1 | SUBROUTINE flow_statistics |
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2 | |
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3 | !------------------------------------------------------------------------------! |
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4 | ! Current revisions: |
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5 | ! ----------------- |
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6 | ! |
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7 | ! |
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8 | ! Former revisions: |
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9 | ! ----------------- |
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10 | ! $Id: flow_statistics.f90 392 2009-09-24 10:39:14Z weinreis $ |
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11 | ! |
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12 | ! 388 2009-09-23 09:40:33Z raasch |
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13 | ! Vertical profiles of potential density and hydrostatic pressure are |
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14 | ! calculated. |
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15 | ! Added missing timeseries calculation of w"q"(0), moved timeseries q* to the |
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16 | ! end. |
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17 | ! Temperature gradient criterion for estimating the boundary layer height |
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18 | ! replaced by the gradient criterion of Sullivan et al. (1998). |
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19 | ! Output of messages replaced by message handling routine. |
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20 | ! |
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21 | ! 197 2008-09-16 15:29:03Z raasch |
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22 | ! Spline timeseries splptx etc. removed, timeseries w'u', w'v', w'q' (k=0) |
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23 | ! added, |
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24 | ! bugfix: divide sums(k,8) (e) and sums(k,34) (e*) by ngp_2dh_s_inner(k,sr) |
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25 | ! (like other scalars) |
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26 | ! |
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27 | ! 133 2007-11-20 10:10:53Z letzel |
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28 | ! Vertical profiles now based on nzb_s_inner; they are divided by |
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29 | ! ngp_2dh_s_inner (scalars, procucts of scalars) and ngp_2dh (staggered |
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30 | ! velocity components and their products, procucts of scalars and velocity |
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31 | ! components), respectively. |
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32 | ! |
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33 | ! 106 2007-08-16 14:30:26Z raasch |
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34 | ! Prescribed momentum fluxes at the top surface are used, |
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35 | ! profiles for w*p* and w"e are calculated |
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36 | ! |
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37 | ! 97 2007-06-21 08:23:15Z raasch |
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38 | ! Statistics for ocean version (salinity, density) added, |
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39 | ! calculation of z_i and Deardorff velocity scale adjusted to be used with |
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40 | ! the ocean version |
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41 | ! |
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42 | ! 87 2007-05-22 15:46:47Z raasch |
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43 | ! Two more arguments added to user_statistics, which is now also called for |
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44 | ! user-defined profiles, |
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45 | ! var_hom and var_sum renamed pr_palm |
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46 | ! |
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47 | ! 82 2007-04-16 15:40:52Z raasch |
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48 | ! Cpp-directive lcmuk changed to intel_openmp_bug |
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49 | ! |
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50 | ! 75 2007-03-22 09:54:05Z raasch |
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51 | ! Collection of time series quantities moved from routine flow_statistics to |
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52 | ! here, routine user_statistics is called for each statistic region, |
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53 | ! moisture renamed humidity |
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54 | ! |
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55 | ! 19 2007-02-23 04:53:48Z raasch |
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56 | ! fluxes at top modified (tswst, qswst) |
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57 | ! |
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58 | ! RCS Log replace by Id keyword, revision history cleaned up |
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59 | ! |
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60 | ! Revision 1.41 2006/08/04 14:37:50 raasch |
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61 | ! Error removed in non-parallel part (sums_l) |
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62 | ! |
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63 | ! Revision 1.1 1997/08/11 06:15:17 raasch |
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64 | ! Initial revision |
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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 | ! Compute average profiles and further average flow quantities for the different |
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70 | ! user-defined (sub-)regions. The region indexed 0 is the total model domain. |
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71 | ! |
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72 | ! NOTE: For simplicity, nzb_s_inner and nzb_diff_s_inner are being used as a |
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73 | ! ---- lower vertical index for k-loops for all variables, although strictly |
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74 | ! speaking the k-loops would have to be split up according to the staggered |
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75 | ! grid. However, this implies no error since staggered velocity components are |
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76 | ! zero at the walls and inside buildings. |
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77 | !------------------------------------------------------------------------------! |
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78 | |
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79 | USE arrays_3d |
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80 | USE cloud_parameters |
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81 | USE cpulog |
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82 | USE grid_variables |
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83 | USE indices |
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84 | USE interfaces |
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85 | USE pegrid |
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86 | USE statistics |
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87 | USE control_parameters |
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88 | |
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89 | IMPLICIT NONE |
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90 | |
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91 | INTEGER :: i, j, k, omp_get_thread_num, sr, tn |
