[1] | 1 | SUBROUTINE flow_statistics |
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| 2 | |
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| 3 | !------------------------------------------------------------------------------! |
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| 4 | ! Actual 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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[3] | 10 | ! $Id: flow_statistics.f90 4 2007-02-13 11:33:16Z raasch $ |
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| 11 | ! RCS Log replace by Id keyword, revision history cleaned up |
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| 12 | ! |
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[1] | 13 | ! Revision 1.41 2006/08/04 14:37:50 raasch |
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| 14 | ! Error removed in non-parallel part (sums_l) |
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| 15 | ! |
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| 16 | ! Revision 1.1 1997/08/11 06:15:17 raasch |
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| 17 | ! Initial revision |
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| 18 | ! |
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| 19 | ! |
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| 20 | ! Description: |
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| 21 | ! ------------ |
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| 22 | ! Compute average profiles and further average flow quantities for the different |
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| 23 | ! user-defined (sub-)regions. The region indexed 0 is the total model domain. |
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| 24 | ! |
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| 25 | ! NOTE: For simplicity, nzb_s_outer and nzb_diff_s_outer are being used as a |
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| 26 | ! ---- lower vertical index for k-loops for all variables so that regardless |
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| 27 | ! of the variable and its respective staggered grid always the same number of |
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| 28 | ! grid points is used for 2D averages. The disadvantage: depending on the |
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| 29 | ! variable, up to one grid layer adjacent to the (vertical walls of the) |
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| 30 | ! topography is missed out by this simplification. |
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| 31 | !------------------------------------------------------------------------------! |
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| 32 | |
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| 33 | USE arrays_3d |
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| 34 | USE cloud_parameters |
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| 35 | USE cpulog |
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| 36 | USE grid_variables |
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| 37 | USE indices |
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| 38 | USE interfaces |
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| 39 | USE pegrid |
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| 40 | USE statistics |
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| 41 | USE control_parameters |
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| 42 | |
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| 43 | IMPLICIT NONE |
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| 44 | |
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| 45 | INTEGER :: i, j, k, omp_get_thread_num, sr, tn |
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| 46 | LOGICAL :: first |
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| 47 | REAL :: height, pts, sums_l_eper, sums_l_etot, ust, ust2, u2, vst, & |
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| 48 | vst2, v2, w2, z_i(2) |
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| 49 | REAL :: sums_ll(nzb:nzt+1,2) |
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| 50 | |
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| 51 | |
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| 52 | CALL cpu_log( log_point(10), 'flow_statistics', 'start' ) |
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| 53 | |
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| 54 | ! |
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| 55 | !-- To be on the safe side, check whether flow_statistics has already been |
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| 56 | !-- called once after the current time step |
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| 57 | IF ( flow_statistics_called ) THEN |
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| 58 | IF ( myid == 0 ) PRINT*, '+++ WARNING: flow_statistics is called two', & |
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| 59 | ' times within one timestep' |
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| 60 | CALL local_stop |
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| 61 | ENDIF |
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| 62 | |
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| 63 | ! |
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| 64 | !-- Compute statistics for each (sub-)region |
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| 65 | DO sr = 0, statistic_regions |
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| 66 | |
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| 67 | ! |
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| 68 | !-- Initialize (local) summation array |
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| 69 | sums_l = 0.0 |
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| 70 | |
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| 71 | ! |
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| 72 | !-- Store sums that have been computed in other subroutines in summation |
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| 73 | !-- array |
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| 74 | sums_l(:,11,:) = sums_l_l(:,sr,:) ! mixing length from diffusivities |
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| 75 | !-- WARNING: next line still has to be adjusted for OpenMP |
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| 76 | sums_l(:,21,0) = sums_wsts_bc_l(:,sr) ! heat flux from advec_s_bc |
