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    Hybrid 4DVAR with a Local Ensemble Tangent Linear Model: Application to the Shallow-Water Model

    Source: Monthly Weather Review:;2016:;volume( 145 ):;issue: 001::page 97
    Author:
    Allen, Douglas R.
    ,
    Bishop, Craig H.
    ,
    Frolov, Sergey
    ,
    Hoppel, Karl W.
    ,
    Kuhl, David D.
    ,
    Nedoluha, Gerald E.
    DOI: 10.1175/MWR-D-16-0184.1
    Publisher: American Meteorological Society
    Abstract: n ensemble-based tangent linear model (TLM) is described and tested in data assimilation experiments using a global shallow-water model (SWM). A hybrid variational data assimilation system was developed with a 4D variational (4DVAR) solver that could be run either with a conventional TLM or a local ensemble TLM (LETLM) that propagates analysis corrections using only ensemble statistics. An offline ensemble Kalman filter (EnKF) is used to generate and maintain the ensemble. The LETLM uses data within a local influence volume, similar to the local ensemble transform Kalman filter, to linearly propagate the state variables at the central grid point. After tuning the LETLM with offline 6-h forecasts of analysis corrections, cycling experiments were performed that assimilated randomly located SWM height observations, based on a truth run with forced bottom topography. The performance using the LETLM is similar to that of the conventional TLM, suggesting that a well-constructed LETLM could free 4D variational methods from dependence on conventional TLMs. This is a first demonstration of the LETLM application within a context of a hybrid-4DVAR system applied to a complex two-dimensional fluid dynamics problem. Sensitivity tests are included that examine LETLM dependence on several factors including length of cycling window, size of analysis correction, spread of initial ensemble perturbations, ensemble size, and model error. LETLM errors are shown to increase linearly with correction size in the linear regime, while TLM errors increase quadratically. As nonlinearity (or forecast model error) increases, the two schemes asymptote to the same solution.
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      Hybrid 4DVAR with a Local Ensemble Tangent Linear Model: Application to the Shallow-Water Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4231008
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    • Monthly Weather Review

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    contributor authorAllen, Douglas R.
    contributor authorBishop, Craig H.
    contributor authorFrolov, Sergey
    contributor authorHoppel, Karl W.
    contributor authorKuhl, David D.
    contributor authorNedoluha, Gerald E.
    date accessioned2017-06-09T17:34:12Z
    date available2017-06-09T17:34:12Z
    date copyright2017/01/01
    date issued2016
    identifier issn0027-0644
    identifier otherams-87349.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4231008
    description abstractn ensemble-based tangent linear model (TLM) is described and tested in data assimilation experiments using a global shallow-water model (SWM). A hybrid variational data assimilation system was developed with a 4D variational (4DVAR) solver that could be run either with a conventional TLM or a local ensemble TLM (LETLM) that propagates analysis corrections using only ensemble statistics. An offline ensemble Kalman filter (EnKF) is used to generate and maintain the ensemble. The LETLM uses data within a local influence volume, similar to the local ensemble transform Kalman filter, to linearly propagate the state variables at the central grid point. After tuning the LETLM with offline 6-h forecasts of analysis corrections, cycling experiments were performed that assimilated randomly located SWM height observations, based on a truth run with forced bottom topography. The performance using the LETLM is similar to that of the conventional TLM, suggesting that a well-constructed LETLM could free 4D variational methods from dependence on conventional TLMs. This is a first demonstration of the LETLM application within a context of a hybrid-4DVAR system applied to a complex two-dimensional fluid dynamics problem. Sensitivity tests are included that examine LETLM dependence on several factors including length of cycling window, size of analysis correction, spread of initial ensemble perturbations, ensemble size, and model error. LETLM errors are shown to increase linearly with correction size in the linear regime, while TLM errors increase quadratically. As nonlinearity (or forecast model error) increases, the two schemes asymptote to the same solution.
    publisherAmerican Meteorological Society
    titleHybrid 4DVAR with a Local Ensemble Tangent Linear Model: Application to the Shallow-Water Model
    typeJournal Paper
    journal volume145
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-16-0184.1
    journal fristpage97
    journal lastpage116
    treeMonthly Weather Review:;2016:;volume( 145 ):;issue: 001
    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
    yabeshDSpacePersian