1 | SUBROUTINE lpm_droplet_condensation |
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2 | |
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3 | !--------------------------------------------------------------------------------! |
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4 | ! This file is part of PALM. |
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5 | ! |
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6 | ! PALM is free software: you can redistribute it and/or modify it under the terms |
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7 | ! of the GNU General Public License as published by the Free Software Foundation, |
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8 | ! either version 3 of the License, or (at your option) any later version. |
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9 | ! |
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10 | ! PALM is distributed in the hope that it will be useful, but WITHOUT ANY |
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11 | ! WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR |
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12 | ! A PARTICULAR PURPOSE. See the GNU General Public License for more details. |
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13 | ! |
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14 | ! You should have received a copy of the GNU General Public License along with |
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15 | ! PALM. If not, see <http://www.gnu.org/licenses/>. |
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16 | ! |
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17 | ! Copyright 1997-2014 Leibniz Universitaet Hannover |
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18 | !--------------------------------------------------------------------------------! |
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19 | ! |
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20 | ! Current revisions: |
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21 | ! ------------------ |
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22 | ! |
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23 | ! |
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24 | ! Former revisions: |
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25 | ! ----------------- |
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26 | ! $Id: lpm_droplet_condensation.f90 1347 2014-03-27 13:23:00Z witha $ |
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27 | ! |
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28 | ! 1346 2014-03-27 13:18:20Z heinze |
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29 | ! Bugfix: REAL constants provided with KIND-attribute especially in call of |
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30 | ! intrinsic function like MAX, MIN, SIGN |
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31 | ! |
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32 | ! 1322 2014-03-20 16:38:49Z raasch |
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33 | ! REAL constants defined as wp-kind |
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34 | ! |
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35 | ! 1320 2014-03-20 08:40:49Z raasch |
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36 | ! ONLY-attribute added to USE-statements, |
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37 | ! kind-parameters added to all INTEGER and REAL declaration statements, |
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38 | ! kinds are defined in new module kinds, |
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39 | ! comment fields (!:) to be used for variable explanations added to |
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40 | ! all variable declaration statements |
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41 | ! |
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42 | ! 1318 2014-03-17 13:35:16Z raasch |
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43 | ! module interfaces removed |
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44 | ! |
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45 | ! 1092 2013-02-02 11:24:22Z raasch |
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46 | ! unused variables removed |
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47 | ! |
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48 | ! 1071 2012-11-29 16:54:55Z franke |
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49 | ! Ventilation effect for evaporation of large droplets included |
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50 | ! Check for unreasonable results included in calculation of Rosenbrock method |
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51 | ! since physically unlikely results were observed and for the same |
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52 | ! reason the first internal time step in Rosenbrock method should be < 1.0E02 in |
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53 | ! case of evaporation |
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54 | ! Unnecessary calculation of ql_int removed |
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55 | ! Unnecessary calculations in Rosenbrock method (d2rdt2, drdt_m, dt_ros_last) |
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56 | ! removed |
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57 | ! Bugfix: factor in calculation of surface tension changed from 0.00155 to |
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58 | ! 0.000155 |
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59 | ! |
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60 | ! 1036 2012-10-22 13:43:42Z raasch |
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61 | ! code put under GPL (PALM 3.9) |
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62 | ! |
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63 | ! 849 2012-03-15 10:35:09Z raasch |
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64 | ! initial revision (former part of advec_particles) |
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65 | ! |
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66 | ! |
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67 | ! Description: |
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68 | ! ------------ |
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69 | ! Calculates change in droplet radius by condensation/evaporation, using |
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70 | ! either an analytic formula or by numerically integrating the radius growth |
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71 | ! equation including curvature and solution effects using Rosenbrocks method |
