[1] | 1 | SUBROUTINE flow_statistics |
---|
| 2 | |
---|
| 3 | !------------------------------------------------------------------------------! |
---|
| 4 | ! Actual revisions: |
---|
| 5 | ! ----------------- |
---|
[94] | 6 | ! Calculation of Deardorff velocity scale adjusted to be used with the ocean |
---|
| 7 | ! version (HAS STILL TO BE COMPLETED!!!) |
---|
[1] | 8 | ! |
---|
| 9 | ! Former revisions: |
---|
| 10 | ! ----------------- |
---|
[3] | 11 | ! $Id: flow_statistics.f90 94 2007-06-01 15:25:22Z raasch $ |
---|
[39] | 12 | ! |
---|
[90] | 13 | ! 87 2007-05-22 15:46:47Z raasch |
---|
| 14 | ! Two more arguments added to user_statistics, which is now also called for |
---|
| 15 | ! user-defined profiles, |
---|
| 16 | ! var_hom and var_sum renamed pr_palm |
---|
| 17 | ! |
---|
[83] | 18 | ! 82 2007-04-16 15:40:52Z raasch |
---|
| 19 | ! Cpp-directive lcmuk changed to intel_openmp_bug |
---|
| 20 | ! |
---|
[77] | 21 | ! 75 2007-03-22 09:54:05Z raasch |
---|
| 22 | ! Collection of time series quantities moved from routine flow_statistics to |
---|
| 23 | ! here, routine user_statistics is called for each statistic region, |
---|
| 24 | ! moisture renamed humidity |
---|
| 25 | ! |
---|
[39] | 26 | ! 19 2007-02-23 04:53:48Z raasch |
---|
[77] | 27 | ! fluxes at top modified (tswst, qswst) |
---|
[39] | 28 | ! |
---|
[3] | 29 | ! RCS Log replace by Id keyword, revision history cleaned up |
---|
| 30 | ! |
---|
[1] | 31 | ! Revision 1.41 2006/08/04 14:37:50 raasch |
---|
| 32 | ! Error removed in non-parallel part (sums_l) |
---|
| 33 | ! |
---|
| 34 | ! Revision 1.1 1997/08/11 06:15:17 raasch |
---|
| 35 | ! Initial revision |
---|
| 36 | ! |
---|
| 37 | ! |
---|
| 38 | ! Description: |
---|
| 39 | ! ------------ |
---|
| 40 | ! Compute average profiles and further average flow quantities for the different |
---|
| 41 | ! user-defined (sub-)regions. The region indexed 0 is the total model domain. |
---|
| 42 | ! |
---|
| 43 | ! NOTE: For simplicity, nzb_s_outer and nzb_diff_s_outer are being used as a |
---|
| 44 | ! ---- lower vertical index for k-loops for all variables so that regardless |
---|
| 45 | ! of the variable and its respective staggered grid always the same number of |
---|
| 46 | ! grid points is used for 2D averages. The disadvantage: depending on the |
---|
| 47 | ! variable, up to one grid layer adjacent to the (vertical walls of the) |
---|
| 48 | ! topography is missed out by this simplification. |
---|
| 49 | !------------------------------------------------------------------------------! |
---|
| 50 | |
---|
| 51 | USE arrays_3d |
---|
| 52 | USE cloud_parameters |
---|
| 53 | USE cpulog |
---|
| 54 | USE grid_variables |
---|
| 55 | USE indices |
---|
| 56 | USE interfaces |
---|
| 57 | USE pegrid |
---|
| 58 | USE statistics |
---|
| 59 | USE control_parameters |
---|
| 60 | |
---|
| 61 | IMPLICIT NONE |
---|
| 62 | |
---|
| 63 | INTEGER :: i, j, k, omp_get_thread_num, sr, tn |
---|
| 64 | LOGICAL :: first |
---|
| 65 | REAL :: height, pts, sums_l_eper, sums_l_etot, ust, ust2, u2, vst, & |
---|
| 66 | vst2, v2, w2, z_i(2) |
---|
| 67 | REAL :: sums_ll(nzb:nzt+1,2) |
---|
| 68 | |
---|
| 69 | |
---|
| 70 | CALL cpu_log( log_point(10), 'flow_statistics', 'start' ) |
---|
| 71 | |
---|
| 72 | ! |
---|
| 73 | !-- To be on the safe side, check whether flow_statistics has already been |
---|
| 74 | !-- called once after the current time step |
---|
| 75 | IF ( flow_statistics_called ) THEN |
---|
| 76 | IF ( myid == 0 ) PRINT*, '+++ WARNING: flow_statistics is called two', & |
---|
| 77 | ' times within one timestep' |
---|
| 78 | CALL local_stop |
---|
| 79 | ENDIF |
---|
| 80 | |
---|
| 81 | ! |
---|
| 82 | !-- Compute statistics for each (sub-)region |
---|
| 83 | DO sr = 0, statistic_regions |
---|
| 84 | |
---|
| 85 | ! |
---|
| 86 | !-- Initialize (local) summation array |
---|
| 87 | sums_l = 0.0 |
---|
| 88 | |
---|
| 89 | ! |
---|
| 90 | !-- Store sums that have been computed in other subroutines in summation |
---|
| 91 | !-- array |
---|
| 92 | sums_l(:,11,:) = sums_l_l(:,sr,:) ! mixing length from diffusivities |
---|
| 93 | !-- WARNING: next line still has to be adjusted for OpenMP |
---|
| 94 | sums_l(:,21,0) = sums_wsts_bc_l(:,sr) ! heat flux from advec_s_bc |
---|
[87] | 95 | sums_l(nzb+9,pr_palm,0) = sums_divold_l(sr) ! old divergence from pres |
---|
| 96 | sums_l(nzb+10,pr_palm,0) = sums_divnew_l(sr) ! new divergence from pres |
---|
[1] | 97 | !-- WARNING: next four lines still may have to be adjusted for OpenMP |
---|
[87] | 98 | sums_l(nzb:nzb+2,pr_palm-1,0) = sums_up_fraction_l(1,1:3,sr)! upstream |
---|
| 99 | sums_l(nzb+3:nzb+5,pr_palm-1,0) = sums_up_fraction_l(2,1:3,sr)! parts |
---|
| 100 | sums_l(nzb+6:nzb+8,pr_palm-1,0) = sums_up_fraction_l(3,1:3,sr)! from |
---|
| 101 | sums_l(nzb+9:nzb+11,pr_palm-1,0) = sums_up_fraction_l(4,1:3,sr)! spline |
---|
[1] | 102 | |
---|
| 103 | ! |
---|
| 104 | !-- Horizontally averaged profiles of horizontal velocities and temperature. |
---|
| 105 | !-- They must have been computed before, because they are already required |
---|
| 106 | !-- for other horizontal averages. |
---|
| 107 | tn = 0 |
