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source: palm/trunk/SOURCE/init_3d_model.f90 @ 671

Last change on this file since 671 was 668, checked in by suehring, 14 years ago
last commit documented
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File size: 53.5 KB

Rev	Line
[1]	1	#if defined( __ibmy_special )
	2	@PROCESS NOOPTimize
	3	#endif
	4	SUBROUTINE init_3d_model
	5
	6	!------------------------------------------------------------------------------!
[254]	7	! Current revisions:
[1]	8	! -----------------
[668]	9	!
	10	! Former revisions:
	11	! -----------------
	12	! $Id: init_3d_model.f90 668 2010-12-23 13:22:58Z heinze $
	13	!
	14	! 667 2010-12-23 12:06:00Z suehring/gryschka
[667]	15	! nxl-1, nxr+1, nys-1, nyn+1 replaced by nxlg, nxrg, nysg, nyng in loops and
	16	! allocation of arrays. Calls of exchange_horiz are modified.
	17	! Call ws_init to initialize arrays needed for statistical evaluation and
	18	! optimization when ws-scheme is used.
	19	! Initial volume flow is now calculated by using the variable hom_sum.
	20	! Therefore the correction of initial volume flow for non-flat topography
	21	! removed (removed u_nzb_p1_for_vfc and v_nzb_p1_for_vfc)
	22	! Changed surface boundary conditions for u and v in case of ibc_uv_b == 0 from
	23	! mirror bc to dirichlet boundary conditions (u=v=0), so that k=nzb is
	24	! representative for the height z0
	25	! Bugfix: type conversion of '1' to 64bit for the MAX function (ngp_3d_inner)
	26	!
[623]	27	! 622 2010-12-10 08:08:13Z raasch
	28	! optional barriers included in order to speed up collective operations
	29	!
[561]	30	! 560 2010-09-09 10:06:09Z weinreis
	31	! bugfix: correction of calculating ngp_3d for 64 bit
	32	!
[486]	33	! 485 2010-02-05 10:57:51Z raasch
	34	! calculation of ngp_3d + ngp_3d_inner changed because they have now 64 bit
	35	!
[482]	36	! 407 2009-12-01 15:01:15Z maronga
	37	! var_ts is replaced by dots_max
	38	! Enabled passive scalar/humidity wall fluxes for non-flat topography
	39	!
[392]	40	! 388 2009-09-23 09:40:33Z raasch
[388]	41	! Initialization of prho added.
[359]	42	! bugfix: correction of initial volume flow for non-flat topography
	43	! bugfix: zero initialization of arrays within buildings for 'cyclic_fill'
[333]	44	! bugfix: avoid that ngp_2dh_s_inner becomes zero
[328]	45	! initializing_actions='read_data_for_recycling' renamed to 'cyclic_fill', now
	46	! independent of turbulent_inflow
[254]	47	! Output of messages replaced by message handling routine.
[240]	48	! Set the starting level and the vertical smoothing factor used for
	49	! the external pressure gradient
[254]	50	! +conserve_volume_flow_mode: 'default', 'initial_profiles', 'inflow_profile'
[241]	51	! and 'bulk_velocity'
[292]	52	! If the inversion height calculated by the prerun is zero,
	53	! inflow_damping_height must be explicitly specified.
[139]	54	!
[198]	55	! 181 2008-07-30 07:07:47Z raasch
	56	! bugfix: zero assignments to tendency arrays in case of restarts,
	57	! further extensions and modifications in the initialisation of the plant
	58	! canopy model,
	59	! allocation of hom_sum moved to parin, initialization of spectrum_x\|y directly
	60	! after allocating theses arrays,
	61	! read data for recycling added as new initialization option,
	62	! dummy allocation for diss
	63	!
[139]	64	! 138 2007-11-28 10:03:58Z letzel
[132]	65	! New counter ngp_2dh_s_inner.
	66	! Allow new case bc_uv_t = 'dirichlet_0' for channel flow.
	67	! Corrected calculation of initial volume flow for 'set_1d-model_profiles' and
	68	! 'set_constant_profiles' in case of buildings in the reference cross-sections.
[77]	69	!
[110]	70	! 108 2007-08-24 15:10:38Z letzel
	71	! Flux initialization in case of coupled runs, +momentum fluxes at top boundary,
	72	! +arrays for phase speed c_u, c_v, c_w, indices for u\|v\|w_m_l\|r changed
	73	! +qswst_remote in case of atmosphere model with humidity coupled to ocean
	74	! Rayleigh damping for ocean, optionally calculate km and kh from initial
	75	! TKE e_init
	76	!
[98]	77	! 97 2007-06-21 08:23:15Z raasch
	78	! Initialization of salinity, call of init_ocean
	79	!
[90]	80	! 87 2007-05-22 15:46:47Z raasch
	81	! var_hom and var_sum renamed pr_palm
	82	!
[77]	83	! 75 2007-03-22 09:54:05Z raasch
[73]	84	! Arrays for radiation boundary conditions are allocated (u_m_l, u_m_r, etc.),
	85	! bugfix for cases with the outflow damping layer extending over more than one
[75]	86	! subdomain, moisture renamed humidity,
	87	! new initializing action "by_user" calls user_init_3d_model,
[72]	88	! precipitation_amount/rate, ts_value are allocated, +module netcdf_control,
[51]	89	! initial velocities at nzb+1 are regarded for volume
	90	! flow control in case they have been set zero before (to avoid small timesteps)
[75]	91	! -uvmean_outflow, uxrp, vynp eliminated
[1]	92	!
[39]	93	! 19 2007-02-23 04:53:48Z raasch
	94	! +handling of top fluxes
	95	!
