1 | !> @file microphysics.f90 |
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2 | !--------------------------------------------------------------------------------! |
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3 | ! This file is part of PALM. |
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4 | ! |
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5 | ! PALM is free software: you can redistribute it and/or modify it under the terms |
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6 | ! of the GNU General Public License as published by the Free Software Foundation, |
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7 | ! either version 3 of the License, or (at your option) any later version. |
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8 | ! |
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9 | ! PALM is distributed in the hope that it will be useful, but WITHOUT ANY |
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10 | ! WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR |
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11 | ! A PARTICULAR PURPOSE. See the GNU General Public License for more details. |
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12 | ! |
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13 | ! You should have received a copy of the GNU General Public License along with |
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14 | ! PALM. If not, see <http://www.gnu.org/licenses/>. |
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15 | ! |
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16 | ! Copyright 1997-2015 Leibniz Universitaet Hannover |
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17 | !--------------------------------------------------------------------------------! |
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18 | ! |
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19 | ! Current revisions: |
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20 | ! ------------------ |
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21 | ! |
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22 | ! |
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23 | ! Former revisions: |
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24 | ! ----------------- |
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25 | ! $Id: microphysics.f90 1692 2015-10-26 16:29:17Z gronemeier $ |
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26 | ! |
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27 | ! 1691 2015-10-26 16:17:44Z maronga |
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28 | ! Added new routine calc_precipitation_amount. The routine now allows to account |
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29 | ! for precipitation due to sedimenation of cloud (fog) droplets |
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30 | ! |
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31 | ! 1682 2015-10-07 23:56:08Z knoop |
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32 | ! Code annotations made doxygen readable |
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33 | ! |
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34 | ! 1646 2015-09-02 16:00:10Z hoffmann |
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35 | ! Bugfix: Wrong computation of d_mean. |
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36 | ! |
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37 | ! 1361 2014-04-16 15:17:48Z hoffmann |
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38 | ! Bugfix in sedimentation_rain: Index corrected. |
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39 | ! Vectorized version of adjust_cloud added. |
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40 | ! Little reformatting of the code. |
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41 | ! |
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42 | ! 1353 2014-04-08 15:21:23Z heinze |
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43 | ! REAL constants provided with KIND-attribute |
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44 | ! |
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45 | ! 1346 2014-03-27 13:18:20Z heinze |
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46 | ! Bugfix: REAL constants provided with KIND-attribute especially in call of |
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47 | ! intrinsic function like MAX, MIN, SIGN |
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48 | ! |
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49 | ! 1334 2014-03-25 12:21:40Z heinze |
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50 | ! Bugfix: REAL constants provided with KIND-attribute |
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51 | ! |
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52 | ! 1322 2014-03-20 16:38:49Z raasch |
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53 | ! REAL constants defined as wp-kind |
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54 | ! |
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55 | ! 1320 2014-03-20 08:40:49Z raasch |
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56 | ! ONLY-attribute added to USE-statements, |
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57 | ! kind-parameters added to all INTEGER and REAL declaration statements, |
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58 | ! kinds are defined in new module kinds, |
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59 | ! comment fields (!:) to be used for variable explanations added to |
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60 | ! all variable declaration statements |
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61 | ! |
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62 | ! 1241 2013-10-30 11:36:58Z heinze |
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63 | ! hyp and rho have to be calculated at each time step if data from external |
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64 | ! file LSF_DATA are used |
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65 | ! |
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66 | ! 1115 2013-03-26 18:16:16Z hoffmann |
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67 | ! microphyical tendencies are calculated in microphysics_control in an optimized |
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68 | ! way; unrealistic values are prevented; bugfix in evaporation; some reformatting |
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69 | ! |
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70 | ! 1106 2013-03-04 05:31:38Z raasch |
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71 | ! small changes in code formatting |
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72 | ! |
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73 | ! 1092 2013-02-02 11:24:22Z raasch |
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74 | ! unused variables removed |
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75 | ! file put under GPL |
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76 | ! |
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77 | ! 1065 2012-11-22 17:42:36Z hoffmann |
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78 | ! Sedimentation process implemented according to Stevens and Seifert (2008). |
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79 | ! Turbulence effects on autoconversion and accretion added (Seifert, Nuijens |
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80 | ! and Stevens, 2010). |
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81 | ! |
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82 | ! 1053 2012-11-13 17:11:03Z hoffmann |
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83 | ! initial revision |
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84 | ! |
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85 | ! Description: |
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86 | ! ------------ |
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87 | !> Calculate cloud microphysics according to the two moment bulk |
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88 | !> scheme by Seifert and Beheng (2006). |
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89 | !------------------------------------------------------------------------------! |
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90 | MODULE microphysics_mod |
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91 | |
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92 | |
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93 | PRIVATE |
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94 | PUBLIC microphysics_control |
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95 | |
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96 | INTERFACE microphysics_control |
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97 | MODULE PROCEDURE microphysics_control |
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98 | MODULE PROCEDURE microphysics_control_ij |
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99 | END INTERFACE microphysics_control |
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100 | |
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101 | INTERFACE adjust_cloud |
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102 | MODULE PROCEDURE adjust_cloud |
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103 | MODULE PROCEDURE adjust_cloud_ij |
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104 | END INTERFACE adjust_cloud |
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105 | |
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106 | INTERFACE autoconversion |
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107 | MODULE PROCEDURE autoconversion |
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108 | MODULE PROCEDURE autoconversion_ij |
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109 | END INTERFACE autoconversion |
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110 | |
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111 | INTERFACE accretion |
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112 | MODULE PROCEDURE accretion |
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113 | MODULE PROCEDURE accretion_ij |
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114 | END INTERFACE accretion |
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115 | |
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116 | INTERFACE selfcollection_breakup |
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117 | MODULE PROCEDURE selfcollection_breakup |
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118 | MODULE PROCEDURE selfcollection_breakup_ij |
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119 | END INTERFACE selfcollection_breakup |
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120 | |
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121 | INTERFACE evaporation_rain |
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122 | MODULE PROCEDURE evaporation_rain |
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123 | MODULE PROCEDURE evaporation_rain_ij |
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124 | END INTERFACE evaporation_rain |
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125 | |
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126 | INTERFACE sedimentation_cloud |
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127 | MODULE PROCEDURE sedimentation_cloud |
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128 | MODULE PROCEDURE sedimentation_cloud_ij |
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129 | END INTERFACE sedimentation_cloud |
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130 | |
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131 | INTERFACE sedimentation_rain |
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132 | MODULE PROCEDURE sedimentation_rain |
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133 | MODULE PROCEDURE sedimentation_rain_ij |
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134 | END INTERFACE sedimentation_rain |
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135 | |
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136 | INTERFACE calc_precipitation_amount |
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137 | MODULE PROCEDURE calc_precipitation_amount |
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138 | MODULE PROCEDURE calc_precipitation_amount_ij |
