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Early warning system for shallow landslides using rainfall threshold and slope stability analysis

机译:利用降雨阈值和边坡稳定性分析的浅层滑坡预警系统

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A combined cluster and regression analysis were performed for the first time to identify rainfall threshold that triggers landslide events in Amboori, Kerala, India. Amboori is a tropical area that is highly vulnerable to landslides. The 2, 3, and 5-day antecedent rainfall data versus daily rainfall was clustered to identify a cluster of critical events that could potentially trigger landslides. Further, the cluster of critical events was utilized for regression analysis to develop the threshold equations. The 5-day antecedent ( x -variable) vs. daily rainfall ( y -variable) provided the best fit to the data with a threshold equation of y ?=?80.7–0.1981 x . The intercept of the equation indicates that if the 5-day antecedent rainfall is zero, the minimum daily rainfall needed to trigger the landslide in the Amboori region would be 80.7?mm. The negative coefficient of the antecedent rainfall indicates that when the cumulative antecedent rainfall increases, the amount of daily rainfall required to trigger monsoon landslide decreases. The coefficient value indicates that the contribution of the 5-day antecedent rainfall is ~20% to the landslide trigger threshold. The slope stability analysis carried out for the area, using Probabilistic Infinite Slope Analysis Model (PISA-m), was utilized to identify the areas vulnerable to landslide in the region. The locations in the area where past landslides have occurred demonstrate lower Factors of Safety (FS) in the slope stability analysis. Thus, rainfall threshold analysis together with the FS values from slope stability can be suitable for developing a simple, cost-effective, and comprehensive early-warning system for shallow landslides in Amboori and similar regions. Graphical abstract Display Omitted Highlights ? Combined cluster and regression analysis used for first time to identify rainfall threshold. ? Cluster analysis was used to identify critical events that could potentially trigger landslides. ? The 5-day antecedent vs daily rainfall provided the best fit to the data. ? PISA-m was utilized to identify areas vulnerable to landslide in the region. ? Such a study can be used to develop cost-effective early warning system.
机译:第一次执行组合的集群和回归分析,以识别降雨阈值,以触发Amboori,喀拉拉邦,印度的滑坡事件。 Amboori是一个热带地区,非常容易受到山体滑坡。每日降雨的2,3和5天的先行降雨数据被聚集成识别可能触发滑坡的关键事件集群。此外,使用关键事件群集用于回归分析以开发阈值方程。为期5天的先发病人(X-Variable)与每日降雨(Y-Variable)提供了与Y的阈值方程的最合适的数据?=?80.7-0.1981 x。等式的截距表明,如果5天的先行降雨为零,则触发振动区域中的滑坡所需的最低日降雨将是80.7?mm。先行降雨的负系数表明,当累计的前进降雨量增加时,触发季风滑坡所需的日落量减少。系数值表明,5天前进降雨的贡献为山体滑坡触发阈值〜20%。利用概率无限斜坡分析模型(PISA-M)对该区域进行的斜率稳定性分析用于识别该区域易受滑坡的区域。发生过去山体滑坡的地区在坡度稳定性分析中表现出较低的安全性(FS)的因素。因此,从坡度稳定性的FS值加入阈值阈值分析可以适用于开发简单,经济高效,以及用于amboori和类似地区的浅层滑坡的全面早期预警系统。图形抽象显示省略了亮点?组合集群和回归分析首次使用以识别降雨阈值。 ?集群分析用于识别可能触发滑坡的关键事件。 ? 5天的先天vs每天降雨量提供最适合数据。 ? PISA-M用于识别该地区易受滑坡的地区。 ?这种研究可用于开发成本效益的预警系统。

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