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| 77 | sums_l(nzb+9,var_sum,0) = sums_divold_l(sr) ! old divergence from pres |
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| 78 | sums_l(nzb+10,var_sum,0) = sums_divnew_l(sr) ! new divergence from pres |
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| 79 | !-- WARNING: next four lines still may have to be adjusted for OpenMP |
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| 80 | sums_l(nzb:nzb+2,var_sum-1,0) = sums_up_fraction_l(1,1:3,sr)! upstream |
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| 81 | sums_l(nzb+3:nzb+5,var_sum-1,0) = sums_up_fraction_l(2,1:3,sr)! parts |
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| 82 | sums_l(nzb+6:nzb+8,var_sum-1,0) = sums_up_fraction_l(3,1:3,sr)! from |
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| 83 | sums_l(nzb+9:nzb+11,var_sum-1,0) = sums_up_fraction_l(4,1:3,sr)! spline |
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| 84 | |
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| 85 | ! |
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| 86 | !-- Horizontally averaged profiles of horizontal velocities and temperature. |
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| 87 | !-- They must have been computed before, because they are already required |
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| 88 | !-- for other horizontal averages. |
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| 89 | tn = 0 |
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| 90 | !$OMP PARALLEL PRIVATE( i, j, k, tn ) |
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| 91 | #if defined( __lcmuk ) |
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| 92 | tn = omp_get_thread_num() |
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| 93 | #else |
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| 94 | !$ tn = omp_get_thread_num() |
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| 95 | #endif |
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| 96 | |
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| 97 | !$OMP DO |
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| 98 | DO i = nxl, nxr |
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| 99 | DO j = nys, nyn |
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| 100 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 101 | sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr) |
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| 102 | sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr) |
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| 103 | sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr) |
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| 104 | ENDDO |
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| 105 | ENDDO |
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| 106 | ENDDO |
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| 107 | |
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| 108 | ! |
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| 109 | !-- Horizontally averaged profiles of virtual potential temperature, |
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| 110 | !-- total water content, specific humidity and liquid water potential |
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| 111 | !-- temperature |
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| 112 | IF ( moisture ) THEN |
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| 113 | !$OMP DO |
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| 114 | DO i = nxl, nxr |
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| 115 | DO j = nys, nyn |
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| 116 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 117 | sums_l(k,44,tn) = sums_l(k,44,tn) + & |
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| 118 | vpt(k,j,i) * rmask(j,i,sr) |
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| 119 | sums_l(k,41,tn) = sums_l(k,41,tn) + & |
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| 120 | q(k,j,i) * rmask(j,i,sr) |
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| 121 | ENDDO |
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| 122 | ENDDO |
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| 123 | ENDDO |
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| 124 | IF ( cloud_physics ) THEN |
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| 125 | !$OMP DO |
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| 126 | DO i = nxl, nxr |
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| 127 | DO j = nys, nyn |
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| 128 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 129 | sums_l(k,42,tn) = sums_l(k,42,tn) + & |
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| 130 | ( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr) |
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| 131 | sums_l(k,43,tn) = sums_l(k,43,tn) + ( & |
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| 132 | pt(k,j,i) + l_d_cp*pt_d_t(k) * ql(k,j,i) & |
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| 133 | ) * rmask(j,i,sr) |
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| 134 | ENDDO |
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| 135 | ENDDO |
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| 136 | ENDDO |
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| 137 | ENDIF |
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| 138 | ENDIF |
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| 139 | |
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| 140 | ! |
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| 141 | !-- Horizontally averaged profiles of passive scalar |
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| 142 | IF ( passive_scalar ) THEN |
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| 143 | !$OMP DO |
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| 144 | DO i = nxl, nxr |
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| 145 | DO j = nys, nyn |
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| 146 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 147 | sums_l(k,41,tn) = sums_l(k,41,tn) + q(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 | ENDIF |
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| 152 | !$OMP END PARALLEL |
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| 153 | |
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| 154 | ! |
