[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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[96] | 6 | ! Statistics for ocean version (salinity, density) added, |
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| 7 | ! calculation of Deardorff velocity scale adjusted to be used with the ocean |
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[94] | 8 | ! version (HAS STILL TO BE COMPLETED!!!) |
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[1] | 9 | ! |
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| 10 | ! Former revisions: |
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| 11 | ! ----------------- |
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[3] | 12 | ! $Id: flow_statistics.f90 96 2007-06-04 08:07:41Z raasch $ |
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[39] | 13 | ! |
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[90] | 14 | ! 87 2007-05-22 15:46:47Z raasch |
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| 15 | ! Two more arguments added to user_statistics, which is now also called for |
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| 16 | ! user-defined profiles, |
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| 17 | ! var_hom and var_sum renamed pr_palm |
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| 18 | ! |
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[83] | 19 | ! 82 2007-04-16 15:40:52Z raasch |
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| 20 | ! Cpp-directive lcmuk changed to intel_openmp_bug |
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| 21 | ! |
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[77] | 22 | ! 75 2007-03-22 09:54:05Z raasch |
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| 23 | ! Collection of time series quantities moved from routine flow_statistics to |
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| 24 | ! here, routine user_statistics is called for each statistic region, |
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| 25 | ! moisture renamed humidity |
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| 26 | ! |
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[39] | 27 | ! 19 2007-02-23 04:53:48Z raasch |
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[77] | 28 | ! fluxes at top modified (tswst, qswst) |
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[39] | 29 | ! |
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[3] | 30 | ! RCS Log replace by Id keyword, revision history cleaned up |
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| 31 | ! |
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[1] | 32 | ! Revision 1.41 2006/08/04 14:37:50 raasch |
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| 33 | ! Error removed in non-parallel part (sums_l) |
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| 34 | ! |
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| 35 | ! Revision 1.1 1997/08/11 06:15:17 raasch |
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| 36 | ! Initial revision |
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| 37 | ! |
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| 38 | ! |
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| 39 | ! Description: |
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| 40 | ! ------------ |
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| 41 | ! Compute average profiles and further average flow quantities for the different |
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| 42 | ! user-defined (sub-)regions. The region indexed 0 is the total model domain. |
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| 43 | ! |
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| 44 | ! NOTE: For simplicity, nzb_s_outer and nzb_diff_s_outer are being used as a |
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| 45 | ! ---- lower vertical index for k-loops for all variables so that regardless |
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| 46 | ! of the variable and its respective staggered grid always the same number of |
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| 47 | ! grid points is used for 2D averages. The disadvantage: depending on the |
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| 48 | ! variable, up to one grid layer adjacent to the (vertical walls of the) |
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| 49 | ! topography is missed out by this simplification. |
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| 50 | !------------------------------------------------------------------------------! |
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| 51 | |
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| 52 | USE arrays_3d |
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| 53 | USE cloud_parameters |
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| 54 | USE cpulog |
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| 55 | USE grid_variables |
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| 56 | USE indices |
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| 57 | USE interfaces |
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| 58 | USE pegrid |
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| 59 | USE statistics |
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| 60 | USE control_parameters |
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| 61 | |
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| 62 | IMPLICIT NONE |
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| 63 | |
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| 64 | INTEGER :: i, j, k, omp_get_thread_num, sr, tn |
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| 65 | LOGICAL :: first |
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| 66 | REAL :: height, pts, sums_l_eper, sums_l_etot, ust, ust2, u2, vst, & |
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| 67 | vst2, v2, w2, z_i(2) |
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| 68 | REAL :: sums_ll(nzb:nzt+1,2) |
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| 69 | |
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| 70 | |
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| 71 | CALL cpu_log( log_point(10), 'flow_statistics', 'start' ) |
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| 72 | |
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| 73 | ! |
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| 74 | !-- To be on the safe side, check whether flow_statistics has already been |
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| 75 | !-- called once after the current time step |
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| 76 | IF ( flow_statistics_called ) THEN |
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| 77 | IF ( myid == 0 ) PRINT*, '+++ WARNING: flow_statistics is called two', & |
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| 78 | ' times within one timestep' |
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| 79 | CALL local_stop |
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| 80 | ENDIF |
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| 81 | |
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| 82 | ! |
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| 83 | !-- Compute statistics for each (sub-)region |
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| 84 | DO sr = 0, statistic_regions |
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| 85 | |
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| 86 | ! |
