Home

Context Navigation

source: palm/trunk/SOURCE/flow_statistics.f90 @ 197

Last change on this file since 197 was 197, checked in by raasch, 16 years ago
further adjustments for SGI and other small changes
Property svn:keywords set to `Id`
File size: 44.4 KB

Rev	Line
[1]	1	SUBROUTINE flow_statistics
	2
	3	!------------------------------------------------------------------------------!
	4	! Actual revisions:
	5	! -----------------
[197]	6	! Spline timeseries splptx etc. removed, timeseries w'u', w'v', w'q' (k=0)
	7	! added
[142]	8	! Bugfix: divide sums(k,8) (e) and sums(k,34) (e*) by ngp_2dh_s_inner(k,sr)
	9	! (like other scalars)
[1]	10	!
	11	! Former revisions:
	12	! -----------------
[3]	13	! $Id: flow_statistics.f90 197 2008-09-16 15:29:03Z raasch $
[39]	14	!
[139]	15	! 133 2007-11-20 10:10:53Z letzel
	16	! Vertical profiles now based on nzb_s_inner; they are divided by
	17	! ngp_2dh_s_inner (scalars, procucts of scalars) and ngp_2dh (staggered
	18	! velocity components and their products, procucts of scalars and velocity
	19	! components), respectively.
	20	!
[110]	21	! 106 2007-08-16 14:30:26Z raasch
	22	! Prescribed momentum fluxes at the top surface are used,
	23	! profiles for wp and w"e are calculated
	24	!
[98]	25	! 97 2007-06-21 08:23:15Z raasch
	26	! Statistics for ocean version (salinity, density) added,
	27	! calculation of z_i and Deardorff velocity scale adjusted to be used with
	28	! the ocean version
	29	!
[90]	30	! 87 2007-05-22 15:46:47Z raasch
	31	! Two more arguments added to user_statistics, which is now also called for
	32	! user-defined profiles,
	33	! var_hom and var_sum renamed pr_palm
	34	!
[83]	35	! 82 2007-04-16 15:40:52Z raasch
	36	! Cpp-directive lcmuk changed to intel_openmp_bug
	37	!
[77]	38	! 75 2007-03-22 09:54:05Z raasch
	39	! Collection of time series quantities moved from routine flow_statistics to
	40	! here, routine user_statistics is called for each statistic region,
	41	! moisture renamed humidity
	42	!
[39]	43	! 19 2007-02-23 04:53:48Z raasch
[77]	44	! fluxes at top modified (tswst, qswst)
[39]	45	!
[3]	46	! RCS Log replace by Id keyword, revision history cleaned up
	47	!
[1]	48	! Revision 1.41 2006/08/04 14:37:50 raasch
	49	! Error removed in non-parallel part (sums_l)
	50	!
	51	! Revision 1.1 1997/08/11 06:15:17 raasch
	52	! Initial revision
	53	!
	54	!
	55	! Description:
	56	! ------------
	57	! Compute average profiles and further average flow quantities for the different
	58	! user-defined (sub-)regions. The region indexed 0 is the total model domain.
	59	!
[132]	60	! NOTE: For simplicity, nzb_s_inner and nzb_diff_s_inner are being used as a
	61	! ---- lower vertical index for k-loops for all variables, although strictly
	62	! speaking the k-loops would have to be split up according to the staggered
	63	! grid. However, this implies no error since staggered velocity components are
	64	! zero at the walls and inside buildings.
[1]	65	!------------------------------------------------------------------------------!
	66
	67	USE arrays_3d
	68	USE cloud_parameters
	69	USE cpulog
	70	USE grid_variables
	71	USE indices
	72	USE interfaces
	73	USE pegrid
	74	USE statistics
	75	USE control_parameters
	76
	77	IMPLICIT NONE
	78
	79	INTEGER :: i, j, k, omp_get_thread_num, sr, tn
	80	LOGICAL :: first
	81	REAL :: height, pts, sums_l_eper, sums_l_etot, ust, ust2, u2, vst, &
	82	vst2, v2, w2, z_i(2)
	83	REAL :: sums_ll(nzb:nzt+1,2)
	84
	85
	86	CALL cpu_log( log_point(10), 'flow_statistics', 'start' )
	87
	88	!
	89	!-- To be on the safe side, check whether flow_statistics has already been
	90	!-- called once after the current time step
	91	IF ( flow_statistics_called ) THEN
	92	IF ( myid == 0 ) PRINT*, '+++ WARNING: flow_statistics is called two', &
	93	' times within one timestep'
	94	CALL local_stop
	95	ENDIF
	96
	97	!
	98	!-- Compute statistics for each (sub-)region
	99	DO sr = 0, statistic_regions
	100
	101	!
	102	!-- Initialize (local) summation array
	103	sums_l = 0.0
	104
	105	!
	106	!-- Store sums that have been computed in other subroutines in summation
	107	!-- array
	108	sums_l(:,11,:) = sums_l_l(:,sr,:) ! mixing length from diffusivities
	109	!-- WARNING: next line still has to be adjusted for OpenMP
	110	sums_l(:,21,0) = sums_wsts_bc_l(:,sr) ! heat flux from advec_s_bc
[87]	111	sums_l(nzb+9,pr_palm,0) = sums_divold_l(sr) ! old divergence from pres
	112	sums_l(nzb+10,pr_palm,0) = sums_divnew_l(sr) ! new divergence from pres
[1]	113
	114	!
	115	!-- Horizontally averaged profiles of horizontal velocities and temperature.
	116	!-- They must have been computed before, because they are already required
	117	!-- for other horizontal averages.
	118	tn = 0
	119	!$OMP PARALLEL PRIVATE( i, j, k, tn )
[82]	120	#if defined( __intel_openmp_bug )
[1]	121	tn = omp_get_thread_num()
	122	#else
	123	!$ tn = omp_get_thread_num()
	124	#endif
	125
	126	!$OMP DO
	127	DO i = nxl, nxr
	128	DO j = nys, nyn
[132]	129	DO k = nzb_s_inner(j,i), nzt+1
[1]	130	sums_l(k,1,tn) = sums_l(k,1,tn) + u(k,j,i) * rmask(j,i,sr)
	131	sums_l(k,2,tn) = sums_l(k,2,tn) + v(k,j,i) * rmask(j,i,sr)
	132	sums_l(k,4,tn) = sums_l(k,4,tn) + pt(k,j,i) * rmask(j,i,sr)
	133	ENDDO
	134	ENDDO
	135	ENDDO
	136
	137	!
[96]	138	!-- Horizontally averaged profile of salinity
	139	IF ( ocean ) THEN
	140	!$OMP DO
	141	DO i = nxl, nxr
	142	DO j = nys, nyn
[132]	143	DO k = nzb_s_inner(j,i), nzt+1
[96]	144	sums_l(k,23,tn) = sums_l(k,23,tn) + &
	145	sa(k,j,i) * rmask(j,i,sr)
	146	ENDDO
	147	ENDDO
	148	ENDDO
	149	ENDIF
	150
	151	!
