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source: palm/trunk/SOURCE/flow_statistics.f90 @ 799

Last change on this file since 799 was 744, checked in by suehring, 13 years ago
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1	SUBROUTINE flow_statistics
2
3	!------------------------------------------------------------------------------!
4	! Current revisions:
5	! -----------------
6	! Calculation of turbulent fluxes with WS-scheme only for the whole model
7	! domain, not for user-defined subregions.
8	!
9	! Former revisions:
10	! -----------------
11	! $Id: flow_statistics.f90 744 2011-08-18 16:12:51Z franke $
12	!
13	! 743 2011-08-18 16:10:16Z suehring
14	! Calculation of turbulent fluxes with WS-scheme only for the whole model
15	! domain, not for user-defined subregions.
16	!
17	! 709 2011-03-30 09:31:40Z raasch
18	! formatting adjustments
19	!
20	! 699 2011-03-22 17:52:22Z suehring
21	! Bugfix in calculation of vertical velocity skewness. The added absolute value
22	! avoid negative values in the root. Negative values of w'w' can occur at the
23	! top or bottom of the model domain due to degrading the order of advection
24	! scheme. Furthermore the calculation will be the same for all advection
25	! schemes.
26	!
27	! 696 2011-03-18 07:03:49Z raasch
28	! Bugfix: Summation of Wicker-Skamarock scheme fluxes and variances for all
29	! threads
30	!
31	! 678 2011-02-02 14:31:56Z raasch
32	! Bugfix in calculation of the divergence of vertical flux of resolved scale
33	! energy, pressure fluctuations, and flux of pressure fluctuation itself
34	!
35	! 673 2011-01-18 16:19:48Z suehring
36	! Top bc for the horizontal velocity variances added for ocean runs.
37	! Setting the corresponding bottom bc moved to advec_ws.
38	!
39	! 667 2010-12-23 12:06:00Z suehring/gryschka
40	! When advection is computed with ws-scheme, turbulent fluxes are already
41	! computed in the respective advection routines and buffered in arrays
42	! sums_xx_ws_l(). This is due to a consistent treatment of statistics with the
43	! numerics and to avoid unphysical kinks near the surface.
44	! So some if requests has to be done to dicern between fluxes from ws-scheme
45	! other advection schemes.
46	! Furthermore the computation of z_i is only done if the heat flux exceeds a
47	! minimum value. This affects only simulations of a neutral boundary layer and
48	! is due to reasons of computations in the advection scheme.
49	!
50	! 624 2010-12-10 11:46:30Z heinze
51	! Calculation of q*2 added
52	!
53	! 622 2010-12-10 08:08:13Z raasch
54	! optional barriers included in order to speed up collective operations
55	!
56	! 388 2009-09-23 09:40:33Z raasch
57	! Vertical profiles of potential density and hydrostatic pressure are
58	! calculated.
59	! Added missing timeseries calculation of w"q"(0), moved timeseries q* to the
60	! end.
61	! Temperature gradient criterion for estimating the boundary layer height
62	! replaced by the gradient criterion of Sullivan et al. (1998).
63	! Output of messages replaced by message handling routine.
64	!
65	! 197 2008-09-16 15:29:03Z raasch
66	! Spline timeseries splptx etc. removed, timeseries w'u', w'v', w'q' (k=0)
67	! added,
68	! bugfix: divide sums(k,8) (e) and sums(k,34) (e*) by ngp_2dh_s_inner(k,sr)
69	! (like other scalars)
70	!
71	! 133 2007-11-20 10:10:53Z letzel
72	! Vertical profiles now based on nzb_s_inner; they are divided by
73	! ngp_2dh_s_inner (scalars, procucts of scalars) and ngp_2dh (staggered
74	! velocity components and their products, procucts of scalars and velocity
75	! components), respectively.
76	!
77	! 106 2007-08-16 14:30:26Z raasch
78	! Prescribed momentum fluxes at the top surface are used,
79	! profiles for wp and w"e are calculated
80	!
81	! 97 2007-06-21 08:23:15Z raasch
82	! Statistics for ocean version (salinity, density) added,
83	! calculation of z_i and Deardorff velocity scale adjusted to be used with
84	! the ocean version
85	!
86	! 87 2007-05-22 15:46:47Z raasch
87	! Two more arguments added to user_statistics, which is now also called for
88	! user-defined profiles,
89	! var_hom and var_sum renamed pr_palm
90	!
91	! 82 2007-04-16 15:40:52Z raasch
92	! Cpp-directive lcmuk changed to intel_openmp_bug
93	!
94	! 75 2007-03-22 09:54:05Z raasch
95	! Collection of time series quantities moved from routine flow_statistics to
96	! here, routine user_statistics is called for each statistic region,
97	! moisture renamed humidity
98	!
99	! 19 2007-02-23 04:53:48Z raasch
100	! fluxes at top modified (tswst, qswst)
101	!
102	! RCS Log replace by Id keyword, revision history cleaned up
103	!
104	! Revision 1.41 2006/08/04 14:37:50 raasch
105	! Error removed in non-parallel part (sums_l)
106	!
107	! Revision 1.1 1997/08/11 06:15:17 raasch
108	! Initial revision
109	!
110	!
111	! Description:
112	! ------------
113	! Compute average profiles and further average flow quantities for the different
114	! user-defined (sub-)regions. The region indexed 0 is the total model domain.
115	!
116	! NOTE: For simplicity, nzb_s_inner and nzb_diff_s_inner are being used as a
117	! ---- lower vertical index for k-loops for all variables, although strictly
118	! speaking the k-loops would have to be split up according to the staggered
119	! grid. However, this implies no error since staggered velocity components are
120	! zero at the walls and inside buildings.
121	!------------------------------------------------------------------------------!
122
123	USE arrays_3d
124	USE cloud_parameters
125	USE control_parameters
126	USE cpulog
127	USE grid_variables
128	USE indices
129	USE interfaces
130	USE pegrid
131	USE statistics
132
133	IMPLICIT NONE
134
135	INTEGER :: i, j, k, omp_get_thread_num, sr, tn
136	LOGICAL :: first
137	REAL :: dptdz_threshold, height, pts, sums_l_eper, sums_l_etot, ust, &
138	ust2, u2, vst, vst2, v2, w2, z_i(2)
139	REAL :: dptdz(nzb+1:nzt+1)
140	REAL :: sums_ll(nzb:nzt+1,2)
141
142	CALL cpu_log( log_point(10), 'flow_statistics', 'start' )
143
144	!
145	!-- To be on the safe side, check whether flow_statistics has already been
146	!-- called once after the current time step
147	IF ( flow_statistics_called ) THEN
148
149	message_string = 'flow_statistics is called two times within one ' // &
150	'timestep'
151	CALL message( 'flow_statistics', 'PA0190', 1, 2, 0, 6, 0 )
152
153	ENDIF
154
155	!
