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    THE OVER-RELAXATION FACTOR IN THE NUMERICAL SOLUTION OF THE OMEGA EQUATION

    Source: Monthly Weather Review:;1967:;volume( 095 ):;issue: 005::page 303
    Author:
    STUART, DAVID W.
    ,
    O'NEILL, THOMAS H. R.
    DOI: 10.1175/1520-0493(1967)095<0303:TORFIT>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: Results of tests for the optimum over-relaxation coefficients in the numerical relaxation of the omega equation are presented. One case considers a strong upper-level development for tests on a fixed grid using one-, two-, and three-dimensional forms of the omega equation. In the other case of a ?classical storm? the omega equation is relaxed in its three-dimensional form using several different horizontal grids. For the one- and two-dimensional tests, the relaxation scheme agreesv ery well with theory. In the three-dimensional tests, the observed over-relaxation coefficients are found to be less than the values given by the theory for all grid sizes considered. A sharp cut-off is found to occur shortly after the optimum over-relaxation value is reached regardless of the number of dimensions of the equation or the size of the grid.
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      THE OVER-RELAXATION FACTOR IN THE NUMERICAL SOLUTION OF THE OMEGA EQUATION

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4198223
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    contributor authorSTUART, DAVID W.
    contributor authorO'NEILL, THOMAS H. R.
    date accessioned2017-06-09T15:58:21Z
    date available2017-06-09T15:58:21Z
    date copyright1967/05/01
    date issued1967
    identifier issn0027-0644
    identifier otherams-57842.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198223
    description abstractResults of tests for the optimum over-relaxation coefficients in the numerical relaxation of the omega equation are presented. One case considers a strong upper-level development for tests on a fixed grid using one-, two-, and three-dimensional forms of the omega equation. In the other case of a ?classical storm? the omega equation is relaxed in its three-dimensional form using several different horizontal grids. For the one- and two-dimensional tests, the relaxation scheme agreesv ery well with theory. In the three-dimensional tests, the observed over-relaxation coefficients are found to be less than the values given by the theory for all grid sizes considered. A sharp cut-off is found to occur shortly after the optimum over-relaxation value is reached regardless of the number of dimensions of the equation or the size of the grid.
    publisherAmerican Meteorological Society
    titleTHE OVER-RELAXATION FACTOR IN THE NUMERICAL SOLUTION OF THE OMEGA EQUATION
    typeJournal Paper
    journal volume95
    journal issue5
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1967)095<0303:TORFIT>2.3.CO;2
    journal fristpage303
    journal lastpage307
    treeMonthly Weather Review:;1967:;volume( 095 ):;issue: 005
    contenttypeFulltext
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