| contributor author | Thacker, W. C. | |
| date accessioned | 2017-06-09T14:44:49Z | |
| date available | 2017-06-09T14:44:49Z | |
| date copyright | 1978/07/01 | |
| date issued | 1978 | |
| identifier issn | 0022-3670 | |
| identifier other | ams-25832.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162659 | |
| description 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. | |
| publisher | American Meteorological Society | |
| title | Comparison of Finite-Element and Finite-Difference Schemes. Part II: Two-Dimensional Gravity Wave Motion | |
| type | Journal Paper | |
| journal volume | 8 | |
| journal issue | 4 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/1520-0485(1978)008<0680:COFEAF>2.0.CO;2 | |
| journal fristpage | 680 | |
| journal lastpage | 689 | |
| tree | Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004 | |
| contenttype | Fulltext | |