[3]	96	! RCS Log replace by Id keyword, revision history cleaned up
	97	!
[1]	98	! Revision 1.49 2006/08/22 15:59:07 raasch
	99	! No optimization of this file on the ibmy (Yonsei Univ.)
	100	!
	101	! Revision 1.1 1998/03/09 16:22:22 raasch
	102	! Initial revision
	103	!
	104	!
	105	! Description:
	106	! ------------
	107	! Allocation of arrays and initialization of the 3D model via
	108	! a) pre-run the 1D model
	109	! or
	110	! b) pre-set constant linear profiles
	111	! or
	112	! c) read values of a previous run
	113	!------------------------------------------------------------------------------!
	114
[667]	115	USE advec_ws
[1]	116	USE arrays_3d
	117	USE averaging
[72]	118	USE cloud_parameters
[1]	119	USE constants
	120	USE control_parameters
	121	USE cpulog
	122	USE indices
	123	USE interfaces
	124	USE model_1d
[51]	125	USE netcdf_control
[1]	126	USE particle_attributes
	127	USE pegrid
	128	USE profil_parameter
	129	USE random_function_mod
	130	USE statistics
	131
	132	IMPLICIT NONE
	133
[559]	134	INTEGER :: i, ind_array(1), j, k, sr
[1]	135
[485]	136	INTEGER, DIMENSION(:), ALLOCATABLE :: ngp_2dh_l
[1]	137
[132]	138	INTEGER, DIMENSION(:,:), ALLOCATABLE :: ngp_2dh_outer_l, &
	139	ngp_2dh_s_inner_l
[1]	140
[153]	141	REAL :: a, b
	142
[1]	143	REAL, DIMENSION(1:2) :: volume_flow_area_l, volume_flow_initial_l
	144
[485]	145	REAL, DIMENSION(:), ALLOCATABLE :: ngp_3d_inner_l, ngp_3d_inner_tmp
[1]	146
[485]	147
[1]	148	!
	149	!-- Allocate arrays
	150	ALLOCATE( ngp_2dh(0:statistic_regions), ngp_2dh_l(0:statistic_regions), &
	151	ngp_3d(0:statistic_regions), &
	152	ngp_3d_inner(0:statistic_regions), &
	153	ngp_3d_inner_l(0:statistic_regions), &
[485]	154	ngp_3d_inner_tmp(0:statistic_regions), &
[1]	155	sums_divnew_l(0:statistic_regions), &
	156	sums_divold_l(0:statistic_regions) )
[240]	157	ALLOCATE( dp_smooth_factor(nzb:nzt), rdf(nzb+1:nzt) )
[143]	158	ALLOCATE( ngp_2dh_outer(nzb:nzt+1,0:statistic_regions), &
[1]	159	ngp_2dh_outer_l(nzb:nzt+1,0:statistic_regions), &
[132]	160	ngp_2dh_s_inner(nzb:nzt+1,0:statistic_regions), &
	161	ngp_2dh_s_inner_l(nzb:nzt+1,0:statistic_regions), &
[667]	162	rmask(nysg:nyng,nxlg:nxrg,0:statistic_regions), &
[87]	163	sums(nzb:nzt+1,pr_palm+max_pr_user), &
	164	sums_l(nzb:nzt+1,pr_palm+max_pr_user,0:threads_per_task-1), &
[1]	165	sums_l_l(nzb:nzt+1,0:statistic_regions,0:threads_per_task-1), &
	166	sums_up_fraction_l(10,3,0:statistic_regions), &
[48]	167	sums_wsts_bc_l(nzb:nzt+1,0:statistic_regions), &
[394]	168	ts_value(dots_max,0:statistic_regions) )
[667]	169	ALLOCATE( km_damp_x(nxlg:nxrg), km_damp_y(nysg:nyng) )
[1]	170
[667]	171	ALLOCATE( rif_1(nysg:nyng,nxlg:nxrg), shf_1(nysg:nyng,nxlg:nxrg), &
	172	ts(nysg:nyng,nxlg:nxrg), tswst_1(nysg:nyng,nxlg:nxrg), &
	173	us(nysg:nyng,nxlg:nxrg), usws_1(nysg:nyng,nxlg:nxrg), &
	174	uswst_1(nysg:nyng,nxlg:nxrg), &
	175	vsws_1(nysg:nyng,nxlg:nxrg), &
	176	vswst_1(nysg:nyng,nxlg:nxrg), z0(nysg:nyng,nxlg:nxrg) )
[1]	177
	178	IF ( timestep_scheme(1:5) /= 'runge' ) THEN
	179	!
	180	!-- Leapfrog scheme needs two timelevels of diffusion quantities
[667]	181	ALLOCATE( rif_2(nysg:nyng,nxlg:nxrg), &
	182	shf_2(nysg:nyng,nxlg:nxrg), &
	183	tswst_2(nysg:nyng,nxlg:nxrg), &
	184	usws_2(nysg:nyng,nxlg:nxrg), &
	185	uswst_2(nysg:nyng,nxlg:nxrg), &
	186	vswst_2(nysg:nyng,nxlg:nxrg), &
	187	vsws_2(nysg:nyng,nxlg:nxrg) )
[1]	188	ENDIF
	189
[75]	190	ALLOCATE( d(nzb+1:nzta,nys:nyna,nxl:nxra), &
[667]	191	e_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	192	e_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	193	e_3(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	194	kh_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	195	km_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	196	p(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	197	pt_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	198	pt_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	199	pt_3(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	200	tend(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	201	u_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	202	u_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	203	u_3(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	204	v_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	205	v_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	206	v_3(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	207	w_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	208	w_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	209	w_3(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[1]	210
	211	IF ( timestep_scheme(1:5) /= 'runge' ) THEN
[667]	212	ALLOCATE( kh_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	213	km_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[1]	214	ENDIF
	215
[75]	216	IF ( humidity .OR. passive_scalar ) THEN
[1]	217	!
