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    Accounting for Skewness in Ensemble Data Assimilation

    Source: Monthly Weather Review:;2012:;volume( 140 ):;issue: 007::page 2346
    Author:
    Hodyss, Daniel
    DOI: 10.1175/MWR-D-11-00198.1
    Publisher: American Meteorological Society
    Abstract: practical data assimilation algorithm is presented that explicitly accounts for skewness in the prior distribution. The algorithm operates as a global solve (all observations are considered at once) using a minimization-based approach and Schur?Hadamard (elementwise) localization. The central feature of this technique is the squaring of the innovation and the ensemble perturbations so as to create an extended state space that accounts for the second, third, and fourth moments of the prior distribution. This new technique is illustrated in a simple scalar system as well as in a Boussinesq model configured to simulate nonlinearly evolving shear instabilities (Kelvin?Helmholtz waves). It is shown that an ensemble size of at least 100 members is needed to adequately resolve the third and fourth moments required for the algorithm. For ensembles of this size it is shown that this new technique is superior to a state-of-the-art ensemble Kalman filter in situations with significant skewness; otherwise, the new algorithm reduces to the performance of the ensemble Kalman filter.
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      Accounting for Skewness in Ensemble Data Assimilation

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    contributor authorHodyss, Daniel
    date accessioned2017-06-09T17:29:35Z
    date available2017-06-09T17:29:35Z
    date copyright2012/07/01
    date issued2012
    identifier issn0027-0644
    identifier otherams-86213.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229747
    description abstractpractical data assimilation algorithm is presented that explicitly accounts for skewness in the prior distribution. The algorithm operates as a global solve (all observations are considered at once) using a minimization-based approach and Schur?Hadamard (elementwise) localization. The central feature of this technique is the squaring of the innovation and the ensemble perturbations so as to create an extended state space that accounts for the second, third, and fourth moments of the prior distribution. This new technique is illustrated in a simple scalar system as well as in a Boussinesq model configured to simulate nonlinearly evolving shear instabilities (Kelvin?Helmholtz waves). It is shown that an ensemble size of at least 100 members is needed to adequately resolve the third and fourth moments required for the algorithm. For ensembles of this size it is shown that this new technique is superior to a state-of-the-art ensemble Kalman filter in situations with significant skewness; otherwise, the new algorithm reduces to the performance of the ensemble Kalman filter.
    publisherAmerican Meteorological Society
    titleAccounting for Skewness in Ensemble Data Assimilation
    typeJournal Paper
    journal volume140
    journal issue7
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-11-00198.1
    journal fristpage2346
    journal lastpage2358
    treeMonthly Weather Review:;2012:;volume( 140 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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