1 | !> @file subsidence_mod.f90 |
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2 | !------------------------------------------------------------------------------! |
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3 | ! This file is part of the PALM model system. |
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4 | ! |
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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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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 1997-2019 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_mod.f90 3655 2019-01-07 16:51:22Z knoop $ |
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27 | ! add subroutine and variable description |
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28 | ! |
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29 | ! 3302 2018-10-03 02:39:40Z raasch |
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30 | ! small message change |
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31 | ! |
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32 | ! 3294 2018-10-01 02:37:10Z raasch |
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33 | ! ocean renamed ocean_mode |
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34 | ! |
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35 | ! 3045 2018-05-28 07:55:41Z Giersch |
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36 | ! Error message revised |
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37 | ! |
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38 | ! 2718 2018-01-02 08:49:38Z maronga |
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39 | ! Corrected "Former revisions" section |
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40 | ! |
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41 | ! 2696 2017-12-14 17:12:51Z kanani |
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42 | ! Change in file header (GPL part) |
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43 | ! |
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44 | ! 2233 2017-05-30 18:08:54Z suehring |
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45 | ! |
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46 | ! 2232 2017-05-30 17:47:52Z suehring |
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47 | ! Adjustments to new topography and surface concept |
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48 | ! |
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49 | ! 2000 2016-08-20 18:09:15Z knoop |
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50 | ! Forced header and separation lines into 80 columns |
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51 | ! |
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52 | ! 1862 2016-04-14 09:07:42Z hoffmann |
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53 | ! Bugfix: In case of vector machine optimized model runs, sums_ls_l should not |
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54 | ! be addressed if large_scale_forcing is false because sums_ls_l is not |
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55 | ! allocated. |
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56 | ! |
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57 | ! 1850 2016-04-08 13:29:27Z maronga |
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58 | ! Module renamed |
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59 | ! |
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60 | ! 1729 2015-11-20 11:01:48Z gronemeier |
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61 | ! Bugfix: shifting of initial profiles only once each time step |
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62 | ! |
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63 | ! 1682 2015-10-07 23:56:08Z knoop |
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64 | ! Code annotations made doxygen readable |
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65 | ! |
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66 | ! 1489 2014-10-30 08:09:12Z raasch |
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67 | ! bugfix: sums_ls_l can only be used if large_scale_forcing is switched on |
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68 | ! |
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69 | ! 1382 2014-04-30 12:15:41Z boeske |
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70 | ! Changed the weighting factor that is used in the summation of subsidence |
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71 | ! tendencies for profile data output from weight_pres to weight_substep |
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72 | ! added Neumann boundary conditions for profile data output of subsidence terms |
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73 | ! at nzt+1 |
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74 | ! |
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75 | ! 1380 2014-04-28 12:40:45Z heinze |
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76 | ! Shifting only necessary in case of scalar Rayleigh damping |
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77 | ! |
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78 | ! 1365 2014-04-22 15:03:56Z boeske |
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79 | ! Summation of subsidence tendencies for data output added |
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80 | ! +ls_index, sums_ls_l, tmp_tend |
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81 | ! |
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82 | ! 1353 2014-04-08 15:21:23Z heinze |
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83 | ! REAL constants provided with KIND-attribute |
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84 | ! |
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85 | ! 1320 2014-03-20 08:40:49Z raasch |
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86 | ! ONLY-attribute added to USE-statements, |
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87 | ! kind-parameters added to all INTEGER and REAL declaration statements, |
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88 | ! kinds are defined in new module kinds, |
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89 | ! old module precision_kind is removed, |
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90 | ! revision history before 2012 removed, |
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91 | ! comment fields (!:) to be used for variable explanations added to |
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92 | ! all variable declaration statements |
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93 | ! |
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94 | ! 1036 2012-10-22 13:43:42Z raasch |
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95 | ! code put under GPL (PALM 3.9) |
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96 | ! |
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97 | ! Revision 3.7 2009-12-11 14:15:58Z heinze |
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98 | ! Initial revision |
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99 | ! |
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100 | ! Description: |
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101 | ! ------------ |
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102 | !> Impact of large-scale subsidence or ascent as tendency term for use |
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103 | !> in the prognostic equation of potential temperature. This enables the |
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104 | !> construction of a constant boundary layer height z_i with time. |
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105 | !-----------------------------------------------------------------------------! |
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106 | MODULE subsidence_mod |
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107 | |
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108 | |
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109 | |
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110 | IMPLICIT NONE |
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111 | |
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112 | PRIVATE |
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113 | PUBLIC init_w_subsidence, subsidence |
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114 | |
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115 | INTERFACE init_w_subsidence |
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116 | MODULE PROCEDURE init_w_subsidence |
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117 | END INTERFACE init_w_subsidence |
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118 | |
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119 | INTERFACE subsidence |
