[1] | 1 | MODULE prognostic_equations_mod |
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| 2 | |
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| 3 | !------------------------------------------------------------------------------! |
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[484] | 4 | ! Current revisions: |
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[1] | 5 | ! ----------------- |
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[531] | 6 | ! add call of subsidence in the equation for humidity / passive scalar |
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[98] | 7 | ! |
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| 8 | ! Former revisions: |
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| 9 | ! ----------------- |
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| 10 | ! $Id: prognostic_equations.f90 531 2010-04-21 06:47:21Z heinze $ |
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| 11 | ! |
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[482] | 12 | ! 411 2009-12-11 14:15:58Z heinze |
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| 13 | ! add call of subsidence in the equation for potential temperature |
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| 14 | ! |
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[392] | 15 | ! 388 2009-09-23 09:40:33Z raasch |
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| 16 | ! prho is used instead of rho in diffusion_e, |
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| 17 | ! external pressure gradient |
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| 18 | ! |
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[198] | 19 | ! 153 2008-03-19 09:41:30Z steinfeld |
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| 20 | ! add call of plant_canopy_model in the prognostic equation for |
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| 21 | ! the potential temperature and for the passive scalar |
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| 22 | ! |
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[139] | 23 | ! 138 2007-11-28 10:03:58Z letzel |
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| 24 | ! add call of subroutines that evaluate the canopy drag terms, |
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| 25 | ! add wall_*flux to parameter list of calls of diffusion_s |
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| 26 | ! |
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[110] | 27 | ! 106 2007-08-16 14:30:26Z raasch |
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| 28 | ! +uswst, vswst as arguments in calls of diffusion_u|v, |
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| 29 | ! loops for u and v are starting from index nxlu, nysv, respectively (needed |
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| 30 | ! for non-cyclic boundary conditions) |
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| 31 | ! |
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[98] | 32 | ! 97 2007-06-21 08:23:15Z raasch |
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[96] | 33 | ! prognostic equation for salinity, density is calculated from equation of |
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[97] | 34 | ! state for seawater and is used for calculation of buoyancy, |
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| 35 | ! +eqn_state_seawater_mod |
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| 36 | ! diffusion_e is called with argument rho in case of ocean runs, |
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| 37 | ! new argument zw in calls of diffusion_e, new argument pt_/prho_reference |
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| 38 | ! in calls of buoyancy and diffusion_e, calc_mean_pt_profile renamed |
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[96] | 39 | ! calc_mean_profile |
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[1] | 40 | ! |
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[77] | 41 | ! 75 2007-03-22 09:54:05Z raasch |
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| 42 | ! checking for negative q and limiting for positive values, |
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| 43 | ! z0 removed from arguments in calls of diffusion_u/v/w, uxrp, vynp eliminated, |
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| 44 | ! subroutine names changed to .._noopt, .._cache, and .._vector, |
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| 45 | ! moisture renamed humidity, Bott-Chlond-scheme can be used in the |
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| 46 | ! _vector-version |
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| 47 | ! |
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[39] | 48 | ! 19 2007-02-23 04:53:48Z raasch |
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| 49 | ! Calculation of e, q, and pt extended for gridpoint nzt, |
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| 50 | ! handling of given temperature/humidity/scalar fluxes at top surface |
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| 51 | ! |
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[3] | 52 | ! RCS Log replace by Id keyword, revision history cleaned up |
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| 53 | ! |
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[1] | 54 | ! Revision 1.21 2006/08/04 15:01:07 raasch |
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| 55 | ! upstream scheme can be forced to be used for tke (use_upstream_for_tke) |
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| 56 | ! regardless of the timestep scheme used for the other quantities, |
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| 57 | ! new argument diss in call of diffusion_e |
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| 58 | ! |
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| 59 | ! Revision 1.1 2000/04/13 14:56:27 schroeter |
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| 60 | ! Initial revision |
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| 61 | ! |
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| 62 | ! |
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| 63 | ! Description: |
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| 64 | ! ------------ |
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[19] | 65 | ! Solving the prognostic equations. |
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[1] | 66 | !------------------------------------------------------------------------------! |
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| 67 | |
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| 68 | USE arrays_3d |
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| 69 | USE control_parameters |
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| 70 | USE cpulog |
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[96] | 71 | USE eqn_state_seawater_mod |
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[1] | 72 | USE grid_variables |
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| 73 | USE indices |
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| 74 | USE interfaces |
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| 75 | USE pegrid |
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| 76 | USE pointer_interfaces |
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| 77 | USE statistics |
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| 78 | |
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| 79 | USE advec_s_pw_mod |
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| 80 | USE advec_s_up_mod |
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| 81 | USE advec_u_pw_mod |
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| 82 | USE advec_u_up_mod |
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| 83 | USE advec_v_pw_mod |
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| 84 | USE advec_v_up_mod |
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| 85 | USE advec_w_pw_mod |
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| 86 | USE advec_w_up_mod |
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| 87 | USE buoyancy_mod |
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| 88 | USE calc_precipitation_mod |
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| 89 | USE calc_radiation_mod |
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| 90 | USE coriolis_mod |
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| 91 | USE diffusion_e_mod |
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| 92 | USE diffusion_s_mod |
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| 93 | USE diffusion_u_mod |
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| 94 | USE diffusion_v_mod |
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| 95 | USE diffusion_w_mod |
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| 96 | USE impact_of_latent_heat_mod |
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[138] | 97 | USE plant_canopy_model_mod |
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[1] | 98 | USE production_e_mod |
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[411] | 99 | USE subsidence_mod |
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[1] | 100 | USE user_actions_mod |
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| 101 | |
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| 102 | |
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| 103 | PRIVATE |
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[63] | 104 | PUBLIC prognostic_equations_noopt, prognostic_equations_cache, & |
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| 105 | prognostic_equations_vector |
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[1] | 106 | |
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[63] | 107 | INTERFACE prognostic_equations_noopt |
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| 108 | MODULE PROCEDURE prognostic_equations_noopt |
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| 109 | END INTERFACE prognostic_equations_noopt |
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[1] | 110 | |
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[63] | 111 | INTERFACE prognostic_equations_cache |
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| 112 | MODULE PROCEDURE prognostic_equations_cache |
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| 113 | END INTERFACE prognostic_equations_cache |
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[1] | 114 | |
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[63] | 115 | INTERFACE prognostic_equations_vector |
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| 116 | MODULE PROCEDURE prognostic_equations_vector |
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| 117 | END INTERFACE prognostic_equations_vector |
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[1] | 118 | |
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| 119 | |
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| 120 | CONTAINS |
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| 121 | |
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| 122 | |
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[63] | 123 | SUBROUTINE prognostic_equations_noopt |
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[1] | 124 | |
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| 125 | !------------------------------------------------------------------------------! |
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| 126 | ! Version with single loop optimization |
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| 127 | ! |
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| 128 | ! (Optimized over each single prognostic equation.) |
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| 129 | !------------------------------------------------------------------------------! |
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| 130 | |
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| 131 | IMPLICIT NONE |
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| 132 | |
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| 133 | CHARACTER (LEN=9) :: time_to_string |
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| 134 | INTEGER :: i, j, k |
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| 135 | REAL :: sat, sbt |
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| 136 | |
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| 137 | ! |
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| 138 | !-- Calculate those variables needed in the tendency terms which need |
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| 139 | !-- global communication |
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[96] | 140 | CALL calc_mean_profile( pt, 4 ) |
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| 141 | IF ( ocean ) CALL calc_mean_profile( rho, 64 ) |
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| 142 | IF ( humidity ) CALL calc_mean_profile( vpt, 44 ) |
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[1] | 143 | |