[1]	152	!-- Horizontally averaged profiles of virtual potential temperature,
	153	!-- total water content, specific humidity and liquid water potential
	154	!-- temperature
[75]	155	IF ( humidity ) THEN
[1]	156	!$OMP DO
	157	DO i = nxl, nxr
	158	DO j = nys, nyn
[132]	159	DO k = nzb_s_inner(j,i), nzt+1
[1]	160	sums_l(k,44,tn) = sums_l(k,44,tn) + &
	161	vpt(k,j,i) * rmask(j,i,sr)
	162	sums_l(k,41,tn) = sums_l(k,41,tn) + &
	163	q(k,j,i) * rmask(j,i,sr)
	164	ENDDO
	165	ENDDO
	166	ENDDO
	167	IF ( cloud_physics ) THEN
	168	!$OMP DO
	169	DO i = nxl, nxr
	170	DO j = nys, nyn
[132]	171	DO k = nzb_s_inner(j,i), nzt+1
[1]	172	sums_l(k,42,tn) = sums_l(k,42,tn) + &
	173	( q(k,j,i) - ql(k,j,i) ) * rmask(j,i,sr)
	174	sums_l(k,43,tn) = sums_l(k,43,tn) + ( &
	175	pt(k,j,i) + l_d_cppt_d_t(k) ql(k,j,i) &
	176	) * rmask(j,i,sr)
	177	ENDDO
	178	ENDDO
	179	ENDDO
	180	ENDIF
	181	ENDIF
	182
	183	!
	184	!-- Horizontally averaged profiles of passive scalar
	185	IF ( passive_scalar ) THEN
	186	!$OMP DO
	187	DO i = nxl, nxr
	188	DO j = nys, nyn
[132]	189	DO k = nzb_s_inner(j,i), nzt+1
[1]	190	sums_l(k,41,tn) = sums_l(k,41,tn) + q(k,j,i) * rmask(j,i,sr)
	191	ENDDO
	192	ENDDO
	193	ENDDO
	194	ENDIF
	195	!$OMP END PARALLEL
	196
	197	!
	198	!-- Summation of thread sums
	199	IF ( threads_per_task > 1 ) THEN
	200	DO i = 1, threads_per_task-1
	201	sums_l(:,1,0) = sums_l(:,1,0) + sums_l(:,1,i)
	202	sums_l(:,2,0) = sums_l(:,2,0) + sums_l(:,2,i)
	203	sums_l(:,4,0) = sums_l(:,4,0) + sums_l(:,4,i)
[96]	204	IF ( ocean ) THEN
	205	sums_l(:,23,0) = sums_l(:,23,0) + sums_l(:,23,i)
	206	ENDIF
[75]	207	IF ( humidity ) THEN
[1]	208	sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i)
	209	sums_l(:,44,0) = sums_l(:,44,0) + sums_l(:,44,i)
	210	IF ( cloud_physics ) THEN
	211	sums_l(:,42,0) = sums_l(:,42,0) + sums_l(:,42,i)
	212	sums_l(:,43,0) = sums_l(:,43,0) + sums_l(:,43,i)
	213	ENDIF
	214	ENDIF
	215	IF ( passive_scalar ) THEN
	216	sums_l(:,41,0) = sums_l(:,41,0) + sums_l(:,41,i)
	217	ENDIF
	218	ENDDO
	219	ENDIF
	220
	221	#if defined( __parallel )
	222	!
	223	!-- Compute total sum from local sums
	224	CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), nzt+2-nzb, MPI_REAL, &
	225	MPI_SUM, comm2d, ierr )
	226	CALL MPI_ALLREDUCE( sums_l(nzb,2,0), sums(nzb,2), nzt+2-nzb, MPI_REAL, &
	227	MPI_SUM, comm2d, ierr )
	228	CALL MPI_ALLREDUCE( sums_l(nzb,4,0), sums(nzb,4), nzt+2-nzb, MPI_REAL, &
	229	MPI_SUM, comm2d, ierr )
[96]	230	IF ( ocean ) THEN
	231	CALL MPI_ALLREDUCE( sums_l(nzb,23,0), sums(nzb,23), nzt+2-nzb, &
	232	MPI_REAL, MPI_SUM, comm2d, ierr )
	233	ENDIF
[75]	234	IF ( humidity ) THEN
[1]	235	CALL MPI_ALLREDUCE( sums_l(nzb,44,0), sums(nzb,44), nzt+2-nzb, &
	236	MPI_REAL, MPI_SUM, comm2d, ierr )
	237	CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, &
	238	MPI_REAL, MPI_SUM, comm2d, ierr )
	239	IF ( cloud_physics ) THEN
	240	CALL MPI_ALLREDUCE( sums_l(nzb,42,0), sums(nzb,42), nzt+2-nzb, &
	241	MPI_REAL, MPI_SUM, comm2d, ierr )
	242	CALL MPI_ALLREDUCE( sums_l(nzb,43,0), sums(nzb,43), nzt+2-nzb, &
	243	MPI_REAL, MPI_SUM, comm2d, ierr )
	244	ENDIF
	245	ENDIF
	246
	247	IF ( passive_scalar ) THEN
	248	CALL MPI_ALLREDUCE( sums_l(nzb,41,0), sums(nzb,41), nzt+2-nzb, &
	249	MPI_REAL, MPI_SUM, comm2d, ierr )
	250	ENDIF
	251	#else
	252	sums(:,1) = sums_l(:,1,0)
	253	sums(:,2) = sums_l(:,2,0)
	254	sums(:,4) = sums_l(:,4,0)
[96]	255	IF ( ocean ) sums(:,23) = sums_l(:,23,0)
[75]	256	IF ( humidity ) THEN
[1]	257	sums(:,44) = sums_l(:,44,0)
	258	sums(:,41) = sums_l(:,41,0)
	259	IF ( cloud_physics ) THEN
	260	sums(:,42) = sums_l(:,42,0)
	261	sums(:,43) = sums_l(:,43,0)
	262	ENDIF
	263	ENDIF
	264	IF ( passive_scalar ) sums(:,41) = sums_l(:,41,0)
	265	#endif
	266
	267	!
	268	!-- Final values are obtained by division by the total number of grid points
	269	!-- used for summation. After that store profiles.
[132]	270	sums(:,1) = sums(:,1) / ngp_2dh(sr)
	271	sums(:,2) = sums(:,2) / ngp_2dh(sr)
	272	sums(:,4) = sums(:,4) / ngp_2dh_s_inner(:,sr)
[1]	273	hom(:,1,1,sr) = sums(:,1) ! u
	274	hom(:,1,2,sr) = sums(:,2) ! v
	275	hom(:,1,4,sr) = sums(:,4) ! pt
	276
	277	!
[96]	278	!-- Salinity
	279	IF ( ocean ) THEN
[132]	280	sums(:,23) = sums(:,23) / ngp_2dh_s_inner(:,sr)
[96]	281	hom(:,1,23,sr) = sums(:,23) ! sa
	282	ENDIF
	283
	284	!