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| 87 | !-- Initialize (local) summation array |
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| 88 | sums_l = 0.0 |
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| 89 | |
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| 90 | ! |
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| 91 | !-- Store sums that have been computed in other subroutines in summation |
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| 92 | !-- array |
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| 93 | sums_l(:,11,:) = sums_l_l(:,sr,:) ! mixing length from diffusivities |
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| 94 | !-- WARNING: next line still has to be adjusted for OpenMP |
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| 95 | sums_l(:,21,0) = sums_wsts_bc_l(:,sr) ! heat flux from advec_s_bc |
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[87] | 96 | sums_l(nzb+9,pr_palm,0) = sums_divold_l(sr) ! old divergence from pres |
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| 97 | sums_l(nzb+10,pr_palm,0) = sums_divnew_l(sr) ! new divergence from pres |
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[1] | 98 | !-- WARNING: next four lines still may have to be adjusted for OpenMP |
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[87] | 99 | sums_l(nzb:nzb+2,pr_palm-1,0) = sums_up_fraction_l(1,1:3,sr)! upstream |
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| 100 | sums_l(nzb+3:nzb+5,pr_palm-1,0) = sums_up_fraction_l(2,1:3,sr)! parts |
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| 101 | sums_l(nzb+6:nzb+8,pr_palm-1,0) = sums_up_fraction_l(3,1:3,sr)! from |
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| 102 | sums_l(nzb+9:nzb+11,pr_palm-1,0) = sums_up_fraction_l(4,1:3,sr)! spline |
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[1] | 103 | |
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| 104 | ! |
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| 105 | !-- Horizontally averaged profiles of horizontal velocities and temperature. |
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| 106 | !-- They must have been computed before, because they are already required |
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| 107 | !-- for other horizontal averages. |
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| 108 | tn = 0 |
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| 109 | !$OMP PARALLEL PRIVATE( i, j, k, tn ) |
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[82] | 110 | #if defined( __intel_openmp_bug ) |
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[1] | 111 | tn = omp_get_thread_num() |
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| 112 | #else |
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| 113 | !$ tn = omp_get_thread_num() |
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| 114 | #endif |
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| 115 | |
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| 116 | !$OMP DO |
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| 117 | DO i = nxl, nxr |
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| 118 | DO j = nys, nyn |
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| 119 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 120 | sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr) |
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| 121 | sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr) |
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| 122 | sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr) |
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| 123 | ENDDO |
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| 124 | ENDDO |
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| 125 | ENDDO |
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| 126 | |
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| 127 | ! |
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[96] | 128 | !-- Horizontally averaged profile of salinity |
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| 129 | IF ( ocean ) THEN |
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| 130 | !$OMP DO |
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| 131 | DO i = nxl, nxr |
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| 132 | DO j = nys, nyn |
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| 133 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 134 | sums_l(k,23,tn) = sums_l(k,23,tn) + & |
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| 135 | sa(k,j,i) * rmask(j,i,sr) |
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| 136 | ENDDO |
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| 137 | ENDDO |
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| 138 | ENDDO |
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| 139 | ENDIF |
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| 140 | |
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| 141 | ! |
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[1] | 142 | !-- Horizontally averaged profiles of virtual potential temperature, |
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| 143 | !-- total water content, specific humidity and liquid water potential |
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| 144 | !-- temperature |
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[75] | 145 | IF ( humidity ) THEN |
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[1] | 146 | !$OMP DO |
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| 147 | DO i = nxl, nxr |
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| 148 | DO j = nys, nyn |
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| 149 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 150 | sums_l(k,44,tn) = sums_l(k,44,tn) + & |
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| 151 | vpt(k,j,i) * rmask(j,i,sr) |
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| 152 | sums_l(k,41,tn) = sums_l(k,41,tn) + & |
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| 153 | q(k,j,i) * rmask(j,i,sr) |
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| 154 | ENDDO |
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| 155 | ENDDO |
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| 156 | ENDDO |
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| 157 | IF ( cloud_physics ) THEN |
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| 158 | !$OMP DO |
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| 159 | DO i = nxl, nxr |
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| 160 | DO j = nys, nyn |
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| 161 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 162 | sums_l(k,42,tn) = sums_l(k,42,tn) + & |
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| 163 | ( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr) |
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| 164 | sums_l(k,43,tn) = sums_l(k,43,tn) + ( & |
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| 165 | pt(k,j,i) + l_d_cp*pt_d_t(k) * ql(k,j,i) & |
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| 166 | ) * rmask(j,i,sr) |
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| 167 | ENDDO |
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| 168 | ENDDO |
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| 169 | ENDDO |
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| 170 | ENDIF |
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| 171 | ENDIF |