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72 | ! (see Numerical recipes in FORTRAN, 2nd edition, p. 731). |
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73 | ! The analytical formula and growth equation follow those given in |
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74 | ! Rogers and Yau (A short course in cloud physics, 3rd edition, p. 102/103). |
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75 | !------------------------------------------------------------------------------! |
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76 | |
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77 | USE arrays_3d, & |
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78 | ONLY: hyp, pt, q, ql_c, ql_v, zu |
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79 | |
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80 | USE cloud_parameters, & |
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81 | ONLY: bfactor, curvature_solution_effects, diff_coeff_l, & |
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82 | eps_ros, l_d_rv, l_v, rho_l, r_v, thermal_conductivity_l |
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83 | |
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84 | USE constants, & |
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85 | ONLY: pi |
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86 | |
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87 | USE control_parameters, & |
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88 | ONLY: atmos_ocean_sign, dt_3d, dz, message_string, & |
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89 | molecular_viscosity, rho_surface |
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90 | USE cpulog, & |
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91 | ONLY: cpu_log, log_point_s |
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92 | |
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93 | USE grid_variables, & |
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94 | ONLY: dx, ddx, dy, ddy |
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95 | |
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96 | USE lpm_collision_kernels_mod, & |
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97 | ONLY: rclass_lbound, rclass_ubound |
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98 | |
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99 | USE kinds |
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100 | |
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101 | USE particle_attributes, & |
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102 | ONLY: hall_kernel, number_of_particles, offset_ocean_nzt, & |
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103 | offset_ocean_nzt_m1, particles, radius_classes, & |
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104 | use_kernel_tables, wang_kernel |
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105 | |
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106 | |
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107 | IMPLICIT NONE |
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108 | |
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109 | INTEGER(iwp) :: i !: |
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110 | INTEGER(iwp) :: internal_timestep_count !: |
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111 | INTEGER(iwp) :: j !: |
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112 | INTEGER(iwp) :: jtry !: |
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113 | INTEGER(iwp) :: k !: |
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114 | INTEGER(iwp) :: n !: |
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115 | INTEGER(iwp) :: ros_count !: |
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116 | |
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117 | INTEGER(iwp), PARAMETER :: maxtry = 40 !: |
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118 | |
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119 | LOGICAL :: repeat !: |
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120 | |
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121 | REAL(wp) :: aa !: |
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122 | REAL(wp) :: afactor !: |
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123 | REAL(wp) :: arg !: |
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124 | REAL(wp) :: bb !: |
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125 | REAL(wp) :: cc !: |
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126 | REAL(wp) :: dd !: |
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127 | REAL(wp) :: ddenom !: |
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128 | REAL(wp) :: delta_r !: |
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129 | REAL(wp) :: drdt !: |
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130 | REAL(wp) :: drdt_ini !: |
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131 | REAL(wp) :: dt_ros !: |
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132 | REAL(wp) :: dt_ros_next !: |
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133 | REAL(wp) :: dt_ros_sum !: |
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134 | REAL(wp) :: dt_ros_sum_ini !: |
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135 | REAL(wp) :: d2rdtdr !: |
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136 | REAL(wp) :: errmax !: |
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137 | REAL(wp) :: err_ros !: |
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138 | REAL(wp) :: g1 !: |
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139 | REAL(wp) :: g2 !: |
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140 | REAL(wp) :: g3 !: |
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141 | REAL(wp) :: g4 !: |
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142 | REAL(wp) :: e_a !: |
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143 | REAL(wp) :: e_s !: |
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144 | REAL(wp) :: gg !: |
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145 | REAL(wp) :: new_r !: |
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146 | REAL(wp) :: p_int !: |
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147 | REAL(wp) :: pt_int !: |
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148 | REAL(wp) :: pt_int_l !: |
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149 | REAL(wp) :: pt_int_u !: |
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150 | REAL(wp) :: q_int !: |
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151 | REAL(wp) :: q_int_l !: |
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152 | REAL(wp) :: q_int_u !: |
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153 | REAL(wp) :: r_ros !: |
