| 5 | |
| 6 | Switching on the ocean mode has several effects: |
| 7 | |
| 8 | * An additional prognostic equation for salinity is solved. |
| 9 | * The potential temperature in buoyancy and stability-related terms is replaced by potential density. |
| 10 | * Potential density is calculated from the equation of state for seawater after each time step, using the algorithm proposed by Jackett et al. (2006, J. Atmos. Oceanic Technol., 23, 1709-1728).[[BR]] |
| 11 | So far, only the initial hydrostatic pressure is entered into this equation. |
| 12 | * z=0 (sea surface) is assumed at the model top (vertical grid index k=[wiki:doc/app/initialization_parameters#nzt nzt] on the w-grid), with negative values of z indicating the depth. |
| 13 | * Initial profiles are constructed (e.g. from [wiki:doc/app/initialization_parameters#pt_vertical_gradient pt_vertical_gradient] / [wiki:doc/app/initialization_parameters#pt_vertical_gradient_level pt_vertical_gradient_level]) starting from the sea surface, using surface values given by [wiki:doc/app/initialization_parameters#pt_surface pt_surface], [#sa_surface sa_surface], [wiki:doc/app/initialization_parameters#ug_surface ug_surface], and [wiki:doc/app/initialization_parameters#vg_surface vg_surface]. |
| 14 | * Zero salinity flux is used as default boundary condition at the bottom of the sea. |
| 15 | * If switched on, random perturbations are by default imposed to the upper model domain from zu(nzt*2/3) to zu(nzt-3).\\\\ |
| 16 | Relevant parameters to be exclusively used for steering ocean mode runs are [#bc_sa_t bc_sa_t], [#bottom_salinityflux bottom_salinityflux], [#sa_surface sa_surface], [#sa_vertical_gradient sa_vertical_gradient], [#sa_vertical_gradient_level sa_vertical_gradient_level], and [#top_salinityflux top_salinityflux].\\\\ |
| 17 | |
| 18 | |
| 19 | |