156	!-- Compute statistics for each (sub-)region
157	DO sr = 0, statistic_regions
158
159	!
160	!-- Initialize (local) summation array
161	sums_l = 0.0
162
163	!
164	!-- Store sums that have been computed in other subroutines in summation
165	!-- array
166	sums_l(:,11,:) = sums_l_l(:,sr,:) ! mixing length from diffusivities
167	!-- WARNING: next line still has to be adjusted for OpenMP
168	sums_l(:,21,0) = sums_wsts_bc_l(:,sr) ! heat flux from advec_s_bc
169	sums_l(nzb+9,pr_palm,0) = sums_divold_l(sr) ! old divergence from pres
170	sums_l(nzb+10,pr_palm,0) = sums_divnew_l(sr) ! new divergence from pres
171
172	!
173	!-- Copy the turbulent quantities, evaluated in the advection routines to
174	!-- the local array sums_l() for further computations
175	IF ( ws_scheme_mom .AND. sr == 0 ) THEN
176
177	!
178	!-- According to the Neumann bc for the horizontal velocity components,
179	!-- the corresponding fluxes has to satisfiy the same bc.
180	IF ( ocean ) THEN
181	sums_us2_ws_l(nzt+1) = sums_us2_ws_l(nzt)
182	sums_vs2_ws_l(nzt+1) = sums_vs2_ws_l(nzt)
183	ENDIF
184
185	DO i = 0, threads_per_task-1
186	!
187	!-- Swap the turbulent quantities evaluated in advec_ws.
188	sums_l(:,13,i) = sums_wsus_ws_l(:) ! wu
189	sums_l(:,15,i) = sums_wsvs_ws_l(:) ! wv
190	sums_l(:,30,i) = sums_us2_ws_l(:) ! u*2
191	sums_l(:,31,i) = sums_vs2_ws_l(:) ! v*2
192	sums_l(:,32,i) = sums_ws2_ws_l(:) ! w*2
193	sums_l(:,34,i) = sums_l(:,34,i) + 0.5 * &
194	( sums_us2_ws_l(:) + sums_vs2_ws_l(:) + &
195	sums_ws2_ws_l(:) ) ! e*
196	DO k = nzb, nzt
197	sums_l(nzb+5,pr_palm,i) = sums_l(nzb+5,pr_palm,i) + 0.5 * ( &
198	sums_us2_ws_l(k) + &
199	sums_vs2_ws_l(k) + &
200	sums_ws2_ws_l(k) )
201	ENDDO
202	ENDDO
203
204	ENDIF
205
206	IF ( ws_scheme_sca .AND. sr == 0 ) THEN
207
208	DO i = 0, threads_per_task-1
209	sums_l(:,17,i) = sums_wspts_ws_l(:) ! wpt from advec_s_ws
210	IF ( ocean ) sums_l(:,66,i) = sums_wssas_ws_l(:) ! wsa
211	IF ( humidity .OR. passive_scalar ) sums_l(:,49,i) = &
212	sums_wsqs_ws_l(:) !wq
213	ENDDO
214
215	ENDIF
216	!
217	!-- Horizontally averaged profiles of horizontal velocities and temperature.
218	!-- They must have been computed before, because they are already required
219	!-- for other horizontal averages.
220	tn = 0
221
222	!$OMP PARALLEL PRIVATE( i, j, k, tn )
223	#if defined( __intel_openmp_bug )
224	tn = omp_get_thread_num()
225	#else
226	!$ tn = omp_get_thread_num()
227	#endif
228
229	!$OMP DO
230	DO i = nxl, nxr
231	DO j = nys, nyn
232	DO k = nzb_s_inner(j,i), nzt+1
233	sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr)
234	sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr)
235	sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr)
236	ENDDO
237	ENDDO
238	ENDDO
239
240	!
241	!-- Horizontally averaged profile of salinity
242	IF ( ocean ) THEN
243	!$OMP DO
244	DO i = nxl, nxr
245	DO j = nys, nyn
246	DO k = nzb_s_inner(j,i), nzt+1
247	sums_l(k,23,tn) = sums_l(k,23,tn) + &
248	sa(k,j,i) * rmask(j,i,sr)
249	ENDDO
250	ENDDO
251	ENDDO
252	ENDIF
253
254	!
255	!-- Horizontally averaged profiles of virtual potential temperature,
256	!-- total water content, specific humidity and liquid water potential
257	!-- temperature
258	IF ( humidity ) THEN
259	!$OMP DO
260	DO i = nxl, nxr
261	DO j = nys, nyn
262	DO k = nzb_s_inner(j,i), nzt+1
263	sums_l(k,44,tn) = sums_l(k,44,tn) + &
264	vpt(k,j,i) * rmask(j,i,sr)
265	sums_l(k,41,tn) = sums_l(k,41,tn) + &
266	q(k,j,i) * rmask(j,i,sr)
267	ENDDO
268	ENDDO
269	ENDDO
270	IF ( cloud_physics ) THEN
271	!$OMP DO
272	DO i = nxl, nxr
273	DO j = nys, nyn
274	DO k = nzb_s_inner(j,i), nzt+1
275	sums_l(k,42,tn) = sums_l(k,42,tn) + &
276	( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr)
277	sums_l(k,43,tn) = sums_l(k,43,tn) + ( &
278	pt(k,j,i) + l_d_cppt_d_t(k) ql(k,j,i) &
279	) * rmask(j,i,sr)
280	ENDDO
281	ENDDO
282	ENDDO
283	ENDIF
284	ENDIF
285
286	!
287	!-- Horizontally averaged profiles of passive scalar
288	IF ( passive_scalar ) THEN
289	!$OMP DO
290	DO i = nxl, nxr
291	DO j = nys, nyn
292	DO k = nzb_s_inner(j,i), nzt+1
293	sums_l(k,41,tn) = sums_l(k,41,tn) + q(k,j,i) * rmask(j,i,sr)
294	ENDDO
295	ENDDO
296	ENDDO
297	ENDIF
298	!$OMP END PARALLEL
299	!
300	!-- Summation of thread sums
301	IF ( threads_per_task > 1 ) THEN
302	DO i = 1, threads_per_task-1
303	sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i)
304	sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i)
305	sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i)
306	IF ( ocean ) THEN
307	sums_l(:,23,0) = sums_l(:,23,0) + sums_l(:,23,i)
308	ENDIF
309	IF ( humidity ) THEN
310	sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i)
311	sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i)
312	IF ( cloud_physics ) THEN
313	sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i)
314	sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i)
315	ENDIF
316	ENDIF
317	IF ( passive_scalar ) THEN
318	sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i)
319	ENDIF
320	ENDDO
321	ENDIF
322
323	#if defined( __parallel )
324	!