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| 172 | |
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| 173 | ! |
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| 174 | !-- Horizontally averaged profiles of passive scalar |
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| 175 | IF ( passive_scalar ) THEN |
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| 176 | !$OMP DO |
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| 177 | DO i = nxl, nxr |
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| 178 | DO j = nys, nyn |
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| 179 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 180 | sums_l(k,41,tn) = sums_l(k,41,tn) + q(k,j,i) * rmask(j,i,sr) |
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| 181 | ENDDO |
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| 182 | ENDDO |
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| 183 | ENDDO |
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| 184 | ENDIF |
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| 185 | !$OMP END PARALLEL |
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| 186 | |
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| 187 | ! |
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| 188 | !-- Summation of thread sums |
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| 189 | IF ( threads_per_task > 1 ) THEN |
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| 190 | DO i = 1, threads_per_task-1 |
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| 191 | sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i) |
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| 192 | sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i) |
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| 193 | sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i) |
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[96] | 194 | IF ( ocean ) THEN |
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| 195 | sums_l(:,23,0) = sums_l(:,23,0) + sums_l(:,23,i) |
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| 196 | ENDIF |
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[75] | 197 | IF ( humidity ) THEN |
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[1] | 198 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 199 | sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i) |
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| 200 | IF ( cloud_physics ) THEN |
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| 201 | sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i) |
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| 202 | sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i) |
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| 203 | ENDIF |
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| 204 | ENDIF |
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| 205 | IF ( passive_scalar ) THEN |
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| 206 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
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| 207 | ENDIF |
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| 208 | ENDDO |
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| 209 | ENDIF |
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| 210 | |
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| 211 | #if defined( __parallel ) |
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| 212 | ! |
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| 213 | !-- Compute total sum from local sums |
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| 214 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), nzt+2-nzb, MPI_REAL, & |
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| 215 | MPI_SUM, comm2d, ierr ) |
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| 216 | CALL MPI_ALLREDUCE( sums_l(nzb,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, & |
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| 217 | MPI_SUM, comm2d, ierr ) |
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| 218 | CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, & |
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| 219 | MPI_SUM, comm2d, ierr ) |
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[96] | 220 | IF ( ocean ) THEN |
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| 221 | CALL MPI_ALLREDUCE( sums_l(nzb,23,0), sums(nzb,23), nzt+2-nzb, & |
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| 222 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 223 | ENDIF |
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[75] | 224 | IF ( humidity ) THEN |
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[1] | 225 | CALL MPI_ALLREDUCE( sums_l(nzb,44,0), sums(nzb,44), nzt+2-nzb, & |
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| 226 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 227 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 228 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 229 | IF ( cloud_physics ) THEN |
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| 230 | CALL MPI_ALLREDUCE( sums_l(nzb,42,0), sums(nzb,42), nzt+2-nzb, & |
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| 231 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 232 | CALL MPI_ALLREDUCE( sums_l(nzb,43,0), sums(nzb,43), nzt+2-nzb, & |
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| 233 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 234 | ENDIF |
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| 235 | ENDIF |
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| 236 | |
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| 237 | IF ( passive_scalar ) THEN |
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| 238 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
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| 239 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
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| 240 | ENDIF |
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| 241 | #else |
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| 242 | sums(:,1) = sums_l(:,1,0) |
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| 243 | sums(:,2) = sums_l(:,2,0) |
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| 244 | sums(:,4) = sums_l(:,4,0) |
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[96] | 245 | IF ( ocean ) sums(:,23) = sums_l(:,23,0) |
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[75] | 246 | IF ( humidity ) THEN |
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[1] | 247 | sums(:,44) = sums_l(:,44,0) |
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| 248 | sums(:,41) = sums_l(:,41,0) |
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| 249 | IF ( cloud_physics ) THEN |
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| 250 | sums(:,42) = sums_l(:,42,0) |
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| 251 | sums(:,43) = sums_l(:,43,0) |
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| 252 | ENDIF |
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| 253 | ENDIF |
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| 254 | IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0) |
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| 255 | #endif |
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| 256 | |
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| 257 | ! |
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| 258 | !-- Final values are obtained by division by the total number of grid points |