[75]	218	!-- 2D-humidity/scalar arrays
[667]	219	ALLOCATE ( qs(nysg:nyng,nxlg:nxrg), &
	220	qsws_1(nysg:nyng,nxlg:nxrg), &
	221	qswst_1(nysg:nyng,nxlg:nxrg) )
[1]	222
	223	IF ( timestep_scheme(1:5) /= 'runge' ) THEN
[667]	224	ALLOCATE( qsws_2(nysg:nyng,nxlg:nxrg), &
	225	qswst_2(nysg:nyng,nxlg:nxrg) )
[1]	226	ENDIF
	227	!
[75]	228	!-- 3D-humidity/scalar arrays
[667]	229	ALLOCATE( q_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	230	q_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	231	q_3(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[1]	232
	233	!
[75]	234	!-- 3D-arrays needed for humidity only
	235	IF ( humidity ) THEN
[667]	236	ALLOCATE( vpt_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[1]	237
	238	IF ( timestep_scheme(1:5) /= 'runge' ) THEN
[667]	239	ALLOCATE( vpt_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[1]	240	ENDIF
	241
	242	IF ( cloud_physics ) THEN
	243	!
	244	!-- Liquid water content
[667]	245	ALLOCATE ( ql_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[72]	246	!
	247	!-- Precipitation amount and rate (only needed if output is switched)
[667]	248	ALLOCATE( precipitation_amount(nysg:nyng,nxlg:nxrg), &
	249	precipitation_rate(nysg:nyng,nxlg:nxrg) )
[1]	250	ENDIF
	251
	252	IF ( cloud_droplets ) THEN
	253	!
	254	!-- Liquid water content, change in liquid water content,
	255	!-- real volume of particles (with weighting), volume of particles
[667]	256	ALLOCATE ( ql_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	257	ql_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	258	ql_v(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	259	ql_vp(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[1]	260	ENDIF
	261
	262	ENDIF
	263
	264	ENDIF
	265
[94]	266	IF ( ocean ) THEN
[667]	267	ALLOCATE( saswsb_1(nysg:nyng,nxlg:nxrg), &
	268	saswst_1(nysg:nyng,nxlg:nxrg) )
	269	ALLOCATE( prho_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	270	rho_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	271	sa_1(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	272	sa_2(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	273	sa_3(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[388]	274	prho => prho_1
	275	rho => rho_1 ! routines calc_mean_profile and diffusion_e require
	276	! density to be apointer
[108]	277	IF ( humidity_remote ) THEN
[667]	278	ALLOCATE( qswst_remote(nysg:nyng,nxlg:nxrg))
[108]	279	qswst_remote = 0.0
	280	ENDIF
[94]	281	ENDIF
	282
[1]	283	!
	284	!-- 3D-array for storing the dissipation, needed for calculating the sgs
	285	!-- particle velocities
	286	IF ( use_sgs_for_particles ) THEN
[667]	287	ALLOCATE ( diss(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[181]	288	ELSE
	289	ALLOCATE ( diss(2,2,2) ) ! required because diss is used as a
	290	! formal parameter
[1]	291	ENDIF
	292
	293	IF ( dt_dosp /= 9999999.9 ) THEN
	294	ALLOCATE( spectrum_x( 1:nx/2, 1:10, 1:10 ), &
	295	spectrum_y( 1:ny/2, 1:10, 1:10 ) )
[146]	296	spectrum_x = 0.0
	297	spectrum_y = 0.0
[1]	298	ENDIF
	299
	300	!
[138]	301	!-- 3D-arrays for the leaf area density and the canopy drag coefficient
	302	IF ( plant_canopy ) THEN
[667]	303	ALLOCATE ( lad_s(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	304	lad_u(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	305	lad_v(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	306	lad_w(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	307	cdc(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[153]	308
	309	IF ( passive_scalar ) THEN
[667]	310	ALLOCATE ( sls(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	311	sec(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[153]	312	ENDIF
	313
	314	IF ( cthf /= 0.0 ) THEN
[667]	315	ALLOCATE ( lai(nzb:nzt+1,nysg:nyng,nxlg:nxrg), &
	316	canopy_heat_flux(nzb:nzt+1,nysg:nyng,nxlg:nxrg) )
[153]	317	ENDIF
	318
[138]	319	ENDIF
	320
	321	!
[51]	322	!-- 4D-array for storing the Rif-values at vertical walls
	323	IF ( topography /= 'flat' ) THEN
[667]	324	ALLOCATE( rif_wall(nzb:nzt+1,nysg:nyng,nxlg:nxrg,1:4) )
[51]	325	rif_wall = 0.0
	326	ENDIF
	327
	328	!