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| 144 | ! |
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| 145 | !-- u-velocity component |
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| 146 | CALL cpu_log( log_point(5), 'u-equation', 'start' ) |
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| 147 | |
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| 148 | ! |
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| 149 | !-- u-tendency terms with communication |
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| 150 | IF ( momentum_advec == 'ups-scheme' ) THEN |
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| 151 | tend = 0.0 |
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| 152 | CALL advec_u_ups |
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| 153 | ENDIF |
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| 154 | |
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| 155 | ! |
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| 156 | !-- u-tendency terms with no communication |
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[106] | 157 | DO i = nxlu, nxr |
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[1] | 158 | DO j = nys, nyn |
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| 159 | ! |
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| 160 | !-- Tendency terms |
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| 161 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
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| 162 | tend(:,j,i) = 0.0 |
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| 163 | CALL advec_u_pw( i, j ) |
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| 164 | ELSE |
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| 165 | IF ( momentum_advec /= 'ups-scheme' ) THEN |
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| 166 | tend(:,j,i) = 0.0 |
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| 167 | CALL advec_u_up( i, j ) |
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| 168 | ENDIF |
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| 169 | ENDIF |
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| 170 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
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| 171 | CALL diffusion_u( i, j, ddzu, ddzw, km_m, km_damp_y, tend, u_m, & |
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[102] | 172 | usws_m, uswst_m, v_m, w_m ) |
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[1] | 173 | ELSE |
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| 174 | CALL diffusion_u( i, j, ddzu, ddzw, km, km_damp_y, tend, u, usws, & |
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[102] | 175 | uswst, v, w ) |
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[1] | 176 | ENDIF |
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| 177 | CALL coriolis( i, j, 1 ) |
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[97] | 178 | IF ( sloping_surface ) CALL buoyancy( i, j, pt, pt_reference, 1, 4 ) |
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[138] | 179 | |
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| 180 | ! |
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| 181 | !-- Drag by plant canopy |
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| 182 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 1 ) |
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[240] | 183 | |
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| 184 | ! |
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| 185 | !-- External pressure gradient |
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| 186 | IF ( dp_external ) THEN |
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| 187 | DO k = dp_level_ind_b+1, nzt |
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| 188 | tend(k,j,i) = tend(k,j,i) - dpdxy(1) * dp_smooth_factor(k) |
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| 189 | ENDDO |
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| 190 | ENDIF |
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| 191 | |
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[1] | 192 | CALL user_actions( i, j, 'u-tendency' ) |
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| 193 | |
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| 194 | ! |
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| 195 | !-- Prognostic equation for u-velocity component |
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| 196 | DO k = nzb_u_inner(j,i)+1, nzt |
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| 197 | u_p(k,j,i) = ( 1.0-tsc(1) ) * u_m(k,j,i) + tsc(1) * u(k,j,i) + & |
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| 198 | dt_3d * ( & |
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| 199 | tsc(2) * tend(k,j,i) + tsc(3) * tu_m(k,j,i) & |
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| 200 | - tsc(4) * ( p(k,j,i) - p(k,j,i-1) ) * ddx & |
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| 201 | ) - & |
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| 202 | tsc(5) * rdf(k) * ( u(k,j,i) - ug(k) ) |
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| 203 | ENDDO |
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| 204 | |
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| 205 | ! |
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| 206 | !-- Calculate tendencies for the next Runge-Kutta step |
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| 207 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
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| 208 | IF ( intermediate_timestep_count == 1 ) THEN |
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| 209 | DO k = nzb_u_inner(j,i)+1, nzt |
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| 210 | tu_m(k,j,i) = tend(k,j,i) |
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| 211 | ENDDO |
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| 212 | ELSEIF ( intermediate_timestep_count < & |
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| 213 | intermediate_timestep_count_max ) THEN |
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| 214 | DO k = nzb_u_inner(j,i)+1, nzt |
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| 215 | tu_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tu_m(k,j,i) |
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| 216 | ENDDO |
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| 217 | ENDIF |
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| 218 | ENDIF |
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| 219 | |
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| 220 | ENDDO |
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| 221 | ENDDO |
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| 222 | |
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| 223 | CALL cpu_log( log_point(5), 'u-equation', 'stop' ) |
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| 224 | |
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| 225 | ! |
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| 226 | !-- v-velocity component |
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| 227 | CALL cpu_log( log_point(6), 'v-equation', 'start' ) |
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| 228 | |
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| 229 | ! |
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| 230 | !-- v-tendency terms with communication |
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| 231 | IF ( momentum_advec == 'ups-scheme' ) THEN |
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| 232 | tend = 0.0 |
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| 233 | CALL advec_v_ups |
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| 234 | ENDIF |
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| 235 | |
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| 236 | ! |
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| 237 | !-- v-tendency terms with no communication |
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| 238 | DO i = nxl, nxr |
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[106] | 239 | DO j = nysv, nyn |
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[1] | 240 | ! |
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| 241 | !-- Tendency terms |
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| 242 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
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| 243 | tend(:,j,i) = 0.0 |
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| 244 | CALL advec_v_pw( i, j ) |
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| 245 | ELSE |
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| 246 | IF ( momentum_advec /= 'ups-scheme' ) THEN |
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| 247 | tend(:,j,i) = 0.0 |
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| 248 | CALL advec_v_up( i, j ) |
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| 249 | ENDIF |
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| 250 | ENDIF |
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| 251 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
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| 252 | CALL diffusion_v( i, j, ddzu, ddzw, km_m, km_damp_x, tend, u_m, & |
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[102] | 253 | v_m, vsws_m, vswst_m, w_m ) |
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[1] | 254 | ELSE |
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| 255 | CALL diffusion_v( i, j, ddzu, ddzw, km, km_damp_x, tend, u, v, & |
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[102] | 256 | vsws, vswst, w ) |
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[1] | 257 | ENDIF |
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| 258 | CALL coriolis( i, j, 2 ) |
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[138] | 259 | |
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| 260 | ! |
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| 261 | !-- Drag by plant canopy |
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| 262 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 2 ) |
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| 263 | |
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[240] | 264 | ! |
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| 265 | !-- External pressure gradient |
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| 266 | IF ( dp_external ) THEN |
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| 267 | DO k = dp_level_ind_b+1, nzt |
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| 268 | tend(k,j,i) = tend(k,j,i) - dpdxy(2) * dp_smooth_factor(k) |
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| 269 | ENDDO |
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| 270 | ENDIF |
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| 271 | |
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[1] | 272 | CALL user_actions( i, j, 'v-tendency' ) |
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| 273 | |
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| 274 | ! |
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| 275 | !-- Prognostic equation for v-velocity component |
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| 276 | DO k = nzb_v_inner(j,i)+1, nzt |
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| 277 | v_p(k,j,i) = ( 1.0-tsc(1) ) * v_m(k,j,i) + tsc(1) * v(k,j,i) + & |
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| 278 | dt_3d * ( & |
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| 279 | tsc(2) * tend(k,j,i) + tsc(3) * tv_m(k,j,i) & |
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| 280 | - tsc(4) * ( p(k,j,i) - p(k,j-1,i) ) * ddy & |
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| 281 | ) - & |
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| 282 | tsc(5) * rdf(k) * ( v(k,j,i) - vg(k) ) |
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| 283 | ENDDO |
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| 284 | |
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| 285 | ! |
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| 286 | !-- Calculate tendencies for the next Runge-Kutta step |
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| 287 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
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| 288 | IF ( intermediate_timestep_count == 1 ) THEN |
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| 289 | DO k = nzb_v_inner(j,i)+1, nzt |
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| 290 | tv_m(k,j,i) = tend(k,j,i) |
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| 291 | ENDDO |
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| 292 | ELSEIF ( intermediate_timestep_count < & |
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| 293 | intermediate_timestep_count_max ) THEN |
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| 294 | DO k = nzb_v_inner(j,i)+1, nzt |
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| 295 | tv_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tv_m(k,j,i) |
