Debris-flow entrainment modelling under climate change: Considering antecedent moisture conditions along the flow path

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Anna Lena Könz, Jacob Hirschberg, Brian W. McArdell, Benjamin B. Mirus, Tjalling de Haas, Perry Bartelt, Peter Molnar
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Abstract

Debris-flow volumes can increase along their flow path by entraining sediment stored in the channel bed and banks, thus also increasing hazard potential. Theoretical considerations, laboratory experiments and field investigations all indicate that the saturation conditions of the sediment along the flow path can greatly influence the amount of sediment entrained. However, this process is usually not considered for practical applications. This study aims to close this gap by combining runout and hydrological models into a predictive framework that is calibrated and tested using unique observations of sediment erosion and debris-flow properties available at a Swiss debris-flow observation station (Illgraben). To this end, hourly water input to the erodible channel is predicted using a simple, process-based hydrological model, and the resulting water saturation level in the upper sediment layer of the channel is modelled based on a Hortonian infiltration concept. Debris-flow entrainment is then predicted using the RAMMS debris-flow runout model. We find a strong correlation between the modelled saturation level of the sediment on the flow path and the channel-bed erodibility for single-surge debris-flow events with distinct fronts, indicating that the modelled water content is a good predictor for erosion simulated in RAMMS. Debris-flow properties with more complex flow behaviour (e.g., multiple surges or roll waves) are not as well predicted using this procedure, indicating that more physically complete models are necessary. Finally, we demonstrate how this modelling framework can be used for climate change impact assessment and show that earlier snowmelt may shift the peak of the debris-flow season to earlier in the year. Our novel modelling framework provides a plausible approach to reproduce saturation-dependent entrainment and thus better constrain event volumes for current and future hazard assessment.

Abstract Image

气候变化下的泥石流夹带模型:考虑沿水流路径的先期湿度条件
泥石流会夹带河床和河岸中储存的沉积物,从而增加其沿流路径的流量,从而增加潜在的危害。理论上的考虑、实验室实验和实地调查都表明,沿水流路径沉积物的饱和条件会在很大程度上影响沉积物的夹带量。然而,在实际应用中通常不会考虑这一过程。本研究旨在缩小这一差距,将径流模型和水文模型结合到一个预测框架中,并利用瑞士泥石流观测站(Illgraben)对泥沙侵蚀和泥石流特性的独特观测结果对该框架进行校准和测试。为此,利用一个简单的、基于过程的水文模型对每小时输入可侵蚀河道的水量进行了预测,并根据霍顿渗透概念对河道上部沉积层的水饱和度进行了模拟。然后使用 RAMMS 泥石流冲刷模型对泥石流夹带进行预测。我们发现,对于具有明显前沿的单次喷发泥石流事件,流道上泥沙的建模饱和度与河床侵蚀性之间具有很强的相关性,这表明建模含水量可以很好地预测 RAMMS 模拟的侵蚀情况。使用该程序并不能很好地预测具有更复杂流动行为的泥石流特性(例如多涌流或滚浪),这表明有必要使用物理上更完整的模型。最后,我们展示了如何将这一建模框架用于气候变化影响评估,并表明融雪期的提前可能会使泥石流季节的峰值提前。我们新颖的建模框架为再现依赖饱和度的夹带提供了一种可行的方法,从而为当前和未来的灾害评估提供了更好的事件量约束。
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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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