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| 259 | !-- used for summation. After that store profiles. |
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| 260 | sums(:,1) = sums(:,1) / ngp_2dh_outer(:,sr) |
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| 261 | sums(:,2) = sums(:,2) / ngp_2dh_outer(:,sr) |
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| 262 | sums(:,4) = sums(:,4) / ngp_2dh_outer(:,sr) |
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| 263 | hom(:,1,1,sr) = sums(:,1) ! u |
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| 264 | hom(:,1,2,sr) = sums(:,2) ! v |
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| 265 | hom(:,1,4,sr) = sums(:,4) ! pt |
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| 266 | |
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| 267 | ! |
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[96] | 268 | !-- Salinity |
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| 269 | IF ( ocean ) THEN |
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| 270 | sums(:,23) = sums(:,23) / ngp_2dh_outer(:,sr) |
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| 271 | hom(:,1,23,sr) = sums(:,23) ! sa |
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| 272 | ENDIF |
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| 273 | |
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| 274 | ! |
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[1] | 275 | !-- Humidity and cloud parameters |
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[75] | 276 | IF ( humidity ) THEN |
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[1] | 277 | sums(:,44) = sums(:,44) / ngp_2dh_outer(:,sr) |
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| 278 | sums(:,41) = sums(:,41) / ngp_2dh_outer(:,sr) |
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| 279 | hom(:,1,44,sr) = sums(:,44) ! vpt |
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| 280 | hom(:,1,41,sr) = sums(:,41) ! qv (q) |
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| 281 | IF ( cloud_physics ) THEN |
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| 282 | sums(:,42) = sums(:,42) / ngp_2dh_outer(:,sr) |
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| 283 | sums(:,43) = sums(:,43) / ngp_2dh_outer(:,sr) |
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| 284 | hom(:,1,42,sr) = sums(:,42) ! qv |
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| 285 | hom(:,1,43,sr) = sums(:,43) ! pt |
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| 286 | ENDIF |
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| 287 | ENDIF |
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| 288 | |
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| 289 | ! |
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| 290 | !-- Passive scalar |
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| 291 | IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / ngp_2dh_outer(:,sr) |
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| 292 | |
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| 293 | ! |
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| 294 | !-- Horizontally averaged profiles of the remaining prognostic variables, |
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| 295 | !-- variances, the total and the perturbation energy (single values in last |
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| 296 | !-- column of sums_l) and some diagnostic quantities. |
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| 297 | !-- NOTE: for simplicity, nzb_s_outer is used below, although strictly |
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| 298 | !-- ---- speaking the following k-loop would have to be split up and |
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| 299 | !-- rearranged according to the staggered grid. |
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| 300 | tn = 0 |
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[82] | 301 | #if defined( __intel_openmp_bug ) |
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[1] | 302 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, & |
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| 303 | !$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
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| 304 | tn = omp_get_thread_num() |
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| 305 | #else |
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| 306 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
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| 307 | !$ tn = omp_get_thread_num() |
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| 308 | #endif |
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| 309 | !$OMP DO |
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| 310 | DO i = nxl, nxr |
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| 311 | DO j = nys, nyn |
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| 312 | sums_l_etot = 0.0 |
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| 313 | sums_l_eper = 0.0 |
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| 314 | DO k = nzb_s_outer(j,i), nzt+1 |
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| 315 | u2 = u(k,j,i)**2 |
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| 316 | v2 = v(k,j,i)**2 |
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| 317 | w2 = w(k,j,i)**2 |
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| 318 | ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2 |
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| 319 | vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2 |
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| 320 | ! |
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| 321 | !-- Prognostic and diagnostic variables |
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| 322 | sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr) |
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| 323 | sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr) |
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| 324 | sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr) |
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| 325 | sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr) |
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| 326 | sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i) |
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| 327 | |
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| 328 | ! |
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| 329 | !-- Variances |
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| 330 | sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr) |
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| 331 | sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr) |
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| 332 | sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr) |
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| 333 | sums_l(k,33,tn) = sums_l(k,33,tn) + & |
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| 334 | ( pt(k,j,i)-hom(k,1,4,sr) )**2 * rmask(j,i,sr) |
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| 335 | ! |
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| 336 | !-- Higher moments |
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| 337 | !-- (Computation of the skewness of w further below) |
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| 338 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