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139 | END INTERFACE calc_precipitation_amount |
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140 | |
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141 | |
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142 | CONTAINS |
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143 | |
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144 | |
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145 | !------------------------------------------------------------------------------! |
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146 | ! Description: |
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147 | ! ------------ |
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148 | !> Call for all grid points |
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149 | !------------------------------------------------------------------------------! |
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150 | SUBROUTINE microphysics_control |
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151 | |
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152 | USE arrays_3d, & |
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153 | ONLY: hyp, nr, pt, pt_init, q, qc, qr, zu |
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154 | |
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155 | USE cloud_parameters, & |
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156 | ONLY: cp, hyrho, nc_const, pt_d_t, r_d, t_d_pt |
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157 | |
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158 | USE control_parameters, & |
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159 | ONLY: call_microphysics_at_all_substeps, drizzle, dt_3d, dt_micro, & |
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160 | g, intermediate_timestep_count, & |
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161 | large_scale_forcing, lsf_surf, precipitation, pt_surface, & |
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162 | rho_surface,surface_pressure |
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163 | |
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164 | USE indices, & |
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165 | ONLY: nzb, nzt |
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166 | |
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167 | USE kinds |
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168 | |
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169 | USE statistics, & |
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170 | ONLY: weight_pres |
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171 | |
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172 | IMPLICIT NONE |
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173 | |
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174 | INTEGER(iwp) :: i !< |
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175 | INTEGER(iwp) :: j !< |
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176 | INTEGER(iwp) :: k !< |
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177 | |
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178 | REAL(wp) :: t_surface !< |
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179 | |
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180 | IF ( large_scale_forcing .AND. lsf_surf ) THEN |
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181 | ! |
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182 | !-- Calculate: |
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183 | !-- pt / t : ratio of potential and actual temperature (pt_d_t) |
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184 | !-- t / pt : ratio of actual and potential temperature (t_d_pt) |
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185 | !-- p_0(z) : vertical profile of the hydrostatic pressure (hyp) |
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186 | t_surface = pt_surface * ( surface_pressure / 1000.0_wp )**0.286_wp |
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187 | DO k = nzb, nzt+1 |
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188 | hyp(k) = surface_pressure * 100.0_wp * & |
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189 | ( ( t_surface - g / cp * zu(k) ) / & |
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190 | t_surface )**(1.0_wp / 0.286_wp) |
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191 | pt_d_t(k) = ( 100000.0_wp / hyp(k) )**0.286_wp |
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192 | t_d_pt(k) = 1.0_wp / pt_d_t(k) |
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193 | hyrho(k) = hyp(k) / ( r_d * t_d_pt(k) * pt_init(k) ) |
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194 | ENDDO |
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195 | ! |
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196 | !-- Compute reference density |
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197 | rho_surface = surface_pressure * 100.0_wp / ( r_d * t_surface ) |
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198 | ENDIF |
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199 | |
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200 | ! |
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201 | !-- Compute length of time step |
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202 | IF ( call_microphysics_at_all_substeps ) THEN |
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203 | dt_micro = dt_3d * weight_pres(intermediate_timestep_count) |
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204 | ELSE |
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205 | dt_micro = dt_3d |
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206 | ENDIF |
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207 | |
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208 | ! |
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209 | !-- Compute cloud physics |
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210 | IF ( precipitation ) THEN |
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211 | CALL adjust_cloud |
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212 | CALL autoconversion |
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213 | CALL accretion |
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214 | CALL selfcollection_breakup |
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215 | CALL evaporation_rain |
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216 | CALL sedimentation_rain |
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217 | ENDIF |
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218 | |
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219 | IF ( drizzle ) CALL sedimentation_cloud |
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220 | |
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221 | IF ( precipitation ) THEN |
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222 | CALL calc_precipitation_amount |
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223 | ENDIF |
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224 | |
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225 | END SUBROUTINE microphysics_control |
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226 | |
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227 | !------------------------------------------------------------------------------! |
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228 | ! Description: |
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229 | ! ------------ |
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230 | !> Adjust number of raindrops to avoid nonlinear effects in sedimentation and |
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231 | !> evaporation of rain drops due to too small or too big weights |
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232 | !> of rain drops (Stevens and Seifert, 2008). |
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233 | !------------------------------------------------------------------------------! |
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234 | SUBROUTINE adjust_cloud |
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235 | |
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236 | USE arrays_3d, & |
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237 | ONLY: qr, nr |
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238 | |
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239 | USE cloud_parameters, & |
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240 | ONLY: eps_sb, xrmin, xrmax, hyrho, k_cc, x0 |
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241 | |
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242 | USE cpulog, & |
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243 | ONLY: cpu_log, log_point_s |
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244 | |
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245 | USE indices, & |
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246 | ONLY: nxl, nxr, nys, nyn, nzb, nzb_s_inner, nzt |
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247 | |
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248 | USE kinds |
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249 | |
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250 | IMPLICIT NONE |
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251 | |
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252 | INTEGER(iwp) :: i !< |
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253 | INTEGER(iwp) :: j !< |
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254 | INTEGER(iwp) :: k !< |
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255 | |
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256 | CALL cpu_log( log_point_s(54), 'adjust_cloud', 'start' ) |
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257 | |
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258 | DO i = nxl, nxr |
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259 | DO j = nys, nyn |
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260 | DO k = nzb_s_inner(j,i)+1, nzt |
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261 | IF ( qr(k,j,i) <= eps_sb ) THEN |
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262 | qr(k,j,i) = 0.0_wp |
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263 | nr(k,j,i) = 0.0_wp |
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264 | ELSE |
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265 | IF ( nr(k,j,i) * xrmin > qr(k,j,i) * hyrho(k) ) THEN |
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266 | nr(k,j,i) = qr(k,j,i) * hyrho(k) / xrmin |
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267 | ELSEIF ( nr(k,j,i) * xrmax < qr(k,j,i) * hyrho(k) ) THEN |
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268 | nr(k,j,i) = qr(k,j,i) * hyrho(k) / xrmax |
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269 | ENDIF |
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270 | ENDIF |
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271 | ENDDO |
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272 | ENDDO |
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273 | ENDDO |
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274 | |
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275 | CALL cpu_log( log_point_s(54), 'adjust_cloud', 'stop' ) |
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276 | |
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277 | END SUBROUTINE adjust_cloud |
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278 | |
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279 | |
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280 | !------------------------------------------------------------------------------! |
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281 | ! Description: |
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282 | ! ------------ |
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283 | !> Autoconversion rate (Seifert and Beheng, 2006). |
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284 | !------------------------------------------------------------------------------! |
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285 | SUBROUTINE autoconversion |
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286 | |
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287 | USE arrays_3d, & |
