| 13 | |---------------- |
| 14 | {{{#!td style="vertical-align:top;width: 50px" |
| 15 | 23/12/10 |
| 16 | }}} |
| 17 | {{{#!td style="vertical-align:top;width: 50px" |
| 18 | MS / MG |
| 19 | }}} |
| 20 | {{{#!td style="vertical-align:top;width: 75px" |
| 21 | r667 |
| 22 | }}} |
| 23 | {{{#!td style="vertical-align:top" |
| 24 | 3.7a |
| 25 | }}} |
| 26 | {{{#!td style="vertical-align:top" |
| 27 | N |
| 28 | }}} |
| 29 | {{{#!td style="vertical-align:top" |
| 30 | New advection scheme added ( Wicker and Skamarock 5th order ) (advec_ws.f90) |
| 31 | Please note the further information in [../../app/inipar/#momentum_advec inipar] . |
| 32 | |
| 33 | Changes in coupling: Different number of processors and different horizontal resolution in ocean and atmosphere is now allowed. |
| 34 | Furthermore u and v from the ocean surface is now used as bottom boundary for the atmosphere. |
| 35 | |
| 36 | Bottom boundary conditions for u and v changed from mirror to dirichlet boundary conditions. |
| 37 | |
| 38 | Detailed information will follow at beginning of January 2011. |
| 39 | |
| 40 | |
| 41 | }}} |