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    Statistical Corrections to Numerical Predictions. Part IV

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 012::page 2402
    Author:
    Schemm, Jae-Kyung E.
    ,
    Faller, Alan J.
    DOI: 10.1175/1520-0493(1986)114<2402:SCTNPP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The NMC Barotropic-Mesh Model has been used to test a statistical correction procedure, designated as M-II, that was developed in Schemm et al. In the present application, statistical corrections at 12 h resulted in significant reductions of the mean-square errors of both vorticity, ?, and ?2h, where h is the 850?500 mb thickness. Predictions to 48 h demonstrated the feasibility of applying corrections at every 12 h in extended forecasts. In addition to these improvements, however, the statistical corrections resulted in a shift of error from smaller to larger-scale motions, improving the smallest scales dramatically but deteriorating the largest scales. This effect is shown to be a consequence of randomization of the residual errors by the regression equations and can be corrected by spatially high-pass filtering the field of corrections before they are applied.
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    • Statistics

      Statistical Corrections to Numerical Predictions. Part IV

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4201653
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    contributor authorSchemm, Jae-Kyung E.
    contributor authorFaller, Alan J.
    date accessioned2017-06-09T16:06:04Z
    date available2017-06-09T16:06:04Z
    date copyright1986/12/01
    date issued1986
    identifier issn0027-0644
    identifier otherams-60929.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201653
    description abstractThe NMC Barotropic-Mesh Model has been used to test a statistical correction procedure, designated as M-II, that was developed in Schemm et al. In the present application, statistical corrections at 12 h resulted in significant reductions of the mean-square errors of both vorticity, ?, and ?2h, where h is the 850?500 mb thickness. Predictions to 48 h demonstrated the feasibility of applying corrections at every 12 h in extended forecasts. In addition to these improvements, however, the statistical corrections resulted in a shift of error from smaller to larger-scale motions, improving the smallest scales dramatically but deteriorating the largest scales. This effect is shown to be a consequence of randomization of the residual errors by the regression equations and can be corrected by spatially high-pass filtering the field of corrections before they are applied.
    publisherAmerican Meteorological Society
    titleStatistical Corrections to Numerical Predictions. Part IV
    typeJournal Paper
    journal volume114
    journal issue12
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1986)114<2402:SCTNPP>2.0.CO;2
    journal fristpage2402
    journal lastpage2417
    treeMonthly Weather Review:;1986:;volume( 114 ):;issue: 012
    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