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120 | MODULE PROCEDURE subsidence |
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121 | MODULE PROCEDURE subsidence_ij |
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122 | END INTERFACE subsidence |
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123 | |
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124 | CONTAINS |
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125 | |
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126 | !------------------------------------------------------------------------------! |
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127 | ! Description: |
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128 | ! ------------ |
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129 | !> Initialize vertical subsidence velocity w_subs. |
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130 | !------------------------------------------------------------------------------! |
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131 | SUBROUTINE init_w_subsidence |
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132 | |
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133 | USE arrays_3d, & |
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134 | ONLY: dzu, w_subs, zu |
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135 | |
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136 | USE control_parameters, & |
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137 | ONLY: message_string, ocean_mode, subs_vertical_gradient, & |
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138 | subs_vertical_gradient_level, subs_vertical_gradient_level_i |
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139 | |
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140 | USE indices, & |
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141 | ONLY: nzb, nzt |
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142 | |
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143 | USE kinds |
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144 | |
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145 | IMPLICIT NONE |
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146 | |
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147 | INTEGER(iwp) :: i !< loop index |
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148 | INTEGER(iwp) :: k !< loop index |
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149 | |
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150 | REAL(wp) :: gradient !< vertical gradient of subsidence velocity |
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151 | REAL(wp) :: ws_surface !< subsidence velocity at the surface |
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152 | |
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153 | IF ( .NOT. ALLOCATED( w_subs ) ) THEN |
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154 | ALLOCATE( w_subs(nzb:nzt+1) ) |
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155 | w_subs = 0.0_wp |
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156 | ENDIF |
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157 | |
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158 | IF ( ocean_mode ) THEN |
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159 | message_string = 'applying large scale vertical motion is not ' // & |
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160 | 'allowed for ocean mode' |
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161 | CALL message( 'init_w_subsidence', 'PA0324', 2, 2, 0, 6, 0 ) |
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162 | ENDIF |
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163 | |
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164 | ! |
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165 | !-- Compute the profile of the subsidence/ascent velocity |
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166 | !-- using the given gradients |
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167 | i = 1 |
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168 | gradient = 0.0_wp |
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169 | ws_surface = 0.0_wp |
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170 | |
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171 | |
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172 | subs_vertical_gradient_level_i(1) = 0 |
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173 | DO k = 1, nzt+1 |
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174 | IF ( i < 11 ) THEN |
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175 | IF ( subs_vertical_gradient_level(i) < zu(k) .AND. & |
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176 | subs_vertical_gradient_level(i) >= 0.0_wp ) THEN |
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177 | gradient = subs_vertical_gradient(i) / 100.0_wp |
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178 | subs_vertical_gradient_level_i(i) = k - 1 |
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179 | i = i + 1 |
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180 | ENDIF |
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181 | ENDIF |
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182 | IF ( gradient /= 0.0_wp ) THEN |
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183 | IF ( k /= 1 ) THEN |
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184 | w_subs(k) = w_subs(k-1) + dzu(k) * gradient |
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185 | ELSE |
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186 | w_subs(k) = ws_surface + 0.5_wp * dzu(k) * gradient |
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187 | ENDIF |
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188 | ELSE |
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189 | w_subs(k) = w_subs(k-1) |
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190 | ENDIF |
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191 | ENDDO |
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192 | |
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193 | ! |
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194 | !-- In case of no given gradients for the subsidence/ascent velocity, |
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195 | !-- choose zero gradient |
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196 | IF ( subs_vertical_gradient_level(1) == -9999999.9_wp ) THEN |
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197 | subs_vertical_gradient_level(1) = 0.0_wp |
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198 | ENDIF |
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199 | |
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200 | END SUBROUTINE init_w_subsidence |
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201 | |
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202 | |
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203 | !------------------------------------------------------------------------------! |
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204 | ! Description: |
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205 | ! ------------ |
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206 | !> Add effect of large-scale subsidence to variable. |
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207 | !------------------------------------------------------------------------------! |
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208 | SUBROUTINE subsidence( tendency, var, var_init, ls_index ) |
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209 | |
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210 | USE arrays_3d, & |
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211 | ONLY: ddzu, w_subs |
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212 | |
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213 | USE control_parameters, & |
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214 | ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing, & |
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215 | scalar_rayleigh_damping |
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216 | |
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217 | USE indices, & |
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218 | ONLY: nxl, nxlg, nxr, nxrg, nyn, nyng, nys, nysg, nzb, nzt, & |
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219 | wall_flags_0 |
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220 | |
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221 | USE kinds |
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222 | |
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223 | USE statistics, & |
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224 | ONLY: sums_ls_l, weight_substep |
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225 | |
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226 | IMPLICIT NONE |