---|
| 108 | !$OMP PARALLEL PRIVATE( i, j, k, tn ) |
---|
[82] | 109 | #if defined( __intel_openmp_bug ) |
---|
[1] | 110 | tn = omp_get_thread_num() |
---|
| 111 | #else |
---|
| 112 | !$ tn = omp_get_thread_num() |
---|
| 113 | #endif |
---|
| 114 | |
---|
| 115 | !$OMP DO |
---|
| 116 | DO i = nxl, nxr |
---|
| 117 | DO j = nys, nyn |
---|
| 118 | DO k = nzb_s_outer(j,i), nzt+1 |
---|
| 119 | sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr) |
---|
| 120 | sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr) |
---|
| 121 | sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr) |
---|
| 122 | ENDDO |
---|
| 123 | ENDDO |
---|
| 124 | ENDDO |
---|
| 125 | |
---|
| 126 | ! |
---|
| 127 | !-- Horizontally averaged profiles of virtual potential temperature, |
---|
| 128 | !-- total water content, specific humidity and liquid water potential |
---|
| 129 | !-- temperature |
---|
[75] | 130 | IF ( humidity ) THEN |
---|
[1] | 131 | !$OMP DO |
---|
| 132 | DO i = nxl, nxr |
---|
| 133 | DO j = nys, nyn |
---|
| 134 | DO k = nzb_s_outer(j,i), nzt+1 |
---|
| 135 | sums_l(k,44,tn) = sums_l(k,44,tn) + & |
---|
| 136 | vpt(k,j,i) * rmask(j,i,sr) |
---|
| 137 | sums_l(k,41,tn) = sums_l(k,41,tn) + & |
---|
| 138 | q(k,j,i) * rmask(j,i,sr) |
---|
| 139 | ENDDO |
---|
| 140 | ENDDO |
---|
| 141 | ENDDO |
---|
| 142 | IF ( cloud_physics ) THEN |
---|
| 143 | !$OMP DO |
---|
| 144 | DO i = nxl, nxr |
---|
| 145 | DO j = nys, nyn |
---|
| 146 | DO k = nzb_s_outer(j,i), nzt+1 |
---|
| 147 | sums_l(k,42,tn) = sums_l(k,42,tn) + & |
---|
| 148 | ( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr) |
---|
| 149 | sums_l(k,43,tn) = sums_l(k,43,tn) + ( & |
---|
| 150 | pt(k,j,i) + l_d_cp*pt_d_t(k) * ql(k,j,i) & |
---|
| 151 | ) * rmask(j,i,sr) |
---|
| 152 | ENDDO |
---|
| 153 | ENDDO |
---|
| 154 | ENDDO |
---|
| 155 | ENDIF |
---|
| 156 | ENDIF |
---|
| 157 | |
---|
| 158 | ! |
---|
| 159 | !-- Horizontally averaged profiles of passive scalar |
---|
| 160 | IF ( passive_scalar ) THEN |
---|
| 161 | !$OMP DO |
---|
| 162 | DO i = nxl, nxr |
---|
| 163 | DO j = nys, nyn |
---|
| 164 | DO k = nzb_s_outer(j,i), nzt+1 |
---|
| 165 | sums_l(k,41,tn) = sums_l(k,41,tn) + q(k,j,i) * rmask(j,i,sr) |
---|
| 166 | ENDDO |
---|
| 167 | ENDDO |
---|
| 168 | ENDDO |
---|
| 169 | ENDIF |
---|
| 170 | !$OMP END PARALLEL |
---|
| 171 | |
---|
| 172 | ! |
---|
| 173 | !-- Summation of thread sums |
---|
| 174 | IF ( threads_per_task > 1 ) THEN |
---|
| 175 | DO i = 1, threads_per_task-1 |
---|
| 176 | sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i) |
---|
| 177 | sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i) |
---|
| 178 | sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i) |
---|
[75] | 179 | IF ( humidity ) THEN |
---|
[1] | 180 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
---|
| 181 | sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i) |
---|
| 182 | IF ( cloud_physics ) THEN |
---|
| 183 | sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i) |
---|
| 184 | sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i) |
---|
| 185 | ENDIF |
---|
| 186 | ENDIF |
---|
| 187 | IF ( passive_scalar ) THEN |
---|
| 188 | sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i) |
---|
| 189 | ENDIF |
---|
| 190 | ENDDO |
---|
| 191 | ENDIF |
---|
| 192 | |
---|
| 193 | #if defined( __parallel ) |
---|
| 194 | ! |
---|
| 195 | !-- Compute total sum from local sums |
---|
| 196 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), nzt+2-nzb, MPI_REAL, & |
---|
| 197 | MPI_SUM, comm2d, ierr ) |
---|
| 198 | CALL MPI_ALLREDUCE( sums_l(nzb,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, & |
---|
| 199 | MPI_SUM, comm2d, ierr ) |
---|
| 200 | CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, & |
---|
| 201 | MPI_SUM, comm2d, ierr ) |
---|
[75] | 202 | IF ( humidity ) THEN |
---|
[1] | 203 | CALL MPI_ALLREDUCE( sums_l(nzb,44,0), sums(nzb,44), nzt+2-nzb, & |
---|
| 204 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
---|
| 205 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
---|
| 206 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
---|
| 207 | IF ( cloud_physics ) THEN |
---|
| 208 | CALL MPI_ALLREDUCE( sums_l(nzb,42,0), sums(nzb,42), nzt+2-nzb, & |
---|
| 209 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
---|
| 210 | CALL MPI_ALLREDUCE( sums_l(nzb,43,0), sums(nzb,43), nzt+2-nzb, & |
---|
| 211 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
---|
| 212 | ENDIF |
---|
| 213 | ENDIF |
---|
| 214 | |
---|
| 215 | IF ( passive_scalar ) THEN |
---|
| 216 | CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, & |
---|
| 217 | MPI_REAL, MPI_SUM, comm2d, ierr ) |
---|
| 218 | ENDIF |
---|
| 219 | #else |
---|
| 220 | sums(:,1) = sums_l(:,1,0) |
---|
| 221 | sums(:,2) = sums_l(:,2,0) |
---|
| 222 | sums(:,4) = sums_l(:,4,0) |
---|
[75] | 223 | IF ( humidity ) THEN |
---|
[1] | 224 | sums(:,44) = sums_l(:,44,0) |
---|
| 225 | sums(:,41) = sums_l(:,41,0) |
---|
| 226 | IF ( cloud_physics ) THEN |
---|
| 227 | sums(:,42) = sums_l(:,42,0) |
---|
| 228 | sums(:,43) = sums_l(:,43,0) |
---|
| 229 | ENDIF |
---|
| 230 | ENDIF |
---|