[106]	329	!-- Arrays to store velocity data from t-dt and the phase speeds which
	330	!-- are needed for radiation boundary conditions
[73]	331	IF ( outflow_l ) THEN
[667]	332	ALLOCATE( u_m_l(nzb:nzt+1,nysg:nyng,1:2), &
	333	v_m_l(nzb:nzt+1,nysg:nyng,0:1), &
	334	w_m_l(nzb:nzt+1,nysg:nyng,0:1) )
[73]	335	ENDIF
	336	IF ( outflow_r ) THEN
[667]	337	ALLOCATE( u_m_r(nzb:nzt+1,nysg:nyng,nx-1:nx), &
	338	v_m_r(nzb:nzt+1,nysg:nyng,nx-1:nx), &
	339	w_m_r(nzb:nzt+1,nysg:nyng,nx-1:nx) )
[73]	340	ENDIF
[106]	341	IF ( outflow_l .OR. outflow_r ) THEN
[667]	342	ALLOCATE( c_u(nzb:nzt+1,nysg:nyng), c_v(nzb:nzt+1,nysg:nyng), &
	343	c_w(nzb:nzt+1,nysg:nyng) )
[106]	344	ENDIF
[73]	345	IF ( outflow_s ) THEN
[667]	346	ALLOCATE( u_m_s(nzb:nzt+1,0:1,nxlg:nxrg), &
	347	v_m_s(nzb:nzt+1,1:2,nxlg:nxrg), &
	348	w_m_s(nzb:nzt+1,0:1,nxlg:nxrg) )
[73]	349	ENDIF
	350	IF ( outflow_n ) THEN
[667]	351	ALLOCATE( u_m_n(nzb:nzt+1,ny-1:ny,nxlg:nxrg), &
	352	v_m_n(nzb:nzt+1,ny-1:ny,nxlg:nxrg), &
	353	w_m_n(nzb:nzt+1,ny-1:ny,nxlg:nxrg) )
[73]	354	ENDIF
[106]	355	IF ( outflow_s .OR. outflow_n ) THEN
[667]	356	ALLOCATE( c_u(nzb:nzt+1,nxlg:nxrg), c_v(nzb:nzt+1,nxlg:nxrg), &
	357	c_w(nzb:nzt+1,nxlg:nxrg) )
[106]	358	ENDIF
[73]	359
	360	!
[1]	361	!-- Initial assignment of the pointers
	362	IF ( timestep_scheme(1:5) /= 'runge' ) THEN
	363
[19]	364	rif_m => rif_1; rif => rif_2
	365	shf_m => shf_1; shf => shf_2
	366	tswst_m => tswst_1; tswst => tswst_2
	367	usws_m => usws_1; usws => usws_2
[102]	368	uswst_m => uswst_1; uswst => uswst_2
[19]	369	vsws_m => vsws_1; vsws => vsws_2
[102]	370	vswst_m => vswst_1; vswst => vswst_2
[1]	371	e_m => e_1; e => e_2; e_p => e_3; te_m => e_3
	372	kh_m => kh_1; kh => kh_2
	373	km_m => km_1; km => km_2
	374	pt_m => pt_1; pt => pt_2; pt_p => pt_3; tpt_m => pt_3
	375	u_m => u_1; u => u_2; u_p => u_3; tu_m => u_3
	376	v_m => v_1; v => v_2; v_p => v_3; tv_m => v_3
	377	w_m => w_1; w => w_2; w_p => w_3; tw_m => w_3
	378
[75]	379	IF ( humidity .OR. passive_scalar ) THEN
[19]	380	qsws_m => qsws_1; qsws => qsws_2
	381	qswst_m => qswst_1; qswst => qswst_2
[1]	382	q_m => q_1; q => q_2; q_p => q_3; tq_m => q_3
[75]	383	IF ( humidity ) vpt_m => vpt_1; vpt => vpt_2
[1]	384	IF ( cloud_physics ) ql => ql_1
	385	IF ( cloud_droplets ) THEN
	386	ql => ql_1
	387	ql_c => ql_2
	388	ENDIF
	389	ENDIF
	390
	391	ELSE
	392
[19]	393	rif => rif_1
	394	shf => shf_1
	395	tswst => tswst_1
	396	usws => usws_1
[102]	397	uswst => uswst_1
[19]	398	vsws => vsws_1
[102]	399	vswst => vswst_1
[19]	400	e => e_1; e_p => e_2; te_m => e_3; e_m => e_3
	401	kh => kh_1
	402	km => km_1
	403	pt => pt_1; pt_p => pt_2; tpt_m => pt_3; pt_m => pt_3
	404	u => u_1; u_p => u_2; tu_m => u_3; u_m => u_3
	405	v => v_1; v_p => v_2; tv_m => v_3; v_m => v_3
	406	w => w_1; w_p => w_2; tw_m => w_3; w_m => w_3
[1]	407
[75]	408	IF ( humidity .OR. passive_scalar ) THEN
[1]	409	qsws => qsws_1
[19]	410	qswst => qswst_1
[94]	411	q => q_1; q_p => q_2; tq_m => q_3; q_m => q_3
[75]	412	IF ( humidity ) vpt => vpt_1
[1]	413	IF ( cloud_physics ) ql => ql_1
	414	IF ( cloud_droplets ) THEN
	415	ql => ql_1
	416	ql_c => ql_2
	417	ENDIF
	418	ENDIF
	419
[94]	420	IF ( ocean ) THEN
[95]	421	saswsb => saswsb_1
[94]	422	saswst => saswst_1
	423	sa => sa_1; sa_p => sa_2; tsa_m => sa_3
	424	ENDIF
	425
[1]	426	ENDIF
	427
	428	!
	429	!-- Initialize model variables
[147]	430	IF ( TRIM( initializing_actions ) /= 'read_restart_data' .AND. &
[328]	431	TRIM( initializing_actions ) /= 'cyclic_fill' ) THEN
[1]	432	!
	433	!-- First model run of a possible job queue.
	434	!-- Initial profiles of the variables must be computes.
	435	IF ( INDEX( initializing_actions, 'set_1d-model_profiles' ) /= 0 ) THEN
	436	!
	437	!-- Use solutions of the 1D model as initial profiles,
	438	!-- start 1D model
	439	CALL init_1d_model
	440	!