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154 | REAL(wp) :: r_ros_ini !: |
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155 | REAL(wp) :: sigma !: |
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156 | REAL(wp) :: t_int !: |
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157 | REAL(wp) :: x !: |
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158 | REAL(wp) :: y !: |
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159 | REAL(wp) :: re_p !: |
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160 | |
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161 | !-- Parameters for Rosenbrock method |
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162 | REAL(wp), PARAMETER :: a21 = 2.0 !: |
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163 | REAL(wp), PARAMETER :: a31 = 48.0/25.0_wp !: |
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164 | REAL(wp), PARAMETER :: a32 = 6.0/25.0_wp !: |
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165 | REAL(wp), PARAMETER :: b1 = 19.0/9.0_wp !: |
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166 | REAL(wp), PARAMETER :: b2 = 0.5 !: |
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167 | REAL(wp), PARAMETER :: b3 = 25.0/108.0_wp !: |
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168 | REAL(wp), PARAMETER :: b4 = 125.0/108.0_wp !: |
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169 | REAL(wp), PARAMETER :: c21 = -8.0 !: |
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170 | REAL(wp), PARAMETER :: c31 = 372.0/25.0_wp !: |
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171 | REAL(wp), PARAMETER :: c32 = 12.0/5.0_wp !: |
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172 | REAL(wp), PARAMETER :: c41 = -112.0/125.0_wp !: |
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173 | REAL(wp), PARAMETER :: c42 = -54.0/125.0_wp !: |
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174 | REAL(wp), PARAMETER :: c43 = -2.0/5.0_wp !: |
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175 | REAL(wp), PARAMETER :: errcon = 0.1296 !: |
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176 | REAL(wp), PARAMETER :: e1 = 17.0/54.0_wp !: |
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177 | REAL(wp), PARAMETER :: e2 = 7.0/36.0_wp !: |
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178 | REAL(wp), PARAMETER :: e3 = 0.0 !: |
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179 | REAL(wp), PARAMETER :: e4 = 125.0/108.0_wp !: |
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180 | REAL(wp), PARAMETER :: gam = 0.5 !: |
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181 | REAL(wp), PARAMETER :: grow = 1.5 !: |
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182 | REAL(wp), PARAMETER :: pgrow = -0.25 !: |
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183 | REAL(wp), PARAMETER :: pshrnk = -1.0/3.0_wp !: |
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184 | REAL(wp), PARAMETER :: shrnk = 0.5 !: |
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185 | |
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186 | |
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187 | |
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188 | CALL cpu_log( log_point_s(42), 'lpm_droplet_condens', 'start' ) |
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189 | |
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190 | DO n = 1, number_of_particles |
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191 | ! |
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192 | !-- Interpolate temperature and humidity. |
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193 | !-- First determine left, south, and bottom index of the arrays. |
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194 | i = particles(n)%x * ddx |
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195 | j = particles(n)%y * ddy |
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196 | k = ( particles(n)%z + 0.5 * dz * atmos_ocean_sign ) / dz & |
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197 | + offset_ocean_nzt ! only exact if equidistant |
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198 | |
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199 | x = particles(n)%x - i * dx |
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200 | y = particles(n)%y - j * dy |
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201 | aa = x**2 + y**2 |
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202 | bb = ( dx - x )**2 + y**2 |
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203 | cc = x**2 + ( dy - y )**2 |
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204 | dd = ( dx - x )**2 + ( dy - y )**2 |
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205 | gg = aa + bb + cc + dd |
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206 | |
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207 | pt_int_l = ( ( gg - aa ) * pt(k,j,i) + ( gg - bb ) * pt(k,j,i+1) & |
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208 | + ( gg - cc ) * pt(k,j+1,i) + ( gg - dd ) * pt(k,j+1,i+1) & |
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209 | ) / ( 3.0 * gg ) |
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210 | |
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211 | pt_int_u = ( ( gg-aa ) * pt(k+1,j,i) + ( gg-bb ) * pt(k+1,j,i+1) & |
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212 | + ( gg-cc ) * pt(k+1,j+1,i) + ( gg-dd ) * pt(k+1,j+1,i+1) & |
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213 | ) / ( 3.0 * gg ) |
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214 | |
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215 | pt_int = pt_int_l + ( particles(n)%z - zu(k) ) / dz * & |
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216 | ( pt_int_u - pt_int_l ) |
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217 | |
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218 | q_int_l = ( ( gg - aa ) * q(k,j,i) + ( gg - bb ) * q(k,j,i+1) & |
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219 | + ( gg - cc ) * q(k,j+1,i) + ( gg - dd ) * q(k,j+1,i+1) & |
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220 | ) / ( 3.0 * gg ) |
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221 | |
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222 | q_int_u = ( ( gg-aa ) * q(k+1,j,i) + ( gg-bb ) * q(k+1,j,i+1) & |
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223 | + ( gg-cc ) * q(k+1,j+1,i) + ( gg-dd ) * q(k+1,j+1,i+1) & |
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224 | ) / ( 3.0 * gg ) |
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225 | |
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226 | q_int = q_int_l + ( particles(n)%z - zu(k) ) / dz * & |
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227 | ( q_int_u - q_int_l ) |
