[411] | 1 | MODULE subsidence_mod |
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| 2 | |
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[1036] | 3 | !--------------------------------------------------------------------------------! |
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| 4 | ! This file is part of PALM. |
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| 5 | ! |
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| 6 | ! PALM is free software: you can redistribute it and/or modify it under the terms |
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| 7 | ! of the GNU General Public License as published by the Free Software Foundation, |
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| 8 | ! either version 3 of the License, or (at your option) any later version. |
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| 9 | ! |
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| 10 | ! PALM is distributed in the hope that it will be useful, but WITHOUT ANY |
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| 11 | ! WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR |
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| 12 | ! A PARTICULAR PURPOSE. See the GNU General Public License for more details. |
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| 13 | ! |
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| 14 | ! You should have received a copy of the GNU General Public License along with |
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| 15 | ! PALM. If not, see <http://www.gnu.org/licenses/>. |
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| 16 | ! |
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[1310] | 17 | ! Copyright 1997-2014 Leibniz Universitaet Hannover |
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[1036] | 18 | !--------------------------------------------------------------------------------! |
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| 19 | ! |
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[411] | 20 | ! Current revisions: |
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| 21 | ! ----------------- |
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[1365] | 22 | ! Summation of subsidence tendencies for data output added |
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| 23 | ! +ls_index, sums_ls_l, tmp_tend |
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[1321] | 24 | ! |
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| 25 | ! Former revisions: |
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| 26 | ! ----------------- |
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| 27 | ! $Id: subsidence.f90 1365 2014-04-22 15:03:56Z boeske $ |
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| 28 | ! |
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[1354] | 29 | ! 1353 2014-04-08 15:21:23Z heinze |
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| 30 | ! REAL constants provided with KIND-attribute |
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| 31 | ! |
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[1321] | 32 | ! 1320 2014-03-20 08:40:49Z raasch |
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[1320] | 33 | ! ONLY-attribute added to USE-statements, |
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| 34 | ! kind-parameters added to all INTEGER and REAL declaration statements, |
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| 35 | ! kinds are defined in new module kinds, |
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| 36 | ! old module precision_kind is removed, |
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| 37 | ! revision history before 2012 removed, |
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| 38 | ! comment fields (!:) to be used for variable explanations added to |
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| 39 | ! all variable declaration statements |
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[411] | 40 | ! |
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[1037] | 41 | ! 1036 2012-10-22 13:43:42Z raasch |
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| 42 | ! code put under GPL (PALM 3.9) |
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| 43 | ! |
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[464] | 44 | ! Revision 3.7 2009-12-11 14:15:58Z heinze |
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| 45 | ! Initial revision |
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[411] | 46 | ! |
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| 47 | ! Description: |
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| 48 | ! ------------ |
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| 49 | ! Impact of large-scale subsidence or ascent as tendency term for use |
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| 50 | ! in the prognostic equation of potential temperature. This enables the |
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| 51 | ! construction of a constant boundary layer height z_i with time. |
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| 52 | !-----------------------------------------------------------------------------! |
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| 53 | |
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| 54 | |
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| 55 | IMPLICIT NONE |
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| 56 | |
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| 57 | PRIVATE |
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| 58 | PUBLIC init_w_subsidence, subsidence |
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| 59 | |
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| 60 | INTERFACE init_w_subsidence |
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| 61 | MODULE PROCEDURE init_w_subsidence |
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| 62 | END INTERFACE init_w_subsidence |
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| 63 | |
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| 64 | INTERFACE subsidence |
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| 65 | MODULE PROCEDURE subsidence |
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| 66 | MODULE PROCEDURE subsidence_ij |
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| 67 | END INTERFACE subsidence |
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| 68 | |
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| 69 | CONTAINS |
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| 70 | |
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| 71 | SUBROUTINE init_w_subsidence |
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| 72 | |
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[1320] | 73 | USE arrays_3d, & |
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| 74 | ONLY: dzu, w_subs, zu |
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[411] | 75 | |
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[1320] | 76 | USE control_parameters, & |
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| 77 | ONLY: message_string, ocean, subs_vertical_gradient, & |
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| 78 | subs_vertical_gradient_level, subs_vertical_gradient_level_i |
