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Input uncertainty propagation methods and hazard mapping of geophysical mass flows

机译:输入不确定性传播方法和地球物理质量流危害图

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This paper presents several standard and new methods for characterizing the effect of input data uncertainty on model output for hazardous geophysical mass flows. Note that we do not attempt here to characterize the inherent randomness of such flow events. We focus here on the problem of characterizing uncertainty in model output due to lack of knowledge of such input for a particular event. Methods applied include classical Monte Carlo and Latin hypercube sampling and more recent stochastic collocation, polynomial chaos, spectral projection and a newly developed extension thereof named polynomial chaos quadrature. The simple and robust samplings based Monte Carlo type methods are usually computationally intractable for reasonable physical models, while the more sophisticated and computationally efficient polynomial chaos method often breaks down for complex models. The spectral projection and polynomial chaos quadrature methods discussed here produce results of quality comparable to the polynomial chaos type methods while preserving the simplicity and robustness of the Monte Carlo-type sampling based approaches at much lower cost. The computational efficiency, however, degrades with increasing numbers of random variables. A procedure for converting the output uncertainty characterization into a map showing the probability of a hazard threshold being exceeded is also presented. The uncertainty quantification procedures are applied first in simple settings to illustrate the procedure and then subsequently applied to the 1991 block-and-ash flows at Colima Volcano, Mexico.
机译:本文提出了几种标准和新方法,用于表征危险地球物理质量流的输入数据不确定性对模型输出的影响。请注意,我们在此不尝试描述此类流事件的固有随机性。由于缺乏对特定事件的这种输入的知识,我们在这里集中讨论表征模型输出的不确定性的问题。所应用的方法包括经典的蒙特卡洛和拉丁超立方体采样以及最近的随机配置,多项式混沌,频谱投影及其最新开发的扩展,称为多项式混沌正交。对于合理的物理模型,基于蒙特卡洛类型方法的简单且健壮的采样通常难以计算,而对于复杂的模型而言,更复杂,计算效率更高的多项式混沌方法通常会崩溃。本文讨论的频谱投影和多项式混沌正交方法产生的结果可与多项式混沌类型方法相媲美,同时以更低的成本保留了基于蒙特卡洛类型采样方法的简单性和鲁棒性。但是,计算效率随着随机变量数量的增加而降低。还提出了将输出不确定性特征转换为表示超出危险阈值的概率的映射的过程。不确定性量化程序首先在简单的环境中应用以说明该程序,然后再应用于1991年墨西哥科利马火山的块状和灰分流量。

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