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Relating simple drivers to snow instability

机译:将简单的驱动程序与雪不稳定相关联

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Snow layers form during and after accumulation due to the interaction of meteorological and physical processes. It is known that the vertical structure and also the lateral continuity of layers depend on these processes and the boundaries set by the terrain. This study addresses the variations seen among vertical penetration resistance profiles and investigates possible forcings at the basin scale. In the past years we acquired a unique dataset with 613 snow micro-penetrometer (SMP) resistance measurements covering a variety of dry-snow conditions. With recent advances,in signal processing all snow layer properties required for snow instability modeling are extracted from a SMP signal so that quantitative metrics of the propensity to failure initiation and crack propagation can be calculated. The modeled values of instability corresponded well with field test results obtained during the measurement campaigns and the verified, local danger. We then analyzed whether snow instability was related to simple drivers such as slope aspect, snow depth, and slope angle. In general, aspect was the most prominent driver as. on all field days we found associations of our measures of snow instability with aspect. For 'old' slab layers the relation between aspect and snow instability was more pronounced than for recently deposited slab layers. However, the relationships between drivers and our measures of snow instability varied depending on whether we analyzed the single field days separately or jointly. Considering all field days jointly, which reflects mean trends over varying snowpack conditions, slope angle was weakly related to the failure initiation propensity and snow depth to the crack propagation propensity. Our findings suggest that with SMP field measurements differences in snow conditions can be resolved which relate to the failure initiation and crack propagation propensity relevant for snow instability assessment. Our analysis of terrain and snow depth data showed that readily and widely available simple drivers have the potential to enhance snow instability predictions from point measurements at the basin scale. (C) 2015 The Authors. Published by Elsevier B.V.
机译:由于气象和物理过程的相互作用,积雪期间和之后形成积雪层。众所周知,层的垂直结构以及横向连续性取决于这些过程和地形设定的边界。这项研究解决了垂直渗透阻力剖面之间的差异,并研究了盆地规模的可能强迫。在过去的几年中,我们获得了一个独特的数据集,该数据集具有613种雪微渗透仪(SMP)的电阻测量值,涵盖了各种干燥雪况。随着最新技术的发展,在信号处理中,从SMP信号中提取了雪不稳定模型所需的所有雪层特性,从而可以计算出破坏引发和裂纹扩展倾向的定量指标。不稳定性的建模值与在测量活动中获得的现场测试结果以及经过验证的局部危险性非常吻合。然后,我们分析了雪的不稳定性是否与简单的驱动因素有关,例如坡度,雪深和坡度。一般而言,aspect是最主要的驱动因素。在所有田间日,我们都发现积雪不稳定性与纵横比之间存在关联。对于“旧”板层,与最近沉积的板层相比,坡向与积雪不稳定性之间的关系更为明显。但是,根据我们是单独分析还是联合分析单个田间日,驾驶员与我们的积雪不稳定性测度之间的关系有所不同。联合考虑所有田间日,这反映了不同积雪条件下的平均趋势,因此倾斜角与破坏起始倾向和降雪深度与裂纹扩展倾向之间的关系微弱。我们的发现表明,通过SMP现场测量,可以解决积雪条件下的差异,这与与积雪不稳定性评估相关的破坏开始和裂纹扩展倾向有关。我们对地形和积雪深度数据的分析表明,现成的,广泛可用的简单驱动程序有可能增强根据流域尺度上的点测量得出的积雪不稳定性预测。 (C)2015作者。由Elsevier B.V.发布

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