[1]	285	!-- Humidity and cloud parameters
[75]	286	IF ( humidity ) THEN
[132]	287	sums(:,44) = sums(:,44) / ngp_2dh_s_inner(:,sr)
	288	sums(:,41) = sums(:,41) / ngp_2dh_s_inner(:,sr)
[1]	289	hom(:,1,44,sr) = sums(:,44) ! vpt
	290	hom(:,1,41,sr) = sums(:,41) ! qv (q)
	291	IF ( cloud_physics ) THEN
[132]	292	sums(:,42) = sums(:,42) / ngp_2dh_s_inner(:,sr)
	293	sums(:,43) = sums(:,43) / ngp_2dh_s_inner(:,sr)
[1]	294	hom(:,1,42,sr) = sums(:,42) ! qv
	295	hom(:,1,43,sr) = sums(:,43) ! pt
	296	ENDIF
	297	ENDIF
	298
	299	!
	300	!-- Passive scalar
[132]	301	IF ( passive_scalar ) hom(:,1,41,sr) = sums(:,41) / &
	302	ngp_2dh_s_inner(:,sr) ! s (q)
[1]	303
	304	!
	305	!-- Horizontally averaged profiles of the remaining prognostic variables,
	306	!-- variances, the total and the perturbation energy (single values in last
	307	!-- column of sums_l) and some diagnostic quantities.
[132]	308	!-- NOTE: for simplicity, nzb_s_inner is used below, although strictly
[1]	309	!-- ---- speaking the following k-loop would have to be split up and
	310	!-- rearranged according to the staggered grid.
[132]	311	!-- However, this implies no error since staggered velocity components
	312	!-- are zero at the walls and inside buildings.
[1]	313	tn = 0
[82]	314	#if defined( __intel_openmp_bug )
[1]	315	!$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, &
	316	!$OMP tn, ust, ust2, u2, vst, vst2, v2, w2 )
	317	tn = omp_get_thread_num()
	318	#else
	319	!$OMP PARALLEL PRIVATE( i, j, k, pts, sums_ll, sums_l_eper, sums_l_etot, tn, ust, ust2, u2, vst, vst2, v2, w2 )
	320	!$ tn = omp_get_thread_num()
	321	#endif
	322	!$OMP DO
	323	DO i = nxl, nxr
	324	DO j = nys, nyn
	325	sums_l_etot = 0.0
	326	sums_l_eper = 0.0
[132]	327	DO k = nzb_s_inner(j,i), nzt+1
[1]	328	u2 = u(k,j,i)**2
	329	v2 = v(k,j,i)**2
	330	w2 = w(k,j,i)**2
	331	ust2 = ( u(k,j,i) - hom(k,1,1,sr) )**2
	332	vst2 = ( v(k,j,i) - hom(k,1,2,sr) )**2
	333	!
	334	!-- Prognostic and diagnostic variables
	335	sums_l(k,3,tn) = sums_l(k,3,tn) + w(k,j,i) * rmask(j,i,sr)
	336	sums_l(k,8,tn) = sums_l(k,8,tn) + e(k,j,i) * rmask(j,i,sr)
	337	sums_l(k,9,tn) = sums_l(k,9,tn) + km(k,j,i) * rmask(j,i,sr)
	338	sums_l(k,10,tn) = sums_l(k,10,tn) + kh(k,j,i) * rmask(j,i,sr)
	339	sums_l(k,40,tn) = sums_l(k,40,tn) + p(k,j,i)
	340
	341	!
	342	!-- Variances
	343	sums_l(k,30,tn) = sums_l(k,30,tn) + ust2 * rmask(j,i,sr)
	344	sums_l(k,31,tn) = sums_l(k,31,tn) + vst2 * rmask(j,i,sr)
	345	sums_l(k,32,tn) = sums_l(k,32,tn) + w2 * rmask(j,i,sr)
	346	sums_l(k,33,tn) = sums_l(k,33,tn) + &
	347	( pt(k,j,i)-hom(k,1,4,sr) )*2 rmask(j,i,sr)
	348	!
	349	!-- Higher moments
	350	!-- (Computation of the skewness of w further below)
	351	sums_l(k,38,tn) = sums_l(k,38,tn) + w(k,j,i) * w2 * &
	352	rmask(j,i,sr)
	353	!
	354	!-- Perturbation energy
	355	sums_l(k,34,tn) = sums_l(k,34,tn) + 0.5 * ( ust2 + vst2 + w2 ) &
	356	* rmask(j,i,sr)
	357	sums_l_etot = sums_l_etot + &
	358	0.5 * ( u2 + v2 + w2 ) * rmask(j,i,sr)
	359	sums_l_eper = sums_l_eper + &
	360	0.5 * ( ust2+vst2+w2 ) * rmask(j,i,sr)
	361	ENDDO
	362	!
	363	!-- Total and perturbation energy for the total domain (being
	364	!-- collected in the last column of sums_l). Summation of these
	365	!-- quantities is seperated from the previous loop in order to
	366	!-- allow vectorization of that loop.
[87]	367	sums_l(nzb+4,pr_palm,tn) = sums_l(nzb+4,pr_palm,tn) + sums_l_etot
	368	sums_l(nzb+5,pr_palm,tn) = sums_l(nzb+5,pr_palm,tn) + sums_l_eper
[1]	369	!
	370	!-- 2D-arrays (being collected in the last column of sums_l)
[87]	371	sums_l(nzb,pr_palm,tn) = sums_l(nzb,pr_palm,tn) + &
[1]	372	us(j,i) * rmask(j,i,sr)
[87]	373	sums_l(nzb+1,pr_palm,tn) = sums_l(nzb+1,pr_palm,tn) + &
[1]	374	usws(j,i) * rmask(j,i,sr)
[87]	375	sums_l(nzb+2,pr_palm,tn) = sums_l(nzb+2,pr_palm,tn) + &
[1]	376	vsws(j,i) * rmask(j,i,sr)
[87]	377	sums_l(nzb+3,pr_palm,tn) = sums_l(nzb+3,pr_palm,tn) + &
[1]	378	ts(j,i) * rmask(j,i,sr)
[197]	379	IF ( humidity ) THEN
	380	sums_l(nzb+12,pr_palm,tn) = sums_l(nzb+12,pr_palm,tn) + &
	381	qs(j,i) * rmask(j,i,sr)
	382	ENDIF
[1]	383	ENDDO
	384	ENDDO
	385
	386	!
	387	!-- Horizontally averaged profiles of the vertical fluxes
	388	!$OMP DO
	389	DO i = nxl, nxr
	390	DO j = nys, nyn
	391	!
	392	!-- Subgridscale fluxes (without Prandtl layer from k=nzb,
	393	!-- oterwise from k=nzb+1)
[132]	394	!-- NOTE: for simplicity, nzb_diff_s_inner is used below, although
[1]	395	!-- ---- strictly speaking the following k-loop would have to be
	396	!-- split up according to the staggered grid.
[132]	397	!-- However, this implies no error since staggered velocity
	398	!-- components are zero at the walls and inside buildings.
	399
	400	DO k = nzb_diff_s_inner(j,i)-1, nzt_diff
[1]	401	!
	402	!-- Momentum flux w"u"
	403	sums_l(k,12,tn) = sums_l(k,12,tn) - 0.25 * ( &
	404	km(k,j,i)+km(k+1,j,i)+km(k,j,i-1)+km(k+1,j,i-1) &
	405	) * ( &
	406	( u(k+1,j,i) - u(k,j,i) ) * ddzu(k+1) &
	407	+ ( w(k,j,i) - w(k,j,i-1) ) * ddx &
	408	) * rmask(j,i,sr)
	409	!
