Variables var_hom and var_sum are both renamed pr_palm.data_output_profiles, flow_statistics, init_3d_model, modules, parin, pres, read_var_list, run_control, time_integration EBugfix: work_fft*_vec removed from some PRIVATE-declarations (poisfft).

Bugfix: field_chr renamed field_char (user_interface).

Bugfix: output of use_upstream_for_tke (header).header, poisfft, user_interface21/06/07SR3.3NThis version allows runs for the ocean. Ocean runs can be switched on with the ne inipar-parameter ocean.

Setting this switch has several effects:

- An additional prognostic equation for salinity is solved.
- Potential temperature in buoyancy and stability-related terms is replaced by potential density.
- Potential
+instead of using a seperate loop.

Variables var_hom and var_sum are both renamed pr_palm.data_output_profiles, flow_statistics, init_3d_model, modules, parin, pres, read_var_list, run_control, time_integration EBugfix: work_fft*_vec removed from some PRIVATE-declarations (poisfft).

Bugfix: field_chr renamed field_char (user_interface).

Bugfix: output of use_upstream_for_tke (header).header, poisfft, user_interface21/06/07SR3.3NThis version allows runs for the ocean. These runs can be switched on with the new inipar-parameter ocean.

Setting this switch has several effects:- An additional prognostic equation for salinity is solved.
- Potential temperature in buoyancy and stability-related terms is replaced by potential density.
- Potential
density is calculated from the equation of state for seawater after
each timestep, using the algorithm proposed by Jackett et al. (2006, J.
-Atmos. Oceanic Technol., 23, 1709-1728).

So far, only the initial hydrostatic pressure is entered into this equation. - z=0 (sea surface) is assumed at the model top (vertical grid index k=nzt on the w-grid), with negative values of z indicating the depth.
- Initial profiles are constructed (e.g. from pt_vertical_gradient / pt_vertical_gradient_level) starting from the sea surface, using surface values given by pt_surface, sa_surface, ug_surface, and vg_surface.
- Zero salinity flux is used as default boundary condition at the bottom of the sea.
- If switched on, random perturbations are by default imposed to the upper model domain from zu(nzt*2/3) to zu(nzt-3).

Salinity (sa) and potential density (rho) are included as new 2d/3d output quantities. Vertical profiles of salinity (sa), salinity fluxes (w"sa", w*sa*, wsa), and potential density (rho) can also be output.advec_s_bc, -average_3d_data, boundary_conds, buoyancy, check_parameters, -data_output_2d, data_output_3d, diffusion_e, flow_statistics, header, -init_grid, init_3d_model, modules, netcdf, parin, production_e, -prognostic_equations, read_var_list, sum_up_3d_data, swap_timelevel, -time_integration, user_interface, write_var_list, write_3d_binary

new:

eqn_state_seawater, init_ocean CInipar-parameter use_pt_reference renamed use_reference.

Internal variable hydro_press renamed hyp, routine calc_mean_pt_profile renamed calc_mean_profile.

The format of the RUN_CONTROL file has been adjusted for ocean runs.advec_particles, -buoyancy, calc_liquid_water_content, check_parameters, diffusion_e, -diffusivities, header, init_cloud_physics, modules, production_e, -prognostic_equations, run_control E +Atmos. Oceanic Technol., 23, 1709-1728).

So far, only the initial hydrostatic pressure is entered into this equation. - z=0 (sea surface) is assumed at the model top (vertical grid index k=nzt on the w-grid), with negative values of z indicating the depth.
- Initial profiles are constructed (e.g. from pt_vertical_gradient / pt_vertical_gradient_level) starting from the sea surface, using surface values given by pt_surface, sa_surface, ug_surface, and vg_surface.
- Zero salinity flux is used as default boundary condition at the bottom of the sea.
- If switched on, random perturbations are by default imposed to the upper model domain from zu(nzt*2/3) to zu(nzt-3).

Salinity (sa) and potential density (rho) are included as new 2d/3d output quantities. Vertical profiles of salinity (sa), salinity fluxes (w"sa", w*sa*, wsa), and potential density (rho) can also be output.advec_s_bc, average_3d_data,

boundary_conds, buoyancy,

check_parameters, data_output_2d,

data_output_3d, diffusion_e,

diffusivities, flow_statistics, header,

init_grid, init_3d_model, modules,

netcdf, parin, production_e,

prognostic_equations,

read_3d_binary, read_var_list,

sum_up_3d_data, swap_timelevel,

time_integration, user_interface,

write_var_list, write_3d_binary

new:

eqn_state_seawater, init_ocean CInipar-parameter use_pt_reference renamed use_reference.

Internal variable hydro_press renamed hyp, routine calc_mean_pt_profile renamed calc_mean_profile.

The format of the RUN_CONTROL file has been adjusted for ocean runs.

Defaults of .._vertical_gradient_levels changed from -1.0 to -9999999.9.advec_particles, buoyancy,

calc_liquid_water_content,

check_parameters, diffusion_e,

diffusivities, header,

init_cloud_physics, modules,

production_e, prognostic_equations,

run_control EBugfix: height above topography instead of height above level k=0 is used for calculating the mixing length (diffusion_e and diffusivities).

Bugfix: error in boundary condition for TKE removed (advec_s_bc).advec_s_bc, diffusion_e, diffusivities