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| 155 | !-- Summation of thread sums |
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| 156 | IF ( threads_per_task > 1 ) THEN |
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| 157 | DO i = 1, threads_per_task-1 |
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| 158 | sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i) |
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| 159 | sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i) |
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| 160 | sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i) |
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| 161 | IF ( moisture ) THEN |
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| 162 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 163 | sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i) |
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| 164 | IF ( cloud_physics ) THEN |
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| 165 | sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i) |
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| 166 | sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i) |
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| 167 | ENDIF |
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| 168 | ENDIF |
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| 169 | IF ( passive_scalar ) THEN |
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| 170 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 171 | ENDIF |
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| 172 | ENDDO |
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| 173 | ENDIF |
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| 174 | |
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| 175 | #if defined( __parallel ) |
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| 176 | ! |
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| 177 | !-- Compute total sum from local sums |
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| 178 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), nzt+2-nzb, MPI_REAL, & |
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| 179 | MPI_SUM, comm2d, ierr ) |
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| 180 | CALL MPI_ALLREDUCE( sums_l(nzb,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, & |
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| 181 | MPI_SUM, comm2d, ierr ) |
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| 182 | CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, & |
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| 183 | MPI_SUM, comm2d, ierr ) |
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| 184 | IF ( moisture ) THEN |
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| 185 | CALL MPI_ALLREDUCE( sums_l(nzb,44,0), sums(nzb,44), nzt+2-nzb, & |
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| 186 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 187 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 188 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 189 | IF ( cloud_physics ) THEN |
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| 190 | CALL MPI_ALLREDUCE( sums_l(nzb,42,0), sums(nzb,42), nzt+2-nzb, & |
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| 191 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 192 | CALL MPI_ALLREDUCE( sums_l(nzb,43,0), sums(nzb,43), nzt+2-nzb, & |
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| 193 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 194 | ENDIF |
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| 195 | ENDIF |
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| 196 | |
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| 197 | IF ( passive_scalar ) THEN |
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| 198 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 199 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 200 | ENDIF |
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| 201 | #else |
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| 202 | sums(:,1) = sums_l(:,1,0) |
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| 203 | sums(:,2) = sums_l(:,2,0) |
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| 204 | sums(:,4) = sums_l(:,4,0) |
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| 205 | IF ( moisture ) THEN |
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| 206 | sums(:,44) = sums_l(:,44,0) |
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| 207 | sums(:,41) = sums_l(:,41,0) |
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| 208 | IF ( cloud_physics ) THEN |
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| 209 | sums(:,42) = sums_l(:,42,0) |
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| 210 | sums(:,43) = sums_l(:,43,0) |
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| 211 | ENDIF |
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| 212 | ENDIF |
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| 213 | IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0) |
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| 214 | #endif |
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| 215 | |
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| 216 | ! |
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| 217 | !-- Final values are obtained by division by the total number of grid points |
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| 218 | !-- used for summation. After that store profiles. |
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| 219 | sums(:,1) = sums(:,1) / ngp_2dh_outer(:,sr) |
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| 220 | sums(:,2) = sums(:,2) / ngp_2dh_outer(:,sr) |
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| 221 | sums(:,4) = sums(:,4) / ngp_2dh_outer(:,sr) |
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| 222 | hom(:,1,1,sr) = sums(:,1) ! u |
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| 223 | hom(:,1,2,sr) = sums(:,2) ! v |
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| 224 | hom(:,1,4,sr) = sums(:,4) ! pt |
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| 225 | |
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| 226 | ! |
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| 227 | !-- Humidity and cloud parameters |
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| 228 | IF ( moisture ) THEN |
