Home

Context Navigation

source: palm/trunk/SOURCE/flow_statistics.f90 @ 729

Last change on this file since 729 was 710, checked in by raasch, 14 years ago
last commit documented
Property svn:keywords set to `Id`
File size: 51.9 KB

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

Note: See TracBrowser for help on using the repository browser.

Download in other formats:

| Impressum | ©Leibniz Universität Hannover |