325	!-- Compute total sum from local sums
326	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
327	CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), nzt+2-nzb, MPI_REAL, &
328	MPI_SUM, comm2d, ierr )
329	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
330	CALL MPI_ALLREDUCE( sums_l(nzb,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, &
331	MPI_SUM, comm2d, ierr )
332	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
333	CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, &
334	MPI_SUM, comm2d, ierr )
335	IF ( ocean ) THEN
336	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
337	CALL MPI_ALLREDUCE( sums_l(nzb,23,0), sums(nzb,23), nzt+2-nzb, &
338	MPI_REAL, MPI_SUM, comm2d, ierr )
339	ENDIF
340	IF ( humidity ) THEN
341	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
342	CALL MPI_ALLREDUCE( sums_l(nzb,44,0), sums(nzb,44), nzt+2-nzb, &
343	MPI_REAL, MPI_SUM, comm2d, ierr )
344	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
345	CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, &
346	MPI_REAL, MPI_SUM, comm2d, ierr )
347	IF ( cloud_physics ) THEN
348	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
349	CALL MPI_ALLREDUCE( sums_l(nzb,42,0), sums(nzb,42), nzt+2-nzb, &
350	MPI_REAL, MPI_SUM, comm2d, ierr )
351	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
352	CALL MPI_ALLREDUCE( sums_l(nzb,43,0), sums(nzb,43), nzt+2-nzb, &
353	MPI_REAL, MPI_SUM, comm2d, ierr )
354	ENDIF
355	ENDIF
356
357	IF ( passive_scalar ) THEN
358	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
359	CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, &
360	MPI_REAL, MPI_SUM, comm2d, ierr )
361	ENDIF
362	#else
363	sums(:,1) = sums_l(:,1,0)
364	sums(:,2) = sums_l(:,2,0)
365	sums(:,4) = sums_l(:,4,0)
366	IF ( ocean ) sums(:,23) = sums_l(:,23,0)
367	IF ( humidity ) THEN
368	sums(:,44) = sums_l(:,44,0)
369	sums(:,41) = sums_l(:,41,0)
370	IF ( cloud_physics ) THEN
371	sums(:,42) = sums_l(:,42,0)
372	sums(:,43) = sums_l(:,43,0)
373	ENDIF
374	ENDIF
375	IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0)
376	#endif
377
378	!
379	!-- Final values are obtained by division by the total number of grid points
380	!-- used for summation. After that store profiles.
381	sums(:,1) = sums(:,1) / ngp_2dh(sr)
382	sums(:,2) = sums(:,2) / ngp_2dh(sr)
383	sums(:,4) = sums(:,4) / ngp_2dh_s_inner(:,sr)
384	hom(:,1,1,sr) = sums(:,1) ! u
385	hom(:,1,2,sr) = sums(:,2) ! v
386	hom(:,1,4,sr) = sums(:,4) ! pt
387
388
389	!
390	!-- Salinity
391	IF ( ocean ) THEN
392	sums(:,23) = sums(:,23) / ngp_2dh_s_inner(:,sr)
393	hom(:,1,23,sr) = sums(:,23) ! sa
394	ENDIF
395
396	!
397	!-- Humidity and cloud parameters
398	IF ( humidity ) THEN
399	sums(:,44) = sums(:,44) / ngp_2dh_s_inner(:,sr)
400	sums(:,41) = sums(:,41) / ngp_2dh_s_inner(:,sr)
401	hom(:,1,44,sr) = sums(:,44) ! vpt
402	hom(:,1,41,sr) = sums(:,41) ! qv (q)
403	IF ( cloud_physics ) THEN
404	sums(:,42) = sums(:,42) / ngp_2dh_s_inner(:,sr)
405	sums(:,43) = sums(:,43) / ngp_2dh_s_inner(:,sr)
406	hom(:,1,42,sr) = sums(:,42) ! qv
407	hom(:,1,43,sr) = sums(:,43) ! pt
408	ENDIF
409	ENDIF
410
411	!
412	!-- Passive scalar
413	IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / &
414	ngp_2dh_s_inner(:,sr) ! s (q)
415
416	!
417	!-- Horizontally averaged profiles of the remaining prognostic variables,
418	!-- variances, the total and the perturbation energy (single values in last
419	!-- column of sums_l) and some diagnostic quantities.
420	!-- NOTE: for simplicity, nzb_s_inner is used below, although strictly
421	!-- ---- speaking the following k-loop would have to be split up and
422	!-- rearranged according to the staggered grid.
423	!-- However, this implies no error since staggered velocity components
424	!-- are zero at the walls and inside buildings.
425	tn = 0
426	#if defined( __intel_openmp_bug )
427	!$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, &
428	!$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 )
429	tn = omp_get_thread_num()
430	#else
431	!$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, tn, ust, ust2, u2, vst, vst2, v2, w2 )
432	!$ tn = omp_get_thread_num()
433	#endif
434	!$OMP DO
435	DO i = nxl, nxr
436	DO j = nys, nyn
437	sums_l_etot = 0.0
438	DO k = nzb_s_inner(j,i), nzt+1
439	!
440	!-- Prognostic and diagnostic variables
441	sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr)
442	sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr)
443	sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr)
444	sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr)
445	sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i)
446
447	sums_l(k,33,tn) = sums_l(k,33,tn) + &
448	( pt(k,j,i)-hom(k,1,4,sr) )*2 rmask(j,i,sr)
449
450	IF ( humidity ) THEN
451	sums_l(k,70,tn) = sums_l(k,70,tn) + &
452	( q(k,j,i)-hom(k,1,41,sr) )*2 rmask(j,i,sr)
453	ENDIF
454
455	!
456	!-- Higher moments
457	!-- (Computation of the skewness of w further below)
458	sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i)*3 rmask(j,i,sr)
459
460	sums_l_etot = sums_l_etot + &
461	0.5 * ( u(k,j,i)2 + v(k,j,i)2 + &
462	w(k,j,i)*2 ) rmask(j,i,sr)
463	ENDDO
464	!
465	!-- Total and perturbation energy for the total domain (being
466	!-- collected in the last column of sums_l). Summation of these
467	!-- quantities is seperated from the previous loop in order to
468	!-- allow vectorization of that loop.
469	sums_l(nzb+4,pr_palm,tn) = sums_l(nzb+4,pr_palm,tn) + sums_l_etot
470	!
471	!-- 2D-arrays (being collected in the last column of sums_l)
472	sums_l(nzb,pr_palm,tn) = sums_l(nzb,pr_palm,tn) + &
473	us(j,i) * rmask(j,i,sr)
474	sums_l(nzb+1,pr_palm,tn) = sums_l(nzb+1,pr_palm,tn) + &
475	usws(j,i) * rmask(j,i,sr)
476	sums_l(nzb+2,pr_palm,tn) = sums_l(nzb+2,pr_palm,tn) + &
477	vsws(j,i) * rmask(j,i,sr)
478	sums_l(nzb+3,pr_palm,tn) = sums_l(nzb+3,pr_palm,tn) + &
479	ts(j,i) * rmask(j,i,sr)
480	IF ( humidity ) THEN
481	sums_l(nzb+12,pr_palm,tn) = sums_l(nzb+12,pr_palm,tn) + &
482	qs(j,i) * rmask(j,i,sr)
483	ENDIF
484	ENDDO
485	ENDDO
486
487	!