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288 | ONLY: diss, dzu, nr, qc, qr |
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289 | |
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290 | USE cloud_parameters, & |
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291 | 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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292 | c_const, dpirho_l, eps_sb, hyrho, k_cc, kin_vis_air, & |
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293 | nc_const, x0 |
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294 | |
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295 | USE control_parameters, & |
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296 | ONLY: dt_micro, rho_surface, turbulence |
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297 | |
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298 | USE cpulog, & |
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299 | ONLY: cpu_log, log_point_s |
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300 | |
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301 | USE grid_variables, & |
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302 | ONLY: dx, dy |
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303 | |
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304 | USE indices, & |
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305 | ONLY: nxl, nxr, nys, nyn, nzb, nzb_s_inner, nzt |
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306 | |
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307 | USE kinds |
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308 | |
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309 | IMPLICIT NONE |
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310 | |
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311 | INTEGER(iwp) :: i !< |
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312 | INTEGER(iwp) :: j !< |
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313 | INTEGER(iwp) :: k !< |
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314 | |
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315 | REAL(wp) :: alpha_cc !< |
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316 | REAL(wp) :: autocon !< |
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317 | REAL(wp) :: dissipation !< |
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318 | REAL(wp) :: k_au !< |
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319 | REAL(wp) :: l_mix !< |
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320 | REAL(wp) :: nu_c !< |
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321 | REAL(wp) :: phi_au !< |
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322 | REAL(wp) :: r_cc !< |
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323 | REAL(wp) :: rc !< |
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324 | REAL(wp) :: re_lambda !< |
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325 | REAL(wp) :: selfcoll !< |
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326 | REAL(wp) :: sigma_cc !< |
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327 | REAL(wp) :: tau_cloud !< |
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328 | REAL(wp) :: xc !< |
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329 | |
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330 | CALL cpu_log( log_point_s(55), 'autoconversion', 'start' ) |
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331 | |
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332 | DO i = nxl, nxr |
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333 | DO j = nys, nyn |
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334 | DO k = nzb_s_inner(j,i)+1, nzt |
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335 | |
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336 | IF ( qc(k,j,i) > eps_sb ) THEN |
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337 | |
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338 | k_au = k_cc / ( 20.0_wp * x0 ) |
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339 | ! |
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340 | !-- Intern time scale of coagulation (Seifert and Beheng, 2006): |
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341 | !-- (1.0_wp - qc(k,j,i) / ( qc(k,j,i) + qr(k,j,i) )) |
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342 | tau_cloud = 1.0_wp - qc(k,j,i) / ( qr(k,j,i) + qc(k,j,i) ) |
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343 | ! |
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344 | !-- Universal function for autoconversion process |
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345 | !-- (Seifert and Beheng, 2006): |
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346 | phi_au = 600.0_wp * tau_cloud**0.68_wp * & |
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347 | ( 1.0_wp - tau_cloud**0.68_wp )**3 |
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348 | ! |
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349 | !-- Shape parameter of gamma distribution (Geoffroy et al., 2010): |
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350 | !-- (Use constant nu_c = 1.0_wp instead?) |
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351 | nu_c = 1.0_wp !MAX( 0.0_wp, 1580.0_wp * hyrho(k) * qc(k,j,i) - 0.28_wp ) |
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352 | ! |
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353 | !-- Mean weight of cloud droplets: |
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354 | xc = hyrho(k) * qc(k,j,i) / nc_const |
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355 | ! |
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356 | !-- Parameterized turbulence effects on autoconversion (Seifert, |
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357 | !-- Nuijens and Stevens, 2010) |
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358 | IF ( turbulence ) THEN |
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359 | ! |
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360 | !-- Weight averaged radius of cloud droplets: |
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361 | rc = 0.5_wp * ( xc * dpirho_l )**( 1.0_wp / 3.0_wp ) |
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362 | |
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363 | alpha_cc = ( a_1 + a_2 * nu_c ) / ( 1.0_wp + a_3 * nu_c ) |
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364 | r_cc = ( b_1 + b_2 * nu_c ) / ( 1.0_wp + b_3 * nu_c ) |
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365 | sigma_cc = ( c_1 + c_2 * nu_c ) / ( 1.0_wp + c_3 * nu_c ) |
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366 | ! |
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367 | !-- Mixing length (neglecting distance to ground and |
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368 | !-- stratification) |
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369 | l_mix = ( dx * dy * dzu(k) )**( 1.0_wp / 3.0_wp ) |
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370 | ! |
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371 | !-- Limit dissipation rate according to Seifert, Nuijens and |
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372 | !-- Stevens (2010) |
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373 | dissipation = MIN( 0.06_wp, diss(k,j,i) ) |
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374 | ! |
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375 | !-- Compute Taylor-microscale Reynolds number: |
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376 | re_lambda = 6.0_wp / 11.0_wp * & |
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377 | ( l_mix / c_const )**( 2.0_wp / 3.0_wp ) * & |
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378 | SQRT( 15.0_wp / kin_vis_air ) * & |
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379 | dissipation**( 1.0_wp / 6.0_wp ) |
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380 | ! |
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381 | !-- The factor of 1.0E4 is needed to convert the dissipation |
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382 | !-- rate from m2 s-3 to cm2 s-3. |
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383 | k_au = k_au * ( 1.0_wp + & |
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384 | dissipation * 1.0E4_wp * & |
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385 | ( re_lambda * 1.0E-3_wp )**0.25_wp * & |
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386 | ( alpha_cc * EXP( -1.0_wp * ( ( rc - & |
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387 | r_cc ) / & |
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388 | sigma_cc )**2 & |
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389 | ) + beta_cc & |
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390 | ) & |
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391 | ) |
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392 | ENDIF |
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393 | ! |
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394 | !-- Autoconversion rate (Seifert and Beheng, 2006): |
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395 | autocon = k_au * ( nu_c + 2.0_wp ) * ( nu_c + 4.0_wp ) / & |
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396 | ( nu_c + 1.0_wp )**2 * qc(k,j,i)**2 * xc**2 * & |
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397 | ( 1.0_wp + phi_au / ( 1.0_wp - tau_cloud )**2 ) * & |
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398 | rho_surface |
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399 | autocon = MIN( autocon, qc(k,j,i) / dt_micro ) |
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400 | |
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401 | qr(k,j,i) = qr(k,j,i) + autocon * dt_micro |
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402 | qc(k,j,i) = qc(k,j,i) - autocon * dt_micro |
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403 | nr(k,j,i) = nr(k,j,i) + autocon / x0 * hyrho(k) * dt_micro |
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404 | |
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405 | ENDIF |
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406 | |
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407 | ENDDO |
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408 | ENDDO |
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409 | ENDDO |
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410 | |
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411 | CALL cpu_log( log_point_s(55), 'autoconversion', 'stop' ) |
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412 | |
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413 | END SUBROUTINE autoconversion |
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414 | |
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415 | |
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416 | !------------------------------------------------------------------------------! |
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417 | ! Description: |
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418 | ! ------------ |
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419 | !> Accretion rate (Seifert and Beheng, 2006). |
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420 | !------------------------------------------------------------------------------! |
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421 | SUBROUTINE accretion |
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422 | |
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423 | USE arrays_3d, & |
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424 | ONLY: diss, qc, qr |
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425 | |
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426 | USE cloud_parameters, & |
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427 | ONLY: eps_sb, hyrho, k_cr0 |
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428 | |
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429 | USE control_parameters, & |
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430 | ONLY: dt_micro, rho_surface, turbulence |
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431 | |
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432 | USE cpulog, & |
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433 | ONLY: cpu_log, log_point_s |
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434 | |
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435 | USE indices, & |