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92 | LOGICAL :: first |
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93 | REAL :: dptdz_threshold, height, pts, sums_l_eper, sums_l_etot, ust, & |
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94 | ust2, u2, vst, vst2, v2, w2, z_i(2) |
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95 | REAL :: dptdz(nzb+1:nzt+1) |
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96 | REAL :: sums_ll(nzb:nzt+1,2) |
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97 | |
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98 | |
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99 | CALL cpu_log( log_point(10), 'flow_statistics', 'start' ) |
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100 | |
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101 | ! |
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102 | !-- To be on the safe side, check whether flow_statistics has already been |
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103 | !-- called once after the current time step |
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104 | IF ( flow_statistics_called ) THEN |
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105 | |
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106 | message_string = 'flow_statistics is called two times within one ' // & |
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107 | 'timestep' |
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108 | CALL message( 'flow_statistics', 'PA0190', 1, 2, 0, 6, 0 ) |
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109 | |
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110 | ENDIF |
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111 | |
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112 | ! |
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113 | !-- Compute statistics for each (sub-)region |
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114 | DO sr = 0, statistic_regions |
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115 | |
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116 | ! |
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117 | !-- Initialize (local) summation array |
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118 | sums_l = 0.0 |
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119 | |
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120 | ! |
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121 | !-- Store sums that have been computed in other subroutines in summation |
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122 | !-- array |
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123 | sums_l(:,11,:) = sums_l_l(:,sr,:) ! mixing length from diffusivities |
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124 | !-- WARNING: next line still has to be adjusted for OpenMP |
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125 | sums_l(:,21,0) = sums_wsts_bc_l(:,sr) ! heat flux from advec_s_bc |
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126 | sums_l(nzb+9,pr_palm,0) = sums_divold_l(sr) ! old divergence from pres |
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127 | sums_l(nzb+10,pr_palm,0) = sums_divnew_l(sr) ! new divergence from pres |
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128 | |
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129 | ! |
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130 | !-- Horizontally averaged profiles of horizontal velocities and temperature. |
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131 | !-- They must have been computed before, because they are already required |
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132 | !-- for other horizontal averages. |
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133 | tn = 0 |
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134 | !$OMP PARALLEL PRIVATE( i, j, k, tn ) |
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135 | #if defined( __intel_openmp_bug ) |
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136 | tn = omp_get_thread_num() |
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137 | #else |
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138 | !$ tn = omp_get_thread_num() |
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139 | #endif |
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140 | |
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141 | !$OMP DO |
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142 | DO i = nxl, nxr |
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143 | DO j = nys, nyn |
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144 | DO k = nzb_s_inner(j,i), nzt+1 |
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145 | sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr) |
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146 | sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr) |
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147 | sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr) |
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148 | ENDDO |
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149 | ENDDO |
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150 | ENDDO |
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151 | |
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152 | ! |
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153 | !-- Horizontally averaged profile of salinity |
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154 | IF ( ocean ) THEN |
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155 | !$OMP DO |
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156 | DO i = nxl, nxr |
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157 | DO j = nys, nyn |
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158 | DO k = nzb_s_inner(j,i), nzt+1 |
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159 | sums_l(k,23,tn) = sums_l(k,23,tn) + & |
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160 | sa(k,j,i) * rmask(j,i,sr) |
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161 | ENDDO |
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162 | ENDDO |
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163 | ENDDO |
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164 | ENDIF |
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165 | |
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166 | ! |
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167 | !-- Horizontally averaged profiles of virtual potential temperature, |
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168 | !-- total water content, specific humidity and liquid water potential |
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169 | !-- temperature |
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170 | IF ( humidity ) THEN |
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171 | !$OMP DO |
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172 | DO i = nxl, nxr |
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173 | DO j = nys, nyn |
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174 | DO k = nzb_s_inner(j,i), nzt+1 |
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175 | sums_l(k,44,tn) = sums_l(k,44,tn) + & |
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176 | vpt(k,j,i) * rmask(j,i,sr) |
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177 | sums_l(k,41,tn) = sums_l(k,41,tn) + & |
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178 | q(k,j,i) * rmask(j,i,sr) |
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179 | ENDDO |
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180 | ENDDO |
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181 | ENDDO |
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182 | IF ( cloud_physics ) THEN |
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183 | !$OMP DO |
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184 | DO i = nxl, nxr |
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185 | DO j = nys, nyn |
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186 | DO k = nzb_s_inner(j,i), nzt+1 |