488	!-- Computation of statistics when ws-scheme is not used. Else these
489	!-- quantities are evaluated in the advection routines.
490	IF ( .NOT. ws_scheme_mom .OR. sr /= 0 ) THEN
491	!$OMP DO
492	DO i = nxl, nxr
493	DO j = nys, nyn
494	sums_l_eper = 0.0
495	DO k = nzb_s_inner(j,i), nzt+1
496	u2 = u(k,j,i)**2
497	v2 = v(k,j,i)**2
498	w2 = w(k,j,i)**2
499	ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2
500	vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2
501
502	sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr)
503	sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr)
504	sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr)
505	!
506	!-- Perturbation energy
507
508	sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * &
509	( ust2 + vst2 + w2 ) * rmask(j,i,sr)
510	sums_l_eper = sums_l_eper + &
511	0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr)
512
513	ENDDO
514	sums_l(nzb+5,pr_palm,tn) = sums_l(nzb+5,pr_palm,tn) &
515	+ sums_l_eper
516	ENDDO
517	ENDDO
518	ENDIF
519	!
520	!-- Horizontally averaged profiles of the vertical fluxes
521
522	!$OMP DO
523	DO i = nxl, nxr
524	DO j = nys, nyn
525	!
526	!-- Subgridscale fluxes (without Prandtl layer from k=nzb,
527	!-- oterwise from k=nzb+1)
528	!-- NOTE: for simplicity, nzb_diff_s_inner is used below, although
529	!-- ---- strictly speaking the following k-loop would have to be
530	!-- split up according to the staggered grid.
531	!-- However, this implies no error since staggered velocity
532	!-- components are zero at the walls and inside buildings.
533
534	DO k = nzb_diff_s_inner(j,i)-1, nzt_diff
535	!
536	!-- Momentum flux w"u"
537	sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( &
538	km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) &
539	) * ( &
540	( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) &
541	+ ( w(k,j,i) - w(k,j,i-1) ) * ddx &
542	) * rmask(j,i,sr)
543	!
544	!-- Momentum flux w"v"
545	sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( &
546	km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) &
547	) * ( &
548	( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) &
549	+ ( w(k,j,i) - w(k,j-1,i) ) * ddy &
550	) * rmask(j,i,sr)
551	!
552	!-- Heat flux w"pt"
553	sums_l(k,16,tn) = sums_l(k,16,tn) &
554	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
555	* ( pt(k+1,j,i) - pt(k,j,i) ) &
556	* ddzu(k+1) * rmask(j,i,sr)
557
558
559	!
560	!-- Salinity flux w"sa"
561	IF ( ocean ) THEN
562	sums_l(k,65,tn) = sums_l(k,65,tn) &
563	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
564	* ( sa(k+1,j,i) - sa(k,j,i) ) &
565	* ddzu(k+1) * rmask(j,i,sr)
566	ENDIF
567
568	!
569	!-- Buoyancy flux, water flux (humidity flux) w"q"
570	IF ( humidity ) THEN
571	sums_l(k,45,tn) = sums_l(k,45,tn) &
572	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
573	* ( vpt(k+1,j,i) - vpt(k,j,i) ) &
574	* ddzu(k+1) * rmask(j,i,sr)
575	sums_l(k,48,tn) = sums_l(k,48,tn) &
576	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
577	* ( q(k+1,j,i) - q(k,j,i) ) &
578	* ddzu(k+1) * rmask(j,i,sr)
579	IF ( cloud_physics ) THEN
580	sums_l(k,51,tn) = sums_l(k,51,tn) &
581	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
582	* ( ( q(k+1,j,i) - ql(k+1,j,i) )&
583	- ( q(k,j,i) - ql(k,j,i) ) ) &
584	* ddzu(k+1) * rmask(j,i,sr)
585	ENDIF
586	ENDIF
587
588	!
589	!-- Passive scalar flux
590	IF ( passive_scalar ) THEN
591	sums_l(k,48,tn) = sums_l(k,48,tn) &
592	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
593	* ( q(k+1,j,i) - q(k,j,i) ) &
594	* ddzu(k+1) * rmask(j,i,sr)
595	ENDIF
596
597	ENDDO
598
599	!
600	!-- Subgridscale fluxes in the Prandtl layer
601	IF ( use_surface_fluxes ) THEN
602	sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + &
603	usws(j,i) * rmask(j,i,sr) ! w"u"
604	sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + &
605	vsws(j,i) * rmask(j,i,sr) ! w"v"
606	sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + &
607	shf(j,i) * rmask(j,i,sr) ! w"pt"
608	sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + &
609	0.0 * rmask(j,i,sr) ! u"pt"
610	sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + &
611	0.0 * rmask(j,i,sr) ! v"pt"
612	IF ( ocean ) THEN
613	sums_l(nzb,65,tn) = sums_l(nzb,65,tn) + &
614	saswsb(j,i) * rmask(j,i,sr) ! w"sa"
615	ENDIF
616	IF ( humidity ) THEN
617	sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + &
618	qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv")
619	IF ( cloud_physics ) THEN
620	sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( &
621	( 1.0 + 0.61 * q(nzb,j,i) ) * &
622	shf(j,i) + 0.61 * pt(nzb,j,i) * &
623	qsws(j,i) &
624	)
625	!
626	!-- Formula does not work if ql(nzb) /= 0.0
627	sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv")
628	qsws(j,i) * rmask(j,i,sr)
629	ENDIF
630	ENDIF
631	IF ( passive_scalar ) THEN
632	sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + &
633	qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv")
634	ENDIF
635	ENDIF
636
637	!
