Data assimilation empowered neural network parametrizations for subgrid processes in geophysical flows

Suraj Pawar, O. San
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引用次数: 30

Abstract

In the past couple of years, there is a proliferation in the use of machine learning approaches to represent subgrid scale processes in geophysical flows with an aim to improve the forecasting capability and to accelerate numerical simulations of these flows. Despite its success for different types of flow, the online deployment of a data-driven closure model can cause instabilities and biases in modeling the overall effect of subgrid scale processes, which in turn leads to inaccurate prediction. To tackle this issue, we exploit the data assimilation technique to correct the physics-based model coupled with the neural network as a surrogate for unresolved flow dynamics in multiscale systems. In particular, we use a set of neural network architectures to learn the correlation between resolved flow variables and the parameterizations of unresolved flow dynamics and formulate a data assimilation approach to correct the hybrid model during their online deployment. We illustrate our framework in a application of the multiscale Lorenz 96 system for which the parameterization model for unresolved scales is exactly known. Our analysis, therefore, comprises a predictive dynamical core empowered by (i) a data-driven closure model for subgrid scale processes, (ii) a data assimilation approach for forecast error correction, and (iii) both data-driven closure and data assimilation procedures. We show significant improvement in the long-term perdition of the underlying chaotic dynamics with our framework compared to using only neural network parameterizations for future prediction. Moreover, we demonstrate that these data-driven parameterization models can handle the non-Gaussian statistics of subgrid scale processes, and effectively improve the accuracy of outer data assimilation workflow loops in a modular non-intrusive way.
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数据同化增强了地球物理流中子网格过程的神经网络参数化
在过去的几年里,为了提高预测能力和加速这些流动的数值模拟,机器学习方法在地球物理流动中表示亚网格尺度过程的使用激增。尽管数据驱动的封闭模型在不同类型的流中取得了成功,但在线部署数据驱动的封闭模型在模拟亚网格尺度过程的整体影响时可能会导致不稳定和偏差,从而导致预测不准确。为了解决这个问题,我们利用数据同化技术来校正基于物理的模型,并将神经网络作为多尺度系统中未解决的流动动力学的替代。特别是,我们使用一组神经网络架构来学习已解决的流动变量与未解决的流动动力学参数化之间的相关性,并制定了一种数据同化方法来纠正混合模型在其在线部署过程中。我们在多尺度洛伦兹96系统的应用中说明了我们的框架,其中未解析尺度的参数化模型是完全已知的。因此,我们的分析包括一个预测动态核心,该核心由(i)用于子网格尺度过程的数据驱动闭合模型,(ii)用于预测误差校正的数据同化方法,以及(iii)数据驱动闭合和数据同化程序。与仅使用神经网络参数化进行未来预测相比,我们的框架在潜在混沌动力学的长期预测方面有了显着改善。此外,我们还证明了这些数据驱动的参数化模型可以处理子网格尺度过程的非高斯统计,并以模块化的非侵入性方式有效地提高了外部数据同化工作流循环的精度。
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