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187 | sums_l(k,42,tn) = sums_l(k,42,tn) + & |
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188 | ( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr) |
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189 | sums_l(k,43,tn) = sums_l(k,43,tn) + ( & |
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190 | pt(k,j,i) + l_d_cp*pt_d_t(k) * ql(k,j,i) & |
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191 | ) * rmask(j,i,sr) |
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192 | ENDDO |
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193 | ENDDO |
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194 | ENDDO |
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195 | ENDIF |
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196 | ENDIF |
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197 | |
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198 | ! |
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199 | !-- Horizontally averaged profiles of passive scalar |
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200 | IF ( passive_scalar ) THEN |
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201 | !$OMP DO |
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202 | DO i = nxl, nxr |
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203 | DO j = nys, nyn |
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204 | DO k = nzb_s_inner(j,i), nzt+1 |
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205 | sums_l(k,41,tn) = sums_l(k,41,tn) + q(k,j,i) * rmask(j,i,sr) |
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206 | ENDDO |
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207 | ENDDO |
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208 | ENDDO |
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209 | ENDIF |
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210 | !$OMP END PARALLEL |
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211 | |
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212 | ! |
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213 | !-- Summation of thread sums |
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214 | IF ( threads_per_task > 1 ) THEN |
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215 | DO i = 1, threads_per_task-1 |
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216 | sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i) |
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217 | sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i) |
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218 | sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i) |
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219 | IF ( ocean ) THEN |
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220 | sums_l(:,23,0) = sums_l(:,23,0) + sums_l(:,23,i) |
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221 | ENDIF |
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222 | IF ( humidity ) THEN |
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223 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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224 | sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i) |
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225 | IF ( cloud_physics ) THEN |
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226 | sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i) |
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227 | sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i) |
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228 | ENDIF |
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229 | ENDIF |
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230 | IF ( passive_scalar ) THEN |
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231 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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232 | ENDIF |
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233 | ENDDO |
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234 | ENDIF |
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235 | |
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236 | #if defined( __parallel ) |
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237 | ! |
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238 | !-- Compute total sum from local sums |
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239 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), nzt+2-nzb, MPI_REAL, & |
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240 | MPI_SUM, comm2d, ierr ) |
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241 | CALL MPI_ALLREDUCE( sums_l(nzb,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, & |
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242 | MPI_SUM, comm2d, ierr ) |
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243 | CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, & |
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244 | MPI_SUM, comm2d, ierr ) |
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245 | IF ( ocean ) THEN |
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246 | CALL MPI_ALLREDUCE( sums_l(nzb,23,0), sums(nzb,23), nzt+2-nzb, & |
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247 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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248 | ENDIF |
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249 | IF ( humidity ) THEN |
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250 | CALL MPI_ALLREDUCE( sums_l(nzb,44,0), sums(nzb,44), nzt+2-nzb, & |
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251 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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252 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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253 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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254 | IF ( cloud_physics ) THEN |
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255 | CALL MPI_ALLREDUCE( sums_l(nzb,42,0), sums(nzb,42), nzt+2-nzb, & |
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256 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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257 | CALL MPI_ALLREDUCE( sums_l(nzb,43,0), sums(nzb,43), nzt+2-nzb, & |
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258 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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259 | ENDIF |
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260 | ENDIF |
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261 | |
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262 | IF ( passive_scalar ) THEN |
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263 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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264 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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265 | ENDIF |
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266 | #else |
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267 | sums(:,1) = sums_l(:,1,0) |
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268 | sums(:,2) = sums_l(:,2,0) |
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269 | sums(:,4) = sums_l(:,4,0) |
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270 | IF ( ocean ) sums(:,23) = sums_l(:,23,0) |
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271 | IF ( humidity ) THEN |
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272 | sums(:,44) = sums_l(:,44,0) |
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273 | sums(:,41) = sums_l(:,41,0) |
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274 | IF ( cloud_physics ) THEN |
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275 | sums(:,42) = sums_l(:,42,0) |
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276 | sums(:,43) = sums_l(:,43,0) |
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277 | ENDIF |
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278 | ENDIF |