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| 79 | |
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| 80 | USE indices, & |
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| 81 | ONLY: nzb, nzt |
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| 82 | |
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| 83 | USE kinds |
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| 84 | |
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[411] | 85 | IMPLICIT NONE |
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| 86 | |
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[1320] | 87 | INTEGER(iwp) :: i !: |
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| 88 | INTEGER(iwp) :: k !: |
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[411] | 89 | |
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[1320] | 90 | REAL(wp) :: gradient !: |
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| 91 | REAL(wp) :: ws_surface !: |
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| 92 | |
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[1365] | 93 | IF ( .NOT. ALLOCATED( w_subs )) THEN |
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[411] | 94 | ALLOCATE( w_subs(nzb:nzt+1) ) |
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[1353] | 95 | w_subs = 0.0_wp |
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[411] | 96 | ENDIF |
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| 97 | |
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[1365] | 98 | IF ( ocean ) THEN |
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[411] | 99 | message_string = 'Applying large scale vertical motion is not ' // & |
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| 100 | 'allowed for ocean runs' |
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| 101 | CALL message( 'init_w_subsidence', 'PA0324', 2, 2, 0, 6, 0 ) |
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| 102 | ENDIF |
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| 103 | |
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| 104 | ! |
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| 105 | !-- Compute the profile of the subsidence/ascent velocity |
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| 106 | !-- using the given gradients |
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| 107 | i = 1 |
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[1353] | 108 | gradient = 0.0_wp |
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| 109 | ws_surface = 0.0_wp |
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[411] | 110 | |
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| 111 | |
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[580] | 112 | subs_vertical_gradient_level_i(1) = 0 |
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[411] | 113 | DO k = 1, nzt+1 |
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[1365] | 114 | IF ( i < 11 ) THEN |
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[580] | 115 | IF ( subs_vertical_gradient_level(i) < zu(k) .AND. & |
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[1353] | 116 | subs_vertical_gradient_level(i) >= 0.0_wp ) THEN |
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| 117 | gradient = subs_vertical_gradient(i) / 100.0_wp |
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[580] | 118 | subs_vertical_gradient_level_i(i) = k - 1 |
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[411] | 119 | i = i + 1 |
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| 120 | ENDIF |
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| 121 | ENDIF |
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[1353] | 122 | IF ( gradient /= 0.0_wp ) THEN |
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[411] | 123 | IF ( k /= 1 ) THEN |
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| 124 | w_subs(k) = w_subs(k-1) + dzu(k) * gradient |
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| 125 | ELSE |
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[1353] | 126 | w_subs(k) = ws_surface + 0.5_wp * dzu(k) * gradient |
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[411] | 127 | ENDIF |
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| 128 | ELSE |
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| 129 | w_subs(k) = w_subs(k-1) |
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| 130 | ENDIF |
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| 131 | ENDDO |
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| 132 | |
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| 133 | ! |
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| 134 | !-- In case of no given gradients for the subsidence/ascent velocity, |
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| 135 | !-- choose zero gradient |
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[1353] | 136 | IF ( subs_vertical_gradient_level(1) == -9999999.9_wp ) THEN |
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| 137 | subs_vertical_gradient_level(1) = 0.0_wp |
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[411] | 138 | ENDIF |
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| 139 | |
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| 140 | END SUBROUTINE init_w_subsidence |
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| 141 | |
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| 142 | |
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[1365] | 143 | SUBROUTINE subsidence( tendency, var, var_init, ls_index ) |
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[411] | 144 | |
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[1320] | 145 | USE arrays_3d, & |
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| 146 | ONLY: ddzu, w_subs |
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[411] | 147 | |
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[1320] | 148 | USE control_parameters, & |
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[1365] | 149 | ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing |
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[1320] | 150 | |
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| 151 | USE indices, & |
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| 152 | ONLY: nxl, nxlg, nxr, nxrg, nyn, nyng, nys, nysg, nzb, nzb_s_inner,& |
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| 153 | nzt |
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| 154 | |
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| 155 | USE kinds |
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| 156 | |
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[1365] | 157 | USE statistics, & |
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| 158 | ONLY: sums_ls_l, weight_pres |
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| 159 | |
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[411] | 160 | IMPLICIT NONE |
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| 161 | |
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[1320] | 162 | INTEGER(iwp) :: i !: |
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| 163 | INTEGER(iwp) :: j !: |
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| 164 | INTEGER(iwp) :: k !: |
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[1365] | 165 | INTEGER(iwp) :: ls_index !: |
