1 | MODULE microphysics_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: microphysics.f90 1347 2014-03-27 13:23:00Z maronga $ |
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27 | ! |
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28 | ! 1346 2014-03-27 13:18:20Z heinze |
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29 | ! Bugfix: REAL constants provided with KIND-attribute especially in call of |
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30 | ! intrinsic function like MAX, MIN, SIGN |
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31 | ! |
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32 | ! 1334 2014-03-25 12:21:40Z heinze |
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33 | ! Bugfix: REAL constants provided with KIND-attribute |
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34 | ! |
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35 | ! 1322 2014-03-20 16:38:49Z raasch |
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36 | ! REAL constants defined as wp-kind |
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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 | ! comment fields (!:) to be used for variable explanations added to |
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43 | ! all variable declaration statements |
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44 | ! |
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45 | ! 1241 2013-10-30 11:36:58Z heinze |
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46 | ! hyp and rho have to be calculated at each time step if data from external |
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47 | ! file LSF_DATA are used |
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48 | ! |
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49 | ! 1115 2013-03-26 18:16:16Z hoffmann |
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50 | ! microphyical tendencies are calculated in microphysics_control in an optimized |
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51 | ! way; unrealistic values are prevented; bugfix in evaporation; some reformatting |
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52 | ! |
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53 | ! 1106 2013-03-04 05:31:38Z raasch |
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54 | ! small changes in code formatting |
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55 | ! |
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56 | ! 1092 2013-02-02 11:24:22Z raasch |
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57 | ! unused variables removed |
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58 | ! file put under GPL |
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59 | ! |
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60 | ! 1065 2012-11-22 17:42:36Z hoffmann |
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61 | ! Sedimentation process implemented according to Stevens and Seifert (2008). |
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62 | ! Turbulence effects on autoconversion and accretion added (Seifert, Nuijens |
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63 | ! and Stevens, 2010). |
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64 | ! |
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65 | ! 1053 2012-11-13 17:11:03Z hoffmann |
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66 | ! initial revision |
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67 | ! |
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68 | ! Description: |
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69 | ! ------------ |
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70 | ! Calculate cloud microphysics according to the two moment bulk |
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71 | ! scheme by Seifert and Beheng (2006). |
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72 | !------------------------------------------------------------------------------! |
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73 | |
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74 | PRIVATE |
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75 | PUBLIC microphysics_control |
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76 | |
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77 | INTERFACE microphysics_control |
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78 | MODULE PROCEDURE microphysics_control |
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79 | MODULE PROCEDURE microphysics_control_ij |
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80 | END INTERFACE microphysics_control |
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81 | |
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82 | INTERFACE adjust_cloud |
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83 | MODULE PROCEDURE adjust_cloud |
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84 | MODULE PROCEDURE adjust_cloud_ij |
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85 | END INTERFACE adjust_cloud |
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86 | |
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87 | INTERFACE autoconversion |
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88 | MODULE PROCEDURE autoconversion |
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89 | MODULE PROCEDURE autoconversion_ij |
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90 | END INTERFACE autoconversion |
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91 | |
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92 | INTERFACE accretion |
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93 | MODULE PROCEDURE accretion |
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94 | MODULE PROCEDURE accretion_ij |
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95 | END INTERFACE accretion |
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96 | |
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97 | INTERFACE selfcollection_breakup |
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98 | MODULE PROCEDURE selfcollection_breakup |
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99 | MODULE PROCEDURE selfcollection_breakup_ij |
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100 | END INTERFACE selfcollection_breakup |
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101 | |
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102 | INTERFACE evaporation_rain |
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103 | MODULE PROCEDURE evaporation_rain |
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104 | MODULE PROCEDURE evaporation_rain_ij |
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105 | END INTERFACE evaporation_rain |
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106 | |
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107 | INTERFACE sedimentation_cloud |
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108 | MODULE PROCEDURE sedimentation_cloud |
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109 | MODULE PROCEDURE sedimentation_cloud_ij |
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110 | END INTERFACE sedimentation_cloud |
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111 | |
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112 | INTERFACE sedimentation_rain |
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113 | MODULE PROCEDURE sedimentation_rain |
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114 | MODULE PROCEDURE sedimentation_rain_ij |
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115 | END INTERFACE sedimentation_rain |
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116 | |
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117 | CONTAINS |
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118 | |
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119 | |
