The paper addresses the scalability issues in numerical weather prediction systems, where data assimilation (DA) is a core component. DA aims to combine earth observations with assumptions about the weather state to produce an updated estimate.
The authors formulate DA as a Bayesian inference problem, with the weather state as the latent variable and the observations as the data. They exploit the Gaussian Markov random field (GMRF) structure of the prior to develop a message-passing algorithm for inference. Message passing is inherently based on local computations, making it well-suited for parallel and distributed computation.
The key steps are:
The authors compare the performance of their message-passing approach against a GPU-accelerated 3D-Var implementation, which is a commonly used variational method in operational weather forecasting. On simulated data and a realistic surface temperature assimilation problem, the message-passing approach achieves similar accuracy to 3D-Var while being more scalable, especially for low observation densities.
The main limitation of the message-passing approach is that it can only reliably compute the posterior mean, and not the full posterior distribution. This prevents using the marginal likelihood for hyperparameter learning. The authors discuss potential extensions to address this limitation.
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by Oscar Key,So... at arxiv.org 04-22-2024
https://arxiv.org/pdf/2404.12968.pdfDeeper Inquiries