Block iterative correction in strongly coupled data assimilation

The ongoing transition to coupled data assimilation (DA) systems encounters substantial technical difficulties associated with the need to merge together different elements of atmospheric and ocean DA systems that typically have had independent development paths for decades. In this study, we consid...

Full description

Saved in:
Bibliographic Details
Published inQuarterly journal of the Royal Meteorological Society Vol. 147; no. 738; pp. 2729 - 2740
Main Authors Yaremchuk, Max, Beattie, Christopher, Frolov, Sergey
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.07.2021
Wiley Subscription Services, Inc
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:The ongoing transition to coupled data assimilation (DA) systems encounters substantial technical difficulties associated with the need to merge together different elements of atmospheric and ocean DA systems that typically have had independent development paths for decades. In this study, we consider the incorporation of strong coupling in the observation space via successive corrections that involve the application of only uncoupled solvers to a sequence of innovation vectors. The coupled increment is then obtained by projecting a coupled innovation vector on the grid using coupled ensemble correlations. The proposed approach is motivated by the classic block Jacobi matrix iteration applied to the coupled system using the uncoupled solvers as a preconditioner. The method is tested via numerical experiments with the CERA ensemble in a simplified setting. A method of recursive corrections is proposed for transitioning a set of uncoupled data assimilation systems to the strongly coupled formulation. The method is based on applying uncoupled solvers to a sequence of coupled innovation vectors. Testing of the method with the CERA ensemble has shown its fast convergence: The approximation error of the strongly coupled solution drops 5–12‐fold per iteration depending on the location of the uncoupled solution subject to correction. Error reduction in the equatorial region of the Tropical Pacific is shown for two types of the localization kernels used to regularize the background error covariance.
Bibliography:Funding information
NSF,DMS‐1923221;DMS‐1819110
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 14
ISSN:0035-9009
1477-870X
DOI:10.1002/qj.4047