| 231 | IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0) |
---|
| 232 | #endif |
---|
| 233 | |
---|
| 234 | ! |
---|
| 235 | !-- Final values are obtained by division by the total number of grid points |
---|
| 236 | !-- used for summation. After that store profiles. |
---|
| 237 | sums(:,1) = sums(:,1) / ngp_2dh_outer(:,sr) |
---|
| 238 | sums(:,2) = sums(:,2) / ngp_2dh_outer(:,sr) |
---|
| 239 | sums(:,4) = sums(:,4) / ngp_2dh_outer(:,sr) |
---|
| 240 | hom(:,1,1,sr) = sums(:,1) ! u |
---|
| 241 | hom(:,1,2,sr) = sums(:,2) ! v |
---|
| 242 | hom(:,1,4,sr) = sums(:,4) ! pt |
---|
| 243 | |
---|
| 244 | ! |
---|
| 245 | !-- Humidity and cloud parameters |
---|
[75] | 246 | IF ( humidity ) THEN |
---|
[1] | 247 | sums(:,44) = sums(:,44) / ngp_2dh_outer(:,sr) |
---|
| 248 | sums(:,41) = sums(:,41) / ngp_2dh_outer(:,sr) |
---|
| 249 | hom(:,1,44,sr) = sums(:,44) ! vpt |
---|
| 250 | hom(:,1,41,sr) = sums(:,41) ! qv (q) |
---|
| 251 | IF ( cloud_physics ) THEN |
---|
| 252 | sums(:,42) = sums(:,42) / ngp_2dh_outer(:,sr) |
---|
| 253 | sums(:,43) = sums(:,43) / ngp_2dh_outer(:,sr) |
---|
| 254 | hom(:,1,42,sr) = sums(:,42) ! qv |
---|
| 255 | hom(:,1,43,sr) = sums(:,43) ! pt |
---|
| 256 | ENDIF |
---|
| 257 | ENDIF |
---|
| 258 | |
---|
| 259 | ! |
---|
| 260 | !-- Passive scalar |
---|
| 261 | IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / ngp_2dh_outer(:,sr) |
---|
| 262 | |
---|
| 263 | ! |
---|
| 264 | !-- Horizontally averaged profiles of the remaining prognostic variables, |
---|
| 265 | !-- variances, the total and the perturbation energy (single values in last |
---|
| 266 | !-- column of sums_l) and some diagnostic quantities. |
---|
| 267 | !-- NOTE: for simplicity, nzb_s_outer is used below, although strictly |
---|
| 268 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 269 | !-- rearranged according to the staggered grid. |
---|
| 270 | tn = 0 |
---|
[82] | 271 | #if defined( __intel_openmp_bug ) |
---|
[1] | 272 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, & |
---|
| 273 | !$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
---|
| 274 | tn = omp_get_thread_num() |
---|
| 275 | #else |
---|
| 276 | !$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, tn, ust, ust2, u2, vst, vst2, v2, w2 ) |
---|
| 277 | !$ tn = omp_get_thread_num() |
---|
| 278 | #endif |
---|
| 279 | !$OMP DO |
---|
| 280 | DO i = nxl, nxr |
---|
| 281 | DO j = nys, nyn |
---|
| 282 | sums_l_etot = 0.0 |
---|
| 283 | sums_l_eper = 0.0 |
---|
| 284 | DO k = nzb_s_outer(j,i), nzt+1 |
---|
| 285 | u2 = u(k,j,i)**2 |
---|
| 286 | v2 = v(k,j,i)**2 |
---|
| 287 | w2 = w(k,j,i)**2 |
---|
| 288 | ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2 |
---|
| 289 | vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2 |
---|
| 290 | ! |
---|
| 291 | !-- Prognostic and diagnostic variables |
---|
| 292 | sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr) |
---|
| 293 | sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr) |
---|
| 294 | sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr) |
---|
| 295 | sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr) |
---|
| 296 | sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i) |
---|
| 297 | |
---|
| 298 | ! |
---|
| 299 | !-- Variances |
---|
| 300 | sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr) |
---|
| 301 | sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr) |
---|
| 302 | sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr) |
---|
| 303 | sums_l(k,33,tn) = sums_l(k,33,tn) + & |
---|
| 304 | ( pt(k,j,i)-hom(k,1,4,sr) )**2 * rmask(j,i,sr) |
---|
| 305 | ! |
---|
| 306 | !-- Higher moments |
---|
| 307 | !-- (Computation of the skewness of w further below) |
---|
| 308 | sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * & |
---|
| 309 | rmask(j,i,sr) |
---|
| 310 | ! |
---|
| 311 | !-- Perturbation energy |
---|
| 312 | sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * ( ust2 + vst2 + w2 ) & |
---|
| 313 | * rmask(j,i,sr) |
---|
| 314 | sums_l_etot = sums_l_etot + & |
---|
| 315 | 0.5 * ( u2 + v2 + w2 ) * rmask(j,i,sr) |
---|
| 316 | sums_l_eper = sums_l_eper + & |
---|
| 317 | 0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr) |
---|
| 318 | ENDDO |
---|
| 319 | ! |
---|
| 320 | !-- Total and perturbation energy for the total domain (being |
---|
| 321 | !-- collected in the last column of sums_l). Summation of these |
---|
| 322 | !-- quantities is seperated from the previous loop in order to |
---|
| 323 | !-- allow vectorization of that loop. |
---|
[87] | 324 | sums_l(nzb+4,pr_palm,tn) = sums_l(nzb+4,pr_palm,tn) + sums_l_etot |
---|
| 325 | sums_l(nzb+5,pr_palm,tn) = sums_l(nzb+5,pr_palm,tn) + sums_l_eper |
---|
[1] | 326 | ! |
---|
| 327 | !-- 2D-arrays (being collected in the last column of sums_l) |
---|
[87] | 328 | sums_l(nzb,pr_palm,tn) = sums_l(nzb,pr_palm,tn) + & |
---|
[1] | 329 | us(j,i) * rmask(j,i,sr) |
---|
[87] | 330 | sums_l(nzb+1,pr_palm,tn) = sums_l(nzb+1,pr_palm,tn) + & |
---|
[1] | 331 | usws(j,i) * rmask(j,i,sr) |
---|
[87] | 332 | sums_l(nzb+2,pr_palm,tn) = sums_l(nzb+2,pr_palm,tn) + & |
---|
[1] | 333 | vsws(j,i) * rmask(j,i,sr) |
---|