638	!-- Subgridscale fluxes at the top surface
639	IF ( use_top_fluxes ) THEN
640	sums_l(nzt:nzt+1,12,tn) = sums_l(nzt:nzt+1,12,tn) + &
641	uswst(j,i) * rmask(j,i,sr) ! w"u"
642	sums_l(nzt:nzt+1,14,tn) = sums_l(nzt:nzt+1,14,tn) + &
643	vswst(j,i) * rmask(j,i,sr) ! w"v"
644	sums_l(nzt:nzt+1,16,tn) = sums_l(nzt:nzt+1,16,tn) + &
645	tswst(j,i) * rmask(j,i,sr) ! w"pt"
646	sums_l(nzt:nzt+1,58,tn) = sums_l(nzt:nzt+1,58,tn) + &
647	0.0 * rmask(j,i,sr) ! u"pt"
648	sums_l(nzt:nzt+1,61,tn) = sums_l(nzt:nzt+1,61,tn) + &
649	0.0 * rmask(j,i,sr) ! v"pt"
650
651	IF ( ocean ) THEN
652	sums_l(nzt,65,tn) = sums_l(nzt,65,tn) + &
653	saswst(j,i) * rmask(j,i,sr) ! w"sa"
654	ENDIF
655	IF ( humidity ) THEN
656	sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + &
657	qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv")
658	IF ( cloud_physics ) THEN
659	sums_l(nzt,45,tn) = sums_l(nzt,45,tn) + ( &
660	( 1.0 + 0.61 * q(nzt,j,i) ) * &
661	tswst(j,i) + 0.61 * pt(nzt,j,i) * &
662	qsws(j,i) &
663	)
664	!
665	!-- Formula does not work if ql(nzb) /= 0.0
666	sums_l(nzt,51,tn) = sums_l(nzt,51,tn) + & ! w"q" (w"qv")
667	qswst(j,i) * rmask(j,i,sr)
668	ENDIF
669	ENDIF
670	IF ( passive_scalar ) THEN
671	sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + &
672	qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv")
673	ENDIF
674	ENDIF
675
676	!
677	!-- Resolved fluxes (can be computed for all horizontal points)
678	!-- NOTE: for simplicity, nzb_s_inner is used below, although strictly
679	!-- ---- speaking the following k-loop would have to be split up and
680	!-- rearranged according to the staggered grid.
681	DO k = nzb_s_inner(j,i), nzt
682	ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + &
683	u(k+1,j,i) - hom(k+1,1,1,sr) )
684	vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + &
685	v(k+1,j,i) - hom(k+1,1,2,sr) )
686	pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + &
687	pt(k+1,j,i) - hom(k+1,1,4,sr) )
688
689	!-- Higher moments
690	sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)*2 &
691	rmask(j,i,sr)
692	sums_l(k,36,tn) = sums_l(k,36,tn) + pts*2 w(k,j,i) * &
693	rmask(j,i,sr)
694
695	!
696	!-- Salinity flux and density (density does not belong to here,
697	!-- but so far there is no other suitable place to calculate)
698	IF ( ocean ) THEN
699	IF( .NOT. ws_scheme_sca .OR. sr /= 0 ) THEN
700	pts = 0.5 * ( sa(k,j,i) - hom(k,1,23,sr) + &
701	sa(k+1,j,i) - hom(k+1,1,23,sr) )
702	sums_l(k,66,tn) = sums_l(k,66,tn) + pts * w(k,j,i) * &
703	rmask(j,i,sr)
704	ENDIF
705	sums_l(k,64,tn) = sums_l(k,64,tn) + rho(k,j,i) * &
706	rmask(j,i,sr)
707	sums_l(k,71,tn) = sums_l(k,71,tn) + prho(k,j,i) * &
708	rmask(j,i,sr)
709	ENDIF
710
711	!
712	!-- Buoyancy flux, water flux, humidity flux and liquid water
713	!-- content
714	IF ( humidity ) THEN
715	pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + &
716	vpt(k+1,j,i) - hom(k+1,1,44,sr) )
717	sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * &
718	rmask(j,i,sr)
719
720	IF ( cloud_physics .OR. cloud_droplets ) THEN
721	pts = 0.5 * &
722	( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) &
723	+ ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) )
724	sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * &
725	rmask(j,i,sr)
726	sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * &
727	rmask(j,i,sr)
728	ENDIF
729	ENDIF
730
731	!
732	!-- Passive scalar flux
733	IF ( passive_scalar .AND. ( .NOT. ws_scheme_sca &
734	.OR. sr /= 0 ) ) THEN
735	pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + &
736	q(k+1,j,i) - hom(k+1,1,41,sr) )
737	sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * &
738	rmask(j,i,sr)
739	ENDIF
740
741	!
742	!-- Energy flux we
743	!-- has to be adjusted
744	sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * &
745	( ust2 + vst2 + w(k,j,i)**2 )&
746	* rmask(j,i,sr)
747	ENDDO
748	ENDDO
749	ENDDO
750	!
751	!-- For speed optimization fluxes which have been computed in part directly
752	!-- inside the WS advection routines are treated seperatly
753	!-- Momentum fluxes first:
754	IF ( .NOT. ws_scheme_mom .OR. sr /= 0 ) THEN
755	!$OMP DO
756	DO i = nxl, nxr
757	DO j = nys, nyn
758	DO k = nzb_diff_s_inner(j,i)-1, nzt_diff
759	ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + &
760	u(k+1,j,i) - hom(k+1,1,1,sr) )
761	vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + &
762	v(k+1,j,i) - hom(k+1,1,2,sr) )
763	!
764	!-- Momentum flux wu
765	sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * &
766	( w(k,j,i-1) + w(k,j,i) ) &
767	* ust * rmask(j,i,sr)
768	!
769	!-- Momentum flux wv
770	sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * &
771	( w(k,j-1,i) + w(k,j,i) ) &
772	* vst * rmask(j,i,sr)
773	ENDDO
774	ENDDO
775	ENDDO
776
777	ENDIF
778	IF ( .NOT. ws_scheme_sca .OR. sr /= 0 ) THEN
779	!$OMP DO
780	DO i = nxl, nxr
781	DO j = nys, nyn
782	DO k = nzb_diff_s_inner(j,i)-1, nzt_diff
783	!
784	!-- Vertical heat flux
785	sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * &
786	( pt(k,j,i) - hom(k,1,4,sr) + &
787	pt(k+1,j,i) - hom(k+1,1,4,sr) ) &
788	* w(k,j,i) * rmask(j,i,sr)
789	IF ( humidity ) THEN
790	pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + &
791	q(k+1,j,i) - hom(k+1,1,41,sr) )
792	sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * &
793	rmask(j,i,sr)
794	ENDIF
795	ENDDO
796	ENDDO
797	ENDDO
798
799	ENDIF
800
801
802	!
803	!-- Density at top follows Neumann condition
804	IF ( ocean ) THEN
805	sums_l(nzt+1,64,tn) = sums_l(nzt,64,tn)
806	sums_l(nzt+1,71,tn) = sums_l(nzt,71,tn)
807	ENDIF
808
809	!
810	!-- Divergence of vertical flux of resolved scale energy and pressure
811	!-- fluctuations as well as flux of pressure fluctuation itself (68).
812	!-- First calculate the products, then the divergence.
813	!-- Calculation is time consuming. Do it only, if profiles shall be plotted.
