, the MCDA and SVR methods were employed to assess the shallow landslide susceptibility of Trabzon province (NE Turkey) using lithology, slope, land cover, aspect, topographic wetness index, drainage density, slope length, elevation, and distance to road as input data. Performances of the methods were compared with that of widely used logistic regression model using ROC and success rate curves. Results showed that the MCDA and SVR outperformed the conventional logistic regression method in the mapping of shallow landslides. Therefore, multi-criteria decision method and support vector regression were employed to determine potential landslide zones in the study area.
机译:识别滑坡和绘制滑坡敏感性图是至关重要的步骤,可以帮助规划人员,地方政府和决策者进行灾难规划。滑坡敏感性图的准确性对于减少生命和财产损失至关重要。用于滑坡敏感性地图绘制的模型需要描述地形特征和气象条件的各种因素的组合。已经开发了许多算法并将其应用于文献中,以提高滑坡敏感性图的准确性。近年来,基于地理信息系统的多准则决策分析(MCDA)和支持向量回归(SVR)已成功地应用于滑坡敏感性地图的制作中。在这项研究中,MCDA和SVR方法被用于利用岩性,坡度,土地覆盖物,坡向,地形湿度指数,排水密度,坡长,高程和距道路的距离来评估特拉布宗省(土耳其东北部)的浅层滑坡敏感性。作为输入数据。使用ROC和成功率曲线,将该方法的性能与广泛使用的逻辑回归模型进行了比较。结果表明,在浅层滑坡测绘中,MCDA和SVR优于传统的Logistic回归方法。因此,采用多准则决策方法和支持向量回归来确定研究区域内潜在的滑坡带。

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