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| 296 | ENDDO |
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| 297 | ENDIF |
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| 298 | ENDIF |
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| 299 | |
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| 300 | ENDDO |
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| 301 | ENDDO |
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| 302 | |
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| 303 | CALL cpu_log( log_point(6), 'v-equation', 'stop' ) |
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| 304 | |
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| 305 | ! |
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| 306 | !-- w-velocity component |
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| 307 | CALL cpu_log( log_point(7), 'w-equation', 'start' ) |
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| 308 | |
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| 309 | ! |
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| 310 | !-- w-tendency terms with communication |
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| 311 | IF ( momentum_advec == 'ups-scheme' ) THEN |
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| 312 | tend = 0.0 |
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| 313 | CALL advec_w_ups |
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| 314 | ENDIF |
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| 315 | |
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| 316 | ! |
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| 317 | !-- w-tendency terms with no communication |
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| 318 | DO i = nxl, nxr |
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| 319 | DO j = nys, nyn |
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| 320 | ! |
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| 321 | !-- Tendency terms |
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| 322 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
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| 323 | tend(:,j,i) = 0.0 |
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| 324 | CALL advec_w_pw( i, j ) |
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| 325 | ELSE |
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| 326 | IF ( momentum_advec /= 'ups-scheme' ) THEN |
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| 327 | tend(:,j,i) = 0.0 |
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| 328 | CALL advec_w_up( i, j ) |
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| 329 | ENDIF |
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| 330 | ENDIF |
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| 331 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
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| 332 | CALL diffusion_w( i, j, ddzu, ddzw, km_m, km_damp_x, km_damp_y, & |
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[57] | 333 | tend, u_m, v_m, w_m ) |
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[1] | 334 | ELSE |
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| 335 | CALL diffusion_w( i, j, ddzu, ddzw, km, km_damp_x, km_damp_y, & |
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[57] | 336 | tend, u, v, w ) |
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[1] | 337 | ENDIF |
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| 338 | CALL coriolis( i, j, 3 ) |
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[97] | 339 | IF ( ocean ) THEN |
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[388] | 340 | CALL buoyancy( i, j, rho, rho_reference, 3, 64 ) |
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[1] | 341 | ELSE |
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[97] | 342 | IF ( .NOT. humidity ) THEN |
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| 343 | CALL buoyancy( i, j, pt, pt_reference, 3, 4 ) |
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| 344 | ELSE |
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| 345 | CALL buoyancy( i, j, vpt, pt_reference, 3, 44 ) |
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| 346 | ENDIF |
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[1] | 347 | ENDIF |
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[138] | 348 | |
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| 349 | ! |
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| 350 | !-- Drag by plant canopy |
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| 351 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 3 ) |
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| 352 | |
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[1] | 353 | CALL user_actions( i, j, 'w-tendency' ) |
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| 354 | |
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| 355 | ! |
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| 356 | !-- Prognostic equation for w-velocity component |
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| 357 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
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| 358 | w_p(k,j,i) = ( 1.0-tsc(1) ) * w_m(k,j,i) + tsc(1) * w(k,j,i) + & |
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| 359 | dt_3d * ( & |
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| 360 | tsc(2) * tend(k,j,i) + tsc(3) * tw_m(k,j,i) & |
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| 361 | - tsc(4) * ( p(k+1,j,i) - p(k,j,i) ) * ddzu(k+1) & |
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| 362 | ) - & |
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| 363 | tsc(5) * rdf(k) * w(k,j,i) |
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| 364 | ENDDO |
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| 365 | |
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| 366 | ! |
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| 367 | !-- Calculate tendencies for the next Runge-Kutta step |
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| 368 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
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| 369 | IF ( intermediate_timestep_count == 1 ) THEN |
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| 370 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
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| 371 | tw_m(k,j,i) = tend(k,j,i) |
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| 372 | ENDDO |
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| 373 | ELSEIF ( intermediate_timestep_count < & |
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| 374 | intermediate_timestep_count_max ) THEN |
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| 375 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
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| 376 | tw_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tw_m(k,j,i) |
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| 377 | ENDDO |
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| 378 | ENDIF |
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| 379 | ENDIF |
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| 380 | |
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| 381 | ENDDO |
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| 382 | ENDDO |
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| 383 | |
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| 384 | CALL cpu_log( log_point(7), 'w-equation', 'stop' ) |
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| 385 | |
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| 386 | ! |
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| 387 | !-- potential temperature |
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| 388 | CALL cpu_log( log_point(13), 'pt-equation', 'start' ) |
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| 389 | |
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| 390 | ! |
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| 391 | !-- pt-tendency terms with communication |
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[70] | 392 | sat = tsc(1) |
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| 393 | sbt = tsc(2) |
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[1] | 394 | IF ( scalar_advec == 'bc-scheme' ) THEN |
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[70] | 395 | |
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| 396 | IF ( timestep_scheme(1:5) /= 'runge' ) THEN |
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[1] | 397 | ! |
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[70] | 398 | !-- Bott-Chlond scheme always uses Euler time step when leapfrog is |
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| 399 | !-- switched on. Thus: |
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| 400 | sat = 1.0 |
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| 401 | sbt = 1.0 |
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| 402 | ENDIF |
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[1] | 403 | tend = 0.0 |
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| 404 | CALL advec_s_bc( pt, 'pt' ) |
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| 405 | ELSE |
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| 406 | IF ( tsc(2) /= 2.0 .AND. scalar_advec == 'ups-scheme' ) THEN |
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| 407 | tend = 0.0 |
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| 408 | CALL advec_s_ups( pt, 'pt' ) |
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| 409 | ENDIF |
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| 410 | ENDIF |
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[407] | 411 | |
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[1] | 412 | ! |
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| 413 | !-- pt-tendency terms with no communication |
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| 414 | DO i = nxl, nxr |
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| 415 | DO j = nys, nyn |
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| 416 | ! |
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| 417 | !-- Tendency terms |
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| 418 | IF ( scalar_advec == 'bc-scheme' ) THEN |
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[129] | 419 | CALL diffusion_s( i, j, ddzu, ddzw, kh, pt, shf, tswst, & |
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| 420 | wall_heatflux, tend ) |
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[1] | 421 | ELSE |
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| 422 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
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| 423 | tend(:,j,i) = 0.0 |
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| 424 | CALL advec_s_pw( i, j, pt ) |
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| 425 | ELSE |
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| 426 | IF ( scalar_advec /= 'ups-scheme' ) THEN |
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| 427 | tend(:,j,i) = 0.0 |
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| 428 | CALL advec_s_up( i, j, pt ) |
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| 429 | ENDIF |
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| 430 | ENDIF |
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| 431 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) & |
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| 432 | THEN |
---|
[19] | 433 | CALL diffusion_s( i, j, ddzu, ddzw, kh_m, pt_m, shf_m, & |
---|
[129] | 434 | tswst_m, wall_heatflux, tend ) |
---|
[1] | 435 | ELSE |
---|
[129] | 436 | CALL diffusion_s( i, j, ddzu, ddzw, kh, pt, shf, tswst, & |
---|
| 437 | wall_heatflux, tend ) |
---|
[1] | 438 | ENDIF |
---|
| 439 | ENDIF |
---|
| 440 | |
---|
| 441 | ! |
---|
| 442 | !-- If required compute heating/cooling due to long wave radiation |
---|
| 443 | !-- processes |
---|
| 444 | IF ( radiation ) THEN |
---|
| 445 | CALL calc_radiation( i, j ) |
---|
| 446 | ENDIF |
---|
| 447 | |
---|
| 448 | ! |
---|
| 449 | !-- If required compute impact of latent heat due to precipitation |
---|
| 450 | IF ( precipitation ) THEN |
---|
| 451 | CALL impact_of_latent_heat( i, j ) |
---|
| 452 | ENDIF |
---|
[153] | 453 | |
---|
| 454 | ! |
---|
| 455 | !-- Consideration of heat sources within the plant canopy |
---|
| 456 | IF ( plant_canopy .AND. ( cthf /= 0.0 ) ) THEN |
---|
| 457 | CALL plant_canopy_model( i, j, 4 ) |
---|
| 458 | ENDIF |
---|
| 459 | |
---|
[411] | 460 | ! |
---|
| 461 | !-- If required compute influence of large-scale subsidence/ascent |
---|
| 462 | IF ( large_scale_subsidence ) THEN |
---|
| 463 | CALL subsidence ( i, j, tend, pt, pt_init ) |
---|
| 464 | ENDIF |
---|
| 465 | |
---|
[1] | 466 | CALL user_actions( i, j, 'pt-tendency' ) |
---|
| 467 | |
---|
| 468 | ! |
---|
| 469 | !-- Prognostic equation for potential temperature |
---|