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279 | IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0) |
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280 | #endif |
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281 | |
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282 | ! |
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283 | !-- Final values are obtained by division by the total number of grid points |
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284 | !-- used for summation. After that store profiles. |
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285 | sums(:,1) = sums(:,1) / ngp_2dh(sr) |
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286 | sums(:,2) = sums(:,2) / ngp_2dh(sr) |
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287 | sums(:,4) = sums(:,4) / ngp_2dh_s_inner(:,sr) |
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288 | hom(:,1,1,sr) = sums(:,1) ! u |
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289 | hom(:,1,2,sr) = sums(:,2) ! v |
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290 | hom(:,1,4,sr) = sums(:,4) ! pt |
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291 | |
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292 | ! |
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293 | !-- Salinity |
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294 | IF ( ocean ) THEN |
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295 | sums(:,23) = sums(:,23) / ngp_2dh_s_inner(:,sr) |
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296 | hom(:,1,23,sr) = sums(:,23) ! sa |
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297 | ENDIF |
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298 | |
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299 | ! |
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300 | !-- Humidity and cloud parameters |
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301 | IF ( humidity ) THEN |
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302 | sums(:,44) = sums(:,44) / ngp_2dh_s_inner(:,sr) |
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303 | sums(:,41) = sums(:,41) / ngp_2dh_s_inner(:,sr) |
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304 | hom(:,1,44,sr) = sums(:,44) ! vpt |
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305 | hom(:,1,41,sr) = sums(:,41) ! qv (q) |
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306 | IF ( cloud_physics ) THEN |
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307 | sums(:,42) = sums(:,42) / ngp_2dh_s_inner(:,sr) |
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308 | sums(:,43) = sums(:,43) / ngp_2dh_s_inner(:,sr) |
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309 | hom(:,1,42,sr) = sums(:,42) ! qv |
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310 | hom(:,1,43,sr) = sums(:,43) ! pt |
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311 | ENDIF |
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312 | ENDIF |
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313 | |
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314 | ! |
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315 | !-- Passive scalar |
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316 | IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / & |
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317 | ngp_2dh_s_inner(:,sr) ! s (q) |
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318 | |
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319 | ! |
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320 | !-- Horizontally averaged profiles of the remaining prognostic variables, |
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321 | !-- variances, the total and the perturbation energy (single values in last |
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322 | !-- column of sums_l) and some diagnostic quantities. |
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323 | !-- NOTE: for simplicity, nzb_s_inner is used below, although strictly |
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324 | !-- ---- speaking the following k-loop would have to be split up and |
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325 | !-- rearranged according to the staggered grid. |
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326 | !-- However, this implies no error since staggered velocity components |
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327 | !-- are zero at the walls and inside buildings. |
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328 | tn = 0 |
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329 | #if defined( __intel_openmp_bug ) |
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330 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, & |
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331 | !$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
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332 | tn = omp_get_thread_num() |
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333 | #else |
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334 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
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335 | !$ tn = omp_get_thread_num() |
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336 | #endif |
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337 | !$OMP DO |
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338 | DO i = nxl, nxr |
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339 | DO j = nys, nyn |
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340 | sums_l_etot = 0.0 |
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341 | sums_l_eper = 0.0 |
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342 | DO k = nzb_s_inner(j,i), nzt+1 |
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343 | u2 = u(k,j,i)**2 |
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344 | v2 = v(k,j,i)**2 |
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345 | w2 = w(k,j,i)**2 |
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346 | ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2 |
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347 | vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2 |
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348 | ! |
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349 | !-- Prognostic and diagnostic variables |
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350 | sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr) |
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351 | sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr) |
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352 | sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr) |
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353 | sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr) |
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354 | sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i) |
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355 | |
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356 | ! |
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357 | !-- Variances |
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358 | sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr) |
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359 | sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr) |
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360 | sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr) |
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361 | sums_l(k,33,tn) = sums_l(k,33,tn) + & |
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362 | ( pt(k,j,i)-hom(k,1,4,sr) )**2 * rmask(j,i,sr) |
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363 | ! |
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364 | !-- Higher moments |
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365 | !-- (Computation of the skewness of w further below) |
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366 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