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| 339 | rmask(j,i,sr) |
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| 340 | ! |
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| 341 | !-- Perturbation energy |
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| 342 | sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * ( ust2 + vst2 + w2 ) & |
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| 343 | * rmask(j,i,sr) |
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| 344 | sums_l_etot = sums_l_etot + & |
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| 345 | 0.5 * ( u2 + v2 + w2 ) * rmask(j,i,sr) |
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| 346 | sums_l_eper = sums_l_eper + & |
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| 347 | 0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr) |
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| 348 | ENDDO |
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| 349 | ! |
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| 350 | !-- Total and perturbation energy for the total domain (being |
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| 351 | !-- collected in the last column of sums_l). Summation of these |
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| 352 | !-- quantities is seperated from the previous loop in order to |
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| 353 | !-- allow vectorization of that loop. |
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[87] | 354 | sums_l(nzb+4,pr_palm,tn) = sums_l(nzb+4,pr_palm,tn) + sums_l_etot |
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| 355 | sums_l(nzb+5,pr_palm,tn) = sums_l(nzb+5,pr_palm,tn) + sums_l_eper |
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[1] | 356 | ! |
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| 357 | !-- 2D-arrays (being collected in the last column of sums_l) |
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[87] | 358 | sums_l(nzb,pr_palm,tn) = sums_l(nzb,pr_palm,tn) + & |
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[1] | 359 | us(j,i) * rmask(j,i,sr) |
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[87] | 360 | sums_l(nzb+1,pr_palm,tn) = sums_l(nzb+1,pr_palm,tn) + & |
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[1] | 361 | usws(j,i) * rmask(j,i,sr) |
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[87] | 362 | sums_l(nzb+2,pr_palm,tn) = sums_l(nzb+2,pr_palm,tn) + & |
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[1] | 363 | vsws(j,i) * rmask(j,i,sr) |
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[87] | 364 | sums_l(nzb+3,pr_palm,tn) = sums_l(nzb+3,pr_palm,tn) + & |
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[1] | 365 | ts(j,i) * rmask(j,i,sr) |
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| 366 | ENDDO |
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| 367 | ENDDO |
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| 368 | |
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| 369 | ! |
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| 370 | !-- Horizontally averaged profiles of the vertical fluxes |
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| 371 | !$OMP DO |
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| 372 | DO i = nxl, nxr |
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| 373 | DO j = nys, nyn |
---|
| 374 | ! |
---|
| 375 | !-- Subgridscale fluxes (without Prandtl layer from k=nzb, |
---|
| 376 | !-- oterwise from k=nzb+1) |
---|
| 377 | !-- NOTE: for simplicity, nzb_diff_s_outer is used below, although |
---|
| 378 | !-- ---- strictly speaking the following k-loop would have to be |
---|
| 379 | !-- split up according to the staggered grid. |
---|
| 380 | DO k = nzb_diff_s_outer(j,i)-1, nzt |
---|
| 381 | ! |
---|
| 382 | !-- Momentum flux w"u" |
---|
| 383 | sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( & |
---|
| 384 | km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) & |
---|
| 385 | ) * ( & |
---|
| 386 | ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
---|
| 387 | + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
---|
| 388 | ) * rmask(j,i,sr) |
---|
| 389 | ! |
---|
| 390 | !-- Momentum flux w"v" |
---|
| 391 | sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( & |
---|
| 392 | km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) & |
---|
| 393 | ) * ( & |
---|
| 394 | ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
---|
| 395 | + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
---|
| 396 | ) * rmask(j,i,sr) |
---|
[19] | 397 | ENDDO |
---|
| 398 | |
---|
| 399 | DO k = nzb_diff_s_outer(j,i)-1, nzt_diff |
---|
[1] | 400 | ! |
---|
| 401 | !-- Heat flux w"pt" |
---|
| 402 | sums_l(k,16,tn) = sums_l(k,16,tn) & |
---|
| 403 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 404 | * ( pt(k+1,j,i) - pt(k,j,i) ) & |
---|
| 405 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 406 | |
---|
| 407 | |
---|
| 408 | ! |
---|
[96] | 409 | !-- Salinity flux w"sa" |
---|
| 410 | IF ( ocean ) THEN |
---|
| 411 | sums_l(k,65,tn) = sums_l(k,65,tn) & |
---|
| 412 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 413 | * ( sa(k+1,j,i) - sa(k,j,i) ) & |
---|
| 414 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 415 | ENDIF |
---|
| 416 | |
---|
| 417 | ! |
---|
[1] | 418 | !-- Buoyancy flux, water flux (humidity flux) w"q" |
---|
[75] | 419 | IF ( humidity ) THEN |
---|
[1] | 420 | sums_l(k,45,tn) = sums_l(k,45,tn) & |
---|
| 421 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 422 | * ( vpt(k+1,j,i) - vpt(k,j,i) ) & |
---|
| 423 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 424 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 425 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 426 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 427 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 428 | IF ( cloud_physics ) THEN |
---|
| 429 | sums_l(k,51,tn) = sums_l(k,51,tn) & |
---|
| 430 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 431 | * ( ( q(k+1,j,i) - ql(k+1,j,i) )& |
---|
| 432 | - ( q(k,j,i) - ql(k,j,i) ) ) & |
---|
| 433 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 434 | ENDIF |
---|
| 435 | ENDIF |
---|
| 436 | |
---|
| 437 | ! |
---|
| 438 | !-- Passive scalar flux |
---|
| 439 | IF ( passive_scalar ) THEN |
---|
| 440 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 441 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 442 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 443 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 444 | ENDIF |
---|
| 445 | |
---|
| 446 | ENDDO |
---|
| 447 | |
---|
| 448 | ! |
---|
| 449 | !-- Subgridscale fluxes in the Prandtl layer |
---|
| 450 | IF ( use_surface_fluxes ) THEN |
---|
| 451 | sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + & |
---|
| 452 | usws(j,i) * rmask(j,i,sr) ! w"u" |
---|
| 453 | sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + & |
---|
| 454 | vsws(j,i) * rmask(j,i,sr) ! w"v" |
---|
| 455 | sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + & |
---|
| 456 | shf(j,i) * rmask(j,i,sr) ! w"pt" |
---|
| 457 | sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + & |
---|
| 458 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
| 459 | sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + & |
---|
| 460 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
[96] | 461 | IF ( ocean ) THEN |
---|
| 462 | sums_l(nzb,65,tn) = sums_l(nzb,65,tn) + & |
---|
| 463 | saswsb(j,i) * rmask(j,i,sr) ! w"sa" |
---|