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227 | |
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228 | INTEGER(iwp) :: i !< loop index |
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229 | INTEGER(iwp) :: j !< loop index |
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230 | INTEGER(iwp) :: k !< loop index |
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231 | INTEGER(iwp) :: ls_index !< index of large-scale subsidence in sums_ls_l |
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232 | |
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233 | REAL(wp) :: tmp_tend !< temporary tendency |
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234 | REAL(wp) :: tmp_grad !< temporary gradient |
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235 | |
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236 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !< variable where to add subsidence |
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237 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !< tendency of var |
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238 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !< initialization profile of var |
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239 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !< modified profile of var |
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240 | |
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241 | var_mod = var_init |
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242 | |
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243 | ! |
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244 | !-- Influence of w_subsidence on the current tendency term |
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245 | DO i = nxl, nxr |
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246 | DO j = nys, nyn |
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247 | |
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248 | DO k = nzb+1, nzt |
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249 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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250 | tmp_tend = - w_subs(k) * & |
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251 | ( var(k+1,j,i) - var(k,j,i) ) * ddzu(k+1) * & |
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252 | MERGE( 1.0_wp, 0.0_wp, & |
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253 | BTEST( wall_flags_0(k,j,i), 0 ) ) |
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254 | ELSE ! large-scale ascent |
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255 | tmp_tend = - w_subs(k) * & |
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256 | ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) * & |
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257 | MERGE( 1.0_wp, 0.0_wp, & |
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258 | BTEST( wall_flags_0(k,j,i), 0 ) ) |
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259 | ENDIF |
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260 | |
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261 | tendency(k,j,i) = tendency(k,j,i) + tmp_tend |
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262 | |
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263 | IF ( large_scale_forcing ) THEN |
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264 | sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend & |
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265 | * weight_substep(intermediate_timestep_count) & |
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266 | * MERGE( 1.0_wp, 0.0_wp, & |
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267 | BTEST( wall_flags_0(k,j,i), 0 ) ) |
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268 | ENDIF |
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269 | ENDDO |
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270 | |
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271 | IF ( large_scale_forcing ) THEN |
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272 | sums_ls_l(nzt+1,ls_index) = sums_ls_l(nzt,ls_index) |
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273 | ENDIF |
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274 | |
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275 | ENDDO |
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276 | ENDDO |
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277 | |
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278 | ! |
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279 | !-- Shifting of the initial profile is especially necessary with Rayleigh |
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280 | !-- damping switched on |
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281 | IF ( scalar_rayleigh_damping .AND. & |
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282 | intermediate_timestep_count == 1 ) THEN |
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283 | DO k = nzb, nzt |
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284 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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285 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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286 | ( var_init(k+1) - var_init(k) ) * ddzu(k+1) |
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287 | ENDIF |
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288 | ENDDO |
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289 | ! |
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290 | !-- At the upper boundary, the initial profile is shifted with aid of |
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291 | !-- the gradient tmp_grad. (This is ok if the gradients are linear.) |
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292 | IF ( w_subs(nzt) < 0.0_wp ) THEN |
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293 | tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1) |
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294 | var_mod(nzt+1) = var_init(nzt+1) - & |
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295 | dt_3d * w_subs(nzt+1) * tmp_grad |
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296 | ENDIF |
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297 | |
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298 | |
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299 | DO k = nzt+1, nzb+1, -1 |
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300 | IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent |
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301 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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302 | ( var_init(k) - var_init(k-1) ) * ddzu(k) |
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303 | ENDIF |
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304 | ENDDO |
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305 | ! |
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306 | !-- At the lower boundary shifting is not necessary because the |
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307 | !-- subsidence velocity w_subs(nzb) vanishes. |
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308 | IF ( w_subs(nzb+1) >= 0.0_wp ) THEN |
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309 | var_mod(nzb) = var_init(nzb) |
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310 | ENDIF |
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311 | |
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312 | var_init = var_mod |
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313 | ENDIF |
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314 | |
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315 | |
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316 | END SUBROUTINE subsidence |
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317 | |
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318 | !------------------------------------------------------------------------------! |
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319 | ! Description: |
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320 | ! ------------ |
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321 | !> Add effect of large-scale subsidence to variable. |
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322 | !------------------------------------------------------------------------------! |
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323 | SUBROUTINE subsidence_ij( i, j, tendency, var, var_init, ls_index ) |
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324 | |
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325 | USE arrays_3d, & |
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326 | ONLY: ddzu, w_subs |
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327 | |
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328 | USE control_parameters, & |