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436 | ONLY: nxl, nxr, nys, nyn, nzb, nzb_s_inner, nzt |
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437 | |
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438 | USE kinds |
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439 | |
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440 | IMPLICIT NONE |
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441 | |
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442 | INTEGER(iwp) :: i !< |
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443 | INTEGER(iwp) :: j !< |
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444 | INTEGER(iwp) :: k !< |
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445 | |
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446 | REAL(wp) :: accr !< |
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447 | REAL(wp) :: k_cr !< |
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448 | REAL(wp) :: phi_ac !< |
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449 | REAL(wp) :: tau_cloud !< |
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450 | REAL(wp) :: xc !< |
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451 | |
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452 | CALL cpu_log( log_point_s(56), 'accretion', 'start' ) |
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453 | |
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454 | DO i = nxl, nxr |
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455 | DO j = nys, nyn |
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456 | DO k = nzb_s_inner(j,i)+1, nzt |
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457 | |
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458 | IF ( ( qc(k,j,i) > eps_sb ) .AND. ( qr(k,j,i) > eps_sb ) ) THEN |
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459 | ! |
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460 | !-- Intern time scale of coagulation (Seifert and Beheng, 2006): |
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461 | tau_cloud = 1.0_wp - qc(k,j,i) / ( qc(k,j,i) + qr(k,j,i) ) |
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462 | ! |
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463 | !-- Universal function for accretion process (Seifert and |
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464 | !-- Beheng, 2001): |
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465 | phi_ac = ( tau_cloud / ( tau_cloud + 5.0E-5_wp ) )**4 |
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466 | ! |
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467 | !-- Parameterized turbulence effects on autoconversion (Seifert, |
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468 | !-- Nuijens and Stevens, 2010). The factor of 1.0E4 is needed to |
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469 | !-- convert the dissipation rate (diss) from m2 s-3 to cm2 s-3. |
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470 | IF ( turbulence ) THEN |
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471 | k_cr = k_cr0 * ( 1.0_wp + 0.05_wp * & |
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472 | MIN( 600.0_wp, & |
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473 | diss(k,j,i) * 1.0E4_wp )**0.25_wp & |
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474 | ) |
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475 | ELSE |
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476 | k_cr = k_cr0 |
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477 | ENDIF |
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478 | ! |
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479 | !-- Accretion rate (Seifert and Beheng, 2006): |
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480 | accr = k_cr * qc(k,j,i) * qr(k,j,i) * phi_ac * & |
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481 | SQRT( rho_surface * hyrho(k) ) |
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482 | accr = MIN( accr, qc(k,j,i) / dt_micro ) |
---|
483 | |
---|
484 | qr(k,j,i) = qr(k,j,i) + accr * dt_micro |
---|
485 | qc(k,j,i) = qc(k,j,i) - accr * dt_micro |
---|
486 | |
---|
487 | ENDIF |
---|
488 | |
---|
489 | ENDDO |
---|
490 | ENDDO |
---|
491 | ENDDO |
---|
492 | |
---|
493 | CALL cpu_log( log_point_s(56), 'accretion', 'stop' ) |
---|
494 | |
---|
495 | END SUBROUTINE accretion |
---|
496 | |
---|
497 | |
---|
498 | !------------------------------------------------------------------------------! |
---|
499 | ! Description: |
---|
500 | ! ------------ |
---|
501 | !> Collisional breakup rate (Seifert, 2008). |
---|
502 | !------------------------------------------------------------------------------! |
---|
503 | SUBROUTINE selfcollection_breakup |
---|
504 | |
---|
505 | USE arrays_3d, & |
---|
506 | ONLY: nr, qr |
---|
507 | |
---|
508 | USE cloud_parameters, & |
---|
509 | ONLY: dpirho_l, eps_sb, hyrho, k_br, k_rr |
---|
510 | |
---|
511 | USE control_parameters, & |
---|
512 | ONLY: dt_micro, rho_surface |
---|
513 | |
---|
514 | USE cpulog, & |
---|
515 | ONLY: cpu_log, log_point_s |
---|
516 | |
---|
517 | USE indices, & |
---|
518 | ONLY: nxl, nxr, nys, nyn, nzb, nzb_s_inner, nzt |
---|
519 | |
---|
520 | USE kinds |
---|
521 | |
---|
522 | IMPLICIT NONE |
---|
523 | |
---|
524 | INTEGER(iwp) :: i !< |
---|
525 | INTEGER(iwp) :: j !< |
---|
526 | INTEGER(iwp) :: k !< |
---|
527 | |
---|
528 | REAL(wp) :: breakup !< |
---|
529 | REAL(wp) :: dr !< |
---|
530 | REAL(wp) :: phi_br !< |
---|
531 | REAL(wp) :: selfcoll !< |
---|
532 | |
---|
533 | CALL cpu_log( log_point_s(57), 'selfcollection', 'start' ) |
---|
534 | |
---|
535 | DO i = nxl, nxr |
---|
536 | DO j = nys, nyn |
---|
537 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
538 | IF ( qr(k,j,i) > eps_sb ) THEN |
---|
539 | ! |
---|
540 | !-- Selfcollection rate (Seifert and Beheng, 2001): |
---|
541 | selfcoll = k_rr * nr(k,j,i) * qr(k,j,i) * & |
---|
542 | SQRT( hyrho(k) * rho_surface ) |
---|
543 | ! |
---|
544 | !-- Weight averaged diameter of rain drops: |
---|
545 | dr = ( hyrho(k) * qr(k,j,i) / & |
---|
546 | nr(k,j,i) * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
547 | ! |
---|
548 | !-- Collisional breakup rate (Seifert, 2008): |
---|
549 | IF ( dr >= 0.3E-3_wp ) THEN |
---|
550 | phi_br = k_br * ( dr - 1.1E-3_wp ) |
---|
551 | breakup = selfcoll * ( phi_br + 1.0_wp ) |
---|
552 | ELSE |
---|
553 | breakup = 0.0_wp |
---|
554 | ENDIF |
---|
555 | |
---|
556 | selfcoll = MAX( breakup - selfcoll, -nr(k,j,i) / dt_micro ) |
---|
557 | nr(k,j,i) = nr(k,j,i) + selfcoll * dt_micro |
---|
558 | |
---|
559 | ENDIF |
---|
560 | ENDDO |
---|
561 | ENDDO |
---|
562 | ENDDO |
---|
563 | |
---|
564 | CALL cpu_log( log_point_s(57), 'selfcollection', 'stop' ) |
---|
565 | |
---|
566 | END SUBROUTINE selfcollection_breakup |
---|
567 | |
---|
568 | |
---|
569 | !------------------------------------------------------------------------------! |
---|
570 | ! Description: |
---|
571 | ! ------------ |
---|
572 | !> Evaporation of precipitable water. Condensation is neglected for |
---|
573 | !> precipitable water. |
---|
574 | !------------------------------------------------------------------------------! |
---|
575 | SUBROUTINE evaporation_rain |
---|
576 | |
---|
577 | USE arrays_3d, & |
---|
578 | ONLY: hyp, nr, pt, q, qc, qr |
---|
579 | |
---|
580 | USE cloud_parameters, & |
---|
581 | ONLY: a_term, a_vent, b_term, b_vent, c_evap, c_term, diff_coeff_l,& |
---|
582 | dpirho_l, eps_sb, hyrho, kin_vis_air, k_st, l_d_cp, l_d_r, & |
---|
583 | l_v, rho_l, r_v, schmidt_p_1d3, thermal_conductivity_l, & |
---|
584 | t_d_pt, ventilation_effect |
---|
585 | |
---|
586 | USE constants, & |
---|
587 | ONLY: pi |
---|
588 | |
---|
589 | USE control_parameters, & |
---|
590 | ONLY: dt_micro |
---|
591 | |
---|
592 | USE cpulog, & |
---|
593 | ONLY: cpu_log, log_point_s |
---|
594 | |
---|
595 | USE indices, & |
---|
596 | ONLY: nxl, nxr, nys, nyn, nzb, nzb_s_inner, nzt |
---|
597 | |
---|
598 | USE kinds |
---|
599 | |
---|
600 | IMPLICIT NONE |
---|
601 | |
---|
602 | INTEGER(iwp) :: i !< |
---|
603 | INTEGER(iwp) :: j !< |
---|
604 | INTEGER(iwp) :: k !< |
---|
605 | |
---|
606 | REAL(wp) :: alpha !< |
---|
607 | REAL(wp) :: dr !< |
---|
608 | REAL(wp) :: e_s !< |
---|
609 | REAL(wp) :: evap !< |
---|
610 | REAL(wp) :: evap_nr !< |
---|
611 | REAL(wp) :: f_vent !< |
---|
612 | REAL(wp) :: g_evap !< |
---|
613 | REAL(wp) :: lambda_r !< |
---|
614 | REAL(wp) :: mu_r !< |
---|
615 | REAL(wp) :: mu_r_2 !< |
---|
616 | REAL(wp) :: mu_r_5d2 !< |
---|
617 | REAL(wp) :: nr_0 !< |
---|
618 | REAL(wp) :: q_s !< |
---|
619 | REAL(wp) :: sat !< |
---|
620 | REAL(wp) :: t_l !< |
---|
621 | REAL(wp) :: temp !< |
---|
622 | REAL(wp) :: xr !< |
---|
623 | |
---|
624 | CALL cpu_log( log_point_s(58), 'evaporation', 'start' ) |
---|
625 | |
---|
626 | DO i = nxl, nxr |
---|
627 | DO j = nys, nyn |
---|
628 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
629 | IF ( qr(k,j,i) > eps_sb ) THEN |
---|
630 | ! |
---|
631 | !-- Actual liquid water temperature: |
---|
632 | t_l = t_d_pt(k) * pt(k,j,i) |
---|
633 | ! |
---|
634 | !-- Saturation vapor pressure at t_l: |
---|
635 | e_s = 610.78_wp * EXP( 17.269_wp * ( t_l - 273.16_wp ) / & |
---|
636 | ( t_l - 35.86_wp ) & |
---|
637 | ) |
---|
638 | ! |
---|
639 | !-- Computation of saturation humidity: |
---|
640 | q_s = 0.622_wp * e_s / ( hyp(k) - 0.378_wp * e_s ) |
---|
641 | alpha = 0.622_wp * l_d_r * l_d_cp / ( t_l * t_l ) |
---|
642 | q_s = q_s * ( 1.0_wp + alpha * q(k,j,i) ) / & |
---|
643 | ( 1.0_wp + alpha * q_s ) |
---|
644 | ! |
---|
645 | !-- Supersaturation: |
---|
646 | sat = ( q(k,j,i) - qr(k,j,i) - qc(k,j,i) ) / q_s - 1.0_wp |
---|
647 | ! |
---|
648 | !-- Evaporation needs only to be calculated in subsaturated regions |
---|
649 | IF ( sat < 0.0_wp ) THEN |
---|
650 | ! |
---|
651 | !-- Actual temperature: |
---|
652 | temp = t_l + l_d_cp * ( qc(k,j,i) + qr(k,j,i) ) |
---|
653 | |
---|
654 | g_evap = 1.0_wp / ( ( l_v / ( r_v * temp ) - 1.0_wp ) * & |
---|
655 | l_v / ( thermal_conductivity_l * temp ) & |
---|
656 | + r_v * temp / ( diff_coeff_l * e_s ) & |
---|
657 | ) |
---|
658 | ! |
---|
659 | !-- Mean weight of rain drops |
---|
660 | xr = hyrho(k) * qr(k,j,i) / nr(k,j,i) |
---|
661 | ! |
---|
662 | !-- Weight averaged diameter of rain drops: |
---|
663 | dr = ( xr * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
664 | ! |
---|
665 | !-- Compute ventilation factor and intercept parameter |
---|
666 | !-- (Seifert and Beheng, 2006; Seifert, 2008): |
---|
667 | IF ( ventilation_effect ) THEN |
---|
668 | ! |
---|
669 | !-- Shape parameter of gamma distribution (Milbrandt and Yau, |
---|
670 | !-- 2005; Stevens and Seifert, 2008): |
---|
671 | mu_r = 10.0_wp * ( 1.0_wp + TANH( 1.2E3_wp * & |
---|
672 | ( dr - 1.4E-3_wp ) ) ) |
---|
673 | ! |
---|
674 | !-- Slope parameter of gamma distribution (Seifert, 2008): |
---|
675 | lambda_r = ( ( mu_r + 3.0_wp ) * ( mu_r + 2.0_wp ) * & |
---|
676 | ( mu_r + 1.0_wp ) & |
---|
677 | )**( 1.0_wp / 3.0_wp ) / dr |
---|
678 | |
---|
679 | mu_r_2 = mu_r + 2.0_wp |
---|
680 | mu_r_5d2 = mu_r + 2.5_wp |
---|
681 | |
---|
682 | f_vent = a_vent * gamm( mu_r_2 ) * & |
---|
683 | lambda_r**( -mu_r_2 ) + b_vent * & |
---|
684 | schmidt_p_1d3 * SQRT( a_term / kin_vis_air ) *& |
---|
685 | gamm( mu_r_5d2 ) * lambda_r**( -mu_r_5d2 ) * & |
---|
686 | ( 1.0_wp - & |
---|
687 | 0.5_wp * ( b_term / a_term ) * & |
---|
688 | ( lambda_r / ( c_term + lambda_r ) & |
---|
689 | )**mu_r_5d2 - & |
---|
690 | 0.125_wp * ( b_term / a_term )**2 * & |
---|
691 | ( lambda_r / ( 2.0_wp * c_term + lambda_r ) & |
---|
692 | )**mu_r_5d2 - & |
---|
693 | 0.0625_wp * ( b_term / a_term )**3 * & |
---|
694 | ( lambda_r / ( 3.0_wp * c_term + lambda_r ) & |
---|
695 | )**mu_r_5d2 - & |
---|
696 | 0.0390625_wp * ( b_term / a_term )**4 * & |
---|
697 | ( lambda_r / ( 4.0_wp * c_term + lambda_r ) & |
---|
698 | )**mu_r_5d2 & |
---|
699 | ) |
---|
700 | |
---|
701 | nr_0 = nr(k,j,i) * lambda_r**( mu_r + 1.0_wp ) / & |
---|
702 | gamm( mu_r + 1.0_wp ) |
---|
703 | ELSE |
---|
704 | f_vent = 1.0_wp |
---|
705 | nr_0 = nr(k,j,i) * dr |
---|
706 | ENDIF |
---|
707 | ! |
---|
708 | !-- Evaporation rate of rain water content (Seifert and |
---|
709 | !-- Beheng, 2006): |
---|
710 | evap = 2.0_wp * pi * nr_0 * g_evap * f_vent * sat / & |
---|
711 | hyrho(k) |
---|
712 | evap = MAX( evap, -qr(k,j,i) / dt_micro ) |
---|
713 | evap_nr = MAX( c_evap * evap / xr * hyrho(k), & |
---|
714 | -nr(k,j,i) / dt_micro ) |
---|
715 | |