[19] | 470 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 471 | pt_p(k,j,i) = ( 1 - sat ) * pt_m(k,j,i) + sat * pt(k,j,i) + & |
---|
| 472 | dt_3d * ( & |
---|
| 473 | sbt * tend(k,j,i) + tsc(3) * tpt_m(k,j,i) & |
---|
| 474 | ) - & |
---|
| 475 | tsc(5) * rdf(k) * ( pt(k,j,i) - pt_init(k) ) |
---|
| 476 | ENDDO |
---|
| 477 | |
---|
| 478 | ! |
---|
| 479 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 480 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 481 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
[19] | 482 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 483 | tpt_m(k,j,i) = tend(k,j,i) |
---|
| 484 | ENDDO |
---|
| 485 | ELSEIF ( intermediate_timestep_count < & |
---|
| 486 | intermediate_timestep_count_max ) THEN |
---|
[19] | 487 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 488 | tpt_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tpt_m(k,j,i) |
---|
| 489 | ENDDO |
---|
| 490 | ENDIF |
---|
| 491 | ENDIF |
---|
| 492 | |
---|
| 493 | ENDDO |
---|
| 494 | ENDDO |
---|
| 495 | |
---|
| 496 | CALL cpu_log( log_point(13), 'pt-equation', 'stop' ) |
---|
| 497 | |
---|
| 498 | ! |
---|
[95] | 499 | !-- If required, compute prognostic equation for salinity |
---|
| 500 | IF ( ocean ) THEN |
---|
| 501 | |
---|
| 502 | CALL cpu_log( log_point(37), 'sa-equation', 'start' ) |
---|
| 503 | |
---|
| 504 | ! |
---|
| 505 | !-- sa-tendency terms with communication |
---|
| 506 | sat = tsc(1) |
---|
| 507 | sbt = tsc(2) |
---|
| 508 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
| 509 | |
---|
| 510 | IF ( timestep_scheme(1:5) /= 'runge' ) THEN |
---|
| 511 | ! |
---|
| 512 | !-- Bott-Chlond scheme always uses Euler time step when leapfrog is |
---|
| 513 | !-- switched on. Thus: |
---|
| 514 | sat = 1.0 |
---|
| 515 | sbt = 1.0 |
---|
| 516 | ENDIF |
---|
| 517 | tend = 0.0 |
---|
| 518 | CALL advec_s_bc( sa, 'sa' ) |
---|
| 519 | ELSE |
---|
| 520 | IF ( tsc(2) /= 2.0 ) THEN |
---|
| 521 | IF ( scalar_advec == 'ups-scheme' ) THEN |
---|
| 522 | tend = 0.0 |
---|
| 523 | CALL advec_s_ups( sa, 'sa' ) |
---|
| 524 | ENDIF |
---|
| 525 | ENDIF |
---|
| 526 | ENDIF |
---|
| 527 | |
---|
| 528 | ! |
---|
| 529 | !-- sa terms with no communication |
---|
| 530 | DO i = nxl, nxr |
---|
| 531 | DO j = nys, nyn |
---|
| 532 | ! |
---|
| 533 | !-- Tendency-terms |
---|
| 534 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
| 535 | CALL diffusion_s( i, j, ddzu, ddzw, kh, sa, saswsb, saswst, & |
---|
[129] | 536 | wall_salinityflux, tend ) |
---|
[95] | 537 | ELSE |
---|
| 538 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 539 | tend(:,j,i) = 0.0 |
---|
| 540 | CALL advec_s_pw( i, j, sa ) |
---|
| 541 | ELSE |
---|
| 542 | IF ( scalar_advec /= 'ups-scheme' ) THEN |
---|
| 543 | tend(:,j,i) = 0.0 |
---|
| 544 | CALL advec_s_up( i, j, sa ) |
---|
| 545 | ENDIF |
---|
| 546 | ENDIF |
---|
| 547 | CALL diffusion_s( i, j, ddzu, ddzw, kh, sa, saswsb, saswst, & |
---|
[129] | 548 | wall_salinityflux, tend ) |
---|
[95] | 549 | ENDIF |
---|
| 550 | |
---|
| 551 | CALL user_actions( i, j, 'sa-tendency' ) |
---|
| 552 | |
---|
| 553 | ! |
---|
| 554 | !-- Prognostic equation for salinity |
---|
| 555 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 556 | sa_p(k,j,i) = sat * sa(k,j,i) + & |
---|
| 557 | dt_3d * ( & |
---|
| 558 | sbt * tend(k,j,i) + tsc(3) * tsa_m(k,j,i) & |
---|
| 559 | ) - & |
---|
| 560 | tsc(5) * rdf(k) * ( sa(k,j,i) - sa_init(k) ) |
---|
| 561 | IF ( sa_p(k,j,i) < 0.0 ) sa_p(k,j,i) = 0.1 * sa(k,j,i) |
---|
| 562 | ENDDO |
---|
| 563 | |
---|
| 564 | ! |
---|
| 565 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 566 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 567 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 568 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 569 | tsa_m(k,j,i) = tend(k,j,i) |
---|
| 570 | ENDDO |
---|
| 571 | ELSEIF ( intermediate_timestep_count < & |
---|
| 572 | intermediate_timestep_count_max ) THEN |
---|
| 573 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 574 | tsa_m(k,j,i) = -9.5625 * tend(k,j,i) + & |
---|
| 575 | 5.3125 * tsa_m(k,j,i) |
---|
| 576 | ENDDO |
---|
| 577 | ENDIF |
---|
| 578 | ENDIF |
---|
| 579 | |
---|
[96] | 580 | ! |
---|
| 581 | !-- Calculate density by the equation of state for seawater |
---|
| 582 | CALL eqn_state_seawater( i, j ) |
---|
| 583 | |
---|
[95] | 584 | ENDDO |
---|
| 585 | ENDDO |
---|
| 586 | |
---|
| 587 | CALL cpu_log( log_point(37), 'sa-equation', 'stop' ) |
---|
| 588 | |
---|
| 589 | ENDIF |
---|
| 590 | |
---|
| 591 | ! |
---|
[1] | 592 | !-- If required, compute prognostic equation for total water content / scalar |
---|
[75] | 593 | IF ( humidity .OR. passive_scalar ) THEN |
---|
[1] | 594 | |
---|
| 595 | CALL cpu_log( log_point(29), 'q/s-equation', 'start' ) |
---|
| 596 | |
---|
| 597 | ! |
---|
| 598 | !-- Scalar/q-tendency terms with communication |
---|
[70] | 599 | sat = tsc(1) |
---|
| 600 | sbt = tsc(2) |
---|
[1] | 601 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[70] | 602 | |
---|
| 603 | IF ( timestep_scheme(1:5) /= 'runge' ) THEN |
---|
[1] | 604 | ! |
---|
[70] | 605 | !-- Bott-Chlond scheme always uses Euler time step when leapfrog is |
---|
| 606 | !-- switched on. Thus: |
---|
| 607 | sat = 1.0 |
---|
| 608 | sbt = 1.0 |
---|
| 609 | ENDIF |
---|
[1] | 610 | tend = 0.0 |
---|
| 611 | CALL advec_s_bc( q, 'q' ) |
---|
| 612 | ELSE |
---|
| 613 | IF ( tsc(2) /= 2.0 ) THEN |
---|
| 614 | IF ( scalar_advec == 'ups-scheme' ) THEN |
---|
| 615 | tend = 0.0 |
---|
| 616 | CALL advec_s_ups( q, 'q' ) |
---|
| 617 | ENDIF |
---|
| 618 | ENDIF |
---|
| 619 | ENDIF |
---|
| 620 | |
---|
| 621 | ! |
---|
| 622 | !-- Scalar/q-tendency terms with no communication |
---|
| 623 | DO i = nxl, nxr |
---|
| 624 | DO j = nys, nyn |
---|
| 625 | ! |
---|
| 626 | !-- Tendency-terms |
---|
| 627 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[129] | 628 | CALL diffusion_s( i, j, ddzu, ddzw, kh, q, qsws, qswst, & |
---|
| 629 | wall_qflux, tend ) |
---|
[1] | 630 | ELSE |
---|
| 631 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 632 | tend(:,j,i) = 0.0 |
---|
| 633 | CALL advec_s_pw( i, j, q ) |
---|
| 634 | ELSE |
---|
| 635 | IF ( scalar_advec /= 'ups-scheme' ) THEN |
---|
| 636 | tend(:,j,i) = 0.0 |
---|
| 637 | CALL advec_s_up( i, j, q ) |
---|
| 638 | ENDIF |
---|
| 639 | ENDIF |
---|
| 640 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' )& |
---|
| 641 | THEN |
---|
| 642 | CALL diffusion_s( i, j, ddzu, ddzw, kh_m, q_m, qsws_m, & |
---|
[129] | 643 | qswst_m, wall_qflux, tend ) |
---|
[19] | 644 | ELSE |
---|
| 645 | CALL diffusion_s( i, j, ddzu, ddzw, kh, q, qsws, qswst, & |
---|
[129] | 646 | wall_qflux, tend ) |
---|
[1] | 647 | ENDIF |
---|
| 648 | ENDIF |
---|
| 649 | |
---|
| 650 | ! |
---|
| 651 | !-- If required compute decrease of total water content due to |
---|
| 652 | !-- precipitation |
---|
| 653 | IF ( precipitation ) THEN |
---|
| 654 | CALL calc_precipitation( i, j ) |
---|
| 655 | ENDIF |
---|
[153] | 656 | |
---|
| 657 | ! |
---|
| 658 | !-- Sink or source of scalar concentration due to canopy elements |
---|
| 659 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 5 ) |
---|
| 660 | |
---|
[531] | 661 | ! |
---|
| 662 | !-- If required compute influence of large-scale subsidence/ascent |
---|
| 663 | IF ( large_scale_subsidence ) THEN |
---|
| 664 | CALL subsidence ( i, j, tend, q, q_init ) |
---|
| 665 | ENDIF |
---|
| 666 | |
---|
[1] | 667 | CALL user_actions( i, j, 'q-tendency' ) |
---|
| 668 | |
---|
| 669 | ! |
---|
| 670 | !-- Prognostic equation for total water content / scalar |
---|
[19] | 671 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 672 | q_p(k,j,i) = ( 1 - sat ) * q_m(k,j,i) + sat * q(k,j,i) + & |
---|
| 673 | dt_3d * ( & |
---|
| 674 | sbt * tend(k,j,i) + tsc(3) * tq_m(k,j,i) & |
---|
| 675 | ) - & |
---|
| 676 | tsc(5) * rdf(k) * ( q(k,j,i) - q_init(k) ) |
---|
[73] | 677 | IF ( q_p(k,j,i) < 0.0 ) q_p(k,j,i) = 0.1 * q(k,j,i) |
---|
[1] | 678 | ENDDO |
---|
| 679 | |
---|
| 680 | ! |
---|
| 681 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 682 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 683 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
[19] | 684 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 685 | tq_m(k,j,i) = tend(k,j,i) |
---|
| 686 | ENDDO |
---|
| 687 | ELSEIF ( intermediate_timestep_count < & |
---|
| 688 | intermediate_timestep_count_max ) THEN |
---|
[19] | 689 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 690 | tq_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tq_m(k,j,i) |
---|
| 691 | ENDDO |
---|
| 692 | ENDIF |
---|
| 693 | ENDIF |
---|
| 694 | |
---|
| 695 | ENDDO |
---|
| 696 | ENDDO |
---|
| 697 | |
---|
| 698 | CALL cpu_log( log_point(29), 'q/s-equation', 'stop' ) |
---|
| 699 | |
---|
| 700 | ENDIF |
---|
| 701 | |
---|
| 702 | ! |
---|
| 703 | !-- If required, compute prognostic equation for turbulent kinetic |
---|
| 704 | !-- energy (TKE) |
---|
| 705 | IF ( .NOT. constant_diffusion ) THEN |
---|
| 706 | |
---|
| 707 | CALL cpu_log( log_point(16), 'tke-equation', 'start' ) |
---|
| 708 | |
---|
| 709 | ! |
---|
| 710 | !-- TKE-tendency terms with communication |
---|
| 711 | CALL production_e_init |
---|
[70] | 712 | |
---|
| 713 | sat = tsc(1) |
---|
| 714 | sbt = tsc(2) |
---|
[1] | 715 | IF ( .NOT. use_upstream_for_tke ) THEN |
---|
| 716 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[70] | 717 | |
---|
| 718 | IF ( timestep_scheme(1:5) /= 'runge' ) THEN |
---|
[1] | 719 | ! |
---|
[70] | 720 | !-- Bott-Chlond scheme always uses Euler time step when leapfrog is |
---|
| 721 | !-- switched on. Thus: |
---|
| 722 | sat = 1.0 |
---|
| 723 | sbt = 1.0 |
---|
| 724 | ENDIF |
---|
[1] | 725 | tend = 0.0 |
---|
| 726 | CALL advec_s_bc( e, 'e' ) |
---|
| 727 | ELSE |
---|
| 728 | IF ( tsc(2) /= 2.0 ) THEN |
---|
| 729 | IF ( scalar_advec == 'ups-scheme' ) THEN |
---|
| 730 | tend = 0.0 |
---|
| 731 | CALL advec_s_ups( e, 'e' ) |
---|
| 732 | ENDIF |
---|
| 733 | ENDIF |
---|
| 734 | ENDIF |
---|
| 735 | ENDIF |
---|
| 736 | |
---|
| 737 | ! |
---|
| 738 | !-- TKE-tendency terms with no communication |
---|
| 739 | DO i = nxl, nxr |
---|
| 740 | DO j = nys, nyn |
---|
| 741 | ! |
---|
| 742 | !-- Tendency-terms |
---|
| 743 | IF ( scalar_advec == 'bc-scheme' .AND. & |
---|
| 744 | .NOT. use_upstream_for_tke ) THEN |
---|
[75] | 745 | IF ( .NOT. humidity ) THEN |
---|
[97] | 746 | IF ( ocean ) THEN |
---|
[388] | 747 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & |
---|
| 748 | l_grid, prho, prho_reference, rif, & |
---|
| 749 | tend, zu, zw ) |
---|
[97] | 750 | ELSE |
---|
[388] | 751 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & |
---|
| 752 | l_grid, pt, pt_reference, rif, tend, & |
---|
[97] | 753 | zu, zw ) |
---|
| 754 | ENDIF |
---|
[1] | 755 | ELSE |
---|
[97] | 756 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & |
---|
| 757 | l_grid, vpt, pt_reference, rif, tend, zu, & |
---|
| 758 | zw ) |
---|
[1] | 759 | ENDIF |
---|
| 760 | ELSE |
---|
| 761 | IF ( use_upstream_for_tke ) THEN |
---|
| 762 | tend(:,j,i) = 0.0 |
---|
| 763 | CALL advec_s_up( i, j, e ) |
---|
| 764 | ELSE |
---|
| 765 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) & |
---|
| 766 | THEN |
---|
| 767 | tend(:,j,i) = 0.0 |
---|
| 768 | CALL advec_s_pw( i, j, e ) |
---|
| 769 | ELSE |
---|
| 770 | IF ( scalar_advec /= 'ups-scheme' ) THEN |
---|
| 771 | tend(:,j,i) = 0.0 |
---|
| 772 | CALL advec_s_up( i, j, e ) |
---|
| 773 | ENDIF |
---|
| 774 | ENDIF |
---|
| 775 | ENDIF |
---|
| 776 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' )& |
---|
| 777 | THEN |
---|
[75] | 778 | IF ( .NOT. humidity ) THEN |
---|
[1] | 779 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, & |
---|
[97] | 780 | km_m, l_grid, pt_m, pt_reference, & |
---|
| 781 | rif_m, tend, zu, zw ) |
---|
[1] | 782 | ELSE |
---|
| 783 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, & |
---|
[97] | 784 | km_m, l_grid, vpt_m, pt_reference, & |
---|
| 785 | rif_m, tend, zu, zw ) |
---|
[1] | 786 | ENDIF |
---|
| 787 | ELSE |
---|
[75] | 788 | IF ( .NOT. humidity ) THEN |
---|
[97] | 789 | IF ( ocean ) THEN |
---|
| 790 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, & |
---|
[388] | 791 | km, l_grid, prho, prho_reference, & |
---|
[97] | 792 | rif, tend, zu, zw ) |
---|
| 793 | ELSE |
---|
| 794 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, & |
---|
| 795 | km, l_grid, pt, pt_reference, rif, & |
---|
| 796 | tend, zu, zw ) |
---|
| 797 | ENDIF |
---|
[1] | 798 | ELSE |
---|
| 799 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & |
---|
[97] | 800 | l_grid, vpt, pt_reference, rif, tend, & |
---|
| 801 | zu, zw ) |
---|
[1] | 802 | ENDIF |
---|
| 803 | ENDIF |
---|
| 804 | ENDIF |
---|
| 805 | CALL production_e( i, j ) |
---|
[138] | 806 | |
---|
| 807 | ! |
---|
| 808 | !-- Additional sink term for flows through plant canopies |
---|
[153] | 809 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 6 ) |
---|
[138] | 810 | |
---|
[1] | 811 | CALL user_actions( i, j, 'e-tendency' ) |
---|
| 812 | |
---|
| 813 | ! |
---|
| 814 | !-- Prognostic equation for TKE. |