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228 | |
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229 | ! |
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230 | !-- Calculate real temperature and saturation vapor pressure |
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231 | p_int = hyp(k) + ( particles(n)%z - zu(k) ) / dz * ( hyp(k+1)-hyp(k) ) |
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232 | t_int = pt_int * ( p_int / 100000.0 )**0.286 |
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233 | |
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234 | e_s = 611.0 * EXP( l_d_rv * ( 3.6609E-3 - 1.0 / t_int ) ) |
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235 | |
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236 | ! |
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237 | !-- Current vapor pressure |
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238 | e_a = q_int * p_int / ( 0.378 * q_int + 0.622 ) |
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239 | |
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240 | ! |
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241 | !-- Thermal conductivity for water (from Rogers and Yau, Table 7.1), |
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242 | !-- diffusivity for water vapor (after Hall und Pruppacher, 1976) |
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243 | thermal_conductivity_l = 7.94048E-05 * t_int + 0.00227011 |
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244 | diff_coeff_l = 0.211E-4 * ( t_int / 273.15 )**1.94 * & |
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245 | ( 101325.0 / p_int) |
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246 | ! |
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247 | !-- Change in radius by condensation/evaporation |
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248 | IF ( particles(n)%radius >= 4.0E-5 .AND. e_a/e_s < 1.0 ) THEN |
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249 | ! |
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250 | !-- Approximation for large radii, where curvature and solution effects |
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251 | !-- can be neglected but ventilation effect has to be included in case of |
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252 | !-- evaporation. |
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253 | !-- First calculate the droplet's Reynolds number |
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254 | re_p = 2.0 * particles(n)%radius * ABS( particles(n)%speed_z ) / & |
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255 | molecular_viscosity |
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256 | ! |
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257 | !-- Ventilation coefficient after Rogers and Yau, 1989 |
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258 | IF ( re_p > 2.5 ) THEN |
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259 | afactor = 0.78 + 0.28 * SQRT( re_p ) |
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260 | ELSE |
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261 | afactor = 1.0 + 0.09 * re_p |
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262 | ENDIF |
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263 | |
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264 | arg = particles(n)%radius**2 + 2.0 * dt_3d * afactor * & |
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265 | ( e_a / e_s - 1.0 ) / & |
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266 | ( ( l_d_rv / t_int - 1.0 ) * l_v * rho_l / t_int / & |
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267 | thermal_conductivity_l + & |
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268 | rho_l * r_v * t_int / diff_coeff_l / e_s ) |
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269 | |
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270 | new_r = SQRT( arg ) |
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271 | |
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272 | ELSEIF ( particles(n)%radius >= 1.0E-6 .OR. & |
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273 | .NOT. curvature_solution_effects ) THEN |
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274 | ! |
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275 | !-- Approximation for larger radii in case that curvature and solution |
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276 | !-- effects are neglected and ventilation effects does not play a role |
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277 | arg = particles(n)%radius**2 + 2.0 * dt_3d * & |
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278 | ( e_a / e_s - 1.0 ) / & |
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279 | ( ( l_d_rv / t_int - 1.0 ) * l_v * rho_l / t_int / & |
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280 | thermal_conductivity_l + & |
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281 | rho_l * r_v * t_int / diff_coeff_l / e_s ) |
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282 | IF ( arg < 1.0E-16 ) THEN |
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283 | new_r = 1.0E-8 |
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284 | ELSE |
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285 | new_r = SQRT( arg ) |
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286 | ENDIF |
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287 | ENDIF |
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288 | |
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289 | IF ( curvature_solution_effects .AND. & |
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290 | ( ( particles(n)%radius < 1.0E-6 ) .OR. ( new_r < 1.0E-6 ) ) ) & |
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291 | THEN |
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292 | ! |
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293 | !-- Curvature and solutions effects are included in growth equation. |
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294 | !-- Change in Radius is calculated with 4th-order Rosenbrock method |
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295 | !-- for stiff o.d.e's with monitoring local truncation error to adjust |
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296 | !-- stepsize (see Numerical recipes in FORTRAN, 2nd edition, p. 731). |
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297 | !-- For larger radii the simple analytic method (see ELSE) gives |
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298 | !-- almost the same results. |
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299 | |
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300 | ros_count = 0 |