	441	!-- Transfer initial profiles to the arrays of the 3D model
[667]	442	DO i = nxlg, nxrg
	443	DO j = nysg, nyng
[1]	444	e(:,j,i) = e1d
	445	kh(:,j,i) = kh1d
	446	km(:,j,i) = km1d
	447	pt(:,j,i) = pt_init
	448	u(:,j,i) = u1d
	449	v(:,j,i) = v1d
	450	ENDDO
	451	ENDDO
	452
[75]	453	IF ( humidity .OR. passive_scalar ) THEN
[667]	454	DO i = nxlg, nxrg
	455	DO j = nysg, nyng
[1]	456	q(:,j,i) = q_init
	457	ENDDO
	458	ENDDO
	459	ENDIF
	460
	461	IF ( .NOT. constant_diffusion ) THEN
[667]	462	DO i = nxlg, nxrg
	463	DO j = nysg, nyng
[1]	464	e(:,j,i) = e1d
	465	ENDDO
	466	ENDDO
	467	!
	468	!-- Store initial profiles for output purposes etc.
	469	hom(:,1,25,:) = SPREAD( l1d, 2, statistic_regions+1 )
	470
	471	IF ( prandtl_layer ) THEN
	472	rif = rif1d(nzb+1)
	473	ts = 0.0 ! could actually be computed more accurately in the
	474	! 1D model. Update when opportunity arises.
	475	us = us1d
	476	usws = usws1d
	477	vsws = vsws1d
	478	ELSE
	479	ts = 0.0 ! must be set, because used in
	480	rif = 0.0 ! flowste
	481	us = 0.0
	482	usws = 0.0
	483	vsws = 0.0
	484	ENDIF
	485
	486	ELSE
	487	e = 0.0 ! must be set, because used in
	488	rif = 0.0 ! flowste
	489	ts = 0.0
	490	us = 0.0
	491	usws = 0.0
	492	vsws = 0.0
	493	ENDIF
[102]	494	uswst = top_momentumflux_u
	495	vswst = top_momentumflux_v
[1]	496
	497	!
	498	!-- In every case qs = 0.0 (see also pt)
	499	!-- This could actually be computed more accurately in the 1D model.
	500	!-- Update when opportunity arises!
[75]	501	IF ( humidity .OR. passive_scalar ) qs = 0.0
[1]	502
	503	!
	504	!-- inside buildings set velocities back to zero
	505	IF ( topography /= 'flat' ) THEN
	506	DO i = nxl-1, nxr+1
	507	DO j = nys-1, nyn+1
	508	u(nzb:nzb_u_inner(j,i),j,i) = 0.0
	509	v(nzb:nzb_v_inner(j,i),j,i) = 0.0
	510	ENDDO
	511	ENDDO
[667]	512
[1]	513	!
	514	!-- WARNING: The extra boundary conditions set after running the
	515	!-- ------- 1D model impose an error on the divergence one layer
	516	!-- below the topography; need to correct later
	517	!-- ATTENTION: Provisional correction for Piacsek & Williams
	518	!-- --------- advection scheme: keep u and v zero one layer below
	519	!-- the topography.
	520	!
[667]	521	!-- Following was removed, because mirror boundary condition are
	522	!-- replaced by dirichlet boundary conditions
[1]	523	!
[667]	524	! IF ( ibc_uv_b == 0 ) THEN
	525	!!
	526	!!-- Satisfying the Dirichlet condition with an extra layer below
	527	!!-- the surface where the u and v component change their sign.
	528	! DO i = nxl-1, nxr+1
	529	! DO j = nys-1, nyn+1
	530	! IF ( nzb_u_inner(j,i) == 0 ) u(0,j,i) = -u(1,j,i)
	531	! IF ( nzb_v_inner(j,i) == 0 ) v(0,j,i) = -v(1,j,i)
	532	! ENDDO
	533	! ENDDO
	534	!
	535	! ELSE
	536	IF ( ibc_uv_b == 1 ) THEN
	537	!
[1]	538	!-- Neumann condition
	539	DO i = nxl-1, nxr+1
	540	DO j = nys-1, nyn+1
	541	IF ( nzb_u_inner(j,i) == 0 ) u(0,j,i) = u(1,j,i)
	542	IF ( nzb_v_inner(j,i) == 0 ) v(0,j,i) = v(1,j,i)
	543	ENDDO
	544	ENDDO
	545
	546	ENDIF
	547
	548	ENDIF
	549
	550	ELSEIF ( INDEX(initializing_actions, 'set_constant_profiles') /= 0 ) &
	551	THEN
	552	!
	553	!-- Use constructed initial profiles (velocity constant with height,
	554	!-- temperature profile with constant gradient)
[667]	555	DO i = nxlg, nxrg
	556	DO j = nysg, nyng
[1]	557	pt(:,j,i) = pt_init
	558	u(:,j,i) = u_init
	559	v(:,j,i) = v_init
	560	ENDDO
	561	ENDDO
[75]	562
[1]	563	!
[292]	564	!-- Set initial horizontal velocities at the lowest computational grid
	565	!-- levels to zero in order to avoid too small time steps caused by the
	566	!-- diffusion limit in the initial phase of a run (at k=1, dz/2 occurs
	567	!-- in the limiting formula!). The original values are stored to be later
	568	!-- used for volume flow control.
