Model and observation‐error covariance matrix information in the physical nudging equations

Abstract In this work we show how to extend the deterministic physical nudging scheme in order to include two important ingredients, the model and observation‐error covariance matrices, which are common features of classical data‐assimilation schemes. The method exploits the relation between a stochastic differential equation and the evolution of its probability density via the Fokker–Planck equation. Observations are introduced by evolving the posterior probability density backward in time to obtain a so‐called smoother. To obtain a computationally feasible scheme, we used the small‐time approximation, resulting in an efficient nudging scheme built from first principles. We explored the capabilities of this new nudging method with the low‐dimensional Lorenz 1963 model and a surface quasi‐geostrophic turbulence model on a grid, with many degrees of freedom. We show that the new method is more accurate than a 3DVar at similar computational cost, and is accurate and easy to implement in the high‐dimensional system. The new scheme has the potential to be used in extremely high‐dimensional systems, because ensemble integrations and adjoint models are avoided.

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Publication Details

Journal
Quarterly Journal of the Royal Meteorological Society
Published
2025-04-06
DOI
https://doi.org/10.1002/qj.4979
Citations
2
Primary Topic
Meteorological Phenomena and Simulations
Type
article
Field-Weighted Citation Impact
2.60
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article

Model and observation‐error covariance matrix information in the physical nudging equations

Peter Jan van Leeuwen, Giovanni Conti, J. G. Anderson
2 citations
Quarterly Journal of the Royal Meteorological Society
Meteorological Phenomena and Simulations
2.60
article

Model and observation‐error covariance matrix information in the physical nudging equations

Peter Jan van Leeuwen, Giovanni Conti, J. G. Anderson
article en
2 citations

Abstract

Abstract In this work we show how to extend the deterministic physical nudging scheme in order to include two important ingredients, the model and observation‐error covariance matrices, which are common features of classical data‐assimilation schemes. The method exploits the relation between a stochastic differential equation and the evolution of its probability density via the Fokker–Planck equation. Observations are introduced by evolving the posterior probability density backward in time to obtain a so‐called smoother. To obtain a computationally feasible scheme, we used the small‐time approximation, resulting in an efficient nudging scheme built from first principles. We explored the capabilities of this new nudging method with the low‐dimensional Lorenz 1963 model and a surface quasi‐geostrophic turbulence model on a grid, with many degrees of freedom. We show that the new method is more accurate than a 3DVar at similar computational cost, and is accurate and easy to implement in the high‐dimensional system. The new scheme has the potential to be used in extremely high‐dimensional systems, because ensemble integrations and adjoint models are avoided.

Quarterly Journal of the Royal Meteorological SocietyVol. 151(770)
NSF National Center for Atmospheric Research (US), CMCC Foundation - Euro-Mediterranean Center on Climate Change (IT), Colorado State University (US)
Openalex Percentile: Top 13%
Meteorological Phenomena and Simulations
2.60
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