25 |
the planetary ocean circulation. The simulation is configured |
the planetary ocean circulation. The simulation is configured |
26 |
with realistic geography and bathymetry on a |
with realistic geography and bathymetry on a |
27 |
$4^{\circ} \times 4^{\circ}$ spherical polar grid. |
$4^{\circ} \times 4^{\circ}$ spherical polar grid. |
28 |
|
The files for this experiment are in the verification directory |
29 |
|
under tutorial\_global\_oce\_latlon. |
30 |
Twenty levels are used in the vertical, ranging in thickness |
Twenty levels are used in the vertical, ranging in thickness |
31 |
from $50\,{\rm m}$ at the surface to $815\,{\rm m}$ at depth, |
from $50\,{\rm m}$ at the surface to $815\,{\rm m}$ at depth, |
32 |
giving a maximum model depth of $6\,{\rm km}$. |
giving a maximum model depth of $6\,{\rm km}$. |
580 |
\fbox{ |
\fbox{ |
581 |
\begin{minipage}{5.0in} |
\begin{minipage}{5.0in} |
582 |
{\it S/R INI\_PARMS}({\it ini\_parms.F})\\ |
{\it S/R INI\_PARMS}({\it ini\_parms.F})\\ |
583 |
{\it S/R CALC\_MOM\_RHS}({\it calc\_mom\_rhs.F}) |
{\it S/R MOM\_FLUXFORM}({\it mom\_fluxform.F}) |
584 |
\end{minipage} |
\end{minipage} |
585 |
} |
} |
586 |
|
|