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120 | !------------------------------------------------------------------------------! |
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121 | ! Call for all grid points |
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122 | !------------------------------------------------------------------------------! |
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123 | SUBROUTINE microphysics_control |
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124 | |
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125 | USE arrays_3d |
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126 | USE cloud_parameters |
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127 | USE control_parameters |
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128 | USE grid_variables |
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129 | USE indices |
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130 | USE kinds |
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131 | USE statistics |
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132 | |
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133 | IMPLICIT NONE |
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134 | |
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135 | INTEGER(iwp) :: i !: |
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136 | INTEGER(iwp) :: j !: |
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137 | INTEGER(iwp) :: k !: |
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138 | |
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139 | DO i = nxl, nxr |
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140 | DO j = nys, nyn |
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141 | DO k = nzb_s_inner(j,i)+1, nzt |
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142 | |
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143 | ENDDO |
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144 | ENDDO |
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145 | ENDDO |
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146 | |
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147 | END SUBROUTINE microphysics_control |
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148 | |
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149 | SUBROUTINE adjust_cloud |
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150 | |
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151 | USE arrays_3d |
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152 | USE cloud_parameters |
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153 | USE indices |
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154 | USE kinds |
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155 | |
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156 | IMPLICIT NONE |
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157 | |
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158 | INTEGER(iwp) :: i !: |
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159 | INTEGER(iwp) :: j !: |
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160 | INTEGER(iwp) :: k !: |
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161 | |
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162 | |
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163 | DO i = nxl, nxr |
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164 | DO j = nys, nyn |
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165 | DO k = nzb_s_inner(j,i)+1, nzt |
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166 | |
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167 | ENDDO |
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168 | ENDDO |
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169 | ENDDO |
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170 | |
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171 | END SUBROUTINE adjust_cloud |
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172 | |
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173 | |
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174 | SUBROUTINE autoconversion |
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175 | |
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176 | USE arrays_3d |
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177 | USE cloud_parameters |
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178 | USE control_parameters |
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179 | USE grid_variables |
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180 | USE indices |
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181 | USE kinds |
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182 | |
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183 | IMPLICIT NONE |
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184 | |
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185 | INTEGER(iwp) :: i !: |
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186 | INTEGER(iwp) :: j !: |
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187 | INTEGER(iwp) :: k !: |
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188 | |
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189 | DO i = nxl, nxr |
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190 | DO j = nys, nyn |
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191 | DO k = nzb_s_inner(j,i)+1, nzt |
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192 | |
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193 | ENDDO |
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194 | ENDDO |
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195 | ENDDO |
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196 | |
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197 | END SUBROUTINE autoconversion |
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198 | |
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199 | |
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200 | SUBROUTINE accretion |
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201 | |
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202 | USE arrays_3d |
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203 | USE cloud_parameters |
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204 | USE control_parameters |
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205 | USE indices |
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206 | USE kinds |
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207 | |
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208 | IMPLICIT NONE |
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209 | |
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210 | INTEGER(iwp) :: i !: |
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211 | INTEGER(iwp) :: j !: |
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212 | INTEGER(iwp) :: k !: |
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213 | |
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214 | DO i = nxl, nxr |
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215 | DO j = nys, nyn |
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216 | DO k = nzb_s_inner(j,i)+1, nzt |
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217 | |
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218 | ENDDO |
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219 | ENDDO |
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220 | ENDDO |
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221 | |
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222 | END SUBROUTINE accretion |
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223 | |
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224 | |
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225 | SUBROUTINE selfcollection_breakup |
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226 | |
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227 | USE arrays_3d |
