1 | !> @file lpm_droplet_condensation.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 |
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6 | ! terms of the GNU General Public License as published by the Free Software |
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7 | ! Foundation, either version 3 of the License, or (at your option) any later |
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8 | ! version. |
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9 | ! |
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10 | ! PALM is distributed in the hope that it will be useful, but WITHOUT ANY |
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11 | ! WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR |
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12 | ! A PARTICULAR PURPOSE. See the GNU General Public License for more details. |
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13 | ! |
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14 | ! You should have received a copy of the GNU General Public License along with |
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15 | ! PALM. If not, see <http://www.gnu.org/licenses/>. |
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16 | ! |
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17 | ! Copyright 1997-2016 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 2001 2016-08-20 18:41:22Z raasch $ |
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27 | ! |
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28 | ! 2000 2016-08-20 18:09:15Z knoop |
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29 | ! Forced header and separation lines into 80 columns |
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30 | ! |
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31 | ! 1890 2016-04-22 08:52:11Z hoffmann |
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32 | ! Some improvements of the Rosenbrock method. If the Rosenbrock method needs more |
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33 | ! than 40 iterations to find a sufficient time setp, the model is not aborted. |
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34 | ! This might lead to small erros. But they can be assumend as negligible, since |
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35 | ! the maximum timesetp of the Rosenbrock method after 40 iterations will be |
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36 | ! smaller than 10^-16 s. |
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37 | ! |
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38 | ! 1871 2016-04-15 11:46:09Z hoffmann |
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39 | ! Initialization of aerosols added. |
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40 | ! |
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41 | ! 1849 2016-04-08 11:33:18Z hoffmann |
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42 | ! Interpolation of supersaturation has been removed because it is not in |
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43 | ! accordance with the release/depletion of latent heat/water vapor in |
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44 | ! interaction_droplets_ptq. |
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45 | ! Calculation of particle Reynolds number has been corrected. |
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46 | ! eps_ros added from modules. |
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47 | ! |
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48 | ! 1831 2016-04-07 13:15:51Z hoffmann |
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49 | ! curvature_solution_effects moved to particle_attributes |
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50 | ! |
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51 | ! 1822 2016-04-07 07:49:42Z hoffmann |
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52 | ! Unused variables removed. |
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53 | ! |
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54 | ! 1682 2015-10-07 23:56:08Z knoop |
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55 | ! Code annotations made doxygen readable |
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56 | ! |
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57 | ! 1359 2014-04-11 17:15:14Z hoffmann |
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58 | ! New particle structure integrated. |
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59 | ! Kind definition added to all floating point numbers. |
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60 | ! |
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61 | ! 1346 2014-03-27 13:18:20Z heinze |
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62 | ! Bugfix: REAL constants provided with KIND-attribute especially in call of |
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63 | ! intrinsic function like MAX, MIN, SIGN |
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64 | ! |
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65 | ! 1322 2014-03-20 16:38:49Z raasch |
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66 | ! REAL constants defined as wp-kind |
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67 | ! |
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68 | ! 1320 2014-03-20 08:40:49Z raasch |
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69 | ! ONLY-attribute added to USE-statements, |
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70 | ! kind-parameters added to all INTEGER and REAL declaration statements, |
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71 | ! kinds are defined in new module kinds, |
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72 | ! comment fields (!:) to be used for variable explanations added to |
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73 | ! all variable declaration statements |
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74 | ! |
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75 | ! 1318 2014-03-17 13:35:16Z raasch |
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76 | ! module interfaces removed |
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77 | ! |
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78 | ! 1092 2013-02-02 11:24:22Z raasch |
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79 | ! unused variables removed |
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80 | ! |
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81 | ! 1071 2012-11-29 16:54:55Z franke |
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82 | ! Ventilation effect for evaporation of large droplets included |
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83 | ! Check for unreasonable results included in calculation of Rosenbrock method |