| 464 | ENDIF |
---|
[75] | 465 | IF ( humidity ) THEN |
---|
[1] | 466 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 467 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 468 | IF ( cloud_physics ) THEN |
---|
| 469 | sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( & |
---|
| 470 | ( 1.0 + 0.61 * q(nzb,j,i) ) * & |
---|
| 471 | shf(j,i) + 0.61 * pt(nzb,j,i) * & |
---|
| 472 | qsws(j,i) & |
---|
| 473 | ) |
---|
| 474 | ! |
---|
| 475 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 476 | sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv") |
---|
| 477 | qsws(j,i) * rmask(j,i,sr) |
---|
| 478 | ENDIF |
---|
| 479 | ENDIF |
---|
| 480 | IF ( passive_scalar ) THEN |
---|
| 481 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 482 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 483 | ENDIF |
---|
| 484 | ENDIF |
---|
| 485 | |
---|
| 486 | ! |
---|
[19] | 487 | !-- Subgridscale fluxes at the top surface |
---|
| 488 | IF ( use_top_fluxes ) THEN |
---|
| 489 | sums_l(nzt,16,tn) = sums_l(nzt,16,tn) + & |
---|
| 490 | tswst(j,i) * rmask(j,i,sr) ! w"pt" |
---|
| 491 | sums_l(nzt,58,tn) = sums_l(nzt,58,tn) + & |
---|
| 492 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
| 493 | sums_l(nzt,61,tn) = sums_l(nzt,61,tn) + & |
---|
| 494 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
[96] | 495 | IF ( ocean ) THEN |
---|
| 496 | sums_l(nzt,65,tn) = sums_l(nzt,65,tn) + & |
---|
| 497 | saswst(j,i) * rmask(j,i,sr) ! w"sa" |
---|
| 498 | ENDIF |
---|
[75] | 499 | IF ( humidity ) THEN |
---|
[19] | 500 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
| 501 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 502 | IF ( cloud_physics ) THEN |
---|
| 503 | sums_l(nzt,45,tn) = sums_l(nzt,45,tn) + ( & |
---|
| 504 | ( 1.0 + 0.61 * q(nzt,j,i) ) * & |
---|
| 505 | tswst(j,i) + 0.61 * pt(nzt,j,i) * & |
---|
| 506 | qsws(j,i) & |
---|
| 507 | ) |
---|
| 508 | ! |
---|
| 509 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 510 | sums_l(nzt,51,tn) = sums_l(nzt,51,tn) + & ! w"q" (w"qv") |
---|
| 511 | qswst(j,i) * rmask(j,i,sr) |
---|
| 512 | ENDIF |
---|
| 513 | ENDIF |
---|
| 514 | IF ( passive_scalar ) THEN |
---|
| 515 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
| 516 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 517 | ENDIF |
---|
| 518 | ENDIF |
---|
| 519 | |
---|
| 520 | ! |
---|
[1] | 521 | !-- Resolved fluxes (can be computed for all horizontal points) |
---|
| 522 | !-- NOTE: for simplicity, nzb_s_outer is used below, although strictly |
---|
| 523 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 524 | !-- rearranged according to the staggered grid. |
---|
| 525 | DO k = nzb_s_outer(j,i), nzt |
---|
| 526 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 527 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 528 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 529 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 530 | pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 531 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) |
---|
| 532 | ! |
---|
| 533 | !-- Momentum flux w*u* |
---|
| 534 | sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * & |
---|
| 535 | ( w(k,j,i-1) + w(k,j,i) ) & |
---|
| 536 | * ust * rmask(j,i,sr) |
---|
| 537 | ! |
---|
| 538 | !-- Momentum flux w*v* |
---|
| 539 | sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * & |
---|
| 540 | ( w(k,j-1,i) + w(k,j,i) ) & |
---|
| 541 | * vst * rmask(j,i,sr) |
---|
| 542 | ! |
---|
| 543 | !-- Heat flux w*pt* |
---|
| 544 | !-- The following formula (comment line, not executed) does not |
---|
| 545 | !-- work if applied to subregions |
---|
| 546 | ! sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * & |
---|
| 547 | ! ( pt(k,j,i)+pt(k+1,j,i) ) & |
---|
| 548 | ! * w(k,j,i) * rmask(j,i,sr) |
---|
| 549 | sums_l(k,17,tn) = sums_l(k,17,tn) + pts * w(k,j,i) * & |
---|
| 550 | rmask(j,i,sr) |
---|
| 551 | ! |
---|
| 552 | !-- Higher moments |
---|
| 553 | sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)**2 * & |
---|
| 554 | rmask(j,i,sr) |
---|
| 555 | sums_l(k,36,tn) = sums_l(k,36,tn) + pts**2 * w(k,j,i) * & |
---|
| 556 | rmask(j,i,sr) |
---|
| 557 | |
---|
| 558 | ! |
---|
[96] | 559 | !-- Salinity flux and density (density does not belong to here, |
---|
| 560 | !-- but so far there is no suitable place to calculate) |
---|
| 561 | IF ( ocean ) THEN |
---|
| 562 | pts = 0.5 * ( sa(k,j,i) - hom(k,1,23,sr) + & |
---|
| 563 | sa(k+1,j,i) - hom(k+1,1,23,sr) ) |
---|
| 564 | sums_l(k,66,tn) = sums_l(k,66,tn) + pts * w(k,j,i) * & |
---|
| 565 | rmask(j,i,sr) |
---|
| 566 | sums_l(k,64,tn) = sums_l(k,64,tn) + rho(k,j,i) * & |
---|
| 567 | rmask(j,i,sr) |
---|
| 568 | ENDIF |
---|
| 569 | |
---|
| 570 | ! |
---|
[1] | 571 | !-- Buoyancy flux, water flux, humidity flux and liquid water |
---|
| 572 | !-- content |
---|
[75] | 573 | IF ( humidity ) THEN |
---|
[1] | 574 | pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + & |
---|
| 575 | vpt(k+1,j,i) - hom(k+1,1,44,sr) ) |
---|
| 576 | sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * & |
---|
| 577 | rmask(j,i,sr) |
---|
| 578 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 579 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 580 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 581 | rmask(j,i,sr) |
---|
| 582 | IF ( cloud_physics .OR. cloud_droplets ) THEN |
---|
| 583 | pts = 0.5 * & |
---|
| 584 | ( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) & |
---|
| 585 | + ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) ) |
---|
| 586 | sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * & |
---|
| 587 | rmask(j,i,sr) |
---|
| 588 | sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * & |
---|
| 589 | rmask(j,i,sr) |
---|
| 590 | ENDIF |
---|
| 591 | ENDIF |
---|
| 592 | |
---|
| 593 | ! |
---|
| 594 | !-- Passive scalar flux |
---|
| 595 | IF ( passive_scalar ) THEN |
---|
| 596 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 597 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 598 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 599 | rmask(j,i,sr) |
---|
| 600 | ENDIF |
---|
| 601 | |
---|
| 602 | ! |
---|
| 603 | !-- Energy flux w*e* |
---|
| 604 | sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * & |
---|
| 605 | ( ust**2 + vst**2 + w(k,j,i)**2 )& |
---|
| 606 | * rmask(j,i,sr) |
---|
| 607 | |
---|
| 608 | ENDDO |
---|
| 609 | ENDDO |
---|
| 610 | ENDDO |
---|
| 611 | |
---|
| 612 | ! |
---|
| 613 | !-- Divergence of vertical flux of resolved scale energy and pressure |
---|
| 614 | !-- fluctuations. First calculate the products, then the divergence. |
---|
| 615 | !-- Calculation is time consuming. Do it only, if profiles shall be plotted. |
---|
| 616 | IF ( hom(nzb+1,2,55,0) /= 0.0 ) THEN |
---|
| 617 | |
---|
| 618 | sums_ll = 0.0 ! local array |
---|
| 619 | |
---|
| 620 | !$OMP DO |
---|
| 621 | DO i = nxl, nxr |
---|
| 622 | DO j = nys, nyn |
---|
| 623 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 624 | |
---|
| 625 | sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( & |
---|
| 626 | ( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) & |
---|
| 627 | - 2.0 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) & |
---|
| 628 | ) )**2 & |
---|
| 629 | + ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) & |
---|
| 630 | - 2.0 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) & |
---|
| 631 | ) )**2 & |
---|
| 632 | + w(k,j,i)**2 ) |
---|
| 633 | |
---|
| 634 | sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) & |
---|
| 635 | * ( p(k,j,i) + p(k+1,j,i) ) |