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228 | USE cloud_parameters |
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229 | USE control_parameters |
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230 | USE indices |
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231 | USE kinds |
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232 | |
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233 | IMPLICIT NONE |
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234 | |
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235 | INTEGER(iwp) :: i !: |
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236 | INTEGER(iwp) :: j !: |
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237 | INTEGER(iwp) :: k !: |
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238 | |
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239 | |
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240 | DO i = nxl, nxr |
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241 | DO j = nys, nyn |
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242 | DO k = nzb_s_inner(j,i)+1, nzt |
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243 | |
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244 | ENDDO |
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245 | ENDDO |
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246 | ENDDO |
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247 | |
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248 | END SUBROUTINE selfcollection_breakup |
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249 | |
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250 | |
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251 | SUBROUTINE evaporation_rain |
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252 | |
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253 | USE arrays_3d |
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254 | USE cloud_parameters |
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255 | USE constants |
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256 | USE control_parameters |
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257 | USE indices |
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258 | USE kinds |
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259 | |
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260 | IMPLICIT NONE |
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261 | |
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262 | INTEGER(iwp) :: i !: |
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263 | INTEGER(iwp) :: j !: |
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264 | INTEGER(iwp) :: k !: |
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265 | |
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266 | DO i = nxl, nxr |
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267 | DO j = nys, nyn |
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268 | DO k = nzb_s_inner(j,i)+1, nzt |
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269 | |
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270 | ENDDO |
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271 | ENDDO |
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272 | ENDDO |
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273 | |
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274 | END SUBROUTINE evaporation_rain |
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275 | |
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276 | |
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277 | SUBROUTINE sedimentation_cloud |
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278 | |
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279 | USE arrays_3d |
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280 | USE cloud_parameters |
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281 | USE constants |
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282 | USE control_parameters |
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283 | USE indices |
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284 | USE kinds |
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285 | |
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286 | IMPLICIT NONE |
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287 | |
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288 | INTEGER(iwp) :: i !: |
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289 | INTEGER(iwp) :: j !: |
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290 | INTEGER(iwp) :: k !: |
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291 | |
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292 | DO i = nxl, nxr |
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293 | DO j = nys, nyn |
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294 | DO k = nzb_s_inner(j,i)+1, nzt |
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295 | |
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296 | ENDDO |
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297 | ENDDO |
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298 | ENDDO |
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299 | |
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300 | END SUBROUTINE sedimentation_cloud |
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301 | |
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302 | |
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303 | SUBROUTINE sedimentation_rain |
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304 | |
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305 | USE arrays_3d |
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306 | USE cloud_parameters |
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307 | USE constants |
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308 | USE control_parameters |
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309 | USE indices |
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310 | USE kinds |
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311 | USE statistics |
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312 | |
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313 | IMPLICIT NONE |
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314 | |
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315 | INTEGER(iwp) :: i !: |
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316 | INTEGER(iwp) :: j !: |
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317 | INTEGER(iwp) :: k !: |
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318 | |
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319 | DO i = nxl, nxr |
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320 | DO j = nys, nyn |
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321 | DO k = nzb_s_inner(j,i)+1, nzt |
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322 | |
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323 | ENDDO |
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324 | ENDDO |
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325 | ENDDO |
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326 | |
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327 | END SUBROUTINE sedimentation_rain |
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328 | |
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329 | |
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330 | !------------------------------------------------------------------------------! |
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331 | ! Call for grid point i,j |
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332 | !------------------------------------------------------------------------------! |
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333 | |
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334 | SUBROUTINE microphysics_control_ij( i, j ) |
