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The effect of horizontal gradients of height-field forecast error variances upon OI forecast error statistics



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    In the formulation of statistical relationships among forecast errors in the optimal interpolation (OI) analysis system at NMC, it is currently assumed that horizontal gradients of the height-field forecast error standard deviation, [sigma]z are negligible. This homogeneity assumption is reasonable only in areas of uniform data density and quality. The dominant feature on the maps of [sigma]z actually produced by the OI system is in fact the rapid change of [sigma]z near boundaries between data-dense and data-sparse regions. In this note we rederive the statistical relationships among forecast errors, without assuming that the [sigma]z field is homogeneous. The resulting forecast error statistics are compared with the conventional ones, using realistic [sigma]z fields. The comparison shows that the wind-field forecast error standard deviations are increased over the entire globe, and by as much as about 30% in some regions. The wind-height and wind-wind forecast error correlations are changed even more dramatically. For example, the correlation between height and zonal wind forecast errors at a point is 0.0 if [sigma]z is constant there, but becomes as large as about °0.6 at points where [sigma]z is changing rapidly. More generally, the wind-height and wind-wind forecast error correlations lose the homogeneity and isotropy properties they possess in conventional OI formulations, in a manner reflecting the variability of data density and quality encountered over the globe.
  • Content Notes:
    Stephen E. Cohn and Lauren L. Morone.

    "October 1984."

    "This is an unreviewed manuscript, primarily intended for informal exchange of information among NMC staff members."

    System requirements: Adobe Acrobat Reader.

    Includes bibliographical references (page 26).

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    Public Domain
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    Library
  • Main Document Checksum:
    urn:sha256:7c3c10db382c25583ea5c2d39e2cbe6cf6d33505b627b9fc2cad59360b034321
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    Filetype[PDF - 1.49 MB ]
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