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[411] | 166 | |
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[1365] | 167 | REAL(wp) :: tmp_tend !: |
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[1320] | 168 | REAL(wp) :: tmp_grad !: |
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[411] | 169 | |
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[1320] | 170 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !: |
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| 171 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !: |
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| 172 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !: |
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| 173 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !: |
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[411] | 174 | |
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[464] | 175 | var_mod = var_init |
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[411] | 176 | |
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| 177 | ! |
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| 178 | !-- Influence of w_subsidence on the current tendency term |
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| 179 | DO i = nxl, nxr |
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| 180 | DO j = nys, nyn |
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| 181 | DO k = nzb_s_inner(j,i)+1, nzt |
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[1365] | 182 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 183 | tmp_tend = - w_subs(k) * & |
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| 184 | ( var(k+1,j,i) - var(k,j,i) ) * ddzu(k+1) |
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| 185 | ELSE ! large-scale ascent |
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| 186 | tmp_tend = - w_subs(k) * & |
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| 187 | ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) |
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[411] | 188 | ENDIF |
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[1365] | 189 | |
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| 190 | tendency(k,j,i) = tendency(k,j,i) + tmp_tend |
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| 191 | |
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| 192 | IF ( large_scale_forcing ) THEN |
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| 193 | sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend & |
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| 194 | * weight_pres(intermediate_timestep_count) |
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| 195 | ENDIF |
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[411] | 196 | ENDDO |
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| 197 | ENDDO |
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| 198 | ENDDO |
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| 199 | |
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| 200 | ! |
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| 201 | !-- Shifting of the initial profile is especially necessary with Rayleigh |
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| 202 | !-- damping switched on |
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| 203 | |
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| 204 | DO k = nzb, nzt |
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[1365] | 205 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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[411] | 206 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 207 | ( var_init(k+1) - var_init(k) ) * ddzu(k+1) |
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| 208 | ENDIF |
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| 209 | ENDDO |
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| 210 | ! |
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| 211 | !-- At the upper boundary, the initial profile is shifted with aid of |
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| 212 | !-- the gradient tmp_grad. (This is ok if the gradients are linear.) |
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[1365] | 213 | IF ( w_subs(nzt) < 0.0_wp ) THEN |
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[411] | 214 | tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1) |
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| 215 | var_mod(nzt+1) = var_init(nzt+1) - & |
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| 216 | dt_3d * w_subs(nzt+1) * tmp_grad |
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| 217 | ENDIF |
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| 218 | |
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| 219 | |
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| 220 | DO k = nzt+1, nzb+1, -1 |
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[1365] | 221 | IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent |
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[411] | 222 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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[671] | 223 | ( var_init(k) - var_init(k-1) ) * ddzu(k) |
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[411] | 224 | ENDIF |
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| 225 | ENDDO |
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| 226 | ! |
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| 227 | !-- At the lower boundary shifting is not necessary because the |
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| 228 | !-- subsidence velocity w_subs(nzb) vanishes. |
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[1365] | 229 | IF ( w_subs(nzb+1) >= 0.0_wp ) THEN |
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[411] | 230 | var_mod(nzb) = var_init(nzb) |
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| 231 | ENDIF |
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| 232 | |
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| 233 | var_init = var_mod |
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| 234 | |
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| 235 | |
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| 236 | END SUBROUTINE subsidence |
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| 237 | |
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[1365] | 238 | SUBROUTINE subsidence_ij( i, j, tendency, var, var_init, ls_index ) |
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[411] | 239 | |
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[1320] | 240 | USE arrays_3d, & |
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| 241 | ONLY: ddzu, w_subs |
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[411] | 242 | |
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[1320] | 243 | USE control_parameters, & |
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[1365] | 244 | ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing |
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[1320] | 245 | |
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| 246 | USE indices, & |
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| 247 | ONLY: nxl, nxlg, nxrg, nyng, nys, nysg, nzb_s_inner, nzb, nzt |
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| 248 | |