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84 | ! since physically unlikely results were observed and for the same |
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85 | ! reason the first internal time step in Rosenbrock method should be < 1.0E02 in |
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86 | ! case of evaporation |
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87 | ! Unnecessary calculation of ql_int removed |
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88 | ! Unnecessary calculations in Rosenbrock method (d2rdt2, drdt_m, dt_ros_last) |
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89 | ! removed |
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90 | ! Bugfix: factor in calculation of surface tension changed from 0.00155 to |
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91 | ! 0.000155 |
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92 | ! |
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93 | ! 1036 2012-10-22 13:43:42Z raasch |
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94 | ! code put under GPL (PALM 3.9) |
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95 | ! |
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96 | ! 849 2012-03-15 10:35:09Z raasch |
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97 | ! initial revision (former part of advec_particles) |
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98 | ! |
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99 | ! |
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100 | ! Description: |
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101 | ! ------------ |
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102 | !> Calculates change in droplet radius by condensation/evaporation, using |
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103 | !> either an analytic formula or by numerically integrating the radius growth |
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104 | !> equation including curvature and solution effects using Rosenbrocks method |
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105 | !> (see Numerical recipes in FORTRAN, 2nd edition, p. 731). |
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106 | !> The analytical formula and growth equation follow those given in |
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107 | !> Rogers and Yau (A short course in cloud physics, 3rd edition, p. 102/103). |
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108 | !------------------------------------------------------------------------------! |
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109 | SUBROUTINE lpm_droplet_condensation (ip,jp,kp) |
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110 | |
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111 | |
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112 | USE arrays_3d, & |
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113 | ONLY: hyp, pt, q, ql_c, ql_v |
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114 | |
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115 | USE cloud_parameters, & |
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116 | ONLY: l_d_rv, l_v, rho_l, r_v |
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117 | |
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118 | USE constants, & |
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119 | ONLY: pi |
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120 | |
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121 | USE control_parameters, & |
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122 | ONLY: dt_3d, dz, message_string, molecular_viscosity, rho_surface |
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123 | |
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124 | USE cpulog, & |
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125 | ONLY: cpu_log, log_point_s |
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126 | |
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127 | USE grid_variables, & |
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128 | ONLY: dx, dy |
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129 | |
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130 | USE lpm_collision_kernels_mod, & |
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131 | ONLY: rclass_lbound, rclass_ubound |
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132 | |
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133 | USE kinds |
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134 | |
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135 | USE particle_attributes, & |
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136 | ONLY: curvature_solution_effects, hall_kernel, & |
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137 | molecular_weight_of_solute, molecular_weight_of_water, & |
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138 | number_of_particles, particles, radius_classes, rho_s, & |
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139 | use_kernel_tables, vanthoff, wang_kernel |
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140 | |
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141 | |
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142 | IMPLICIT NONE |
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143 | |
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144 | INTEGER(iwp) :: ip !< |
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145 | INTEGER(iwp) :: internal_timestep_count !< |
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146 | INTEGER(iwp) :: jp !< |
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147 | INTEGER(iwp) :: jtry !< |
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148 | INTEGER(iwp) :: kp !< |
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149 | INTEGER(iwp) :: n !< |
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150 | INTEGER(iwp) :: ros_count !< |
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151 | |
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152 | INTEGER(iwp), PARAMETER :: maxtry = 40 !< |
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153 | |
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154 | LOGICAL :: repeat !< |
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155 | |
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156 | REAL(wp) :: aa !< |
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157 | REAL(wp) :: afactor !< curvature effects |
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158 | REAL(wp) :: arg !< |
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159 | REAL(wp) :: bfactor !< solute effects |
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160 | REAL(wp) :: ddenom !< |
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161 | REAL(wp) :: delta_r !< |
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162 | REAL(wp) :: diameter !< diameter of cloud droplets |
