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Improved rainfall threshold for landslides in data sparse and diverse geomorphic milieu: a cluster analysis based approach

机译:改进了数据稀疏和多种地貌Milieu中山体滑坡的降雨阈值:基于集群分析的方法

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Rainfall-triggered landslides are the most common type of mass movement seen along the tropical belt due to the prevalence of monsoons. These landslides can be forecasted by understanding the spatial and temporal rainfall distribution patterns, and subsequent generation of rainfall threshold (RT). However, deriving a regional RT in a geologically, geographically and physiographically diverse milieu is a formidable task. The data on spatial and intra-seasonal variability of monsoons can be widely dispersed in such diversified terrains. Clustering analysis provides a promising approach to handle such widely dispersed data. This study intends to develop a methodology using 2-stage clustering process to create RT in such terrains by using daily rainfall versus antecedent rainfall and rainfall versus antecedent rainfall versus soil depth. Sixteen rainfall-induced landslides, located in different terrains in the Western Ghats of India, were subjected to this analysis. Majority of the landslides were modeled, and different RTs were derived for different conditions. The landslides belong to four different classes, viz., landslides occurring at steep slopes; those occurring at knickpoints of highland and midland; in the plateau region and others characterized by a thin veneer of soil. Out of 16 landslides subjected to RT, this method was able to model 13 landslides with a success rate of 81.25%, which is a fair figure.
机译:降雨触发的山体滑坡是由于季风的普及,沿热带皮带看到的最常见的群众运动。通过了解空间和时间降雨分布模式以及随后产生降雨阈值(RT),可以预测这些滑坡。然而,在地质上,地理上和地理学和地理学上不同的Milieu获得区域RT是一个强大的任务。季风的空间和季节性变异性的数据可以广泛分散在这种多样化的地形中。聚类分析提供了处理这种广泛分散的数据的有希望的方法。本研究打算利用2级聚类过程制定一种方法,通过使用日落降雨与前进降雨,降雨与未经降雨量相比,在这种地形中产生RT。在印度西戈斯西戈斯的不同地形中,十六天降雨诱导的山体滑坡遭到了此分析。大多数山体滑坡被建模,不同的RTS被衍生出不同的条件。山体滑坡属于四种不同的班级,viz。,陡峭斜坡发生的山体滑坡;那些在高地和米德兰的Knickpoints发生的人;在高原地区等,其特征在于薄薄的土壤。在16个山体滑坡中进行RT,这种方法能够模拟13次滑坡,成功率为81.25%,这是一个公平的数字。

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