| 1 | MODULE subsidence_mod |
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| 2 | |
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| 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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| 17 | ! Copyright 1997-2014 Leibniz Universitaet Hannover |
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| 18 | !--------------------------------------------------------------------------------! |
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| 19 | ! |
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| 20 | ! Current revisions: |
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| 21 | ! ----------------- |
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| 22 | ! |
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| 23 | ! |
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| 24 | ! Former revisions: |
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| 25 | ! ----------------- |
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| 26 | ! $Id: subsidence.f90 1381 2014-04-28 12:41:59Z heinze $ |
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| 27 | ! |
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| 28 | ! 1380 2014-04-28 12:40:45Z heinze |
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| 29 | ! Shifting only necessary in case of scalar Rayleigh damping |
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| 30 | ! |
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| 31 | ! 1365 2014-04-22 15:03:56Z boeske |
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| 32 | ! Summation of subsidence tendencies for data output added |
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| 33 | ! +ls_index, sums_ls_l, tmp_tend |
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| 34 | ! |
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| 35 | ! 1353 2014-04-08 15:21:23Z heinze |
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| 36 | ! REAL constants provided with KIND-attribute |
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| 37 | ! |
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| 38 | ! 1320 2014-03-20 08:40:49Z raasch |
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| 39 | ! ONLY-attribute added to USE-statements, |
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| 40 | ! kind-parameters added to all INTEGER and REAL declaration statements, |
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| 41 | ! kinds are defined in new module kinds, |
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| 42 | ! old module precision_kind is removed, |
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| 43 | ! revision history before 2012 removed, |
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| 44 | ! comment fields (!:) to be used for variable explanations added to |
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| 45 | ! all variable declaration statements |
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| 46 | ! |
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| 47 | ! 1036 2012-10-22 13:43:42Z raasch |
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| 48 | ! code put under GPL (PALM 3.9) |
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| 49 | ! |
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| 50 | ! Revision 3.7 2009-12-11 14:15:58Z heinze |
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| 51 | ! Initial revision |
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| 52 | ! |
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| 53 | ! Description: |
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| 54 | ! ------------ |
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| 55 | ! Impact of large-scale subsidence or ascent as tendency term for use |
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| 56 | ! in the prognostic equation of potential temperature. This enables the |
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| 57 | ! construction of a constant boundary layer height z_i with time. |
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| 58 | !-----------------------------------------------------------------------------! |
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| 59 | |
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| 60 | |
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| 61 | IMPLICIT NONE |
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| 62 | |
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| 63 | PRIVATE |
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| 64 | PUBLIC init_w_subsidence, subsidence |
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| 65 | |
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| 66 | INTERFACE init_w_subsidence |
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| 67 | MODULE PROCEDURE init_w_subsidence |
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| 68 | END INTERFACE init_w_subsidence |
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| 69 | |
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| 70 | INTERFACE subsidence |
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| 71 | MODULE PROCEDURE subsidence |
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| 72 | MODULE PROCEDURE subsidence_ij |
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| 73 | END INTERFACE subsidence |
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| 74 | |
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| 75 | CONTAINS |
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| 76 | |
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| 77 | SUBROUTINE init_w_subsidence |
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| 78 | |
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| 79 | USE arrays_3d, & |
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| 80 | ONLY: dzu, w_subs, zu |
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| 81 | |
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| 82 | USE control_parameters, & |
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| 83 | ONLY: message_string, ocean, subs_vertical_gradient, & |
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| 84 | subs_vertical_gradient_level, subs_vertical_gradient_level_i |
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| 85 | |
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| 86 | USE indices, & |
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| 87 | ONLY: nzb, nzt |
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| 88 | |
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| 89 | USE kinds |
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| 90 | |
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| 91 | IMPLICIT NONE |
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| 92 | |
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| 93 | INTEGER(iwp) :: i !: |
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| 94 | INTEGER(iwp) :: k !: |
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| 95 | |
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| 96 | REAL(wp) :: gradient !: |
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| 97 | REAL(wp) :: ws_surface !: |
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| 98 | |
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| 99 | IF ( .NOT. ALLOCATED( w_subs )) THEN |
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| 100 | ALLOCATE( w_subs(nzb:nzt+1) ) |
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| 101 | w_subs = 0.0_wp |
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| 102 | ENDIF |
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| 103 | |
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| 104 | IF ( ocean ) THEN |
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| 105 | message_string = 'Applying large scale vertical motion is not ' // & |
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| 106 | 'allowed for ocean runs' |
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| 107 | CALL message( 'init_w_subsidence', 'PA0324', 2, 2, 0, 6, 0 ) |
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| 108 | ENDIF |
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| 109 | |
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| 110 | ! |
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| 111 | !-- Compute the profile of the subsidence/ascent velocity |
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| 112 | !-- using the given gradients |
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| 113 | i = 1 |
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| 114 | gradient = 0.0_wp |
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| 115 | ws_surface = 0.0_wp |
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| 116 | |
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| 117 | |
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| 118 | subs_vertical_gradient_level_i(1) = 0 |
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| 119 | DO k = 1, nzt+1 |
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| 120 | IF ( i < 11 ) THEN |
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| 121 | IF ( subs_vertical_gradient_level(i) < zu(k) .AND. & |
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| 122 | subs_vertical_gradient_level(i) >= 0.0_wp ) THEN |