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163 | REAL(wp) :: diff_coeff_v !< diffusivity for water vapor |
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164 | REAL(wp) :: drdt !< |
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165 | REAL(wp) :: drdt_ini !< |
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166 | REAL(wp) :: dt_ros !< |
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167 | REAL(wp) :: dt_ros_next !< |
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168 | REAL(wp) :: dt_ros_sum !< |
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169 | REAL(wp) :: dt_ros_sum_ini !< |
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170 | REAL(wp) :: d2rdtdr !< |
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171 | REAL(wp) :: errmax !< |
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172 | REAL(wp) :: e_a !< current vapor pressure |
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173 | REAL(wp) :: e_s !< current saturation vapor pressure |
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174 | REAL(wp) :: err_ros !< |
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175 | REAL(wp) :: g1 !< |
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176 | REAL(wp) :: g2 !< |
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177 | REAL(wp) :: g3 !< |
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178 | REAL(wp) :: g4 !< |
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179 | REAL(wp) :: r_ros !< |
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180 | REAL(wp) :: r_ros_ini !< |
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181 | REAL(wp) :: sigma !< |
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182 | REAL(wp) :: thermal_conductivity_v !< thermal conductivity for water |
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183 | REAL(wp) :: t_int !< temperature |
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184 | REAL(wp) :: w_s !< terminal velocity of droplets |
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185 | REAL(wp) :: re_p !< |
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186 | |
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187 | ! |
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188 | !-- Parameters for Rosenbrock method |
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189 | REAL(wp), PARAMETER :: a21 = 2.0_wp !< |
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190 | REAL(wp), PARAMETER :: a31 = 48.0_wp / 25.0_wp !< |
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191 | REAL(wp), PARAMETER :: a32 = 6.0_wp / 25.0_wp !< |
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192 | REAL(wp), PARAMETER :: b1 = 19.0_wp / 9.0_wp !< |
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193 | REAL(wp), PARAMETER :: b2 = 0.5_wp !< |
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194 | REAL(wp), PARAMETER :: b3 = 25.0_wp / 108.0_wp !< |
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195 | REAL(wp), PARAMETER :: b4 = 125.0_wp / 108.0_wp !< |
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196 | REAL(wp), PARAMETER :: c21 = -8.0_wp !< |
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197 | REAL(wp), PARAMETER :: c31 = 372.0_wp / 25.0_wp !< |
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198 | REAL(wp), PARAMETER :: c32 = 12.0_wp / 5.0_wp !< |
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199 | REAL(wp), PARAMETER :: c41 = -112.0_wp / 125.0_wp !< |
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200 | REAL(wp), PARAMETER :: c42 = -54.0_wp / 125.0_wp !< |
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201 | REAL(wp), PARAMETER :: c43 = -2.0_wp / 5.0_wp !< |
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202 | REAL(wp), PARAMETER :: errcon = 0.1296_wp !< |
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203 | REAL(wp), PARAMETER :: e1 = 17.0_wp / 54.0_wp !< |
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204 | REAL(wp), PARAMETER :: e2 = 7.0_wp / 36.0_wp !< |
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205 | REAL(wp), PARAMETER :: e3 = 0.0_wp !< |
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206 | REAL(wp), PARAMETER :: e4 = 125.0_wp / 108.0_wp !< |
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207 | REAL(wp), PARAMETER :: eps_ros = 1.0E-3_wp !< accuracy of Rosenbrock method |
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208 | REAL(wp), PARAMETER :: gam = 0.5_wp !< |
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209 | REAL(wp), PARAMETER :: grow = 1.5_wp !< |
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210 | REAL(wp), PARAMETER :: pgrow = -0.25_wp !< |
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211 | REAL(wp), PARAMETER :: pshrnk = -1.0_wp /3.0_wp !< |
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212 | REAL(wp), PARAMETER :: shrnk = 0.5_wp !< |
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213 | |
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214 | ! |
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215 | !-- Parameters for terminal velocity |
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216 | REAL(wp), PARAMETER :: a_rog = 9.65_wp !< parameter for fall velocity |
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217 | REAL(wp), PARAMETER :: b_rog = 10.43_wp !< parameter for fall velocity |
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218 | REAL(wp), PARAMETER :: c_rog = 0.6_wp !< parameter for fall velocity |
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219 | REAL(wp), PARAMETER :: k_cap_rog = 4.0_wp !< parameter for fall velocity |
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220 | REAL(wp), PARAMETER :: k_low_rog = 12.0_wp !< parameter for fall velocity |
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221 | REAL(wp), PARAMETER :: d0_rog = 0.745_wp !< separation diameter |
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222 | |
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223 | REAL(wp), DIMENSION(number_of_particles) :: ventilation_effect !< |
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224 | REAL(wp), DIMENSION(number_of_particles) :: new_r !< |
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225 | |
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226 | |
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227 | |
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228 | CALL cpu_log( log_point_s(42), 'lpm_droplet_condens', 'start' ) |
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229 | |
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230 | ! |
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231 | !-- Calculate temperature, saturation vapor pressure and current vapor pressure |
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232 | t_int = pt(kp,jp,ip) * ( hyp(kp) / 100000.0_wp )**0.286_wp |