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367 | rmask(j,i,sr) |
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368 | ! |
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369 | !-- Perturbation energy |
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370 | sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * ( ust2 + vst2 + w2 ) & |
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371 | * rmask(j,i,sr) |
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372 | sums_l_etot = sums_l_etot + & |
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373 | 0.5 * ( u2 + v2 + w2 ) * rmask(j,i,sr) |
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374 | sums_l_eper = sums_l_eper + & |
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375 | 0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr) |
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376 | ENDDO |
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377 | ! |
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378 | !-- Total and perturbation energy for the total domain (being |
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379 | !-- collected in the last column of sums_l). Summation of these |
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380 | !-- quantities is seperated from the previous loop in order to |
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381 | !-- allow vectorization of that loop. |
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382 | sums_l(nzb+4,pr_palm,tn) = sums_l(nzb+4,pr_palm,tn) + sums_l_etot |
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383 | sums_l(nzb+5,pr_palm,tn) = sums_l(nzb+5,pr_palm,tn) + sums_l_eper |
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384 | ! |
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385 | !-- 2D-arrays (being collected in the last column of sums_l) |
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386 | sums_l(nzb,pr_palm,tn) = sums_l(nzb,pr_palm,tn) + & |
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387 | us(j,i) * rmask(j,i,sr) |
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388 | sums_l(nzb+1,pr_palm,tn) = sums_l(nzb+1,pr_palm,tn) + & |
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389 | usws(j,i) * rmask(j,i,sr) |
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390 | sums_l(nzb+2,pr_palm,tn) = sums_l(nzb+2,pr_palm,tn) + & |
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391 | vsws(j,i) * rmask(j,i,sr) |
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392 | sums_l(nzb+3,pr_palm,tn) = sums_l(nzb+3,pr_palm,tn) + & |
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393 | ts(j,i) * rmask(j,i,sr) |
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394 | IF ( humidity ) THEN |
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395 | sums_l(nzb+12,pr_palm,tn) = sums_l(nzb+12,pr_palm,tn) + & |
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396 | qs(j,i) * rmask(j,i,sr) |
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397 | ENDIF |
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398 | ENDDO |
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399 | ENDDO |
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400 | |
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401 | ! |
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402 | !-- Horizontally averaged profiles of the vertical fluxes |
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403 | !$OMP DO |
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404 | DO i = nxl, nxr |
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405 | DO j = nys, nyn |
---|
406 | ! |
---|
407 | !-- Subgridscale fluxes (without Prandtl layer from k=nzb, |
---|
408 | !-- oterwise from k=nzb+1) |
---|
409 | !-- NOTE: for simplicity, nzb_diff_s_inner is used below, although |
---|
410 | !-- ---- strictly speaking the following k-loop would have to be |
---|
411 | !-- split up according to the staggered grid. |
---|
412 | !-- However, this implies no error since staggered velocity |
---|
413 | !-- components are zero at the walls and inside buildings. |
---|
414 | |
---|
415 | DO k = nzb_diff_s_inner(j,i)-1, nzt_diff |
---|
416 | ! |
---|
417 | !-- Momentum flux w"u" |
---|
418 | sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( & |
---|
419 | km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) & |
---|
420 | ) * ( & |
---|
421 | ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
---|
422 | + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
---|
423 | ) * rmask(j,i,sr) |
---|
424 | ! |
---|
425 | !-- Momentum flux w"v" |
---|
426 | sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( & |
---|
427 | km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) & |
---|
428 | ) * ( & |
---|
429 | ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
---|
430 | + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
---|
431 | ) * rmask(j,i,sr) |
---|
432 | ! |
---|
433 | !-- Heat flux w"pt" |
---|
434 | sums_l(k,16,tn) = sums_l(k,16,tn) & |
---|
435 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
436 | * ( pt(k+1,j,i) - pt(k,j,i) ) & |
---|
437 | * ddzu(k+1) * rmask(j,i,sr) |
---|
438 | |
---|
439 | |
---|
440 | ! |
---|
441 | !-- Salinity flux w"sa" |
---|
442 | IF ( ocean ) THEN |
---|
443 | sums_l(k,65,tn) = sums_l(k,65,tn) & |
---|
444 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
445 | * ( sa(k+1,j,i) - sa(k,j,i) ) & |
---|
446 | * ddzu(k+1) * rmask(j,i,sr) |
---|
447 | ENDIF |
---|
448 | |
---|
449 | ! |
---|
450 | !-- Buoyancy flux, water flux (humidity flux) w"q" |
---|
451 | IF ( humidity ) THEN |
---|
452 | sums_l(k,45,tn) = sums_l(k,45,tn) & |
---|
453 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
454 | * ( vpt(k+1,j,i) - vpt(k,j,i) ) & |
---|
455 | * ddzu(k+1) * rmask(j,i,sr) |
---|
456 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
457 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
458 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
459 | * ddzu(k+1) * rmask(j,i,sr) |
---|
460 | IF ( cloud_physics ) THEN |
---|
461 | sums_l(k,51,tn) = sums_l(k,51,tn) & |
---|
462 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
463 | * ( ( q(k+1,j,i) - ql(k+1,j,i) )& |
---|
464 | - ( q(k,j,i) - ql(k,j,i) ) ) & |
---|
465 | * ddzu(k+1) * rmask(j,i,sr) |
---|
466 | ENDIF |
---|
467 | ENDIF |
---|
468 | |
---|
469 | ! |
---|
470 | !-- Passive scalar flux |
---|
471 | IF ( passive_scalar ) THEN |
---|
472 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
473 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
474 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
475 | * ddzu(k+1) * rmask(j,i,sr) |
---|
476 | ENDIF |
---|
477 | |
---|
478 | ENDDO |
---|
479 | |
---|
480 | ! |
---|
481 | !-- Subgridscale fluxes in the Prandtl layer |
---|
482 | IF ( use_surface_fluxes ) THEN |
---|
483 | sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + & |
---|
484 | usws(j,i) * rmask(j,i,sr) ! w"u" |
---|
485 | sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + & |
---|
486 | vsws(j,i) * rmask(j,i,sr) ! w"v" |
---|
487 | sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + & |
---|
488 | shf(j,i) * rmask(j,i,sr) ! w"pt" |
---|
489 | sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + & |
---|
490 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
491 | sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + & |
---|
492 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
493 | IF ( ocean ) THEN |
---|
494 | sums_l(nzb,65,tn) = sums_l(nzb,65,tn) + & |
---|
495 | saswsb(j,i) * rmask(j,i,sr) ! w"sa" |
---|
496 | ENDIF |
---|
497 | IF ( humidity ) THEN |
---|
498 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
499 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
500 | IF ( cloud_physics ) THEN |
---|
501 | sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( & |
---|
502 | ( 1.0 + 0.61 * q(nzb,j,i) ) * & |
---|
503 | shf(j,i) + 0.61 * pt(nzb,j,i) * & |
---|
504 | qsws(j,i) & |
---|
505 | ) |
---|
506 | ! |
---|
507 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
508 | sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv") |
---|
509 | qsws(j,i) * rmask(j,i,sr) |
---|
510 | ENDIF |