814	IF ( hom(nzb+1,2,55,0) /= 0.0 .OR. hom(nzb+1,2,68,0) /= 0.0 ) THEN
815
816	sums_ll = 0.0 ! local array
817
818	!$OMP DO
819	DO i = nxl, nxr
820	DO j = nys, nyn
821	DO k = nzb_s_inner(j,i)+1, nzt
822
823	sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( &
824	( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) &
825	- 0.5 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) &
826	) )**2 &
827	+ ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) &
828	- 0.5 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) &
829	) )**2 &
830	+ w(k,j,i)**2 )
831
832	sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) &
833	* ( p(k,j,i) + p(k+1,j,i) )
834
835	ENDDO
836	ENDDO
837	ENDDO
838	sums_ll(0,1) = 0.0 ! because w is zero at the bottom
839	sums_ll(nzt+1,1) = 0.0
840	sums_ll(0,2) = 0.0
841	sums_ll(nzt+1,2) = 0.0
842
843	DO k = nzb+1, nzt
844	sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k)
845	sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k)
846	sums_l(k,68,tn) = sums_ll(k,2)
847	ENDDO
848	sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn)
849	sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn)
850	sums_l(nzb,68,tn) = 0.0 ! because w* = 0 at nzb
851
852	ENDIF
853
854	!
855	!-- Divergence of vertical flux of SGS TKE and the flux itself (69)
856	IF ( hom(nzb+1,2,57,0) /= 0.0 .OR. hom(nzb+1,2,69,0) /= 0.0 ) THEN
857
858	!$OMP DO
859	DO i = nxl, nxr
860	DO j = nys, nyn
861	DO k = nzb_s_inner(j,i)+1, nzt
862
863	sums_l(k,57,tn) = sums_l(k,57,tn) - 0.5 * ( &
864	(km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) &
865	- (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) &
866	) * ddzw(k)
867
868	sums_l(k,69,tn) = sums_l(k,69,tn) - 0.5 * ( &
869	(km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) &
870	)
871
872	ENDDO
873	ENDDO
874	ENDDO
875	sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn)
876	sums_l(nzb,69,tn) = sums_l(nzb+1,69,tn)
877
878	ENDIF
879
880	!
881	!-- Horizontal heat fluxes (subgrid, resolved, total).
882	!-- Do it only, if profiles shall be plotted.
883	IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN
884
885	!$OMP DO
886	DO i = nxl, nxr
887	DO j = nys, nyn
888	DO k = nzb_s_inner(j,i)+1, nzt
889	!
890	!-- Subgrid horizontal heat fluxes u"pt", v"pt"
891	sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * &
892	( kh(k,j,i) + kh(k,j,i-1) ) &
893	* ( pt(k,j,i-1) - pt(k,j,i) ) &
894	* ddx * rmask(j,i,sr)
895	sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * &
896	( kh(k,j,i) + kh(k,j-1,i) ) &
897	* ( pt(k,j-1,i) - pt(k,j,i) ) &
898	* ddy * rmask(j,i,sr)
899	!
900	!-- Resolved horizontal heat fluxes upt, vpt
901	sums_l(k,59,tn) = sums_l(k,59,tn) + &
902	( u(k,j,i) - hom(k,1,1,sr) ) &
903	* 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + &
904	pt(k,j,i) - hom(k,1,4,sr) )
905	pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + &
906	pt(k,j,i) - hom(k,1,4,sr) )
907	sums_l(k,62,tn) = sums_l(k,62,tn) + &
908	( v(k,j,i) - hom(k,1,2,sr) ) &
909	* 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + &
910	pt(k,j,i) - hom(k,1,4,sr) )
911	ENDDO
912	ENDDO
913	ENDDO
914	!
915	!-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer)
916	sums_l(nzb,58,tn) = 0.0
917	sums_l(nzb,59,tn) = 0.0
918	sums_l(nzb,60,tn) = 0.0
919	sums_l(nzb,61,tn) = 0.0
920	sums_l(nzb,62,tn) = 0.0
921	sums_l(nzb,63,tn) = 0.0
922
923	ENDIF
924
925	!
926	!-- Calculate the user-defined profiles
927	CALL user_statistics( 'profiles', sr, tn )
928	!$OMP END PARALLEL
929
930	!
931	!-- Summation of thread sums
932	IF ( threads_per_task > 1 ) THEN
933	DO i = 1, threads_per_task-1
934	sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i)
935	sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i)
936	sums_l(:,45:pr_palm,0) = sums_l(:,45:pr_palm,0) + &
937	sums_l(:,45:pr_palm,i)
938	IF ( max_pr_user > 0 ) THEN
939	sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) = &
940	sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) + &
941	sums_l(:,pr_palm+1:pr_palm+max_pr_user,i)
942	ENDIF
943	ENDDO
944	ENDIF
945
946	#if defined( __parallel )
947
948	!
949	!-- Compute total sum from local sums
950	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
951	CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, &
952	MPI_SUM, comm2d, ierr )
953	#else
954	sums = sums_l(:,:,0)
955	#endif
956
957	!
958	!-- Final values are obtained by division by the total number of grid points
959	!-- used for summation. After that store profiles.
960	!-- Profiles:
961	DO k = nzb, nzt+1
962	sums(k,3) = sums(k,3) / ngp_2dh(sr)
963	sums(k,8:11) = sums(k,8:11) / ngp_2dh_s_inner(k,sr)
964	sums(k,12:22) = sums(k,12:22) / ngp_2dh(sr)
965	sums(k,23:29) = sums(k,23:29) / ngp_2dh_s_inner(k,sr)
966	sums(k,30:32) = sums(k,30:32) / ngp_2dh(sr)
967	sums(k,33:34) = sums(k,33:34) / ngp_2dh_s_inner(k,sr)
968	sums(k,35:39) = sums(k,35:39) / ngp_2dh(sr)
969	sums(k,40) = sums(k,40) / ngp_2dh_s_inner(k,sr)
970	sums(k,45:53) = sums(k,45:53) / ngp_2dh(sr)
971	sums(k,54) = sums(k,54) / ngp_2dh_s_inner(k,sr)
972	sums(k,55:63) = sums(k,55:63) / ngp_2dh(sr)
973	sums(k,64) = sums(k,64) / ngp_2dh_s_inner(k,sr)
974	sums(k,65:69) = sums(k,65:69) / ngp_2dh(sr)
975	sums(k,70:pr_palm-2) = sums(k,70:pr_palm-2)/ ngp_2dh_s_inner(k,sr)
976	ENDDO
977
978	!-- Upstream-parts
979	sums(nzb:nzb+11,pr_palm-1) = sums(nzb:nzb+11,pr_palm-1) / ngp_3d(sr)
980	!-- u* and so on
981	!-- As sums(nzb:nzb+3,pr_palm) are full 2D arrays (us, usws, vsws, ts) whose
982	!-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer
983	!-- above the topography, they are being divided by ngp_2dh(sr)
984	sums(nzb:nzb+3,pr_palm) = sums(nzb:nzb+3,pr_palm) / &
985	ngp_2dh(sr)
986	sums(nzb+12,pr_palm) = sums(nzb+12,pr_palm) / & ! qs
987	ngp_2dh(sr)
988	!-- eges, e*
989	sums(nzb+4:nzb+5,pr_palm) = sums(nzb+4:nzb+5,pr_palm) / &
990	ngp_3d(sr)
991	!-- Old and new divergence
992	sums(nzb+9:nzb+10,pr_palm) = sums(nzb+9:nzb+10,pr_palm) / &
993	ngp_3d_inner(sr)
994
995	!-- User-defined profiles
996	IF ( max_pr_user > 0 ) THEN
997	DO k = nzb, nzt+1
998	sums(k,pr_palm+1:pr_palm+max_pr_user) = &
999	sums(k,pr_palm+1:pr_palm+max_pr_user) / &
1000	ngp_2dh_s_inner(k,sr)
1001	ENDDO
1002	ENDIF
1003	!
