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A new approach to temporal modelling for landslide hazard assessment using an extreme rainfall induced-landslide index

机译:利用极端降雨诱发滑坡指数进行滑坡灾害评估的时间建模的新方法

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摘要

An ever-increasing trend of extreme rainfall events hi South Korea due to climate change is causing shallow landslides and shallow landslide induced debris flows in the mountains that cover 70% of the total land area of the nation. These catastrophic, gravity-driven processes cost the government several billion won in losses,, and attendant fatalities, every year. The most common type of landslide observed is the shallow landslide occurring at 13 m depth, which may mobilize into a catastrophic debris flow. A landslide early warning system encompassing different scale-based stages is used to predict potential areas for both the landslide types. Current study focusing on the first stage landslide hazard assessment at regional or medium scale requires the development of spatially evolving landslide hazard maps for both types of landslides based on the real-time rainfall. However, lack of complete landslide inventory data motivates the development of temporal and spatial models as independent components of the landslide hazard. Most of the existing temporal assessment schemes traditionally rooted in recurrence-based concepts does not consider soil factors and are not suitable to be incorporated in to the landslide early warning system since real-time rainfall cannot be considered. This motivated the development of a new probabilistic temporal model termed the extreme rainfall-induced landslide index. The probabilistic index was developed in Gangwon Province through a logistic regression using four factors; namely, continuous rainfall, 20-days antecedent rainfall, saturated'hydraulic conductivity, and storage capacity. The developed model exhibited high area under the curve (AUC) values of 82% and 91% obtained for the training and validation curves, exhibiting good performance of the statistical index. Also, a high performance susceptibility model (training and validation AUC values of 96% and 94%, respectively) was developed using a logistic regression analysis, for Deokjeok-ri Creek, located in Gangwon province. Assuming the independence of the hazard components, a dynamic hazard index (DHI) was established through a joint probability of both the well validated models. The DHI was used to study the evolution of landslide hazard for the July 2006 extreme rainfall-induced landslide events in Deokjeok-ri Creek. (C) 2016 Published by Elsevier B.V.
机译:在韩国,由于气候变化,极端降雨事件呈不断增加的趋势,导致浅层滑坡和浅层滑坡诱发的泥石流在占全国土地总面积70%的山脉中流动。这些灾难性的,引力驱动的过程每年给政府造成数十亿韩元的损失,并伴随着死亡。观察到的最常见的滑坡类型是发生在13 m深度的浅层滑坡,它可能动员为灾难性的泥石流。包含不同规模阶段的滑坡预警系统用于预测两种滑坡类型的潜在面积。当前针对区域或中等规模的第一阶段滑坡灾害评估的研究要求根据实时降雨为两种类型的滑坡建立空间演化的滑坡灾害图。然而,缺乏完整的滑坡清单数据促使作为滑坡灾害的独立组成部分的时空模型的发展。传统上基于递归概念的大多数现有时间评估方案都没有考虑土壤因素,并且由于无法考虑实时降雨,因此不适合纳入滑坡预警系统。这激励了新的概率时间模型的发展,该模型被称为极端降雨诱发的滑坡指数。江原道省的概率指数是通过使用四个因素进行的逻辑回归得出的。即连续降雨,20天前期降雨,饱和水导率和储水能力。所开发的模型在训练和验证曲线上显示的曲线下面积(AUC)值分别为82%和91%,具有良好的统计指标性能。此外,针对江原道市的德-里溪,使用逻辑回归分析开发了一个高性能磁化率模型(训练和验证的AUC值分别为96%和94%)。假设危险因素的独立性,通过两个经过充分验证的模型的联合概率建立了动态​​危险指数(DHI)。 DHI用于研究Deokjeok-ri Creek 2006年7月的极端降雨诱发的滑坡事件的滑坡灾害演变。 (C)2016由Elsevier B.V.发布

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