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Potential slab avalanche release area identification from estimated winter terrain: a multi-scale, fuzzy logic approach

机译:从估计的冬季地形中识别潜在的平板雪崩释放区域:一种多尺度模糊逻辑方法

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摘要

Avalanche hazard assessment requires a very precise estimation of the release area, which still depends, to a large extent, on expert judgement of avalanche specialists. Therefore, a new algorithm for automated identification of potential avalanche release areas was developed. It overcomes some of the limitations of previous tools, which are currently not often applied in hazard mitigation practice. By introducing a multi-scale roughness parameter, fine-scale topography and its attenuation under snow influence is captured. This allows the assessment of snow influence on terrain morphology and, consequently, potential release area size and location. The integration of a wind shelter index enables the user to define release area scenarios as a function of the prevailing wind direction or single storm events. A case study illustrates the practical usefulness of this approach for the definition of release area scenarios under varying snow cover and wind conditions. A validation with historical data demonstrated an improved estimation of avalanche release areas. Our method outperforms a slope-based approach, in particular for more frequent avalanches; however, the application of the algorithm as a forecasting tool remains limited, as snowpack stability is not integrated. Future research activity should therefore focus on the coupling of the algorithm with snowpack conditions.
机译:雪崩危害评估需要对释放区域进行非常精确的估算,这在很大程度上仍取决于雪崩专家的专业判断。因此,开发了一种自动识别潜在雪崩释放区域的新算法。它克服了先前工具的某些局限性,这些工具目前在减轻危害的实践中并不经常使用。通过引入多尺度粗糙度参数,可以捕获小尺度地形及其在雪影响下的衰减。这样可以评估积雪对地形形态的影响,并因此评估潜在释放区域的大小和位置。风挡指数的集成使用户能够根据主要风向或单个暴风雨事件定义释放区域方案。案例研究表明,这种方法对于定义不同的积雪和风况下的释放区域方案的实际有用性。根据历史数据进行的验证表明,雪崩释放面积的估算值得到了改善。我们的方法优于基于坡度的方法,尤其是对于更频繁的雪崩而言;但是,由于未集成积雪堆稳定性,因此该算法作为预测工具的应用仍然受到限制。因此,未来的研究活动应集中在算法与积雪条件的耦合上。

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