Enhancement of the ensemble nonlinear least‐squares algorithm for <scp>i4DVar</scp>

Abstract The integral‐correcting 4DVar method (i4DVar) is an evolution of the traditional strongly constrained 4DVar method (s4DVar), which performs much better than s4DVar without increasing computational cost and complexity, and is solved using an ensemble, adjoint‐free algorithm (i.e., NLS‐i4DVar). However, like most previous ensemble‐based methods, NLS‐i4DVar also faces the paradox of using the same set of perturbed samples to approximate the background error covariance matrix and the joint tangent linear (TL) operator, making it difficult to guarantee their accuracy. To solve this problem, we divide ensemble anomalies with a (very large) shrinkage factor to ensure the validity of the TL operator approximation, while still using the original (unshrunk) samples to approximate the background error covariance matrix, which ultimately solves the above difficulty. Finally, the advantages of the newly developed algorithm are verified by numerical evaluation experiments.

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Publication Details

Journal
Quarterly Journal of the Royal Meteorological Society
Published
2025-04-13
DOI
https://doi.org/10.1002/qj.4981
Primary Topic
Meteorological Phenomena and Simulations
Type
article
Field-Weighted Citation Impact
0.00

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article

Enhancement of the ensemble nonlinear least‐squares algorithm for i4DVar

Xiangjun Tian
Quarterly Journal of the Royal Meteorological Society
Meteorological Phenomena and Simulations
article

Enhancement of the ensemble nonlinear least‐squares algorithm for i4DVar

Xiangjun Tian
article en

Abstract

Abstract The integral‐correcting 4DVar method (i4DVar) is an evolution of the traditional strongly constrained 4DVar method (s4DVar), which performs much better than s4DVar without increasing computational cost and complexity, and is solved using an ensemble, adjoint‐free algorithm (i.e., NLS‐i4DVar). However, like most previous ensemble‐based methods, NLS‐i4DVar also faces the paradox of using the same set of perturbed samples to approximate the background error covariance matrix and the joint tangent linear (TL) operator, making it difficult to guarantee their accuracy. To solve this problem, we divide ensemble anomalies with a (very large) shrinkage factor to ensure the validity of the TL operator approximation, while still using the original (unshrunk) samples to approximate the background error covariance matrix, which ultimately solves the above difficulty. Finally, the advantages of the newly developed algorithm are verified by numerical evaluation experiments.

Quarterly Journal of the Royal Meteorological SocietyVol. 151(770)
Chinese Academy of Sciences (CN), Institute of Tibetan Plateau Research (CN), University of Chinese Academy of Sciences (CN)
National Natural Science Foundation of China, National Key Research and Development Program of China
Openalex Percentile: Top 88%
Meteorological Phenomena and Simulations
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