	410	!-- Momentum flux w"v"
	411	sums_l(k,14,tn) = sums_l(k,14,tn) - 0.25 * ( &
	412	km(k,j,i)+km(k+1,j,i)+km(k,j-1,i)+km(k+1,j-1,i) &
	413	) * ( &
	414	( v(k+1,j,i) - v(k,j,i) ) * ddzu(k+1) &
	415	+ ( w(k,j,i) - w(k,j-1,i) ) * ddy &
	416	) * rmask(j,i,sr)
	417	!
	418	!-- Heat flux w"pt"
	419	sums_l(k,16,tn) = sums_l(k,16,tn) &
	420	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
	421	* ( pt(k+1,j,i) - pt(k,j,i) ) &
	422	* ddzu(k+1) * rmask(j,i,sr)
	423
	424
	425	!
[96]	426	!-- Salinity flux w"sa"
	427	IF ( ocean ) THEN
	428	sums_l(k,65,tn) = sums_l(k,65,tn) &
	429	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
	430	* ( sa(k+1,j,i) - sa(k,j,i) ) &
	431	* ddzu(k+1) * rmask(j,i,sr)
	432	ENDIF
	433
	434	!
[1]	435	!-- Buoyancy flux, water flux (humidity flux) w"q"
[75]	436	IF ( humidity ) THEN
[1]	437	sums_l(k,45,tn) = sums_l(k,45,tn) &
	438	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
	439	* ( vpt(k+1,j,i) - vpt(k,j,i) ) &
	440	* ddzu(k+1) * rmask(j,i,sr)
	441	sums_l(k,48,tn) = sums_l(k,48,tn) &
	442	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
	443	* ( q(k+1,j,i) - q(k,j,i) ) &
	444	* ddzu(k+1) * rmask(j,i,sr)
	445	IF ( cloud_physics ) THEN
	446	sums_l(k,51,tn) = sums_l(k,51,tn) &
	447	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
	448	* ( ( q(k+1,j,i) - ql(k+1,j,i) )&
	449	- ( q(k,j,i) - ql(k,j,i) ) ) &
	450	* ddzu(k+1) * rmask(j,i,sr)
	451	ENDIF
	452	ENDIF
	453
	454	!
	455	!-- Passive scalar flux
	456	IF ( passive_scalar ) THEN
	457	sums_l(k,48,tn) = sums_l(k,48,tn) &
	458	- 0.5 * ( kh(k,j,i) + kh(k+1,j,i) ) &
	459	* ( q(k+1,j,i) - q(k,j,i) ) &
	460	* ddzu(k+1) * rmask(j,i,sr)
	461	ENDIF
	462
	463	ENDDO
	464
	465	!
	466	!-- Subgridscale fluxes in the Prandtl layer
	467	IF ( use_surface_fluxes ) THEN
	468	sums_l(nzb,12,tn) = sums_l(nzb,12,tn) + &
	469	usws(j,i) * rmask(j,i,sr) ! w"u"
	470	sums_l(nzb,14,tn) = sums_l(nzb,14,tn) + &
	471	vsws(j,i) * rmask(j,i,sr) ! w"v"
	472	sums_l(nzb,16,tn) = sums_l(nzb,16,tn) + &
	473	shf(j,i) * rmask(j,i,sr) ! w"pt"
	474	sums_l(nzb,58,tn) = sums_l(nzb,58,tn) + &
	475	0.0 * rmask(j,i,sr) ! u"pt"
	476	sums_l(nzb,61,tn) = sums_l(nzb,61,tn) + &
	477	0.0 * rmask(j,i,sr) ! v"pt"
[96]	478	IF ( ocean ) THEN
	479	sums_l(nzb,65,tn) = sums_l(nzb,65,tn) + &
	480	saswsb(j,i) * rmask(j,i,sr) ! w"sa"
	481	ENDIF
[75]	482	IF ( humidity ) THEN
[1]	483	sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + &
	484	qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv")
	485	IF ( cloud_physics ) THEN
	486	sums_l(nzb,45,tn) = sums_l(nzb,45,tn) + ( &
	487	( 1.0 + 0.61 * q(nzb,j,i) ) * &
	488	shf(j,i) + 0.61 * pt(nzb,j,i) * &
	489	qsws(j,i) &
	490	)
	491	!
	492	!-- Formula does not work if ql(nzb) /= 0.0
	493	sums_l(nzb,51,tn) = sums_l(nzb,51,tn) + & ! w"q" (w"qv")
	494	qsws(j,i) * rmask(j,i,sr)
	495	ENDIF
	496	ENDIF
	497	IF ( passive_scalar ) THEN
	498	sums_l(nzb,48,tn) = sums_l(nzb,48,tn) + &
	499	qsws(j,i) * rmask(j,i,sr) ! w"q" (w"qv")
	500	ENDIF
	501	ENDIF
	502
	503	!
[19]	504	!-- Subgridscale fluxes at the top surface
	505	IF ( use_top_fluxes ) THEN
[102]	506	sums_l(nzt,12,tn) = sums_l(nzt,12,tn) + &
	507	uswst(j,i) * rmask(j,i,sr) ! w"u"
	508	sums_l(nzt,14,tn) = sums_l(nzt,14,tn) + &
	509	vswst(j,i) * rmask(j,i,sr) ! w"v"
[19]	510	sums_l(nzt,16,tn) = sums_l(nzt,16,tn) + &
	511	tswst(j,i) * rmask(j,i,sr) ! w"pt"
	512	sums_l(nzt,58,tn) = sums_l(nzt,58,tn) + &
	513	0.0 * rmask(j,i,sr) ! u"pt"
	514	sums_l(nzt,61,tn) = sums_l(nzt,61,tn) + &
	515	0.0 * rmask(j,i,sr) ! v"pt"
[96]	516	IF ( ocean ) THEN
	517	sums_l(nzt,65,tn) = sums_l(nzt,65,tn) + &
	518	saswst(j,i) * rmask(j,i,sr) ! w"sa"
	519	ENDIF
[75]	520	IF ( humidity ) THEN
[19]	521	sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + &
	522	qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv")
	523	IF ( cloud_physics ) THEN
	524	sums_l(nzt,45,tn) = sums_l(nzt,45,tn) + ( &
	525	( 1.0 + 0.61 * q(nzt,j,i) ) * &
	526	tswst(j,i) + 0.61 * pt(nzt,j,i) * &
	527	qsws(j,i) &
	528	)
	529	!
	530	!-- Formula does not work if ql(nzb) /= 0.0
	531	sums_l(nzt,51,tn) = sums_l(nzt,51,tn) + & ! w"q" (w"qv")
	532	qswst(j,i) * rmask(j,i,sr)
	533	ENDIF
	534	ENDIF
	535	IF ( passive_scalar ) THEN
	536	sums_l(nzt,48,tn) = sums_l(nzt,48,tn) + &
	537	qswst(j,i) * rmask(j,i,sr) ! w"q" (w"qv")
	538	ENDIF
	539	ENDIF
	540
	541	!
