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    Estimation of Three-Dimensional Error Covariances. Part III: Height–Wind Forecast Error Correlation and Related Geostrophy

    Source: Monthly Weather Review:;2002:;volume( 130 ):;issue: 004::page 1052
    Author:
    Xu, Qin
    ,
    Wei, Li
    DOI: 10.1175/1520-0493(2002)130<1052:EOTDEC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The method of statistical analysis of wind innovation (observation minus forecast) vectors is extended and applied to the innovation data collected over North America for a 3-month period from the Navy Operational Global Atmospheric Prediction System to estimate the height?wind forecast error correlation and to evaluate the related geostrophy. Both single-level and multilevel analyses are performed. The single-level analysis shows that the geostrophy is well satisfied in the middle troposphere but is not well satisfied in the boundary layer and around the tropopause. The multilevel analysis indicates that the cross correlation between height and tangential wind forecast errors at different vertical levels is not small and thus should not be neglected.
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      Estimation of Three-Dimensional Error Covariances. Part III: Height–Wind Forecast Error Correlation and Related Geostrophy

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4204986
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    • Monthly Weather Review

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    contributor authorXu, Qin
    contributor authorWei, Li
    date accessioned2017-06-09T16:14:18Z
    date available2017-06-09T16:14:18Z
    date copyright2002/04/01
    date issued2002
    identifier issn0027-0644
    identifier otherams-63929.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4204986
    description abstractThe method of statistical analysis of wind innovation (observation minus forecast) vectors is extended and applied to the innovation data collected over North America for a 3-month period from the Navy Operational Global Atmospheric Prediction System to estimate the height?wind forecast error correlation and to evaluate the related geostrophy. Both single-level and multilevel analyses are performed. The single-level analysis shows that the geostrophy is well satisfied in the middle troposphere but is not well satisfied in the boundary layer and around the tropopause. The multilevel analysis indicates that the cross correlation between height and tangential wind forecast errors at different vertical levels is not small and thus should not be neglected.
    publisherAmerican Meteorological Society
    titleEstimation of Three-Dimensional Error Covariances. Part III: Height–Wind Forecast Error Correlation and Related Geostrophy
    typeJournal Paper
    journal volume130
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(2002)130<1052:EOTDEC>2.0.CO;2
    journal fristpage1052
    journal lastpage1062
    treeMonthly Weather Review:;2002:;volume( 130 ):;issue: 004
    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