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233 | e_s = 611.0_wp * EXP( l_d_rv * ( 3.6609E-3_wp - 1.0_wp / t_int ) ) |
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234 | e_a = q(kp,jp,ip) * hyp(kp) / ( 0.378_wp * q(kp,jp,ip) + 0.622_wp ) |
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235 | ! |
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236 | !-- Thermal conductivity for water (from Rogers and Yau, Table 7.1), |
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237 | !-- diffusivity for water vapor (after Hall und Pruppacher, 1976) |
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238 | thermal_conductivity_v = 7.94048E-05_wp * t_int + 0.00227011_wp |
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239 | diff_coeff_v = 0.211E-4_wp * ( t_int / 273.15_wp )**1.94_wp * & |
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240 | ( 101325.0_wp / hyp(kp) ) |
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241 | ! |
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242 | !-- Calculate effects of heat conductivity and diffusion of water vapor on the |
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243 | !-- condensation/evaporation process (typically known as 1.0 / (F_k + F_d) ) |
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244 | ddenom = 1.0_wp / ( rho_l * r_v * t_int / ( e_s * diff_coeff_v ) + & |
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245 | ( l_v / ( r_v * t_int ) - 1.0_wp ) * rho_l * & |
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246 | l_v / ( thermal_conductivity_v * t_int ) & |
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247 | ) |
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248 | |
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249 | new_r = 0.0_wp |
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250 | |
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251 | ! |
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252 | !-- Determine ventilation effect on evaporation of large drops |
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253 | DO n = 1, number_of_particles |
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254 | |
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255 | IF ( particles(n)%radius >= 4.0E-5_wp .AND. e_a / e_s < 1.0_wp ) THEN |
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256 | ! |
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257 | !-- Terminal velocity is computed for vertical direction (Rogers et al., |
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258 | !-- 1993, J. Appl. Meteorol.) |
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259 | diameter = particles(n)%radius * 2000.0_wp !diameter in mm |
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260 | IF ( diameter <= d0_rog ) THEN |
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261 | w_s = k_cap_rog * diameter * ( 1.0_wp - EXP( -k_low_rog * diameter ) ) |
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262 | ELSE |
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263 | w_s = a_rog - b_rog * EXP( -c_rog * diameter ) |
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264 | ENDIF |
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265 | ! |
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266 | !-- First calculate droplet's Reynolds number |
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267 | re_p = 2.0_wp * particles(n)%radius * w_s / molecular_viscosity |
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268 | ! |
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269 | !-- Ventilation coefficient (Rogers and Yau, 1989): |
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270 | IF ( re_p > 2.5_wp ) THEN |
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271 | ventilation_effect(n) = 0.78_wp + 0.28_wp * SQRT( re_p ) |
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272 | ELSE |
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273 | ventilation_effect(n) = 1.0_wp + 0.09_wp * re_p |
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274 | ENDIF |
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275 | ELSE |
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276 | ! |
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277 | !-- For small droplets or in supersaturated environments, the ventilation |
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278 | !-- effect does not play a role |
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279 | ventilation_effect(n) = 1.0_wp |
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280 | ENDIF |
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281 | ENDDO |
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282 | |
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283 | ! |
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284 | !-- Use analytic model for condensational growth |
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285 | IF( .NOT. curvature_solution_effects ) then |
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286 | DO n = 1, number_of_particles |
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287 | arg = particles(n)%radius**2 + 2.0_wp * dt_3d * ddenom * & |
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288 | ventilation_effect(n) * & |
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289 | ( e_a / e_s - 1.0_wp ) |
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290 | arg = MAX( arg, 1.0E-16_wp ) |
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291 | new_r(n) = SQRT( arg ) |
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292 | ENDDO |
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293 | ENDIF |
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294 | |
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295 | ! |
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296 | !-- If selected, use numerical solution of the condensational growth |
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297 | !-- equation (e.g., for studying the activation of aerosols). |
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298 | !-- Curvature and solutions effects are included in growth equation. |
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299 | !-- Change in Radius is calculated with a 4th-order Rosenbrock method |
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300 | !-- for stiff o.d.e's with monitoring local truncation error to adjust |
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301 | !-- stepsize (see Numerical recipes in FORTRAN, 2nd edition, p. 731). |
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302 | DO n = 1, number_of_particles |
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303 | IF ( curvature_solution_effects ) THEN |
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304 | |