---|
| 815 | !-- Eliminate negative TKE values, which can occur due to numerical |
---|
| 816 | !-- reasons in the course of the integration. In such cases the old TKE |
---|
| 817 | !-- value is reduced by 90%. |
---|
[19] | 818 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 819 | e_p(k,j,i) = ( 1 - sat ) * e_m(k,j,i) + sat * e(k,j,i) + & |
---|
| 820 | dt_3d * ( & |
---|
| 821 | sbt * tend(k,j,i) + tsc(3) * te_m(k,j,i) & |
---|
| 822 | ) |
---|
| 823 | IF ( e_p(k,j,i) < 0.0 ) e_p(k,j,i) = 0.1 * e(k,j,i) |
---|
| 824 | ENDDO |
---|
| 825 | |
---|
| 826 | ! |
---|
| 827 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 828 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 829 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
[19] | 830 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 831 | te_m(k,j,i) = tend(k,j,i) |
---|
| 832 | ENDDO |
---|
| 833 | ELSEIF ( intermediate_timestep_count < & |
---|
| 834 | intermediate_timestep_count_max ) THEN |
---|
[19] | 835 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 836 | te_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * te_m(k,j,i) |
---|
| 837 | ENDDO |
---|
| 838 | ENDIF |
---|
| 839 | ENDIF |
---|
| 840 | |
---|
| 841 | ENDDO |
---|
| 842 | ENDDO |
---|
| 843 | |
---|
| 844 | CALL cpu_log( log_point(16), 'tke-equation', 'stop' ) |
---|
| 845 | |
---|
| 846 | ENDIF |
---|
| 847 | |
---|
| 848 | |
---|
[63] | 849 | END SUBROUTINE prognostic_equations_noopt |
---|
[1] | 850 | |
---|
| 851 | |
---|
[63] | 852 | SUBROUTINE prognostic_equations_cache |
---|
[1] | 853 | |
---|
| 854 | !------------------------------------------------------------------------------! |
---|
| 855 | ! Version with one optimized loop over all equations. It is only allowed to |
---|
| 856 | ! be called for the standard Piascek-Williams advection scheme. |
---|
| 857 | ! |
---|
[95] | 858 | ! Here the calls of most subroutines are embedded in two DO loops over i and j, |
---|
| 859 | ! so communication between CPUs is not allowed (does not make sense) within |
---|
| 860 | ! these loops. |
---|
[1] | 861 | ! |
---|
| 862 | ! (Optimized to avoid cache missings, i.e. for Power4/5-architectures.) |
---|
| 863 | !------------------------------------------------------------------------------! |
---|
| 864 | |
---|
| 865 | IMPLICIT NONE |
---|
| 866 | |
---|
| 867 | CHARACTER (LEN=9) :: time_to_string |
---|
| 868 | INTEGER :: i, j, k |
---|
| 869 | |
---|
| 870 | |
---|
| 871 | ! |
---|
| 872 | !-- Time measurement can only be performed for the whole set of equations |
---|
| 873 | CALL cpu_log( log_point(32), 'all progn.equations', 'start' ) |
---|
| 874 | |
---|
| 875 | |
---|
| 876 | ! |
---|
| 877 | !-- Calculate those variables needed in the tendency terms which need |
---|
| 878 | !-- global communication |
---|
[96] | 879 | CALL calc_mean_profile( pt, 4 ) |
---|
| 880 | IF ( ocean ) CALL calc_mean_profile( rho, 64 ) |
---|
| 881 | IF ( humidity ) CALL calc_mean_profile( vpt, 44 ) |
---|
[1] | 882 | IF ( .NOT. constant_diffusion ) CALL production_e_init |
---|
| 883 | |
---|
| 884 | |
---|
| 885 | ! |
---|
| 886 | !-- Loop over all prognostic equations |
---|
| 887 | !$OMP PARALLEL private (i,j,k) |
---|
| 888 | !$OMP DO |
---|
[75] | 889 | DO i = nxl, nxr |
---|
| 890 | DO j = nys, nyn |
---|
[1] | 891 | ! |
---|
| 892 | !-- Tendency terms for u-velocity component |
---|
[106] | 893 | IF ( .NOT. outflow_l .OR. i > nxl ) THEN |
---|
[1] | 894 | |
---|
| 895 | tend(:,j,i) = 0.0 |
---|
| 896 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 897 | CALL advec_u_pw( i, j ) |
---|
| 898 | ELSE |
---|
| 899 | CALL advec_u_up( i, j ) |
---|
| 900 | ENDIF |
---|
| 901 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) & |
---|
| 902 | THEN |
---|
| 903 | CALL diffusion_u( i, j, ddzu, ddzw, km_m, km_damp_y, tend, & |
---|
[102] | 904 | u_m, usws_m, uswst_m, v_m, w_m ) |
---|
[1] | 905 | ELSE |
---|
| 906 | CALL diffusion_u( i, j, ddzu, ddzw, km, km_damp_y, tend, u, & |
---|
[102] | 907 | usws, uswst, v, w ) |
---|
[1] | 908 | ENDIF |
---|
| 909 | CALL coriolis( i, j, 1 ) |
---|
[97] | 910 | IF ( sloping_surface ) CALL buoyancy( i, j, pt, pt_reference, 1, & |
---|
| 911 | 4 ) |
---|
[138] | 912 | |
---|
| 913 | ! |
---|
| 914 | !-- Drag by plant canopy |
---|
| 915 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 1 ) |
---|
| 916 | |
---|
[240] | 917 | ! |
---|
| 918 | !-- External pressure gradient |
---|
| 919 | IF ( dp_external ) THEN |
---|
| 920 | DO k = dp_level_ind_b+1, nzt |
---|
| 921 | tend(k,j,i) = tend(k,j,i) - dpdxy(1) * dp_smooth_factor(k) |
---|
| 922 | ENDDO |
---|
| 923 | ENDIF |
---|
| 924 | |
---|
[1] | 925 | CALL user_actions( i, j, 'u-tendency' ) |
---|
| 926 | |
---|
| 927 | ! |
---|
| 928 | !-- Prognostic equation for u-velocity component |
---|
| 929 | DO k = nzb_u_inner(j,i)+1, nzt |
---|
| 930 | u_p(k,j,i) = ( 1.0-tsc(1) ) * u_m(k,j,i) + tsc(1) * u(k,j,i) + & |
---|
| 931 | dt_3d * ( & |
---|
| 932 | tsc(2) * tend(k,j,i) + tsc(3) * tu_m(k,j,i) & |
---|
| 933 | - tsc(4) * ( p(k,j,i) - p(k,j,i-1) ) * ddx & |
---|
| 934 | ) - & |
---|
| 935 | tsc(5) * rdf(k) * ( u(k,j,i) - ug(k) ) |
---|
| 936 | ENDDO |
---|
| 937 | |
---|
| 938 | ! |
---|
| 939 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 940 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 941 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 942 | DO k = nzb_u_inner(j,i)+1, nzt |
---|
| 943 | tu_m(k,j,i) = tend(k,j,i) |
---|
| 944 | ENDDO |
---|
| 945 | ELSEIF ( intermediate_timestep_count < & |
---|
| 946 | intermediate_timestep_count_max ) THEN |
---|
| 947 | DO k = nzb_u_inner(j,i)+1, nzt |
---|
| 948 | tu_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tu_m(k,j,i) |
---|
| 949 | ENDDO |
---|
| 950 | ENDIF |
---|
| 951 | ENDIF |
---|
| 952 | |
---|
| 953 | ENDIF |
---|
| 954 | |
---|
| 955 | ! |
---|
| 956 | !-- Tendency terms for v-velocity component |
---|
[106] | 957 | IF ( .NOT. outflow_s .OR. j > nys ) THEN |
---|
[1] | 958 | |
---|
| 959 | tend(:,j,i) = 0.0 |
---|
| 960 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 961 | CALL advec_v_pw( i, j ) |
---|
| 962 | ELSE |
---|
| 963 | CALL advec_v_up( i, j ) |
---|
| 964 | ENDIF |
---|
| 965 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) & |
---|
| 966 | THEN |
---|
| 967 | CALL diffusion_v( i, j, ddzu, ddzw, km_m, km_damp_x, tend, & |
---|
[102] | 968 | u_m, v_m, vsws_m, vswst_m, w_m ) |
---|
[1] | 969 | ELSE |
---|
| 970 | CALL diffusion_v( i, j, ddzu, ddzw, km, km_damp_x, tend, u, v, & |
---|
[102] | 971 | vsws, vswst, w ) |
---|
[1] | 972 | ENDIF |
---|
| 973 | CALL coriolis( i, j, 2 ) |
---|
[138] | 974 | |
---|
| 975 | ! |
---|
| 976 | !-- Drag by plant canopy |
---|
| 977 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 2 ) |
---|
| 978 | |
---|
[240] | 979 | ! |
---|
| 980 | !-- External pressure gradient |
---|
| 981 | IF ( dp_external ) THEN |
---|
| 982 | DO k = dp_level_ind_b+1, nzt |
---|
| 983 | tend(k,j,i) = tend(k,j,i) - dpdxy(2) * dp_smooth_factor(k) |
---|
| 984 | ENDDO |
---|
| 985 | ENDIF |
---|
| 986 | |
---|
[1] | 987 | CALL user_actions( i, j, 'v-tendency' ) |
---|
| 988 | |
---|
| 989 | ! |
---|
| 990 | !-- Prognostic equation for v-velocity component |
---|
| 991 | DO k = nzb_v_inner(j,i)+1, nzt |
---|
| 992 | v_p(k,j,i) = ( 1.0-tsc(1) ) * v_m(k,j,i) + tsc(1) * v(k,j,i) + & |
---|
| 993 | dt_3d * ( & |
---|
| 994 | tsc(2) * tend(k,j,i) + tsc(3) * tv_m(k,j,i) & |
---|
| 995 | - tsc(4) * ( p(k,j,i) - p(k,j-1,i) ) * ddy & |
---|
| 996 | ) - & |
---|
| 997 | tsc(5) * rdf(k) * ( v(k,j,i) - vg(k) ) |
---|
| 998 | ENDDO |
---|
| 999 | |
---|
| 1000 | ! |
---|
| 1001 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1002 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1003 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1004 | DO k = nzb_v_inner(j,i)+1, nzt |
---|
| 1005 | tv_m(k,j,i) = tend(k,j,i) |
---|
| 1006 | ENDDO |
---|
| 1007 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1008 | intermediate_timestep_count_max ) THEN |
---|
| 1009 | DO k = nzb_v_inner(j,i)+1, nzt |
---|
| 1010 | tv_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tv_m(k,j,i) |
---|
| 1011 | ENDDO |
---|
| 1012 | ENDIF |
---|
| 1013 | ENDIF |
---|
| 1014 | |
---|
| 1015 | ENDIF |
---|
| 1016 | |
---|
| 1017 | ! |
---|
| 1018 | !-- Tendency terms for w-velocity component |
---|
[106] | 1019 | tend(:,j,i) = 0.0 |
---|
| 1020 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1021 | CALL advec_w_pw( i, j ) |
---|
| 1022 | ELSE |
---|
| 1023 | CALL advec_w_up( i, j ) |
---|
| 1024 | ENDIF |
---|
| 1025 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) & |
---|
| 1026 | THEN |
---|
| 1027 | CALL diffusion_w( i, j, ddzu, ddzw, km_m, km_damp_x, & |
---|
| 1028 | km_damp_y, tend, u_m, v_m, w_m ) |
---|
| 1029 | ELSE |
---|
| 1030 | CALL diffusion_w( i, j, ddzu, ddzw, km, km_damp_x, km_damp_y, & |
---|
| 1031 | tend, u, v, w ) |
---|
| 1032 | ENDIF |
---|
| 1033 | CALL coriolis( i, j, 3 ) |
---|
| 1034 | IF ( ocean ) THEN |
---|
[388] | 1035 | CALL buoyancy( i, j, rho, rho_reference, 3, 64 ) |
---|
[106] | 1036 | ELSE |
---|
| 1037 | IF ( .NOT. humidity ) THEN |
---|
| 1038 | CALL buoyancy( i, j, pt, pt_reference, 3, 4 ) |
---|
| 1039 | ELSE |
---|
| 1040 | CALL buoyancy( i, j, vpt, pt_reference, 3, 44 ) |
---|
| 1041 | ENDIF |
---|
| 1042 | ENDIF |
---|
[138] | 1043 | |
---|
| 1044 | ! |
---|
| 1045 | !-- Drag by plant canopy |
---|
| 1046 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 3 ) |
---|
| 1047 | |
---|
[106] | 1048 | CALL user_actions( i, j, 'w-tendency' ) |
---|
[1] | 1049 | |
---|
[106] | 1050 | ! |
---|
| 1051 | !-- Prognostic equation for w-velocity component |
---|
| 1052 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
---|
| 1053 | w_p(k,j,i) = ( 1.0-tsc(1) ) * w_m(k,j,i) + tsc(1) * w(k,j,i) + & |
---|
| 1054 | dt_3d * ( & |
---|
| 1055 | tsc(2) * tend(k,j,i) + tsc(3) * tw_m(k,j,i) & |
---|
| 1056 | - tsc(4) * ( p(k+1,j,i) - p(k,j,i) ) * ddzu(k+1) & |
---|
| 1057 | ) - & |
---|
| 1058 | tsc(5) * rdf(k) * w(k,j,i) |
---|
| 1059 | ENDDO |
---|
| 1060 | |
---|
| 1061 | ! |
---|
| 1062 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1063 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1064 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1065 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
---|
| 1066 | tw_m(k,j,i) = tend(k,j,i) |
---|
| 1067 | ENDDO |
---|
| 1068 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1069 | intermediate_timestep_count_max ) THEN |
---|
| 1070 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
---|
| 1071 | tw_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tw_m(k,j,i) |
---|
| 1072 | ENDDO |
---|
| 1073 | ENDIF |
---|
| 1074 | ENDIF |
---|
| 1075 | |
---|
| 1076 | ! |
---|
| 1077 | !-- Tendency terms for potential temperature |
---|
| 1078 | tend(:,j,i) = 0.0 |
---|
| 1079 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1080 | CALL advec_s_pw( i, j, pt ) |
---|
| 1081 | ELSE |
---|
| 1082 | CALL advec_s_up( i, j, pt ) |
---|
| 1083 | ENDIF |
---|
| 1084 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) & |
---|
| 1085 | THEN |
---|
| 1086 | CALL diffusion_s( i, j, ddzu, ddzw, kh_m, pt_m, shf_m, & |
---|
[129] | 1087 | tswst_m, wall_heatflux, tend ) |
---|
[106] | 1088 | ELSE |
---|
[129] | 1089 | CALL diffusion_s( i, j, ddzu, ddzw, kh, pt, shf, tswst, & |
---|
| 1090 | wall_heatflux, tend ) |
---|
[106] | 1091 | ENDIF |
---|
| 1092 | |
---|
| 1093 | ! |
---|
| 1094 | !-- If required compute heating/cooling due to long wave radiation |
---|
| 1095 | !-- processes |
---|
| 1096 | IF ( radiation ) THEN |
---|
| 1097 | CALL calc_radiation( i, j ) |
---|
| 1098 | ENDIF |
---|
| 1099 | |
---|
| 1100 | ! |
---|
| 1101 | !-- If required compute impact of latent heat due to precipitation |
---|
| 1102 | IF ( precipitation ) THEN |
---|
| 1103 | CALL impact_of_latent_heat( i, j ) |
---|
| 1104 | ENDIF |
---|
[153] | 1105 | |
---|
| 1106 | ! |
---|
| 1107 | !-- Consideration of heat sources within the plant canopy |
---|
| 1108 | IF ( plant_canopy .AND. ( cthf /= 0.0 ) ) THEN |
---|
| 1109 | CALL plant_canopy_model( i, j, 4 ) |
---|
| 1110 | ENDIF |
---|
| 1111 | |
---|
[411] | 1112 | |
---|
| 1113 | !-- If required compute influence of large-scale subsidence/ascent |
---|
| 1114 | IF ( large_scale_subsidence ) THEN |
---|
| 1115 | CALL subsidence ( i, j, tend, pt, pt_init ) |
---|
| 1116 | ENDIF |
---|
| 1117 | |
---|
[106] | 1118 | CALL user_actions( i, j, 'pt-tendency' ) |
---|
| 1119 | |
---|
| 1120 | ! |
---|
| 1121 | !-- Prognostic equation for potential temperature |
---|
| 1122 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1123 | pt_p(k,j,i) = ( 1.0-tsc(1) ) * pt_m(k,j,i) + tsc(1)*pt(k,j,i) +& |
---|
| 1124 | dt_3d * ( & |
---|
| 1125 | tsc(2) * tend(k,j,i) + tsc(3) * tpt_m(k,j,i) & |
---|
| 1126 | ) - & |
---|
| 1127 | tsc(5) * rdf(k) * ( pt(k,j,i) - pt_init(k) ) |
---|
| 1128 | ENDDO |
---|
| 1129 | |
---|
| 1130 | ! |
---|
| 1131 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1132 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1133 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1134 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1135 | tpt_m(k,j,i) = tend(k,j,i) |
