用随机模型方法预测地震诱发的滑坡:以2001年萨尔瓦多同震滑坡为例

Claudio Mercurio, Laura Paola Calderón-Cucunuba, Abel Alexei Argueta-Platero, Grazia Azzara, C. Cappadonia, C. Martinello, E. Rotigliano, C. Conoscenti
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引用次数: 3

摘要

2001年1月和2月,萨尔瓦多遭受了两次强烈地震,引发了数千次山体滑坡,造成1259人死亡和大面积破坏。对航空和SPOT-4卫星图像的分析使我们能够绘制出6491个同震滑坡,主要是发生在火山碎屑岩和火山碎屑岩中的碎屑滑坡和泥石流。利用不同的预测因子和滑坡清单建立了四种不同的多元自适应回归样条(MARS)模型,其中包括2009年极端降雨事件引发的边坡破坏和2001年地震引起的边坡破坏。在预测分析中,采用了三种验证情景:第一种和第二种分别包含25%和95%的滑坡,而第三种基于k-fold空间交叉验证。我们的分析结果表明:(1)MARS算法提供了同震滑坡的可靠预测;(ii)当将降雨引发的滑坡的易感性作为一个独立变量时,可以更好地预测同震边坡的破坏;(iii)同时使用准备变量和触发变量训练的模型达到最佳精度;(iv)地震发生后建立的同震滑坡的不完整清单可用于确定尚未报告的滑坡的潜在位置。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Predicting Earthquake-Induced Landslides by Using a Stochastic Modeling Approach: A Case Study of the 2001 El Salvador Coseismic Landslides
In January and February 2001, El Salvador was hit by two strong earthquakes that triggered thousands of landslides, causing 1259 fatalities and extensive damage. The analysis of aerial and SPOT-4 satellite images allowed us to map 6491 coseismic landslides, mainly debris slides and flows that occurred in volcanic epiclastites and pyroclastites. Four different multivariate adaptive regression splines (MARS) models were produced using different predictors and landslide inventories which contain slope failures triggered by an extreme rainfall event in 2009 and those induced by the earthquakes of 2001. In a predictive analysis, three validation scenarios were employed: the first and the second included 25% and 95% of the landslides, respectively, while the third was based on a k-fold spatial cross-validation. The results of our analysis revealed that: (i) the MARS algorithm provides reliable predictions of coseismic landslides; (ii) a better ability to predict coseismic slope failures was observed when including susceptibility to rainfall-triggered landslides as an independent variable; (iii) the best accuracy is achieved by models trained with both preparatory and trigger variables; (iv) an incomplete inventory of coseismic slope failures built just after the earthquake event can be used to identify potential locations of yet unreported landslides.
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