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contributor authorKrysta, Monika
contributor authorBlayo, Eric
contributor authorCosme, Emmanuel
contributor authorVerron, Jacques
date accessioned2017-06-09T16:40:57Z
date available2017-06-09T16:40:57Z
date copyright2011/11/01
date issued2011
identifier issn0027-0644
identifier otherams-72140.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214110
description abstractn the standard four-dimensional variational data assimilation (4D-Var) algorithm the background error covariance matrix remains static over time. It may therefore be unable to correctly take into account the information accumulated by a system into which data are gradually being assimilated.A possible method for remedying this flaw is presented and tested in this paper. A hybrid variational-smoothing algorithm is based on a reduced-rank incremental 4D-Var. Its consistent coupling to a singular evolutive extended Kalman (SEEK) smoother ensures the evolution of the matrix. In the analysis step, a low-dimensional error covariance matrix is updated so as to take into account the increased confidence level in the state vector it describes, once the observations have been introduced into the system. In the forecast step, the basis spanning the corresponding control subspace is propagated via the tangent linear model.The hybrid method is implemented and tested in twin experiments employing a shallow-water model. The background error covariance matrix is initialized using an EOF decomposition of a sample of model states. The quality of the analyses and the information content in the bases spanning control subspaces are also assessed. Several numerical experiments are conducted that differ with regard to the initialization of the matrix. The feasibility of the method is illustrated. Since improvement due to the hybrid method is not universal, configurations that benefit from employing it instead of the standard 4D-Var are described and an explanation of the possible reasons for this is proposed.
publisherAmerican Meteorological Society
titleA Consistent Hybrid Variational-Smoothing Data Assimilation Method: Application to a Simple Shallow-Water Model of the Turbulent Midlatitude Ocean
typeJournal Paper
journal volume139
journal issue11
journal titleMonthly Weather Review
identifier doi10.1175/2011MWR3150.1
journal fristpage3333
journal lastpage3347
treeMonthly Weather Review:;2011:;volume( 139 ):;issue: 011
contenttypeFulltext


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