---|
| 1136 | ENDDO |
---|
| 1137 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1138 | intermediate_timestep_count_max ) THEN |
---|
| 1139 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1140 | tpt_m(k,j,i) = -9.5625 * tend(k,j,i) + & |
---|
| 1141 | 5.3125 * tpt_m(k,j,i) |
---|
| 1142 | ENDDO |
---|
| 1143 | ENDIF |
---|
| 1144 | ENDIF |
---|
| 1145 | |
---|
| 1146 | ! |
---|
| 1147 | !-- If required, compute prognostic equation for salinity |
---|
| 1148 | IF ( ocean ) THEN |
---|
| 1149 | |
---|
| 1150 | ! |
---|
| 1151 | !-- Tendency-terms for salinity |
---|
[1] | 1152 | tend(:,j,i) = 0.0 |
---|
[106] | 1153 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) & |
---|
[1] | 1154 | THEN |
---|
[106] | 1155 | CALL advec_s_pw( i, j, sa ) |
---|
[1] | 1156 | ELSE |
---|
[106] | 1157 | CALL advec_s_up( i, j, sa ) |
---|
[1] | 1158 | ENDIF |
---|
[106] | 1159 | CALL diffusion_s( i, j, ddzu, ddzw, kh, sa, saswsb, saswst, & |
---|
[129] | 1160 | wall_salinityflux, tend ) |
---|
[1] | 1161 | |
---|
[106] | 1162 | CALL user_actions( i, j, 'sa-tendency' ) |
---|
| 1163 | |
---|
[1] | 1164 | ! |
---|
[106] | 1165 | !-- Prognostic equation for salinity |
---|
| 1166 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1167 | sa_p(k,j,i) = tsc(1) * sa(k,j,i) + & |
---|
| 1168 | dt_3d * ( & |
---|
| 1169 | tsc(2) * tend(k,j,i) + tsc(3) * tsa_m(k,j,i) & |
---|
| 1170 | ) - & |
---|
| 1171 | tsc(5) * rdf(k) * ( sa(k,j,i) - sa_init(k) ) |
---|
| 1172 | IF ( sa_p(k,j,i) < 0.0 ) sa_p(k,j,i) = 0.1 * sa(k,j,i) |
---|
[1] | 1173 | ENDDO |
---|
| 1174 | |
---|
| 1175 | ! |
---|
| 1176 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1177 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1178 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
[106] | 1179 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1180 | tsa_m(k,j,i) = tend(k,j,i) |
---|
[1] | 1181 | ENDDO |
---|
| 1182 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1183 | intermediate_timestep_count_max ) THEN |
---|
[106] | 1184 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1185 | tsa_m(k,j,i) = -9.5625 * tend(k,j,i) + & |
---|
| 1186 | 5.3125 * tsa_m(k,j,i) |
---|
[1] | 1187 | ENDDO |
---|
| 1188 | ENDIF |
---|
| 1189 | ENDIF |
---|
| 1190 | |
---|
| 1191 | ! |
---|
[106] | 1192 | !-- Calculate density by the equation of state for seawater |
---|
| 1193 | CALL eqn_state_seawater( i, j ) |
---|
| 1194 | |
---|
| 1195 | ENDIF |
---|
| 1196 | |
---|
| 1197 | ! |
---|
| 1198 | !-- If required, compute prognostic equation for total water content / |
---|
| 1199 | !-- scalar |
---|
| 1200 | IF ( humidity .OR. passive_scalar ) THEN |
---|
| 1201 | |
---|
| 1202 | ! |
---|
| 1203 | !-- Tendency-terms for total water content / scalar |
---|
[1] | 1204 | tend(:,j,i) = 0.0 |
---|
[106] | 1205 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) & |
---|
| 1206 | THEN |
---|
| 1207 | CALL advec_s_pw( i, j, q ) |
---|
[1] | 1208 | ELSE |
---|
[106] | 1209 | CALL advec_s_up( i, j, q ) |
---|
[1] | 1210 | ENDIF |
---|
[106] | 1211 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' )& |
---|
[1] | 1212 | THEN |
---|
[106] | 1213 | CALL diffusion_s( i, j, ddzu, ddzw, kh_m, q_m, qsws_m, & |
---|
[129] | 1214 | qswst_m, wall_qflux, tend ) |
---|
[1] | 1215 | ELSE |
---|
[106] | 1216 | CALL diffusion_s( i, j, ddzu, ddzw, kh, q, qsws, qswst, & |
---|
[129] | 1217 | wall_qflux, tend ) |
---|
[1] | 1218 | ENDIF |
---|
[106] | 1219 | |
---|
[1] | 1220 | ! |
---|
[106] | 1221 | !-- If required compute decrease of total water content due to |
---|
| 1222 | !-- precipitation |
---|
[1] | 1223 | IF ( precipitation ) THEN |
---|
[106] | 1224 | CALL calc_precipitation( i, j ) |
---|
[1] | 1225 | ENDIF |
---|
[153] | 1226 | |
---|
| 1227 | ! |
---|
| 1228 | !-- Sink or source of scalar concentration due to canopy elements |
---|
| 1229 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 5 ) |
---|
| 1230 | |
---|
| 1231 | |
---|
[531] | 1232 | !-- If required compute influence of large-scale subsidence/ascent |
---|
| 1233 | IF ( large_scale_subsidence ) THEN |
---|
| 1234 | CALL subsidence ( i, j, tend, q, q_init ) |
---|
| 1235 | ENDIF |
---|
| 1236 | |
---|
| 1237 | |
---|
[106] | 1238 | CALL user_actions( i, j, 'q-tendency' ) |
---|
[1] | 1239 | |
---|
| 1240 | ! |
---|
[106] | 1241 | !-- Prognostic equation for total water content / scalar |
---|
[19] | 1242 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[106] | 1243 | q_p(k,j,i) = ( 1.0-tsc(1) ) * q_m(k,j,i) + tsc(1)*q(k,j,i) +& |
---|
| 1244 | dt_3d * ( & |
---|
| 1245 | tsc(2) * tend(k,j,i) + tsc(3) * tq_m(k,j,i) & |
---|
| 1246 | ) - & |
---|
| 1247 | tsc(5) * rdf(k) * ( q(k,j,i) - q_init(k) ) |
---|
| 1248 | IF ( q_p(k,j,i) < 0.0 ) q_p(k,j,i) = 0.1 * q(k,j,i) |
---|
[1] | 1249 | ENDDO |
---|
| 1250 | |
---|
| 1251 | ! |
---|
| 1252 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1253 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1254 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
[19] | 1255 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[106] | 1256 | tq_m(k,j,i) = tend(k,j,i) |
---|
[1] | 1257 | ENDDO |
---|
| 1258 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1259 | intermediate_timestep_count_max ) THEN |
---|
[19] | 1260 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[106] | 1261 | tq_m(k,j,i) = -9.5625 * tend(k,j,i) + & |
---|
| 1262 | 5.3125 * tq_m(k,j,i) |
---|
[1] | 1263 | ENDDO |
---|
| 1264 | ENDIF |
---|
| 1265 | ENDIF |
---|
| 1266 | |
---|
[106] | 1267 | ENDIF |
---|
[95] | 1268 | |
---|
| 1269 | ! |
---|
[106] | 1270 | !-- If required, compute prognostic equation for turbulent kinetic |
---|
| 1271 | !-- energy (TKE) |
---|
| 1272 | IF ( .NOT. constant_diffusion ) THEN |
---|
[95] | 1273 | |
---|
| 1274 | ! |
---|
[106] | 1275 | !-- Tendency-terms for TKE |
---|
| 1276 | tend(:,j,i) = 0.0 |
---|
| 1277 | IF ( ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) & |
---|
| 1278 | .AND. .NOT. use_upstream_for_tke ) THEN |
---|
| 1279 | CALL advec_s_pw( i, j, e ) |
---|
| 1280 | ELSE |
---|
| 1281 | CALL advec_s_up( i, j, e ) |
---|
[95] | 1282 | ENDIF |
---|
[106] | 1283 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' )& |
---|
| 1284 | THEN |
---|
| 1285 | IF ( .NOT. humidity ) THEN |
---|
| 1286 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, & |
---|
| 1287 | km_m, l_grid, pt_m, pt_reference, & |
---|
| 1288 | rif_m, tend, zu, zw ) |
---|
[1] | 1289 | ELSE |
---|
[106] | 1290 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, & |
---|
| 1291 | km_m, l_grid, vpt_m, pt_reference, & |
---|
| 1292 | rif_m, tend, zu, zw ) |
---|
[1] | 1293 | ENDIF |
---|
[106] | 1294 | ELSE |
---|
| 1295 | IF ( .NOT. humidity ) THEN |
---|
| 1296 | IF ( ocean ) THEN |
---|
[388] | 1297 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, & |
---|
| 1298 | km, l_grid, prho, prho_reference, & |
---|
[106] | 1299 | rif, tend, zu, zw ) |
---|
[1] | 1300 | ELSE |
---|
[106] | 1301 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, & |
---|
| 1302 | km, l_grid, pt, pt_reference, rif, & |
---|
| 1303 | tend, zu, zw ) |
---|
[1] | 1304 | ENDIF |
---|
| 1305 | ELSE |
---|
[106] | 1306 | CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & |
---|
| 1307 | l_grid, vpt, pt_reference, rif, tend, & |
---|
| 1308 | zu, zw ) |
---|
[1] | 1309 | ENDIF |
---|
[106] | 1310 | ENDIF |
---|
| 1311 | CALL production_e( i, j ) |
---|
[138] | 1312 | |
---|
| 1313 | ! |
---|
| 1314 | !-- Additional sink term for flows through plant canopies |
---|
[153] | 1315 | IF ( plant_canopy ) CALL plant_canopy_model( i, j, 6 ) |
---|
[138] | 1316 | |
---|
[106] | 1317 | CALL user_actions( i, j, 'e-tendency' ) |
---|
[1] | 1318 | |
---|
| 1319 | ! |
---|
[106] | 1320 | !-- Prognostic equation for TKE. |
---|
| 1321 | !-- Eliminate negative TKE values, which can occur due to numerical |
---|
| 1322 | !-- reasons in the course of the integration. In such cases the old |
---|
| 1323 | !-- TKE value is reduced by 90%. |
---|
| 1324 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1325 | e_p(k,j,i) = ( 1.0-tsc(1) ) * e_m(k,j,i) + tsc(1)*e(k,j,i) +& |
---|
| 1326 | dt_3d * ( & |
---|
| 1327 | tsc(2) * tend(k,j,i) + tsc(3) * te_m(k,j,i) & |
---|
| 1328 | ) |
---|
| 1329 | IF ( e_p(k,j,i) < 0.0 ) e_p(k,j,i) = 0.1 * e(k,j,i) |
---|
| 1330 | ENDDO |
---|
[1] | 1331 | |
---|
| 1332 | ! |
---|
[106] | 1333 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1334 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1335 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1336 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1337 | te_m(k,j,i) = tend(k,j,i) |
---|
| 1338 | ENDDO |
---|
| 1339 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1340 | intermediate_timestep_count_max ) THEN |
---|
| 1341 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1342 | te_m(k,j,i) = -9.5625 * tend(k,j,i) + & |
---|
| 1343 | 5.3125 * te_m(k,j,i) |
---|
| 1344 | ENDDO |
---|
[1] | 1345 | ENDIF |
---|
[106] | 1346 | ENDIF |
---|
[1] | 1347 | |
---|
[106] | 1348 | ENDIF ! TKE equation |
---|
[1] | 1349 | |
---|
| 1350 | ENDDO |
---|
| 1351 | ENDDO |
---|
| 1352 | !$OMP END PARALLEL |
---|
| 1353 | |
---|
| 1354 | CALL cpu_log( log_point(32), 'all progn.equations', 'stop' ) |
---|
| 1355 | |
---|
| 1356 | |
---|
[63] | 1357 | END SUBROUTINE prognostic_equations_cache |
---|
[1] | 1358 | |
---|
| 1359 | |
---|
[63] | 1360 | SUBROUTINE prognostic_equations_vector |
---|
[1] | 1361 | |
---|
| 1362 | !------------------------------------------------------------------------------! |
---|
| 1363 | ! Version for vector machines |
---|
| 1364 | !------------------------------------------------------------------------------! |
---|
| 1365 | |
---|
| 1366 | IMPLICIT NONE |
---|
| 1367 | |
---|
| 1368 | CHARACTER (LEN=9) :: time_to_string |
---|
| 1369 | INTEGER :: i, j, k |
---|
| 1370 | REAL :: sat, sbt |
---|
| 1371 | |
---|
| 1372 | ! |
---|
| 1373 | !-- Calculate those variables needed in the tendency terms which need |
---|
| 1374 | !-- global communication |
---|
[96] | 1375 | CALL calc_mean_profile( pt, 4 ) |
---|
| 1376 | IF ( ocean ) CALL calc_mean_profile( rho, 64 ) |
---|
| 1377 | IF ( humidity ) CALL calc_mean_profile( vpt, 44 ) |
---|
[1] | 1378 | |
---|
| 1379 | ! |
---|
| 1380 | !-- u-velocity component |
---|
| 1381 | CALL cpu_log( log_point(5), 'u-equation', 'start' ) |
---|
| 1382 | |
---|
| 1383 | ! |
---|
| 1384 | !-- u-tendency terms with communication |
---|
| 1385 | IF ( momentum_advec == 'ups-scheme' ) THEN |
---|
| 1386 | tend = 0.0 |
---|
| 1387 | CALL advec_u_ups |
---|
| 1388 | ENDIF |
---|
| 1389 | |
---|
| 1390 | ! |
---|
| 1391 | !-- u-tendency terms with no communication |
---|
| 1392 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1393 | tend = 0.0 |
---|
| 1394 | CALL advec_u_pw |
---|
| 1395 | ELSE |
---|
| 1396 | IF ( momentum_advec /= 'ups-scheme' ) THEN |
---|
| 1397 | tend = 0.0 |
---|
| 1398 | CALL advec_u_up |
---|
| 1399 | ENDIF |
---|
| 1400 | ENDIF |
---|
| 1401 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
---|
[102] | 1402 | CALL diffusion_u( ddzu, ddzw, km_m, km_damp_y, tend, u_m, usws_m, & |
---|
| 1403 | uswst_m, v_m, w_m ) |
---|
[1] | 1404 | ELSE |
---|
[102] | 1405 | CALL diffusion_u( ddzu, ddzw, km, km_damp_y, tend, u, usws, uswst, v, w ) |
---|
[1] | 1406 | ENDIF |
---|
| 1407 | CALL coriolis( 1 ) |
---|
[97] | 1408 | IF ( sloping_surface ) CALL buoyancy( pt, pt_reference, 1, 4 ) |
---|
[138] | 1409 | |
---|
| 1410 | ! |
---|
| 1411 | !-- Drag by plant canopy |
---|
| 1412 | IF ( plant_canopy ) CALL plant_canopy_model( 1 ) |
---|
| 1413 | |
---|
[240] | 1414 | ! |
---|
| 1415 | !-- External pressure gradient |
---|
| 1416 | IF ( dp_external ) THEN |
---|
| 1417 | DO i = nxlu, nxr |
---|
| 1418 | DO j = nys, nyn |
---|
| 1419 | DO k = dp_level_ind_b+1, nzt |
---|
| 1420 | tend(k,j,i) = tend(k,j,i) - dpdxy(1) * dp_smooth_factor(k) |
---|
| 1421 | ENDDO |
---|
| 1422 | ENDDO |
---|
| 1423 | ENDDO |
---|
| 1424 | ENDIF |
---|
| 1425 | |
---|
[1] | 1426 | CALL user_actions( 'u-tendency' ) |
---|
| 1427 | |
---|
| 1428 | ! |
---|
| 1429 | !-- Prognostic equation for u-velocity component |
---|
[106] | 1430 | DO i = nxlu, nxr |
---|
[1] | 1431 | DO j = nys, nyn |
---|
| 1432 | DO k = nzb_u_inner(j,i)+1, nzt |
---|
| 1433 | u_p(k,j,i) = ( 1.0-tsc(1) ) * u_m(k,j,i) + tsc(1) * u(k,j,i) + & |
---|
| 1434 | dt_3d * ( & |
---|
| 1435 | tsc(2) * tend(k,j,i) + tsc(3) * tu_m(k,j,i) & |
---|
| 1436 | - tsc(4) * ( p(k,j,i) - p(k,j,i-1) ) * ddx & |
---|
| 1437 | ) - & |
---|
| 1438 | tsc(5) * rdf(k) * ( u(k,j,i) - ug(k) ) |
---|
| 1439 | ENDDO |
---|
| 1440 | ENDDO |
---|
| 1441 | ENDDO |
---|
| 1442 | |
---|
| 1443 | ! |
---|
| 1444 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1445 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1446 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
[106] | 1447 | DO i = nxlu, nxr |
---|
[1] | 1448 | DO j = nys, nyn |
---|
| 1449 | DO k = nzb_u_inner(j,i)+1, nzt |
---|
| 1450 | tu_m(k,j,i) = tend(k,j,i) |
---|
| 1451 | ENDDO |
---|
| 1452 | ENDDO |
---|
| 1453 | ENDDO |
---|