---|
716 | qr(k,j,i) = qr(k,j,i) + evap * dt_micro |
---|
717 | nr(k,j,i) = nr(k,j,i) + evap_nr * dt_micro |
---|
718 | |
---|
719 | ENDIF |
---|
720 | ENDIF |
---|
721 | |
---|
722 | ENDDO |
---|
723 | ENDDO |
---|
724 | ENDDO |
---|
725 | |
---|
726 | CALL cpu_log( log_point_s(58), 'evaporation', 'stop' ) |
---|
727 | |
---|
728 | END SUBROUTINE evaporation_rain |
---|
729 | |
---|
730 | |
---|
731 | !------------------------------------------------------------------------------! |
---|
732 | ! Description: |
---|
733 | ! ------------ |
---|
734 | !> Sedimentation of cloud droplets (Ackermann et al., 2009, MWR). |
---|
735 | !------------------------------------------------------------------------------! |
---|
736 | SUBROUTINE sedimentation_cloud |
---|
737 | |
---|
738 | USE arrays_3d, & |
---|
739 | ONLY: ddzu, dzu, pt, q, qc |
---|
740 | |
---|
741 | USE cloud_parameters, & |
---|
742 | ONLY: eps_sb, hyrho, l_d_cp, nc_const, prr, pt_d_t, sed_qc_const |
---|
743 | |
---|
744 | USE constants, & |
---|
745 | ONLY: pi |
---|
746 | |
---|
747 | USE control_parameters, & |
---|
748 | ONLY: call_microphysics_at_all_substeps, dt_micro, & |
---|
749 | intermediate_timestep_count, precipitation |
---|
750 | |
---|
751 | USE cpulog, & |
---|
752 | ONLY: cpu_log, log_point_s |
---|
753 | |
---|
754 | USE indices, & |
---|
755 | ONLY: nxl, nxr, nys, nyn, nzb, nzb_s_inner, nzt |
---|
756 | |
---|
757 | USE kinds |
---|
758 | |
---|
759 | USE statistics, & |
---|
760 | ONLY: weight_substep |
---|
761 | |
---|
762 | |
---|
763 | IMPLICIT NONE |
---|
764 | |
---|
765 | INTEGER(iwp) :: i !< |
---|
766 | INTEGER(iwp) :: j !< |
---|
767 | INTEGER(iwp) :: k !< |
---|
768 | |
---|
769 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_qc !< |
---|
770 | |
---|
771 | CALL cpu_log( log_point_s(59), 'sed_cloud', 'start' ) |
---|
772 | |
---|
773 | sed_qc(nzt+1) = 0.0_wp |
---|
774 | |
---|
775 | DO i = nxl, nxr |
---|
776 | DO j = nys, nyn |
---|
777 | DO k = nzt, nzb_s_inner(j,i)+1, -1 |
---|
778 | |
---|
779 | IF ( qc(k,j,i) > eps_sb ) THEN |
---|
780 | sed_qc(k) = sed_qc_const * nc_const**( -2.0_wp / 3.0_wp ) * & |
---|
781 | ( qc(k,j,i) * hyrho(k) )**( 5.0_wp / 3.0_wp ) |
---|
782 | ELSE |
---|
783 | sed_qc(k) = 0.0_wp |
---|
784 | ENDIF |
---|
785 | |
---|
786 | sed_qc(k) = MIN( sed_qc(k), hyrho(k) * dzu(k+1) * q(k,j,i) / & |
---|
787 | dt_micro + sed_qc(k+1) & |
---|
788 | ) |
---|
789 | |
---|
790 | q(k,j,i) = q(k,j,i) + ( sed_qc(k+1) - sed_qc(k) ) * & |
---|
791 | ddzu(k+1) / hyrho(k) * dt_micro |
---|
792 | qc(k,j,i) = qc(k,j,i) + ( sed_qc(k+1) - sed_qc(k) ) * & |
---|
793 | ddzu(k+1) / hyrho(k) * dt_micro |
---|
794 | pt(k,j,i) = pt(k,j,i) - ( sed_qc(k+1) - sed_qc(k) ) * & |
---|
795 | ddzu(k+1) / hyrho(k) * l_d_cp * & |
---|
796 | pt_d_t(k) * dt_micro |
---|
797 | |
---|
798 | ! |
---|
799 | !-- Compute the precipitation rate due to cloud (fog) droplets |
---|
800 | IF ( precipitation ) THEN |
---|
801 | IF ( call_microphysics_at_all_substeps ) THEN |
---|
802 | prr(k,j,i) = prr(k,j,i) + sed_qc(k) / hyrho(k) & |
---|
803 | * weight_substep(intermediate_timestep_count) |
---|
804 | ELSE |
---|
805 | prr(k,j,i) = prr(k,j,i) + sed_qc(k) / hyrho(k) |
---|
806 | ENDIF |
---|
807 | ENDIF |
---|
808 | |
---|
809 | ENDDO |
---|
810 | ENDDO |
---|
811 | ENDDO |
---|
812 | |
---|
813 | CALL cpu_log( log_point_s(59), 'sed_cloud', 'stop' ) |
---|
814 | |
---|
815 | END SUBROUTINE sedimentation_cloud |
---|
816 | |
---|
817 | |
---|
818 | !------------------------------------------------------------------------------! |
---|
819 | ! Description: |
---|
820 | ! ------------ |
---|
821 | !> Computation of sedimentation flux. Implementation according to Stevens |
---|
822 | !> and Seifert (2008). Code is based on UCLA-LES. |
---|
823 | !------------------------------------------------------------------------------! |
---|
824 | SUBROUTINE sedimentation_rain |
---|
825 | |
---|
826 | USE arrays_3d, & |
---|
827 | ONLY: ddzu, dzu, nr, pt, q, qr |
---|
828 | |
---|
829 | USE cloud_parameters, & |
---|
830 | ONLY: a_term, b_term, c_term, cof, dpirho_l, eps_sb, hyrho, & |
---|
831 | limiter_sedimentation, l_d_cp, prr, pt_d_t, stp |
---|
832 | |
---|
833 | USE control_parameters, & |
---|
834 | ONLY: call_microphysics_at_all_substeps, dt_micro, & |
---|
835 | intermediate_timestep_count |
---|
836 | USE cpulog, & |
---|
837 | ONLY: cpu_log, log_point_s |
---|
838 | |
---|
839 | USE indices, & |
---|
840 | ONLY: nxl, nxr, nys, nyn, nzb, nzb_s_inner, nzt |
---|
841 | |
---|
842 | USE kinds |
---|
843 | |
---|
844 | USE statistics, & |
---|
845 | ONLY: weight_substep |
---|
846 | |
---|
847 | IMPLICIT NONE |
---|
848 | |
---|
849 | INTEGER(iwp) :: i !< |
---|
850 | INTEGER(iwp) :: j !< |
---|
851 | INTEGER(iwp) :: k !< |
---|
852 | INTEGER(iwp) :: k_run !< |
---|
853 | |
---|
854 | REAL(wp) :: c_run !< |
---|
855 | REAL(wp) :: d_max !< |
---|
856 | REAL(wp) :: d_mean !< |
---|
857 | REAL(wp) :: d_min !< |
---|
858 | REAL(wp) :: dr !< |
---|
859 | REAL(wp) :: dt_sedi !< |
---|
860 | REAL(wp) :: flux !< |
---|
861 | REAL(wp) :: lambda_r !< |
---|
862 | REAL(wp) :: mu_r !< |
---|
863 | REAL(wp) :: z_run !< |
---|
864 | |
---|
865 | REAL(wp), DIMENSION(nzb:nzt+1) :: c_nr !< |
---|
866 | REAL(wp), DIMENSION(nzb:nzt+1) :: c_qr !< |
---|
867 | REAL(wp), DIMENSION(nzb:nzt+1) :: d_nr !< |
---|
868 | REAL(wp), DIMENSION(nzb:nzt+1) :: d_qr !< |
---|
869 | REAL(wp), DIMENSION(nzb:nzt+1) :: nr_slope !< |
---|
870 | REAL(wp), DIMENSION(nzb:nzt+1) :: qr_slope !< |
---|
871 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_nr !< |
---|
872 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_qr !< |
---|
873 | REAL(wp), DIMENSION(nzb:nzt+1) :: w_nr !< |
---|
874 | REAL(wp), DIMENSION(nzb:nzt+1) :: w_qr !< |
---|
875 | |
---|
876 | CALL cpu_log( log_point_s(60), 'sed_rain', 'start' ) |
---|
877 | |
---|
878 | IF ( intermediate_timestep_count == 1 ) prr(:,:,:) = 0.0_wp |
---|
879 | ! |
---|
880 | !-- Compute velocities |
---|
881 | DO i = nxl, nxr |
---|
882 | DO j = nys, nyn |
---|
883 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
884 | IF ( qr(k,j,i) > eps_sb ) THEN |
---|
885 | ! |
---|
886 | !-- Weight averaged diameter of rain drops: |
---|
887 | dr = ( hyrho(k) * qr(k,j,i) / & |
---|
888 | nr(k,j,i) * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
889 | ! |
---|
890 | !-- Shape parameter of gamma distribution (Milbrandt and Yau, 2005; |
---|
891 | !-- Stevens and Seifert, 2008): |
---|
892 | mu_r = 10.0_wp * ( 1.0_wp + TANH( 1.2E3_wp * & |
---|
893 | ( dr - 1.4E-3_wp ) ) ) |
---|
894 | ! |
---|
895 | !-- Slope parameter of gamma distribution (Seifert, 2008): |
---|
896 | lambda_r = ( ( mu_r + 3.0_wp ) * ( mu_r + 2.0_wp ) * & |
---|
897 | ( mu_r + 1.0_wp ) )**( 1.0_wp / 3.0_wp ) / dr |
---|
898 | |
---|
899 | w_nr(k) = MAX( 0.1_wp, MIN( 20.0_wp, & |
---|
900 | a_term - b_term * ( 1.0_wp + & |
---|
901 | c_term / & |
---|
902 | lambda_r )**( -1.0_wp * & |
---|
903 | ( mu_r + 1.0_wp ) ) & |
---|
904 | ) & |
---|
905 | ) |
---|
906 | |
---|
907 | w_qr(k) = MAX( 0.1_wp, MIN( 20.0_wp, & |
---|
908 | a_term - b_term * ( 1.0_wp + & |
---|
909 | c_term / & |
---|
910 | lambda_r )**( -1.0_wp * & |
---|
911 | ( mu_r + 4.0_wp ) ) & |
---|
912 | ) & |
---|
913 | ) |
---|
914 | ELSE |
---|
915 | w_nr(k) = 0.0_wp |
---|
916 | w_qr(k) = 0.0_wp |
---|
917 | ENDIF |
---|
918 | ENDDO |
---|
919 | ! |
---|
920 | !-- Adjust boundary values |
---|
921 | w_nr(nzb_s_inner(j,i)) = w_nr(nzb_s_inner(j,i)+1) |
---|
922 | w_qr(nzb_s_inner(j,i)) = w_qr(nzb_s_inner(j,i)+1) |
---|
923 | w_nr(nzt+1) = 0.0_wp |
---|
924 | w_qr(nzt+1) = 0.0_wp |
---|
925 | ! |
---|
926 | !-- Compute Courant number |
---|
927 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
928 | c_nr(k) = 0.25_wp * ( w_nr(k-1) + & |
---|
929 | 2.0_wp * w_nr(k) + w_nr(k+1) ) * & |
---|
930 | dt_micro * ddzu(k) |
---|
931 | c_qr(k) = 0.25_wp * ( w_qr(k-1) + & |
---|
932 | 2.0_wp * w_qr(k) + w_qr(k+1) ) * & |
---|
933 | dt_micro * ddzu(k) |
---|
934 | ENDDO |
---|
935 | ! |
---|
936 | !-- Limit slopes with monotonized centered (MC) limiter (van Leer, 1977): |
---|
937 | IF ( limiter_sedimentation ) THEN |
---|
938 | |
---|
939 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
940 | d_mean = 0.5_wp * ( qr(k+1,j,i) - qr(k-1,j,i) ) |
---|
941 | d_min = qr(k,j,i) - MIN( qr(k+1,j,i), qr(k,j,i), qr(k-1,j,i) ) |
---|
942 | d_max = MAX( qr(k+1,j,i), qr(k,j,i), qr(k-1,j,i) ) - qr(k,j,i) |
---|
943 | |
---|
944 | qr_slope(k) = SIGN(1.0_wp, d_mean) * MIN ( 2.0_wp * d_min, & |
---|
945 | 2.0_wp * d_max, & |
---|
946 | ABS( d_mean ) ) |
---|
947 | |
---|
948 | d_mean = 0.5_wp * ( nr(k+1,j,i) - nr(k-1,j,i) ) |
---|
949 | d_min = nr(k,j,i) - MIN( nr(k+1,j,i), nr(k,j,i), nr(k-1,j,i) ) |
---|
950 | d_max = MAX( nr(k+1,j,i), nr(k,j,i), nr(k-1,j,i) ) - nr(k,j,i) |
---|
951 | |
---|
952 | nr_slope(k) = SIGN(1.0_wp, d_mean) * MIN ( 2.0_wp * d_min, & |
---|
953 | 2.0_wp * d_max, & |
---|
954 | ABS( d_mean ) ) |
---|
955 | ENDDO |
---|
956 | |
---|
957 | ELSE |
---|
958 | |
---|
959 | nr_slope = 0.0_wp |
---|
960 | qr_slope = 0.0_wp |
---|
961 | |
---|
962 | ENDIF |
---|
963 | |
---|
964 | sed_nr(nzt+1) = 0.0_wp |
---|
965 | sed_qr(nzt+1) = 0.0_wp |
---|
966 | ! |
---|
967 | !-- Compute sedimentation flux |
---|
968 | DO k = nzt, nzb_s_inner(j,i)+1, -1 |
---|
969 | ! |
---|
970 | !-- Sum up all rain drop number densities which contribute to the flux |
---|
971 | !-- through k-1/2 |
---|
972 | flux = 0.0_wp |
---|
973 | z_run = 0.0_wp ! height above z(k) |
---|
974 | k_run = k |
---|
975 | c_run = MIN( 1.0_wp, c_nr(k) ) |
---|
976 | DO WHILE ( c_run > 0.0_wp .AND. k_run <= nzt ) |
---|
977 | flux = flux + hyrho(k_run) * & |
---|
978 | ( nr(k_run,j,i) + nr_slope(k_run) * & |
---|
979 | ( 1.0_wp - c_run ) * 0.5_wp ) * c_run * dzu(k_run) |
---|
980 | z_run = z_run + dzu(k_run) |
---|
981 | k_run = k_run + 1 |
---|
982 | c_run = MIN( 1.0_wp, c_nr(k_run) - z_run * ddzu(k_run) ) |
---|
983 | ENDDO |
---|
984 | ! |
---|
985 | !-- It is not allowed to sediment more rain drop number density than |
---|
986 | !-- available |
---|
987 | flux = MIN( flux, & |
---|
988 | hyrho(k) * dzu(k+1) * nr(k,j,i) + sed_nr(k+1) * & |
---|
989 | dt_micro & |
---|
990 | ) |
---|
991 | |
---|
992 | sed_nr(k) = flux / dt_micro |
---|
993 | nr(k,j,i) = nr(k,j,i) + ( sed_nr(k+1) - sed_nr(k) ) * & |
---|
994 | ddzu(k+1) / hyrho(k) * dt_micro |
---|
995 | ! |
---|
996 | !-- Sum up all rain water content which contributes to the flux |
---|
997 | !-- through k-1/2 |
---|
998 | flux = 0.0_wp |
---|
999 | z_run = 0.0_wp ! height above z(k) |
---|
1000 | k_run = k |
---|
1001 | c_run = MIN( 1.0_wp, c_qr(k) ) |
---|
1002 | |
---|
1003 | DO WHILE ( c_run > 0.0_wp .AND. k_run <= nzt ) |
---|
1004 | |
---|
1005 | flux = flux + hyrho(k_run) * ( qr(k_run,j,i) + & |
---|
1006 | qr_slope(k_run) * ( 1.0_wp - c_run ) * & |
---|
1007 | 0.5_wp ) * c_run * dzu(k_run) |
---|
1008 | z_run = z_run + dzu(k_run) |
---|
1009 | k_run = k_run + 1 |
---|
1010 | c_run = MIN( 1.0_wp, c_qr(k_run) - z_run * ddzu(k_run) ) |
---|
1011 | |
---|
1012 | ENDDO |
---|
1013 | ! |
---|
1014 | !-- It is not allowed to sediment more rain water content than |
---|
1015 | !-- available |
---|
1016 | flux = MIN( flux, & |
---|
1017 | hyrho(k) * dzu(k) * qr(k,j,i) + sed_qr(k+1) * & |
---|
1018 | dt_micro & |
---|
1019 | ) |
---|
1020 | |
---|
1021 | sed_qr(k) = flux / dt_micro |
---|
1022 | |
---|
1023 | qr(k,j,i) = qr(k,j,i) + ( sed_qr(k+1) - sed_qr(k) ) * & |
---|
1024 | ddzu(k+1) / hyrho(k) * dt_micro |
---|
1025 | q(k,j,i) = q(k,j,i) + ( sed_qr(k+1) - sed_qr(k) ) * & |
---|
1026 | ddzu(k+1) / hyrho(k) * dt_micro |
---|
1027 | pt(k,j,i) = pt(k,j,i) - ( sed_qr(k+1) - sed_qr(k) ) * & |
---|
1028 | ddzu(k+1) / hyrho(k) * l_d_cp * & |
---|
1029 | pt_d_t(k) * dt_micro |
---|
1030 | ! |
---|
1031 | !-- Compute the rain rate |
---|
1032 | IF ( call_microphysics_at_all_substeps ) THEN |
---|
1033 | prr(k,j,i) = prr(k,j,i) + sed_qr(k) / hyrho(k) & |
---|
1034 | * weight_substep(intermediate_timestep_count) |
---|
1035 | ELSE |
---|
1036 | prr(k,j,i) = prr(k,j,i) + sed_qr(k) / hyrho(k) |
---|
1037 | ENDIF |
---|
1038 | |
---|
1039 | ENDDO |
---|
1040 | ENDDO |
---|
1041 | ENDDO |
---|
1042 | |
---|
1043 | CALL cpu_log( log_point_s(60), 'sed_rain', 'stop' ) |
---|
1044 | |
---|
1045 | END SUBROUTINE sedimentation_rain |
---|
1046 | |
---|
1047 | |
---|
1048 | !------------------------------------------------------------------------------! |
---|
1049 | ! Description: |
---|
1050 | ! ------------ |
---|
1051 | !> Computation of the precipitation amount due to gravitational settling of |
---|
