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Assessment of susceptibility to earth-flow landslide using logistic regression and multivariate adaptive regression splines: A case of the Bence River basin (western Sicily, Italy)

机译:使用逻辑回归和多元自适应回归样条对泥石流滑坡敏感性进行评估:以本斯河流域(意大利西西里岛)为例

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摘要

In this paper, terrain susceptibility to earth-flow occurrence was evaluated by using geographic information systems (GIS) and two statistical methods: Logistic regression (LR) and multivariate adaptive regression splines (MARS). LR has been already demonstrated to provide reliable predictions of earth-flow occurrence, whereas MARS, as far as we know, has never been used to generate earth-flow susceptibility models. The experiment was carried out in a basin of western Sicily (Italy), which extends for 51 km(2) and is severely affected by earth-flows. In total, we mapped 1376 earth-flows, covering an area of 4.59 km(2). To explore the effect of pre-failure topography on earth-flow spatial distribution, we performed a reconstruction of topography before the landslide occurrence. This was achieved by preparing a digital terrain model (DTM) where altitude of areas hosting landslides was interpolated from the adjacent undisturbed land surface by using the algorithm topo-to-raster. This DTM was exploited to extract 15 morphological and hydrological variables that, in addition to outcropping lithology, were employed as explanatory variables of earth-flow spatial distribution. The predictive skill of the earth-flow susceptibility models and the robustness of the procedure were tested by preparing five datasets, each including a different subset of landslides and stable areas. The accuracy of the predictive models was evaluated by drawing receiver operating characteristic (ROC) curves and by calculating the area under the ROC curve (AUC). The results demonstrate that the overall accuracy of LR and MARS earth-flow susceptibility models is from excellent to outstanding. However, AUC values of the validation datasets attest to a higher predictive power of MARS-models (AUC between 0.881 and 0.912) with respect to LR-models (AUC between 0.823 and 0.870). The adopted procedure proved to be resistant to overfitting and stable when changes of the learning and validation samples are performed.
机译:本文利用地理信息系统(GIS)和两种统计方法,即Logistic回归(LR)和多元自适应回归样条(MARS),评估了地形对土流发生的敏感性。 LR已经被证明可以可靠地预测土流的发生,而就我们所知,MARS从未用于生成土流敏感性模型。该实验在西西里岛(意大利)西部的盆地中进行,该盆地延伸51 km(2),并受到泥石流的严重影响。我们总共绘制了1376条泥石流,覆盖4.59 km(2)。为了探究失效前地形对泥石流空间分布的影响,我们在滑坡发生之前对地形进行了重建。这是通过准备一个数字地形模型(DTM)来实现的,该模型通过使用地形栅格技术从相邻的未扰动地表内插入了滑坡区域的高度。利用该DTM提取了15个形态和水文变量,除了露头岩性外,还用作解释土流空间分布的变量。通过准备五个数据集来测试泥石流敏感性模型的预测技巧和程序的鲁棒性,每个数据集都包括滑坡和稳定区域的不同子集。通过绘制接收器工作特性(ROC)曲线并计算ROC曲线下的面积(AUC)来评估预测模型的准确性。结果表明,LR和MARS泥石流敏感性模型的整体精度从优异到卓越。但是,相对于LR模型(AUC在0.823和0.870之间),验证数据集的AUC值证明了MARS模型(AUC在0.881和0.912之间)的更高预测能力。事实证明,在进行学习和验证样本更改时,所采用的程序耐过度拟合且稳定。

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