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| 229 | sums(:,44) = sums(:,44) / ngp_2dh_outer(:,sr) |
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| 230 | sums(:,41) = sums(:,41) / ngp_2dh_outer(:,sr) |
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| 231 | hom(:,1,44,sr) = sums(:,44) ! vpt |
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| 232 | hom(:,1,41,sr) = sums(:,41) ! qv (q) |
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| 233 | IF ( cloud_physics ) THEN |
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| 234 | sums(:,42) = sums(:,42) / ngp_2dh_outer(:,sr) |
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| 235 | sums(:,43) = sums(:,43) / ngp_2dh_outer(:,sr) |
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| 236 | hom(:,1,42,sr) = sums(:,42) ! qv |
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| 237 | hom(:,1,43,sr) = sums(:,43) ! pt |
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| 238 | ENDIF |
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| 239 | ENDIF |
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| 240 | |
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| 241 | ! |
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| 242 | !-- Passive scalar |
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| 243 | IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / ngp_2dh_outer(:,sr) |
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| 244 | |
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| 245 | ! |
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| 246 | !-- Horizontally averaged profiles of the remaining prognostic variables, |
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| 247 | !-- variances, the total and the perturbation energy (single values in last |
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| 248 | !-- column of sums_l) and some diagnostic quantities. |
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| 249 | !-- NOTE: for simplicity, nzb_s_outer is used below, although strictly |
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| 250 | !-- ---- speaking the following k-loop would have to be split up and |
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| 251 | !-- rearranged according to the staggered grid. |
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| 252 | tn = 0 |
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| 253 | #if defined( __lcmuk ) |
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| 254 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, & |
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| 255 | !$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
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| 256 | tn = omp_get_thread_num() |
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| 257 | #else |
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| 258 | !$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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| 259 | !$ tn = omp_get_thread_num() |
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| 260 | #endif |
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| 261 | !$OMP DO |
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| 262 | DO i = nxl, nxr |
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| 263 | DO j = nys, nyn |
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| 264 | sums_l_etot = 0.0 |
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| 265 | sums_l_eper = 0.0 |
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| 266 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 267 | u2 = u(k,j,i)**2 |
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| 268 | v2 = v(k,j,i)**2 |
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| 269 | w2 = w(k,j,i)**2 |
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| 270 | ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2 |
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| 271 | vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2 |
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| 272 | ! |
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| 273 | !-- Prognostic and diagnostic variables |
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| 274 | sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr) |
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| 275 | sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr) |
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| 276 | sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr) |
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| 277 | sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr) |
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| 278 | sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i) |
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| 279 | |
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| 280 | ! |
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| 281 | !-- Variances |
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| 282 | sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr) |
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| 283 | sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr) |
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| 284 | sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr) |
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| 285 | sums_l(k,33,tn) = sums_l(k,33,tn) + & |
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| 286 | ( pt(k,j,i)-hom(k,1,4,sr) )**2 * rmask(j,i,sr) |
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| 287 | ! |
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| 288 | !-- Higher moments |
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| 289 | !-- (Computation of the skewness of w further below) |
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| 290 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
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| 291 | rmask(j,i,sr) |
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| 292 | ! |
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| 293 | !-- Perturbation energy |
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| 294 | sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * ( ust2 + vst2 + w2 ) & |
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| 295 | * rmask(j,i,sr) |
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| 296 | sums_l_etot = sums_l_etot + & |