1052 | !> rain and cloud (fog) droplets |
---|
1053 | !------------------------------------------------------------------------------! |
---|
1054 | SUBROUTINE calc_precipitation_amount |
---|
1055 | |
---|
1056 | USE cloud_parameters, & |
---|
1057 | ONLY: hyrho, precipitation_amount, prr |
---|
1058 | |
---|
1059 | USE control_parameters, & |
---|
1060 | ONLY: call_microphysics_at_all_substeps, dt_do2d_xy, dt_3d, & |
---|
1061 | intermediate_timestep_count, intermediate_timestep_count_max,& |
---|
1062 | precipitation_amount_interval, time_do2d_xy |
---|
1063 | |
---|
1064 | USE indices, & |
---|
1065 | ONLY: nxl, nxr, nys, nyn, nzb_s_inner |
---|
1066 | |
---|
1067 | USE kinds |
---|
1068 | |
---|
1069 | IMPLICIT NONE |
---|
1070 | |
---|
1071 | INTEGER(iwp) :: i !: |
---|
1072 | INTEGER(iwp) :: j !: |
---|
1073 | |
---|
1074 | |
---|
1075 | IF ( ( dt_do2d_xy - time_do2d_xy ) < precipitation_amount_interval .AND.& |
---|
1076 | ( .NOT. call_microphysics_at_all_substeps .OR. & |
---|
1077 | intermediate_timestep_count == intermediate_timestep_count_max ) ) & |
---|
1078 | THEN |
---|
1079 | |
---|
1080 | DO i = nxl, nxr |
---|
1081 | DO j = nys, nyn |
---|
1082 | |
---|
1083 | precipitation_amount(j,i) = precipitation_amount(j,i) + & |
---|
1084 | prr(nzb_s_inner(j,i)+1,j,i) * & |
---|
1085 | hyrho(nzb_s_inner(j,i)+1) * dt_3d |
---|
1086 | |
---|
1087 | ENDDO |
---|
1088 | ENDDO |
---|
1089 | ENDIF |
---|
1090 | |
---|
1091 | END SUBROUTINE calc_precipitation_amount |
---|
1092 | |
---|
1093 | |
---|
1094 | !------------------------------------------------------------------------------! |
---|
1095 | ! Description: |
---|
1096 | ! ------------ |
---|
1097 | !> Call for grid point i,j |
---|
1098 | !------------------------------------------------------------------------------! |
---|
1099 | |
---|
1100 | SUBROUTINE microphysics_control_ij( i, j ) |
---|
1101 | |
---|
1102 | USE arrays_3d, & |
---|
1103 | ONLY: hyp, nc_1d, nr, nr_1d, pt, pt_init, pt_1d, q, q_1d, qc, & |
---|
1104 | qc_1d, qr, qr_1d, zu |
---|
1105 | |
---|
1106 | USE cloud_parameters, & |
---|
1107 | ONLY: cp, hyrho, nc_const, pt_d_t, r_d, t_d_pt |
---|
1108 | |
---|
1109 | USE control_parameters, & |
---|
1110 | ONLY: call_microphysics_at_all_substeps, drizzle, dt_3d, dt_micro, & |
---|
1111 | g, intermediate_timestep_count, large_scale_forcing, & |
---|
1112 | lsf_surf, precipitation, pt_surface, & |
---|
1113 | rho_surface,surface_pressure |
---|
1114 | |
---|
1115 | USE indices, & |
---|
1116 | ONLY: nzb, nzt |
---|
1117 | |
---|
1118 | USE kinds |
---|
1119 | |
---|
1120 | USE statistics, & |
---|
1121 | ONLY: weight_pres |
---|
1122 | |
---|
1123 | IMPLICIT NONE |
---|
1124 | |
---|
1125 | INTEGER(iwp) :: i !< |
---|
1126 | INTEGER(iwp) :: j !< |
---|
1127 | INTEGER(iwp) :: k !< |
---|
1128 | |
---|
1129 | REAL(wp) :: t_surface !< |
---|
1130 | |
---|
1131 | IF ( large_scale_forcing .AND. lsf_surf ) THEN |
---|
1132 | ! |
---|
1133 | !-- Calculate: |
---|
1134 | !-- pt / t : ratio of potential and actual temperature (pt_d_t) |
---|
1135 | !-- t / pt : ratio of actual and potential temperature (t_d_pt) |
---|
1136 | !-- p_0(z) : vertical profile of the hydrostatic pressure (hyp) |
---|
1137 | t_surface = pt_surface * ( surface_pressure / 1000.0_wp )**0.286_wp |
---|
1138 | DO k = nzb, nzt+1 |
---|
1139 | hyp(k) = surface_pressure * 100.0_wp * & |
---|
1140 | ( ( t_surface - g / cp * zu(k) ) / t_surface )**(1.0_wp / 0.286_wp) |
---|
1141 | pt_d_t(k) = ( 100000.0_wp / hyp(k) )**0.286_wp |
---|
1142 | t_d_pt(k) = 1.0_wp / pt_d_t(k) |
---|
1143 | hyrho(k) = hyp(k) / ( r_d * t_d_pt(k) * pt_init(k) ) |
---|
1144 | ENDDO |
---|
1145 | ! |
---|
1146 | !-- Compute reference density |
---|
1147 | rho_surface = surface_pressure * 100.0_wp / ( r_d * t_surface ) |
---|
1148 | ENDIF |
---|
1149 | |
---|
1150 | ! |
---|
1151 | !-- Compute length of time step |
---|
1152 | IF ( call_microphysics_at_all_substeps ) THEN |
---|
1153 | dt_micro = dt_3d * weight_pres(intermediate_timestep_count) |
---|
1154 | ELSE |
---|
1155 | dt_micro = dt_3d |
---|
1156 | ENDIF |
---|
1157 | |
---|
1158 | ! |
---|
1159 | !-- Use 1d arrays |
---|
1160 | q_1d(:) = q(:,j,i) |
---|
1161 | pt_1d(:) = pt(:,j,i) |
---|
1162 | qc_1d(:) = qc(:,j,i) |
---|
1163 | nc_1d(:) = nc_const |
---|
1164 | IF ( precipitation ) THEN |
---|
1165 | qr_1d(:) = qr(:,j,i) |
---|
1166 | nr_1d(:) = nr(:,j,i) |
---|
1167 | ENDIF |
---|
1168 | |
---|
1169 | ! |
---|
1170 | !-- Compute cloud physics |
---|
1171 | IF ( precipitation ) THEN |
---|
1172 | CALL adjust_cloud( i,j ) |
---|
1173 | CALL autoconversion( i,j ) |
---|
1174 | CALL accretion( i,j ) |
---|
1175 | CALL selfcollection_breakup( i,j ) |
---|
1176 | CALL evaporation_rain( i,j ) |
---|
1177 | CALL sedimentation_rain( i,j ) |
---|
1178 | ENDIF |
---|
1179 | |
---|
1180 | IF ( drizzle ) CALL sedimentation_cloud( i,j ) |
---|
1181 | |
---|
1182 | IF ( precipitation ) THEN |
---|
1183 | CALL calc_precipitation_amount( i,j ) |
---|
1184 | ENDIF |
---|
1185 | |
---|
1186 | ! |
---|
1187 | !-- Store results on the 3d arrays |
---|
1188 | q(:,j,i) = q_1d(:) |
---|
1189 | pt(:,j,i) = pt_1d(:) |
---|
1190 | IF ( precipitation ) THEN |
---|
1191 | qr(:,j,i) = qr_1d(:) |
---|
1192 | nr(:,j,i) = nr_1d(:) |
---|
1193 | ENDIF |
---|
1194 | |
---|
1195 | END SUBROUTINE microphysics_control_ij |
---|
1196 | |
---|
1197 | !------------------------------------------------------------------------------! |
---|
1198 | ! Description: |
---|
1199 | ! ------------ |
---|
1200 | !> Adjust number of raindrops to avoid nonlinear effects in |
---|
1201 | !> sedimentation and evaporation of rain drops due to too small or |
---|
1202 | !> too big weights of rain drops (Stevens and Seifert, 2008). |
---|
1203 | !> The same procedure is applied to cloud droplets if they are determined |
---|
1204 | !> prognostically. Call for grid point i,j |
---|
1205 | !------------------------------------------------------------------------------! |
---|
1206 | SUBROUTINE adjust_cloud_ij( i, j ) |
---|
1207 | |
---|
1208 | USE arrays_3d, & |
---|
1209 | ONLY: qr_1d, nr_1d |
---|
1210 | |
---|
1211 | USE cloud_parameters, & |
---|
1212 | ONLY: eps_sb, xrmin, xrmax, hyrho, k_cc, x0 |
---|
1213 | |
---|
1214 | USE indices, & |
---|
1215 | ONLY: nzb, nzb_s_inner, nzt |
---|
1216 | |
---|
1217 | USE kinds |
---|
1218 | |
---|
1219 | IMPLICIT NONE |
---|
1220 | |
---|
1221 | INTEGER(iwp) :: i !< |
---|
1222 | INTEGER(iwp) :: j !< |
---|
1223 | INTEGER(iwp) :: k !< |
---|
1224 | |
---|
1225 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
1226 | |
---|
1227 | IF ( qr_1d(k) <= eps_sb ) THEN |
---|
1228 | qr_1d(k) = 0.0_wp |
---|
1229 | nr_1d(k) = 0.0_wp |
---|
1230 | ELSE |
---|
1231 | ! |
---|
1232 | !-- Adjust number of raindrops to avoid nonlinear effects in |
---|
1233 | !-- sedimentation and evaporation of rain drops due to too small or |
---|
1234 | !-- too big weights of rain drops (Stevens and Seifert, 2008). |
---|
1235 | IF ( nr_1d(k) * xrmin > qr_1d(k) * hyrho(k) ) THEN |
---|
1236 | nr_1d(k) = qr_1d(k) * hyrho(k) / xrmin |
---|
1237 | ELSEIF ( nr_1d(k) * xrmax < qr_1d(k) * hyrho(k) ) THEN |
---|
1238 | nr_1d(k) = qr_1d(k) * hyrho(k) / xrmax |
---|
1239 | ENDIF |
---|
1240 | |
---|
1241 | ENDIF |
---|
1242 | |
---|
1243 | ENDDO |
---|
1244 | |
---|
1245 | END SUBROUTINE adjust_cloud_ij |
---|
1246 | |
---|
1247 | |
---|
1248 | !------------------------------------------------------------------------------! |
---|
1249 | ! Description: |
---|
1250 | ! ------------ |
---|
1251 | !> Autoconversion rate (Seifert and Beheng, 2006). Call for grid point i,j |
---|
1252 | !------------------------------------------------------------------------------! |
---|
1253 | SUBROUTINE autoconversion_ij( i, j ) |
---|
1254 | |
---|
1255 | USE arrays_3d, & |
---|
1256 | ONLY: diss, dzu, nc_1d, nr_1d, qc_1d, qr_1d |
---|
1257 | |
---|
1258 | USE cloud_parameters, & |
---|
1259 | ONLY: a_1, a_2, a_3, b_1, b_2, b_3, beta_cc, c_1, c_2, c_3, & |
---|
1260 | c_const, dpirho_l, eps_sb, hyrho, k_cc, kin_vis_air, x0 |
---|
1261 | |
---|
1262 | USE control_parameters, & |
---|
1263 | ONLY: dt_micro, rho_surface, turbulence |
---|
1264 | |
---|
1265 | USE grid_variables, & |
---|
1266 | ONLY: dx, dy |
---|
1267 | |
---|
1268 | USE indices, & |
---|
1269 | ONLY: nzb, nzb_s_inner, nzt |
---|
1270 | |
---|
1271 | USE kinds |
---|
1272 | |
---|
1273 | IMPLICIT NONE |
---|
1274 | |
---|
1275 | INTEGER(iwp) :: i !< |
---|
1276 | INTEGER(iwp) :: j !< |
---|
1277 | INTEGER(iwp) :: k !< |
---|
1278 | |
---|
1279 | REAL(wp) :: alpha_cc !< |
---|
1280 | REAL(wp) :: autocon !< |
---|
1281 | REAL(wp) :: dissipation !< |
---|
1282 | REAL(wp) :: k_au !< |
---|
1283 | REAL(wp) :: l_mix !< |
---|
1284 | REAL(wp) :: nu_c !< |
---|
1285 | REAL(wp) :: phi_au !< |
---|
1286 | REAL(wp) :: r_cc !< |
---|
1287 | REAL(wp) :: rc !< |
---|
1288 | REAL(wp) :: re_lambda !< |
---|
1289 | REAL(wp) :: selfcoll !< |
---|
1290 | REAL(wp) :: sigma_cc !< |
---|
1291 | REAL(wp) :: tau_cloud !< |
---|
1292 | REAL(wp) :: xc !< |
---|
1293 | |
---|
1294 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
1295 | |
---|
1296 | IF ( qc_1d(k) > eps_sb ) THEN |
---|
1297 | |
---|
1298 | k_au = k_cc / ( 20.0_wp * x0 ) |
---|
1299 | ! |
---|
1300 | !-- Intern time scale of coagulation (Seifert and Beheng, 2006): |
---|
1301 | !-- (1.0_wp - qc(k,j,i) / ( qc(k,j,i) + qr_1d(k) )) |
---|
1302 | tau_cloud = 1.0_wp - qc_1d(k) / ( qr_1d(k) + qc_1d(k) ) |
---|
1303 | ! |
---|
1304 | !-- Universal function for autoconversion process |
---|
1305 | !-- (Seifert and Beheng, 2006): |
---|
1306 | phi_au = 600.0_wp * tau_cloud**0.68_wp * ( 1.0_wp - tau_cloud**0.68_wp )**3 |
---|
1307 | ! |
---|
1308 | !-- Shape parameter of gamma distribution (Geoffroy et al., 2010): |
---|
1309 | !-- (Use constant nu_c = 1.0_wp instead?) |
---|
1310 | nu_c = 1.0_wp !MAX( 0.0_wp, 1580.0_wp * hyrho(k) * qc_1d(k) - 0.28_wp ) |
---|
1311 | ! |
---|
1312 | !-- Mean weight of cloud droplets: |
---|
1313 | xc = hyrho(k) * qc_1d(k) / nc_1d(k) |
---|
1314 | ! |
---|
1315 | !-- Parameterized turbulence effects on autoconversion (Seifert, |
---|
1316 | !-- Nuijens and Stevens, 2010) |
---|
1317 | IF ( turbulence ) THEN |
---|
1318 | ! |
---|
1319 | !-- Weight averaged radius of cloud droplets: |
---|
1320 | rc = 0.5_wp * ( xc * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
1321 | |
---|
1322 | alpha_cc = ( a_1 + a_2 * nu_c ) / ( 1.0_wp + a_3 * nu_c ) |
---|
1323 | r_cc = ( b_1 + b_2 * nu_c ) / ( 1.0_wp + b_3 * nu_c ) |
---|
1324 | sigma_cc = ( c_1 + c_2 * nu_c ) / ( 1.0_wp + c_3 * nu_c ) |
---|
1325 | ! |
---|
1326 | !-- Mixing length (neglecting distance to ground and stratification) |
---|
1327 | l_mix = ( dx * dy * dzu(k) )**( 1.0_wp / 3.0_wp ) |
---|
1328 | ! |
---|
1329 | !-- Limit dissipation rate according to Seifert, Nuijens and |
---|
1330 | !-- Stevens (2010) |
---|
1331 | dissipation = MIN( 0.06_wp, diss(k,j,i) ) |
---|
1332 | ! |
---|
1333 | !-- Compute Taylor-microscale Reynolds number: |
---|
1334 | re_lambda = 6.0_wp / 11.0_wp * & |
---|
1335 | ( l_mix / c_const )**( 2.0_wp / 3.0_wp ) * & |
---|
1336 | SQRT( 15.0_wp / kin_vis_air ) * & |
---|
1337 | dissipation**( 1.0_wp / 6.0_wp ) |
---|
1338 | ! |
---|
1339 | !-- The factor of 1.0E4 is needed to convert the dissipation rate |
---|
1340 | !-- from m2 s-3 to cm2 s-3. |
---|
1341 | k_au = k_au * ( 1.0_wp + & |
---|
1342 | dissipation * 1.0E4_wp * & |
---|
1343 | ( re_lambda * 1.0E-3_wp )**0.25_wp * & |
---|
1344 | ( alpha_cc * EXP( -1.0_wp * ( ( rc - r_cc ) / & |
---|
1345 | sigma_cc )**2 & |
---|
1346 | ) + beta_cc & |
---|
1347 | ) & |
---|
1348 | ) |
---|
1349 | ENDIF |
---|
1350 | ! |
---|
1351 | !-- Autoconversion rate (Seifert and Beheng, 2006): |
---|
1352 | autocon = k_au * ( nu_c + 2.0_wp ) * ( nu_c + 4.0_wp ) / & |
---|
1353 | ( nu_c + 1.0_wp )**2 * qc_1d(k)**2 * xc**2 * & |
---|
1354 | ( 1.0_wp + phi_au / ( 1.0_wp - tau_cloud )**2 ) * & |
---|
1355 | rho_surface |
---|
1356 | autocon = MIN( autocon, qc_1d(k) / dt_micro ) |
---|
1357 | |
---|
1358 | qr_1d(k) = qr_1d(k) + autocon * dt_micro |
---|
1359 | qc_1d(k) = qc_1d(k) - autocon * dt_micro |
---|
1360 | nr_1d(k) = nr_1d(k) + autocon / x0 * hyrho(k) * dt_micro |
---|
1361 | |
---|
1362 | ENDIF |
---|
1363 | |
---|
1364 | ENDDO |
---|
1365 | |
---|
1366 | END SUBROUTINE autoconversion_ij |
---|
1367 | |
---|
1368 | |
---|
1369 | !------------------------------------------------------------------------------! |
---|
1370 | ! Description: |
---|
1371 | ! ------------ |
---|
1372 | !> Accretion rate (Seifert and Beheng, 2006). Call for grid point i,j |