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335 | |
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336 | USE arrays_3d, & |
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337 | ONLY: hyp, nc_1d, nr, nr_1d, pt, pt_init, pt_1d, q, q_1d, qc, & |
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338 | qc_1d, qr, qr_1d, tend_nr, tend_pt, tend_q, tend_qr, zu |
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339 | |
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340 | USE cloud_parameters, & |
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341 | ONLY: cp, hyrho, nc_const, pt_d_t, r_d, t_d_pt |
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342 | |
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343 | USE control_parameters, & |
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344 | ONLY: drizzle, dt_3d, dt_micro, g, intermediate_timestep_count, & |
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345 | large_scale_forcing, lsf_surf, precipitation, pt_surface, & |
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346 | rho_surface,surface_pressure |
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347 | |
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348 | USE indices, & |
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349 | ONLY: nzb, nzt |
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350 | |
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351 | USE kinds |
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352 | |
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353 | USE statistics, & |
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354 | ONLY: weight_pres |
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355 | |
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356 | IMPLICIT NONE |
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357 | |
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358 | INTEGER(iwp) :: i !: |
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359 | INTEGER(iwp) :: j !: |
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360 | INTEGER(iwp) :: k !: |
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361 | |
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362 | REAL(wp) :: t_surface !: |
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363 | |
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364 | IF ( large_scale_forcing .AND. lsf_surf ) THEN |
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365 | ! |
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366 | !-- Calculate: |
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367 | !-- pt / t : ratio of potential and actual temperature (pt_d_t) |
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368 | !-- t / pt : ratio of actual and potential temperature (t_d_pt) |
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369 | !-- p_0(z) : vertical profile of the hydrostatic pressure (hyp) |
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370 | t_surface = pt_surface * ( surface_pressure / 1000.0 )**0.286_wp |
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371 | DO k = nzb, nzt+1 |
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372 | hyp(k) = surface_pressure * 100.0 * & |
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373 | ( (t_surface - g/cp * zu(k)) / t_surface )**(1.0_wp/0.286_wp) |
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374 | pt_d_t(k) = ( 100000.0 / hyp(k) )**0.286_wp |
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375 | t_d_pt(k) = 1.0 / pt_d_t(k) |
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376 | hyrho(k) = hyp(k) / ( r_d * t_d_pt(k) * pt_init(k) ) |
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377 | ENDDO |
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378 | ! |
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379 | !-- Compute reference density |
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380 | rho_surface = surface_pressure * 100.0 / ( r_d * t_surface ) |
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381 | ENDIF |
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382 | |
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383 | |
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384 | dt_micro = dt_3d * weight_pres(intermediate_timestep_count) |
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385 | ! |
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386 | !-- Adjust unrealistic values |
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387 | IF ( precipitation ) CALL adjust_cloud( i,j ) |
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388 | ! |
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389 | !-- Use 1-d arrays |
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390 | q_1d(:) = q(:,j,i) |
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391 | pt_1d(:) = pt(:,j,i) |
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392 | qc_1d(:) = qc(:,j,i) |
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393 | nc_1d(:) = nc_const |
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394 | IF ( precipitation ) THEN |
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395 | qr_1d(:) = qr(:,j,i) |
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396 | nr_1d(:) = nr(:,j,i) |
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397 | ENDIF |
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398 | ! |
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399 | !-- Compute cloud physics |
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400 | IF ( precipitation ) THEN |
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401 | CALL autoconversion( i,j ) |
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402 | CALL accretion( i,j ) |
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403 | CALL selfcollection_breakup( i,j ) |
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404 | CALL evaporation_rain( i,j ) |
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405 | CALL sedimentation_rain( i,j ) |
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406 | ENDIF |
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407 | |
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408 | IF ( drizzle ) CALL sedimentation_cloud( i,j ) |
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409 | ! |
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410 | !-- Derive tendencies |
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411 | tend_q(:,j,i) = ( q_1d(:) - q(:,j,i) ) / dt_micro |
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412 | tend_pt(:,j,i) = ( pt_1d(:) - pt(:,j,i) ) / dt_micro |
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413 | IF ( precipitation ) THEN |
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414 | tend_qr(:,j,i) = ( qr_1d(:) - qr(:,j,i) ) / dt_micro |
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415 | tend_nr(:,j,i) = ( nr_1d(:) - nr(:,j,i) ) / dt_micro |
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416 | ENDIF |
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417 | |
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418 | END SUBROUTINE microphysics_control_ij |
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419 | |
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420 | SUBROUTINE adjust_cloud_ij( i, j ) |
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421 | |
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422 | USE arrays_3d, & |
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423 | ONLY: qr, nr |
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424 | |
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425 | USE cloud_parameters, & |
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426 | ONLY: eps_sb, xrmin, xrmax, hyrho, k_cc, x0 |
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427 | |
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428 | USE indices, & |
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429 | ONLY: nzb, nzb_s_inner, nzt |