[87] | 334 | sums_l(nzb+3,pr_palm,tn) = sums_l(nzb+3,pr_palm,tn) + & |
---|
[1] | 335 | ts(j,i) * rmask(j,i,sr) |
---|
| 336 | ENDDO |
---|
| 337 | ENDDO |
---|
| 338 | |
---|
| 339 | ! |
---|
| 340 | !-- Horizontally averaged profiles of the vertical fluxes |
---|
| 341 | !$OMP DO |
---|
| 342 | DO i = nxl, nxr |
---|
| 343 | DO j = nys, nyn |
---|
| 344 | ! |
---|
| 345 | !-- Subgridscale fluxes (without Prandtl layer from k=nzb, |
---|
| 346 | !-- oterwise from k=nzb+1) |
---|
| 347 | !-- NOTE: for simplicity, nzb_diff_s_outer is used below, although |
---|
| 348 | !-- ---- strictly speaking the following k-loop would have to be |
---|
| 349 | !-- split up according to the staggered grid. |
---|
| 350 | DO k = nzb_diff_s_outer(j,i)-1, nzt |
---|
| 351 | ! |
---|
| 352 | !-- Momentum flux w"u" |
---|
| 353 | sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( & |
---|
| 354 | km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) & |
---|
| 355 | ) * ( & |
---|
| 356 | ( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) & |
---|
| 357 | + ( w(k,j,i) - w(k,j,i-1) ) * ddx & |
---|
| 358 | ) * rmask(j,i,sr) |
---|
| 359 | ! |
---|
| 360 | !-- Momentum flux w"v" |
---|
| 361 | sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( & |
---|
| 362 | km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) & |
---|
| 363 | ) * ( & |
---|
| 364 | ( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) & |
---|
| 365 | + ( w(k,j,i) - w(k,j-1,i) ) * ddy & |
---|
| 366 | ) * rmask(j,i,sr) |
---|
[19] | 367 | ENDDO |
---|
| 368 | |
---|
| 369 | DO k = nzb_diff_s_outer(j,i)-1, nzt_diff |
---|
[1] | 370 | ! |
---|
| 371 | !-- Heat flux w"pt" |
---|
| 372 | sums_l(k,16,tn) = sums_l(k,16,tn) & |
---|
| 373 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 374 | * ( pt(k+1,j,i) - pt(k,j,i) ) & |
---|
| 375 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 376 | |
---|
| 377 | |
---|
| 378 | ! |
---|
| 379 | !-- Buoyancy flux, water flux (humidity flux) w"q" |
---|
[75] | 380 | IF ( humidity ) THEN |
---|
[1] | 381 | sums_l(k,45,tn) = sums_l(k,45,tn) & |
---|
| 382 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 383 | * ( vpt(k+1,j,i) - vpt(k,j,i) ) & |
---|
| 384 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 385 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 386 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 387 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 388 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 389 | IF ( cloud_physics ) THEN |
---|
| 390 | sums_l(k,51,tn) = sums_l(k,51,tn) & |
---|
| 391 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 392 | * ( ( q(k+1,j,i) - ql(k+1,j,i) )& |
---|
| 393 | - ( q(k,j,i) - ql(k,j,i) ) ) & |
---|
| 394 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 395 | ENDIF |
---|
| 396 | ENDIF |
---|
| 397 | |
---|
| 398 | ! |
---|
| 399 | !-- Passive scalar flux |
---|
| 400 | IF ( passive_scalar ) THEN |
---|
| 401 | sums_l(k,48,tn) = sums_l(k,48,tn) & |
---|
| 402 | - 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) & |
---|
| 403 | * ( q(k+1,j,i) - q(k,j,i) ) & |
---|
| 404 | * ddzu(k+1) * rmask(j,i,sr) |
---|
| 405 | ENDIF |
---|
| 406 | |
---|
| 407 | ENDDO |
---|
| 408 | |
---|
| 409 | ! |
---|
| 410 | !-- Subgridscale fluxes in the Prandtl layer |
---|
| 411 | IF ( use_surface_fluxes ) THEN |
---|
| 412 | sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + & |
---|
| 413 | usws(j,i) * rmask(j,i,sr) ! w"u" |
---|
| 414 | sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + & |
---|
| 415 | vsws(j,i) * rmask(j,i,sr) ! w"v" |
---|
| 416 | sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + & |
---|
| 417 | shf(j,i) * rmask(j,i,sr) ! w"pt" |
---|
| 418 | sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + & |
---|
| 419 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
| 420 | sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + & |
---|
| 421 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
[75] | 422 | IF ( humidity ) THEN |
---|
[1] | 423 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 424 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 425 | IF ( cloud_physics ) THEN |
---|
| 426 | sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( & |
---|
| 427 | ( 1.0 + 0.61 * q(nzb,j,i) ) * & |
---|
| 428 | shf(j,i) + 0.61 * pt(nzb,j,i) * & |
---|
| 429 | qsws(j,i) & |
---|
| 430 | ) |
---|
| 431 | ! |
---|
| 432 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 433 | sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv") |
---|
| 434 | qsws(j,i) * rmask(j,i,sr) |
---|
| 435 | ENDIF |
---|
| 436 | ENDIF |
---|
| 437 | IF ( passive_scalar ) THEN |
---|
| 438 | sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + & |
---|
| 439 | qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 440 | ENDIF |
---|
| 441 | ENDIF |
---|
| 442 | |
---|
| 443 | ! |
---|
[19] | 444 | !-- Subgridscale fluxes at the top surface |
---|
| 445 | IF ( use_top_fluxes ) THEN |
---|
| 446 | sums_l(nzt,16,tn) = sums_l(nzt,16,tn) + & |
---|
| 447 | tswst(j,i) * rmask(j,i,sr) ! w"pt" |
---|
| 448 | sums_l(nzt,58,tn) = sums_l(nzt,58,tn) + & |
---|
| 449 | 0.0 * rmask(j,i,sr) ! u"pt" |
