用非参数贝叶斯字典学习,从有限观测数据中同时外推风场并量化不确定性。
Joint space-time wind field data extrapolation and uncertainty quantification using nonparametric Bayesian dictionary learning
- 基于观测数据自适应学习低维表示,无需预设基函数。
- 在高维、大距离外推下仍保持高精度,支持任意形式数据。
- 适合传感器受限的风工程场景,可同时给出预测置信度。
提出一种基于非参数贝叶斯字典学习的方法,实现对有限/不完整测量数据下的风场时空外推及统计量估计。通过稀疏或不完整的实测数据,构建时变优化问题以求解随机风场低维表示的展开系数。相比传统压缩感知方法,该方法兼具以下优势:首先,贝叶斯框架可量化估计结果的不确定性;其次,避免了标准压缩感知中需事先选定展开基的限制,而是根据实际数据自适应确定。整体上,在高维、任意形态数据及较大外推距离条件下均表现出更优的外推精度。方法有效性通过两个案例验证:一是三维域(2D+时间)内符合指定联合波数-频率功率谱密度的模拟风速记录外推;二是具有显著空间变异性和非高斯特征的四维(3D+时间)边界层风洞实验数据外推。
原文摘要 · Abstract (English)
A methodology is developed, based on nonparametric Bayesian dictionary learning, for joint space-time wind field data extrapolation and estimation of related statistics by relying on limited/incomplete measurements. Specifically, utilizing sparse/incomplete measured data, a time-dependent optimization problem is formulated for determining the expansion coefficients of an associated low-dimensional representation of the stochastic wind field. Compared to an alternative, standard, compressive sampling treatment of the problem, the developed methodology exhibits the following advantages. First, the Bayesian formulation enables also the quantification of the uncertainty in the estimates. Second, the requirement in standard CS-based applications for an a priori selection of the expansion basis is circumvented. Instead, this is done herein in an adaptive manner based on the acquired data. Overall, the methodology exhibits enhanced extrapolation accuracy, even in cases of high-dimensional data of arbitrary form, and of relatively large extrapolation distances. Thus, it can be used, potentially, in a wide range of wind engineering applications where various constraints dictate the use of a limited number of sensors. The efficacy of the methodology is demonstrated by considering two case studies. The first relates to the extrapolation of simulated wind velocity records consistent with a prescribed joint wavenumber-frequency power spectral density in a three-dimensional domain (2D and time). The second pertains to the extrapolation of four-dimensional (3D and time) boundary layer wind tunnel experimental data that exhibit significant spatial variability and non-Gaussian characteristics.
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