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    Comparison of Finite-Element and Finite-Difference Schemes. Part II: Two-Dimensional Gravity Wave Motion

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004::page 680
    Author:
    Thacker, W. C.
    DOI: 10.1175/1520-0485(1978)008<0680:COFEAF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Irregular grid finite-difference techniques lead to equations similar to those obtained using finite-element techniques. The simpler finite-difference equations offer the advantage of greater computational economy. The time-implicit finite-element equations must be inverted at each time step, and the maximum size of the time step is only half that which can be used with the finite-difference equations. Both techniques result in instabilities when used with highly irregular grids, and the finite-element equations are also unstable if the basin depth is variable. Although the finite-element results are better when compared with finite-difference results from the same grid, comparable finite-difference results can be obtained using a finer grid at less computational expense.
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      Comparison of Finite-Element and Finite-Difference Schemes. Part II: Two-Dimensional Gravity Wave Motion

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    contributor authorThacker, W. C.
    date accessioned2017-06-09T14:44:49Z
    date available2017-06-09T14:44:49Z
    date copyright1978/07/01
    date issued1978
    identifier issn0022-3670
    identifier otherams-25832.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162659
    description abstractIrregular grid finite-difference techniques lead to equations similar to those obtained using finite-element techniques. The simpler finite-difference equations offer the advantage of greater computational economy. The time-implicit finite-element equations must be inverted at each time step, and the maximum size of the time step is only half that which can be used with the finite-difference equations. Both techniques result in instabilities when used with highly irregular grids, and the finite-element equations are also unstable if the basin depth is variable. Although the finite-element results are better when compared with finite-difference results from the same grid, comparable finite-difference results can be obtained using a finer grid at less computational expense.
    publisherAmerican Meteorological Society
    titleComparison of Finite-Element and Finite-Difference Schemes. Part II: Two-Dimensional Gravity Wave Motion
    typeJournal Paper
    journal volume8
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1978)008<0680:COFEAF>2.0.CO;2
    journal fristpage680
    journal lastpage689
    treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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