[1]	542	!-- Resolved fluxes (can be computed for all horizontal points)
[132]	543	!-- NOTE: for simplicity, nzb_s_inner is used below, although strictly
[1]	544	!-- ---- speaking the following k-loop would have to be split up and
	545	!-- rearranged according to the staggered grid.
[132]	546	DO k = nzb_s_inner(j,i), nzt
[1]	547	ust = 0.5 * ( u(k,j,i) - hom(k,1,1,sr) + &
	548	u(k+1,j,i) - hom(k+1,1,1,sr) )
	549	vst = 0.5 * ( v(k,j,i) - hom(k,1,2,sr) + &
	550	v(k+1,j,i) - hom(k+1,1,2,sr) )
	551	pts = 0.5 * ( pt(k,j,i) - hom(k,1,4,sr) + &
	552	pt(k+1,j,i) - hom(k+1,1,4,sr) )
	553	!
	554	!-- Momentum flux wu
	555	sums_l(k,13,tn) = sums_l(k,13,tn) + 0.5 * &
	556	( w(k,j,i-1) + w(k,j,i) ) &
	557	* ust * rmask(j,i,sr)
	558	!
	559	!-- Momentum flux wv
	560	sums_l(k,15,tn) = sums_l(k,15,tn) + 0.5 * &
	561	( w(k,j-1,i) + w(k,j,i) ) &
	562	* vst * rmask(j,i,sr)
	563	!
	564	!-- Heat flux wpt
	565	!-- The following formula (comment line, not executed) does not
	566	!-- work if applied to subregions
	567	! sums_l(k,17,tn) = sums_l(k,17,tn) + 0.5 * &
	568	! ( pt(k,j,i)+pt(k+1,j,i) ) &
	569	! * w(k,j,i) * rmask(j,i,sr)
	570	sums_l(k,17,tn) = sums_l(k,17,tn) + pts * w(k,j,i) * &
	571	rmask(j,i,sr)
	572	!
	573	!-- Higher moments
	574	sums_l(k,35,tn) = sums_l(k,35,tn) + pts * w(k,j,i)*2 &
	575	rmask(j,i,sr)
	576	sums_l(k,36,tn) = sums_l(k,36,tn) + pts*2 w(k,j,i) * &
	577	rmask(j,i,sr)
	578
	579	!
[96]	580	!-- Salinity flux and density (density does not belong to here,
[97]	581	!-- but so far there is no other suitable place to calculate)
[96]	582	IF ( ocean ) THEN
	583	pts = 0.5 * ( sa(k,j,i) - hom(k,1,23,sr) + &
	584	sa(k+1,j,i) - hom(k+1,1,23,sr) )
	585	sums_l(k,66,tn) = sums_l(k,66,tn) + pts * w(k,j,i) * &
	586	rmask(j,i,sr)
	587	sums_l(k,64,tn) = sums_l(k,64,tn) + rho(k,j,i) * &
	588	rmask(j,i,sr)
	589	ENDIF
	590
	591	!
[1]	592	!-- Buoyancy flux, water flux, humidity flux and liquid water
	593	!-- content
[75]	594	IF ( humidity ) THEN
[1]	595	pts = 0.5 * ( vpt(k,j,i) - hom(k,1,44,sr) + &
	596	vpt(k+1,j,i) - hom(k+1,1,44,sr) )
	597	sums_l(k,46,tn) = sums_l(k,46,tn) + pts * w(k,j,i) * &
	598	rmask(j,i,sr)
	599	pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + &
	600	q(k+1,j,i) - hom(k+1,1,41,sr) )
	601	sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * &
	602	rmask(j,i,sr)
	603	IF ( cloud_physics .OR. cloud_droplets ) THEN
	604	pts = 0.5 * &
	605	( ( q(k,j,i) - ql(k,j,i) ) - hom(k,1,42,sr) &
	606	+ ( q(k+1,j,i) - ql(k+1,j,i) ) - hom(k+1,1,42,sr) )
	607	sums_l(k,52,tn) = sums_l(k,52,tn) + pts * w(k,j,i) * &
	608	rmask(j,i,sr)
	609	sums_l(k,54,tn) = sums_l(k,54,tn) + ql(k,j,i) * &
	610	rmask(j,i,sr)
	611	ENDIF
	612	ENDIF
	613
	614	!
	615	!-- Passive scalar flux
	616	IF ( passive_scalar ) THEN
	617	pts = 0.5 * ( q(k,j,i) - hom(k,1,41,sr) + &
	618	q(k+1,j,i) - hom(k+1,1,41,sr) )
	619	sums_l(k,49,tn) = sums_l(k,49,tn) + pts * w(k,j,i) * &
	620	rmask(j,i,sr)
	621	ENDIF
	622
	623	!
	624	!-- Energy flux we
	625	sums_l(k,37,tn) = sums_l(k,37,tn) + w(k,j,i) * 0.5 * &
	626	( ust2 + vst2 + w(k,j,i)**2 )&
	627	* rmask(j,i,sr)
	628
	629	ENDDO
	630	ENDDO
	631	ENDDO
	632
	633	!
[97]	634	!-- Density at top follows Neumann condition
	635	IF ( ocean ) sums_l(nzt+1,64,tn) = sums_l(nzt,64,tn)
	636
	637	!
[1]	638	!-- Divergence of vertical flux of resolved scale energy and pressure
[106]	639	!-- fluctuations as well as flux of pressure fluctuation itself (68).
	640	!-- First calculate the products, then the divergence.
[1]	641	!-- Calculation is time consuming. Do it only, if profiles shall be plotted.
[106]	642	IF ( hom(nzb+1,2,55,0) /= 0.0 .OR. hom(nzb+1,2,68,0) /= 0.0 ) THEN
[1]	643
	644	sums_ll = 0.0 ! local array
	645
	646	!$OMP DO
	647	DO i = nxl, nxr
	648	DO j = nys, nyn
[132]	649	DO k = nzb_s_inner(j,i)+1, nzt
[1]	650
	651	sums_ll(k,1) = sums_ll(k,1) + 0.5 * w(k,j,i) * ( &
	652	( 0.25 * ( u(k,j,i)+u(k+1,j,i)+u(k,j,i+1)+u(k+1,j,i+1) &
	653	- 2.0 * ( hom(k,1,1,sr) + hom(k+1,1,1,sr) ) &
	654	) )**2 &
	655	+ ( 0.25 * ( v(k,j,i)+v(k+1,j,i)+v(k,j+1,i)+v(k+1,j+1,i) &
	656	- 2.0 * ( hom(k,1,2,sr) + hom(k+1,1,2,sr) ) &
	657	) )**2 &
	658	+ w(k,j,i)**2 )
	659
	660	sums_ll(k,2) = sums_ll(k,2) + 0.5 * w(k,j,i) &
	661	* ( p(k,j,i) + p(k+1,j,i) )
	662
	663	ENDDO
	664	ENDDO
	665	ENDDO
	666	sums_ll(0,1) = 0.0 ! because w is zero at the bottom
	667	sums_ll(nzt+1,1) = 0.0
	668	sums_ll(0,2) = 0.0
	669	sums_ll(nzt+1,2) = 0.0
	670
[132]	671	DO k = nzb_s_inner(j,i)+1, nzt
[1]	672	sums_l(k,55,tn) = ( sums_ll(k,1) - sums_ll(k-1,1) ) * ddzw(k)
	673	sums_l(k,56,tn) = ( sums_ll(k,2) - sums_ll(k-1,2) ) * ddzw(k)
[106]	674	sums_l(k,68,tn) = sums_ll(k,2)
[1]	675	ENDDO
	676	sums_l(nzb,55,tn) = sums_l(nzb+1,55,tn)
	677	sums_l(nzb,56,tn) = sums_l(nzb+1,56,tn)
[106]	678	sums_l(nzb,68,tn) = 0.0 ! because w* = 0 at nzb
[1]	679
	680	ENDIF
	681
	682	!