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| 297 | 0.5 * ( u2 + v2 + w2 ) * rmask(j,i,sr) |
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| 298 | sums_l_eper = sums_l_eper + & |
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| 299 | 0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr) |
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| 300 | ENDDO |
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| 301 | ! |
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| 302 | !-- Total and perturbation energy for the total domain (being |
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| 303 | !-- collected in the last column of sums_l). Summation of these |
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| 304 | !-- quantities is seperated from the previous loop in order to |
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| 305 | !-- allow vectorization of that loop. |
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| 306 | sums_l(nzb+4,var_sum,tn) = sums_l(nzb+4,var_sum,tn) + sums_l_etot |
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| 307 | sums_l(nzb+5,var_sum,tn) = sums_l(nzb+5,var_sum,tn) + sums_l_eper |
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| 308 | ! |
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| 309 | !-- 2D-arrays (being collected in the last column of sums_l) |
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| 310 | sums_l(nzb,var_sum,tn) = sums_l(nzb,var_sum,tn) + & |
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| 311 | us(j,i) * rmask(j,i,sr) |
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| 312 | sums_l(nzb+1,var_sum,tn) = sums_l(nzb+1,var_sum,tn) + & |
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| 313 | usws(j,i) * rmask(j,i,sr) |
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| 314 | sums_l(nzb+2,var_sum,tn) = sums_l(nzb+2,var_sum,tn) + & |
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| 315 | vsws(j,i) * rmask(j,i,sr) |
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| 316 | sums_l(nzb+3,var_sum,tn) = sums_l(nzb+3,var_sum,tn) + & |
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| 317 | ts(j,i) * rmask(j,i,sr) |
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| 318 | ENDDO |
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| 319 | ENDDO |
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| 320 | |
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| 321 | ! |
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| 322 | !-- Horizontally averaged profiles of the vertical fluxes |
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| 323 | !$OMP DO |
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| 324 | DO i = nxl, nxr |
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| 325 | DO j = nys, nyn |
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| 326 | ! |
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| 327 | !-- Subgridscale fluxes (without Prandtl layer from k=nzb, |
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| 328 | !-- oterwise from k=nzb+1) |
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| 329 | !-- NOTE: for simplicity, nzb_diff_s_outer is used below, although |
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| 330 | !-- ---- strictly speaking the following k-loop would have to be |
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| 331 | !-- split up according to the staggered grid. |
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| 332 | DO k = nzb_diff_s_outer(j,i)-1, nzt |
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| 333 | ! |
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| 334 | !-- Momentum flux w"u" |
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| 335 | sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( & |
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| 336 | km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) & |
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| 337 | ) * ( & |
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| 338 | ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
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| 339 | + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
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| 340 | ) * rmask(j,i,sr) |
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| 341 | ! |
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| 342 | !-- Momentum flux w"v" |
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| 343 | sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( & |
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| 344 | km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) & |
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| 345 | ) * ( & |
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| 346 | ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
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| 347 | + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
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| 348 | ) * rmask(j,i,sr) |
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| 349 | ! |
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| 350 | !-- Heat flux w"pt" |
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| 351 | sums_l(k,16,tn) = sums_l(k,16,tn) & |
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| 352 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
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| 353 | * ( pt(k+1,j,i) - pt(k,j,i) ) & |
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| 354 | * ddzu(k+1) * rmask(j,i,sr) |
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| 355 | |
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| 356 | |
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| 357 | ! |
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| 358 | !-- Buoyancy flux, water flux (humidity flux) w"q" |
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| 359 | IF ( moisture ) THEN |
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| 360 | sums_l(k,45,tn) = sums_l(k,45,tn) & |
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| 361 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
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| 362 | * ( vpt(k+1,j,i) - vpt(k,j,i) ) & |
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| 363 | * ddzu(k+1) * rmask(j,i,sr) |
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| 364 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
