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arXiv 2603.04697stat.ME

多保真度张量模拟器用于时空输出:北极海冰动力学的模拟

A Multi-Fidelity Tensor Emulator for Spatiotemporal Outputs: Emulation of Arctic Sea-Ice Dynamics

Colorado State University(科罗拉多州立大学);Los Alamos National Laboratory(洛斯阿拉莫斯国家实验室);University of New Mexico(新墨西哥大学)

Tristan Contant, Yawen Guan, Ander Wilson, Adrian K. Turner, Deborah Sulsky

AI总结:

本文提出一种多保真度张量模拟器,结合张量分解、高斯过程和加法差异模型,用于高效模拟北极海冰动力学的时空输出,减少计算成本并提高预测准确性。

摘要:

数值模型被广泛用于模拟地球系统,但它们计算成本高且通常依赖许多不确定的输入参数。其有效使用需要校准和不确定性量化,这通常涉及在许多输入配置下运行模型,因此会产生显著的计算成本。统计模拟提供了一种实用的替代方法,以高效地探索模型行为。我们受到能量exascale地球系统模型(MPAS-Seaice)中的北极海冰组件的启发,该模型在多个空间分辨率下生成大规模时空输出,高分辨率(或高保真度,HF)模拟比低分辨率(低保真度,LF)模拟更准确但计算成本更高。多保真度(MF)模拟整合不同分辨率的信息以构建高效且准确的替代模型,但现有方法难以扩展到大规模时空数据。我们开发了一个MF模拟器,结合张量分解进行降维、高斯过程先验用于灵活的功能近似,以及加法差异模型以捕捉LF和HF数据之间的系统性差异。所提出的框架实现了可扩展的模拟,同时保持了准确的预测和良好的不确定性校准,能够在模拟研究和MPAS-Seaice分析中一致地实现更低的预测误差和更小的不确定性,优于仅使用LF或仅使用HF模型。通过利用LF和HF数据的互补优势,并采用高效的张量分解方法,我们的模拟器大大降低了计算成本,使其非常适合涉及复杂物理模型的大规模模拟任务。

英文摘要:

Numerical models are widely used to simulate the Earth system, but they are computationally expensive and often depend on many uncertain input parameters. Calibration and uncertainty quantification require running them across many input configurations, so their effective use is costly. Statistical emulation provides a practical alternative for efficiently exploring model behavior. We are motivated by the Arctic sea-ice component of the Energy Exascale Earth System Model (MPAS-Seaice), which generates large spatiotemporal outputs at multiple spatial resolutions, with high-resolution (or high-fidelity, HF) simulations being more accurate but computationally more expensive than lower-resolution (low-fidelity, LF) simulations. Multi-fidelity (MF) emulation integrates information across resolutions to construct efficient and accurate surrogate models, yet existing approaches struggle to scale to large spatiotemporal data. We develop a MF emulator that combines tensor decomposition for dimensionality reduction, Gaussian process priors for flexible function approximation, and an additive discrepancy model to capture systematic differences between LF and HF data. The proposed framework scales to complex spatiotemporal fields while keeping predictions accurate and uncertainty well calibrated. In the MPAS-Seaice analysis, it attains the lowest prediction error of all emulators considered, including separable-covariance and neural-network approaches, especially throughout the summer melt season, when sea-ice concentration varies most across model settings and matters most scientifically, and best reproduces the spatiotemporal dependence of the output. By combining many inexpensive low-resolution runs with a few expensive high-resolution ones, the emulator substantially reduces the simulation cost of exploring model behavior, and suits large-scale studies involving complex physical models.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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