降水诱发的意大利南蒂罗尔浅层滑坡时空预报的功能回归

IF 3.5 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Mateo Moreno, Luigi Lombardo, Stefan Steger, Lotte de Vugt, Thomas Zieher, Alice Crespi, Francesco Marra, Cees van Westen, Thomas Opitz
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引用次数: 0

摘要

滑坡是全球山地地形的地貌灾害,由静态和动态控制的复杂相互作用驱动。采用数据驱动的方法,分别从空间和时变两方面分析滑坡发生的区域尺度。然而,在空间和时间上对滑坡进行联合评估仍然具有挑战性。本研究旨在预测意大利南蒂罗尔省(7400平方公里)降水引起的浅层滑坡在空间和时间上的发生。我们引入了一个功能预测器框架,其中降水表示为连续时间序列,与将降水视为标量预测器的传统方法形成对比。利用2012 - 2021年的逐时降水数据和过去的滑坡发生情况,我们实现了一个功能广义加性模型,以获得滑坡发生、各种静态标量因子和之前的逐时降水之间的统计关系,作为功能预测因子。我们通过几个交叉验证例程评估结果预测,产生的性能分数经常超过0.90。为了证明模型的预测能力,我们对2016年8月4日至5日在帕塞耶山谷发生的一次风暴事件进行了后播,捕捉了观测到的滑坡位置,并说明了预测概率的逐小时演变。与标准的早期预警方法相比,该框架消除了预先定义降水聚集的固定时间窗口的需要,同时固有地考虑了滞后效应。通过整合静态和动态控制,本研究在空间和时间上推进了大面积滑坡的预测,解决了季节性影响和潜在的数据限制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Functional Regression for Space-Time Prediction of Precipitation-Induced Shallow Landslides in South Tyrol, Italy

Functional Regression for Space-Time Prediction of Precipitation-Induced Shallow Landslides in South Tyrol, Italy

Landslides are geomorphic hazards in mountainous terrains across the globe, driven by a complex interplay of static and dynamic controls. Data-driven approaches have been employed to assess landslide occurrence at regional scales by analyzing the spatial aspects and time-varying conditions separately. However, the joint assessment of landslides in space and time remains challenging. This study aims to predict the occurrence of precipitation-induced shallow landslides in space and time within the Italian province of South Tyrol (7,400 km2). We introduce a functional predictor framework where precipitation is represented as a continuous time series, in contrast to conventional approaches that treat precipitation as a scalar predictor. Using hourly precipitation data and past landslide occurrences from 2012 to 2021, we implemented a functional generalized additive model to derive statistical relationships between landslide occurrence, various static scalar factors, and the preceding hourly precipitation as a functional predictor. We evaluated the resulting predictions through several cross-validation routines, yielding performance scores frequently exceeding 0.90. To demonstrate the model predictive capabilities, we performed a hindcast for a storm event in the Passeier Valley on 4–5 August 2016, capturing the observed landslide locations and illustrating the hourly evolution of the predicted probabilities. Compared to standard early warning approaches, this framework eliminates the need to predefine fixed time windows for precipitation aggregation while inherently accounting for lagged effects. By integrating static and dynamic controls, this research advances the prediction of landslides in space and time for large areas, addressing seasonal effects and underlying data limitations.

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来源期刊
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
6.30
自引率
10.30%
发文量
162
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