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301 | repeat = .TRUE. |
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302 | ! |
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303 | !-- Carry out the Rosenbrock algorithm. In case of unreasonable results |
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304 | !-- the switch "repeat" will be set true and the algorithm will be carried |
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305 | !-- out again with the internal time step set to its initial (small) value. |
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306 | !-- Unreasonable results may occur if the external conditions, especially the |
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307 | !-- supersaturation, has significantly changed compared to the last PALM |
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308 | !-- timestep. |
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309 | DO WHILE ( repeat ) |
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310 | |
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311 | repeat = .FALSE. |
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312 | ! |
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313 | !-- Surface tension after (Straka, 2009) |
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314 | sigma = 0.0761 - 0.000155 * ( t_int - 273.15 ) |
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315 | |
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316 | r_ros = particles(n)%radius |
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317 | dt_ros_sum = 0.0 ! internal integrated time (s) |
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318 | internal_timestep_count = 0 |
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319 | |
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320 | ddenom = 1.0 / ( rho_l * r_v * t_int / ( e_s * diff_coeff_l ) + & |
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321 | ( l_v / ( r_v * t_int ) - 1.0 ) * & |
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322 | rho_l * l_v / ( thermal_conductivity_l * t_int )& |
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323 | ) |
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324 | |
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325 | afactor = 2.0 * sigma / ( rho_l * r_v * t_int ) |
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326 | |
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327 | ! |
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328 | !-- Take internal time step values from the end of last PALM time step |
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329 | dt_ros_next = particles(n)%rvar1 |
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330 | |
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331 | ! |
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332 | !-- Internal time step should not be > 1.0E-2 in case of evaporation |
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333 | !-- because larger values may lead to secondary solutions which are |
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334 | !-- physically unlikely |
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335 | IF ( dt_ros_next > 1.0E-2 .AND. e_a/e_s < 1.0 ) THEN |
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336 | dt_ros_next = 1.0E-3 |
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337 | ENDIF |
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338 | ! |
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339 | !-- If calculation of Rosenbrock method is repeated due to unreasonalble |
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340 | !-- results during previous try the initial internal time step has to be |
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341 | !-- reduced |
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342 | IF ( ros_count > 1 ) THEN |
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343 | dt_ros_next = dt_ros_next - ( 0.2 * dt_ros_next ) |
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344 | ELSEIF ( ros_count > 5 ) THEN |
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345 | ! |
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346 | !-- Prevent creation of infinite loop |
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347 | message_string = 'ros_count > 5 in Rosenbrock method' |
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348 | CALL message( 'lpm_droplet_condensation', 'PA0018', 2, 2, & |
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349 | 0, 6, 0 ) |
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350 | ENDIF |
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351 | |
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352 | ! |
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353 | !-- Internal time step must not be larger than PALM time step |
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354 | dt_ros = MIN( dt_ros_next, dt_3d ) |
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355 | ! |
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356 | !-- Integrate growth equation in time unless PALM time step is reached |
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357 | DO WHILE ( dt_ros_sum < dt_3d ) |
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358 | |
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359 | internal_timestep_count = internal_timestep_count + 1 |
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360 | |
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361 | ! |
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362 | !-- Derivative at starting value |
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363 | drdt = ddenom / r_ros * ( e_a / e_s - 1.0 - afactor / r_ros + & |
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364 | bfactor / r_ros**3 ) |
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365 | drdt_ini = drdt |
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366 | dt_ros_sum_ini = dt_ros_sum |
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367 | r_ros_ini = r_ros |
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368 | |
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369 | ! |
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370 | !-- Calculate radial derivative of dr/dt |
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371 | d2rdtdr = ddenom * ( ( 1.0 - e_a/e_s ) / r_ros**2 + & |
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372 | 2.0 * afactor / r_ros**3 - & |
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373 | 4.0 * bfactor / r_ros**5 ) |
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374 | ! |
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375 | !-- Adjust stepsize unless required accuracy is reached |
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376 | DO jtry = 1, maxtry+1 |