---|
511 | ENDIF |
---|
512 | IF ( passive_scalar ) THEN |
---|
513 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
514 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
515 | ENDIF |
---|
516 | ENDIF |
---|
517 | |
---|
518 | ! |
---|
519 | !-- Subgridscale fluxes at the top surface |
---|
520 | IF ( use_top_fluxes ) THEN |
---|
521 | sums_l(nzt,12,tn) = sums_l(nzt,12,tn) + & |
---|
522 | uswst(j,i) * rmask(j,i,sr) ! w"u" |
---|
523 | sums_l(nzt,14,tn) = sums_l(nzt,14,tn) + & |
---|
524 | vswst(j,i) * rmask(j,i,sr) ! w"v" |
---|
525 | sums_l(nzt,16,tn) = sums_l(nzt,16,tn) + & |
---|
526 | tswst(j,i) * rmask(j,i,sr) ! w"pt" |
---|
527 | sums_l(nzt,58,tn) = sums_l(nzt,58,tn) + & |
---|
528 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
529 | sums_l(nzt,61,tn) = sums_l(nzt,61,tn) + & |
---|
530 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
531 | IF ( ocean ) THEN |
---|
532 | sums_l(nzt,65,tn) = sums_l(nzt,65,tn) + & |
---|
533 | saswst(j,i) * rmask(j,i,sr) ! w"sa" |
---|
534 | ENDIF |
---|
535 | IF ( humidity ) THEN |
---|
536 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
537 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
538 | IF ( cloud_physics ) THEN |
---|
539 | sums_l(nzt,45,tn) = sums_l(nzt,45,tn) + ( & |
---|
540 | ( 1.0 + 0.61 * q(nzt,j,i) ) * & |
---|
541 | tswst(j,i) + 0.61 * pt(nzt,j,i) * & |
---|
542 | qsws(j,i) & |
---|
543 | ) |
---|
544 | ! |
---|
545 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
546 | sums_l(nzt,51,tn) = sums_l(nzt,51,tn) + & ! w"q" (w"qv") |
---|
547 | qswst(j,i) * rmask(j,i,sr) |
---|
548 | ENDIF |
---|
549 | ENDIF |
---|
550 | IF ( passive_scalar ) THEN |
---|
551 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
552 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
553 | ENDIF |
---|
554 | ENDIF |
---|
555 | |
---|
556 | ! |
---|
557 | !-- Resolved fluxes (can be computed for all horizontal points) |
---|
558 | !-- NOTE: for simplicity, nzb_s_inner is used below, although strictly |
---|
559 | !-- ---- speaking the following k-loop would have to be split up and |
---|
560 | !-- rearranged according to the staggered grid. |
---|
561 | DO k = nzb_s_inner(j,i), nzt |
---|
562 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
563 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
564 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
565 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
566 | pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
567 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) |
---|
568 | ! |
---|
569 | !-- Momentum flux w*u* |
---|
570 | sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * & |
---|
571 | ( w(k,j,i-1) + w(k,j,i) ) & |
---|
572 | * ust * rmask(j,i,sr) |
---|
573 | ! |
---|
574 | !-- Momentum flux w*v* |
---|
575 | sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * & |
---|
576 | ( w(k,j-1,i) + w(k,j,i) ) & |
---|
577 | * vst * rmask(j,i,sr) |
---|
578 | ! |
---|
579 | !-- Heat flux w*pt* |
---|
580 | !-- The following formula (comment line, not executed) does not |
---|
581 | !-- work if applied to subregions |
---|
582 | ! sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * & |
---|
583 | ! ( pt(k,j,i)+pt(k+1,j,i) ) & |
---|
584 | ! * w(k,j,i) * rmask(j,i,sr) |
---|
585 | sums_l(k,17,tn) = sums_l(k,17,tn) + pts * w(k,j,i) * & |
---|
586 | rmask(j,i,sr) |
---|
587 | ! |
---|
588 | !-- Higher moments |
---|
589 | sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)**2 * & |
---|
590 | rmask(j,i,sr) |
---|
591 | sums_l(k,36,tn) = sums_l(k,36,tn) + pts**2 * w(k,j,i) * & |
---|
592 | rmask(j,i,sr) |
---|
593 | |
---|
594 | ! |
---|
595 | !-- Salinity flux and density (density does not belong to here, |
---|
596 | !-- but so far there is no other suitable place to calculate) |
---|
597 | IF ( ocean ) THEN |
---|
598 | pts = 0.5 * ( sa(k,j,i) - hom(k,1,23,sr) + & |
---|
599 | sa(k+1,j,i) - hom(k+1,1,23,sr) ) |
---|
600 | sums_l(k,66,tn) = sums_l(k,66,tn) + pts * w(k,j,i) * & |
---|
601 | rmask(j,i,sr) |
---|
602 | sums_l(k,64,tn) = sums_l(k,64,tn) + rho(k,j,i) * & |
---|
603 | rmask(j,i,sr) |
---|
604 | sums_l(k,71,tn) = sums_l(k,71,tn) + prho(k,j,i) * & |
---|
605 | rmask(j,i,sr) |
---|
606 | ENDIF |
---|
607 | |
---|
608 | ! |
---|
609 | !-- Buoyancy flux, water flux, humidity flux and liquid water |
---|
610 | !-- content |
---|
611 | IF ( humidity ) THEN |
---|
612 | pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + & |
---|
613 | vpt(k+1,j,i) - hom(k+1,1,44,sr) ) |
---|
614 | sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * & |
---|
615 | rmask(j,i,sr) |
---|
616 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
617 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
618 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
619 | rmask(j,i,sr) |
---|
620 | IF ( cloud_physics .OR. cloud_droplets ) THEN |
---|
621 | pts = 0.5 * & |
---|
622 | ( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) & |
---|
623 | + ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) ) |
---|
624 | sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * & |
---|
625 | rmask(j,i,sr) |
---|
626 | sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * & |
---|
627 | rmask(j,i,sr) |
---|
628 | ENDIF |
---|
629 | ENDIF |
---|
630 | |
---|
631 | ! |
---|
632 | !-- Passive scalar flux |
---|
633 | IF ( passive_scalar ) THEN |
---|
634 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
635 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
636 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
637 | rmask(j,i,sr) |
---|
638 | ENDIF |
---|
639 | |
---|
640 | ! |
---|
641 | !-- Energy flux w*e* |
---|
642 | sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * & |
---|
643 | ( ust**2 + vst**2 + w(k,j,i)**2 )& |
---|
644 | * rmask(j,i,sr) |
---|
645 | |
---|
646 | ENDDO |
---|
647 | ENDDO |
---|
648 | ENDDO |
---|
649 | |
---|
650 | ! |
---|
651 | !-- Density at top follows Neumann condition |
---|
652 | IF ( ocean ) THEN |
---|
653 | sums_l(nzt+1,64,tn) = sums_l(nzt,64,tn) |
---|
654 | sums_l(nzt+1,71,tn) = sums_l(nzt,71,tn) |
---|
655 | ENDIF |
---|
656 | |
---|
657 | ! |
---|
658 | !-- Divergence of vertical flux of resolved scale energy and pressure |
---|
659 | !-- fluctuations as well as flux of pressure fluctuation itself (68). |
---|
660 | !-- First calculate the products, then the divergence. |
---|
661 | !-- Calculation is time consuming. Do it only, if profiles shall be plotted. |
---|
662 | IF ( hom(nzb+1,2,55,0) /= 0.0 .OR. hom(nzb+1,2,68,0) /= 0.0 ) THEN |
---|
663 | |
---|
664 | sums_ll = 0.0 ! local array |
---|
665 | |
---|
666 | !$OMP DO |
---|
667 | DO i = nxl, nxr |
---|
668 | DO j = nys, nyn |
---|
669 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
670 | |
---|
671 | sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( & |
---|
672 | ( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) & |
---|
673 | - 2.0 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) & |
---|
674 | ) )**2 & |
---|
675 | + ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) & |
---|
676 | - 2.0 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) & |
---|
677 | ) )**2 & |
---|
678 | + w(k,j,i)**2 ) |
---|
679 | |
---|
680 | sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) & |
---|
681 | * ( p(k,j,i) + p(k+1,j,i) ) |
---|
682 | |
---|
683 | ENDDO |
---|
684 | ENDDO |
---|
685 | ENDDO |
---|
686 | sums_ll(0,1) = 0.0 ! because w is zero at the bottom |
---|
687 | sums_ll(nzt+1,1) = 0.0 |
---|
688 | sums_ll(0,2) = 0.0 |
---|
689 | sums_ll(nzt+1,2) = 0.0 |
---|
690 | |
---|
691 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
692 | sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k) |
---|
693 | sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k) |
---|
694 | sums_l(k,68,tn) = sums_ll(k,2) |
---|
695 | ENDDO |
---|
696 | sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn) |
---|
697 | sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn) |
---|
698 | sums_l(nzb,68,tn) = 0.0 ! because w* = 0 at nzb |
---|
699 | |
---|
700 | ENDIF |
---|
701 | |
---|
702 | ! |
---|
703 | !-- Divergence of vertical flux of SGS TKE and the flux itself (69) |
---|
