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    Filter Transfer Functions for the Method of Successive Corrections

    Source: Monthly Weather Review:;2002:;volume( 130 ):;issue: 002::page 372
    Author:
    Schlax, Michael G.
    ,
    Chelton, Dudley B.
    DOI: 10.1175/1520-0493(2002)130<0372:FTFFTM>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The frequency-domain characteristics of the successive corrections method in one dimension are investigated through the calculation of smoother weights and filter transfer functions. The successive corrections algorithm acts as a low-pass filter that behaves similarly to noniterative smoothers. The spectral content of fixed-span successive corrections estimates depends upon the number of iterations, the selected weighting function and the grid to which the dataset is interpolated. For a given weighting function and grid, increasing the number of iterations for the fixed-span case results in filter transfer functions with increased cutoff frequency and rolloff. Within data gaps, the use of more than one iteration leads to estimates that are more likely to be contaminated by high-frequency variability in the data. It is shown that variable-span successive corrections estimates are nearly independent of the choice of weights for the initial iterations and are almost equivalent to estimates obtained using a single iteration. The greater computational requirements of multiple-iteration successive corrections is a disadvantage for general applications.
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      Filter Transfer Functions for the Method of Successive Corrections

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4204939
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    contributor authorSchlax, Michael G.
    contributor authorChelton, Dudley B.
    date accessioned2017-06-09T16:14:11Z
    date available2017-06-09T16:14:11Z
    date copyright2002/02/01
    date issued2002
    identifier issn0027-0644
    identifier otherams-63887.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4204939
    description abstractThe frequency-domain characteristics of the successive corrections method in one dimension are investigated through the calculation of smoother weights and filter transfer functions. The successive corrections algorithm acts as a low-pass filter that behaves similarly to noniterative smoothers. The spectral content of fixed-span successive corrections estimates depends upon the number of iterations, the selected weighting function and the grid to which the dataset is interpolated. For a given weighting function and grid, increasing the number of iterations for the fixed-span case results in filter transfer functions with increased cutoff frequency and rolloff. Within data gaps, the use of more than one iteration leads to estimates that are more likely to be contaminated by high-frequency variability in the data. It is shown that variable-span successive corrections estimates are nearly independent of the choice of weights for the initial iterations and are almost equivalent to estimates obtained using a single iteration. The greater computational requirements of multiple-iteration successive corrections is a disadvantage for general applications.
    publisherAmerican Meteorological Society
    titleFilter Transfer Functions for the Method of Successive Corrections
    typeJournal Paper
    journal volume130
    journal issue2
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(2002)130<0372:FTFFTM>2.0.CO;2
    journal fristpage372
    journal lastpage385
    treeMonthly Weather Review:;2002:;volume( 130 ):;issue: 002
    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