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| 123 | gradient = subs_vertical_gradient(i) / 100.0_wp |
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| 124 | subs_vertical_gradient_level_i(i) = k - 1 |
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| 125 | i = i + 1 |
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| 126 | ENDIF |
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| 127 | ENDIF |
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| 128 | IF ( gradient /= 0.0_wp ) THEN |
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| 129 | IF ( k /= 1 ) THEN |
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| 130 | w_subs(k) = w_subs(k-1) + dzu(k) * gradient |
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| 131 | ELSE |
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| 132 | w_subs(k) = ws_surface + 0.5_wp * dzu(k) * gradient |
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| 133 | ENDIF |
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| 134 | ELSE |
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| 135 | w_subs(k) = w_subs(k-1) |
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| 136 | ENDIF |
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| 137 | ENDDO |
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| 138 | |
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| 139 | ! |
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| 140 | !-- In case of no given gradients for the subsidence/ascent velocity, |
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| 141 | !-- choose zero gradient |
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| 142 | IF ( subs_vertical_gradient_level(1) == -9999999.9_wp ) THEN |
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| 143 | subs_vertical_gradient_level(1) = 0.0_wp |
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| 144 | ENDIF |
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| 145 | |
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| 146 | END SUBROUTINE init_w_subsidence |
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| 147 | |
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| 148 | |
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| 149 | SUBROUTINE subsidence( tendency, var, var_init, ls_index ) |
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| 150 | |
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| 151 | USE arrays_3d, & |
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| 152 | ONLY: ddzu, w_subs |
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| 153 | |
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| 154 | USE control_parameters, & |
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| 155 | ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing, & |
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| 156 | scalar_rayleigh_damping |
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| 157 | |
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| 158 | USE indices, & |
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| 159 | ONLY: nxl, nxlg, nxr, nxrg, nyn, nyng, nys, nysg, nzb, nzb_s_inner,& |
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| 160 | nzt |
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| 161 | |
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| 162 | USE kinds |
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| 163 | |
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| 164 | USE statistics, & |
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| 165 | ONLY: sums_ls_l, weight_pres |
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| 166 | |
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| 167 | IMPLICIT NONE |
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| 168 | |
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| 169 | INTEGER(iwp) :: i !: |
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| 170 | INTEGER(iwp) :: j !: |
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| 171 | INTEGER(iwp) :: k !: |
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| 172 | INTEGER(iwp) :: ls_index !: |
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| 173 | |
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| 174 | REAL(wp) :: tmp_tend !: |
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| 175 | REAL(wp) :: tmp_grad !: |
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| 176 | |
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| 177 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !: |
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| 178 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !: |
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| 179 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !: |
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| 180 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !: |
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| 181 | |
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| 182 | var_mod = var_init |
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| 183 | |
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| 184 | ! |
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| 185 | !-- Influence of w_subsidence on the current tendency term |
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| 186 | DO i = nxl, nxr |
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| 187 | DO j = nys, nyn |
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| 188 | DO k = nzb_s_inner(j,i)+1, nzt |
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| 189 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 190 | tmp_tend = - w_subs(k) * & |
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| 191 | ( var(k+1,j,i) - var(k,j,i) ) * ddzu(k+1) |
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| 192 | ELSE ! large-scale ascent |
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| 193 | tmp_tend = - w_subs(k) * & |
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| 194 | ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) |
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| 195 | ENDIF |
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| 196 | |
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| 197 | tendency(k,j,i) = tendency(k,j,i) + tmp_tend |
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| 198 | |
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| 199 | IF ( large_scale_forcing ) THEN |
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| 200 | sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend & |
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| 201 | * weight_pres(intermediate_timestep_count) |
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| 202 | ENDIF |
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| 203 | ENDDO |
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| 204 | ENDDO |
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| 205 | ENDDO |
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| 206 | |
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| 207 | ! |
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| 208 | !-- Shifting of the initial profile is especially necessary with Rayleigh |
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| 209 | !-- damping switched on |
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| 210 | IF ( scalar_rayleigh_damping ) THEN |
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| 211 | DO k = nzb, nzt |
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| 212 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 213 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 214 | ( var_init(k+1) - var_init(k) ) * ddzu(k+1) |
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| 215 | ENDIF |
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| 216 | ENDDO |
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| 217 | ! |
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| 218 | !-- At the upper boundary, the initial profile is shifted with aid of |
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| 219 | !-- the gradient tmp_grad. (This is ok if the gradients are linear.) |
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| 220 | IF ( w_subs(nzt) < 0.0_wp ) THEN |
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| 221 | tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1) |
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| 222 | var_mod(nzt+1) = var_init(nzt+1) - & |
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| 223 | dt_3d * w_subs(nzt+1) * tmp_grad |
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| 224 | ENDIF |
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| 225 | |
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| 226 | |
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| 227 | DO k = nzt+1, nzb+1, -1 |
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| 228 | IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent |
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| 229 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 230 | ( var_init(k) - var_init(k-1) ) * ddzu(k) |
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| 231 | ENDIF |
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| 232 | ENDDO |