---|
| 450 | sums_l(nzt,61,tn) = sums_l(nzt,61,tn) + & |
---|
| 451 | 0.0 * rmask(j,i,sr) ! v"pt" |
---|
[75] | 452 | IF ( humidity ) THEN |
---|
[19] | 453 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
| 454 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 455 | IF ( cloud_physics ) THEN |
---|
| 456 | sums_l(nzt,45,tn) = sums_l(nzt,45,tn) + ( & |
---|
| 457 | ( 1.0 + 0.61 * q(nzt,j,i) ) * & |
---|
| 458 | tswst(j,i) + 0.61 * pt(nzt,j,i) * & |
---|
| 459 | qsws(j,i) & |
---|
| 460 | ) |
---|
| 461 | ! |
---|
| 462 | !-- Formula does not work if ql(nzb) /= 0.0 |
---|
| 463 | sums_l(nzt,51,tn) = sums_l(nzt,51,tn) + & ! w"q" (w"qv") |
---|
| 464 | qswst(j,i) * rmask(j,i,sr) |
---|
| 465 | ENDIF |
---|
| 466 | ENDIF |
---|
| 467 | IF ( passive_scalar ) THEN |
---|
| 468 | sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + & |
---|
| 469 | qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv") |
---|
| 470 | ENDIF |
---|
| 471 | ENDIF |
---|
| 472 | |
---|
| 473 | ! |
---|
[1] | 474 | !-- Resolved fluxes (can be computed for all horizontal points) |
---|
| 475 | !-- NOTE: for simplicity, nzb_s_outer is used below, although strictly |
---|
| 476 | !-- ---- speaking the following k-loop would have to be split up and |
---|
| 477 | !-- rearranged according to the staggered grid. |
---|
| 478 | DO k = nzb_s_outer(j,i), nzt |
---|
| 479 | ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + & |
---|
| 480 | u(k+1,j,i) - hom(k+1,1,1,sr) ) |
---|
| 481 | vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + & |
---|
| 482 | v(k+1,j,i) - hom(k+1,1,2,sr) ) |
---|
| 483 | pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + & |
---|
| 484 | pt(k+1,j,i) - hom(k+1,1,4,sr) ) |
---|
| 485 | ! |
---|
| 486 | !-- Momentum flux w*u* |
---|
| 487 | sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * & |
---|
| 488 | ( w(k,j,i-1) + w(k,j,i) ) & |
---|
| 489 | * ust * rmask(j,i,sr) |
---|
| 490 | ! |
---|
| 491 | !-- Momentum flux w*v* |
---|
| 492 | sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * & |
---|
| 493 | ( w(k,j-1,i) + w(k,j,i) ) & |
---|
| 494 | * vst * rmask(j,i,sr) |
---|
| 495 | ! |
---|
| 496 | !-- Heat flux w*pt* |
---|
| 497 | !-- The following formula (comment line, not executed) does not |
---|
| 498 | !-- work if applied to subregions |
---|
| 499 | ! sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * & |
---|
| 500 | ! ( pt(k,j,i)+pt(k+1,j,i) ) & |
---|
| 501 | ! * w(k,j,i) * rmask(j,i,sr) |
---|
| 502 | sums_l(k,17,tn) = sums_l(k,17,tn) + pts * w(k,j,i) * & |
---|
| 503 | rmask(j,i,sr) |
---|
| 504 | ! |
---|
| 505 | !-- Higher moments |
---|
| 506 | sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)**2 * & |
---|
| 507 | rmask(j,i,sr) |
---|
| 508 | sums_l(k,36,tn) = sums_l(k,36,tn) + pts**2 * w(k,j,i) * & |
---|
| 509 | rmask(j,i,sr) |
---|
| 510 | |
---|
| 511 | ! |
---|
| 512 | !-- Buoyancy flux, water flux, humidity flux and liquid water |
---|
| 513 | !-- content |
---|
[75] | 514 | IF ( humidity ) THEN |
---|
[1] | 515 | pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + & |
---|
| 516 | vpt(k+1,j,i) - hom(k+1,1,44,sr) ) |
---|
| 517 | sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * & |
---|
| 518 | rmask(j,i,sr) |
---|
| 519 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 520 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 521 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 522 | rmask(j,i,sr) |
---|
| 523 | IF ( cloud_physics .OR. cloud_droplets ) THEN |
---|
| 524 | pts = 0.5 * & |
---|
| 525 | ( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) & |
---|
| 526 | + ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) ) |
---|
| 527 | sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * & |
---|
| 528 | rmask(j,i,sr) |
---|
| 529 | sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * & |
---|
| 530 | rmask(j,i,sr) |
---|
| 531 | ENDIF |
---|
| 532 | ENDIF |
---|
| 533 | |
---|
| 534 | ! |
---|
| 535 | !-- Passive scalar flux |
---|
| 536 | IF ( passive_scalar ) THEN |
---|
| 537 | pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + & |
---|
| 538 | q(k+1,j,i) - hom(k+1,1,41,sr) ) |
---|
| 539 | sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * & |
---|
| 540 | rmask(j,i,sr) |
---|
| 541 | ENDIF |
---|
| 542 | |
---|
| 543 | ! |
---|
| 544 | !-- Energy flux w*e* |
---|
| 545 | sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * & |
---|
| 546 | ( ust**2 + vst**2 + w(k,j,i)**2 )& |
---|
| 547 | * rmask(j,i,sr) |
---|
| 548 | |
---|
| 549 | ENDDO |
---|
| 550 | ENDDO |
---|
| 551 | ENDDO |
---|
| 552 | |
---|
| 553 | ! |
---|
| 554 | !-- Divergence of vertical flux of resolved scale energy and pressure |
---|
| 555 | !-- fluctuations. First calculate the products, then the divergence. |
---|
| 556 | !-- Calculation is time consuming. Do it only, if profiles shall be plotted. |
---|
| 557 | IF ( hom(nzb+1,2,55,0) /= 0.0 ) THEN |
---|
| 558 | |
---|
| 559 | sums_ll = 0.0 ! local array |
---|
| 560 | |
---|
| 561 | !$OMP DO |
---|
| 562 | DO i = nxl, nxr |
---|
| 563 | DO j = nys, nyn |
---|
| 564 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 565 | |