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| 249 | USE kinds |
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| 250 | |
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[1365] | 251 | USE statistics, & |
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| 252 | ONLY: sums_ls_l, weight_pres |
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| 253 | |
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[411] | 254 | IMPLICIT NONE |
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| 255 | |
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[1320] | 256 | INTEGER(iwp) :: i !: |
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| 257 | INTEGER(iwp) :: j !: |
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| 258 | INTEGER(iwp) :: k !: |
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[1365] | 259 | INTEGER(iwp) :: ls_index !: |
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[411] | 260 | |
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[1365] | 261 | REAL(wp) :: tmp_tend !: |
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[1320] | 262 | REAL(wp) :: tmp_grad !: |
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[411] | 263 | |
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[1320] | 264 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !: |
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| 265 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !: |
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| 266 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !: |
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| 267 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !: |
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[411] | 268 | |
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[464] | 269 | var_mod = var_init |
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[411] | 270 | |
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| 271 | ! |
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| 272 | !-- Influence of w_subsidence on the current tendency term |
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| 273 | DO k = nzb_s_inner(j,i)+1, nzt |
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[1365] | 274 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 275 | tmp_tend = - w_subs(k) * ( var(k+1,j,i) - var(k,j,i) ) * ddzu(k+1) |
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| 276 | ELSE ! large-scale ascent |
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| 277 | tmp_tend = - w_subs(k) * ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) |
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[411] | 278 | ENDIF |
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[1365] | 279 | |
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| 280 | tendency(k,j,i) = tendency(k,j,i) + tmp_tend |
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| 281 | |
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| 282 | IF ( large_scale_forcing ) THEN |
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| 283 | sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend & |
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| 284 | * weight_pres(intermediate_timestep_count) |
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| 285 | ENDIF |
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[411] | 286 | ENDDO |
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| 287 | |
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| 288 | |
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| 289 | ! |
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| 290 | !-- Shifting of the initial profile is especially necessary with Rayleigh |
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| 291 | !-- damping switched on |
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[1365] | 292 | IF ( i == nxl .AND. j == nys ) THEN ! shifting only once per PE |
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[411] | 293 | |
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| 294 | DO k = nzb, nzt |
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[1365] | 295 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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[411] | 296 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 297 | ( var_init(k+1) - var_init(k) ) * ddzu(k+1) |
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| 298 | ENDIF |
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| 299 | ENDDO |
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| 300 | ! |
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| 301 | !-- At the upper boundary, the initial profile is shifted with aid of |
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| 302 | !-- the gradient tmp_grad. (This is ok if the gradients are linear.) |
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[1365] | 303 | IF ( w_subs(nzt) < 0.0_wp ) THEN |
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[411] | 304 | tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1) |
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| 305 | var_mod(nzt+1) = var_init(nzt+1) - & |
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| 306 | dt_3d * w_subs(nzt+1) * tmp_grad |
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| 307 | ENDIF |
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| 308 | |
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| 309 | |
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| 310 | DO k = nzt+1, nzb+1, -1 |
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[1365] | 311 | IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent |
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[411] | 312 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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[671] | 313 | ( var_init(k) - var_init(k-1) ) * ddzu(k) |
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[411] | 314 | ENDIF |
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| 315 | ENDDO |
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| 316 | ! |
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| 317 | !-- At the lower boundary shifting is not necessary because the |
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| 318 | !-- subsidence velocity w_subs(nzb) vanishes. |
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[1365] | 319 | IF ( w_subs(nzb+1) >= 0.0_wp ) THEN |
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[411] | 320 | var_mod(nzb) = var_init(nzb) |
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| 321 | ENDIF |
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| 322 | |
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[464] | 323 | var_init = var_mod |
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[411] | 324 | |
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| 325 | ENDIF |
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| 326 | |
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| 327 | END SUBROUTINE subsidence_ij |
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| 328 | |
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| 329 | |
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| 330 | END MODULE subsidence_mod |
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