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430 | |
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431 | USE kinds |
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432 | |
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433 | IMPLICIT NONE |
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434 | |
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435 | INTEGER(iwp) :: i !: |
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436 | INTEGER(iwp) :: j !: |
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437 | INTEGER(iwp) :: k !: |
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438 | ! |
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439 | !-- Adjust number of raindrops to avoid nonlinear effects in |
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440 | !-- sedimentation and evaporation of rain drops due to too small or |
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441 | !-- too big weights of rain drops (Stevens and Seifert, 2008). |
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442 | !-- The same procedure is applied to cloud droplets if they are determined |
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443 | !-- prognostically. |
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444 | DO k = nzb_s_inner(j,i)+1, nzt |
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445 | |
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446 | IF ( qr(k,j,i) <= eps_sb ) THEN |
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447 | qr(k,j,i) = 0.0 |
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448 | nr(k,j,i) = 0.0 |
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449 | ELSE |
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450 | ! |
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451 | !-- Adjust number of raindrops to avoid nonlinear effects in |
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452 | !-- sedimentation and evaporation of rain drops due to too small or |
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453 | !-- too big weights of rain drops (Stevens and Seifert, 2008). |
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454 | IF ( nr(k,j,i) * xrmin > qr(k,j,i) * hyrho(k) ) THEN |
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455 | nr(k,j,i) = qr(k,j,i) * hyrho(k) / xrmin |
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456 | ELSEIF ( nr(k,j,i) * xrmax < qr(k,j,i) * hyrho(k) ) THEN |
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457 | nr(k,j,i) = qr(k,j,i) * hyrho(k) / xrmax |
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458 | ENDIF |
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459 | |
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460 | ENDIF |
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461 | |
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462 | ENDDO |
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463 | |
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464 | END SUBROUTINE adjust_cloud_ij |
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465 | |
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466 | |
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467 | SUBROUTINE autoconversion_ij( i, j ) |
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468 | |
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469 | USE arrays_3d, & |
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470 | ONLY: diss, dzu, nc_1d, nr_1d, qc_1d, qr_1d |
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471 | |
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472 | USE cloud_parameters, & |
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473 | ONLY: a_1, a_2, a_3, b_1, b_2, b_3, beta_cc, c_1, c_2, c_3, & |
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474 | c_const, dpirho_l, eps_sb, hyrho, k_cc, kin_vis_air, x0 |
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475 | |
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476 | USE control_parameters, & |
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477 | ONLY: dt_micro, rho_surface, turbulence |
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478 | |
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479 | USE grid_variables, & |
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480 | ONLY: dx, dy |
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481 | |
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482 | USE indices, & |
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483 | ONLY: nzb, nzb_s_inner, nzt |
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484 | |
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485 | USE kinds |
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486 | |
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487 | IMPLICIT NONE |
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488 | |
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489 | INTEGER(iwp) :: i !: |
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490 | INTEGER(iwp) :: j !: |
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491 | INTEGER(iwp) :: k !: |
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492 | |
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493 | REAL(wp) :: alpha_cc !: |
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494 | REAL(wp) :: autocon !: |
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495 | REAL(wp) :: epsilon !: |
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496 | REAL(wp) :: k_au !: |
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497 | REAL(wp) :: l_mix !: |
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498 | REAL(wp) :: nu_c !: |
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499 | REAL(wp) :: phi_au !: |
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500 | REAL(wp) :: r_cc !: |
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501 | REAL(wp) :: rc !: |
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502 | REAL(wp) :: re_lambda !: |
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503 | REAL(wp) :: selfcoll !: |
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504 | REAL(wp) :: sigma_cc !: |
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505 | REAL(wp) :: tau_cloud !: |
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506 | REAL(wp) :: xc !: |
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507 | |
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508 | k_au = k_cc / ( 20.0 * x0 ) |
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509 | |
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510 | DO k = nzb_s_inner(j,i)+1, nzt |
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511 | |
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512 | IF ( qc_1d(k) > eps_sb ) THEN |
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513 | ! |
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514 | !-- Intern time scale of coagulation (Seifert and Beheng, 2006): |
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515 | !-- (1.0 - qc(k,j,i) / ( qc(k,j,i) + qr_1d(k) )) |
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516 | tau_cloud = 1.0 - qc_1d(k) / ( qr_1d(k) + qc_1d(k) ) |
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517 | ! |
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518 | !-- Universal function for autoconversion process |
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519 | !-- (Seifert and Beheng, 2006): |
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520 | phi_au = 600.0 * tau_cloud**0.68_wp * ( 1.0 - tau_cloud**0.68_wp )**3 |
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521 | ! |
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522 | !-- Shape parameter of gamma distribution (Geoffroy et al., 2010): |
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523 | !-- (Use constant nu_c = 1.0 instead?) |