---|
| 566 | sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( & |
---|
| 567 | ( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) & |
---|
| 568 | - 2.0 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) & |
---|
| 569 | ) )**2 & |
---|
| 570 | + ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) & |
---|
| 571 | - 2.0 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) & |
---|
| 572 | ) )**2 & |
---|
| 573 | + w(k,j,i)**2 ) |
---|
| 574 | |
---|
| 575 | sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) & |
---|
| 576 | * ( p(k,j,i) + p(k+1,j,i) ) |
---|
| 577 | |
---|
| 578 | ENDDO |
---|
| 579 | ENDDO |
---|
| 580 | ENDDO |
---|
| 581 | sums_ll(0,1) = 0.0 ! because w is zero at the bottom |
---|
| 582 | sums_ll(nzt+1,1) = 0.0 |
---|
| 583 | sums_ll(0,2) = 0.0 |
---|
| 584 | sums_ll(nzt+1,2) = 0.0 |
---|
| 585 | |
---|
| 586 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 587 | sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k) |
---|
| 588 | sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k) |
---|
| 589 | ENDDO |
---|
| 590 | sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn) |
---|
| 591 | sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn) |
---|
| 592 | |
---|
| 593 | ENDIF |
---|
| 594 | |
---|
| 595 | ! |
---|
| 596 | !-- Divergence of vertical flux of SGS TKE |
---|
| 597 | IF ( hom(nzb+1,2,57,0) /= 0.0 ) THEN |
---|
| 598 | |
---|
| 599 | !$OMP DO |
---|
| 600 | DO i = nxl, nxr |
---|
| 601 | DO j = nys, nyn |
---|
| 602 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 603 | |
---|
| 604 | sums_l(k,57,tn) = sums_l(k,57,tn) + ( & |
---|
| 605 | (km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) & |
---|
| 606 | - (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) & |
---|
| 607 | ) * ddzw(k) |
---|
| 608 | |
---|
| 609 | ENDDO |
---|
| 610 | ENDDO |
---|
| 611 | ENDDO |
---|
| 612 | sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn) |
---|
| 613 | |
---|
| 614 | ENDIF |
---|
| 615 | |
---|
| 616 | ! |
---|
| 617 | !-- Horizontal heat fluxes (subgrid, resolved, total). |
---|
| 618 | !-- Do it only, if profiles shall be plotted. |
---|
| 619 | IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN |
---|
| 620 | |
---|
| 621 | !$OMP DO |
---|
| 622 | DO i = nxl, nxr |
---|
| 623 | DO j = nys, nyn |
---|
| 624 | DO k = nzb_s_outer(j,i)+1, nzt |
---|
| 625 | ! |
---|
| 626 | !-- Subgrid horizontal heat fluxes u"pt", v"pt" |
---|
| 627 | sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * & |
---|
| 628 | ( kh(k,j,i) + kh(k,j,i-1) ) & |
---|
| 629 | * ( pt(k,j,i-1) - pt(k,j,i) ) & |
---|
| 630 | * ddx * rmask(j,i,sr) |
---|
| 631 | sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * & |
---|
| 632 | ( kh(k,j,i) + kh(k,j-1,i) ) & |
---|
| 633 | * ( pt(k,j-1,i) - pt(k,j,i) ) & |
---|
| 634 | * ddy * rmask(j,i,sr) |
---|
| 635 | ! |
---|
| 636 | !-- Resolved horizontal heat fluxes u*pt*, v*pt* |
---|
| 637 | sums_l(k,59,tn) = sums_l(k,59,tn) + & |
---|
| 638 | ( u(k,j,i) - hom(k,1,1,sr) ) & |
---|
| 639 | * 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + & |
---|
| 640 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 641 | pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 642 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 643 | sums_l(k,62,tn) = sums_l(k,62,tn) + & |
---|
| 644 | ( v(k,j,i) - hom(k,1,2,sr) ) & |
---|
| 645 | * 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + & |
---|
| 646 | pt(k,j,i) - hom(k,1,4,sr) ) |
---|
| 647 | ENDDO |
---|
| 648 | ENDDO |
---|
| 649 | ENDDO |
---|
| 650 | ! |
---|
| 651 | !-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer) |
---|
| 652 | sums(nzb,58) = 0.0 |
---|
| 653 | sums(nzb,59) = 0.0 |
---|
| 654 | sums(nzb,60) = 0.0 |
---|
| 655 | sums(nzb,61) = 0.0 |
---|
| 656 | sums(nzb,62) = 0.0 |
---|
| 657 | sums(nzb,63) = 0.0 |
---|
| 658 | |
---|
| 659 | ENDIF |
---|
[87] | 660 | |
---|
| 661 | ! |
---|
| 662 | !-- Calculate the user-defined profiles |
---|
| 663 | CALL user_statistics( 'profiles', sr, tn ) |
---|
[1] | 664 | !$OMP END PARALLEL |
---|
| 665 | |
---|
| 666 | ! |
---|
| 667 | !-- Summation of thread sums |
---|
| 668 | IF ( threads_per_task > 1 ) THEN |
---|
| 669 | DO i = 1, threads_per_task-1 |
---|
| 670 | sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i) |
---|
| 671 | sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i) |
---|
[87] | 672 | sums_l(:,45:pr_palm,0) = sums_l(:,45:pr_palm,0) + & |
---|
| 673 | sums_l(:,45:pr_palm,i) |
---|
| 674 | IF ( max_pr_user > 0 ) THEN |
---|
| 675 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) = & |
---|
| 676 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) + & |
---|
| 677 | sums_l(:,pr_palm+1:pr_palm+max_pr_user,i) |
---|
| 678 | ENDIF |
---|
[1] | 679 | ENDDO |
---|
| 680 | ENDIF |
---|
| 681 | |
---|
| 682 | #if defined( __parallel ) |
---|
| 683 | ! |
---|
| 684 | !-- Compute total sum from local sums |
---|
| 685 | CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, & |
---|
| 686 | MPI_SUM, comm2d, ierr ) |
---|
| 687 | #else |
---|
| 688 | sums = sums_l(:,:,0) |
---|
| 689 | #endif |
---|
| 690 | |
---|
| 691 | ! |
---|