[667]	569	DO i = nxlg, nxrg
	570	DO j = nysg, nyng
[1]	571	u(nzb:nzb_u_inner(j,i)+1,j,i) = 0.0
	572	v(nzb:nzb_v_inner(j,i)+1,j,i) = 0.0
	573	ENDDO
	574	ENDDO
	575
[75]	576	IF ( humidity .OR. passive_scalar ) THEN
[667]	577	DO i = nxlg, nxrg
	578	DO j = nysg, nyng
[1]	579	q(:,j,i) = q_init
	580	ENDDO
	581	ENDDO
	582	ENDIF
	583
[94]	584	IF ( ocean ) THEN
[667]	585	DO i = nxlg, nxrg
	586	DO j = nysg, nyng
[94]	587	sa(:,j,i) = sa_init
	588	ENDDO
	589	ENDDO
	590	ENDIF
[1]	591
	592	IF ( constant_diffusion ) THEN
	593	km = km_constant
	594	kh = km / prandtl_number
[108]	595	e = 0.0
	596	ELSEIF ( e_init > 0.0 ) THEN
	597	DO k = nzb+1, nzt
	598	km(k,:,:) = 0.1 * l_grid(k) * SQRT( e_init )
	599	ENDDO
	600	km(nzb,:,:) = km(nzb+1,:,:)
	601	km(nzt+1,:,:) = km(nzt,:,:)
	602	kh = km / prandtl_number
	603	e = e_init
[1]	604	ELSE
[108]	605	IF ( .NOT. ocean ) THEN
	606	kh = 0.01 ! there must exist an initial diffusion, because
	607	km = 0.01 ! otherwise no TKE would be produced by the
	608	! production terms, as long as not yet
	609	! e = (u/cm)*2 at k=nzb+1
	610	ELSE
	611	kh = 0.00001
	612	km = 0.00001
	613	ENDIF
	614	e = 0.0
[1]	615	ENDIF
[102]	616	rif = 0.0
	617	ts = 0.0
	618	us = 0.0
	619	usws = 0.0
	620	uswst = top_momentumflux_u
	621	vsws = 0.0
	622	vswst = top_momentumflux_v
[75]	623	IF ( humidity .OR. passive_scalar ) qs = 0.0
[1]	624
	625	!
	626	!-- Compute initial temperature field and other constants used in case
	627	!-- of a sloping surface
	628	IF ( sloping_surface ) CALL init_slope
	629
[46]	630	ELSEIF ( INDEX(initializing_actions, 'by_user') /= 0 ) &
	631	THEN
	632	!
	633	!-- Initialization will completely be done by the user
	634	CALL user_init_3d_model
	635
[1]	636	ENDIF
[667]	637	!
	638	!-- Bottom boundary
	639	IF ( ibc_uv_b == 0 .OR. ibc_uv_b == 2 ) THEN
	640	u(nzb,:,:) = 0.0
	641	v(nzb,:,:) = 0.0
	642	ENDIF
[1]	643
	644	!
[151]	645	!-- Apply channel flow boundary condition
[132]	646	IF ( TRIM( bc_uv_t ) == 'dirichlet_0' ) THEN
	647
	648	u(nzt+1,:,:) = 0.0
	649	v(nzt+1,:,:) = 0.0
	650
[151]	651	!-- For the Dirichlet condition to be correctly applied at the top, set
[132]	652	!-- ug and vg to zero there
	653	ug(nzt+1) = 0.0
	654	vg(nzt+1) = 0.0
	655
	656	ENDIF
	657
	658	!
[1]	659	!-- Calculate virtual potential temperature
[75]	660	IF ( humidity ) vpt = pt * ( 1.0 + 0.61 * q )
[1]	661
	662	!
	663	!-- Store initial profiles for output purposes etc.
	664	hom(:,1,5,:) = SPREAD( u(:,nys,nxl), 2, statistic_regions+1 )
	665	hom(:,1,6,:) = SPREAD( v(:,nys,nxl), 2, statistic_regions+1 )
[667]	666	IF ( ibc_uv_b == 0 .OR. ibc_uv_b == 2) THEN
	667	hom(nzb,1,5,:) = 0.0
	668	hom(nzb,1,6,:) = 0.0
[1]	669	ENDIF
	670	hom(:,1,7,:) = SPREAD( pt(:,nys,nxl), 2, statistic_regions+1 )
	671	hom(:,1,23,:) = SPREAD( km(:,nys,nxl), 2, statistic_regions+1 )
	672	hom(:,1,24,:) = SPREAD( kh(:,nys,nxl), 2, statistic_regions+1 )
	673
[97]	674	IF ( ocean ) THEN
	675	!
	676	!-- Store initial salinity profile
	677	hom(:,1,26,:) = SPREAD( sa(:,nys,nxl), 2, statistic_regions+1 )
	678	ENDIF
[1]	679
[75]	680	IF ( humidity ) THEN
[1]	681	!
	682	!-- Store initial profile of total water content, virtual potential
	683	!-- temperature
	684	hom(:,1,26,:) = SPREAD( q(:,nys,nxl), 2, statistic_regions+1 )
	685	hom(:,1,29,:) = SPREAD( vpt(:,nys,nxl), 2, statistic_regions+1 )
	686	IF ( cloud_physics .OR. cloud_droplets ) THEN
	687	!
	688	!-- Store initial profile of specific humidity and potential
	689	!-- temperature
	690	hom(:,1,27,:) = SPREAD( q(:,nys,nxl), 2, statistic_regions+1 )
	691	hom(:,1,28,:) = SPREAD( pt(:,nys,nxl), 2, statistic_regions+1 )
	692	ENDIF
	693	ENDIF
	694
	695	IF ( passive_scalar ) THEN
	696	!
	697	!-- Store initial scalar profile
	698	hom(:,1,26,:) = SPREAD( q(:,nys,nxl), 2, statistic_regions+1 )
	699	ENDIF
	700
	701	!
[19]	702	!-- Initialize fluxes at bottom surface
[1]	703	IF ( use_surface_fluxes ) THEN
	704
	705	IF ( constant_heatflux ) THEN
	706	!
