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    NUMERICAL EXPERIMENTS WITH A TWO-DIMENSIONAL HORIZONTAL VARIABLE GRID

    Source: Monthly Weather Review:;1970:;volume( 098 ):;issue: 011::page 810
    Author:
    ANTHES, RICHARD A.
    DOI: 10.1175/1520-0493(1970)098<0810:NEWATD>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: A two-dimensional horizontal variable grid is derived that has maximum resolution at the center and minimum resolution near the boundaries of the grid. By using the analytic transformation that defines the variable grid, the equations of motion for a free-surface model are transformed in terms of new independent space variables in a computational domain with constant resolution. Numerical experiments utilize the variable grid to (1) increase the domain size with a fixed resolution at the center and (2) increase the resolution at the center with a fixed domain size. Several finite-difference analogs and three time-integration schemes are tested. For a given domain size and number of grid points, several variable grid experiments show superior results in the mass and momentum fields compared to constant grid results. Most variable grid experiments, however, show a small (less than 1 percent) increase in total energy after 2000 time steps due apparently to the presence of additional nonlinear terms in the forecast equations. The results show that, although care must be taken with the nonlinear terms, the variable grid may be effectively used in certain physical problems to economically gain resolution at the center of the domain.
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      NUMERICAL EXPERIMENTS WITH A TWO-DIMENSIONAL HORIZONTAL VARIABLE GRID

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4198688
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    • Monthly Weather Review

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    contributor authorANTHES, RICHARD A.
    date accessioned2017-06-09T15:59:27Z
    date available2017-06-09T15:59:27Z
    date copyright1970/11/01
    date issued1970
    identifier issn0027-0644
    identifier otherams-58261.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198688
    description abstractA two-dimensional horizontal variable grid is derived that has maximum resolution at the center and minimum resolution near the boundaries of the grid. By using the analytic transformation that defines the variable grid, the equations of motion for a free-surface model are transformed in terms of new independent space variables in a computational domain with constant resolution. Numerical experiments utilize the variable grid to (1) increase the domain size with a fixed resolution at the center and (2) increase the resolution at the center with a fixed domain size. Several finite-difference analogs and three time-integration schemes are tested. For a given domain size and number of grid points, several variable grid experiments show superior results in the mass and momentum fields compared to constant grid results. Most variable grid experiments, however, show a small (less than 1 percent) increase in total energy after 2000 time steps due apparently to the presence of additional nonlinear terms in the forecast equations. The results show that, although care must be taken with the nonlinear terms, the variable grid may be effectively used in certain physical problems to economically gain resolution at the center of the domain.
    publisherAmerican Meteorological Society
    titleNUMERICAL EXPERIMENTS WITH A TWO-DIMENSIONAL HORIZONTAL VARIABLE GRID
    typeJournal Paper
    journal volume98
    journal issue11
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1970)098<0810:NEWATD>2.3.CO;2
    journal fristpage810
    journal lastpage822
    treeMonthly Weather Review:;1970:;volume( 098 ):;issue: 011
    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
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