| 692 | !-- Final values are obtained by division by the total number of grid points |
---|
| 693 | !-- used for summation. After that store profiles. |
---|
| 694 | !-- Profiles: |
---|
| 695 | DO k = nzb, nzt+1 |
---|
[87] | 696 | sums(k,:pr_palm-2) = sums(k,:pr_palm-2) / ngp_2dh_outer(k,sr) |
---|
[1] | 697 | ENDDO |
---|
| 698 | !-- Upstream-parts |
---|
[87] | 699 | sums(nzb:nzb+11,pr_palm-1) = sums(nzb:nzb+11,pr_palm-1) / ngp_3d(sr) |
---|
[1] | 700 | !-- u* and so on |
---|
[87] | 701 | !-- As sums(nzb:nzb+3,pr_palm) are full 2D arrays (us, usws, vsws, ts) whose |
---|
[1] | 702 | !-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer |
---|
| 703 | !-- above the topography, they are being divided by ngp_2dh(sr) |
---|
[87] | 704 | sums(nzb:nzb+3,pr_palm) = sums(nzb:nzb+3,pr_palm) / & |
---|
[1] | 705 | ngp_2dh(sr) |
---|
| 706 | !-- eges, e* |
---|
[87] | 707 | sums(nzb+4:nzb+5,pr_palm) = sums(nzb+4:nzb+5,pr_palm) / & |
---|
[1] | 708 | ngp_3d_inner(sr) |
---|
| 709 | !-- Old and new divergence |
---|
[87] | 710 | sums(nzb+9:nzb+10,pr_palm) = sums(nzb+9:nzb+10,pr_palm) / & |
---|
[1] | 711 | ngp_3d_inner(sr) |
---|
| 712 | |
---|
[87] | 713 | !-- User-defined profiles |
---|
| 714 | IF ( max_pr_user > 0 ) THEN |
---|
| 715 | DO k = nzb, nzt+1 |
---|
| 716 | sums(k,pr_palm+1:pr_palm+max_pr_user) = & |
---|
| 717 | sums(k,pr_palm+1:pr_palm+max_pr_user) / & |
---|
| 718 | ngp_2dh_outer(k,sr) |
---|
| 719 | ENDDO |
---|
| 720 | ENDIF |
---|
| 721 | |
---|
[1] | 722 | ! |
---|
| 723 | !-- Collect horizontal average in hom. |
---|
| 724 | !-- Compute deduced averages (e.g. total heat flux) |
---|
| 725 | hom(:,1,3,sr) = sums(:,3) ! w |
---|
| 726 | hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles |
---|
| 727 | hom(:,1,9,sr) = sums(:,9) ! km |
---|
| 728 | hom(:,1,10,sr) = sums(:,10) ! kh |
---|
| 729 | hom(:,1,11,sr) = sums(:,11) ! l |
---|
| 730 | hom(:,1,12,sr) = sums(:,12) ! w"u" |
---|
| 731 | hom(:,1,13,sr) = sums(:,13) ! w*u* |
---|
| 732 | hom(:,1,14,sr) = sums(:,14) ! w"v" |
---|
| 733 | hom(:,1,15,sr) = sums(:,15) ! w*v* |
---|
| 734 | hom(:,1,16,sr) = sums(:,16) ! w"pt" |
---|
| 735 | hom(:,1,17,sr) = sums(:,17) ! w*pt* |
---|
| 736 | hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt |
---|
| 737 | hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu |
---|
| 738 | hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv |
---|
| 739 | hom(:,1,21,sr) = sums(:,21) ! w*pt*BC |
---|
| 740 | hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC |
---|
| 741 | ! profiles 23-29 left empty for initial |
---|
| 742 | ! profiles |
---|
| 743 | hom(:,1,30,sr) = sums(:,30) ! u*2 |
---|
| 744 | hom(:,1,31,sr) = sums(:,31) ! v*2 |
---|
| 745 | hom(:,1,32,sr) = sums(:,32) ! w*2 |
---|
| 746 | hom(:,1,33,sr) = sums(:,33) ! pt*2 |
---|
| 747 | hom(:,1,34,sr) = sums(:,34) ! e* |
---|
| 748 | hom(:,1,35,sr) = sums(:,35) ! w*2pt* |
---|
| 749 | hom(:,1,36,sr) = sums(:,36) ! w*pt*2 |
---|
| 750 | hom(:,1,37,sr) = sums(:,37) ! w*e* |
---|
| 751 | hom(:,1,38,sr) = sums(:,38) ! w*3 |
---|
| 752 | hom(:,1,39,sr) = sums(:,38) / ( sums(:,32) + 1E-20 )**1.5 ! Sw |
---|
| 753 | hom(:,1,40,sr) = sums(:,40) ! p |
---|
| 754 | hom(:,1,45,sr) = sums(:,45) ! w"q" |
---|
| 755 | hom(:,1,46,sr) = sums(:,46) ! w*vpt* |
---|
| 756 | hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt |
---|
| 757 | hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv") |
---|
| 758 | hom(:,1,49,sr) = sums(:,49) ! w*q* (w*qv*) |
---|
| 759 | hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv) |
---|
| 760 | hom(:,1,51,sr) = sums(:,51) ! w"qv" |
---|
| 761 | hom(:,1,52,sr) = sums(:,52) ! w*qv* |
---|
| 762 | hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv) |
---|
| 763 | hom(:,1,54,sr) = sums(:,54) ! ql |
---|
| 764 | hom(:,1,55,sr) = sums(:,55) ! w*u*u*/dz |
---|
| 765 | hom(:,1,56,sr) = sums(:,56) ! w*p*/dz |
---|
| 766 | hom(:,1,57,sr) = sums(:,57) ! w"e/dz |
---|
| 767 | hom(:,1,58,sr) = sums(:,58) ! u"pt" |
---|
| 768 | hom(:,1,59,sr) = sums(:,59) ! u*pt* |
---|
| 769 | hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t |
---|
| 770 | hom(:,1,61,sr) = sums(:,61) ! v"pt" |
---|
| 771 | hom(:,1,62,sr) = sums(:,62) ! v*pt* |
---|
| 772 | hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t |
---|
| 773 | |
---|
[87] | 774 | hom(:,1,pr_palm-1,sr) = sums(:,pr_palm-1) |
---|
[1] | 775 | ! upstream-parts u_x, u_y, u_z, v_x, |
---|
| 776 | ! v_y, usw. (in last but one profile) |
---|
[87] | 777 | hom(:,1,pr_palm,sr) = sums(:,pr_palm) |
---|
[1] | 778 | ! u*, w'u', w'v', t* (in last profile) |
---|
| 779 | |
---|
[87] | 780 | IF ( max_pr_user > 0 ) THEN ! user-defined profiles |
---|
| 781 | hom(:,1,pr_palm+1:pr_palm+max_pr_user,sr) = & |
---|
| 782 | sums(:,pr_palm+1:pr_palm+max_pr_user) |
---|
| 783 | ENDIF |
---|
| 784 | |
---|
[1] | 785 | ! |
---|
| 786 | !-- Determine the boundary layer height using two different schemes. |
---|
[94] | 787 | !-- First scheme: Starting from the Earth's (Ocean's) surface, look for the |
---|
| 788 | !-- first relative minimum (maximum) of the total heat flux. |
---|
| 789 | !-- The corresponding height is assumed as the boundary layer height, if it |