	707	!-- Heat flux is prescribed
	708	IF ( random_heatflux ) THEN
	709	CALL disturb_heatflux
	710	ELSE
	711	shf = surface_heatflux
	712	!
	713	!-- Over topography surface_heatflux is replaced by wall_heatflux(0)
	714	IF ( TRIM( topography ) /= 'flat' ) THEN
[667]	715	DO i = nxlg, nxrg
	716	DO j = nysg, nyng
[1]	717	IF ( nzb_s_inner(j,i) /= 0 ) THEN
	718	shf(j,i) = wall_heatflux(0)
	719	ENDIF
	720	ENDDO
	721	ENDDO
	722	ENDIF
	723	ENDIF
	724	IF ( ASSOCIATED( shf_m ) ) shf_m = shf
	725	ENDIF
	726
	727	!
	728	!-- Determine the near-surface water flux
[75]	729	IF ( humidity .OR. passive_scalar ) THEN
[1]	730	IF ( constant_waterflux ) THEN
	731	qsws = surface_waterflux
[407]	732	!
	733	!-- Over topography surface_waterflux is replaced by
	734	!-- wall_humidityflux(0)
	735	IF ( TRIM( topography ) /= 'flat' ) THEN
	736	wall_qflux = wall_humidityflux
[667]	737	DO i = nxlg, nxrg
	738	DO j = nysg, nyng
[407]	739	IF ( nzb_s_inner(j,i) /= 0 ) THEN
	740	qsws(j,i) = wall_qflux(0)
	741	ENDIF
	742	ENDDO
	743	ENDDO
	744	ENDIF
[1]	745	IF ( ASSOCIATED( qsws_m ) ) qsws_m = qsws
	746	ENDIF
	747	ENDIF
	748
	749	ENDIF
	750
	751	!
[19]	752	!-- Initialize fluxes at top surface
[94]	753	!-- Currently, only the heatflux and salinity flux can be prescribed.
	754	!-- The latent flux is zero in this case!
[19]	755	IF ( use_top_fluxes ) THEN
	756
	757	IF ( constant_top_heatflux ) THEN
	758	!
	759	!-- Heat flux is prescribed
	760	tswst = top_heatflux
	761	IF ( ASSOCIATED( tswst_m ) ) tswst_m = tswst
	762
[75]	763	IF ( humidity .OR. passive_scalar ) THEN
[19]	764	qswst = 0.0
	765	IF ( ASSOCIATED( qswst_m ) ) qswst_m = qswst
	766	ENDIF
[94]	767
	768	IF ( ocean ) THEN
[95]	769	saswsb = bottom_salinityflux
[94]	770	saswst = top_salinityflux
	771	ENDIF
[102]	772	ENDIF
[19]	773
[102]	774	!
	775	!-- Initialization in case of a coupled model run
	776	IF ( coupling_mode == 'ocean_to_atmosphere' ) THEN
	777	tswst = 0.0
	778	IF ( ASSOCIATED( tswst_m ) ) tswst_m = tswst
	779	ENDIF
	780
[19]	781	ENDIF
	782
	783	!
[1]	784	!-- Initialize Prandtl layer quantities
	785	IF ( prandtl_layer ) THEN
	786
	787	z0 = roughness_length
	788
	789	IF ( .NOT. constant_heatflux ) THEN
	790	!
	791	!-- Surface temperature is prescribed. Here the heat flux cannot be
	792	!-- simply estimated, because therefore rif, u* and theta* would have
	793	!-- to be computed by iteration. This is why the heat flux is assumed
	794	!-- to be zero before the first time step. It approaches its correct
	795	!-- value in the course of the first few time steps.
	796	shf = 0.0
	797	IF ( ASSOCIATED( shf_m ) ) shf_m = 0.0
	798	ENDIF
	799
[75]	800	IF ( humidity .OR. passive_scalar ) THEN
[1]	801	IF ( .NOT. constant_waterflux ) THEN
	802	qsws = 0.0
	803	IF ( ASSOCIATED( qsws_m ) ) qsws_m = 0.0
	804	ENDIF
	805	ENDIF
	806
	807	ENDIF
	808
[152]	809
	810	!
[1]	811	!-- For the moment, perturbation pressure and vertical velocity are zero
	812	p = 0.0; w = 0.0
	813
	814	!
	815	!-- Initialize array sums (must be defined in first call of pres)
	816	sums = 0.0
	817
	818	!
[72]	819	!-- Treating cloud physics, liquid water content and precipitation amount
	820	!-- are zero at beginning of the simulation
	821	IF ( cloud_physics ) THEN
	822	ql = 0.0
	823	IF ( precipitation ) precipitation_amount = 0.0
	824	ENDIF
[1]	825
	826	!
	827	!-- Impose vortex with vertical axis on the initial velocity profile
	828	IF ( INDEX( initializing_actions, 'initialize_vortex' ) /= 0 ) THEN
	829	CALL init_rankine
	830	ENDIF
	831
	832	!
	833	!-- Impose temperature anomaly (advection test only)
	834	IF ( INDEX( initializing_actions, 'initialize_ptanom' ) /= 0 ) THEN
	835	CALL init_pt_anomaly
	836	ENDIF
	837
	838	!
	839	!-- If required, change the surface temperature at the start of the 3D run
	840	IF ( pt_surface_initial_change /= 0.0 ) THEN
	841	pt(nzb,:,:) = pt(nzb,:,:) + pt_surface_initial_change
	842	ENDIF
	843
	844	!