---|
| 636 | |
---|
| 637 | ENDDO |
---|
| 638 | ENDDO |
---|
| 639 | ENDDO |
---|
| 640 | sums_ll(0,1) = 0.0 ! because w is zero at the bottom |
---|
| 641 | sums_ll(nzt+1,1) = 0.0 |
---|
| 642 | sums_ll(0,2) = 0.0 |
---|
| 643 | sums_ll(nzt+1,2) = 0.0 |
---|
| 644 | |
---|
| 645 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 646 | sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k) |
---|
| 647 | sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k) |
---|
| 648 | ENDDO |
---|
| 649 | sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn) |
---|
| 650 | sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn) |
---|
| 651 | |
---|
| 652 | ENDIF |
---|
| 653 | |
---|
| 654 | ! |
---|
| 655 | !-- Divergence of vertical flux of SGS TKE |
---|
| 656 | IF ( hom(nzb+1,2,57,0) /= 0.0 ) THEN |
---|
| 657 | |
---|
| 658 | !$OMP DO |
---|
| 659 | DO i = nxl, nxr |
---|
| 660 | DO j = nys, nyn |
---|
| 661 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 662 | |
---|
| 663 | sums_l(k,57,tn) = sums_l(k,57,tn) + ( & |
---|
| 664 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 665 | - (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) & |
---|
| 666 | ) * ddzw(k) |
---|
| 667 | |
---|
| 668 | ENDDO |
---|
| 669 | ENDDO |
---|
| 670 | ENDDO |
---|
| 671 | sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn) |
---|
| 672 | |
---|
| 673 | ENDIF |
---|
| 674 | |
---|
| 675 | ! |
---|
| 676 | !-- Horizontal heat fluxes (subgrid, resolved, total). |
---|
| 677 | !-- Do it only, if profiles shall be plotted. |
---|
| 678 | IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN |
---|
| 679 | |
---|
| 680 | !$OMP DO |
---|
| 681 | DO i = nxl, nxr |
---|
| 682 | DO j = nys, nyn |
---|
| 683 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 684 | ! |
---|
| 685 | !-- Subgrid horizontal heat fluxes u"pt", v"pt" |
---|
| 686 | sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * & |
---|
| 687 | ( kh(k,j,i) + kh(k,j,i-1) ) & |
---|
| 688 | * ( pt(k,j,i-1) - pt(k,j,i) ) & |
---|
| 689 | * ddx * rmask(j,i,sr) |
---|
| 690 | sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * & |
---|
| 691 | ( kh(k,j,i) + kh(k,j-1,i) ) & |
---|
| 692 | * ( pt(k,j-1,i) - pt(k,j,i) ) & |
---|
| 693 | * ddy * rmask(j,i,sr) |
---|
| 694 | ! |
---|
| 695 | !-- Resolved horizontal heat fluxes u*pt*, v*pt* |
---|
| 696 | sums_l(k,59,tn) = sums_l(k,59,tn) + & |
---|
| 697 | ( u(k,j,i) - hom(k,1,1,sr) ) & |
---|
| 698 | * 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + & |
---|
| 699 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 700 | pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 701 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 702 | sums_l(k,62,tn) = sums_l(k,62,tn) + & |
---|
| 703 | ( v(k,j,i) - hom(k,1,2,sr) ) & |
---|
| 704 | * 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 705 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 706 | ENDDO |
---|
| 707 | ENDDO |
---|
| 708 | ENDDO |
---|
| 709 | ! |
---|
| 710 | !-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer) |
---|
| 711 | sums(nzb,58) = 0.0 |
---|
| 712 | sums(nzb,59) = 0.0 |
---|
| 713 | sums(nzb,60) = 0.0 |
---|
| 714 | sums(nzb,61) = 0.0 |
---|
| 715 | sums(nzb,62) = 0.0 |
---|
| 716 | sums(nzb,63) = 0.0 |
---|
| 717 | |
---|
| 718 | ENDIF |
---|
[87] | 719 | |
---|
| 720 | ! |
---|
| 721 | !-- Calculate the user-defined profiles |
---|
| 722 | CALL user_statistics( 'profiles', sr, tn ) |
---|
[1] | 723 | !$OMP END PARALLEL |
---|
| 724 | |
---|
| 725 | ! |
---|
| 726 | !-- Summation of thread sums |
---|
| 727 | IF ( threads_per_task > 1 ) THEN |
---|
| 728 | DO i = 1, threads_per_task-1 |
---|
| 729 | sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i) |
---|
| 730 | sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i) |
---|
[87] | 731 | sums_l(:,45:pr_palm,0) = sums_l(:,45:pr_palm,0) + & |
---|
| 732 | sums_l(:,45:pr_palm,i) |
---|
| 733 | IF ( max_pr_user > 0 ) THEN |
---|
| 734 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) = & |
---|
| 735 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) + & |
---|
| 736 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,i) |
---|
| 737 | ENDIF |
---|
[1] | 738 | ENDDO |
---|
| 739 | ENDIF |
---|
| 740 | |
---|
| 741 | #if defined( __parallel ) |
---|
| 742 | ! |
---|
| 743 | !-- Compute total sum from local sums |
---|
| 744 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, & |
---|
| 745 | MPI_SUM, comm2d, ierr ) |
---|
| 746 | #else |
---|
| 747 | sums = sums_l(:,:,0) |
---|
| 748 | #endif |
---|
| 749 | |
---|
| 750 | ! |
---|
| 751 | !-- Final values are obtained by division by the total number of grid points |
---|
| 752 | !-- used for summation. After that store profiles. |
---|
| 753 | !-- Profiles: |
---|
| 754 | DO k = nzb, nzt+1 |
---|
[87] | 755 | sums(k,:pr_palm-2) = sums(k,:pr_palm-2) / ngp_2dh_outer(k,sr) |
---|
[1] | 756 | ENDDO |
---|
| 757 | !-- Upstream-parts |
---|
[87] | 758 | sums(nzb:nzb+11,pr_palm-1) = sums(nzb:nzb+11,pr_palm-1) / ngp_3d(sr) |
---|
[1] | 759 | !-- u* and so on |
---|
[87] | 760 | !-- As sums(nzb:nzb+3,pr_palm) are full 2D arrays (us, usws, vsws, ts) whose |
---|
[1] | 761 | !-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer |
---|
| 762 | !-- above the topography, they are being divided by ngp_2dh(sr) |
---|
[87] | 763 | sums(nzb:nzb+3,pr_palm) = sums(nzb:nzb+3,pr_palm) / & |
---|
[1] | 764 | ngp_2dh(sr) |
---|
| 765 | !-- eges, e* |
---|
[87] | 766 | sums(nzb+4:nzb+5,pr_palm) = sums(nzb+4:nzb+5,pr_palm) / & |
---|
[1] | 767 | ngp_3d_inner(sr) |
---|
| 768 | !-- Old and new divergence |
---|
[87] | 769 | sums(nzb+9:nzb+10,pr_palm) = sums(nzb+9:nzb+10,pr_palm) / & |
---|
[1] | 770 | ngp_3d_inner(sr) |
---|
| 771 | |
---|
[87] | 772 | !-- User-defined profiles |
---|
| 773 | IF ( max_pr_user > 0 ) THEN |
---|
| 774 | DO k = nzb, nzt+1 |
---|
| 775 | sums(k,pr_palm+1:pr_palm+max_pr_user) = & |
---|
| 776 | sums(k,pr_palm+1:pr_palm+max_pr_user) / & |
---|
| 777 | ngp_2dh_outer(k,sr) |
---|
| 778 | ENDDO |
---|
| 779 | ENDIF |
---|
| 780 | |
---|
[1] | 781 | ! |
---|
| 782 | !-- Collect horizontal average in hom. |
---|
| 783 | !-- Compute deduced averages (e.g. total heat flux) |
---|
| 784 | hom(:,1,3,sr) = sums(:,3) ! w |
---|
| 785 | hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles |
---|
| 786 | hom(:,1,9,sr) = sums(:,9) ! km |
---|
| 787 | hom(:,1,10,sr) = sums(:,10) ! kh |
---|
| 788 | hom(:,1,11,sr) = sums(:,11) ! l |
---|
| 789 | hom(:,1,12,sr) = sums(:,12) ! w"u" |
---|
| 790 | hom(:,1,13,sr) = sums(:,13) ! w*u* |
---|
| 791 | hom(:,1,14,sr) = sums(:,14) ! w"v" |
---|
| 792 | hom(:,1,15,sr) = sums(:,15) ! w*v* |
---|
| 793 | hom(:,1,16,sr) = sums(:,16) ! w"pt" |
---|
| 794 | hom(:,1,17,sr) = sums(:,17) ! w*pt* |
---|
| 795 | hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt |
---|
| 796 | hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu |
---|
| 797 | hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv |
---|
| 798 | hom(:,1,21,sr) = sums(:,21) ! w*pt*BC |
---|
| 799 | hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC |
---|
[96] | 800 | ! profile 24 is initial profile (sa) |
---|
| 801 | ! profiles 25-29 left empty for initial |
---|
[1] | 802 | ! profiles |
---|
| 803 | hom(:,1,30,sr) = sums(:,30) ! u*2 |
---|
| 804 | hom(:,1,31,sr) = sums(:,31) ! v*2 |
---|
| 805 | hom(:,1,32,sr) = sums(:,32) ! w*2 |
---|
| 806 | hom(:,1,33,sr) = sums(:,33) ! pt*2 |
---|
| 807 | hom(:,1,34,sr) = sums(:,34) ! e* |
---|
| 808 | hom(:,1,35,sr) = sums(:,35) ! w*2pt* |
---|
| 809 | hom(:,1,36,sr) = sums(:,36) ! w*pt*2 |
---|
