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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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