[106]	683	!-- Divergence of vertical flux of SGS TKE and the flux itself (69)
	684	IF ( hom(nzb+1,2,57,0) /= 0.0 .OR. hom(nzb+1,2,69,0) /= 0.0 ) THEN
[1]	685
	686	!$OMP DO
	687	DO i = nxl, nxr
	688	DO j = nys, nyn
[132]	689	DO k = nzb_s_inner(j,i)+1, nzt
[1]	690
[106]	691	sums_l(k,57,tn) = sums_l(k,57,tn) - 0.5 * ( &
[1]	692	(km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) &
	693	- (km(k-1,j,i)+km(k,j,i)) * (e(k,j,i)-e(k-1,j,i)) * ddzu(k) &
[106]	694	) * ddzw(k)
[1]	695
[106]	696	sums_l(k,69,tn) = sums_l(k,69,tn) - 0.5 * ( &
	697	(km(k,j,i)+km(k+1,j,i)) * (e(k+1,j,i)-e(k,j,i)) * ddzu(k+1) &
	698	)
	699
[1]	700	ENDDO
	701	ENDDO
	702	ENDDO
	703	sums_l(nzb,57,tn) = sums_l(nzb+1,57,tn)
[106]	704	sums_l(nzb,69,tn) = sums_l(nzb+1,69,tn)
[1]	705
	706	ENDIF
	707
	708	!
	709	!-- Horizontal heat fluxes (subgrid, resolved, total).
	710	!-- Do it only, if profiles shall be plotted.
	711	IF ( hom(nzb+1,2,58,0) /= 0.0 ) THEN
	712
	713	!$OMP DO
	714	DO i = nxl, nxr
	715	DO j = nys, nyn
[132]	716	DO k = nzb_s_inner(j,i)+1, nzt
[1]	717	!
	718	!-- Subgrid horizontal heat fluxes u"pt", v"pt"
	719	sums_l(k,58,tn) = sums_l(k,58,tn) - 0.5 * &
	720	( kh(k,j,i) + kh(k,j,i-1) ) &
	721	* ( pt(k,j,i-1) - pt(k,j,i) ) &
	722	* ddx * rmask(j,i,sr)
	723	sums_l(k,61,tn) = sums_l(k,61,tn) - 0.5 * &
	724	( kh(k,j,i) + kh(k,j-1,i) ) &
	725	* ( pt(k,j-1,i) - pt(k,j,i) ) &
	726	* ddy * rmask(j,i,sr)
	727	!
	728	!-- Resolved horizontal heat fluxes upt, vpt
	729	sums_l(k,59,tn) = sums_l(k,59,tn) + &
	730	( u(k,j,i) - hom(k,1,1,sr) ) &
	731	* 0.5 * ( pt(k,j,i-1) - hom(k,1,4,sr) + &
	732	pt(k,j,i) - hom(k,1,4,sr) )
	733	pts = 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + &
	734	pt(k,j,i) - hom(k,1,4,sr) )
	735	sums_l(k,62,tn) = sums_l(k,62,tn) + &
	736	( v(k,j,i) - hom(k,1,2,sr) ) &
	737	* 0.5 * ( pt(k,j-1,i) - hom(k,1,4,sr) + &
	738	pt(k,j,i) - hom(k,1,4,sr) )
	739	ENDDO
	740	ENDDO
	741	ENDDO
	742	!
	743	!-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer)
[97]	744	sums_l(nzb,58,tn) = 0.0
	745	sums_l(nzb,59,tn) = 0.0
	746	sums_l(nzb,60,tn) = 0.0
	747	sums_l(nzb,61,tn) = 0.0
	748	sums_l(nzb,62,tn) = 0.0
	749	sums_l(nzb,63,tn) = 0.0
[1]	750
	751	ENDIF
[87]	752
	753	!
	754	!-- Calculate the user-defined profiles
	755	CALL user_statistics( 'profiles', sr, tn )
[1]	756	!$OMP END PARALLEL
	757
	758	!
	759	!-- Summation of thread sums
	760	IF ( threads_per_task > 1 ) THEN
	761	DO i = 1, threads_per_task-1
	762	sums_l(:,3,0) = sums_l(:,3,0) + sums_l(:,3,i)
	763	sums_l(:,4:40,0) = sums_l(:,4:40,0) + sums_l(:,4:40,i)
[87]	764	sums_l(:,45:pr_palm,0) = sums_l(:,45:pr_palm,0) + &
	765	sums_l(:,45:pr_palm,i)
	766	IF ( max_pr_user > 0 ) THEN
	767	sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) = &
	768	sums_l(:,pr_palm+1:pr_palm+max_pr_user,0) + &
	769	sums_l(:,pr_palm+1:pr_palm+max_pr_user,i)
	770	ENDIF
[1]	771	ENDDO
	772	ENDIF
	773
	774	#if defined( __parallel )
	775	!
	776	!-- Compute total sum from local sums
	777	CALL MPI_ALLREDUCE( sums_l(nzb,1,0), sums(nzb,1), ngp_sums, MPI_REAL, &
	778	MPI_SUM, comm2d, ierr )
	779	#else
	780	sums = sums_l(:,:,0)
	781	#endif
	782
	783	!
	784	!-- Final values are obtained by division by the total number of grid points
	785	!-- used for summation. After that store profiles.