---|
| 790 | !-- is less than 1.5 times the height where the heat flux becomes negative |
---|
| 791 | !-- (positive) for the first time. |
---|
[1] | 792 | !-- NOTE: This criterion is still capable of improving! |
---|
| 793 | z_i(1) = 0.0 |
---|
| 794 | first = .TRUE. |
---|
[94] | 795 | ! IF ( .NOT. ocean ) THEN |
---|
| 796 | DO k = nzb, nzt-1 |
---|
| 797 | IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN |
---|
| 798 | first = .FALSE. |
---|
| 799 | height = zw(k) |
---|
[1] | 800 | ENDIF |
---|
[94] | 801 | IF ( hom(k,1,18,sr) < 0.0 .AND. & |
---|
| 802 | hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN |
---|
| 803 | IF ( zw(k) < 1.5 * height ) THEN |
---|
| 804 | z_i(1) = zw(k) |
---|
| 805 | ELSE |
---|
| 806 | z_i(1) = height |
---|
| 807 | ENDIF |
---|
| 808 | EXIT |
---|
| 809 | ENDIF |
---|
| 810 | ENDDO |
---|
| 811 | ! ELSE |
---|
| 812 | ! ENDIF |
---|
[1] | 813 | |
---|
| 814 | ! |
---|
| 815 | !-- Second scheme: Starting from the top model boundary, look for the first |
---|
| 816 | !-- characteristic kink in the temperature profile, where the originally |
---|
| 817 | !-- stable stratification notably weakens. |
---|
| 818 | z_i(2) = 0.0 |
---|
| 819 | DO k = nzt-1, nzb+1, -1 |
---|
| 820 | IF ( ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) > & |
---|
| 821 | 2.0 * ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) ) THEN |
---|
| 822 | z_i(2) = zu(k) |
---|
| 823 | EXIT |
---|
| 824 | ENDIF |
---|
| 825 | ENDDO |
---|
| 826 | |
---|
[87] | 827 | hom(nzb+6,1,pr_palm,sr) = z_i(1) |
---|
| 828 | hom(nzb+7,1,pr_palm,sr) = z_i(2) |
---|
[1] | 829 | |
---|
| 830 | ! |
---|
| 831 | !-- Computation of both the characteristic vertical velocity and |
---|
| 832 | !-- the characteristic convective boundary layer temperature. |
---|
| 833 | !-- The horizontal average at nzb+1 is input for the average temperature. |
---|
| 834 | IF ( hom(nzb,1,18,sr) > 0.0 .AND. z_i(1) /= 0.0 ) THEN |
---|
[87] | 835 | hom(nzb+8,1,pr_palm,sr) = ( g / hom(nzb+1,1,4,sr) * & |
---|
[94] | 836 | hom(nzb,1,18,sr) * & |
---|
| 837 | ABS( z_i(1) ) )**0.333333333 |
---|
[1] | 838 | !-- so far this only works if Prandtl layer is used |
---|
[87] | 839 | hom(nzb+11,1,pr_palm,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,pr_palm,sr) |
---|
[1] | 840 | ELSE |
---|
[87] | 841 | hom(nzb+8,1,pr_palm,sr) = 0.0 |
---|
| 842 | hom(nzb+11,1,pr_palm,sr) = 0.0 |
---|
[1] | 843 | ENDIF |
---|
| 844 | |
---|
[48] | 845 | ! |
---|
| 846 | !-- Collect the time series quantities |
---|
[87] | 847 | ts_value(1,sr) = hom(nzb+4,1,pr_palm,sr) ! E |
---|
| 848 | ts_value(2,sr) = hom(nzb+5,1,pr_palm,sr) ! E* |
---|
[48] | 849 | ts_value(3,sr) = dt_3d |
---|
[87] | 850 | ts_value(4,sr) = hom(nzb,1,pr_palm,sr) ! u* |
---|
| 851 | ts_value(5,sr) = hom(nzb+3,1,pr_palm,sr) ! th* |
---|
[48] | 852 | ts_value(6,sr) = u_max |
---|
| 853 | ts_value(7,sr) = v_max |
---|
| 854 | ts_value(8,sr) = w_max |
---|
[87] | 855 | ts_value(9,sr) = hom(nzb+10,1,pr_palm,sr) ! new divergence |
---|
| 856 | ts_value(10,sr) = hom(nzb+9,1,pr_palm,sr) ! old Divergence |
---|
| 857 | ts_value(11,sr) = hom(nzb+6,1,pr_palm,sr) ! z_i(1) |
---|
| 858 | ts_value(12,sr) = hom(nzb+7,1,pr_palm,sr) ! z_i(2) |
---|
| 859 | ts_value(13,sr) = hom(nzb+8,1,pr_palm,sr) ! w* |
---|
[48] | 860 | ts_value(14,sr) = hom(nzb,1,16,sr) ! w'pt' at k=0 |
---|
| 861 | ts_value(15,sr) = hom(nzb+1,1,16,sr) ! w'pt' at k=1 |
---|
| 862 | ts_value(16,sr) = hom(nzb+1,1,18,sr) ! wpt at k=1 |
---|
| 863 | ts_value(17,sr) = hom(nzb,1,4,sr) ! pt(0) |
---|
| 864 | ts_value(18,sr) = hom(nzb+1,1,4,sr) ! pt(zp) |
---|
[87] | 865 | ts_value(19,sr) = hom(nzb+9,1,pr_palm-1,sr) ! splptx |
---|
| 866 | ts_value(20,sr) = hom(nzb+10,1,pr_palm-1,sr) ! splpty |
---|
| 867 | ts_value(21,sr) = hom(nzb+11,1,pr_palm-1,sr) ! splptz |
---|
[48] | 868 | IF ( ts_value(5,sr) /= 0.0 ) THEN |
---|
| 869 | ts_value(22,sr) = ts_value(4,sr)**2 / & |
---|
| 870 | ( kappa * g * ts_value(5,sr) / ts_value(18,sr) ) ! L |
---|
| 871 | ELSE |
---|
| 872 | ts_value(22,sr) = 10000.0 |
---|
| 873 | ENDIF |
---|
[1] | 874 | |
---|
| 875 | ! |
---|
[48] | 876 | !-- Calculate additional statistics provided by the user interface |
---|
[87] | 877 | CALL user_statistics( 'time_series', sr, 0 ) |
---|
[1] | 878 | |
---|
[48] | 879 | ENDDO ! loop of the subregions |
---|
| 880 | |
---|
[1] | 881 | ! |
---|
| 882 | !-- If required, sum up horizontal averages for subsequent time averaging |
---|
| 883 | IF ( do_sum ) THEN |
---|
| 884 | IF ( average_count_pr == 0 ) hom_sum = 0.0 |
---|
| 885 | hom_sum = hom_sum + hom(:,1,:,:) |
---|
| 886 | average_count_pr = average_count_pr + 1 |
---|
| 887 | do_sum = .FALSE. |
---|
| 888 | ENDIF |
---|
| 889 | |
---|
| 890 | ! |
---|
| 891 | !-- Set flag for other UPs (e.g. output routines, but also buoyancy). |
---|
| 892 | !-- This flag is reset after each time step in time_integration. |
---|
| 893 | flow_statistics_called = .TRUE. |
---|
| 894 | |
---|
| 895 | CALL cpu_log( log_point(10), 'flow_statistics', 'stop' ) |
---|
| 896 | |
---|
| 897 | |
---|
| 898 | END SUBROUTINE flow_statistics |
---|
| 899 | |
---|
| 900 | |
---|
| 901 | |
---|