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| 365 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
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| 366 | * ( q(k+1,j,i) - q(k,j,i) ) & |
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| 367 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 368 | IF ( cloud_physics ) THEN |
---|
| 369 | sums_l(k,51,tn) = sums_l(k,51,tn) & |
---|
| 370 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 371 | * ( ( q(k+1,j,i) - ql(k+1,j,i) )& |
---|
| 372 | - ( q(k,j,i) - ql(k,j,i) ) ) & |
---|
| 373 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 374 | ENDIF |
---|
| 375 | ENDIF |
---|
| 376 | |
---|
| 377 | ! |
---|
| 378 | !-- Passive scalar flux |
---|
| 379 | IF ( passive_scalar ) THEN |
---|
| 380 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 381 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 382 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 383 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 384 | ENDIF |
---|
| 385 | |
---|
| 386 | ENDDO |
---|
| 387 | |
---|
| 388 | ! |
---|
| 389 | !-- Subgridscale fluxes in the Prandtl layer |
---|
| 390 | IF ( use_surface_fluxes ) THEN |
---|
| 391 | sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + & |
---|
| 392 | usws(j,i) * rmask(j,i,sr) ! w"u" |
---|
| 393 | sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + & |
---|
| 394 | vsws(j,i) * rmask(j,i,sr) ! w"v" |
---|
| 395 | sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + & |
---|
| 396 | shf(j,i) * rmask(j,i,sr) ! w"pt" |
---|
| 397 | sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + & |
---|
| 398 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
| 399 | sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + & |
---|
| 400 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
| 401 | IF ( moisture ) THEN |
---|
| 402 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 403 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 404 | IF ( cloud_physics ) THEN |
---|
| 405 | sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( & |
---|
| 406 | ( 1.0 + 0.61 * q(nzb,j,i) ) * & |
---|
| 407 | shf(j,i) + 0.61 * pt(nzb,j,i) * & |
---|
| 408 | qsws(j,i) & |
---|
| 409 | ) |
---|
| 410 | ! |
---|
| 411 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 412 | sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv") |
---|
| 413 | qsws(j,i) * rmask(j,i,sr) |
---|
| 414 | ENDIF |
---|
| 415 | ENDIF |
---|
| 416 | IF ( passive_scalar ) THEN |
---|
| 417 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 418 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 419 | ENDIF |
---|
| 420 | ENDIF |
---|
| 421 | |
---|
| 422 | ! |
---|
| 423 | !-- Resolved fluxes (can be computed for all horizontal points) |
---|
| 424 | !-- NOTE: for simplicity, nzb_s_outer is used below, although strictly |
---|
| 425 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 426 | !-- rearranged according to the staggered grid. |
---|
| 427 | DO k = nzb_s_outer(j,i), nzt |
---|
| 428 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 429 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 430 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 431 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 432 | pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 433 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) |
---|
| 434 | ! |
---|
| 435 | !-- Momentum flux w*u* |
---|
| 436 | sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * & |
---|
| 437 | ( w(k,j,i-1) + w(k,j,i) ) & |
---|
| 438 | * ust * rmask(j,i,sr) |
---|
| 439 | ! |
---|
| 440 | !-- Momentum flux w*v* |
---|
| 441 | sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * & |
---|
| 442 | ( w(k,j-1,i) + w(k,j,i) ) & |
---|
| 443 | * vst * rmask(j,i,sr) |
---|
| 444 | ! |
---|
| 445 | !-- Heat flux w*pt* |
---|
| 446 | !-- The following formula (comment line, not executed) does not |
---|
| 447 | !-- work if applied to subregions |
---|
| 448 | ! sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * & |
---|
| 449 | ! ( pt(k,j,i)+pt(k+1,j,i) ) & |
---|
| 450 | ! * w(k,j,i) * rmask(j,i,sr) |
---|
| 451 | sums_l(k,17,tn) = sums_l(k,17,tn) + pts * w(k,j,i) * & |
---|
| 452 | rmask(j,i,sr) |
---|
| 453 | ! |
---|
| 454 | !-- Higher moments |
---|
| 455 | sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)**2 * & |
---|
| 456 | rmask(j,i,sr) |
---|
| 457 | sums_l(k,36,tn) = sums_l(k,36,tn) + pts**2 * w(k,j,i) * & |
---|
| 458 | rmask(j,i,sr) |
---|
| 459 | |
---|
| 460 | ! |
---|
| 461 | !-- Buoyancy flux, water flux, humidity flux and liquid water |
---|
| 462 | !-- content |
---|
| 463 | IF ( moisture ) THEN |
---|
| 464 | pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + & |
---|
| 465 | vpt(k+1,j,i) - hom(k+1,1,44,sr) ) |
---|
| 466 | sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * & |
---|
| 467 | rmask(j,i,sr) |
---|
| 468 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 469 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 470 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 471 | rmask(j,i,sr) |
---|
| 472 | IF ( cloud_physics .OR. cloud_droplets ) THEN |
---|
| 473 | pts = 0.5 * & |
---|
| 474 | ( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) & |
---|
| 475 | + ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) ) |
---|
| 476 | sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * & |
---|
| 477 | rmask(j,i,sr) |
---|
| 478 | sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * & |
---|
| 479 | rmask(j,i,sr) |
---|
| 480 | ENDIF |
---|
| 481 | ENDIF |
---|
| 482 | |
---|
| 483 | ! |
---|
| 484 | !-- Passive scalar flux |
---|
| 485 | IF ( passive_scalar ) THEN |
---|
| 486 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 487 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 488 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 489 | rmask(j,i,sr) |
---|
| 490 | ENDIF |
---|
| 491 | |
---|
| 492 | ! |
---|
| 493 | !-- Energy flux w*e* |
---|
| 494 | sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * & |
---|
| 495 | ( ust**2 + vst**2 + w(k,j,i)**2 )& |
---|
| 496 | * rmask(j,i,sr) |
---|
| 497 | |
---|
| 498 | ENDDO |
---|
| 499 | ENDDO |
---|
| 500 | ENDDO |
---|
| 501 | |
---|
| 502 | ! |
---|
| 503 | !-- Divergence of vertical flux of resolved scale energy and pressure |
---|
| 504 | !-- fluctuations. First calculate the products, then the divergence. |
---|
| 505 | !-- Calculation is time consuming. Do it only, if profiles shall be plotted. |
---|
| 506 | IF ( hom(nzb+1,2,55,0) /= 0.0 ) THEN |
---|
| 507 | |
---|
| 508 | sums_ll = 0.0 ! local array |