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305 | ros_count = 0 |
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306 | repeat = .TRUE. |
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307 | ! |
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308 | !-- Carry out the Rosenbrock algorithm. In case of unreasonable results |
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309 | !-- the switch "repeat" will be set true and the algorithm will be carried |
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310 | !-- out again with the internal time step set to its initial (small) value. |
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311 | !-- Unreasonable results may occur if the external conditions, especially |
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312 | !-- the supersaturation, has significantly changed compared to the last |
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313 | !-- PALM timestep. |
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314 | DO WHILE ( repeat ) |
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315 | |
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316 | repeat = .FALSE. |
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317 | ! |
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318 | !-- Curvature effect (afactor) with surface tension parameterization |
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319 | !-- by Straka (2009) |
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320 | sigma = 0.0761_wp - 0.000155_wp * ( t_int - 273.15_wp ) |
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321 | afactor = 2.0_wp * sigma / ( rho_l * r_v * t_int ) |
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322 | ! |
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323 | !-- Solute effect (bfactor) |
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324 | bfactor = vanthoff * rho_s * particles(n)%rvar2**3 * & |
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325 | molecular_weight_of_water / & |
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326 | ( rho_l * molecular_weight_of_solute ) |
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327 | |
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328 | r_ros = particles(n)%radius |
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329 | dt_ros_sum = 0.0_wp ! internal integrated time (s) |
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330 | internal_timestep_count = 0 |
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331 | ! |
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332 | !-- Take internal time step values from the end of last PALM time step |
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333 | dt_ros_next = particles(n)%rvar1 |
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334 | |
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335 | ! |
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336 | !-- Internal time step should not be > 1.0E-2 and < 1.0E-6 |
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337 | IF ( dt_ros_next > 1.0E-2_wp ) THEN |
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338 | dt_ros_next = 1.0E-2_wp |
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339 | ELSEIF ( dt_ros_next < 1.0E-6_wp ) THEN |
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340 | dt_ros_next = 1.0E-6_wp |
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341 | ENDIF |
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342 | |
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343 | ! |
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344 | !-- If calculation of Rosenbrock method is repeated due to unreasonalble |
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345 | !-- results during previous try the initial internal time step has to be |
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346 | !-- reduced |
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347 | IF ( ros_count > 1 ) THEN |
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348 | dt_ros_next = dt_ros_next * 0.1_wp |
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349 | ELSEIF ( ros_count > 5 ) THEN |
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350 | ! |
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351 | !-- Prevent creation of infinite loop |
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352 | message_string = 'ros_count > 5 in Rosenbrock method' |
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353 | CALL message( 'lpm_droplet_condensation', 'PA0018', 2, 2, & |
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354 | 0, 6, 0 ) |
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355 | ENDIF |
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356 | |
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357 | ! |
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358 | !-- Internal time step must not be larger than PALM time step |
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359 | dt_ros = MIN( dt_ros_next, dt_3d ) |
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360 | |
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361 | ! |
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362 | !-- Integrate growth equation in time unless PALM time step is reached |
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363 | DO WHILE ( dt_ros_sum < dt_3d ) |
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364 | |
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365 | internal_timestep_count = internal_timestep_count + 1 |
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366 | |
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367 | ! |
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368 | !-- Derivative at starting value |
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369 | drdt = ddenom * ventilation_effect(n) * ( e_a / e_s - 1.0_wp - & |
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370 | afactor / r_ros + & |
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371 | bfactor / r_ros**3 & |
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372 | ) / r_ros |
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373 | |
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374 | drdt_ini = drdt |
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375 | dt_ros_sum_ini = dt_ros_sum |
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376 | r_ros_ini = r_ros |
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377 | |
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378 | ! |
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379 | !-- Calculate radial derivative of dr/dt |
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380 | d2rdtdr = ddenom * ventilation_effect(n) * & |
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381 | ( ( 1.0_wp - e_a / e_s ) / r_ros**2 + & |
