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Validating the Space-Time model for infrequent snow avalanche events using field observations from the Columbia and Rocky Mountains, Canada

机译:使用加拿大哥伦比亚和落基山脉的实地观察验证时空雪崩事件的时空模型

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摘要

Avalanche runout distance and return period estimates are essential to snow avalanche risk assessment for hazard mapping and mitigation design. We present a validation of the Space-Time (ST) model, a statistical model that expresses runout distance as a function of return period. The validation is based on field observations of tree damage and tree ring data of infrequent (1:5 to 1:100 year return period) avalanches from 34 paths in the Canadian Rocky and Columbia Mountains. While the ST model has been applied successfully for a longer return period (>100 year) runouts in one path, our validation showed that it does not independently estimate infrequent runout distances with sufficient accuracy for hazard mapping and mitigation design. As with estimating extreme runouts, it should be used in combination with other methods. The model was found to perform differently across mountain ranges, and tended to estimate runout distance downslope of those observed in the field.
机译:雪崩跳动距离和返回期估计对于雪灾雪崩风险评估和危害设计至关重要。我们提出了对时空(ST)模型的验证,该模型是将跳动距离表示为返回周期的函数的统计模型。验证是基于对加拿大落基山脉和哥伦比亚山脉34条路径上不频繁(1:5至1:100年回归期)雪崩的树木观察和年轮数据进行的实地观察。虽然ST模型已成功地在一条路径上用于较长的返回期(> 100年)跳动,但我们的验证表明,它并不能以足够的精度独立估计不频繁的跳动距离,以进行危害图和缓解设计。与估算极端跳动一样,应将其与其他方法结合使用。发现该模型在整个山脉上表现不同,并且倾向于估计野外观测到的跳动距离下坡。

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