首页> 外文期刊>Acta Geologica Slovaca >Assessment of debris flow susceptibility using bivariate and multivariate statistical analyses and verification based on catastrophic events from 2014 in the Krivánska Malá Fatra Mountains, Slovakia
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Assessment of debris flow susceptibility using bivariate and multivariate statistical analyses and verification based on catastrophic events from 2014 in the Krivánska Malá Fatra Mountains, Slovakia

机译:使用双变量和多变量统计分析以及基于2014年斯洛伐克KrivánskaMaláFatra山区灾难性事件的验证,对泥石流敏感性进行评估

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The presented study shows using of bivariate and multivariate statistical analyses in mountain area of the Krivánska Fatra Mountains affected by debris flows. Three generations of data were studied in order to assess the debris flows in the area, from these two main periods of debris flows were taken into the analysis: the debris flows from 1950s to 1970s and catastrophic debris flows from July 2014. Various input data were used in the statistical analyses: elevation, slope angle, plan curvature, topographic wetness index, flow accumulation, lithology, and land cover. Two main evaluations were made: first using the older debris flow data and second using debris flow data from the both periods. Receiver operating characteristic analysis was performed in order to assess the reliability of the models with the area under curve more than 95?% for both evaluations and more than 85% for the first evaluation checked by both periods of debris flows in case of multivariate analysis, respectively almost 83% and 80% in case of bivariate analysis. The comparison with existing avalanche tracks was performed as well and shows satisfactory results. The tracks of debris flows from July 2014 show the extraordinariness of the event in comparison with older debris flows. Experimental assessment of natural hazard was performed using the map of difference between the two susceptibility maps in order to find out the areas of possible high magnitude low frequency events.
机译:提出的研究表明在受泥石流影响的克里瓦斯卡法特拉山山区使用双变量和多变量统计分析。为了评估该地区的泥石流,研究了三代数据,从这两个主要的泥石流时期开始进行了分析:1950年代至1970年代的泥石流和2014年7月以来的灾难性泥石流。用于统计分析:高程,倾斜角,平面曲率,地形湿度指数,流量累积,岩性和土地覆盖。进行了两项主要评估:第一项使用较旧的泥石流数据,第二项使用两个时期的泥石流数据。进行接收器工作特性分析是为了评估模型的可靠性,在两次评估中,曲线下面积在两次评估中均超过95%,两次泥石流检查的首次评估均超过85%,在双变量分析的情况下,分别接近83%和80%。还与现有雪崩轨道进行了比较,结果令人满意。从2014年7月开始的泥石流轨迹显示,与较旧的泥石流相比,该事件异常出色。使用两个磁化率图之间的差异图进行了自然灾害的实验评估,以找出可能发生的高强度低频事件的区域。

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