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377 | |
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378 | IF ( jtry == maxtry+1 ) THEN |
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379 | message_string = 'maxtry > 40 in Rosenbrock method' |
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380 | CALL message( 'lpm_droplet_condensation', 'PA0347', 2, 2, & |
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381 | 0, 6, 0 ) |
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382 | ENDIF |
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383 | |
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384 | aa = 1.0 / ( gam * dt_ros ) - d2rdtdr |
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385 | g1 = drdt_ini / aa |
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386 | r_ros = r_ros_ini + a21 * g1 |
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387 | drdt = ddenom / r_ros * ( e_a / e_s - 1.0 - & |
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388 | afactor / r_ros + & |
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389 | bfactor / r_ros**3 ) |
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390 | |
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391 | g2 = ( drdt + c21 * g1 / dt_ros )& |
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392 | / aa |
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393 | r_ros = r_ros_ini + a31 * g1 + a32 * g2 |
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394 | drdt = ddenom / r_ros * ( e_a / e_s - 1.0 - & |
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395 | afactor / r_ros + & |
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396 | bfactor / r_ros**3 ) |
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397 | |
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398 | g3 = ( drdt + & |
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399 | ( c31 * g1 + c32 * g2 ) / dt_ros ) / aa |
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400 | g4 = ( drdt + & |
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401 | ( c41 * g1 + c42 * g2 + c43 * g3 ) / dt_ros ) / aa |
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402 | r_ros = r_ros_ini + b1 * g1 + b2 * g2 + b3 * g3 + b4 * g4 |
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403 | |
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404 | dt_ros_sum = dt_ros_sum_ini + dt_ros |
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405 | |
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406 | IF ( dt_ros_sum == dt_ros_sum_ini ) THEN |
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407 | message_string = 'zero stepsize in Rosenbrock method' |
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408 | CALL message( 'lpm_droplet_condensation', 'PA0348', 2, 2, & |
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409 | 0, 6, 0 ) |
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410 | ENDIF |
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411 | ! |
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412 | !-- Calculate error |
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413 | err_ros = e1*g1 + e2*g2 + e3*g3 + e4*g4 |
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414 | errmax = 0.0 |
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415 | errmax = MAX( errmax, ABS( err_ros / r_ros_ini ) ) / eps_ros |
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416 | ! |
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417 | !-- Leave loop if accuracy is sufficient, otherwise try again |
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418 | !-- with a reduced stepsize |
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419 | IF ( errmax <= 1.0 ) THEN |
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420 | EXIT |
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421 | ELSE |
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422 | dt_ros = SIGN( MAX( ABS( 0.9 * dt_ros * errmax**pshrnk ), & |
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423 | shrnk * ABS( dt_ros ) ), dt_ros ) |
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424 | ENDIF |
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425 | |
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426 | ENDDO ! loop for stepsize adjustment |
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427 | |
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428 | ! |
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429 | !-- Calculate next internal time step |
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430 | IF ( errmax > errcon ) THEN |
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431 | dt_ros_next = 0.9 * dt_ros * errmax**pgrow |
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432 | ELSE |
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433 | dt_ros_next = grow * dt_ros |
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434 | ENDIF |
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435 | |
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436 | ! |
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437 | !-- Estimated time step is reduced if the PALM time step is exceeded |
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438 | IF ( ( dt_ros_next + dt_ros_sum ) >= dt_3d ) THEN |
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439 | dt_ros = dt_3d - dt_ros_sum |
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440 | ELSE |
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441 | dt_ros = dt_ros_next |
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442 | ENDIF |
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443 | |
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444 | ENDDO |
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445 | ! |
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446 | !-- Store internal time step value for next PALM step |
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447 | particles(n)%rvar1 = dt_ros_next |
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448 | |
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449 | new_r = r_ros |
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450 | ! |
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451 | !-- Radius should not fall below 1E-8 because Rosenbrock method may |
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452 | !-- lead to errors otherwise |
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453 | new_r = MAX( new_r, 1.0E-8_wp ) |
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454 | ! |
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455 | !-- Check if calculated droplet radius change is reasonable since in |
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456 | !-- case of droplet evaporation the Rosenbrock method may lead to |