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524 | nu_c = 1.0 !MAX( 0.0_wp, 1580.0 * hyrho(k) * qc(k,j,i) - 0.28_wp ) |
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525 | ! |
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526 | !-- Mean weight of cloud droplets: |
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527 | xc = hyrho(k) * qc_1d(k) / nc_1d(k) |
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528 | ! |
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529 | !-- Parameterized turbulence effects on autoconversion (Seifert, |
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530 | !-- Nuijens and Stevens, 2010) |
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531 | IF ( turbulence ) THEN |
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532 | ! |
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533 | !-- Weight averaged radius of cloud droplets: |
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534 | rc = 0.5 * ( xc * dpirho_l )**( 1.0_wp / 3.0_wp ) |
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535 | |
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536 | alpha_cc = ( a_1 + a_2 * nu_c ) / ( 1.0 + a_3 * nu_c ) |
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537 | r_cc = ( b_1 + b_2 * nu_c ) / ( 1.0 + b_3 * nu_c ) |
---|
538 | sigma_cc = ( c_1 + c_2 * nu_c ) / ( 1.0 + c_3 * nu_c ) |
---|
539 | ! |
---|
540 | !-- Mixing length (neglecting distance to ground and stratification) |
---|
541 | l_mix = ( dx * dy * dzu(k) )**( 1.0_wp / 3.0_wp ) |
---|
542 | ! |
---|
543 | !-- Limit dissipation rate according to Seifert, Nuijens and |
---|
544 | !-- Stevens (2010) |
---|
545 | epsilon = MIN( 0.06_wp, diss(k,j,i) ) |
---|
546 | ! |
---|
547 | !-- Compute Taylor-microscale Reynolds number: |
---|
548 | re_lambda = 6.0 / 11.0 * ( l_mix / c_const )**( 2.0_wp / 3.0_wp ) * & |
---|
549 | SQRT( 15.0 / kin_vis_air ) * epsilon**( 1.0_wp / 6.0_wp ) |
---|
550 | ! |
---|
551 | !-- The factor of 1.0E4 is needed to convert the dissipation rate |
---|
552 | !-- from m2 s-3 to cm2 s-3. |
---|
553 | k_au = k_au * ( 1.0_wp + & |
---|
554 | epsilon * 1.0E4 * ( re_lambda * 1.0E-3 )**0.25_wp * & |
---|
555 | ( alpha_cc * EXP( -1.0 * ( ( rc - r_cc ) / & |
---|
556 | sigma_cc )**2 ) + beta_cc ) ) |
---|
557 | ENDIF |
---|
558 | ! |
---|
559 | !-- Autoconversion rate (Seifert and Beheng, 2006): |
---|
560 | autocon = k_au * ( nu_c + 2.0 ) * ( nu_c + 4.0 ) / & |
---|
561 | ( nu_c + 1.0 )**2.0_wp * qc_1d(k)**2.0_wp * xc**2.0_wp * & |
---|
562 | ( 1.0 + phi_au / ( 1.0 - tau_cloud )**2.0_wp ) * & |
---|
563 | rho_surface |
---|
564 | autocon = MIN( autocon, qc_1d(k) / dt_micro ) |
---|
565 | |
---|
566 | qr_1d(k) = qr_1d(k) + autocon * dt_micro |
---|
567 | qc_1d(k) = qc_1d(k) - autocon * dt_micro |
---|
568 | nr_1d(k) = nr_1d(k) + autocon / x0 * hyrho(k) * dt_micro |
---|
569 | |
---|
570 | ENDIF |
---|
571 | |
---|
572 | ENDDO |
---|
573 | |
---|
574 | END SUBROUTINE autoconversion_ij |
---|
575 | |
---|
576 | |
---|
577 | SUBROUTINE accretion_ij( i, j ) |
---|
578 | |
---|
579 | USE arrays_3d, & |
---|
580 | ONLY: diss, qc_1d, qr_1d |
---|
581 | |
---|
582 | USE cloud_parameters, & |
---|
583 | ONLY: eps_sb, hyrho, k_cr0 |
---|
584 | |
---|
585 | USE control_parameters, & |
---|
586 | ONLY: dt_micro, rho_surface, turbulence |
---|
587 | |
---|
588 | USE indices, & |
---|
589 | ONLY: nzb, nzb_s_inner, nzt |
---|
590 | |
---|
591 | USE kinds |
---|
592 | |
---|
593 | IMPLICIT NONE |
---|
594 | |
---|
595 | INTEGER(iwp) :: i !: |
---|
596 | INTEGER(iwp) :: j !: |
---|
597 | INTEGER(iwp) :: k !: |
---|
598 | |
---|
599 | REAL(wp) :: accr !: |
---|
600 | REAL(wp) :: k_cr !: |
---|
601 | REAL(wp) :: phi_ac !: |
---|
602 | REAL(wp) :: tau_cloud !: |
---|
603 | REAL(wp) :: xc !: |
---|
604 | |
---|
605 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
606 | IF ( ( qc_1d(k) > eps_sb ) .AND. ( qr_1d(k) > eps_sb ) ) THEN |
---|
607 | ! |
---|
608 | !-- Intern time scale of coagulation (Seifert and Beheng, 2006): |
---|
609 | tau_cloud = 1.0 - qc_1d(k) / ( qc_1d(k) + qr_1d(k) ) |
---|
610 | ! |
---|
611 | !-- Universal function for accretion process |
---|
612 | !-- (Seifert and Beheng, 2001): |
---|
613 | phi_ac = tau_cloud / ( tau_cloud + 5.0E-5 ) |
---|
614 | phi_ac = ( phi_ac**2.0_wp )**2.0_wp |
---|
615 | ! |
---|
616 | !-- Parameterized turbulence effects on autoconversion (Seifert, |
---|
617 | !-- Nuijens and Stevens, 2010). The factor of 1.0E4 is needed to |
---|
618 | !-- convert the dissipation (diss) from m2 s-3 to cm2 s-3. |
---|
619 | IF ( turbulence ) THEN |
---|
620 | k_cr = k_cr0 * ( 1.0 + 0.05 * & |
---|
621 | MIN( 600.0_wp, diss(k,j,i) * 1.0E4 )**0.25_wp ) |
---|
622 | ELSE |
---|
623 | k_cr = k_cr0 |
---|
624 | ENDIF |
---|
625 | ! |
---|
626 | !-- Accretion rate (Seifert and Beheng, 2006): |
---|
627 | accr = k_cr * qc_1d(k) * qr_1d(k) * phi_ac * & |
---|
628 | SQRT( rho_surface * hyrho(k) ) |
---|
629 | accr = MIN( accr, qc_1d(k) / dt_micro ) |
---|
630 | |
---|
631 | qr_1d(k) = qr_1d(k) + accr * dt_micro |
---|
632 | qc_1d(k) = qc_1d(k) - accr * dt_micro |
---|
633 | |
---|
634 | ENDIF |
---|
635 | |
---|
636 | ENDDO |
---|
637 | |
---|
638 | END SUBROUTINE accretion_ij |
---|
639 | |
---|
640 | |
---|
641 | SUBROUTINE selfcollection_breakup_ij( i, j ) |
---|
642 | |
---|
643 | USE arrays_3d, & |
---|
644 | ONLY: nr_1d, qr_1d |
---|
645 | |
---|
646 | USE cloud_parameters, & |
---|
647 | ONLY: dpirho_l, eps_sb, hyrho, k_br, k_rr |
---|
648 | |
---|
649 | USE control_parameters, & |
---|
650 | ONLY: dt_micro, rho_surface |
---|
651 | |
---|
652 | USE indices, & |
---|
653 | ONLY: nzb, nzb_s_inner, nzt |
---|
654 | |
---|
655 | USE kinds |
---|
656 | |
---|
657 | IMPLICIT NONE |
---|
658 | |
---|
659 | INTEGER(iwp) :: i !: |
---|
660 | INTEGER(iwp) :: j !: |
---|
661 | INTEGER(iwp) :: k !: |
---|
662 | |
---|
663 | REAL(wp) :: breakup !: |
---|
664 | REAL(wp) :: dr !: |
---|
665 | REAL(wp) :: phi_br !: |
---|
666 | REAL(wp) :: selfcoll !: |
---|
667 | |
---|
668 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
669 | IF ( qr_1d(k) > eps_sb ) THEN |
---|
670 | ! |
---|
671 | !-- Selfcollection rate (Seifert and Beheng, 2001): |
---|
672 | selfcoll = k_rr * nr_1d(k) * qr_1d(k) * & |
---|
673 | SQRT( hyrho(k) * rho_surface ) |
---|
674 | ! |
---|
675 | !-- Weight averaged diameter of rain drops: |
---|
676 | dr = ( hyrho(k) * qr_1d(k) / nr_1d(k) * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
677 | ! |
---|
678 | !-- Collisional breakup rate (Seifert, 2008): |
---|
679 | IF ( dr >= 0.3E-3 ) THEN |
---|
680 | phi_br = k_br * ( dr - 1.1E-3 ) |
---|
681 | breakup = selfcoll * ( phi_br + 1.0 ) |
---|
682 | ELSE |
---|
683 | breakup = 0.0 |
---|
684 | ENDIF |
---|
685 | |
---|
686 | selfcoll = MAX( breakup - selfcoll, -nr_1d(k) / dt_micro ) |
---|
687 | nr_1d(k) = nr_1d(k) + selfcoll * dt_micro |
---|
688 | |
---|
689 | ENDIF |
---|
690 | ENDDO |
---|
691 | |
---|
692 | END SUBROUTINE selfcollection_breakup_ij |
---|
693 | |
---|
694 | |
---|
695 | SUBROUTINE evaporation_rain_ij( i, j ) |
---|
696 | ! |
---|
697 | !-- Evaporation of precipitable water. Condensation is neglected for |
---|
698 | !-- precipitable water. |
---|
699 | |
---|
700 | USE arrays_3d, & |
---|
701 | ONLY: hyp, nr_1d, pt_1d, q_1d, qc_1d, qr_1d |
---|
702 | |
---|
703 | USE cloud_parameters, & |
---|
704 | ONLY: a_term, a_vent, b_term, b_vent, c_evap, c_term, diff_coeff_l,& |
---|
705 | dpirho_l, eps_sb, hyrho, kin_vis_air, k_st, l_d_cp, l_d_r, & |
---|
706 | l_v, rho_l, r_v, schmidt_p_1d3, thermal_conductivity_l, & |
---|
707 | t_d_pt, ventilation_effect |
---|
708 | |
---|
709 | USE constants, & |
---|
710 | ONLY: pi |
---|
711 | |
---|
712 | USE control_parameters, & |
---|
713 | ONLY: dt_micro |
---|
714 | |
---|
715 | USE indices, & |
---|
716 | ONLY: nzb, nzb_s_inner, nzt |
---|
717 | |
---|
718 | USE kinds |
---|
719 | |
---|
720 | IMPLICIT NONE |
---|
721 | |
---|
722 | INTEGER(iwp) :: i !: |
---|
723 | INTEGER(iwp) :: j !: |
---|