	786	!-- Profiles:
	787	DO k = nzb, nzt+1
[132]	788	sums(k,3) = sums(k,3) / ngp_2dh(sr)
[142]	789	sums(k,8:11) = sums(k,8:11) / ngp_2dh_s_inner(k,sr)
[132]	790	sums(k,12:22) = sums(k,12:22) / ngp_2dh(sr)
	791	sums(k,23:29) = sums(k,23:29) / ngp_2dh_s_inner(k,sr)
	792	sums(k,30:32) = sums(k,30:32) / ngp_2dh(sr)
[142]	793	sums(k,33:34) = sums(k,33:34) / ngp_2dh_s_inner(k,sr)
	794	sums(k,35:39) = sums(k,35:39) / ngp_2dh(sr)
[132]	795	sums(k,40) = sums(k,40) / ngp_2dh_s_inner(k,sr)
	796	sums(k,45:53) = sums(k,45:53) / ngp_2dh(sr)
	797	sums(k,54) = sums(k,54) / ngp_2dh_s_inner(k,sr)
	798	sums(k,55:63) = sums(k,55:63) / ngp_2dh(sr)
	799	sums(k,64) = sums(k,64) / ngp_2dh_s_inner(k,sr)
	800	sums(k,65:69) = sums(k,65:69) / ngp_2dh(sr)
	801	sums(k,70:pr_palm-2) = sums(k,70:pr_palm-2)/ ngp_2dh_s_inner(k,sr)
[1]	802	ENDDO
	803	!-- Upstream-parts
[87]	804	sums(nzb:nzb+11,pr_palm-1) = sums(nzb:nzb+11,pr_palm-1) / ngp_3d(sr)
[1]	805	!-- u* and so on
[87]	806	!-- As sums(nzb:nzb+3,pr_palm) are full 2D arrays (us, usws, vsws, ts) whose
[1]	807	!-- size is always ( nx + 1 ) * ( ny + 1 ), defined at the first grid layer
	808	!-- above the topography, they are being divided by ngp_2dh(sr)
[87]	809	sums(nzb:nzb+3,pr_palm) = sums(nzb:nzb+3,pr_palm) / &
[1]	810	ngp_2dh(sr)
[197]	811	sums(nzb+12,pr_palm) = sums(nzb+12,pr_palm) / & ! qs
	812	ngp_2dh(sr)
[1]	813	!-- eges, e*
[87]	814	sums(nzb+4:nzb+5,pr_palm) = sums(nzb+4:nzb+5,pr_palm) / &
[132]	815	ngp_3d(sr)
[1]	816	!-- Old and new divergence
[87]	817	sums(nzb+9:nzb+10,pr_palm) = sums(nzb+9:nzb+10,pr_palm) / &
[1]	818	ngp_3d_inner(sr)
	819
[87]	820	!-- User-defined profiles
	821	IF ( max_pr_user > 0 ) THEN
	822	DO k = nzb, nzt+1
	823	sums(k,pr_palm+1:pr_palm+max_pr_user) = &
	824	sums(k,pr_palm+1:pr_palm+max_pr_user) / &
[132]	825	ngp_2dh_s_inner(k,sr)
[87]	826	ENDDO
	827	ENDIF
	828
[1]	829	!
	830	!-- Collect horizontal average in hom.
	831	!-- Compute deduced averages (e.g. total heat flux)
	832	hom(:,1,3,sr) = sums(:,3) ! w
	833	hom(:,1,8,sr) = sums(:,8) ! e profiles 5-7 are initial profiles
	834	hom(:,1,9,sr) = sums(:,9) ! km
	835	hom(:,1,10,sr) = sums(:,10) ! kh
	836	hom(:,1,11,sr) = sums(:,11) ! l
	837	hom(:,1,12,sr) = sums(:,12) ! w"u"
	838	hom(:,1,13,sr) = sums(:,13) ! wu
	839	hom(:,1,14,sr) = sums(:,14) ! w"v"
	840	hom(:,1,15,sr) = sums(:,15) ! wv
	841	hom(:,1,16,sr) = sums(:,16) ! w"pt"
	842	hom(:,1,17,sr) = sums(:,17) ! wpt
	843	hom(:,1,18,sr) = sums(:,16) + sums(:,17) ! wpt
	844	hom(:,1,19,sr) = sums(:,12) + sums(:,13) ! wu
	845	hom(:,1,20,sr) = sums(:,14) + sums(:,15) ! wv
	846	hom(:,1,21,sr) = sums(:,21) ! wptBC
	847	hom(:,1,22,sr) = sums(:,16) + sums(:,21) ! wptBC
[96]	848	! profile 24 is initial profile (sa)
	849	! profiles 25-29 left empty for initial
[1]	850	! profiles
	851	hom(:,1,30,sr) = sums(:,30) ! u*2
	852	hom(:,1,31,sr) = sums(:,31) ! v*2
	853	hom(:,1,32,sr) = sums(:,32) ! w*2
	854	hom(:,1,33,sr) = sums(:,33) ! pt*2
	855	hom(:,1,34,sr) = sums(:,34) ! e*
	856	hom(:,1,35,sr) = sums(:,35) ! w2pt
	857	hom(:,1,36,sr) = sums(:,36) ! wpt2
	858	hom(:,1,37,sr) = sums(:,37) ! we
	859	hom(:,1,38,sr) = sums(:,38) ! w*3
	860	hom(:,1,39,sr) = sums(:,38) / ( sums(:,32) + 1E-20 )**1.5 ! Sw
	861	hom(:,1,40,sr) = sums(:,40) ! p
	862	hom(:,1,45,sr) = sums(:,45) ! w"q"
	863	hom(:,1,46,sr) = sums(:,46) ! wvpt
	864	hom(:,1,47,sr) = sums(:,45) + sums(:,46) ! wvpt
	865	hom(:,1,48,sr) = sums(:,48) ! w"q" (w"qv")
	866	hom(:,1,49,sr) = sums(:,49) ! wq (wqv)
	867	hom(:,1,50,sr) = sums(:,48) + sums(:,49) ! wq (wqv)
	868	hom(:,1,51,sr) = sums(:,51) ! w"qv"
	869	hom(:,1,52,sr) = sums(:,52) ! wqv
	870	hom(:,1,53,sr) = sums(:,52) + sums(:,51) ! wq (wqv)
	871	hom(:,1,54,sr) = sums(:,54) ! ql
	872	hom(:,1,55,sr) = sums(:,55) ! wuu*/dz
	873	hom(:,1,56,sr) = sums(:,56) ! wp/dz
[106]	874	hom(:,1,57,sr) = sums(:,57) ! ( w"e + w"p"/rho )/dz
[1]	875	hom(:,1,58,sr) = sums(:,58) ! u"pt"
	876	hom(:,1,59,sr) = sums(:,59) ! upt
	877	hom(:,1,60,sr) = sums(:,58) + sums(:,59) ! upt_t
	878	hom(:,1,61,sr) = sums(:,61) ! v"pt"
	879	hom(:,1,62,sr) = sums(:,62) ! vpt
	880	hom(:,1,63,sr) = sums(:,61) + sums(:,62) ! vpt_t
[96]	881	hom(:,1,64,sr) = sums(:,64) ! rho
	882	hom(:,1,65,sr) = sums(:,65) ! w"sa"
	883	hom(:,1,66,sr) = sums(:,66) ! wsa
	884	hom(:,1,67,sr) = sums(:,65) + sums(:,66) ! wsa
[106]	885	hom(:,1,68,sr) = sums(:,68) ! wp
	886	hom(:,1,69,sr) = sums(:,69) ! w"e + w"p"/rho
[197]	887	hom(:,1,70,sr) = sums(:,70) ! q*2
[1]	888
[87]	889	hom(:,1,pr_palm-1,sr) = sums(:,pr_palm-1)
[1]	890	! upstream-parts u_x, u_y, u_z, v_x,
	891	! v_y, usw. (in last but one profile)
[87]	892	hom(:,1,pr_palm,sr) = sums(:,pr_palm)
[1]	893	! u, w'u', w'v', t (in last profile)
	894
[87]	895	IF ( max_pr_user > 0 ) THEN ! user-defined profiles
	896	hom(:,1,pr_palm+1:pr_palm+max_pr_user,sr) = &
	897	sums(:,pr_palm+1:pr_palm+max_pr_user)
	898	ENDIF
	899
[1]	900	!
	901	!-- Determine the boundary layer height using two different schemes.