1004	!-- Collect horizontal average in hom.
1005	!-- Compute deduced averages (e.g. total heat flux)
1006	hom(:,1,3,sr) = sums(:,3) ! w
1007	hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles
1008	hom(:,1,9,sr) = sums(:,9) ! km
1009	hom(:,1,10,sr) = sums(:,10) ! kh
1010	hom(:,1,11,sr) = sums(:,11) ! l
1011	hom(:,1,12,sr) = sums(:,12) ! w"u"
1012	hom(:,1,13,sr) = sums(:,13) ! wu
1013	hom(:,1,14,sr) = sums(:,14) ! w"v"
1014	hom(:,1,15,sr) = sums(:,15) ! wv
1015	hom(:,1,16,sr) = sums(:,16) ! w"pt"
1016	hom(:,1,17,sr) = sums(:,17) ! wpt
1017	hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt
1018	hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu
1019	hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv
1020	hom(:,1,21,sr) = sums(:,21) ! wptBC
1021	hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC
1022	! profile 24 is initial profile (sa)
1023	! profiles 25-29 left empty for initial
1024	! profiles
1025	hom(:,1,30,sr) = sums(:,30) ! u*2
1026	hom(:,1,31,sr) = sums(:,31) ! v*2
1027	hom(:,1,32,sr) = sums(:,32) ! w*2
1028	hom(:,1,33,sr) = sums(:,33) ! pt*2
1029	hom(:,1,34,sr) = sums(:,34) ! e*
1030	hom(:,1,35,sr) = sums(:,35) ! w2pt
1031	hom(:,1,36,sr) = sums(:,36) ! wpt2
1032	hom(:,1,37,sr) = sums(:,37) ! we
1033	hom(:,1,38,sr) = sums(:,38) ! w*3
1034	hom(:,1,39,sr) = sums(:,38) / ( abs( sums(:,32) ) + 1E-20 )**1.5 ! Sw
1035	hom(:,1,40,sr) = sums(:,40) ! p
1036	hom(:,1,45,sr) = sums(:,45) ! w"vpt"
1037	hom(:,1,46,sr) = sums(:,46) ! wvpt
1038	hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt
1039	hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv")
1040	hom(:,1,49,sr) = sums(:,49) ! wq (wqv)
1041	hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv)
1042	hom(:,1,51,sr) = sums(:,51) ! w"qv"
1043	hom(:,1,52,sr) = sums(:,52) ! wqv
1044	hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv)
1045	hom(:,1,54,sr) = sums(:,54) ! ql
1046	hom(:,1,55,sr) = sums(:,55) ! wuu*/dz
1047	hom(:,1,56,sr) = sums(:,56) ! wp/dz
1048	hom(:,1,57,sr) = sums(:,57) ! ( w"e + w"p"/rho )/dz
1049	hom(:,1,58,sr) = sums(:,58) ! u"pt"
1050	hom(:,1,59,sr) = sums(:,59) ! upt
1051	hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t
1052	hom(:,1,61,sr) = sums(:,61) ! v"pt"
1053	hom(:,1,62,sr) = sums(:,62) ! vpt
1054	hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t
1055	hom(:,1,64,sr) = sums(:,64) ! rho
1056	hom(:,1,65,sr) = sums(:,65) ! w"sa"
1057	hom(:,1,66,sr) = sums(:,66) ! wsa
1058	hom(:,1,67,sr) = sums(:,65) + sums(:,66) ! wsa
1059	hom(:,1,68,sr) = sums(:,68) ! wp
1060	hom(:,1,69,sr) = sums(:,69) ! w"e + w"p"/rho
1061	hom(:,1,70,sr) = sums(:,70) ! q*2
1062	hom(:,1,71,sr) = sums(:,71) ! prho
1063	hom(:,1,72,sr) = hyp * 1E-4 ! hyp in dbar
1064
1065	hom(:,1,pr_palm-1,sr) = sums(:,pr_palm-1)
1066	! upstream-parts u_x, u_y, u_z, v_x,
1067	! v_y, usw. (in last but one profile)
1068	hom(:,1,pr_palm,sr) = sums(:,pr_palm)
1069	! u, w'u', w'v', t (in last profile)
1070
1071	IF ( max_pr_user > 0 ) THEN ! user-defined profiles
1072	hom(:,1,pr_palm+1:pr_palm+max_pr_user,sr) = &
1073	sums(:,pr_palm+1:pr_palm+max_pr_user)
1074	ENDIF
1075
1076	!
1077	!-- Determine the boundary layer height using two different schemes.
1078	!-- First scheme: Starting from the Earth's (Ocean's) surface, look for the
1079	!-- first relative minimum (maximum) of the total heat flux.
1080	!-- The corresponding height is assumed as the boundary layer height, if it
1081	!-- is less than 1.5 times the height where the heat flux becomes negative
1082	!-- (positive) for the first time.
1083	z_i(1) = 0.0
1084	first = .TRUE.
1085
1086	IF ( ocean ) THEN
1087	DO k = nzt, nzb+1, -1
1088	IF ( first .AND. hom(k,1,18,sr) < 0.0 &
1089	.AND. abs(hom(k,1,18,sr)) > 1.0E-8) THEN
1090	first = .FALSE.
1091	height = zw(k)
1092	ENDIF
1093	IF ( hom(k,1,18,sr) < 0.0 .AND. &
1094	abs(hom(k,1,18,sr)) > 1.0E-8 .AND. &
1095	hom(k-1,1,18,sr) > hom(k,1,18,sr) ) THEN
1096	IF ( zw(k) < 1.5 * height ) THEN
1097	z_i(1) = zw(k)
1098	ELSE
1099	z_i(1) = height
1100	ENDIF
1101	EXIT
1102	ENDIF
1103	ENDDO
1104	ELSE
1105	DO k = nzb, nzt-1
1106	IF ( first .AND. hom(k,1,18,sr) < 0.0 &
1107	.AND. abs(hom(k,1,18,sr)) > 1.0E-8 ) THEN
1108	first = .FALSE.
