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    A Simulation Study Using a Local Ensemble Transform Kalman Filter for Data Assimilation in New York Harbor

    Source: Journal of Atmospheric and Oceanic Technology:;2008:;volume( 025 ):;issue: 009::page 1638
    Author:
    Hoffman, Ross N.
    ,
    Ponte, Rui M.
    ,
    Kostelich, Eric J.
    ,
    Blumberg, Alan
    ,
    Szunyogh, Istvan
    ,
    Vinogradov, Sergey V.
    ,
    Henderson, John M.
    DOI: 10.1175/2008JTECHO565.1
    Publisher: American Meteorological Society
    Abstract: Data assimilation approaches that use ensembles to approximate a Kalman filter have many potential advantages for oceanographic applications. To explore the extent to which this holds, the Estuarine and Coastal Ocean Model (ECOM) is coupled with a modern data assimilation method based on the local ensemble transform Kalman filter (LETKF), and a series of simulation experiments is conducted. In these experiments, a long ECOM ?nature? run is taken to be the ?truth.? Observations are generated at analysis times by perturbing the nature run at randomly chosen model grid points with errors of known statistics. A diverse collection of model states is used for the initial ensemble. All experiments use the same lateral boundary conditions and external forcing fields as in the nature run. In the data assimilation, the analysis step combines the observations and the ECOM forecasts using the Kalman filter equations. As a control, a free-running forecast (FRF) is made from the initial ensemble mean to check the relative importance of external forcing versus data assimilation on the analysis skill. Results of the assimilation cycle and the FRF are compared to truth to quantify the skill of each. The LETKF performs well for the cases studied here. After just a few assimilation cycles, the analysis errors are smaller than the observation errors and are much smaller than the errors in the FRF. The assimilation quickly eliminates the domain-averaged bias of the initial ensemble. The filter accurately tracks the truth at all data densities examined, from observations at 50% of the model grid points down to 2% of the model grid points. As the data density increases, the ensemble spread, bias, and error standard deviation decrease. As the ensemble size increases, the ensemble spread increases and the error standard deviation decreases. Increases in the size of the observation error lead to a larger ensemble spread but have a small impact on the analysis accuracy.
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      A Simulation Study Using a Local Ensemble Transform Kalman Filter for Data Assimilation in New York Harbor

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4209210
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorHoffman, Ross N.
    contributor authorPonte, Rui M.
    contributor authorKostelich, Eric J.
    contributor authorBlumberg, Alan
    contributor authorSzunyogh, Istvan
    contributor authorVinogradov, Sergey V.
    contributor authorHenderson, John M.
    date accessioned2017-06-09T16:25:48Z
    date available2017-06-09T16:25:48Z
    date copyright2008/09/01
    date issued2008
    identifier issn0739-0572
    identifier otherams-67731.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209210
    description abstractData assimilation approaches that use ensembles to approximate a Kalman filter have many potential advantages for oceanographic applications. To explore the extent to which this holds, the Estuarine and Coastal Ocean Model (ECOM) is coupled with a modern data assimilation method based on the local ensemble transform Kalman filter (LETKF), and a series of simulation experiments is conducted. In these experiments, a long ECOM ?nature? run is taken to be the ?truth.? Observations are generated at analysis times by perturbing the nature run at randomly chosen model grid points with errors of known statistics. A diverse collection of model states is used for the initial ensemble. All experiments use the same lateral boundary conditions and external forcing fields as in the nature run. In the data assimilation, the analysis step combines the observations and the ECOM forecasts using the Kalman filter equations. As a control, a free-running forecast (FRF) is made from the initial ensemble mean to check the relative importance of external forcing versus data assimilation on the analysis skill. Results of the assimilation cycle and the FRF are compared to truth to quantify the skill of each. The LETKF performs well for the cases studied here. After just a few assimilation cycles, the analysis errors are smaller than the observation errors and are much smaller than the errors in the FRF. The assimilation quickly eliminates the domain-averaged bias of the initial ensemble. The filter accurately tracks the truth at all data densities examined, from observations at 50% of the model grid points down to 2% of the model grid points. As the data density increases, the ensemble spread, bias, and error standard deviation decrease. As the ensemble size increases, the ensemble spread increases and the error standard deviation decreases. Increases in the size of the observation error lead to a larger ensemble spread but have a small impact on the analysis accuracy.
    publisherAmerican Meteorological Society
    titleA Simulation Study Using a Local Ensemble Transform Kalman Filter for Data Assimilation in New York Harbor
    typeJournal Paper
    journal volume25
    journal issue9
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/2008JTECHO565.1
    journal fristpage1638
    journal lastpage1656
    treeJournal of Atmospheric and Oceanic Technology:;2008:;volume( 025 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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