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| 233 | ! |
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| 234 | !-- At the lower boundary shifting is not necessary because the |
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| 235 | !-- subsidence velocity w_subs(nzb) vanishes. |
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| 236 | IF ( w_subs(nzb+1) >= 0.0_wp ) THEN |
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| 237 | var_mod(nzb) = var_init(nzb) |
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| 238 | ENDIF |
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| 239 | |
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| 240 | var_init = var_mod |
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| 241 | ENDIF |
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| 242 | |
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| 243 | |
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| 244 | END SUBROUTINE subsidence |
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| 245 | |
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| 246 | SUBROUTINE subsidence_ij( i, j, tendency, var, var_init, ls_index ) |
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| 247 | |
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| 248 | USE arrays_3d, & |
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| 249 | ONLY: ddzu, w_subs |
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| 250 | |
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| 251 | USE control_parameters, & |
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| 252 | ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing, & |
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| 253 | scalar_rayleigh_damping |
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| 254 | |
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| 255 | USE indices, & |
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| 256 | ONLY: nxl, nxlg, nxrg, nyng, nys, nysg, nzb_s_inner, nzb, nzt |
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| 257 | |
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| 258 | USE kinds |
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| 259 | |
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| 260 | USE statistics, & |
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| 261 | ONLY: sums_ls_l, weight_pres |
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| 262 | |
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| 263 | IMPLICIT NONE |
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| 264 | |
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| 265 | INTEGER(iwp) :: i !: |
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| 266 | INTEGER(iwp) :: j !: |
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| 267 | INTEGER(iwp) :: k !: |
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| 268 | INTEGER(iwp) :: ls_index !: |
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| 269 | |
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| 270 | REAL(wp) :: tmp_tend !: |
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| 271 | REAL(wp) :: tmp_grad !: |
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| 272 | |
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| 273 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !: |
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| 274 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !: |
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| 275 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !: |
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| 276 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !: |
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| 277 | |
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| 278 | var_mod = var_init |
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| 279 | |
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| 280 | ! |
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| 281 | !-- Influence of w_subsidence on the current tendency term |
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| 282 | DO k = nzb_s_inner(j,i)+1, nzt |
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| 283 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 284 | tmp_tend = - w_subs(k) * ( var(k+1,j,i) - var(k,j,i) ) * ddzu(k+1) |
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| 285 | ELSE ! large-scale ascent |
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| 286 | tmp_tend = - w_subs(k) * ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) |
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| 287 | ENDIF |
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| 288 | |
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| 289 | tendency(k,j,i) = tendency(k,j,i) + tmp_tend |
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| 290 | |
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| 291 | IF ( large_scale_forcing ) THEN |
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| 292 | sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend & |
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| 293 | * weight_pres(intermediate_timestep_count) |
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| 294 | ENDIF |
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| 295 | ENDDO |
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| 296 | |
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| 297 | |
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| 298 | ! |
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| 299 | !-- Shifting of the initial profile is especially necessary with Rayleigh |
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| 300 | !-- damping switched on |
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| 301 | IF ( scalar_rayleigh_damping ) THEN |
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| 302 | IF ( i == nxl .AND. j == nys ) THEN ! shifting only once per PE |
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| 303 | |
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| 304 | DO k = nzb, nzt |
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| 305 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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| 306 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 307 | ( var_init(k+1) - var_init(k) ) * ddzu(k+1) |
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| 308 | ENDIF |
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| 309 | ENDDO |
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| 310 | ! |
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| 311 | !-- At the upper boundary, the initial profile is shifted with aid of |
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| 312 | !-- the gradient tmp_grad. (This is ok if the gradients are linear.) |
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| 313 | IF ( w_subs(nzt) < 0.0_wp ) THEN |
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| 314 | tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1) |
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| 315 | var_mod(nzt+1) = var_init(nzt+1) - & |
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| 316 | dt_3d * w_subs(nzt+1) * tmp_grad |
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| 317 | ENDIF |
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| 318 | |
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| 319 | |
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| 320 | DO k = nzt+1, nzb+1, -1 |
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| 321 | IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent |
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| 322 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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| 323 | ( var_init(k) - var_init(k-1) ) * ddzu(k) |
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| 324 | ENDIF |
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| 325 | ENDDO |
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| 326 | ! |
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| 327 | !-- At the lower boundary shifting is not necessary because the |
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| 328 | !-- subsidence velocity w_subs(nzb) vanishes. |
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| 329 | IF ( w_subs(nzb+1) >= 0.0_wp ) THEN |
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| 330 | var_mod(nzb) = var_init(nzb) |
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| 331 | ENDIF |
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| 332 | |
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| 333 | var_init = var_mod |
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| 334 | |
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| 335 | ENDIF |
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| 336 | ENDIF |
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| 337 | |
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| 338 | END SUBROUTINE subsidence_ij |
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| 339 | |
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| 340 | |
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| 341 | END MODULE subsidence_mod |
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