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Long-term relationship between landslide occurrences and precipitation in southern Lower Saxony and northern Hesse

机译:南下萨克森州和北黑森州山体滑坡发生和降水之间的长期关系

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A dataset with information about 394 landslide events between 1901 and 2016 is used for the analysis of the long-term relationship between landslides and precipitation in southern Lower Saxony, northern Hesse and the surroundings. The present study investigates the relationship between landslides and annual precipitation as well as selected monthly landslide distributions and their connection with weather anomalies. Landslide distributions are correlated with precipitation records of a synthetic precipitation series as a representative for the study area. The annual landslide distribution shows an overall increasing number of events with alternating periods of low and high landslide activity. Correlation with the annual precipitation predominantly reveals a more frequent occurrence of landslides in humid years. The monthly landslide distribution between 1901 and 2016 shows a first accumulation of events in winter months (January-March: 31%) and a second one in summer months (June-August: 32%). In general, this monthly landslide distribution follows the annual course of precipitation. Particular monthly landslide distributions are apparent for periods of increased landslide activity which coincide with exceptional long-term winter and summer precipitation trends. In these periods the monthly distributions widely follow the annual precipitation courses. Overall, the results show that the precipitation is basically suitable for an explanation for the occurrence of landslide events. Whereas the annual precipitation is only partially meaningful for the annual landslide activity, the influence of exceptional seasonal precipitation is reflected in the monthly landslide distributions. The results provide a promising basis for more detailed analyses of the relationship between landslides and the precipitation in the study area.
机译:一个关于1901年至2016年间394个滑坡事件的数据集的数据集用于分析南部下萨克森州,北黑森州和周围环境的山体滑坡和降水之间的长期关系。本研究调查了山体滑坡与年降水量之间的关系以及选定的每月滑坡分布及其与天气异常的关系。滑坡分布与合成降水系列的降水记录相关,作为研究区域的代表。年山体滑坡分布显示了整体越来越多的事件,交替的低滑坡活动。与年降水量的相关性主要揭示了潮湿年度更频繁地发生山体滑坡。 1901年至2016年间的每月滑坡分布显示冬季(1月至3月:31%)和夏季(6月至8月:32%)的第二个活动的第一次积累。一般而言,该月山体滑坡分布遵循年度降水量。特定的每月滑坡分布对于增加山体滑坡活动的时期是明显的,这与卓越的长期冬季和夏季降水趋势一致。在这些时期,每月分配广泛遵循年度降水课程。总体而言,结果表明,降水基本上适用于山体滑坡事件的发生解释。然而,年降水量仅对年坡度活动部分有意义,而卓越的季节降水量则反映在每月滑坡分布中。结果为更详细地分析了研究区内山体滑坡与降水的关系提供了有希望的基础。

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