704 | IF ( hom(nzb+1,2,57,0) /= 0.0 .OR. hom(nzb+1,2,69,0) /= 0.0 ) THEN |
---|
705 | |
---|
706 | !$OMP DO |
---|
707 | DO i = nxl, nxr |
---|
708 | DO j = nys, nyn |
---|
709 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
710 | |
---|
711 | sums_l(k,57,tn) = sums_l(k,57,tn) - 0.5 * ( & |
---|
712 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
713 | - (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) & |
---|
714 | ) * ddzw(k) |
---|
715 | |
---|
716 | sums_l(k,69,tn) = sums_l(k,69,tn) - 0.5 * ( & |
---|
717 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
718 | ) |
---|
719 | |
---|
720 | ENDDO |
---|
721 | ENDDO |
---|
722 | ENDDO |
---|
723 | sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn) |
---|
724 | sums_l(nzb,69,tn) = sums_l(nzb+1,69,tn) |
---|
725 | |
---|
726 | ENDIF |
---|
727 | |
---|
728 | ! |
---|
729 | !-- Horizontal heat fluxes (subgrid, resolved, total). |
---|
730 | !-- Do it only, if profiles shall be plotted. |
---|
731 | IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN |
---|
732 | |
---|
733 | !$OMP DO |
---|
734 | DO i = nxl, nxr |
---|
735 | DO j = nys, nyn |
---|
736 | DO k = nzb_s_inner(j,i)+1, nzt |
---|
737 | ! |
---|
738 | !-- Subgrid horizontal heat fluxes u"pt", v"pt" |
---|
739 | sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * & |
---|
740 | ( kh(k,j,i) + kh(k,j,i-1) ) & |
---|
741 | * ( pt(k,j,i-1) - pt(k,j,i) ) & |
---|
742 | * ddx * rmask(j,i,sr) |
---|
743 | sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * & |
---|
744 | ( kh(k,j,i) + kh(k,j-1,i) ) & |
---|
745 | * ( pt(k,j-1,i) - pt(k,j,i) ) & |
---|
746 | * ddy * rmask(j,i,sr) |
---|
747 | ! |
---|
748 | !-- Resolved horizontal heat fluxes u*pt*, v*pt* |
---|
749 | sums_l(k,59,tn) = sums_l(k,59,tn) + & |
---|
750 | ( u(k,j,i) - hom(k,1,1,sr) ) & |
---|
751 | * 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + & |
---|
752 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
753 | pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
754 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
755 | sums_l(k,62,tn) = sums_l(k,62,tn) + & |
---|
756 | ( v(k,j,i) - hom(k,1,2,sr) ) & |
---|
757 | * 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
758 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
759 | ENDDO |
---|
760 | ENDDO |
---|
761 | ENDDO |
---|
762 | ! |
---|
763 | !-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer) |
---|
764 | sums_l(nzb,58,tn) = 0.0 |
---|
765 | sums_l(nzb,59,tn) = 0.0 |
---|
766 | sums_l(nzb,60,tn) = 0.0 |
---|
767 | sums_l(nzb,61,tn) = 0.0 |
---|
768 | sums_l(nzb,62,tn) = 0.0 |
---|
769 | sums_l(nzb,63,tn) = 0.0 |
---|
770 | |
---|
771 | ENDIF |
---|
772 | |
---|
773 | ! |
---|
774 | !-- Calculate the user-defined profiles |
---|
775 | CALL user_statistics( 'profiles', sr, tn ) |
---|
776 | !$OMP END PARALLEL |
---|
777 | |
---|
778 | ! |
---|
779 | !-- Summation of thread sums |
---|
780 | IF ( threads_per_task > 1 ) THEN |
---|
781 | DO i = 1, threads_per_task-1 |
---|
782 | sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i) |
---|
783 | sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i) |
---|
784 | sums_l(:,45:pr_palm,0) = sums_l(:,45:pr_palm,0) + & |
---|
785 | sums_l(:,45:pr_palm,i) |
---|
786 | IF ( max_pr_user > 0 ) THEN |
---|
787 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) = & |
---|
788 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) + & |
---|
789 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,i) |
---|
790 | ENDIF |
---|
791 | ENDDO |
---|
792 | ENDIF |
---|
793 | |
---|
794 | #if defined( __parallel ) |
---|
795 | ! |
---|
796 | !-- Compute total sum from local sums |
---|
797 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, & |
---|
798 | MPI_SUM, comm2d, ierr ) |
---|
799 | #else |
---|
800 | sums = sums_l(:,:,0) |
---|
801 | #endif |
---|
802 | |
---|
803 | ! |
---|
804 | !-- Final values are obtained by division by the total number of grid points |
---|
805 | !-- used for summation. After that store profiles. |
---|
806 | !-- Profiles: |
---|
807 | DO k = nzb, nzt+1 |
---|
808 | sums(k,3) = sums(k,3) / ngp_2dh(sr) |
---|
809 | sums(k,8:11) = sums(k,8:11) / ngp_2dh_s_inner(k,sr) |
---|
810 | sums(k,12:22) = sums(k,12:22) / ngp_2dh(sr) |
---|
811 | sums(k,23:29) = sums(k,23:29) / ngp_2dh_s_inner(k,sr) |
---|
812 | sums(k,30:32) = sums(k,30:32) / ngp_2dh(sr) |
---|
813 | sums(k,33:34) = sums(k,33:34) / ngp_2dh_s_inner(k,sr) |
---|
814 | sums(k,35:39) = sums(k,35:39) / ngp_2dh(sr) |
---|
815 | sums(k,40) = sums(k,40) / ngp_2dh_s_inner(k,sr) |
---|
816 | sums(k,45:53) = sums(k,45:53) / ngp_2dh(sr) |
---|
817 | sums(k,54) = sums(k,54) / ngp_2dh_s_inner(k,sr) |
---|
818 | sums(k,55:63) = sums(k,55:63) / ngp_2dh(sr) |
---|
819 | sums(k,64) = sums(k,64) / ngp_2dh_s_inner(k,sr) |
---|
820 | sums(k,65:69) = sums(k,65:69) / ngp_2dh(sr) |
---|
821 | sums(k,70:pr_palm-2) = sums(k,70:pr_palm-2)/ ngp_2dh_s_inner(k,sr) |
---|
822 | ENDDO |
---|
823 | !-- Upstream-parts |
---|
824 | sums(nzb:nzb+11,pr_palm-1) = sums(nzb:nzb+11,pr_palm-1) / ngp_3d(sr) |
---|
825 | !-- u* and so on |
---|
826 | !-- As sums(nzb:nzb+3,pr_palm) are full 2D arrays (us, usws, vsws, ts) whose |
---|
827 | !-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer |
---|
828 | !-- above the topography, they are being divided by ngp_2dh(sr) |
---|
829 | sums(nzb:nzb+3,pr_palm) = sums(nzb:nzb+3,pr_palm) / & |
---|
830 | ngp_2dh(sr) |
---|
831 | sums(nzb+12,pr_palm) = sums(nzb+12,pr_palm) / & ! qs |
---|
832 | ngp_2dh(sr) |
---|
833 | !-- eges, e* |
---|
834 | sums(nzb+4:nzb+5,pr_palm) = sums(nzb+4:nzb+5,pr_palm) / & |
---|
835 | ngp_3d(sr) |
---|
836 | !-- Old and new divergence |
---|
837 | sums(nzb+9:nzb+10,pr_palm) = sums(nzb+9:nzb+10,pr_palm) / & |
---|
838 | ngp_3d_inner(sr) |
---|
839 | |
---|
840 | !-- User-defined profiles |
---|
841 | IF ( max_pr_user > 0 ) THEN |
---|
842 | DO k = nzb, nzt+1 |
---|
843 | sums(k,pr_palm+1:pr_palm+max_pr_user) = & |
---|
844 | sums(k,pr_palm+1:pr_palm+max_pr_user) / & |
---|
845 | ngp_2dh_s_inner(k,sr) |
---|
846 | ENDDO |
---|
847 | ENDIF |
---|
848 | |
---|
849 | ! |
---|
850 | !-- Collect horizontal average in hom. |
---|
851 | !-- Compute deduced averages (e.g. total heat flux) |
---|
852 | hom(:,1,3,sr) = sums(:,3) ! w |
---|
853 | hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles |
---|
854 | hom(:,1,9,sr) = sums(:,9) ! km |
---|
855 | hom(:,1,10,sr) = sums(:,10) ! kh |
---|
856 | hom(:,1,11,sr) = sums(:,11) ! l |
---|
857 | hom(:,1,12,sr) = sums(:,12) ! w"u" |
---|
858 | hom(:,1,13,sr) = sums(:,13) ! w*u* |
---|
859 | hom(:,1,14,sr) = sums(:,14) ! w"v" |
---|
860 | hom(:,1,15,sr) = sums(:,15) ! w*v* |
---|
861 | hom(:,1,16,sr) = sums(:,16) ! w"pt" |
---|
862 | hom(:,1,17,sr) = sums(:,17) ! w*pt* |
---|
863 | hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt |
---|
864 | hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu |
---|
865 | hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv |
---|
866 | hom(:,1,21,sr) = sums(:,21) ! w*pt*BC |
---|
867 | hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC |
---|
868 | ! profile 24 is initial profile (sa) |
---|
869 | ! profiles 25-29 left empty for initial |
---|
870 | ! profiles |
---|
871 | hom(:,1,30,sr) = sums(:,30) ! u*2 |
---|
872 | hom(:,1,31,sr) = sums(:,31) ! v*2 |
---|
873 | hom(:,1,32,sr) = sums(:,32) ! w*2 |
---|
874 | hom(:,1,33,sr) = sums(:,33) ! pt*2 |
---|
875 | hom(:,1,34,sr) = sums(:,34) ! e* |
---|
876 | hom(:,1,35,sr) = sums(:,35) ! w*2pt* |
---|
877 | hom(:,1,36,sr) = sums(:,36) ! w*pt*2 |
---|
878 | hom(:,1,37,sr) = sums(:,37) ! w*e* |
---|
879 | hom(:,1,38,sr) = sums(:,38) ! w*3 |
---|
880 | hom(:,1,39,sr) = sums(:,38) / ( sums(:,32) + 1E-20 )**1.5 ! Sw |
---|
881 | hom(:,1,40,sr) = sums(:,40) ! p |
---|
882 | hom(:,1,45,sr) = sums(:,45) ! w"q" |
---|
883 | hom(:,1,46,sr) = sums(:,46) ! w*vpt* |
---|
884 | hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt |
---|
885 | hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv") |
---|
886 | hom(:,1,49,sr) = sums(:,49) ! w*q* (w*qv*) |
---|
887 | hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv) |
---|
888 | hom(:,1,51,sr) = sums(:,51) ! w"qv" |
---|
889 | hom(:,1,52,sr) = sums(:,52) ! w*qv* |
