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    Distributed Forcing of Forecast and Assimilation Error Systems

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 002::page 460
    Author:
    Farrell, Brian F.
    ,
    Ioannou, Petros J.
    DOI: 10.1175/JAS-3374.1
    Publisher: American Meteorological Society
    Abstract: Temporally distributed deterministic and stochastic excitation of the tangent linear forecast system governing forecast error growth and the tangent linear observer system governing assimilation error growth is examined. The method used is to determine the optimal set of distributed deterministic and stochastic forcings of the forecast and observer systems over a chosen time interval. Distributed forcing of an unstable system addresses the effect of model error on forecast error in the presumably unstable forecast error system. Distributed forcing of a stable system addresses the effect on the assimilation of model error in the presumably stable data assimilation system viewed as a stable observer. In this study, model error refers both to extrinsic physical error forcing, such as that which arises from unresolved cumulus activity, and to intrinsic error sources arising from imperfections in the numerical model and in the physical parameterizations.
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      Distributed Forcing of Forecast and Assimilation Error Systems

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4217912
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    contributor authorFarrell, Brian F.
    contributor authorIoannou, Petros J.
    date accessioned2017-06-09T16:52:00Z
    date available2017-06-09T16:52:00Z
    date copyright2005/02/01
    date issued2005
    identifier issn0022-4928
    identifier otherams-75562.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217912
    description abstractTemporally distributed deterministic and stochastic excitation of the tangent linear forecast system governing forecast error growth and the tangent linear observer system governing assimilation error growth is examined. The method used is to determine the optimal set of distributed deterministic and stochastic forcings of the forecast and observer systems over a chosen time interval. Distributed forcing of an unstable system addresses the effect of model error on forecast error in the presumably unstable forecast error system. Distributed forcing of a stable system addresses the effect on the assimilation of model error in the presumably stable data assimilation system viewed as a stable observer. In this study, model error refers both to extrinsic physical error forcing, such as that which arises from unresolved cumulus activity, and to intrinsic error sources arising from imperfections in the numerical model and in the physical parameterizations.
    publisherAmerican Meteorological Society
    titleDistributed Forcing of Forecast and Assimilation Error Systems
    typeJournal Paper
    journal volume62
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-3374.1
    journal fristpage460
    journal lastpage475
    treeJournal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 002
    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