724 | INTEGER(iwp) :: k !: |
---|
725 | |
---|
726 | REAL(wp) :: alpha !: |
---|
727 | REAL(wp) :: dr !: |
---|
728 | REAL(wp) :: e_s !: |
---|
729 | REAL(wp) :: evap !: |
---|
730 | REAL(wp) :: evap_nr !: |
---|
731 | REAL(wp) :: f_vent !: |
---|
732 | REAL(wp) :: g_evap !: |
---|
733 | REAL(wp) :: lambda_r !: |
---|
734 | REAL(wp) :: mu_r !: |
---|
735 | REAL(wp) :: mu_r_2 !: |
---|
736 | REAL(wp) :: mu_r_5d2 !: |
---|
737 | REAL(wp) :: nr_0 !: |
---|
738 | REAL(wp) :: q_s !: |
---|
739 | REAL(wp) :: sat !: |
---|
740 | REAL(wp) :: t_l !: |
---|
741 | REAL(wp) :: temp !: |
---|
742 | REAL(wp) :: xr !: |
---|
743 | |
---|
744 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
745 | IF ( qr_1d(k) > eps_sb ) THEN |
---|
746 | ! |
---|
747 | !-- Actual liquid water temperature: |
---|
748 | t_l = t_d_pt(k) * pt_1d(k) |
---|
749 | ! |
---|
750 | !-- Saturation vapor pressure at t_l: |
---|
751 | e_s = 610.78 * EXP( 17.269 * ( t_l - 273.16 ) / ( t_l - 35.86 ) ) |
---|
752 | ! |
---|
753 | !-- Computation of saturation humidity: |
---|
754 | q_s = 0.622 * e_s / ( hyp(k) - 0.378 * e_s ) |
---|
755 | alpha = 0.622 * l_d_r * l_d_cp / ( t_l * t_l ) |
---|
756 | q_s = q_s * ( 1.0 + alpha * q_1d(k) ) / ( 1.0 + alpha * q_s ) |
---|
757 | ! |
---|
758 | !-- Supersaturation: |
---|
759 | sat = MIN( 0.0_wp, ( q_1d(k) - qr_1d(k) - qc_1d(k) ) / q_s - 1.0 ) |
---|
760 | ! |
---|
761 | !-- Actual temperature: |
---|
762 | temp = t_l + l_d_cp * ( qc_1d(k) + qr_1d(k) ) |
---|
763 | |
---|
764 | g_evap = 1.0 / ( ( l_v / ( r_v * temp ) - 1.0 ) * l_v / & |
---|
765 | ( thermal_conductivity_l * temp ) + r_v * temp / & |
---|
766 | ( diff_coeff_l * e_s ) ) |
---|
767 | ! |
---|
768 | !-- Mean weight of rain drops |
---|
769 | xr = hyrho(k) * qr_1d(k) / nr_1d(k) |
---|
770 | ! |
---|
771 | !-- Weight averaged diameter of rain drops: |
---|
772 | dr = ( xr * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
773 | ! |
---|
774 | !-- Compute ventilation factor and intercept parameter |
---|
775 | !-- (Seifert and Beheng, 2006; Seifert, 2008): |
---|
776 | IF ( ventilation_effect ) THEN |
---|
777 | ! |
---|
778 | !-- Shape parameter of gamma distribution (Milbrandt and Yau, 2005; |
---|
779 | !-- Stevens and Seifert, 2008): |
---|
780 | mu_r = 10.0 * ( 1.0 + TANH( 1.2E3 * ( dr - 1.4E-3 ) ) ) |
---|
781 | ! |
---|
782 | !-- Slope parameter of gamma distribution (Seifert, 2008): |
---|
783 | lambda_r = ( ( mu_r + 3.0 ) * ( mu_r + 2.0 ) * & |
---|
784 | ( mu_r + 1.0 ) )**( 1.0_wp / 3.0_wp ) / dr |
---|
785 | |
---|
786 | mu_r_2 = mu_r + 2.0 |
---|
787 | mu_r_5d2 = mu_r + 2.5 |
---|
788 | f_vent = a_vent * gamm( mu_r_2 ) * & |
---|
789 | lambda_r**( -mu_r_2 ) + & |
---|
790 | b_vent * schmidt_p_1d3 * & |
---|
791 | SQRT( a_term / kin_vis_air ) * gamm( mu_r_5d2 ) * & |
---|
792 | lambda_r**( -mu_r_5d2 ) * & |
---|
793 | ( 1.0 - 0.5 * ( b_term / a_term ) * & |
---|
794 | ( lambda_r / & |
---|
795 | ( c_term + lambda_r ) )**mu_r_5d2 - & |
---|
796 | 0.125 * ( b_term / a_term )**2.0_wp * & |
---|
797 | ( lambda_r / & |
---|
798 | ( 2.0 * c_term + lambda_r ) )**mu_r_5d2 - & |
---|
799 | 0.0625 * ( b_term / a_term )**3.0_wp * & |
---|
800 | ( lambda_r / & |
---|
801 | ( 3.0 * c_term + lambda_r ) )**mu_r_5d2 - & |
---|
802 | 0.0390625 * ( b_term / a_term )**4.0_wp * & |
---|
803 | ( lambda_r / & |
---|
804 | ( 4.0 * c_term + lambda_r ) )**mu_r_5d2 ) |
---|
805 | nr_0 = nr_1d(k) * lambda_r**( mu_r + 1.0 ) / & |
---|
806 | gamm( mu_r + 1.0 ) |
---|
807 | ELSE |
---|
808 | f_vent = 1.0 |
---|
809 | nr_0 = nr_1d(k) * dr |
---|
810 | ENDIF |
---|
811 | ! |
---|
812 | !-- Evaporation rate of rain water content (Seifert and Beheng, 2006): |
---|
813 | evap = 2.0 * pi * nr_0 * g_evap * f_vent * sat / & |
---|
814 | hyrho(k) |
---|
815 | |
---|
816 | evap = MAX( evap, -qr_1d(k) / dt_micro ) |
---|
817 | evap_nr = MAX( c_evap * evap / xr * hyrho(k), & |
---|
818 | -nr_1d(k) / dt_micro ) |
---|
819 | |
---|
820 | qr_1d(k) = qr_1d(k) + evap * dt_micro |
---|
821 | nr_1d(k) = nr_1d(k) + evap_nr * dt_micro |
---|
822 | ENDIF |
---|
823 | |
---|
824 | ENDDO |
---|
825 | |
---|
826 | END SUBROUTINE evaporation_rain_ij |
---|
827 | |
---|
828 | |
---|
829 | SUBROUTINE sedimentation_cloud_ij( i, j ) |
---|
830 | |
---|
831 | USE arrays_3d, & |
---|
832 | ONLY: ddzu, dzu, nc_1d, pt_1d, q_1d, qc_1d |
---|
833 | |
---|
834 | USE cloud_parameters, & |
---|
835 | ONLY: eps_sb, hyrho, k_st, l_d_cp, prr, pt_d_t, rho_l, sigma_gc |
---|
836 | |
---|
837 | USE constants, & |
---|
838 | ONLY: pi |
---|
839 | |
---|
840 | USE control_parameters, & |
---|
841 | ONLY: dt_do2d_xy, dt_micro, intermediate_timestep_count |
---|
842 | |
---|
843 | USE indices, & |
---|
844 | ONLY: nzb, nzb_s_inner, nzt |
---|
845 | |
---|
846 | USE kinds |
---|
847 | |
---|
848 | IMPLICIT NONE |
---|
849 | |
---|
850 | INTEGER(iwp) :: i !: |
---|
851 | INTEGER(iwp) :: j !: |
---|
852 | INTEGER(iwp) :: k !: |
---|
853 | |
---|
854 | REAL(wp) :: sed_qc_const !: |
---|
855 | |
---|
856 | |
---|
857 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_qc |
---|
858 | |
---|
859 | ! |
---|
860 | !-- Sedimentation of cloud droplets (Heus et al., 2010): |
---|
861 | sed_qc_const = k_st * ( 3.0 / ( 4.0 * pi * rho_l ))**( 2.0_wp / 3.0_wp ) * & |
---|
862 | EXP( 5.0 * LOG( sigma_gc )**2 ) |
---|
863 | |
---|
864 | sed_qc(nzt+1) = 0.0 |
---|
865 | |
---|
866 | DO k = nzt, nzb_s_inner(j,i)+1, -1 |
---|
867 | IF ( qc_1d(k) > eps_sb ) THEN |
---|
868 | sed_qc(k) = sed_qc_const * nc_1d(k)**( -2.0_wp / 3.0_wp ) * & |
---|
869 | ( qc_1d(k) * hyrho(k) )**( 5.0_wp / 3.0_wp ) |
---|
870 | ELSE |
---|
871 | sed_qc(k) = 0.0 |
---|
872 | ENDIF |
---|
873 | |
---|
874 | sed_qc(k) = MIN( sed_qc(k), hyrho(k) * dzu(k+1) * q_1d(k) / & |
---|
875 | dt_micro + sed_qc(k+1) ) |
---|
876 | |
---|
877 | q_1d(k) = q_1d(k) + ( sed_qc(k+1) - sed_qc(k) ) * ddzu(k+1) / & |
---|
878 | hyrho(k) * dt_micro |
---|
879 | qc_1d(k) = qc_1d(k) + ( sed_qc(k+1) - sed_qc(k) ) * ddzu(k+1) / & |
---|
880 | hyrho(k) * dt_micro |
---|
881 | pt_1d(k) = pt_1d(k) - ( sed_qc(k+1) - sed_qc(k) ) * ddzu(k+1) / & |
---|
882 | hyrho(k) * l_d_cp * pt_d_t(k) * dt_micro |
---|
883 | |
---|
884 | ENDDO |
---|
885 | |
---|
886 | END SUBROUTINE sedimentation_cloud_ij |
---|
887 | |
---|
888 | |
---|
889 | SUBROUTINE sedimentation_rain_ij( i, j ) |
---|
890 | |
---|
891 | USE arrays_3d, & |
---|
892 | ONLY: ddzu, dzu, nr_1d, pt_1d, q_1d, qr_1d |
---|
893 | |
---|
894 | USE cloud_parameters, & |
---|
895 | ONLY: a_term, b_term, c_term, cof, dpirho_l, eps_sb, hyrho, & |
---|
896 | limiter_sedimentation, l_d_cp, precipitation_amount, prr, & |
---|
897 | pt_d_t, stp |
---|
898 | |
---|
899 | USE control_parameters, & |
---|
900 | ONLY: dt_do2d_xy, dt_micro, dt_3d, intermediate_timestep_count, & |
---|
901 | intermediate_timestep_count_max, & |
---|
902 | precipitation_amount_interval, time_do2d_xy |
---|
903 | |
---|
904 | USE indices, & |
---|
905 | ONLY: nzb, nzb_s_inner, nzt |
---|
906 | |
---|
907 | USE kinds |
---|
908 | |
---|
909 | USE statistics, & |
---|
910 | ONLY: weight_substep |
---|
911 | |
---|
912 | IMPLICIT NONE |
---|
913 | |
---|
914 | INTEGER(iwp) :: i !: |
---|
915 | INTEGER(iwp) :: j !: |
---|
916 | INTEGER(iwp) :: k !: |
---|
917 | INTEGER(iwp) :: k_run !: |
---|
918 | |
---|
919 | REAL(wp) :: c_run !: |
---|
920 | REAL(wp) :: d_max !: |
---|
921 | REAL(wp) :: d_mean !: |
---|
922 | REAL(wp) :: d_min !: |
---|
923 | REAL(wp) :: dr !: |
---|
924 | REAL(wp) :: dt_sedi !: |
---|
925 | REAL(wp) :: flux !: |
---|
926 | REAL(wp) :: lambda_r !: |
---|
927 | REAL(wp) :: mu_r !: |
---|
928 | REAL(wp) :: z_run !: |
---|
929 | |
---|
930 | REAL(wp), DIMENSION(nzb:nzt+1) :: c_nr !: |
---|
931 | REAL(wp), DIMENSION(nzb:nzt+1) :: c_qr !: |
---|
932 | REAL(wp), DIMENSION(nzb:nzt+1) :: d_nr !: |
---|
933 | REAL(wp), DIMENSION(nzb:nzt+1) :: d_qr !: |
---|
934 | REAL(wp), DIMENSION(nzb:nzt+1) :: nr_slope !: |
---|
935 | REAL(wp), DIMENSION(nzb:nzt+1) :: qr_slope !: |
---|
936 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_nr !: |