---|
890 | hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv) |
---|
891 | hom(:,1,54,sr) = sums(:,54) ! ql |
---|
892 | hom(:,1,55,sr) = sums(:,55) ! w*u*u*/dz |
---|
893 | hom(:,1,56,sr) = sums(:,56) ! w*p*/dz |
---|
894 | hom(:,1,57,sr) = sums(:,57) ! ( w"e + w"p"/rho )/dz |
---|
895 | hom(:,1,58,sr) = sums(:,58) ! u"pt" |
---|
896 | hom(:,1,59,sr) = sums(:,59) ! u*pt* |
---|
897 | hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t |
---|
898 | hom(:,1,61,sr) = sums(:,61) ! v"pt" |
---|
899 | hom(:,1,62,sr) = sums(:,62) ! v*pt* |
---|
900 | hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t |
---|
901 | hom(:,1,64,sr) = sums(:,64) ! rho |
---|
902 | hom(:,1,65,sr) = sums(:,65) ! w"sa" |
---|
903 | hom(:,1,66,sr) = sums(:,66) ! w*sa* |
---|
904 | hom(:,1,67,sr) = sums(:,65) + sums(:,66) ! wsa |
---|
905 | hom(:,1,68,sr) = sums(:,68) ! w*p* |
---|
906 | hom(:,1,69,sr) = sums(:,69) ! w"e + w"p"/rho |
---|
907 | hom(:,1,70,sr) = sums(:,70) ! q*2 |
---|
908 | hom(:,1,71,sr) = sums(:,71) ! prho |
---|
909 | hom(:,1,72,sr) = hyp * 1E-4 ! hyp in kPa |
---|
910 | |
---|
911 | hom(:,1,pr_palm-1,sr) = sums(:,pr_palm-1) |
---|
912 | ! upstream-parts u_x, u_y, u_z, v_x, |
---|
913 | ! v_y, usw. (in last but one profile) |
---|
914 | hom(:,1,pr_palm,sr) = sums(:,pr_palm) |
---|
915 | ! u*, w'u', w'v', t* (in last profile) |
---|
916 | |
---|
917 | IF ( max_pr_user > 0 ) THEN ! user-defined profiles |
---|
918 | hom(:,1,pr_palm+1:pr_palm+max_pr_user,sr) = & |
---|
919 | sums(:,pr_palm+1:pr_palm+max_pr_user) |
---|
920 | ENDIF |
---|
921 | |
---|
922 | ! |
---|
923 | !-- Determine the boundary layer height using two different schemes. |
---|
924 | !-- First scheme: Starting from the Earth's (Ocean's) surface, look for the |
---|
925 | !-- first relative minimum (maximum) of the total heat flux. |
---|
926 | !-- The corresponding height is assumed as the boundary layer height, if it |
---|
927 | !-- is less than 1.5 times the height where the heat flux becomes negative |
---|
928 | !-- (positive) for the first time. |
---|
929 | z_i(1) = 0.0 |
---|
930 | first = .TRUE. |
---|
931 | IF ( ocean ) THEN |
---|
932 | DO k = nzt, nzb+1, -1 |
---|
933 | IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN |
---|
934 | first = .FALSE. |
---|
935 | height = zw(k) |
---|
936 | ENDIF |
---|
937 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
938 | hom(k-1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
939 | IF ( zw(k) < 1.5 * height ) THEN |
---|
940 | z_i(1) = zw(k) |
---|
941 | ELSE |
---|
942 | z_i(1) = height |
---|
943 | ENDIF |
---|
944 | EXIT |
---|
945 | ENDIF |
---|
946 | ENDDO |
---|
947 | ELSE |
---|
948 | DO k = nzb, nzt-1 |
---|
949 | IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN |
---|
950 | first = .FALSE. |
---|
951 | height = zw(k) |
---|
952 | ENDIF |
---|
953 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
954 | hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
955 | IF ( zw(k) < 1.5 * height ) THEN |
---|
956 | z_i(1) = zw(k) |
---|
957 | ELSE |
---|
958 | z_i(1) = height |
---|
959 | ENDIF |
---|
960 | EXIT |
---|
961 | ENDIF |
---|
962 | ENDDO |
---|
963 | ENDIF |
---|
964 | |
---|
965 | ! |
---|
966 | !-- Second scheme: Gradient scheme from Sullivan et al. (1998), modified |
---|
967 | !-- by Uhlenbrock(2006). The boundary layer height is the height with the |
---|
968 | !-- maximal local temperature gradient: starting from the second (the last |
---|
969 | !-- but one) vertical gridpoint, the local gradient must be at least |
---|
970 | !-- 0.2K/100m and greater than the next four gradients. |
---|
971 | !-- WARNING: The threshold value of 0.2K/100m must be adjusted for the |
---|
972 | !-- ocean case! |
---|
973 | z_i(2) = 0.0 |
---|
974 | DO k = nzb+1, nzt+1 |
---|
975 | dptdz(k) = ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) * ddzu(k) |
---|
976 | ENDDO |
---|
977 | dptdz_threshold = 0.2 / 100.0 |
---|
978 | |
---|
979 | IF ( ocean ) THEN |
---|
980 | DO k = nzt+1, nzb+5, -1 |
---|
981 | IF ( dptdz(k) > dptdz_threshold .AND. & |
---|
982 | dptdz(k) > dptdz(k-1) .AND. dptdz(k) > dptdz(k-2) .AND. & |
---|
983 | dptdz(k) > dptdz(k-3) .AND. dptdz(k) > dptdz(k-4) ) THEN |
---|
984 | z_i(2) = zw(k-1) |
---|
985 | EXIT |
---|
986 | ENDIF |
---|
987 | ENDDO |
---|
988 | ELSE |
---|
989 | DO k = nzb+1, nzt-3 |
---|
990 | IF ( dptdz(k) > dptdz_threshold .AND. & |
---|
991 | dptdz(k) > dptdz(k+1) .AND. dptdz(k) > dptdz(k+2) .AND. & |
---|
992 | dptdz(k) > dptdz(k+3) .AND. dptdz(k) > dptdz(k+4) ) THEN |
---|
993 | z_i(2) = zw(k-1) |
---|
994 | EXIT |
---|
995 | ENDIF |
---|
996 | ENDDO |
---|
997 | ENDIF |
---|
998 | |
---|
999 | hom(nzb+6,1,pr_palm,sr) = z_i(1) |
---|
1000 | hom(nzb+7,1,pr_palm,sr) = z_i(2) |
---|
1001 | |
---|
1002 | ! |
---|
1003 | !-- Computation of both the characteristic vertical velocity and |
---|
1004 | !-- the characteristic convective boundary layer temperature. |
---|
1005 | !-- The horizontal average at nzb+1 is input for the average temperature. |
---|
1006 | IF ( hom(nzb,1,18,sr) > 0.0 .AND. z_i(1) /= 0.0 ) THEN |
---|
1007 | hom(nzb+8,1,pr_palm,sr) = ( g / hom(nzb+1,1,4,sr) * & |
---|
1008 | hom(nzb,1,18,sr) * & |
---|
1009 | ABS( z_i(1) ) )**0.333333333 |
---|
1010 | !-- so far this only works if Prandtl layer is used |
---|
1011 | hom(nzb+11,1,pr_palm,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,pr_palm,sr) |
---|
1012 | ELSE |
---|
1013 | hom(nzb+8,1,pr_palm,sr) = 0.0 |
---|
1014 | hom(nzb+11,1,pr_palm,sr) = 0.0 |
---|
1015 | ENDIF |
---|
1016 | |
---|
1017 | ! |
---|
1018 | !-- Collect the time series quantities |
---|
1019 | ts_value(1,sr) = hom(nzb+4,1,pr_palm,sr) ! E |
---|
1020 | ts_value(2,sr) = hom(nzb+5,1,pr_palm,sr) ! E* |
---|
1021 | ts_value(3,sr) = dt_3d |
---|
1022 | ts_value(4,sr) = hom(nzb,1,pr_palm,sr) ! u* |
---|
1023 | ts_value(5,sr) = hom(nzb+3,1,pr_palm,sr) ! th* |
---|
1024 | ts_value(6,sr) = u_max |
---|
1025 | ts_value(7,sr) = v_max |
---|
1026 | ts_value(8,sr) = w_max |
---|
1027 | ts_value(9,sr) = hom(nzb+10,1,pr_palm,sr) ! new divergence |
---|
1028 | ts_value(10,sr) = hom(nzb+9,1,pr_palm,sr) ! old Divergence |
---|
1029 | ts_value(11,sr) = hom(nzb+6,1,pr_palm,sr) ! z_i(1) |
---|
1030 | ts_value(12,sr) = hom(nzb+7,1,pr_palm,sr) ! z_i(2) |
---|
1031 | ts_value(13,sr) = hom(nzb+8,1,pr_palm,sr) ! w* |
---|
1032 | ts_value(14,sr) = hom(nzb,1,16,sr) ! w'pt' at k=0 |
---|
1033 | ts_value(15,sr) = hom(nzb+1,1,16,sr) ! w'pt' at k=1 |
---|
1034 | ts_value(16,sr) = hom(nzb+1,1,18,sr) ! wpt at k=1 |
---|
1035 | ts_value(17,sr) = hom(nzb,1,4,sr) ! pt(0) |
---|
1036 | ts_value(18,sr) = hom(nzb+1,1,4,sr) ! pt(zp) |
---|
1037 | ts_value(19,sr) = hom(nzb+1,1,pr_palm,sr) ! u'w' at k=0 |
---|
1038 | ts_value(20,sr) = hom(nzb+2,1,pr_palm,sr) ! v'w' at k=0 |
---|
1039 | ts_value(21,sr) = hom(nzb,1,48,sr) ! w"q" at k=0 |
---|
1040 | |
---|
1041 | IF ( ts_value(5,sr) /= 0.0 ) THEN |
---|
1042 | ts_value(22,sr) = ts_value(4,sr)**2 / & |
---|
1043 | ( kappa * g * ts_value(5,sr) / ts_value(18,sr) ) ! L |
---|
1044 | ELSE |
---|
1045 | ts_value(22,sr) = 10000.0 |
---|
1046 | ENDIF |
---|
1047 | |
---|
1048 | ts_value(23,sr) = hom(nzb+12,1,pr_palm,sr) ! q* |
---|
1049 | ! |
---|
1050 | !-- Calculate additional statistics provided by the user interface |
---|
1051 | CALL user_statistics( 'time_series', sr, 0 ) |
---|
1052 | |
---|
1053 | ENDDO ! loop of the subregions |
---|
1054 | |
---|
1055 | ! |
---|
1056 | !-- If required, sum up horizontal averages for subsequent time averaging |
---|
1057 | IF ( do_sum ) THEN |
---|
1058 | IF ( average_count_pr == 0 ) hom_sum = 0.0 |
---|
1059 | hom_sum = hom_sum + hom(:,1,:,:) |
---|
1060 | average_count_pr = average_count_pr + 1 |
---|
1061 | do_sum = .FALSE. |
---|
1062 | ENDIF |
---|
1063 | |
---|
1064 | ! |
---|
1065 | !-- Set flag for other UPs (e.g. output routines, but also buoyancy). |
---|
1066 | !-- This flag is reset after each time step in time_integration. |
---|
1067 | flow_statistics_called = .TRUE. |
---|
1068 | |
---|
1069 | CALL cpu_log( log_point(10), 'flow_statistics', 'stop' ) |
---|
1070 | |
---|
1071 | |
---|
1072 | END SUBROUTINE flow_statistics |
---|
1073 | |
---|
1074 | |
---|
1075 | |
---|