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382 | 2.0_wp * afactor / r_ros**3 - & |
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383 | 4.0_wp * bfactor / r_ros**5 & |
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384 | ) |
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385 | ! |
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386 | !-- Adjust stepsize unless required accuracy is reached |
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387 | DO jtry = 1, maxtry+1 |
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388 | |
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389 | IF ( jtry == maxtry+1 ) THEN |
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390 | message_string = 'maxtry > 40 in Rosenbrock method' |
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391 | CALL message( 'lpm_droplet_condensation', 'PA0347', 0, & |
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392 | 1, 0, 6, 0 ) |
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393 | ENDIF |
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394 | |
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395 | aa = 1.0_wp / ( gam * dt_ros ) - d2rdtdr |
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396 | g1 = drdt_ini / aa |
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397 | r_ros = r_ros_ini + a21 * g1 |
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398 | drdt = ddenom * ventilation_effect(n) * ( e_a / e_s - 1.0_wp - & |
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399 | afactor / r_ros + & |
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400 | bfactor / r_ros**3 & |
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401 | ) / r_ros |
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402 | |
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403 | g2 = ( drdt + c21 * g1 / dt_ros )& |
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404 | / aa |
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405 | r_ros = r_ros_ini + a31 * g1 + a32 * g2 |
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406 | drdt = ddenom * ventilation_effect(n) * ( e_a / e_s - 1.0_wp - & |
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407 | afactor / r_ros + & |
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408 | bfactor / r_ros**3 & |
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409 | ) / r_ros |
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410 | |
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411 | g3 = ( drdt + & |
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412 | ( c31 * g1 + c32 * g2 ) / dt_ros ) / aa |
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413 | g4 = ( drdt + & |
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414 | ( c41 * g1 + c42 * g2 + c43 * g3 ) / dt_ros ) / aa |
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415 | r_ros = r_ros_ini + b1 * g1 + b2 * g2 + b3 * g3 + b4 * g4 |
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416 | |
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417 | dt_ros_sum = dt_ros_sum_ini + dt_ros |
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418 | |
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419 | IF ( dt_ros_sum == dt_ros_sum_ini ) THEN |
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420 | message_string = 'zero stepsize in Rosenbrock method' |
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421 | CALL message( 'lpm_droplet_condensation', 'PA0348', 2, & |
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422 | 2, 0, 6, 0 ) |
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423 | ENDIF |
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424 | ! |
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425 | !-- Calculate error |
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426 | err_ros = e1 * g1 + e2 * g2 + e3 * g3 + e4 * g4 |
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427 | errmax = 0.0_wp |
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428 | errmax = MAX( errmax, ABS( err_ros / r_ros_ini ) ) / eps_ros |
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429 | ! |
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430 | !-- Leave loop if accuracy is sufficient, otherwise try again |
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431 | !-- with a reduced stepsize |
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432 | IF ( errmax <= 1.0_wp ) THEN |
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433 | EXIT |
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434 | ELSE |
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435 | dt_ros = MAX( ABS( 0.9_wp * dt_ros * errmax**pshrnk ), & |
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436 | shrnk * ABS( dt_ros ) ) |
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437 | ENDIF |
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438 | |
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439 | ENDDO ! loop for stepsize adjustment |
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440 | |
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441 | ! |
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442 | !-- Calculate next internal time step |
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443 | IF ( errmax > errcon ) THEN |
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444 | dt_ros_next = 0.9_wp * dt_ros * errmax**pgrow |
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445 | ELSE |
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446 | dt_ros_next = grow * dt_ros |
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447 | ENDIF |
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448 | |
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449 | ! |
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450 | !-- Estimated time step is reduced if the PALM time step is exceeded |
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451 | IF ( ( dt_ros_next + dt_ros_sum ) >= dt_3d ) THEN |
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452 | dt_ros = dt_3d - dt_ros_sum |
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453 | ELSE |
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454 | dt_ros = dt_ros_next |
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455 | ENDIF |
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456 | |
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457 | ENDDO |
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458 | ! |
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459 | !-- Store internal time step value for next PALM step |
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460 | particles(n)%rvar1 = dt_ros_next |
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461 | |
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462 | ! |
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463 | !-- Radius should not fall below 1E-8 because Rosenbrock method may |
