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The influence of topographic parameters on avalanche release dimension and frequency

机译:地形参数对雪崩释放尺度和频率的影响

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摘要

Avalanche hazard zones in Switzerland are defined by the frequency and the impact pressure of a potential avalanche event. Therefore, it is necessary to accurately estimate the release frequency and, related to the frequency, the release area for a specific avalanche track. In order to improve this hazard mapping procedure, a statistical analysis of avalanche releases on well-documented avalanche paths was performed. In the region of Davos, an almost complete database of avalanche events over the last 50 years exists. Using Geographic Information System (GIS) technologies in combination with Digital Elevation Models (DEMs), the recorded avalanche release areas were analysed with respect to topographic characteristics. Topographic parameters like "slope", "confinement", "aspect" and "distance to the next ridge" are derived from the DEM. The statistical analysis results in general rules and probability distributions for release extents as a function of the frequency and the topographic parameters. The general rules are a valuable aid for avalanche experts in cases where information about historical avalanche is lacking for a particular track. Furthermore, the probability distributions can be directly used as input for uncertainty modelling of avalanche run-out distances using Monte Carlo methods. This preliminary analysis indicates that mean slope, curvature and distance to the ridge are the most important parameters influencing the avalanche release area frequency; higher average slope angles lead to the frequent release of small avalanches.
机译:瑞士的雪崩危险区由潜在雪崩事件的发生频率和冲击压力确定。因此,有必要针对特定​​的雪崩轨道准确地估计释放频率以及与该频率相关的释放面积。为了改进此危害图绘制程序,对有据可查的雪崩路径上的雪崩释放进行了统计分析。在达沃斯地区,存在过去50年几乎完整的雪崩事件数据库。通过结合使用地理信息系统(GIS)技术和数字高程模型(DEM),可以分析地形特征记录的雪崩释放区域。像“坡度”,“约束”,“纵横比”和“到下一个山脊的距离”之类的地形参数是从DEM派生的。统计分析得出释放范围的一般规则和概率分布,作为频率和地形参数的函数。在缺少特定雪道的历史雪崩信息的情况下,一般规则对于雪崩专家是非常有用的帮助。此外,概率分布可以直接用作使用蒙特卡洛方法对雪崩跳动距离进行不确定性建模的输入。初步分析表明,平均坡度,曲率和到山脊的距离是影响雪崩释放区域频率的最重要参数。较高的平均倾斜角度会导致频繁释放小雪崩。

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