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Physically Based Susceptibility Assessment of Rainfall-Induced Shallow Landslides Using a Fuzzy Point Estimate Method

机译:基于模糊点估计的基于物理的降雨诱发浅层滑坡敏感性评价

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摘要

The physically based model has been widely used in rainfall-induced shallow landslide susceptibility analysis because of its capacity to reproduce the physical processes governing landslide occurrence and a higher predictive capability. However, one of the difficulties in applying the physically based model is that uncertainties arising from spatial variability, measurement errors, and incomplete information apply to the input parameters and analysis procedure. Uncertainties have been recognized as an important cause of mismatch between predicted and observed distributions of landslide occurrence. Therefore, probabilistic analysis has been used to quantify the uncertainties. However, some uncertainties, because of incomplete information, cannot be managed satisfactorily using a probabilistic approach. Fuzzy set theory is applicable in this case. In this study, in order to handle uncertainty propagation through a physical model, fuzzy set theory, coupled with the vertex method and the point estimate method, was adopted for regional landslide susceptibility assessment. The proposed approach was used to evaluate susceptibility to rainfall-induced shallow landslides for a regional study area, and the analysis results were compared with landslide inventory to evaluate the performance of the proposed approach. The AUC values arising from the landslide susceptibility analyses using the proposed approach and probabilistic analysis were 0.734 and 0.736, respectively. However, when the COV values of the input parameters were reduced, the AUC values of the proposed approach and the probabilistic analysis were reduced to 0.722 and 0.688, respectively. It means that the performance of the fuzzy approach is similar to that of probabilistic analysis but is more robust against variation of input parameters. Thus, at catchment scale, the fuzzy approach can respond appropriately to the uncertainties inherent in physically based landslide susceptibility analysis, and is especially advantageous when the amount of quality data is very limited.
机译:基于物理的模型由于具有再现控制滑坡发生的物理过程的能力和较高的预测能力,因此已广泛用于降雨引起的浅层滑坡敏感性分析。然而,应用基于物理的模型的困难之一是由空间变异性,测量误差和不完整信息引起的不确定性适用于输入参数和分析过程。不确定性已被认为是预测和观察到的滑坡分布分布不匹配的重要原因。因此,概率分析已用于量化不确定性。但是,由于信息不完整,使用不确定性方法无法令人满意地管理某些不确定性。模糊集理论在这种情况下适用。在这项研究中,为了通过物理模型处理不确定性的传播,采用模糊集理论,结合顶点法和点估计法,对区域滑坡敏感性进行评估。该方法被用于评估区域研究区域对降雨引起的浅层滑坡的敏感性,并将分析结果与滑坡清单进行比较以评估该方法的性能。使用提议的方法和概率分析从滑坡敏感性分析中得出的AUC值分别为0.734和0.736。但是,当输入参数的COV值降低时,建议方法的AUC值和概率分析分别降低到0.722和0.688。这意味着模糊方法的性能与概率分析的性能类似,但是对输入参数的变化更健壮。因此,在流域尺度上,模糊方法可以适当地响应基于物理的滑坡敏感性分析中固有的不确定性,并且在质量数据量非常有限的情况下尤其有利。

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