1109	height = zw(k)
1110	ENDIF
1111	IF ( hom(k,1,18,sr) < 0.0 .AND. &
1112	abs(hom(k,1,18,sr)) > 1.0E-8 .AND. &
1113	hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN
1114	IF ( zw(k) < 1.5 * height ) THEN
1115	z_i(1) = zw(k)
1116	ELSE
1117	z_i(1) = height
1118	ENDIF
1119	EXIT
1120	ENDIF
1121	ENDDO
1122	ENDIF
1123
1124	!
1125	!-- Second scheme: Gradient scheme from Sullivan et al. (1998), modified
1126	!-- by Uhlenbrock(2006). The boundary layer height is the height with the
1127	!-- maximal local temperature gradient: starting from the second (the last
1128	!-- but one) vertical gridpoint, the local gradient must be at least
1129	!-- 0.2K/100m and greater than the next four gradients.
1130	!-- WARNING: The threshold value of 0.2K/100m must be adjusted for the
1131	!-- ocean case!
1132	z_i(2) = 0.0
1133	DO k = nzb+1, nzt+1
1134	dptdz(k) = ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) * ddzu(k)
1135	ENDDO
1136	dptdz_threshold = 0.2 / 100.0
1137
1138	IF ( ocean ) THEN
1139	DO k = nzt+1, nzb+5, -1
1140	IF ( dptdz(k) > dptdz_threshold .AND. &
1141	dptdz(k) > dptdz(k-1) .AND. dptdz(k) > dptdz(k-2) .AND. &
1142	dptdz(k) > dptdz(k-3) .AND. dptdz(k) > dptdz(k-4) ) THEN
1143	z_i(2) = zw(k-1)
1144	EXIT
1145	ENDIF
1146	ENDDO
1147	ELSE
1148	DO k = nzb+1, nzt-3
1149	IF ( dptdz(k) > dptdz_threshold .AND. &
1150	dptdz(k) > dptdz(k+1) .AND. dptdz(k) > dptdz(k+2) .AND. &
1151	dptdz(k) > dptdz(k+3) .AND. dptdz(k) > dptdz(k+4) ) THEN
1152	z_i(2) = zw(k-1)
1153	EXIT
1154	ENDIF
1155	ENDDO
1156	ENDIF
1157
1158	hom(nzb+6,1,pr_palm,sr) = z_i(1)
1159	hom(nzb+7,1,pr_palm,sr) = z_i(2)
1160
1161	!
1162	!-- Computation of both the characteristic vertical velocity and
1163	!-- the characteristic convective boundary layer temperature.
1164	!-- The horizontal average at nzb+1 is input for the average temperature.
1165	IF ( hom(nzb,1,18,sr) > 0.0 .AND. abs(hom(nzb,1,18,sr)) > 1.0E-8 &
1166	.AND. z_i(1) /= 0.0 ) THEN
1167	hom(nzb+8,1,pr_palm,sr) = ( g / hom(nzb+1,1,4,sr) * &
1168	hom(nzb,1,18,sr) * &
1169	ABS( z_i(1) ) )**0.333333333
1170	!-- so far this only works if Prandtl layer is used
1171	hom(nzb+11,1,pr_palm,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,pr_palm,sr)
1172	ELSE
1173	hom(nzb+8,1,pr_palm,sr) = 0.0
1174	hom(nzb+11,1,pr_palm,sr) = 0.0
1175	ENDIF
1176
1177	!
1178	!-- Collect the time series quantities
1179	ts_value(1,sr) = hom(nzb+4,1,pr_palm,sr) ! E
1180	ts_value(2,sr) = hom(nzb+5,1,pr_palm,sr) ! E*
1181	ts_value(3,sr) = dt_3d
1182	ts_value(4,sr) = hom(nzb,1,pr_palm,sr) ! u*
1183	ts_value(5,sr) = hom(nzb+3,1,pr_palm,sr) ! th*
1184	ts_value(6,sr) = u_max
1185	ts_value(7,sr) = v_max
1186	ts_value(8,sr) = w_max
1187	ts_value(9,sr) = hom(nzb+10,1,pr_palm,sr) ! new divergence
1188	ts_value(10,sr) = hom(nzb+9,1,pr_palm,sr) ! old Divergence
1189	ts_value(11,sr) = hom(nzb+6,1,pr_palm,sr) ! z_i(1)
1190	ts_value(12,sr) = hom(nzb+7,1,pr_palm,sr) ! z_i(2)
1191	ts_value(13,sr) = hom(nzb+8,1,pr_palm,sr) ! w*
1192	ts_value(14,sr) = hom(nzb,1,16,sr) ! w'pt' at k=0
1193	ts_value(15,sr) = hom(nzb+1,1,16,sr) ! w'pt' at k=1
1194	ts_value(16,sr) = hom(nzb+1,1,18,sr) ! wpt at k=1
1195	ts_value(17,sr) = hom(nzb,1,4,sr) ! pt(0)
1196	ts_value(18,sr) = hom(nzb+1,1,4,sr) ! pt(zp)
1197	ts_value(19,sr) = hom(nzb+1,1,pr_palm,sr) ! u'w' at k=0
1198	ts_value(20,sr) = hom(nzb+2,1,pr_palm,sr) ! v'w' at k=0
1199	ts_value(21,sr) = hom(nzb,1,48,sr) ! w"q" at k=0
1200
1201	IF ( ts_value(5,sr) /= 0.0 ) THEN
1202	ts_value(22,sr) = ts_value(4,sr)**2 / &
1203	( kappa * g * ts_value(5,sr) / ts_value(18,sr) ) ! L
1204	ELSE
1205	ts_value(22,sr) = 10000.0
1206	ENDIF
1207
1208	ts_value(23,sr) = hom(nzb+12,1,pr_palm,sr) ! q*
1209	!
1210	!-- Calculate additional statistics provided by the user interface
1211	CALL user_statistics( 'time_series', sr, 0 )
1212
1213	ENDDO ! loop of the subregions
1214
1215	!
1216	!-- If required, sum up horizontal averages for subsequent time averaging
1217	IF ( do_sum ) THEN
1218	IF ( average_count_pr == 0 ) hom_sum = 0.0
1219	hom_sum = hom_sum + hom(:,1,:,:)
1220	average_count_pr = average_count_pr + 1
1221	do_sum = .FALSE.
1222	ENDIF
1223
1224	!
1225	!-- Set flag for other UPs (e.g. output routines, but also buoyancy).
1226	!-- This flag is reset after each time step in time_integration.
1227	flow_statistics_called = .TRUE.
1228
1229	CALL cpu_log( log_point(10), 'flow_statistics', 'stop' )
1230
1231
1232	END SUBROUTINE flow_statistics

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