---|
| 509 | |
---|
| 510 | !$OMP DO |
---|
| 511 | DO i = nxl, nxr |
---|
| 512 | DO j = nys, nyn |
---|
| 513 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 514 | |
---|
| 515 | sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( & |
---|
| 516 | ( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) & |
---|
| 517 | - 2.0 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) & |
---|
| 518 | ) )**2 & |
---|
| 519 | + ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) & |
---|
| 520 | - 2.0 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) & |
---|
| 521 | ) )**2 & |
---|
| 522 | + w(k,j,i)**2 ) |
---|
| 523 | |
---|
| 524 | sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) & |
---|
| 525 | * ( p(k,j,i) + p(k+1,j,i) ) |
---|
| 526 | |
---|
| 527 | ENDDO |
---|
| 528 | ENDDO |
---|
| 529 | ENDDO |
---|
| 530 | sums_ll(0,1) = 0.0 ! because w is zero at the bottom |
---|
| 531 | sums_ll(nzt+1,1) = 0.0 |
---|
| 532 | sums_ll(0,2) = 0.0 |
---|
| 533 | sums_ll(nzt+1,2) = 0.0 |
---|
| 534 | |
---|
| 535 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 536 | sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k) |
---|
| 537 | sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k) |
---|
| 538 | ENDDO |
---|
| 539 | sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn) |
---|
| 540 | sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn) |
---|
| 541 | |
---|
| 542 | ENDIF |
---|
| 543 | |
---|
| 544 | ! |
---|
| 545 | !-- Divergence of vertical flux of SGS TKE |
---|
| 546 | IF ( hom(nzb+1,2,57,0) /= 0.0 ) THEN |
---|
| 547 | |
---|
| 548 | !$OMP DO |
---|
| 549 | DO i = nxl, nxr |
---|
| 550 | DO j = nys, nyn |
---|
| 551 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 552 | |
---|
| 553 | sums_l(k,57,tn) = sums_l(k,57,tn) + ( & |
---|
| 554 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 555 | - (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) & |
---|
| 556 | ) * ddzw(k) |
---|
| 557 | |
---|
| 558 | ENDDO |
---|
| 559 | ENDDO |
---|
| 560 | ENDDO |
---|
| 561 | sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn) |
---|
| 562 | |
---|
| 563 | ENDIF |
---|
| 564 | |
---|
| 565 | ! |
---|
| 566 | !-- Horizontal heat fluxes (subgrid, resolved, total). |
---|
| 567 | !-- Do it only, if profiles shall be plotted. |
---|
| 568 | IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN |
---|
| 569 | |
---|
| 570 | !$OMP DO |
---|
| 571 | DO i = nxl, nxr |
---|
| 572 | DO j = nys, nyn |
---|
| 573 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 574 | ! |
---|
| 575 | !-- Subgrid horizontal heat fluxes u"pt", v"pt" |
---|
| 576 | sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * & |
---|
| 577 | ( kh(k,j,i) + kh(k,j,i-1) ) & |
---|
| 578 | * ( pt(k,j,i-1) - pt(k,j,i) ) & |
---|
| 579 | * ddx * rmask(j,i,sr) |
---|
| 580 | sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * & |
---|
| 581 | ( kh(k,j,i) + kh(k,j-1,i) ) & |
---|
| 582 | * ( pt(k,j-1,i) - pt(k,j,i) ) & |
---|
| 583 | * ddy * rmask(j,i,sr) |
---|
| 584 | ! |
---|
| 585 | !-- Resolved horizontal heat fluxes u*pt*, v*pt* |
---|
| 586 | sums_l(k,59,tn) = sums_l(k,59,tn) + & |
---|
| 587 | ( u(k,j,i) - hom(k,1,1,sr) ) & |
---|
| 588 | * 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + & |
---|
| 589 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 590 | pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 591 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 592 | sums_l(k,62,tn) = sums_l(k,62,tn) + & |
---|
| 593 | ( v(k,j,i) - hom(k,1,2,sr) ) & |
---|
| 594 | * 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 595 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 596 | ENDDO |
---|
| 597 | ENDDO |
---|
| 598 | ENDDO |
---|
| 599 | ! |
---|
| 600 | !-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer) |
---|
| 601 | sums(nzb,58) = 0.0 |
---|
| 602 | sums(nzb,59) = 0.0 |
---|
| 603 | sums(nzb,60) = 0.0 |
---|
| 604 | sums(nzb,61) = 0.0 |
---|
| 605 | sums(nzb,62) = 0.0 |
---|
| 606 | sums(nzb,63) = 0.0 |
---|
| 607 | |
---|
| 608 | ENDIF |
---|
| 609 | !$OMP END PARALLEL |
---|
| 610 | |
---|
| 611 | ! |
---|
| 612 | !-- Summation of thread sums |
---|
| 613 | IF ( threads_per_task > 1 ) THEN |
---|
| 614 | DO i = 1, threads_per_task-1 |
---|
| 615 | sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i) |
---|
| 616 | sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i) |
---|
| 617 | sums_l(:,45:var_sum,0) = sums_l(:,45:var_sum,0) + & |
---|
| 618 | sums_l(:,45:var_sum,i) |
---|
| 619 | ENDDO |
---|
| 620 | ENDIF |
---|
| 621 | |
---|
| 622 | #if defined( __parallel ) |
---|
| 623 | ! |
---|
| 624 | !-- Compute total sum from local sums |
---|
| 625 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, & |
---|
| 626 | MPI_SUM, comm2d, ierr ) |
---|
| 627 | #else |
---|
| 628 | sums = sums_l(:,:,0) |
---|
| 629 | #endif |
---|
| 630 | |
---|
| 631 | ! |
---|
| 632 | !-- Final values are obtained by division by the total number of grid points |
---|
| 633 | !-- used for summation. After that store profiles. |
---|
| 634 | !-- Profiles: |
---|
| 635 | DO k = nzb, nzt+1 |
---|
| 636 | sums(k,:var_sum-2) = sums(k,:var_sum-2) / ngp_2dh_outer(k,sr) |
---|
| 637 | ENDDO |
---|
| 638 | !-- Upstream-parts |
---|
| 639 | sums(nzb:nzb+11,var_sum-1) = sums(nzb:nzb+11,var_sum-1) / ngp_3d(sr) |
---|
| 640 | !-- u* and so on |
---|
| 641 | !-- As sums(nzb:nzb+3,var_sum) are full 2D arrays (us, usws, vsws, ts) whose |
---|
| 642 | !-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer |
---|
| 643 | !-- above the topography, they are being divided by ngp_2dh(sr) |
---|
| 644 | sums(nzb:nzb+3,var_sum) = sums(nzb:nzb+3,var_sum) / & |
---|
| 645 | ngp_2dh(sr) |
---|
| 646 | !-- eges, e* |
---|
| 647 | sums(nzb+4:nzb+5,var_sum) = sums(nzb+4:nzb+5,var_sum) / & |
---|
| 648 | ngp_3d_inner(sr) |
---|
| 649 | !-- Old and new divergence |
---|
| 650 | sums(nzb+9:nzb+10,var_sum) = sums(nzb+9:nzb+10,var_sum) / & |
---|
| 651 | ngp_3d_inner(sr) |
---|
| 652 | |
---|
| 653 | ! |
---|
| 654 | !-- Collect horizontal average in hom. |
---|
| 655 | !-- Compute deduced averages (e.g. total heat flux) |
---|
| 656 | hom(:,1,3,sr) = sums(:,3) ! w |
---|
| 657 | hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles |
---|
| 658 | hom(:,1,9,sr) = sums(:,9) ! km |
---|
| 659 | hom(:,1,10,sr) = sums(:,10) ! kh |
---|
| 660 | hom(:,1,11,sr) = sums(:,11) ! l |
---|
| 661 | hom(:,1,12,sr) = sums(:,12) ! w"u" |
---|
| 662 | hom(:,1,13,sr) = sums(:,13) ! w*u* |
---|
| 663 | hom(:,1,14,sr) = sums(:,14) ! w"v" |