| 1454 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1455 | intermediate_timestep_count_max ) THEN |
---|
[106] | 1456 | DO i = nxlu, nxr |
---|
[1] | 1457 | DO j = nys, nyn |
---|
| 1458 | DO k = nzb_u_inner(j,i)+1, nzt |
---|
| 1459 | tu_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tu_m(k,j,i) |
---|
| 1460 | ENDDO |
---|
| 1461 | ENDDO |
---|
| 1462 | ENDDO |
---|
| 1463 | ENDIF |
---|
| 1464 | ENDIF |
---|
| 1465 | |
---|
| 1466 | CALL cpu_log( log_point(5), 'u-equation', 'stop' ) |
---|
| 1467 | |
---|
| 1468 | ! |
---|
| 1469 | !-- v-velocity component |
---|
| 1470 | CALL cpu_log( log_point(6), 'v-equation', 'start' ) |
---|
| 1471 | |
---|
| 1472 | ! |
---|
| 1473 | !-- v-tendency terms with communication |
---|
| 1474 | IF ( momentum_advec == 'ups-scheme' ) THEN |
---|
| 1475 | tend = 0.0 |
---|
| 1476 | CALL advec_v_ups |
---|
| 1477 | ENDIF |
---|
| 1478 | |
---|
| 1479 | ! |
---|
| 1480 | !-- v-tendency terms with no communication |
---|
| 1481 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1482 | tend = 0.0 |
---|
| 1483 | CALL advec_v_pw |
---|
| 1484 | ELSE |
---|
| 1485 | IF ( momentum_advec /= 'ups-scheme' ) THEN |
---|
| 1486 | tend = 0.0 |
---|
| 1487 | CALL advec_v_up |
---|
| 1488 | ENDIF |
---|
| 1489 | ENDIF |
---|
| 1490 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
---|
| 1491 | CALL diffusion_v( ddzu, ddzw, km_m, km_damp_x, tend, u_m, v_m, vsws_m, & |
---|
[102] | 1492 | vswst_m, w_m ) |
---|
[1] | 1493 | ELSE |
---|
[102] | 1494 | CALL diffusion_v( ddzu, ddzw, km, km_damp_x, tend, u, v, vsws, vswst, w ) |
---|
[1] | 1495 | ENDIF |
---|
| 1496 | CALL coriolis( 2 ) |
---|
[138] | 1497 | |
---|
| 1498 | ! |
---|
| 1499 | !-- Drag by plant canopy |
---|
| 1500 | IF ( plant_canopy ) CALL plant_canopy_model( 2 ) |
---|
[240] | 1501 | |
---|
| 1502 | ! |
---|
| 1503 | !-- External pressure gradient |
---|
| 1504 | IF ( dp_external ) THEN |
---|
| 1505 | DO i = nxl, nxr |
---|
| 1506 | DO j = nysv, nyn |
---|
| 1507 | DO k = dp_level_ind_b+1, nzt |
---|
| 1508 | tend(k,j,i) = tend(k,j,i) - dpdxy(2) * dp_smooth_factor(k) |
---|
| 1509 | ENDDO |
---|
| 1510 | ENDDO |
---|
| 1511 | ENDDO |
---|
| 1512 | ENDIF |
---|
| 1513 | |
---|
[1] | 1514 | CALL user_actions( 'v-tendency' ) |
---|
| 1515 | |
---|
| 1516 | ! |
---|
| 1517 | !-- Prognostic equation for v-velocity component |
---|
| 1518 | DO i = nxl, nxr |
---|
[106] | 1519 | DO j = nysv, nyn |
---|
[1] | 1520 | DO k = nzb_v_inner(j,i)+1, nzt |
---|
| 1521 | v_p(k,j,i) = ( 1.0-tsc(1) ) * v_m(k,j,i) + tsc(1) * v(k,j,i) + & |
---|
| 1522 | dt_3d * ( & |
---|
| 1523 | tsc(2) * tend(k,j,i) + tsc(3) * tv_m(k,j,i) & |
---|
| 1524 | - tsc(4) * ( p(k,j,i) - p(k,j-1,i) ) * ddy & |
---|
| 1525 | ) - & |
---|
| 1526 | tsc(5) * rdf(k) * ( v(k,j,i) - vg(k) ) |
---|
| 1527 | ENDDO |
---|
| 1528 | ENDDO |
---|
| 1529 | ENDDO |
---|
| 1530 | |
---|
| 1531 | ! |
---|
| 1532 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1533 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1534 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1535 | DO i = nxl, nxr |
---|
[106] | 1536 | DO j = nysv, nyn |
---|
[1] | 1537 | DO k = nzb_v_inner(j,i)+1, nzt |
---|
| 1538 | tv_m(k,j,i) = tend(k,j,i) |
---|
| 1539 | ENDDO |
---|
| 1540 | ENDDO |
---|
| 1541 | ENDDO |
---|
| 1542 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1543 | intermediate_timestep_count_max ) THEN |
---|
| 1544 | DO i = nxl, nxr |
---|
[106] | 1545 | DO j = nysv, nyn |
---|
[1] | 1546 | DO k = nzb_v_inner(j,i)+1, nzt |
---|
| 1547 | tv_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tv_m(k,j,i) |
---|
| 1548 | ENDDO |
---|
| 1549 | ENDDO |
---|
| 1550 | ENDDO |
---|
| 1551 | ENDIF |
---|
| 1552 | ENDIF |
---|
| 1553 | |
---|
| 1554 | CALL cpu_log( log_point(6), 'v-equation', 'stop' ) |
---|
| 1555 | |
---|
| 1556 | ! |
---|
| 1557 | !-- w-velocity component |
---|
| 1558 | CALL cpu_log( log_point(7), 'w-equation', 'start' ) |
---|
| 1559 | |
---|
| 1560 | ! |
---|
| 1561 | !-- w-tendency terms with communication |
---|
| 1562 | IF ( momentum_advec == 'ups-scheme' ) THEN |
---|
| 1563 | tend = 0.0 |
---|
| 1564 | CALL advec_w_ups |
---|
| 1565 | ENDIF |
---|
| 1566 | |
---|
| 1567 | ! |
---|
| 1568 | !-- w-tendency terms with no communication |
---|
| 1569 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1570 | tend = 0.0 |
---|
| 1571 | CALL advec_w_pw |
---|
| 1572 | ELSE |
---|
| 1573 | IF ( momentum_advec /= 'ups-scheme' ) THEN |
---|
| 1574 | tend = 0.0 |
---|
| 1575 | CALL advec_w_up |
---|
| 1576 | ENDIF |
---|
| 1577 | ENDIF |
---|
| 1578 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
---|
| 1579 | CALL diffusion_w( ddzu, ddzw, km_m, km_damp_x, km_damp_y, tend, u_m, & |
---|
[57] | 1580 | v_m, w_m ) |
---|
[1] | 1581 | ELSE |
---|
[57] | 1582 | CALL diffusion_w( ddzu, ddzw, km, km_damp_x, km_damp_y, tend, u, v, w ) |
---|
[1] | 1583 | ENDIF |
---|
| 1584 | CALL coriolis( 3 ) |
---|
[97] | 1585 | IF ( ocean ) THEN |
---|
[388] | 1586 | CALL buoyancy( rho, rho_reference, 3, 64 ) |
---|
[1] | 1587 | ELSE |
---|
[97] | 1588 | IF ( .NOT. humidity ) THEN |
---|
| 1589 | CALL buoyancy( pt, pt_reference, 3, 4 ) |
---|
| 1590 | ELSE |
---|
| 1591 | CALL buoyancy( vpt, pt_reference, 3, 44 ) |
---|
| 1592 | ENDIF |
---|
[1] | 1593 | ENDIF |
---|
[138] | 1594 | |
---|
| 1595 | ! |
---|
| 1596 | !-- Drag by plant canopy |
---|
| 1597 | IF ( plant_canopy ) CALL plant_canopy_model( 3 ) |
---|
| 1598 | |
---|
[1] | 1599 | CALL user_actions( 'w-tendency' ) |
---|
| 1600 | |
---|
| 1601 | ! |
---|
| 1602 | !-- Prognostic equation for w-velocity component |
---|
| 1603 | DO i = nxl, nxr |
---|
| 1604 | DO j = nys, nyn |
---|
| 1605 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
---|
| 1606 | w_p(k,j,i) = ( 1-tsc(1) ) * w_m(k,j,i) + tsc(1) * w(k,j,i) + & |
---|
| 1607 | dt_3d * ( & |
---|
| 1608 | tsc(2) * tend(k,j,i) + tsc(3) * tw_m(k,j,i) & |
---|
| 1609 | - tsc(4) * ( p(k+1,j,i) - p(k,j,i) ) * ddzu(k+1) & |
---|
| 1610 | ) - & |
---|
| 1611 | tsc(5) * rdf(k) * w(k,j,i) |
---|
| 1612 | ENDDO |
---|
| 1613 | ENDDO |
---|
| 1614 | ENDDO |
---|
| 1615 | |
---|
| 1616 | ! |
---|
| 1617 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1618 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1619 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1620 | DO i = nxl, nxr |
---|
| 1621 | DO j = nys, nyn |
---|
| 1622 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
---|
| 1623 | tw_m(k,j,i) = tend(k,j,i) |
---|
| 1624 | ENDDO |
---|
| 1625 | ENDDO |
---|
| 1626 | ENDDO |
---|
| 1627 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1628 | intermediate_timestep_count_max ) THEN |
---|
| 1629 | DO i = nxl, nxr |
---|
| 1630 | DO j = nys, nyn |
---|
| 1631 | DO k = nzb_w_inner(j,i)+1, nzt-1 |
---|
| 1632 | tw_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tw_m(k,j,i) |
---|
| 1633 | ENDDO |
---|
| 1634 | ENDDO |
---|
| 1635 | ENDDO |
---|
| 1636 | ENDIF |
---|
| 1637 | ENDIF |
---|
| 1638 | |
---|
| 1639 | CALL cpu_log( log_point(7), 'w-equation', 'stop' ) |
---|
| 1640 | |
---|
| 1641 | ! |
---|
| 1642 | !-- potential temperature |
---|
| 1643 | CALL cpu_log( log_point(13), 'pt-equation', 'start' ) |
---|
| 1644 | |
---|
| 1645 | ! |
---|
| 1646 | !-- pt-tendency terms with communication |
---|
[63] | 1647 | sat = tsc(1) |
---|
| 1648 | sbt = tsc(2) |
---|
[1] | 1649 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[63] | 1650 | |
---|
| 1651 | IF ( timestep_scheme(1:5) /= 'runge' ) THEN |
---|
[1] | 1652 | ! |
---|
[63] | 1653 | !-- Bott-Chlond scheme always uses Euler time step when leapfrog is |
---|
| 1654 | !-- switched on. Thus: |
---|
| 1655 | sat = 1.0 |
---|
| 1656 | sbt = 1.0 |
---|
| 1657 | ENDIF |
---|
[1] | 1658 | tend = 0.0 |
---|
| 1659 | CALL advec_s_bc( pt, 'pt' ) |
---|
| 1660 | ELSE |
---|
| 1661 | IF ( tsc(2) /= 2.0 .AND. scalar_advec == 'ups-scheme' ) THEN |
---|
| 1662 | tend = 0.0 |
---|
| 1663 | CALL advec_s_ups( pt, 'pt' ) |
---|
| 1664 | ENDIF |
---|
| 1665 | ENDIF |
---|
| 1666 | |
---|
| 1667 | ! |
---|
| 1668 | !-- pt-tendency terms with no communication |
---|
| 1669 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[129] | 1670 | CALL diffusion_s( ddzu, ddzw, kh, pt, shf, tswst, wall_heatflux, & |
---|
| 1671 | tend ) |
---|
[1] | 1672 | ELSE |
---|
| 1673 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1674 | tend = 0.0 |
---|
| 1675 | CALL advec_s_pw( pt ) |
---|
| 1676 | ELSE |
---|
| 1677 | IF ( scalar_advec /= 'ups-scheme' ) THEN |
---|
| 1678 | tend = 0.0 |
---|
| 1679 | CALL advec_s_up( pt ) |
---|
| 1680 | ENDIF |
---|
| 1681 | ENDIF |
---|
| 1682 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
---|
[129] | 1683 | CALL diffusion_s( ddzu, ddzw, kh_m, pt_m, shf_m, tswst_m, & |
---|
| 1684 | wall_heatflux, tend ) |
---|
[1] | 1685 | ELSE |
---|
[129] | 1686 | CALL diffusion_s( ddzu, ddzw, kh, pt, shf, tswst, wall_heatflux, & |
---|
| 1687 | tend ) |
---|
[1] | 1688 | ENDIF |
---|
| 1689 | ENDIF |
---|
| 1690 | |
---|
| 1691 | ! |
---|
| 1692 | !-- If required compute heating/cooling due to long wave radiation |
---|
| 1693 | !-- processes |
---|
| 1694 | IF ( radiation ) THEN |
---|
| 1695 | CALL calc_radiation |
---|
| 1696 | ENDIF |
---|
| 1697 | |
---|
| 1698 | ! |
---|
| 1699 | !-- If required compute impact of latent heat due to precipitation |
---|
| 1700 | IF ( precipitation ) THEN |
---|
| 1701 | CALL impact_of_latent_heat |
---|
| 1702 | ENDIF |
---|
[153] | 1703 | |
---|
| 1704 | ! |
---|
| 1705 | !-- Consideration of heat sources within the plant canopy |
---|
| 1706 | IF ( plant_canopy .AND. ( cthf /= 0.0 ) ) THEN |
---|
| 1707 | CALL plant_canopy_model( 4 ) |
---|
| 1708 | ENDIF |
---|
| 1709 | |
---|
[411] | 1710 | !--If required compute influence of large-scale subsidence/ascent |
---|
| 1711 | IF ( large_scale_subsidence ) THEN |
---|
| 1712 | CALL subsidence ( tend, pt, pt_init ) |
---|
| 1713 | ENDIF |
---|
[153] | 1714 | |
---|
[1] | 1715 | CALL user_actions( 'pt-tendency' ) |
---|
| 1716 | |
---|
| 1717 | ! |
---|
| 1718 | !-- Prognostic equation for potential temperature |
---|
| 1719 | DO i = nxl, nxr |
---|
| 1720 | DO j = nys, nyn |
---|
[19] | 1721 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 1722 | pt_p(k,j,i) = ( 1 - sat ) * pt_m(k,j,i) + sat * pt(k,j,i) + & |
---|
| 1723 | dt_3d * ( & |
---|
| 1724 | sbt * tend(k,j,i) + tsc(3) * tpt_m(k,j,i) & |
---|
| 1725 | ) - & |
---|
| 1726 | tsc(5) * rdf(k) * ( pt(k,j,i) - pt_init(k) ) |
---|
| 1727 | ENDDO |
---|
| 1728 | ENDDO |
---|
| 1729 | ENDDO |
---|
| 1730 | |
---|
| 1731 | ! |
---|
| 1732 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1733 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1734 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1735 | DO i = nxl, nxr |
---|
| 1736 | DO j = nys, nyn |
---|
[19] | 1737 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 1738 | tpt_m(k,j,i) = tend(k,j,i) |
---|
| 1739 | ENDDO |
---|
| 1740 | ENDDO |
---|
| 1741 | ENDDO |
---|
| 1742 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1743 | intermediate_timestep_count_max ) THEN |
---|
| 1744 | DO i = nxl, nxr |
---|
| 1745 | DO j = nys, nyn |
---|
[19] | 1746 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 1747 | tpt_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tpt_m(k,j,i) |
---|
| 1748 | ENDDO |
---|
| 1749 | ENDDO |
---|
| 1750 | ENDDO |
---|
| 1751 | ENDIF |
---|
| 1752 | ENDIF |
---|
| 1753 | |
---|
| 1754 | CALL cpu_log( log_point(13), 'pt-equation', 'stop' ) |
---|
| 1755 | |
---|
| 1756 | ! |
---|
[95] | 1757 | !-- If required, compute prognostic equation for salinity |
---|
| 1758 | IF ( ocean ) THEN |
---|
| 1759 | |
---|
| 1760 | CALL cpu_log( log_point(37), 'sa-equation', 'start' ) |
---|
| 1761 | |
---|
| 1762 | ! |
---|
| 1763 | !-- sa-tendency terms with communication |
---|
| 1764 | sat = tsc(1) |
---|
| 1765 | sbt = tsc(2) |
---|
| 1766 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
| 1767 | |
---|
| 1768 | IF ( timestep_scheme(1:5) /= 'runge' ) THEN |
---|
| 1769 | ! |
---|
| 1770 | !-- Bott-Chlond scheme always uses Euler time step when leapfrog is |
---|
| 1771 | !-- switched on. Thus: |
---|
| 1772 | sat = 1.0 |
---|
| 1773 | sbt = 1.0 |
---|
| 1774 | ENDIF |
---|
| 1775 | tend = 0.0 |
---|
| 1776 | CALL advec_s_bc( sa, 'sa' ) |
---|
| 1777 | ELSE |
---|
| 1778 | IF ( tsc(2) /= 2.0 ) THEN |
---|
| 1779 | IF ( scalar_advec == 'ups-scheme' ) THEN |
---|
| 1780 | tend = 0.0 |
---|
| 1781 | CALL advec_s_ups( sa, 'sa' ) |
---|
| 1782 | ENDIF |
---|
| 1783 | ENDIF |
---|
| 1784 | ENDIF |
---|
| 1785 | |
---|
| 1786 | ! |
---|
[129] | 1787 | !-- sa-tendency terms with no communication |
---|
[95] | 1788 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[129] | 1789 | CALL diffusion_s( ddzu, ddzw, kh, sa, saswsb, saswst, & |
---|
| 1790 | wall_salinityflux, tend ) |
---|
[95] | 1791 | ELSE |
---|
| 1792 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1793 | tend = 0.0 |
---|
| 1794 | CALL advec_s_pw( sa ) |
---|
| 1795 | ELSE |
---|
| 1796 | IF ( scalar_advec /= 'ups-scheme' ) THEN |
---|
| 1797 | tend = 0.0 |
---|
| 1798 | CALL advec_s_up( sa ) |
---|
| 1799 | ENDIF |
---|
| 1800 | ENDIF |
---|
[129] | 1801 | CALL diffusion_s( ddzu, ddzw, kh, sa, saswsb, saswst, & |