---|
937 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_qr !: |
---|
938 | REAL(wp), DIMENSION(nzb:nzt+1) :: w_nr !: |
---|
939 | REAL(wp), DIMENSION(nzb:nzt+1) :: w_qr !: |
---|
940 | |
---|
941 | |
---|
942 | ! |
---|
943 | !-- Computation of sedimentation flux. Implementation according to Stevens |
---|
944 | !-- and Seifert (2008). |
---|
945 | IF ( intermediate_timestep_count == 1 ) prr(:,j,i) = 0.0 |
---|
946 | ! |
---|
947 | !-- Compute velocities |
---|
948 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
949 | IF ( qr_1d(k) > eps_sb ) THEN |
---|
950 | ! |
---|
951 | !-- Weight averaged diameter of rain drops: |
---|
952 | dr = ( hyrho(k) * qr_1d(k) / nr_1d(k) * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
953 | ! |
---|
954 | !-- Shape parameter of gamma distribution (Milbrandt and Yau, 2005; |
---|
955 | !-- Stevens and Seifert, 2008): |
---|
956 | mu_r = 10.0 * ( 1.0 + TANH( 1.2E3 * ( dr - 1.4E-3 ) ) ) |
---|
957 | ! |
---|
958 | !-- Slope parameter of gamma distribution (Seifert, 2008): |
---|
959 | lambda_r = ( ( mu_r + 3.0 ) * ( mu_r + 2.0 ) * & |
---|
960 | ( mu_r + 1.0 ) )**( 1.0_wp / 3.0_wp ) / dr |
---|
961 | |
---|
962 | w_nr(k) = MAX( 0.1_wp, MIN( 20.0_wp, a_term - b_term * ( 1.0 + & |
---|
963 | c_term / lambda_r )**( -1.0 * ( mu_r + 1.0 ) ) ) ) |
---|
964 | w_qr(k) = MAX( 0.1_wp, MIN( 20.0_wp, a_term - b_term * ( 1.0 + & |
---|
965 | c_term / lambda_r )**( -1.0 * ( mu_r + 4.0 ) ) ) ) |
---|
966 | ELSE |
---|
967 | w_nr(k) = 0.0 |
---|
968 | w_qr(k) = 0.0 |
---|
969 | ENDIF |
---|
970 | ENDDO |
---|
971 | ! |
---|
972 | !-- Adjust boundary values |
---|
973 | w_nr(nzb_s_inner(j,i)) = w_nr(nzb_s_inner(j,i)+1) |
---|
974 | w_qr(nzb_s_inner(j,i)) = w_qr(nzb_s_inner(j,i)+1) |
---|
975 | w_nr(nzt+1) = 0.0 |
---|
976 | w_qr(nzt+1) = 0.0 |
---|
977 | ! |
---|
978 | !-- Compute Courant number |
---|
979 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
980 | c_nr(k) = 0.25 * ( w_nr(k-1) + 2.0 * w_nr(k) + w_nr(k+1) ) * & |
---|
981 | dt_micro * ddzu(k) |
---|
982 | c_qr(k) = 0.25 * ( w_qr(k-1) + 2.0 * w_qr(k) + w_qr(k+1) ) * & |
---|
983 | dt_micro * ddzu(k) |
---|
984 | ENDDO |
---|
985 | ! |
---|
986 | !-- Limit slopes with monotonized centered (MC) limiter (van Leer, 1977): |
---|
987 | IF ( limiter_sedimentation ) THEN |
---|
988 | |
---|
989 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
990 | d_mean = 0.5 * ( qr_1d(k+1) + qr_1d(k-1) ) |
---|
991 | d_min = qr_1d(k) - MIN( qr_1d(k+1), qr_1d(k), qr_1d(k-1) ) |
---|
992 | d_max = MAX( qr_1d(k+1), qr_1d(k), qr_1d(k-1) ) - qr_1d(k) |
---|
993 | |
---|
994 | qr_slope(k) = SIGN(1.0_wp, d_mean) * MIN ( 2.0 * d_min, 2.0 * d_max, & |
---|
995 | ABS( d_mean ) ) |
---|
996 | |
---|
997 | d_mean = 0.5 * ( nr_1d(k+1) + nr_1d(k-1) ) |
---|
998 | d_min = nr_1d(k) - MIN( nr_1d(k+1), nr_1d(k), nr_1d(k-1) ) |
---|
999 | d_max = MAX( nr_1d(k+1), nr_1d(k), nr_1d(k-1) ) - nr_1d(k) |
---|
1000 | |
---|
1001 | nr_slope(k) = SIGN(1.0_wp, d_mean) * MIN ( 2.0 * d_min, 2.0 * d_max, & |
---|
1002 | ABS( d_mean ) ) |
---|
1003 | ENDDO |
---|
1004 | |
---|
1005 | ELSE |
---|
1006 | |
---|
1007 | nr_slope = 0.0 |
---|
1008 | qr_slope = 0.0 |
---|
1009 | |
---|
1010 | ENDIF |
---|
1011 | |
---|
1012 | sed_nr(nzt+1) = 0.0 |
---|
1013 | sed_qr(nzt+1) = 0.0 |
---|
1014 | ! |
---|
1015 | !-- Compute sedimentation flux |
---|
1016 | DO k = nzt, nzb_s_inner(j,i)+1, -1 |
---|
1017 | ! |
---|
1018 | !-- Sum up all rain drop number densities which contribute to the flux |
---|
1019 | !-- through k-1/2 |
---|
1020 | flux = 0.0 |
---|
1021 | z_run = 0.0 ! height above z(k) |
---|
1022 | k_run = k |
---|
1023 | c_run = MIN( 1.0_wp, c_nr(k) ) |
---|
1024 | DO WHILE ( c_run > 0.0 .AND. k_run <= nzt ) |
---|
1025 | flux = flux + hyrho(k_run) * & |
---|
1026 | ( nr_1d(k_run) + nr_slope(k_run) * ( 1.0 - c_run ) * & |
---|
1027 | 0.5 ) * c_run * dzu(k_run) |
---|
1028 | z_run = z_run + dzu(k_run) |
---|
1029 | k_run = k_run + 1 |
---|
1030 | c_run = MIN( 1.0_wp, c_nr(k_run) - z_run * ddzu(k_run) ) |
---|
1031 | ENDDO |
---|
1032 | ! |
---|
1033 | !-- It is not allowed to sediment more rain drop number density than |
---|
1034 | !-- available |
---|
1035 | flux = MIN( flux, & |
---|
1036 | hyrho(k) * dzu(k+1) * nr_1d(k) + sed_nr(k+1) * dt_micro ) |
---|
1037 | |
---|
1038 | sed_nr(k) = flux / dt_micro |
---|
1039 | nr_1d(k) = nr_1d(k) + ( sed_nr(k+1) - sed_nr(k) ) * ddzu(k+1) / & |
---|
1040 | hyrho(k) * dt_micro |
---|
1041 | ! |
---|
1042 | !-- Sum up all rain water content which contributes to the flux |
---|
1043 | !-- through k-1/2 |
---|
1044 | flux = 0.0 |
---|
1045 | z_run = 0.0 ! height above z(k) |
---|
1046 | k_run = k |
---|
1047 | c_run = MIN( 1.0_wp, c_qr(k) ) |
---|
1048 | |
---|
1049 | DO WHILE ( c_run > 0.0 .AND. k_run <= nzt-1 ) |
---|
1050 | |
---|
1051 | flux = flux + hyrho(k_run) * & |
---|
1052 | ( qr_1d(k_run) + qr_slope(k_run) * ( 1.0 - c_run ) * & |
---|
1053 | 0.5 ) * c_run * dzu(k_run) |
---|
1054 | z_run = z_run + dzu(k_run) |
---|
1055 | k_run = k_run + 1 |
---|
1056 | c_run = MIN( 1.0_wp, c_qr(k_run) - z_run * ddzu(k_run) ) |
---|
1057 | |
---|
1058 | ENDDO |
---|
1059 | ! |
---|
1060 | !-- It is not allowed to sediment more rain water content than available |
---|
1061 | flux = MIN( flux, & |
---|
1062 | hyrho(k) * dzu(k) * qr_1d(k) + sed_qr(k+1) * dt_micro ) |
---|
1063 | |
---|
1064 | sed_qr(k) = flux / dt_micro |
---|
1065 | |
---|
1066 | qr_1d(k) = qr_1d(k) + ( sed_qr(k+1) - sed_qr(k) ) * ddzu(k+1) / & |
---|
1067 | hyrho(k) * dt_micro |
---|
1068 | q_1d(k) = q_1d(k) + ( sed_qr(k+1) - sed_qr(k) ) * ddzu(k+1) / & |
---|
1069 | hyrho(k) * dt_micro |
---|
1070 | pt_1d(k) = pt_1d(k) - ( sed_qr(k+1) - sed_qr(k) ) * ddzu(k+1) / & |
---|
1071 | hyrho(k) * l_d_cp * pt_d_t(k) * dt_micro |
---|
1072 | ! |
---|
1073 | !-- Compute the rain rate |
---|
1074 | prr(k,j,i) = prr(k,j,i) + sed_qr(k) / hyrho(k) * & |
---|
1075 | weight_substep(intermediate_timestep_count) |
---|
1076 | ENDDO |
---|
1077 | |
---|
1078 | ! |
---|
1079 | !-- Precipitation amount |
---|
1080 | IF ( intermediate_timestep_count == intermediate_timestep_count_max & |
---|
1081 | .AND. ( dt_do2d_xy - time_do2d_xy ) < & |
---|
1082 | precipitation_amount_interval ) THEN |
---|
1083 | |
---|
1084 | precipitation_amount(j,i) = precipitation_amount(j,i) + & |
---|
1085 | prr(nzb_s_inner(j,i)+1,j,i) * & |
---|
1086 | hyrho(nzb_s_inner(j,i)+1) * dt_3d |
---|
1087 | ENDIF |
---|
1088 | |
---|
1089 | END SUBROUTINE sedimentation_rain_ij |
---|
1090 | |
---|
1091 | |
---|
1092 | ! |
---|
1093 | !-- This function computes the gamma function (Press et al., 1992). |
---|
1094 | !-- The gamma function is needed for the calculation of the evaporation |
---|
1095 | !-- of rain drops. |
---|
1096 | FUNCTION gamm( xx ) |
---|
1097 | |
---|
1098 | USE cloud_parameters, & |
---|
1099 | ONLY: cof, stp |
---|
1100 | |
---|
1101 | USE kinds |
---|
1102 | |
---|
1103 | IMPLICIT NONE |
---|
1104 | |
---|
1105 | INTEGER(iwp) :: j !: |
---|
1106 | |
---|
1107 | REAL(wp) :: gamm !: |
---|
1108 | REAL(wp) :: ser !: |
---|
1109 | REAL(wp) :: tmp !: |
---|
1110 | REAL(wp) :: x_gamm !: |
---|
1111 | REAL(wp) :: xx !: |
---|
1112 | REAL(wp) :: y_gamm !: |
---|
1113 | |
---|
1114 | x_gamm = xx |
---|
1115 | y_gamm = x_gamm |
---|
1116 | tmp = x_gamm + 5.5 |
---|
1117 | tmp = ( x_gamm + 0.5 ) * LOG( tmp ) - tmp |
---|
1118 | ser = 1.000000000190015_wp |
---|
1119 | |
---|
1120 | DO j = 1, 6 |
---|
1121 | y_gamm = y_gamm + 1.0 |
---|
1122 | ser = ser + cof( j ) / y_gamm |
---|
1123 | ENDDO |
---|
1124 | |
---|
1125 | ! |
---|
1126 | !-- Until this point the algorithm computes the logarithm of the gamma |
---|
1127 | !-- function. Hence, the exponential function is used. |
---|
1128 | ! gamm = EXP( tmp + LOG( stp * ser / x_gamm ) ) |
---|
1129 | gamm = EXP( tmp ) * stp * ser / x_gamm |
---|
1130 | |
---|
1131 | RETURN |
---|
1132 | |
---|
1133 | END FUNCTION gamm |
---|
1134 | |
---|
1135 | END MODULE microphysics_mod |
---|