---|
1373 | !------------------------------------------------------------------------------! |
---|
1374 | SUBROUTINE accretion_ij( i, j ) |
---|
1375 | |
---|
1376 | USE arrays_3d, & |
---|
1377 | ONLY: diss, qc_1d, qr_1d |
---|
1378 | |
---|
1379 | USE cloud_parameters, & |
---|
1380 | ONLY: eps_sb, hyrho, k_cr0 |
---|
1381 | |
---|
1382 | USE control_parameters, & |
---|
1383 | ONLY: dt_micro, rho_surface, turbulence |
---|
1384 | |
---|
1385 | USE indices, & |
---|
1386 | ONLY: nzb, nzb_s_inner, nzt |
---|
1387 | |
---|
1388 | USE kinds |
---|
1389 | |
---|
1390 | IMPLICIT NONE |
---|
1391 | |
---|
1392 | INTEGER(iwp) :: i !< |
---|
1393 | INTEGER(iwp) :: j !< |
---|
1394 | INTEGER(iwp) :: k !< |
---|
1395 | |
---|
1396 | REAL(wp) :: accr !< |
---|
1397 | REAL(wp) :: k_cr !< |
---|
1398 | REAL(wp) :: phi_ac !< |
---|
1399 | REAL(wp) :: tau_cloud !< |
---|
1400 | REAL(wp) :: xc !< |
---|
1401 | |
---|
1402 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
1403 | IF ( ( qc_1d(k) > eps_sb ) .AND. ( qr_1d(k) > eps_sb ) ) THEN |
---|
1404 | ! |
---|
1405 | !-- Intern time scale of coagulation (Seifert and Beheng, 2006): |
---|
1406 | tau_cloud = 1.0_wp - qc_1d(k) / ( qc_1d(k) + qr_1d(k) ) |
---|
1407 | ! |
---|
1408 | !-- Universal function for accretion process |
---|
1409 | !-- (Seifert and Beheng, 2001): |
---|
1410 | phi_ac = ( tau_cloud / ( tau_cloud + 5.0E-5_wp ) )**4 |
---|
1411 | ! |
---|
1412 | !-- Parameterized turbulence effects on autoconversion (Seifert, |
---|
1413 | !-- Nuijens and Stevens, 2010). The factor of 1.0E4 is needed to |
---|
1414 | !-- convert the dissipation rate (diss) from m2 s-3 to cm2 s-3. |
---|
1415 | IF ( turbulence ) THEN |
---|
1416 | k_cr = k_cr0 * ( 1.0_wp + 0.05_wp * & |
---|
1417 | MIN( 600.0_wp, & |
---|
1418 | diss(k,j,i) * 1.0E4_wp )**0.25_wp & |
---|
1419 | ) |
---|
1420 | ELSE |
---|
1421 | k_cr = k_cr0 |
---|
1422 | ENDIF |
---|
1423 | ! |
---|
1424 | !-- Accretion rate (Seifert and Beheng, 2006): |
---|
1425 | accr = k_cr * qc_1d(k) * qr_1d(k) * phi_ac * SQRT( rho_surface * hyrho(k) ) |
---|
1426 | accr = MIN( accr, qc_1d(k) / dt_micro ) |
---|
1427 | |
---|
1428 | qr_1d(k) = qr_1d(k) + accr * dt_micro |
---|
1429 | qc_1d(k) = qc_1d(k) - accr * dt_micro |
---|
1430 | |
---|
1431 | ENDIF |
---|
1432 | |
---|
1433 | ENDDO |
---|
1434 | |
---|
1435 | END SUBROUTINE accretion_ij |
---|
1436 | |
---|
1437 | |
---|
1438 | !------------------------------------------------------------------------------! |
---|
1439 | ! Description: |
---|
1440 | ! ------------ |
---|
1441 | !> Collisional breakup rate (Seifert, 2008). Call for grid point i,j |
---|
1442 | !------------------------------------------------------------------------------! |
---|
1443 | SUBROUTINE selfcollection_breakup_ij( i, j ) |
---|
1444 | |
---|
1445 | USE arrays_3d, & |
---|
1446 | ONLY: nr_1d, qr_1d |
---|
1447 | |
---|
1448 | USE cloud_parameters, & |
---|
1449 | ONLY: dpirho_l, eps_sb, hyrho, k_br, k_rr |
---|
1450 | |
---|
1451 | USE control_parameters, & |
---|
1452 | ONLY: dt_micro, rho_surface |
---|
1453 | |
---|
1454 | USE indices, & |
---|
1455 | ONLY: nzb, nzb_s_inner, nzt |
---|
1456 | |
---|
1457 | USE kinds |
---|
1458 | |
---|
1459 | IMPLICIT NONE |
---|
1460 | |
---|
1461 | INTEGER(iwp) :: i !< |
---|
1462 | INTEGER(iwp) :: j !< |
---|
1463 | INTEGER(iwp) :: k !< |
---|
1464 | |
---|
1465 | REAL(wp) :: breakup !< |
---|
1466 | REAL(wp) :: dr !< |
---|
1467 | REAL(wp) :: phi_br !< |
---|
1468 | REAL(wp) :: selfcoll !< |
---|
1469 | |
---|
1470 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
1471 | IF ( qr_1d(k) > eps_sb ) THEN |
---|
1472 | ! |
---|
1473 | !-- Selfcollection rate (Seifert and Beheng, 2001): |
---|
1474 | selfcoll = k_rr * nr_1d(k) * qr_1d(k) * SQRT( hyrho(k) * rho_surface ) |
---|
1475 | ! |
---|
1476 | !-- Weight averaged diameter of rain drops: |
---|
1477 | dr = ( hyrho(k) * qr_1d(k) / nr_1d(k) * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
1478 | ! |
---|
1479 | !-- Collisional breakup rate (Seifert, 2008): |
---|
1480 | IF ( dr >= 0.3E-3_wp ) THEN |
---|
1481 | phi_br = k_br * ( dr - 1.1E-3_wp ) |
---|
1482 | breakup = selfcoll * ( phi_br + 1.0_wp ) |
---|
1483 | ELSE |
---|
1484 | breakup = 0.0_wp |
---|
1485 | ENDIF |
---|
1486 | |
---|
1487 | selfcoll = MAX( breakup - selfcoll, -nr_1d(k) / dt_micro ) |
---|
1488 | nr_1d(k) = nr_1d(k) + selfcoll * dt_micro |
---|
1489 | |
---|
1490 | ENDIF |
---|
1491 | ENDDO |
---|
1492 | |
---|
1493 | END SUBROUTINE selfcollection_breakup_ij |
---|
1494 | |
---|
1495 | |
---|
1496 | !------------------------------------------------------------------------------! |
---|
1497 | ! Description: |
---|
1498 | ! ------------ |
---|
1499 | !> Evaporation of precipitable water. Condensation is neglected for |
---|
1500 | !> precipitable water. Call for grid point i,j |
---|
1501 | !------------------------------------------------------------------------------! |
---|
1502 | SUBROUTINE evaporation_rain_ij( i, j ) |
---|
1503 | |
---|
1504 | USE arrays_3d, & |
---|
1505 | ONLY: hyp, nr_1d, pt_1d, q_1d, qc_1d, qr_1d |
---|
1506 | |
---|
1507 | USE cloud_parameters, & |
---|
1508 | ONLY: a_term, a_vent, b_term, b_vent, c_evap, c_term, diff_coeff_l,& |
---|
1509 | dpirho_l, eps_sb, hyrho, kin_vis_air, k_st, l_d_cp, l_d_r, & |
---|
1510 | l_v, rho_l, r_v, schmidt_p_1d3, thermal_conductivity_l, & |
---|
1511 | t_d_pt, ventilation_effect |
---|
1512 | |
---|
1513 | USE constants, & |
---|
1514 | ONLY: pi |
---|
1515 | |
---|
1516 | USE control_parameters, & |
---|
1517 | ONLY: dt_micro |
---|
1518 | |
---|
1519 | USE indices, & |
---|
1520 | ONLY: nzb, nzb_s_inner, nzt |
---|
1521 | |
---|
1522 | USE kinds |
---|
1523 | |
---|
1524 | IMPLICIT NONE |
---|
1525 | |
---|
1526 | INTEGER(iwp) :: i !< |
---|
1527 | INTEGER(iwp) :: j !< |
---|
1528 | INTEGER(iwp) :: k !< |
---|
1529 | |
---|
1530 | REAL(wp) :: alpha !< |
---|
1531 | REAL(wp) :: dr !< |
---|
1532 | REAL(wp) :: e_s !< |
---|
1533 | REAL(wp) :: evap !< |
---|
1534 | REAL(wp) :: evap_nr !< |
---|
1535 | REAL(wp) :: f_vent !< |
---|
1536 | REAL(wp) :: g_evap !< |
---|
1537 | REAL(wp) :: lambda_r !< |
---|
1538 | REAL(wp) :: mu_r !< |
---|
1539 | REAL(wp) :: mu_r_2 !< |
---|
1540 | REAL(wp) :: mu_r_5d2 !< |
---|
1541 | REAL(wp) :: nr_0 !< |
---|
1542 | REAL(wp) :: q_s !< |
---|
1543 | REAL(wp) :: sat !< |
---|
1544 | REAL(wp) :: t_l !< |
---|
1545 | REAL(wp) :: temp !< |
---|
1546 | REAL(wp) :: xr !< |
---|
1547 | |
---|
1548 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
1549 | IF ( qr_1d(k) > eps_sb ) THEN |
---|
1550 | ! |
---|
1551 | !-- Actual liquid water temperature: |
---|
1552 | t_l = t_d_pt(k) * pt_1d(k) |
---|
1553 | ! |
---|
1554 | !-- Saturation vapor pressure at t_l: |
---|
1555 | e_s = 610.78_wp * EXP( 17.269_wp * ( t_l - 273.16_wp ) / & |
---|
1556 | ( t_l - 35.86_wp ) & |
---|
1557 | ) |
---|
1558 | ! |
---|
1559 | !-- Computation of saturation humidity: |
---|
1560 | q_s = 0.622_wp * e_s / ( hyp(k) - 0.378_wp * e_s ) |
---|
1561 | alpha = 0.622_wp * l_d_r * l_d_cp / ( t_l * t_l ) |
---|
1562 | q_s = q_s * ( 1.0_wp + alpha * q_1d(k) ) / ( 1.0_wp + alpha * q_s ) |
---|
1563 | ! |
---|
1564 | !-- Supersaturation: |
---|
1565 | sat = ( q_1d(k) - qr_1d(k) - qc_1d(k) ) / q_s - 1.0_wp |
---|
1566 | ! |
---|
1567 | !-- Evaporation needs only to be calculated in subsaturated regions |
---|
1568 | IF ( sat < 0.0_wp ) THEN |
---|
1569 | ! |
---|
1570 | !-- Actual temperature: |
---|
1571 | temp = t_l + l_d_cp * ( qc_1d(k) + qr_1d(k) ) |
---|
1572 | |
---|
1573 | g_evap = 1.0_wp / ( ( l_v / ( r_v * temp ) - 1.0_wp ) * l_v / & |
---|
1574 | ( thermal_conductivity_l * temp ) + & |
---|
1575 | r_v * temp / ( diff_coeff_l * e_s ) & |
---|
1576 | ) |
---|
1577 | ! |
---|
1578 | !-- Mean weight of rain drops |
---|
1579 | xr = hyrho(k) * qr_1d(k) / nr_1d(k) |
---|
1580 | ! |
---|
1581 | !-- Weight averaged diameter of rain drops: |
---|
1582 | dr = ( xr * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
1583 | ! |
---|
1584 | !-- Compute ventilation factor and intercept parameter |
---|
1585 | !-- (Seifert and Beheng, 2006; Seifert, 2008): |
---|
1586 | IF ( ventilation_effect ) THEN |
---|
1587 | ! |
---|
1588 | !-- Shape parameter of gamma distribution (Milbrandt and Yau, 2005; |
---|
1589 | !-- Stevens and Seifert, 2008): |
---|
1590 | mu_r = 10.0_wp * ( 1.0_wp + TANH( 1.2E3_wp * ( dr - 1.4E-3_wp ) ) ) |
---|
1591 | ! |
---|
1592 | !-- Slope parameter of gamma distribution (Seifert, 2008): |
---|
1593 | lambda_r = ( ( mu_r + 3.0_wp ) * ( mu_r + 2.0_wp ) * & |
---|
1594 | ( mu_r + 1.0_wp ) & |
---|
1595 | )**( 1.0_wp / 3.0_wp ) / dr |
---|
1596 | |
---|
1597 | mu_r_2 = mu_r + 2.0_wp |
---|
1598 | mu_r_5d2 = mu_r + 2.5_wp |
---|
1599 | |
---|
1600 | f_vent = a_vent * gamm( mu_r_2 ) * lambda_r**( -mu_r_2 ) + & |
---|
1601 | b_vent * schmidt_p_1d3 * & |
---|
1602 | SQRT( a_term / kin_vis_air ) * gamm( mu_r_5d2 ) * & |
---|
1603 | lambda_r**( -mu_r_5d2 ) * & |
---|
1604 | ( 1.0_wp - & |
---|
1605 | 0.5_wp * ( b_term / a_term ) * & |
---|
1606 | ( lambda_r / ( c_term + lambda_r ) & |
---|
1607 | )**mu_r_5d2 - & |
---|
1608 | 0.125_wp * ( b_term / a_term )**2 * & |
---|
1609 | ( lambda_r / ( 2.0_wp * c_term + lambda_r ) & |
---|
1610 | )**mu_r_5d2 - & |
---|
1611 | 0.0625_wp * ( b_term / a_term )**3 * & |
---|
1612 | ( lambda_r / ( 3.0_wp * c_term + lambda_r ) & |
---|
1613 | )**mu_r_5d2 - & |
---|
1614 | 0.0390625_wp * ( b_term / a_term )**4 * & |
---|
1615 | ( lambda_r / ( 4.0_wp * c_term + lambda_r ) & |
---|
1616 | )**mu_r_5d2 & |
---|
1617 | ) |
---|
1618 | |
---|
1619 | nr_0 = nr_1d(k) * lambda_r**( mu_r + 1.0_wp ) / & |
---|
1620 | gamm( mu_r + 1.0_wp ) |
---|
1621 | ELSE |
---|
1622 | f_vent = 1.0_wp |
---|
1623 | nr_0 = nr_1d(k) * dr |
---|
1624 | ENDIF |
---|
1625 | ! |
---|
1626 | !-- Evaporation rate of rain water content (Seifert and Beheng, 2006): |
---|
1627 | evap = 2.0_wp * pi * nr_0 * g_evap * f_vent * sat / hyrho(k) |
---|
1628 | evap = MAX( evap, -qr_1d(k) / dt_micro ) |
---|
1629 | evap_nr = MAX( c_evap * evap / xr * hyrho(k), & |
---|
1630 | -nr_1d(k) / dt_micro ) |
---|
1631 | |
---|
1632 | qr_1d(k) = qr_1d(k) + evap * dt_micro |
---|
1633 | nr_1d(k) = nr_1d(k) + evap_nr * dt_micro |
---|
1634 | |
---|
1635 | ENDIF |
---|
1636 | ENDIF |
---|
1637 | |
---|
1638 | ENDDO |
---|
1639 | |
---|
1640 | END SUBROUTINE evaporation_rain_ij |
---|
1641 | |
---|
1642 | |
---|
1643 | !------------------------------------------------------------------------------! |
---|
1644 | ! Description: |
---|
1645 | ! ------------ |
---|
1646 | !> Sedimentation of cloud droplets (Ackermann et al., 2009, MWR). |
---|
1647 | !> Call for grid point i,j |
---|
1648 | !------------------------------------------------------------------------------! |
---|
1649 | SUBROUTINE sedimentation_cloud_ij( i, j ) |
---|
1650 | |
---|
1651 | USE arrays_3d, & |
---|
1652 | ONLY: ddzu, dzu, nc_1d, pt_1d, q_1d, qc_1d |
---|
1653 | |
---|
1654 | USE cloud_parameters, & |
---|
1655 | ONLY: eps_sb, hyrho, l_d_cp, prr, pt_d_t, sed_qc_const |
---|
1656 | |
---|
1657 | USE constants, & |
---|
1658 | ONLY: pi |
---|
1659 | |
---|
1660 | USE control_parameters, & |
---|
1661 | ONLY: call_microphysics_at_all_substeps, dt_do2d_xy, dt_micro, & |
---|
1662 | intermediate_timestep_count, precipitation |
---|
1663 | |
---|
1664 | USE indices, & |
---|
1665 | ONLY: nzb, nzb_s_inner, nzt |
---|
1666 | |
---|
1667 | USE kinds |
---|
1668 | |
---|
1669 | USE statistics, & |
---|
1670 | ONLY: weight_substep |
---|
1671 | |
---|
1672 | IMPLICIT NONE |
---|
1673 | |
---|
1674 | INTEGER(iwp) :: i !< |
---|
1675 | INTEGER(iwp) :: j !< |
---|
1676 | INTEGER(iwp) :: k !< |
---|
1677 | |
---|
1678 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_qc !< |
---|
1679 | |
---|
1680 | sed_qc(nzt+1) = 0.0_wp |
---|
1681 | |
---|
1682 | DO k = nzt, nzb_s_inner(j,i)+1, -1 |
---|
1683 | IF ( qc_1d(k) > eps_sb ) THEN |
---|
1684 | sed_qc(k) = sed_qc_const * nc_1d(k)**( -2.0_wp / 3.0_wp ) * & |
---|
1685 | ( qc_1d(k) * hyrho(k) )**( 5.0_wp / 3.0_wp ) |
---|
1686 | ELSE |
---|
1687 | sed_qc(k) = 0.0_wp |
---|
1688 | ENDIF |
---|
1689 | |
---|
1690 | sed_qc(k) = MIN( sed_qc(k), hyrho(k) * dzu(k+1) * q_1d(k) / & |
---|
1691 | dt_micro + sed_qc(k+1) & |
---|
1692 | ) |
---|
1693 | |
---|
1694 | q_1d(k) = q_1d(k) + ( sed_qc(k+1) - sed_qc(k) ) * ddzu(k+1) / & |
---|
1695 | hyrho(k) * dt_micro |
---|
1696 | qc_1d(k) = qc_1d(k) + ( sed_qc(k+1) - sed_qc(k) ) * ddzu(k+1) / & |
---|
1697 | hyrho(k) * dt_micro |
---|
1698 | pt_1d(k) = pt_1d(k) - ( sed_qc(k+1) - sed_qc(k) ) * ddzu(k+1) / & |
---|
1699 | hyrho(k) * l_d_cp * pt_d_t(k) * dt_micro |