| 810 | hom(:,1,37,sr) = sums(:,37) ! w*e* |
---|
| 811 | hom(:,1,38,sr) = sums(:,38) ! w*3 |
---|
| 812 | hom(:,1,39,sr) = sums(:,38) / ( sums(:,32) + 1E-20 )**1.5 ! Sw |
---|
| 813 | hom(:,1,40,sr) = sums(:,40) ! p |
---|
| 814 | hom(:,1,45,sr) = sums(:,45) ! w"q" |
---|
| 815 | hom(:,1,46,sr) = sums(:,46) ! w*vpt* |
---|
| 816 | hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt |
---|
| 817 | hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv") |
---|
| 818 | hom(:,1,49,sr) = sums(:,49) ! w*q* (w*qv*) |
---|
| 819 | hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv) |
---|
| 820 | hom(:,1,51,sr) = sums(:,51) ! w"qv" |
---|
| 821 | hom(:,1,52,sr) = sums(:,52) ! w*qv* |
---|
| 822 | hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv) |
---|
| 823 | hom(:,1,54,sr) = sums(:,54) ! ql |
---|
| 824 | hom(:,1,55,sr) = sums(:,55) ! w*u*u*/dz |
---|
| 825 | hom(:,1,56,sr) = sums(:,56) ! w*p*/dz |
---|
| 826 | hom(:,1,57,sr) = sums(:,57) ! w"e/dz |
---|
| 827 | hom(:,1,58,sr) = sums(:,58) ! u"pt" |
---|
| 828 | hom(:,1,59,sr) = sums(:,59) ! u*pt* |
---|
| 829 | hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t |
---|
| 830 | hom(:,1,61,sr) = sums(:,61) ! v"pt" |
---|
| 831 | hom(:,1,62,sr) = sums(:,62) ! v*pt* |
---|
| 832 | hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t |
---|
[96] | 833 | hom(:,1,64,sr) = sums(:,64) ! rho |
---|
| 834 | hom(:,1,65,sr) = sums(:,65) ! w"sa" |
---|
| 835 | hom(:,1,66,sr) = sums(:,66) ! w*sa* |
---|
| 836 | hom(:,1,67,sr) = sums(:,65) + sums(:,66) ! wsa |
---|
[1] | 837 | |
---|
[87] | 838 | hom(:,1,pr_palm-1,sr) = sums(:,pr_palm-1) |
---|
[1] | 839 | ! upstream-parts u_x, u_y, u_z, v_x, |
---|
| 840 | ! v_y, usw. (in last but one profile) |
---|
[87] | 841 | hom(:,1,pr_palm,sr) = sums(:,pr_palm) |
---|
[1] | 842 | ! u*, w'u', w'v', t* (in last profile) |
---|
| 843 | |
---|
[87] | 844 | IF ( max_pr_user > 0 ) THEN ! user-defined profiles |
---|
| 845 | hom(:,1,pr_palm+1:pr_palm+max_pr_user,sr) = & |
---|
| 846 | sums(:,pr_palm+1:pr_palm+max_pr_user) |
---|
| 847 | ENDIF |
---|
| 848 | |
---|
[1] | 849 | ! |
---|
| 850 | !-- Determine the boundary layer height using two different schemes. |
---|
[94] | 851 | !-- First scheme: Starting from the Earth's (Ocean's) surface, look for the |
---|
| 852 | !-- first relative minimum (maximum) of the total heat flux. |
---|
| 853 | !-- The corresponding height is assumed as the boundary layer height, if it |
---|
| 854 | !-- is less than 1.5 times the height where the heat flux becomes negative |
---|
| 855 | !-- (positive) for the first time. |
---|
[1] | 856 | !-- NOTE: This criterion is still capable of improving! |
---|
| 857 | z_i(1) = 0.0 |
---|
| 858 | first = .TRUE. |
---|
[94] | 859 | ! IF ( .NOT. ocean ) THEN |
---|
| 860 | DO k = nzb, nzt-1 |
---|
| 861 | IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN |
---|
| 862 | first = .FALSE. |
---|
| 863 | height = zw(k) |
---|
[1] | 864 | ENDIF |
---|
[94] | 865 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
| 866 | hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
| 867 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 868 | z_i(1) = zw(k) |
---|
| 869 | ELSE |
---|
| 870 | z_i(1) = height |
---|
| 871 | ENDIF |
---|
| 872 | EXIT |
---|
| 873 | ENDIF |
---|
| 874 | ENDDO |
---|
| 875 | ! ELSE |
---|
| 876 | ! ENDIF |
---|
[1] | 877 | |
---|
| 878 | ! |
---|
| 879 | !-- Second scheme: Starting from the top model boundary, look for the first |
---|
| 880 | !-- characteristic kink in the temperature profile, where the originally |
---|
| 881 | !-- stable stratification notably weakens. |
---|
| 882 | z_i(2) = 0.0 |
---|
| 883 | DO k = nzt-1, nzb+1, -1 |
---|
| 884 | IF ( ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) > & |
---|
| 885 | 2.0 * ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) ) THEN |
---|
| 886 | z_i(2) = zu(k) |
---|
| 887 | EXIT |
---|
| 888 | ENDIF |
---|
| 889 | ENDDO |
---|
| 890 | |
---|
[87] | 891 | hom(nzb+6,1,pr_palm,sr) = z_i(1) |
---|
| 892 | hom(nzb+7,1,pr_palm,sr) = z_i(2) |
---|
[1] | 893 | |
---|
| 894 | ! |
---|
| 895 | !-- Computation of both the characteristic vertical velocity and |
---|
| 896 | !-- the characteristic convective boundary layer temperature. |
---|
| 897 | !-- The horizontal average at nzb+1 is input for the average temperature. |
---|
| 898 | IF ( hom(nzb,1,18,sr) > 0.0 .AND. z_i(1) /= 0.0 ) THEN |
---|
[87] | 899 | hom(nzb+8,1,pr_palm,sr) = ( g / hom(nzb+1,1,4,sr) * & |
---|
[94] | 900 | hom(nzb,1,18,sr) * & |
---|
| 901 | ABS( z_i(1) ) )**0.333333333 |
---|
[1] | 902 | !-- so far this only works if Prandtl layer is used |
---|
[87] | 903 | hom(nzb+11,1,pr_palm,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,pr_palm,sr) |
---|
[1] | 904 | ELSE |
---|
[87] | 905 | hom(nzb+8,1,pr_palm,sr) = 0.0 |
---|
| 906 | hom(nzb+11,1,pr_palm,sr) = 0.0 |
---|
[1] | 907 | ENDIF |
---|
| 908 | |
---|
[48] | 909 | ! |
---|
| 910 | !-- Collect the time series quantities |
---|
[87] | 911 | ts_value(1,sr) = hom(nzb+4,1,pr_palm,sr) ! E |
---|
| 912 | ts_value(2,sr) = hom(nzb+5,1,pr_palm,sr) ! E* |
---|
[48] | 913 | ts_value(3,sr) = dt_3d |
---|
[87] | 914 | ts_value(4,sr) = hom(nzb,1,pr_palm,sr) ! u* |
---|
| 915 | ts_value(5,sr) = hom(nzb+3,1,pr_palm,sr) ! th* |
---|
[48] | 916 | ts_value(6,sr) = u_max |
---|
| 917 | ts_value(7,sr) = v_max |
---|
| 918 | ts_value(8,sr) = w_max |
---|
[87] | 919 | ts_value(9,sr) = hom(nzb+10,1,pr_palm,sr) ! new divergence |
---|
| 920 | ts_value(10,sr) = hom(nzb+9,1,pr_palm,sr) ! old Divergence |
---|
| 921 | ts_value(11,sr) = hom(nzb+6,1,pr_palm,sr) ! z_i(1) |
---|
| 922 | ts_value(12,sr) = hom(nzb+7,1,pr_palm,sr) ! z_i(2) |
---|
| 923 | ts_value(13,sr) = hom(nzb+8,1,pr_palm,sr) ! w* |
---|
[48] | 924 | ts_value(14,sr) = hom(nzb,1,16,sr) ! w'pt' at k=0 |
---|
| 925 | ts_value(15,sr) = hom(nzb+1,1,16,sr) ! w'pt' at k=1 |
---|
| 926 | ts_value(16,sr) = hom(nzb+1,1,18,sr) ! wpt at k=1 |
---|
| 927 | ts_value(17,sr) = hom(nzb,1,4,sr) ! pt(0) |
---|
| 928 | ts_value(18,sr) = hom(nzb+1,1,4,sr) ! pt(zp) |
---|
[87] | 929 | ts_value(19,sr) = hom(nzb+9,1,pr_palm-1,sr) ! splptx |
---|
| 930 | ts_value(20,sr) = hom(nzb+10,1,pr_palm-1,sr) ! splpty |
---|
| 931 | ts_value(21,sr) = hom(nzb+11,1,pr_palm-1,sr) ! splptz |
---|
[48] | 932 | IF ( ts_value(5,sr) /= 0.0 ) THEN |
---|
| 933 | ts_value(22,sr) = ts_value(4,sr)**2 / & |
---|
| 934 | ( kappa * g * ts_value(5,sr) / ts_value(18,sr) ) ! L |
---|
| 935 | ELSE |
---|
| 936 | ts_value(22,sr) = 10000.0 |
---|
| 937 | ENDIF |
---|
[1] | 938 | |
---|
| 939 | ! |
---|
[48] | 940 | !-- Calculate additional statistics provided by the user interface |
---|
[87] | 941 | CALL user_statistics( 'time_series', sr, 0 ) |
---|
[1] | 942 | |
---|
[48] | 943 | ENDDO ! loop of the subregions |
---|
| 944 | |
---|
[1] | 945 | ! |
---|
| 946 | !-- If required, sum up horizontal averages for subsequent time averaging |
---|
| 947 | IF ( do_sum ) THEN |
---|
| 948 | IF ( average_count_pr == 0 ) hom_sum = 0.0 |
---|
| 949 | hom_sum = hom_sum + hom(:,1,:,:) |
---|
| 950 | average_count_pr = average_count_pr + 1 |
---|
| 951 | do_sum = .FALSE. |
---|
| 952 | ENDIF |
---|
| 953 | |
---|
| 954 | ! |
---|
| 955 | !-- Set flag for other UPs (e.g. output routines, but also buoyancy). |
---|
| 956 | !-- This flag is reset after each time step in time_integration. |
---|
| 957 | flow_statistics_called = .TRUE. |
---|
| 958 | |
---|
| 959 | CALL cpu_log( log_point(10), 'flow_statistics', 'stop' ) |
---|
| 960 | |
---|
| 961 | |
---|
| 962 | END SUBROUTINE flow_statistics |
---|
| 963 | |
---|
| 964 | |
---|
| 965 | |
---|