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    A Consistent Hybrid Variational-Smoothing Data Assimilation Method: Application to a Simple Shallow-Water Model of the Turbulent Midlatitude Ocean

    Source: Monthly Weather Review:;2011:;volume( 139 ):;issue: 011::page 3333
    Author:
    Krysta, Monika
    ,
    Blayo, Eric
    ,
    Cosme, Emmanuel
    ,
    Verron, Jacques
    DOI: 10.1175/2011MWR3150.1
    Publisher: American Meteorological Society
    Abstract: n 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.
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      A Consistent Hybrid Variational-Smoothing Data Assimilation Method: Application to a Simple Shallow-Water Model of the Turbulent Midlatitude Ocean

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4214110
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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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