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329 | ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing, & |
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330 | scalar_rayleigh_damping |
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331 | |
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332 | USE indices, & |
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333 | ONLY: nxl, nxlg, nxrg, nyng, nys, nysg, nzb, nzt, wall_flags_0 |
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334 | |
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335 | USE kinds |
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336 | |
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337 | USE statistics, & |
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338 | ONLY: sums_ls_l, weight_substep |
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339 | |
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340 | IMPLICIT NONE |
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341 | |
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342 | INTEGER(iwp) :: i !< loop variable |
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343 | INTEGER(iwp) :: j !< loop variable |
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344 | INTEGER(iwp) :: k !< loop variable |
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345 | INTEGER(iwp) :: ls_index !< index of large-scale subsidence in sums_ls_l |
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346 | |
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347 | REAL(wp) :: tmp_tend !< temporary tendency |
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348 | REAL(wp) :: tmp_grad !< temporary gradient |
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349 | |
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350 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !< variable where to add subsidence |
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351 | REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !< tendency of var |
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352 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !< initialization profile of var |
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353 | REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !< modified profile of var |
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354 | |
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355 | var_mod = var_init |
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356 | |
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357 | ! |
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358 | !-- Influence of w_subsidence on the current tendency term |
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359 | DO k = nzb+1, nzt |
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360 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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361 | tmp_tend = - w_subs(k) * ( var(k+1,j,i) - var(k,j,i) ) & |
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362 | * ddzu(k+1) & |
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363 | * MERGE( 1.0_wp, 0.0_wp, & |
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364 | BTEST( wall_flags_0(k,j,i), 0 ) ) |
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365 | ELSE ! large-scale ascent |
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366 | tmp_tend = - w_subs(k) * ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) & |
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367 | * MERGE( 1.0_wp, 0.0_wp, & |
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368 | BTEST( wall_flags_0(k,j,i), 0 ) ) |
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369 | ENDIF |
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370 | |
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371 | tendency(k,j,i) = tendency(k,j,i) + tmp_tend |
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372 | |
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373 | IF ( large_scale_forcing ) THEN |
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374 | sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend & |
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375 | * weight_substep(intermediate_timestep_count)& |
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376 | * MERGE( 1.0_wp, 0.0_wp, & |
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377 | BTEST( wall_flags_0(k,j,i), 0 ) ) |
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378 | ENDIF |
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379 | ENDDO |
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380 | |
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381 | IF ( large_scale_forcing ) THEN |
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382 | sums_ls_l(nzt+1,ls_index) = sums_ls_l(nzt,ls_index) |
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383 | ENDIF |
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384 | |
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385 | ! |
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386 | !-- Shifting of the initial profile is especially necessary with Rayleigh |
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387 | !-- damping switched on |
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388 | IF ( scalar_rayleigh_damping .AND. & |
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389 | intermediate_timestep_count == 1 ) THEN |
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390 | IF ( i == nxl .AND. j == nys ) THEN ! shifting only once per PE |
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391 | |
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392 | DO k = nzb, nzt |
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393 | IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence |
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394 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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395 | ( var_init(k+1) - var_init(k) ) * ddzu(k+1) |
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396 | ENDIF |
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397 | ENDDO |
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398 | ! |
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399 | !-- At the upper boundary, the initial profile is shifted with aid of |
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400 | !-- the gradient tmp_grad. (This is ok if the gradients are linear.) |
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401 | IF ( w_subs(nzt) < 0.0_wp ) THEN |
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402 | tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1) |
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403 | var_mod(nzt+1) = var_init(nzt+1) - & |
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404 | dt_3d * w_subs(nzt+1) * tmp_grad |
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405 | ENDIF |
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406 | |
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407 | |
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408 | DO k = nzt+1, nzb+1, -1 |
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409 | IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent |
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410 | var_mod(k) = var_init(k) - dt_3d * w_subs(k) * & |
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411 | ( var_init(k) - var_init(k-1) ) * ddzu(k) |
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412 | ENDIF |
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413 | ENDDO |
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414 | ! |
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415 | !-- At the lower boundary shifting is not necessary because the |
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416 | !-- subsidence velocity w_subs(nzb) vanishes. |
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417 | IF ( w_subs(nzb+1) >= 0.0_wp ) THEN |
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418 | var_mod(nzb) = var_init(nzb) |
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419 | ENDIF |
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420 | |
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421 | var_init = var_mod |
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422 | |
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423 | ENDIF |
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424 | ENDIF |
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425 | |
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426 | END SUBROUTINE subsidence_ij |
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427 | |
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428 | |
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429 | END MODULE subsidence_mod |
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