404 | | coupling mode "...: ny+1 in ocean is not divisible without remainder with ny+1 in atmosphere |
405 | | }}} |
406 | | {{{#!td |
407 | | For the coupling between atmosphere and ocean, a smaller grid length in the y-direction can be chosen for the ocean, so that the ocean has more grid points in the y-direction then the atmosphere. In this case, the information must be interpolated for the data exchange between atmosphere and ocean. Therefor it must be ensured that each interpolation interval has the same number of gridpoints. This is ensured if the following equation is fulfilled: |
| 404 | coupling mode "...": ny+1 in ocean is not divisible by ny+1 in atmosphere without remainder |
| 405 | }}} |
| 406 | {{{#!td |
| 407 | For coupling of atmosphere and ocean, a smaller grid length in the y-direction can be chosen for the ocean, so that the ocean has more grid points in the y-direction than the atmosphere. In this case, the information must be interpolated for the data exchange between atmosphere and ocean. It must therefore be ensured that each interpolation interval has the same number of gridpoints. This is ensured if the following holds: |