---|
| 664 | hom(:,1,15,sr) = sums(:,15) ! w*v* |
---|
| 665 | hom(:,1,16,sr) = sums(:,16) ! w"pt" |
---|
| 666 | hom(:,1,17,sr) = sums(:,17) ! w*pt* |
---|
| 667 | hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt |
---|
| 668 | hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu |
---|
| 669 | hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv |
---|
| 670 | hom(:,1,21,sr) = sums(:,21) ! w*pt*BC |
---|
| 671 | hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC |
---|
| 672 | ! profiles 23-29 left empty for initial |
---|
| 673 | ! profiles |
---|
| 674 | hom(:,1,30,sr) = sums(:,30) ! u*2 |
---|
| 675 | hom(:,1,31,sr) = sums(:,31) ! v*2 |
---|
| 676 | hom(:,1,32,sr) = sums(:,32) ! w*2 |
---|
| 677 | hom(:,1,33,sr) = sums(:,33) ! pt*2 |
---|
| 678 | hom(:,1,34,sr) = sums(:,34) ! e* |
---|
| 679 | hom(:,1,35,sr) = sums(:,35) ! w*2pt* |
---|
| 680 | hom(:,1,36,sr) = sums(:,36) ! w*pt*2 |
---|
| 681 | hom(:,1,37,sr) = sums(:,37) ! w*e* |
---|
| 682 | hom(:,1,38,sr) = sums(:,38) ! w*3 |
---|
| 683 | hom(:,1,39,sr) = sums(:,38) / ( sums(:,32) + 1E-20 )**1.5 ! Sw |
---|
| 684 | hom(:,1,40,sr) = sums(:,40) ! p |
---|
| 685 | hom(:,1,45,sr) = sums(:,45) ! w"q" |
---|
| 686 | hom(:,1,46,sr) = sums(:,46) ! w*vpt* |
---|
| 687 | hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt |
---|
| 688 | hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv") |
---|
| 689 | hom(:,1,49,sr) = sums(:,49) ! w*q* (w*qv*) |
---|
| 690 | hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv) |
---|
| 691 | hom(:,1,51,sr) = sums(:,51) ! w"qv" |
---|
| 692 | hom(:,1,52,sr) = sums(:,52) ! w*qv* |
---|
| 693 | hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv) |
---|
| 694 | hom(:,1,54,sr) = sums(:,54) ! ql |
---|
| 695 | hom(:,1,55,sr) = sums(:,55) ! w*u*u*/dz |
---|
| 696 | hom(:,1,56,sr) = sums(:,56) ! w*p*/dz |
---|
| 697 | hom(:,1,57,sr) = sums(:,57) ! w"e/dz |
---|
| 698 | hom(:,1,58,sr) = sums(:,58) ! u"pt" |
---|
| 699 | hom(:,1,59,sr) = sums(:,59) ! u*pt* |
---|
| 700 | hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t |
---|
| 701 | hom(:,1,61,sr) = sums(:,61) ! v"pt" |
---|
| 702 | hom(:,1,62,sr) = sums(:,62) ! v*pt* |
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| 703 | hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t |
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| 704 | |
---|
| 705 | hom(:,1,var_hom-1,sr) = sums(:,var_sum-1) |
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| 706 | ! upstream-parts u_x, u_y, u_z, v_x, |
---|
| 707 | ! v_y, usw. (in last but one profile) |
---|
| 708 | hom(:,1,var_hom,sr) = sums(:,var_sum) |
---|
| 709 | ! u*, w'u', w'v', t* (in last profile) |
---|
| 710 | |
---|
| 711 | ! |
---|
| 712 | !-- Determine the boundary layer height using two different schemes. |
---|
| 713 | !-- First scheme: Starting from the Earth's surface, look for the first |
---|
| 714 | !-- relative minimum of the total heat flux. The corresponding height is |
---|
| 715 | !-- accepted as the boundary layer height, if it is less than 1.5 times the |
---|
| 716 | !-- height where the heat flux becomes negative for the first time. |
---|
| 717 | !-- NOTE: This criterion is still capable of improving! |
---|
| 718 | z_i(1) = 0.0 |
---|
| 719 | first = .TRUE. |
---|
| 720 | DO k = nzb, nzt-1 |
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| 721 | IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN |
---|
| 722 | first = .FALSE. |
---|
| 723 | height = zw(k) |
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| 724 | ENDIF |
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| 725 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
| 726 | hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN |
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| 727 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 728 | z_i(1) = zw(k) |
---|
| 729 | ELSE |
---|
| 730 | z_i(1) = height |
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| 731 | ENDIF |
---|
| 732 | EXIT |
---|
| 733 | ENDIF |
---|
| 734 | ENDDO |
---|
| 735 | |
---|
| 736 | ! |
---|
| 737 | !-- Second scheme: Starting from the top model boundary, look for the first |
---|
| 738 | !-- characteristic kink in the temperature profile, where the originally |
---|
| 739 | !-- stable stratification notably weakens. |
---|
| 740 | z_i(2) = 0.0 |
---|
| 741 | DO k = nzt-1, nzb+1, -1 |
---|
| 742 | IF ( ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) > & |
---|
| 743 | 2.0 * ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) ) THEN |
---|
| 744 | z_i(2) = zu(k) |
---|
| 745 | EXIT |
---|
| 746 | ENDIF |
---|
| 747 | ENDDO |
---|
| 748 | |
---|
| 749 | hom(nzb+6,1,var_hom,sr) = z_i(1) |
---|
| 750 | hom(nzb+7,1,var_hom,sr) = z_i(2) |
---|
| 751 | |
---|
| 752 | ! |
---|
| 753 | !-- Computation of both the characteristic vertical velocity and |
---|
| 754 | !-- the characteristic convective boundary layer temperature. |
---|
| 755 | !-- The horizontal average at nzb+1 is input for the average temperature. |
---|
| 756 | IF ( hom(nzb,1,18,sr) > 0.0 .AND. z_i(1) /= 0.0 ) THEN |
---|
| 757 | hom(nzb+8,1,var_hom,sr) = ( g / hom(nzb+1,1,4,sr) * & |
---|
| 758 | hom(nzb,1,18,sr) * z_i(1) )**0.333333333 |
---|
| 759 | !-- so far this only works if Prandtl layer is used |
---|
| 760 | hom(nzb+11,1,var_hom,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,var_hom,sr) |
---|
| 761 | ELSE |
---|
| 762 | hom(nzb+8,1,var_hom,sr) = 0.0 |
---|
| 763 | hom(nzb+11,1,var_hom,sr) = 0.0 |
---|
| 764 | ENDIF |
---|
| 765 | |
---|
| 766 | ENDDO ! loop of the subregions |
---|
| 767 | |
---|
| 768 | ! |
---|
| 769 | !-- Calculate additional statistics provided by the user interface |
---|
| 770 | CALL user_statistics |
---|
| 771 | |
---|
| 772 | ! |
---|
| 773 | !-- If required, sum up horizontal averages for subsequent time averaging |
---|
| 774 | IF ( do_sum ) THEN |
---|
| 775 | IF ( average_count_pr == 0 ) hom_sum = 0.0 |
---|
| 776 | hom_sum = hom_sum + hom(:,1,:,:) |
---|
| 777 | average_count_pr = average_count_pr + 1 |
---|
| 778 | do_sum = .FALSE. |
---|
| 779 | ENDIF |
---|
| 780 | |
---|
| 781 | ! |
---|
| 782 | !-- Set flag for other UPs (e.g. output routines, but also buoyancy). |
---|
| 783 | !-- This flag is reset after each time step in time_integration. |
---|
| 784 | flow_statistics_called = .TRUE. |
---|
| 785 | |
---|
| 786 | CALL cpu_log( log_point(10), 'flow_statistics', 'stop' ) |
---|
| 787 | |
---|
| 788 | |
---|
| 789 | END SUBROUTINE flow_statistics |
---|
| 790 | |
---|
| 791 | |
---|
| 792 | |
---|