---|
1700 | |
---|
1701 | ! |
---|
1702 | !-- Compute the precipitation rate of cloud (fog) droplets |
---|
1703 | IF ( precipitation ) THEN |
---|
1704 | IF ( call_microphysics_at_all_substeps ) THEN |
---|
1705 | prr(k,j,i) = prr(k,j,i) + sed_qc(k) / hyrho(k) * & |
---|
1706 | weight_substep(intermediate_timestep_count) |
---|
1707 | ELSE |
---|
1708 | prr(k,j,i) = prr(k,j,i) + sed_qc(k) / hyrho(k) |
---|
1709 | ENDIF |
---|
1710 | ENDIF |
---|
1711 | |
---|
1712 | ENDDO |
---|
1713 | |
---|
1714 | END SUBROUTINE sedimentation_cloud_ij |
---|
1715 | |
---|
1716 | |
---|
1717 | !------------------------------------------------------------------------------! |
---|
1718 | ! Description: |
---|
1719 | ! ------------ |
---|
1720 | !> Computation of sedimentation flux. Implementation according to Stevens |
---|
1721 | !> and Seifert (2008). Code is based on UCLA-LES. Call for grid point i,j |
---|
1722 | !------------------------------------------------------------------------------! |
---|
1723 | SUBROUTINE sedimentation_rain_ij( i, j ) |
---|
1724 | |
---|
1725 | USE arrays_3d, & |
---|
1726 | ONLY: ddzu, dzu, nr_1d, pt_1d, q_1d, qr_1d |
---|
1727 | |
---|
1728 | USE cloud_parameters, & |
---|
1729 | ONLY: a_term, b_term, c_term, cof, dpirho_l, eps_sb, hyrho, & |
---|
1730 | limiter_sedimentation, l_d_cp, precipitation_amount, prr, & |
---|
1731 | pt_d_t, stp |
---|
1732 | |
---|
1733 | USE control_parameters, & |
---|
1734 | ONLY: call_microphysics_at_all_substeps, dt_do2d_xy, dt_micro, & |
---|
1735 | dt_3d, intermediate_timestep_count, & |
---|
1736 | intermediate_timestep_count_max, & |
---|
1737 | precipitation_amount_interval, time_do2d_xy |
---|
1738 | |
---|
1739 | USE indices, & |
---|
1740 | ONLY: nzb, nzb_s_inner, nzt |
---|
1741 | |
---|
1742 | USE kinds |
---|
1743 | |
---|
1744 | USE statistics, & |
---|
1745 | ONLY: weight_substep |
---|
1746 | |
---|
1747 | IMPLICIT NONE |
---|
1748 | |
---|
1749 | INTEGER(iwp) :: i !< |
---|
1750 | INTEGER(iwp) :: j !< |
---|
1751 | INTEGER(iwp) :: k !< |
---|
1752 | INTEGER(iwp) :: k_run !< |
---|
1753 | |
---|
1754 | REAL(wp) :: c_run !< |
---|
1755 | REAL(wp) :: d_max !< |
---|
1756 | REAL(wp) :: d_mean !< |
---|
1757 | REAL(wp) :: d_min !< |
---|
1758 | REAL(wp) :: dr !< |
---|
1759 | REAL(wp) :: dt_sedi !< |
---|
1760 | REAL(wp) :: flux !< |
---|
1761 | REAL(wp) :: lambda_r !< |
---|
1762 | REAL(wp) :: mu_r !< |
---|
1763 | REAL(wp) :: z_run !< |
---|
1764 | |
---|
1765 | REAL(wp), DIMENSION(nzb:nzt+1) :: c_nr !< |
---|
1766 | REAL(wp), DIMENSION(nzb:nzt+1) :: c_qr !< |
---|
1767 | REAL(wp), DIMENSION(nzb:nzt+1) :: d_nr !< |
---|
1768 | REAL(wp), DIMENSION(nzb:nzt+1) :: d_qr !< |
---|
1769 | REAL(wp), DIMENSION(nzb:nzt+1) :: nr_slope !< |
---|
1770 | REAL(wp), DIMENSION(nzb:nzt+1) :: qr_slope !< |
---|
1771 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_nr !< |
---|
1772 | REAL(wp), DIMENSION(nzb:nzt+1) :: sed_qr !< |
---|
1773 | REAL(wp), DIMENSION(nzb:nzt+1) :: w_nr !< |
---|
1774 | REAL(wp), DIMENSION(nzb:nzt+1) :: w_qr !< |
---|
1775 | |
---|
1776 | IF ( intermediate_timestep_count == 1 ) prr(:,j,i) = 0.0_wp |
---|
1777 | ! |
---|
1778 | !-- Compute velocities |
---|
1779 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
1780 | IF ( qr_1d(k) > eps_sb ) THEN |
---|
1781 | ! |
---|
1782 | !-- Weight averaged diameter of rain drops: |
---|
1783 | dr = ( hyrho(k) * qr_1d(k) / nr_1d(k) * dpirho_l )**( 1.0_wp / 3.0_wp ) |
---|
1784 | ! |
---|
1785 | !-- Shape parameter of gamma distribution (Milbrandt and Yau, 2005; |
---|
1786 | !-- Stevens and Seifert, 2008): |
---|
1787 | mu_r = 10.0_wp * ( 1.0_wp + TANH( 1.2E3_wp * ( dr - 1.4E-3_wp ) ) ) |
---|
1788 | ! |
---|
1789 | !-- Slope parameter of gamma distribution (Seifert, 2008): |
---|
1790 | lambda_r = ( ( mu_r + 3.0_wp ) * ( mu_r + 2.0_wp ) * & |
---|
1791 | ( mu_r + 1.0_wp ) )**( 1.0_wp / 3.0_wp ) / dr |
---|
1792 | |
---|
1793 | w_nr(k) = MAX( 0.1_wp, MIN( 20.0_wp, & |
---|
1794 | a_term - b_term * ( 1.0_wp + & |
---|
1795 | c_term / lambda_r )**( -1.0_wp * & |
---|
1796 | ( mu_r + 1.0_wp ) ) & |
---|
1797 | ) & |
---|
1798 | ) |
---|
1799 | w_qr(k) = MAX( 0.1_wp, MIN( 20.0_wp, & |
---|
1800 | a_term - b_term * ( 1.0_wp + & |
---|
1801 | c_term / lambda_r )**( -1.0_wp * & |
---|
1802 | ( mu_r + 4.0_wp ) ) & |
---|
1803 | ) & |
---|
1804 | ) |
---|
1805 | ELSE |
---|
1806 | w_nr(k) = 0.0_wp |
---|
1807 | w_qr(k) = 0.0_wp |
---|
1808 | ENDIF |
---|
1809 | ENDDO |
---|
1810 | ! |
---|
1811 | !-- Adjust boundary values |
---|
1812 | w_nr(nzb_s_inner(j,i)) = w_nr(nzb_s_inner(j,i)+1) |
---|
1813 | w_qr(nzb_s_inner(j,i)) = w_qr(nzb_s_inner(j,i)+1) |
---|
1814 | w_nr(nzt+1) = 0.0_wp |
---|
1815 | w_qr(nzt+1) = 0.0_wp |
---|
1816 | ! |
---|
1817 | !-- Compute Courant number |
---|
1818 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
1819 | c_nr(k) = 0.25_wp * ( w_nr(k-1) + 2.0_wp * w_nr(k) + w_nr(k+1) ) * & |
---|
1820 | dt_micro * ddzu(k) |
---|
1821 | c_qr(k) = 0.25_wp * ( w_qr(k-1) + 2.0_wp * w_qr(k) + w_qr(k+1) ) * & |
---|
1822 | dt_micro * ddzu(k) |
---|
1823 | ENDDO |
---|
1824 | ! |
---|
1825 | !-- Limit slopes with monotonized centered (MC) limiter (van Leer, 1977): |
---|
1826 | IF ( limiter_sedimentation ) THEN |
---|
1827 | |
---|
1828 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
1829 | d_mean = 0.5_wp * ( qr_1d(k+1) - qr_1d(k-1) ) |
---|
1830 | d_min = qr_1d(k) - MIN( qr_1d(k+1), qr_1d(k), qr_1d(k-1) ) |
---|
1831 | d_max = MAX( qr_1d(k+1), qr_1d(k), qr_1d(k-1) ) - qr_1d(k) |
---|
1832 | |
---|
1833 | qr_slope(k) = SIGN(1.0_wp, d_mean) * MIN ( 2.0_wp * d_min, & |
---|
1834 | 2.0_wp * d_max, & |
---|
1835 | ABS( d_mean ) ) |
---|
1836 | |
---|
1837 | d_mean = 0.5_wp * ( nr_1d(k+1) - nr_1d(k-1) ) |
---|
1838 | d_min = nr_1d(k) - MIN( nr_1d(k+1), nr_1d(k), nr_1d(k-1) ) |
---|
1839 | d_max = MAX( nr_1d(k+1), nr_1d(k), nr_1d(k-1) ) - nr_1d(k) |
---|
1840 | |
---|
1841 | nr_slope(k) = SIGN(1.0_wp, d_mean) * MIN ( 2.0_wp * d_min, & |
---|
1842 | 2.0_wp * d_max, & |
---|
1843 | ABS( d_mean ) ) |
---|
1844 | ENDDO |
---|
1845 | |
---|
1846 | ELSE |
---|
1847 | |
---|
1848 | nr_slope = 0.0_wp |
---|
1849 | qr_slope = 0.0_wp |
---|
1850 | |
---|
1851 | ENDIF |
---|
1852 | |
---|
1853 | sed_nr(nzt+1) = 0.0_wp |
---|
1854 | sed_qr(nzt+1) = 0.0_wp |
---|
1855 | ! |
---|
1856 | !-- Compute sedimentation flux |
---|
1857 | DO k = nzt, nzb_s_inner(j,i)+1, -1 |
---|
1858 | ! |
---|
1859 | !-- Sum up all rain drop number densities which contribute to the flux |
---|
1860 | !-- through k-1/2 |
---|
1861 | flux = 0.0_wp |
---|
1862 | z_run = 0.0_wp ! height above z(k) |
---|
1863 | k_run = k |
---|
1864 | c_run = MIN( 1.0_wp, c_nr(k) ) |
---|
1865 | DO WHILE ( c_run > 0.0_wp .AND. k_run <= nzt ) |
---|
1866 | flux = flux + hyrho(k_run) * & |
---|
1867 | ( nr_1d(k_run) + nr_slope(k_run) * ( 1.0_wp - c_run ) * & |
---|
1868 | 0.5_wp ) * c_run * dzu(k_run) |
---|
1869 | z_run = z_run + dzu(k_run) |
---|
1870 | k_run = k_run + 1 |
---|
1871 | c_run = MIN( 1.0_wp, c_nr(k_run) - z_run * ddzu(k_run) ) |
---|
1872 | ENDDO |
---|
1873 | ! |
---|
1874 | !-- It is not allowed to sediment more rain drop number density than |
---|
1875 | !-- available |
---|
1876 | flux = MIN( flux, & |
---|
1877 | hyrho(k) * dzu(k+1) * nr_1d(k) + sed_nr(k+1) * dt_micro ) |
---|
1878 | |
---|
1879 | sed_nr(k) = flux / dt_micro |
---|
1880 | nr_1d(k) = nr_1d(k) + ( sed_nr(k+1) - sed_nr(k) ) * ddzu(k+1) / & |
---|
1881 | hyrho(k) * dt_micro |
---|
1882 | ! |
---|
1883 | !-- Sum up all rain water content which contributes to the flux |
---|
1884 | !-- through k-1/2 |
---|
1885 | flux = 0.0_wp |
---|
1886 | z_run = 0.0_wp ! height above z(k) |
---|
1887 | k_run = k |
---|
1888 | c_run = MIN( 1.0_wp, c_qr(k) ) |
---|
1889 | |
---|
1890 | DO WHILE ( c_run > 0.0_wp .AND. k_run <= nzt ) |
---|
1891 | |
---|
1892 | flux = flux + hyrho(k_run) * & |
---|
1893 | ( qr_1d(k_run) + qr_slope(k_run) * ( 1.0_wp - c_run ) * & |
---|
1894 | 0.5_wp ) * c_run * dzu(k_run) |
---|
1895 | z_run = z_run + dzu(k_run) |
---|
1896 | k_run = k_run + 1 |
---|
1897 | c_run = MIN( 1.0_wp, c_qr(k_run) - z_run * ddzu(k_run) ) |
---|
1898 | |
---|
1899 | ENDDO |
---|
1900 | ! |
---|
1901 | !-- It is not allowed to sediment more rain water content than available |
---|
1902 | flux = MIN( flux, & |
---|
1903 | hyrho(k) * dzu(k) * qr_1d(k) + sed_qr(k+1) * dt_micro ) |
---|
1904 | |
---|
1905 | sed_qr(k) = flux / dt_micro |
---|
1906 | |
---|
1907 | qr_1d(k) = qr_1d(k) + ( sed_qr(k+1) - sed_qr(k) ) * ddzu(k+1) / & |
---|
1908 | hyrho(k) * dt_micro |
---|
1909 | q_1d(k) = q_1d(k) + ( sed_qr(k+1) - sed_qr(k) ) * ddzu(k+1) / & |
---|
1910 | hyrho(k) * dt_micro |
---|
1911 | pt_1d(k) = pt_1d(k) - ( sed_qr(k+1) - sed_qr(k) ) * ddzu(k+1) / & |
---|
1912 | hyrho(k) * l_d_cp * pt_d_t(k) * dt_micro |
---|
1913 | ! |
---|
1914 | !-- Compute the rain rate |
---|
1915 | IF ( call_microphysics_at_all_substeps ) THEN |
---|
1916 | prr(k,j,i) = prr(k,j,i) + sed_qr(k) / hyrho(k) & |
---|
1917 | * weight_substep(intermediate_timestep_count) |
---|
1918 | ELSE |
---|
1919 | prr(k,j,i) = prr(k,j,i) + sed_qr(k) / hyrho(k) |
---|
1920 | ENDIF |
---|
1921 | |
---|
1922 | ENDDO |
---|
1923 | |
---|
1924 | END SUBROUTINE sedimentation_rain_ij |
---|
1925 | |
---|
1926 | |
---|
1927 | !------------------------------------------------------------------------------! |
---|
1928 | ! Description: |
---|
1929 | ! ------------ |
---|
1930 | !> This subroutine computes the precipitation amount due to gravitational |
---|
1931 | !> settling of rain and cloud (fog) droplets |
---|
1932 | !------------------------------------------------------------------------------! |
---|
1933 | SUBROUTINE calc_precipitation_amount_ij( i, j ) |
---|
1934 | |
---|
1935 | USE cloud_parameters, & |
---|
1936 | ONLY: hyrho, precipitation_amount, prr |
---|
1937 | |
---|
1938 | USE control_parameters, & |
---|
1939 | ONLY: call_microphysics_at_all_substeps, dt_do2d_xy, dt_3d, & |
---|
1940 | intermediate_timestep_count, intermediate_timestep_count_max,& |
---|
1941 | precipitation_amount_interval, & |
---|
1942 | time_do2d_xy |
---|
1943 | |
---|
1944 | USE indices, & |
---|
1945 | ONLY: nzb_s_inner |
---|
1946 | |
---|
1947 | USE kinds |
---|
1948 | |
---|
1949 | IMPLICIT NONE |
---|
1950 | |
---|
1951 | INTEGER(iwp) :: i !: |
---|
1952 | INTEGER(iwp) :: j !: |
---|
1953 | |
---|
1954 | |
---|
1955 | IF ( ( dt_do2d_xy - time_do2d_xy ) < precipitation_amount_interval .AND.& |
---|
1956 | ( .NOT. call_microphysics_at_all_substeps .OR. & |
---|
1957 | intermediate_timestep_count == intermediate_timestep_count_max ) ) & |
---|
1958 | THEN |
---|
1959 | |
---|
1960 | precipitation_amount(j,i) = precipitation_amount(j,i) + & |
---|
1961 | prr(nzb_s_inner(j,i)+1,j,i) * & |
---|
1962 | hyrho(nzb_s_inner(j,i)+1) * dt_3d |
---|
1963 | ENDIF |
---|
1964 | |
---|
1965 | END SUBROUTINE calc_precipitation_amount_ij |
---|
1966 | |
---|
1967 | !------------------------------------------------------------------------------! |
---|
1968 | ! Description: |
---|
1969 | ! ------------ |
---|
1970 | !> This function computes the gamma function (Press et al., 1992). |
---|
1971 | !> The gamma function is needed for the calculation of the evaporation |
---|
1972 | !> of rain drops. |
---|
1973 | !------------------------------------------------------------------------------! |
---|
1974 | FUNCTION gamm( xx ) |
---|
1975 | |
---|
1976 | USE cloud_parameters, & |
---|
1977 | ONLY: cof, stp |
---|
1978 | |
---|
1979 | USE kinds |
---|
1980 | |
---|
1981 | IMPLICIT NONE |
---|
1982 | |
---|
1983 | INTEGER(iwp) :: j !< |
---|
1984 | |
---|
1985 | REAL(wp) :: gamm !< |
---|
1986 | REAL(wp) :: ser !< |
---|
1987 | REAL(wp) :: tmp !< |
---|
1988 | REAL(wp) :: x_gamm !< |
---|
1989 | REAL(wp) :: xx !< |
---|
1990 | REAL(wp) :: y_gamm !< |
---|
1991 | |
---|
1992 | x_gamm = xx |
---|
1993 | y_gamm = x_gamm |
---|
1994 | tmp = x_gamm + 5.5_wp |
---|
1995 | tmp = ( x_gamm + 0.5_wp ) * LOG( tmp ) - tmp |
---|
1996 | ser = 1.000000000190015_wp |
---|
1997 | |
---|
1998 | DO j = 1, 6 |
---|
1999 | y_gamm = y_gamm + 1.0_wp |
---|
2000 | ser = ser + cof( j ) / y_gamm |
---|
2001 | ENDDO |
---|
2002 | |
---|
2003 | ! |
---|
2004 | !-- Until this point the algorithm computes the logarithm of the gamma |
---|
2005 | !-- function. Hence, the exponential function is used. |
---|
2006 | ! gamm = EXP( tmp + LOG( stp * ser / x_gamm ) ) |
---|
2007 | gamm = EXP( tmp ) * stp * ser / x_gamm |
---|
2008 | |
---|
2009 | RETURN |
---|
2010 | |
---|
2011 | END FUNCTION gamm |
---|
2012 | |
---|
2013 | END MODULE microphysics_mod |
---|