mom_pressureforce mom_pressureforce::pressureforce_cs subroutine, public subroutine, public mom_pressureforce::pressureforce (h, tv, PFu, PFv, G, GV, US, CS, ALE_CSp, p_atm, pbce, eta) pressureforce h h tv tv PFu PFu PFv PFv G G GV GV US US CS CS ALE_CSp ALE_CSp p_atm p_atm pbce pbce eta eta A thin layer between the model and the Boussinesq and non-Boussinesq pressure force routines. g The ocean's grid structure gv The ocean's vertical grid structure us A dimensional unit scaling type h Layer thicknesses [H ~> m or kg m-2] tv A structure pointing to various thermodynamic variables pfu Zonal pressure force acceleration [L T-2 ~> m s-2] pfv Meridional pressure force acceleration [L T-2 ~> m s-2] cs Pressure force control structure ale_csp ALE control structure p_atm The pressure at the ice-ocean or pbce The baroclinic pressure anomaly in each layer eta The bottom mass used to calculate PFu and PFv, mom_dynamics_split_rk2::step_mom_dyn_split_rk2 mom_dynamics_unsplit::step_mom_dyn_unsplit mom_dynamics_unsplit_rk2::step_mom_dyn_unsplit_rk2 subroutine, public subroutine, public mom_pressureforce::pressureforce_init (Time, G, GV, US, param_file, diag, CS, tides_CSp) pressureforce_init Time Time G G GV GV US US param_file param_file diag diag CS CS tides_CSp tides_CSp Initialize the pressure force control structure. time Current model time g Ocean grid structure gv Vertical grid structure us A dimensional unit scaling type param_file Parameter file handles diag Diagnostics control structure cs Pressure force control structure tides_csp Tide control structure mom_error_handler::mom_error subroutine, public subroutine, public mom_pressureforce::pressureforce_end (CS) pressureforce_end CS CS Deallocate the pressure force control structure. cs Pressure force control structure A thin wrapper for Boussinesq/non-Boussinesq forms of the pressure force calculation. This thin module provides a branch to two forms of the horizontal accelerations due to pressure gradients. The two options currently available are a Montgomery potential form (used in traditional isopycnal layer models), and the analytic finite volume form.