---|
| 1802 | wall_salinityflux, tend ) |
---|
[95] | 1803 | ENDIF |
---|
| 1804 | |
---|
| 1805 | CALL user_actions( 'sa-tendency' ) |
---|
| 1806 | |
---|
| 1807 | ! |
---|
| 1808 | !-- Prognostic equation for salinity |
---|
| 1809 | DO i = nxl, nxr |
---|
| 1810 | DO j = nys, nyn |
---|
| 1811 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1812 | sa_p(k,j,i) = sat * sa(k,j,i) + & |
---|
| 1813 | dt_3d * ( & |
---|
| 1814 | sbt * tend(k,j,i) + tsc(3) * tsa_m(k,j,i) & |
---|
| 1815 | ) - & |
---|
| 1816 | tsc(5) * rdf(k) * ( sa(k,j,i) - sa_init(k) ) |
---|
| 1817 | IF ( sa_p(k,j,i) < 0.0 ) sa_p(k,j,i) = 0.1 * sa(k,j,i) |
---|
| 1818 | ENDDO |
---|
| 1819 | ENDDO |
---|
| 1820 | ENDDO |
---|
| 1821 | |
---|
| 1822 | ! |
---|
| 1823 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1824 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1825 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1826 | DO i = nxl, nxr |
---|
| 1827 | DO j = nys, nyn |
---|
| 1828 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1829 | tsa_m(k,j,i) = tend(k,j,i) |
---|
| 1830 | ENDDO |
---|
| 1831 | ENDDO |
---|
| 1832 | ENDDO |
---|
| 1833 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1834 | intermediate_timestep_count_max ) THEN |
---|
| 1835 | DO i = nxl, nxr |
---|
| 1836 | DO j = nys, nyn |
---|
| 1837 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
| 1838 | tsa_m(k,j,i) = -9.5625 * tend(k,j,i) + & |
---|
| 1839 | 5.3125 * tsa_m(k,j,i) |
---|
| 1840 | ENDDO |
---|
| 1841 | ENDDO |
---|
| 1842 | ENDDO |
---|
| 1843 | ENDIF |
---|
| 1844 | ENDIF |
---|
| 1845 | |
---|
| 1846 | CALL cpu_log( log_point(37), 'sa-equation', 'stop' ) |
---|
| 1847 | |
---|
[96] | 1848 | ! |
---|
| 1849 | !-- Calculate density by the equation of state for seawater |
---|
| 1850 | CALL cpu_log( log_point(38), 'eqns-seawater', 'start' ) |
---|
| 1851 | CALL eqn_state_seawater |
---|
| 1852 | CALL cpu_log( log_point(38), 'eqns-seawater', 'stop' ) |
---|
| 1853 | |
---|
[95] | 1854 | ENDIF |
---|
| 1855 | |
---|
| 1856 | ! |
---|
[1] | 1857 | !-- If required, compute prognostic equation for total water content / scalar |
---|
[75] | 1858 | IF ( humidity .OR. passive_scalar ) THEN |
---|
[1] | 1859 | |
---|
| 1860 | CALL cpu_log( log_point(29), 'q/s-equation', 'start' ) |
---|
| 1861 | |
---|
| 1862 | ! |
---|
| 1863 | !-- Scalar/q-tendency terms with communication |
---|
[63] | 1864 | sat = tsc(1) |
---|
| 1865 | sbt = tsc(2) |
---|
[1] | 1866 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[63] | 1867 | |
---|
| 1868 | IF ( timestep_scheme(1:5) /= 'runge' ) THEN |
---|
[1] | 1869 | ! |
---|
[63] | 1870 | !-- Bott-Chlond scheme always uses Euler time step when leapfrog is |
---|
| 1871 | !-- switched on. Thus: |
---|
| 1872 | sat = 1.0 |
---|
| 1873 | sbt = 1.0 |
---|
| 1874 | ENDIF |
---|
[1] | 1875 | tend = 0.0 |
---|
| 1876 | CALL advec_s_bc( q, 'q' ) |
---|
| 1877 | ELSE |
---|
| 1878 | IF ( tsc(2) /= 2.0 ) THEN |
---|
| 1879 | IF ( scalar_advec == 'ups-scheme' ) THEN |
---|
| 1880 | tend = 0.0 |
---|
| 1881 | CALL advec_s_ups( q, 'q' ) |
---|
| 1882 | ENDIF |
---|
| 1883 | ENDIF |
---|
| 1884 | ENDIF |
---|
| 1885 | |
---|
| 1886 | ! |
---|
| 1887 | !-- Scalar/q-tendency terms with no communication |
---|
| 1888 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[129] | 1889 | CALL diffusion_s( ddzu, ddzw, kh, q, qsws, qswst, wall_qflux, tend ) |
---|
[1] | 1890 | ELSE |
---|
| 1891 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1892 | tend = 0.0 |
---|
| 1893 | CALL advec_s_pw( q ) |
---|
| 1894 | ELSE |
---|
| 1895 | IF ( scalar_advec /= 'ups-scheme' ) THEN |
---|
| 1896 | tend = 0.0 |
---|
| 1897 | CALL advec_s_up( q ) |
---|
| 1898 | ENDIF |
---|
| 1899 | ENDIF |
---|
| 1900 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
---|
[129] | 1901 | CALL diffusion_s( ddzu, ddzw, kh_m, q_m, qsws_m, qswst_m, & |
---|
| 1902 | wall_qflux, tend ) |
---|
[1] | 1903 | ELSE |
---|
[129] | 1904 | CALL diffusion_s( ddzu, ddzw, kh, q, qsws, qswst, & |
---|
| 1905 | wall_qflux, tend ) |
---|
[1] | 1906 | ENDIF |
---|
| 1907 | ENDIF |
---|
| 1908 | |
---|
| 1909 | ! |
---|
| 1910 | !-- If required compute decrease of total water content due to |
---|
| 1911 | !-- precipitation |
---|
| 1912 | IF ( precipitation ) THEN |
---|
| 1913 | CALL calc_precipitation |
---|
| 1914 | ENDIF |
---|
[153] | 1915 | |
---|
| 1916 | ! |
---|
| 1917 | !-- Sink or source of scalar concentration due to canopy elements |
---|
| 1918 | IF ( plant_canopy ) CALL plant_canopy_model( 5 ) |
---|
| 1919 | |
---|
[531] | 1920 | ! |
---|
| 1921 | !-- If required compute influence of large-scale subsidence/ascent |
---|
| 1922 | IF ( large_scale_subsidence ) THEN |
---|
| 1923 | CALL subsidence ( tend, q, q_init ) |
---|
| 1924 | ENDIF |
---|
| 1925 | |
---|
[1] | 1926 | CALL user_actions( 'q-tendency' ) |
---|
| 1927 | |
---|
| 1928 | ! |
---|
| 1929 | !-- Prognostic equation for total water content / scalar |
---|
| 1930 | DO i = nxl, nxr |
---|
| 1931 | DO j = nys, nyn |
---|
[19] | 1932 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 1933 | q_p(k,j,i) = ( 1 - sat ) * q_m(k,j,i) + sat * q(k,j,i) + & |
---|
| 1934 | dt_3d * ( & |
---|
| 1935 | sbt * tend(k,j,i) + tsc(3) * tq_m(k,j,i) & |
---|
| 1936 | ) - & |
---|
| 1937 | tsc(5) * rdf(k) * ( q(k,j,i) - q_init(k) ) |
---|
[73] | 1938 | IF ( q_p(k,j,i) < 0.0 ) q_p(k,j,i) = 0.1 * q(k,j,i) |
---|
[1] | 1939 | ENDDO |
---|
| 1940 | ENDDO |
---|
| 1941 | ENDDO |
---|
| 1942 | |
---|
| 1943 | ! |
---|
| 1944 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 1945 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 1946 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 1947 | DO i = nxl, nxr |
---|
| 1948 | DO j = nys, nyn |
---|
[19] | 1949 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 1950 | tq_m(k,j,i) = tend(k,j,i) |
---|
| 1951 | ENDDO |
---|
| 1952 | ENDDO |
---|
| 1953 | ENDDO |
---|
| 1954 | ELSEIF ( intermediate_timestep_count < & |
---|
| 1955 | intermediate_timestep_count_max ) THEN |
---|
| 1956 | DO i = nxl, nxr |
---|
| 1957 | DO j = nys, nyn |
---|
[19] | 1958 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 1959 | tq_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * tq_m(k,j,i) |
---|
| 1960 | ENDDO |
---|
| 1961 | ENDDO |
---|
| 1962 | ENDDO |
---|
| 1963 | ENDIF |
---|
| 1964 | ENDIF |
---|
| 1965 | |
---|
| 1966 | CALL cpu_log( log_point(29), 'q/s-equation', 'stop' ) |
---|
| 1967 | |
---|
| 1968 | ENDIF |
---|
| 1969 | |
---|
| 1970 | ! |
---|
| 1971 | !-- If required, compute prognostic equation for turbulent kinetic |
---|
| 1972 | !-- energy (TKE) |
---|
| 1973 | IF ( .NOT. constant_diffusion ) THEN |
---|
| 1974 | |
---|
| 1975 | CALL cpu_log( log_point(16), 'tke-equation', 'start' ) |
---|
| 1976 | |
---|
| 1977 | ! |
---|
| 1978 | !-- TKE-tendency terms with communication |
---|
| 1979 | CALL production_e_init |
---|
[63] | 1980 | |
---|
| 1981 | sat = tsc(1) |
---|
| 1982 | sbt = tsc(2) |
---|
[1] | 1983 | IF ( .NOT. use_upstream_for_tke ) THEN |
---|
| 1984 | IF ( scalar_advec == 'bc-scheme' ) THEN |
---|
[63] | 1985 | |
---|
| 1986 | IF ( timestep_scheme(1:5) /= 'runge' ) THEN |
---|
[1] | 1987 | ! |
---|
[63] | 1988 | !-- Bott-Chlond scheme always uses Euler time step when leapfrog is |
---|
| 1989 | !-- switched on. Thus: |
---|
| 1990 | sat = 1.0 |
---|
| 1991 | sbt = 1.0 |
---|
| 1992 | ENDIF |
---|
[1] | 1993 | tend = 0.0 |
---|
| 1994 | CALL advec_s_bc( e, 'e' ) |
---|
| 1995 | ELSE |
---|
| 1996 | IF ( tsc(2) /= 2.0 ) THEN |
---|
| 1997 | IF ( scalar_advec == 'ups-scheme' ) THEN |
---|
| 1998 | tend = 0.0 |
---|
| 1999 | CALL advec_s_ups( e, 'e' ) |
---|
| 2000 | ENDIF |
---|
| 2001 | ENDIF |
---|
| 2002 | ENDIF |
---|
| 2003 | ENDIF |
---|
| 2004 | |
---|
| 2005 | ! |
---|
| 2006 | !-- TKE-tendency terms with no communication |
---|
| 2007 | IF ( scalar_advec == 'bc-scheme' .AND. .NOT. use_upstream_for_tke ) & |
---|
| 2008 | THEN |
---|
[75] | 2009 | IF ( .NOT. humidity ) THEN |
---|
[97] | 2010 | IF ( ocean ) THEN |
---|
[388] | 2011 | CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, & |
---|
| 2012 | prho, prho_reference, rif, tend, zu, zw ) |
---|
[97] | 2013 | ELSE |
---|
| 2014 | CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, pt, & |
---|
| 2015 | pt_reference, rif, tend, zu, zw ) |
---|
| 2016 | ENDIF |
---|
[1] | 2017 | ELSE |
---|
| 2018 | CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, vpt, & |
---|
[97] | 2019 | pt_reference, rif, tend, zu, zw ) |
---|
[1] | 2020 | ENDIF |
---|
| 2021 | ELSE |
---|
| 2022 | IF ( use_upstream_for_tke ) THEN |
---|
| 2023 | tend = 0.0 |
---|
| 2024 | CALL advec_s_up( e ) |
---|
| 2025 | ELSE |
---|
| 2026 | IF ( tsc(2) == 2.0 .OR. timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 2027 | tend = 0.0 |
---|
| 2028 | CALL advec_s_pw( e ) |
---|
| 2029 | ELSE |
---|
| 2030 | IF ( scalar_advec /= 'ups-scheme' ) THEN |
---|
| 2031 | tend = 0.0 |
---|
| 2032 | CALL advec_s_up( e ) |
---|
| 2033 | ENDIF |
---|
| 2034 | ENDIF |
---|
| 2035 | ENDIF |
---|
| 2036 | IF ( tsc(2) == 2.0 .AND. timestep_scheme(1:8) == 'leapfrog' ) THEN |
---|
[75] | 2037 | IF ( .NOT. humidity ) THEN |
---|
[1] | 2038 | CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e_m, km_m, l_grid, & |
---|
[97] | 2039 | pt_m, pt_reference, rif_m, tend, zu, zw ) |
---|
[1] | 2040 | ELSE |
---|
| 2041 | CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e_m, km_m, l_grid, & |
---|
[97] | 2042 | vpt_m, pt_reference, rif_m, tend, zu, zw ) |
---|
[1] | 2043 | ENDIF |
---|
| 2044 | ELSE |
---|
[75] | 2045 | IF ( .NOT. humidity ) THEN |
---|
[97] | 2046 | IF ( ocean ) THEN |
---|
| 2047 | CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, & |
---|
[388] | 2048 | prho, prho_reference, rif, tend, zu, zw ) |
---|
[97] | 2049 | ELSE |
---|
| 2050 | CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, & |
---|
| 2051 | pt, pt_reference, rif, tend, zu, zw ) |
---|
| 2052 | ENDIF |
---|
[1] | 2053 | ELSE |
---|
| 2054 | CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, vpt, & |
---|
[97] | 2055 | pt_reference, rif, tend, zu, zw ) |
---|
[1] | 2056 | ENDIF |
---|
| 2057 | ENDIF |
---|
| 2058 | ENDIF |
---|
| 2059 | CALL production_e |
---|
[138] | 2060 | |
---|
| 2061 | ! |
---|
| 2062 | !-- Additional sink term for flows through plant canopies |
---|
[153] | 2063 | IF ( plant_canopy ) CALL plant_canopy_model( 6 ) |
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[1] | 2064 | CALL user_actions( 'e-tendency' ) |
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| 2065 | |
---|
| 2066 | ! |
---|
| 2067 | !-- Prognostic equation for TKE. |
---|
| 2068 | !-- Eliminate negative TKE values, which can occur due to numerical |
---|
| 2069 | !-- reasons in the course of the integration. In such cases the old TKE |
---|
| 2070 | !-- value is reduced by 90%. |
---|
| 2071 | DO i = nxl, nxr |
---|
| 2072 | DO j = nys, nyn |
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[19] | 2073 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 2074 | e_p(k,j,i) = ( 1 - sat ) * e_m(k,j,i) + sat * e(k,j,i) + & |
---|
| 2075 | dt_3d * ( & |
---|
| 2076 | sbt * tend(k,j,i) + tsc(3) * te_m(k,j,i) & |
---|
| 2077 | ) |
---|
| 2078 | IF ( e_p(k,j,i) < 0.0 ) e_p(k,j,i) = 0.1 * e(k,j,i) |
---|
| 2079 | ENDDO |
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| 2080 | ENDDO |
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| 2081 | ENDDO |
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| 2082 | |
---|
| 2083 | ! |
---|
| 2084 | !-- Calculate tendencies for the next Runge-Kutta step |
---|
| 2085 | IF ( timestep_scheme(1:5) == 'runge' ) THEN |
---|
| 2086 | IF ( intermediate_timestep_count == 1 ) THEN |
---|
| 2087 | DO i = nxl, nxr |
---|
| 2088 | DO j = nys, nyn |
---|
[19] | 2089 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 2090 | te_m(k,j,i) = tend(k,j,i) |
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| 2091 | ENDDO |
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| 2092 | ENDDO |
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| 2093 | ENDDO |
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| 2094 | ELSEIF ( intermediate_timestep_count < & |
---|
| 2095 | intermediate_timestep_count_max ) THEN |
---|
| 2096 | DO i = nxl, nxr |
---|
| 2097 | DO j = nys, nyn |
---|
[19] | 2098 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
[1] | 2099 | te_m(k,j,i) = -9.5625 * tend(k,j,i) + 5.3125 * te_m(k,j,i) |
---|
| 2100 | ENDDO |
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| 2101 | ENDDO |
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| 2102 | ENDDO |
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| 2103 | ENDIF |
---|
| 2104 | ENDIF |
---|
| 2105 | |
---|
| 2106 | CALL cpu_log( log_point(16), 'tke-equation', 'stop' ) |
---|
| 2107 | |
---|
| 2108 | ENDIF |
---|
| 2109 | |
---|
| 2110 | |
---|
[63] | 2111 | END SUBROUTINE prognostic_equations_vector |
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[1] | 2112 | |
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| 2113 | |
---|
| 2114 | END MODULE prognostic_equations_mod |
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