[94]	902	!-- First scheme: Starting from the Earth's (Ocean's) surface, look for the
	903	!-- first relative minimum (maximum) of the total heat flux.
	904	!-- The corresponding height is assumed as the boundary layer height, if it
	905	!-- is less than 1.5 times the height where the heat flux becomes negative
	906	!-- (positive) for the first time.
[1]	907	!-- NOTE: This criterion is still capable of improving!
	908	z_i(1) = 0.0
	909	first = .TRUE.
[97]	910	IF ( ocean ) THEN
	911	DO k = nzt, nzb+1, -1
	912	IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN
	913	first = .FALSE.
	914	height = zw(k)
	915	ENDIF
	916	IF ( hom(k,1,18,sr) < 0.0 .AND. &
	917	hom(k-1,1,18,sr) > hom(k,1,18,sr) ) THEN
	918	IF ( zw(k) < 1.5 * height ) THEN
	919	z_i(1) = zw(k)
	920	ELSE
	921	z_i(1) = height
	922	ENDIF
	923	EXIT
	924	ENDIF
	925	ENDDO
	926	ELSE
[94]	927	DO k = nzb, nzt-1
	928	IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN
	929	first = .FALSE.
	930	height = zw(k)
[1]	931	ENDIF
[94]	932	IF ( hom(k,1,18,sr) < 0.0 .AND. &
	933	hom(k+1,1,18,sr) > hom(k,1,18,sr) ) THEN
	934	IF ( zw(k) < 1.5 * height ) THEN
	935	z_i(1) = zw(k)
	936	ELSE
	937	z_i(1) = height
	938	ENDIF
	939	EXIT
	940	ENDIF
	941	ENDDO
[97]	942	ENDIF
[1]	943
	944	!
[97]	945	!-- Second scheme: Starting from the top/bottom model boundary, look for
	946	!-- the first characteristic kink in the temperature profile, where the
	947	!-- originally stable stratification notably weakens.
[1]	948	z_i(2) = 0.0
[97]	949	IF ( ocean ) THEN
	950	DO k = nzb+1, nzt-1
	951	IF ( ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) > &
	952	2.0 * ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) ) THEN
	953	z_i(2) = zu(k)
	954	EXIT
	955	ENDIF
	956	ENDDO
	957	ELSE
	958	DO k = nzt-1, nzb+1, -1
	959	IF ( ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) > &
	960	2.0 * ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) ) THEN
	961	z_i(2) = zu(k)
	962	EXIT
	963	ENDIF
	964	ENDDO
	965	ENDIF
[1]	966
[87]	967	hom(nzb+6,1,pr_palm,sr) = z_i(1)
	968	hom(nzb+7,1,pr_palm,sr) = z_i(2)
[1]	969
	970	!
	971	!-- Computation of both the characteristic vertical velocity and
	972	!-- the characteristic convective boundary layer temperature.
	973	!-- The horizontal average at nzb+1 is input for the average temperature.
	974	IF ( hom(nzb,1,18,sr) > 0.0 .AND. z_i(1) /= 0.0 ) THEN
[87]	975	hom(nzb+8,1,pr_palm,sr) = ( g / hom(nzb+1,1,4,sr) * &
[94]	976	hom(nzb,1,18,sr) * &
	977	ABS( z_i(1) ) )**0.333333333
[1]	978	!-- so far this only works if Prandtl layer is used
[87]	979	hom(nzb+11,1,pr_palm,sr) = hom(nzb,1,16,sr) / hom(nzb+8,1,pr_palm,sr)
[1]	980	ELSE
[87]	981	hom(nzb+8,1,pr_palm,sr) = 0.0
	982	hom(nzb+11,1,pr_palm,sr) = 0.0
[1]	983	ENDIF
	984
[48]	985	!
	986	!-- Collect the time series quantities
[87]	987	ts_value(1,sr) = hom(nzb+4,1,pr_palm,sr) ! E
	988	ts_value(2,sr) = hom(nzb+5,1,pr_palm,sr) ! E*
[48]	989	ts_value(3,sr) = dt_3d
[87]	990	ts_value(4,sr) = hom(nzb,1,pr_palm,sr) ! u*
	991	ts_value(5,sr) = hom(nzb+3,1,pr_palm,sr) ! th*
[48]	992	ts_value(6,sr) = u_max
	993	ts_value(7,sr) = v_max
	994	ts_value(8,sr) = w_max
[87]	995	ts_value(9,sr) = hom(nzb+10,1,pr_palm,sr) ! new divergence
	996	ts_value(10,sr) = hom(nzb+9,1,pr_palm,sr) ! old Divergence
	997	ts_value(11,sr) = hom(nzb+6,1,pr_palm,sr) ! z_i(1)
	998	ts_value(12,sr) = hom(nzb+7,1,pr_palm,sr) ! z_i(2)
	999	ts_value(13,sr) = hom(nzb+8,1,pr_palm,sr) ! w*
[48]	1000	ts_value(14,sr) = hom(nzb,1,16,sr) ! w'pt' at k=0
	1001	ts_value(15,sr) = hom(nzb+1,1,16,sr) ! w'pt' at k=1
	1002	ts_value(16,sr) = hom(nzb+1,1,18,sr) ! wpt at k=1
	1003	ts_value(17,sr) = hom(nzb,1,4,sr) ! pt(0)
	1004	ts_value(18,sr) = hom(nzb+1,1,4,sr) ! pt(zp)
[197]	1005	ts_value(19,sr) = hom(nzb+1,1,pr_palm,sr) ! u'w' at k=0
	1006	ts_value(20,sr) = hom(nzb+2,1,pr_palm,sr) ! v'w' at k=0
	1007	ts_value(21,sr) = hom(nzb+12,1,pr_palm,sr) ! w'q' at k=0
	1008
[48]	1009	IF ( ts_value(5,sr) /= 0.0 ) THEN
	1010	ts_value(22,sr) = ts_value(4,sr)**2 / &
	1011	( kappa * g * ts_value(5,sr) / ts_value(18,sr) ) ! L
	1012	ELSE
	1013	ts_value(22,sr) = 10000.0
	1014	ENDIF
[1]	1015
	1016	!
[48]	1017	!-- Calculate additional statistics provided by the user interface
[87]	1018	CALL user_statistics( 'time_series', sr, 0 )
[1]	1019
[48]	1020	ENDDO ! loop of the subregions
	1021
[1]	1022	!
	1023	!-- If required, sum up horizontal averages for subsequent time averaging
	1024	IF ( do_sum ) THEN
	1025	IF ( average_count_pr == 0 ) hom_sum = 0.0
	1026	hom_sum = hom_sum + hom(:,1,:,:)
	1027	average_count_pr = average_count_pr + 1
	1028	do_sum = .FALSE.
	1029	ENDIF
	1030
	1031	!
	1032	!-- Set flag for other UPs (e.g. output routines, but also buoyancy).
	1033	!-- This flag is reset after each time step in time_integration.
	1034	flow_statistics_called = .TRUE.
	1035
	1036	CALL cpu_log( log_point(10), 'flow_statistics', 'stop' )
	1037
	1038
	1039	END SUBROUTINE flow_statistics
	1040
	1041
	1042

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

Download in other formats:

| Impressum | ©Leibniz Universität Hannover |