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457 | !-- secondary solutions which are physically unlikely. |
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458 | !-- Due to the solution effect the droplets may grow for relative |
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459 | !-- humidities below 100%, but change of radius should not be too large. |
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460 | !-- In case of unreasonable droplet growth the Rosenbrock method is |
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461 | !-- recalculated using a smaller initial time step. |
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462 | !-- Limiting values are tested for droplets down to 1.0E-7 |
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463 | IF ( new_r - particles(n)%radius >= 3.0E-7 .AND. & |
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464 | e_a/e_s < 0.97 ) THEN |
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465 | ros_count = ros_count + 1 |
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466 | repeat = .TRUE. |
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467 | ENDIF |
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468 | |
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469 | ENDDO ! Rosenbrock method |
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470 | |
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471 | ENDIF |
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472 | |
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473 | delta_r = new_r - particles(n)%radius |
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474 | |
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475 | ! |
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476 | !-- Sum up the change in volume of liquid water for the respective grid |
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477 | !-- volume (this is needed later in lpm_calc_liquid_water_content for |
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478 | !-- calculating the release of latent heat) |
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479 | i = ( particles(n)%x + 0.5 * dx ) * ddx |
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480 | j = ( particles(n)%y + 0.5 * dy ) * ddy |
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481 | k = particles(n)%z / dz + 1 + offset_ocean_nzt_m1 |
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482 | ! only exact if equidistant |
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483 | |
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484 | ql_c(k,j,i) = ql_c(k,j,i) + particles(n)%weight_factor * & |
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485 | rho_l * 1.33333333 * pi * & |
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486 | ( new_r**3 - particles(n)%radius**3 ) / & |
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487 | ( rho_surface * dx * dy * dz ) |
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488 | IF ( ql_c(k,j,i) > 100.0 ) THEN |
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489 | WRITE( message_string, * ) 'k=',k,' j=',j,' i=',i, & |
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490 | ' ql_c=',ql_c(k,j,i), ' &part(',n,')%wf=', & |
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491 | particles(n)%weight_factor,' delta_r=',delta_r |
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492 | CALL message( 'lpm_droplet_condensation', 'PA0143', 2, 2, -1, 6, 1 ) |
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493 | ENDIF |
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494 | |
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495 | ! |
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496 | !-- Change the droplet radius |
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497 | IF ( ( new_r - particles(n)%radius ) < 0.0 .AND. new_r < 0.0 ) & |
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498 | THEN |
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499 | WRITE( message_string, * ) '#1 k=',k,' j=',j,' i=',i, & |
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500 | ' e_s=',e_s, ' e_a=',e_a,' t_int=',t_int, & |
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501 | ' &delta_r=',delta_r, & |
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502 | ' particle_radius=',particles(n)%radius |
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503 | CALL message( 'lpm_droplet_condensation', 'PA0144', 2, 2, -1, 6, 1 ) |
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504 | ENDIF |
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505 | |
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506 | ! |
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507 | !-- Sum up the total volume of liquid water (needed below for |
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508 | !-- re-calculating the weighting factors) |
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509 | ql_v(k,j,i) = ql_v(k,j,i) + particles(n)%weight_factor * new_r**3 |
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510 | |
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511 | particles(n)%radius = new_r |
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512 | |
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513 | ! |
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514 | !-- Determine radius class of the particle needed for collision |
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515 | IF ( ( hall_kernel .OR. wang_kernel ) .AND. use_kernel_tables ) & |
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516 | THEN |
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517 | particles(n)%class = ( LOG( new_r ) - rclass_lbound ) / & |
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518 | ( rclass_ubound - rclass_lbound ) * & |
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519 | radius_classes |
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520 | particles(n)%class = MIN( particles(n)%class, radius_classes ) |
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521 | particles(n)%class = MAX( particles(n)%class, 1 ) |
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522 | ENDIF |
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523 | |
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524 | ENDDO |
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525 | |
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526 | CALL cpu_log( log_point_s(42), 'lpm_droplet_condens', 'stop' ) |
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527 | |
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528 | |
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529 | END SUBROUTINE lpm_droplet_condensation |
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