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    Three-Dimensional Covariance Functions for NOGAPS Data

    Source: Monthly Weather Review:;1999:;volume( 127 ):;issue: 010::page 2293
    Author:
    Franke, Richard
    DOI: 10.1175/1520-0493(1999)127<2293:TDCFFN>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Height innovation data for a 2-month period from NOGAPS was analyzed to obtain height prediction and observation error covariances. Different methods of weighting the data in least squares approximations of the spatial covariance data were investigated using the second-order autoregressive (SOAR) correlation function, both with and without an additive constant (varying with pressure level). Based on the properties of the derived covariance matrices and the SOAR parameters, the SOAR without an additive constant was used for the horizontal approximations. The vertical correlations were fit using a combination of SOAR plus an additive constant and a transformation of the logP coordinate to another coordinate to achieve a best fit. The resulting three-dimensional approximation is partially separable, being the product of the horizontal covariance function (which depends on height) and the vertical correlation function. Figures demonstrating various aspects of the process and the results are given.
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      Three-Dimensional Covariance Functions for NOGAPS Data

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    contributor authorFranke, Richard
    date accessioned2017-06-09T16:12:38Z
    date available2017-06-09T16:12:38Z
    date copyright1999/10/01
    date issued1999
    identifier issn0027-0644
    identifier otherams-63383.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4204380
    description abstractHeight innovation data for a 2-month period from NOGAPS was analyzed to obtain height prediction and observation error covariances. Different methods of weighting the data in least squares approximations of the spatial covariance data were investigated using the second-order autoregressive (SOAR) correlation function, both with and without an additive constant (varying with pressure level). Based on the properties of the derived covariance matrices and the SOAR parameters, the SOAR without an additive constant was used for the horizontal approximations. The vertical correlations were fit using a combination of SOAR plus an additive constant and a transformation of the logP coordinate to another coordinate to achieve a best fit. The resulting three-dimensional approximation is partially separable, being the product of the horizontal covariance function (which depends on height) and the vertical correlation function. Figures demonstrating various aspects of the process and the results are given.
    publisherAmerican Meteorological Society
    titleThree-Dimensional Covariance Functions for NOGAPS Data
    typeJournal Paper
    journal volume127
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1999)127<2293:TDCFFN>2.0.CO;2
    journal fristpage2293
    journal lastpage2308
    treeMonthly Weather Review:;1999:;volume( 127 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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