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464 | !-- lead to errors otherwise |
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465 | new_r(n) = MAX( r_ros, particles(n)%rvar2 ) |
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466 | ! |
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467 | !-- Check if calculated droplet radius change is reasonable since in |
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468 | !-- case of droplet evaporation the Rosenbrock method may lead to |
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469 | !-- secondary solutions which are physically unlikely. |
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470 | !-- Due to the solution effect the droplets may grow for relative |
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471 | !-- humidities below 100%, but change of radius should not be too |
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472 | !-- large. In case of unreasonable droplet growth the Rosenbrock |
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473 | !-- method is recalculated using a smaller initial time step. |
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474 | !-- Limiting values are tested for droplets down to 1.0E-7 |
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475 | IF ( new_r(n) - particles(n)%radius >= 3.0E-7_wp .AND. & |
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476 | e_a / e_s < 0.97_wp ) THEN |
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477 | ros_count = ros_count + 1 |
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478 | repeat = .TRUE. |
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479 | ENDIF |
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480 | |
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481 | ENDDO ! Rosenbrock method |
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482 | |
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483 | ENDIF |
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484 | |
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485 | delta_r = new_r(n) - particles(n)%radius |
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486 | |
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487 | ! |
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488 | !-- Sum up the change in volume of liquid water for the respective grid |
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489 | !-- volume (this is needed later in lpm_calc_liquid_water_content for |
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490 | !-- calculating the release of latent heat) |
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491 | ql_c(kp,jp,ip) = ql_c(kp,jp,ip) + particles(n)%weight_factor * & |
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492 | rho_l * 1.33333333_wp * pi * & |
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493 | ( new_r(n)**3 - particles(n)%radius**3 ) / & |
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494 | ( rho_surface * dx * dy * dz ) |
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495 | IF ( ql_c(kp,jp,ip) > 100.0_wp ) THEN |
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496 | WRITE( message_string, * ) 'k=',kp,' j=',jp,' i=',ip, & |
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497 | ' ql_c=',ql_c(kp,jp,ip), ' &part(',n,')%wf=', & |
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498 | particles(n)%weight_factor,' delta_r=',delta_r |
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499 | CALL message( 'lpm_droplet_condensation', 'PA0143', 2, 2, -1, 6, 1 ) |
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500 | ENDIF |
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501 | |
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502 | ! |
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503 | !-- Change the droplet radius |
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504 | IF ( ( new_r(n) - particles(n)%radius ) < 0.0_wp .AND. & |
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505 | new_r(n) < 0.0_wp ) THEN |
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506 | WRITE( message_string, * ) '#1 k=',kp,' j=',jp,' i=',ip, & |
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507 | ' e_s=',e_s, ' e_a=',e_a,' t_int=',t_int, & |
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508 | ' &delta_r=',delta_r, & |
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509 | ' particle_radius=',particles(n)%radius |
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510 | CALL message( 'lpm_droplet_condensation', 'PA0144', 2, 2, -1, 6, 1 ) |
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511 | ENDIF |
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512 | |
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513 | ! |
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514 | !-- Sum up the total volume of liquid water (needed below for |
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515 | !-- re-calculating the weighting factors) |
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516 | ql_v(kp,jp,ip) = ql_v(kp,jp,ip) + particles(n)%weight_factor * new_r(n)**3 |
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517 | |
---|
518 | particles(n)%radius = new_r(n) |
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519 | |
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520 | ! |
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521 | !-- Determine radius class of the particle needed for collision |
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522 | IF ( ( hall_kernel .OR. wang_kernel ) .AND. use_kernel_tables ) & |
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523 | THEN |
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524 | particles(n)%class = ( LOG( new_r(n) ) - rclass_lbound ) / & |
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525 | ( rclass_ubound - rclass_lbound ) * & |
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526 | radius_classes |
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527 | particles(n)%class = MIN( particles(n)%class, radius_classes ) |
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528 | particles(n)%class = MAX( particles(n)%class, 1 ) |
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529 | ENDIF |
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530 | |
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531 | ENDDO |
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532 | |
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533 | CALL cpu_log( log_point_s(42), 'lpm_droplet_condens', 'stop' ) |
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534 | |
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535 | |
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536 | END SUBROUTINE lpm_droplet_condensation |
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