YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Monthly Weather Review
    • View Item
    •   YE&T Library
    • AMS
    • Monthly Weather Review
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    A Fixed-Lag Kalman Smoother for Retrospective Data Assimilation

    Source: Monthly Weather Review:;1994:;volume( 122 ):;issue: 012::page 2838
    Author:
    Cohn, Stephen E.
    ,
    Sivakumaran, N. S.
    ,
    Todling, Ricardo
    DOI: 10.1175/1520-0493(1994)122<2838:AFLKSF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Data assimilation has traditionally been employed to provide initial conditions for numerical weather prediction (NWP). A multiyear time sequence of objective analyses produced by data assimilation can also be used as an archival record from which to carry out a variety of atmospheric process studies. For this latter propose, NWP analyses are not as accurate as they could be, for each analysis is based only on current and past observed data, and not on any future data. Analyses incorporating future data, as well as current and past data, are termed retrospective analyses. The problem of retrospective objective analysis has not yet received attention in the meteorological literature. In this paper, the fixed-lag Kalman smoother (FLKS) is proposed as a means of providing retrospective analysis capability in data assimilation. The FLKS is a direct generalization of the Kalman filter. It incorporates all data observed up to and including some fixed amount of time past each analysis time. A computationally efficient form of the FLKS is derived. A simple scalar examination of the FLKS demonstrates that incorporating future data improves analyses the most in the presence of dynamical instabilities, for accurate models and for accurate observations. An implementation of the FLKS for a two-dimensional linear shallow-water model corroborates the scalar analysis. The numerical experiments also demonstrate the ability of the FLKS to propagate information upstream as well as downstream, thus improving analysis quality substantially in data voids.
    • Download: (1.971Mb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      A Fixed-Lag Kalman Smoother for Retrospective Data Assimilation

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4203398
    Collections
    • Monthly Weather Review

    Show full item record

    contributor authorCohn, Stephen E.
    contributor authorSivakumaran, N. S.
    contributor authorTodling, Ricardo
    date accessioned2017-06-09T16:10:14Z
    date available2017-06-09T16:10:14Z
    date copyright1994/12/01
    date issued1994
    identifier issn0027-0644
    identifier otherams-62500.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203398
    description abstractData assimilation has traditionally been employed to provide initial conditions for numerical weather prediction (NWP). A multiyear time sequence of objective analyses produced by data assimilation can also be used as an archival record from which to carry out a variety of atmospheric process studies. For this latter propose, NWP analyses are not as accurate as they could be, for each analysis is based only on current and past observed data, and not on any future data. Analyses incorporating future data, as well as current and past data, are termed retrospective analyses. The problem of retrospective objective analysis has not yet received attention in the meteorological literature. In this paper, the fixed-lag Kalman smoother (FLKS) is proposed as a means of providing retrospective analysis capability in data assimilation. The FLKS is a direct generalization of the Kalman filter. It incorporates all data observed up to and including some fixed amount of time past each analysis time. A computationally efficient form of the FLKS is derived. A simple scalar examination of the FLKS demonstrates that incorporating future data improves analyses the most in the presence of dynamical instabilities, for accurate models and for accurate observations. An implementation of the FLKS for a two-dimensional linear shallow-water model corroborates the scalar analysis. The numerical experiments also demonstrate the ability of the FLKS to propagate information upstream as well as downstream, thus improving analysis quality substantially in data voids.
    publisherAmerican Meteorological Society
    titleA Fixed-Lag Kalman Smoother for Retrospective Data Assimilation
    typeJournal Paper
    journal volume122
    journal issue12
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1994)122<2838:AFLKSF>2.0.CO;2
    journal fristpage2838
    journal lastpage2867
    treeMonthly Weather Review:;1994:;volume( 122 ):;issue: 012
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian