[1850] | 1 | !> @file subsidence_mod.f90 |
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[2000] | 2 | !------------------------------------------------------------------------------! |
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[2696] | 3 | ! This file is part of the PALM model system. |
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[1036] | 4 | ! |
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[2000] | 5 | ! PALM is free software: you can redistribute it and/or modify it under the |
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| 6 | ! terms of the GNU General Public License as published by the Free Software |
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| 7 | ! Foundation, either version 3 of the License, or (at your option) any later |
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| 8 | ! version. |
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[1036] | 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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[4360] | 17 | ! Copyright 1997-2020 Leibniz Universitaet Hannover |
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[2000] | 18 | !------------------------------------------------------------------------------! |
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[1036] | 19 | ! |
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[411] | 20 | ! Current revisions: |
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| 21 | ! ----------------- |
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[1683] | 22 | ! |
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[2233] | 23 | ! |
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[1383] | 24 | ! Former revisions: |
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| 25 | ! ----------------- |
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| 26 | ! $Id: subsidence_mod.f90 4360 2020-01-07 11:25:50Z schwenkel $ |
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[4346] | 27 | ! Introduction of wall_flags_total_0, which currently sets bits based on static |
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| 28 | ! topography information used in wall_flags_static_0 |
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| 29 | ! |
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| 30 | ! 4329 2019-12-10 15:46:36Z motisi |
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[4329] | 31 | ! Renamed wall_flags_0 to wall_flags_static_0 |
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| 32 | ! |
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| 33 | ! 4182 2019-08-22 15:20:23Z scharf |
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[4182] | 34 | ! Corrected "Former revisions" section |
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| 35 | ! |
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| 36 | ! 3655 2019-01-07 16:51:22Z knoop |
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[3554] | 37 | ! add subroutine and variable description |
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[1383] | 38 | ! |
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[4182] | 39 | ! Revision 3.7 2009-12-11 14:15:58Z heinze |
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| 40 | ! Initial revision |
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| 41 | ! |
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[411] | 42 | ! Description: |
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| 43 | ! ------------ |
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[1682] | 44 | !> Impact of large-scale subsidence or ascent as tendency term for use |
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| 45 | !> in the prognostic equation of potential temperature. This enables the |
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| 46 | !> construction of a constant boundary layer height z_i with time. |
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[411] | 47 | !-----------------------------------------------------------------------------! |
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[1682] | 48 | MODULE subsidence_mod |
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| 49 | |
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[411] | 50 | |
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| 51 | |
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| 52 | IMPLICIT NONE |
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| 53 | |
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| 54 | PRIVATE |
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| 55 | PUBLIC init_w_subsidence, subsidence |
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| 56 | |
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| 57 | INTERFACE init_w_subsidence |
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| 58 | MODULE PROCEDURE init_w_subsidence |
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| 59 | END INTERFACE init_w_subsidence |
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| 60 | |
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| 61 | INTERFACE subsidence |
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| 62 | MODULE PROCEDURE subsidence |
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| 63 | MODULE PROCEDURE subsidence_ij |
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| 64 | END INTERFACE subsidence |
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| 65 | |
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| 66 | CONTAINS |
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| 67 | |
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[1682] | 68 | !------------------------------------------------------------------------------! |
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| 69 | ! Description: |
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| 70 | ! ------------ |
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[3554] | 71 | !> Initialize vertical subsidence velocity w_subs. |
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[1682] | 72 | !------------------------------------------------------------------------------! |
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[411] | 73 | SUBROUTINE init_w_subsidence |
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| 74 | |
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[1320] | 75 | USE arrays_3d, & |
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| 76 | ONLY: dzu, w_subs, zu |
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[411] | 77 | |
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[1320] | 78 | USE control_parameters, & |
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[3294] | 79 | ONLY: message_string, ocean_mode, subs_vertical_gradient, & |
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[1320] | 80 | subs_vertical_gradient_level, subs_vertical_gradient_level_i |
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| 81 | |
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| 82 | USE indices, & |
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| 83 | ONLY: nzb, nzt |
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| 84 | |
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| 85 | USE kinds |
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| 86 | |
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[411] | 87 | IMPLICIT NONE |
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| 88 | |
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[3554] | 89 | INTEGER(iwp) :: i !< loop index |
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| 90 | INTEGER(iwp) :: k !< loop index |
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[411] | 91 | |
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[3554] | 92 | REAL(wp) :: gradient !< vertical gradient of subsidence velocity |
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| 93 | REAL(wp) :: ws_surface !< subsidence velocity at the surface |
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[1320] | 94 | |
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[1862] | 95 | IF ( .NOT. ALLOCATED( w_subs ) ) THEN |
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[411] | 96 | ALLOCATE( w_subs(nzb:nzt+1) ) |
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[1353] | 97 | w_subs = 0.0_wp |
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[411] | 98 | ENDIF |
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| 99 | |
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[3294] | 100 | IF ( ocean_mode ) THEN |
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[3302] | 101 | message_string = 'applying large scale vertical motion is not ' // & |
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[3294] | 102 | 'allowed for ocean mode' |
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[411] | 103 | CALL message( 'init_w_subsidence', 'PA0324', 2, 2, 0, 6, 0 ) |
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| 104 | ENDIF |
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| 105 | |
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| 106 | ! |
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| 107 | !-- Compute the profile of the subsidence/ascent velocity |
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| 108 | !-- using the given gradients |
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| 109 | i = 1 |
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[1353] | 110 | gradient = 0.0_wp |
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| 111 | ws_surface = 0.0_wp |
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[411] | 112 | |
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| 113 | |
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[580] | 114 | subs_vertical_gradient_level_i(1) = 0 |
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[411] | 115 | DO k = 1, nzt+1 |
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[1365] | 116 | IF ( i < 11 ) THEN |
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[580] | 117 | IF ( subs_vertical_gradient_level(i) < zu(k) .AND. & |
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[1353] | 118 | subs_vertical_gradient_level(i) >= 0.0_wp ) THEN |
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| 119 | gradient = subs_vertical_gradient(i) / 100.0_wp |
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[580] | 120 | subs_vertical_gradient_level_i(i) = k - 1 |
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[411] | 121 | i = i + 1 |
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| 122 | ENDIF |
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| 123 | ENDIF |
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[1353] | 124 | IF ( gradient /= 0.0_wp ) THEN |
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[411] | 125 | IF ( k /= 1 ) THEN |
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| 126 | w_subs(k) = w_subs(k-1) + dzu(k) * gradient |
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| 127 | ELSE |
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[1353] | 128 | w_subs(k) = ws_surface + 0.5_wp * dzu(k) * gradient |
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[411] | 129 | ENDIF |
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| 130 | ELSE |
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| 131 | w_subs(k) = w_subs(k-1) |
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| 132 | ENDIF |
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| 133 | ENDDO |
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| 134 | |
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| 135 | ! |
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| 136 | !-- In case of no given gradients for the subsidence/ascent velocity, |
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| 137 | !-- choose zero gradient |
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[1353] | 138 | IF ( subs_vertical_gradient_level(1) == -9999999.9_wp ) THEN |
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| 139 | subs_vertical_gradient_level(1) = 0.0_wp |
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[411] | 140 | ENDIF |
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| 141 | |
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| 142 | END SUBROUTINE init_w_subsidence |
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| 143 | |
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| 144 | |
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[1682] | 145 | !------------------------------------------------------------------------------! |
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| 146 | ! Description: |
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| 147 | ! ------------ |
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[3554] | 148 | !> Add effect of large-scale subsidence to variable. |
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[1682] | 149 | !------------------------------------------------------------------------------! |
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[1365] | 150 | SUBROUTINE subsidence( tendency, var, var_init, ls_index ) |
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[411] | 151 | |
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[1320] | 152 | USE arrays_3d, & |
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| 153 | ONLY: ddzu, w_subs |
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[411] | 154 | |
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[1320] | 155 | USE control_parameters, & |
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[1380] | 156 | ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing, & |
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| 157 | scalar_rayleigh_damping |
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[1320] | 158 | |
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| 159 | USE indices, & |
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[2232] | 160 | ONLY: nxl, nxlg, nxr, nxrg, nyn, nyng, nys, nysg, nzb, nzt, & |
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[4346] | 161 | wall_flags_total_0 |
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[1320] | 162 | |
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| 163 | USE kinds |
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| 164 | |
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[1365] | 165 | USE statistics, & |
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[1382] | 166 | ONLY: sums_ls_l, weight_substep |
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[1365] | 167 | |
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[411] | 168 | IMPLICIT NONE |
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| 169 | |
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[3554] | 170 | INTEGER(iwp) :: i !< loop index |
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| 171 | INTEGER(iwp) :: j !< loop index |
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| 172 | INTEGER(iwp) :: k !< loop index |
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| 173 | INTEGER(iwp) :: ls_index !< index of large-scale subsidence in sums_ls_l |
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[411] | 174 | |
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[3554] | 175 | REAL(wp) :: tmp_tend !< temporary tendency |
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| 176 | REAL(wp) :: tmp_grad !< temporary gradient |
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[411] | 177 | |
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[3554] | 178 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !< variable where to add subsidence |
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| 179 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !< tendency of var |
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| 180 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !< initialization profile of var |
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| 181 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !< modified profile of var |
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[411] | 182 | |
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[464] | 183 | var_mod = var_init |
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[411] | 184 | |
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| 185 | ! |
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| 186 | !-- Influence of w_subsidence on the current tendency term |
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| 187 | DO i = nxl, nxr |
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| 188 | DO j = nys, nyn |
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[1382] | 189 | |
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[2232] | 190 | DO k = nzb+1, nzt |
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[1365] | 191 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 192 | tmp_tend = - w_subs(k) * & |
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[2232] | 193 | ( var(k+1,j,i) - var(k,j,i) ) * ddzu(k+1) * & |
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| 194 | MERGE( 1.0_wp, 0.0_wp, & |
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[4346] | 195 | BTEST( wall_flags_total_0(k,j,i), 0 ) ) |
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[1365] | 196 | ELSE ! large-scale ascent |
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| 197 | tmp_tend = - w_subs(k) * & |
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[2232] | 198 | ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) * & |
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| 199 | MERGE( 1.0_wp, 0.0_wp, & |
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[4346] | 200 | BTEST( wall_flags_total_0(k,j,i), 0 ) ) |
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[411] | 201 | ENDIF |
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[1365] | 202 | |
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| 203 | tendency(k,j,i) = tendency(k,j,i) + tmp_tend |
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| 204 | |
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| 205 | IF ( large_scale_forcing ) THEN |
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| 206 | sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend & |
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[2232] | 207 | * weight_substep(intermediate_timestep_count) & |
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| 208 | * MERGE( 1.0_wp, 0.0_wp, & |
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[4346] | 209 | BTEST( wall_flags_total_0(k,j,i), 0 ) ) |
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[1365] | 210 | ENDIF |
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[411] | 211 | ENDDO |
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[1382] | 212 | |
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[1862] | 213 | IF ( large_scale_forcing ) THEN |
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| 214 | sums_ls_l(nzt+1,ls_index) = sums_ls_l(nzt,ls_index) |
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| 215 | ENDIF |
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[1382] | 216 | |
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[411] | 217 | ENDDO |
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| 218 | ENDDO |
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| 219 | |
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| 220 | ! |
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| 221 | !-- Shifting of the initial profile is especially necessary with Rayleigh |
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| 222 | !-- damping switched on |
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[1729] | 223 | IF ( scalar_rayleigh_damping .AND. & |
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| 224 | intermediate_timestep_count == 1 ) THEN |
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[1380] | 225 | DO k = nzb, nzt |
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| 226 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 227 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 228 | ( var_init(k+1) - var_init(k) ) * ddzu(k+1) |
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| 229 | ENDIF |
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| 230 | ENDDO |
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[411] | 231 | ! |
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[1380] | 232 | !-- At the upper boundary, the initial profile is shifted with aid of |
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| 233 | !-- the gradient tmp_grad. (This is ok if the gradients are linear.) |
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| 234 | IF ( w_subs(nzt) < 0.0_wp ) THEN |
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| 235 | tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1) |
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| 236 | var_mod(nzt+1) = var_init(nzt+1) - & |
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| 237 | dt_3d * w_subs(nzt+1) * tmp_grad |
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| 238 | ENDIF |
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[411] | 239 | |
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| 240 | |
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[1380] | 241 | DO k = nzt+1, nzb+1, -1 |
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| 242 | IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent |
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| 243 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 244 | ( var_init(k) - var_init(k-1) ) * ddzu(k) |
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| 245 | ENDIF |
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| 246 | ENDDO |
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| 247 | ! |
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| 248 | !-- At the lower boundary shifting is not necessary because the |
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| 249 | !-- subsidence velocity w_subs(nzb) vanishes. |
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| 250 | IF ( w_subs(nzb+1) >= 0.0_wp ) THEN |
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| 251 | var_mod(nzb) = var_init(nzb) |
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[411] | 252 | ENDIF |
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[1380] | 253 | |
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| 254 | var_init = var_mod |
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[411] | 255 | ENDIF |
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| 256 | |
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| 257 | |
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| 258 | END SUBROUTINE subsidence |
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| 259 | |
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[1682] | 260 | !------------------------------------------------------------------------------! |
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| 261 | ! Description: |
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| 262 | ! ------------ |
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[3554] | 263 | !> Add effect of large-scale subsidence to variable. |
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[1682] | 264 | !------------------------------------------------------------------------------! |
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[1365] | 265 | SUBROUTINE subsidence_ij( i, j, tendency, var, var_init, ls_index ) |
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[411] | 266 | |
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[1320] | 267 | USE arrays_3d, & |
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| 268 | ONLY: ddzu, w_subs |
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[411] | 269 | |
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[1320] | 270 | USE control_parameters, & |
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[1380] | 271 | ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing, & |
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| 272 | scalar_rayleigh_damping |
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[1320] | 273 | |
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| 274 | USE indices, & |
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[4346] | 275 | ONLY: nxl, nxlg, nxrg, nyng, nys, nysg, nzb, nzt, & |
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| 276 | wall_flags_total_0 |
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[1320] | 277 | |
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| 278 | USE kinds |
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| 279 | |
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[1365] | 280 | USE statistics, & |
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[1382] | 281 | ONLY: sums_ls_l, weight_substep |
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[1365] | 282 | |
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[411] | 283 | IMPLICIT NONE |
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| 284 | |
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[3554] | 285 | INTEGER(iwp) :: i !< loop variable |
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| 286 | INTEGER(iwp) :: j !< loop variable |
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| 287 | INTEGER(iwp) :: k !< loop variable |
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| 288 | INTEGER(iwp) :: ls_index !< index of large-scale subsidence in sums_ls_l |
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[411] | 289 | |
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[3554] | 290 | REAL(wp) :: tmp_tend !< temporary tendency |
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| 291 | REAL(wp) :: tmp_grad !< temporary gradient |
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[411] | 292 | |
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[3554] | 293 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !< variable where to add subsidence |
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| 294 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !< tendency of var |
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| 295 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !< initialization profile of var |
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| 296 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !< modified profile of var |
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[411] | 297 | |
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[464] | 298 | var_mod = var_init |
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[411] | 299 | |
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| 300 | ! |
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| 301 | !-- Influence of w_subsidence on the current tendency term |
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[2232] | 302 | DO k = nzb+1, nzt |
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[1365] | 303 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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[2232] | 304 | tmp_tend = - w_subs(k) * ( var(k+1,j,i) - var(k,j,i) ) & |
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| 305 | * ddzu(k+1) & |
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| 306 | * MERGE( 1.0_wp, 0.0_wp, & |
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[4346] | 307 | BTEST( wall_flags_total_0(k,j,i), 0 ) ) |
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[1365] | 308 | ELSE ! large-scale ascent |
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[2232] | 309 | tmp_tend = - w_subs(k) * ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) & |
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| 310 | * MERGE( 1.0_wp, 0.0_wp, & |
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[4346] | 311 | BTEST( wall_flags_total_0(k,j,i), 0 ) ) |
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[411] | 312 | ENDIF |
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[1365] | 313 | |
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| 314 | tendency(k,j,i) = tendency(k,j,i) + tmp_tend |
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| 315 | |
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| 316 | IF ( large_scale_forcing ) THEN |
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| 317 | sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend & |
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[2232] | 318 | * weight_substep(intermediate_timestep_count)& |
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| 319 | * MERGE( 1.0_wp, 0.0_wp, & |
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[4346] | 320 | BTEST( wall_flags_total_0(k,j,i), 0 ) ) |
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[1365] | 321 | ENDIF |
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[411] | 322 | ENDDO |
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| 323 | |
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[1489] | 324 | IF ( large_scale_forcing ) THEN |
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| 325 | sums_ls_l(nzt+1,ls_index) = sums_ls_l(nzt,ls_index) |
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| 326 | ENDIF |
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[411] | 327 | |
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| 328 | ! |
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| 329 | !-- Shifting of the initial profile is especially necessary with Rayleigh |
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| 330 | !-- damping switched on |
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[1729] | 331 | IF ( scalar_rayleigh_damping .AND. & |
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| 332 | intermediate_timestep_count == 1 ) THEN |
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[1380] | 333 | IF ( i == nxl .AND. j == nys ) THEN ! shifting only once per PE |
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[411] | 334 | |
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[1380] | 335 | DO k = nzb, nzt |
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| 336 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 337 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 338 | ( var_init(k+1) - var_init(k) ) * ddzu(k+1) |
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| 339 | ENDIF |
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| 340 | ENDDO |
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| 341 | ! |
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| 342 | !-- At the upper boundary, the initial profile is shifted with aid of |
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| 343 | !-- the gradient tmp_grad. (This is ok if the gradients are linear.) |
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| 344 | IF ( w_subs(nzt) < 0.0_wp ) THEN |
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| 345 | tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1) |
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| 346 | var_mod(nzt+1) = var_init(nzt+1) - & |
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| 347 | dt_3d * w_subs(nzt+1) * tmp_grad |
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[411] | 348 | ENDIF |
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| 349 | |
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| 350 | |
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[1380] | 351 | DO k = nzt+1, nzb+1, -1 |
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| 352 | IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent |
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| 353 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 354 | ( var_init(k) - var_init(k-1) ) * ddzu(k) |
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| 355 | ENDIF |
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| 356 | ENDDO |
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| 357 | ! |
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| 358 | !-- At the lower boundary shifting is not necessary because the |
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| 359 | !-- subsidence velocity w_subs(nzb) vanishes. |
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| 360 | IF ( w_subs(nzb+1) >= 0.0_wp ) THEN |
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| 361 | var_mod(nzb) = var_init(nzb) |
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[411] | 362 | ENDIF |
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| 363 | |
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[1380] | 364 | var_init = var_mod |
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[411] | 365 | |
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[1380] | 366 | ENDIF |
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[411] | 367 | ENDIF |
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| 368 | |
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| 369 | END SUBROUTINE subsidence_ij |
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| 370 | |
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| 371 | |
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| 372 | END MODULE subsidence_mod |
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