	845	!-- If required, change the surface humidity/scalar at the start of the 3D
	846	!-- run
[75]	847	IF ( ( humidity .OR. passive_scalar ) .AND. &
[1]	848	q_surface_initial_change /= 0.0 ) THEN
	849	q(nzb,:,:) = q(nzb,:,:) + q_surface_initial_change
	850	ENDIF
	851
	852	!
	853	!-- Initialize the random number generator (from numerical recipes)
	854	CALL random_function_ini
	855
	856	!
	857	!-- Impose random perturbation on the horizontal velocity field and then
	858	!-- remove the divergences from the velocity field
	859	IF ( create_disturbances ) THEN
[75]	860	CALL disturb_field( nzb_u_inner, tend, u )
	861	CALL disturb_field( nzb_v_inner, tend, v )
[1]	862	n_sor = nsor_ini
	863	CALL pres
	864	n_sor = nsor
	865	ENDIF
	866
	867	!
	868	!-- Once again set the perturbation pressure explicitly to zero in order to
	869	!-- assure that it does not generate any divergences in the first time step.
	870	!-- At t=0 the velocity field is free of divergence (as constructed above).
	871	!-- Divergences being created during a time step are not yet known and thus
	872	!-- cannot be corrected during the time step yet.
	873	p = 0.0
	874
	875	!
	876	!-- Initialize old and new time levels.
	877	IF ( timestep_scheme(1:5) /= 'runge' ) THEN
	878	e_m = e; pt_m = pt; u_m = u; v_m = v; w_m = w; kh_m = kh; km_m = km
	879	ELSE
	880	te_m = 0.0; tpt_m = 0.0; tu_m = 0.0; tv_m = 0.0; tw_m = 0.0
	881	ENDIF
	882	e_p = e; pt_p = pt; u_p = u; v_p = v; w_p = w
	883
[75]	884	IF ( humidity .OR. passive_scalar ) THEN
[1]	885	IF ( ASSOCIATED( q_m ) ) q_m = q
	886	IF ( timestep_scheme(1:5) == 'runge' ) tq_m = 0.0
	887	q_p = q
[75]	888	IF ( humidity .AND. ASSOCIATED( vpt_m ) ) vpt_m = vpt
[1]	889	ENDIF
	890
[94]	891	IF ( ocean ) THEN
	892	tsa_m = 0.0
	893	sa_p = sa
	894	ENDIF
[667]	895
[94]	896
[147]	897	ELSEIF ( TRIM( initializing_actions ) == 'read_restart_data' .OR. &
[667]	898	TRIM( initializing_actions ) == 'cyclic_fill' ) &
[1]	899	THEN
	900	!
[328]	901	!-- When reading data for cyclic fill of 3D prerun data, first read
[147]	902	!-- some of the global variables from restart file
[328]	903	IF ( TRIM( initializing_actions ) == 'cyclic_fill' ) THEN
[559]	904
	905	CALL read_parts_of_var_list
[147]	906	CALL close_file( 13 )
[328]	907
[151]	908	!
[328]	909	!-- Initialization of the turbulence recycling method
	910	IF ( turbulent_inflow ) THEN
	911	!
	912	!-- Store temporally and horizontally averaged vertical profiles to be
	913	!-- used as mean inflow profiles
	914	ALLOCATE( mean_inflow_profiles(nzb:nzt+1,5) )
[151]	915
[328]	916	mean_inflow_profiles(:,1) = hom_sum(:,1,0) ! u
	917	mean_inflow_profiles(:,2) = hom_sum(:,2,0) ! v
	918	mean_inflow_profiles(:,4) = hom_sum(:,4,0) ! pt
	919	mean_inflow_profiles(:,5) = hom_sum(:,8,0) ! e
[151]	920
	921	!
[328]	922	!-- Use these mean profiles for the inflow (provided that Dirichlet
	923	!-- conditions are used)
	924	IF ( inflow_l ) THEN
[667]	925	DO j = nysg, nyng
[328]	926	DO k = nzb, nzt+1
[667]	927	u(k,j,nxlg:-1) = mean_inflow_profiles(k,1)
	928	v(k,j,nxlg:-1) = mean_inflow_profiles(k,2)
	929	w(k,j,nxlg:-1) = 0.0
	930	pt(k,j,nxlg:-1) = mean_inflow_profiles(k,4)
	931	e(k,j,nxlg:-1) = mean_inflow_profiles(k,5)
[328]	932	ENDDO
[151]	933	ENDDO
[328]	934	ENDIF
[151]	935
	936	!
[328]	937	!-- Calculate the damping factors to be used at the inflow. For a
	938	!-- turbulent inflow the turbulent fluctuations have to be limited
	939	!-- vertically because otherwise the turbulent inflow layer will grow
	940	!-- in time.
	941	IF ( inflow_damping_height == 9999999.9 ) THEN
[151]	942	!
[328]	943	!-- Default: use the inversion height calculated by the prerun; if
	944	!-- this is zero, inflow_damping_height must be explicitly
	945	!-- specified.
	946	IF ( hom_sum(nzb+6,pr_palm,0) /= 0.0 ) THEN
	947	inflow_damping_height = hom_sum(nzb+6,pr_palm,0)
	948	ELSE
	949	WRITE( message_string, * ) 'inflow_damping_height must be ',&
	950	'explicitly specified because&the inversion height ', &
	951	'calculated by the prerun is zero.'
	952	CALL message( 'init_3d_model', 'PA0318', 1, 2, 0, 6, 0 )
	953	ENDIF
	954
[292]	955	ENDIF
[151]	956
[328]	957	IF ( inflow_damping_width == 9999999.9 ) THEN
[151]	958	!
[328]	959	!-- Default for the transition range: one tenth of the undamped
	960	!-- layer
	961	inflow_damping_width = 0.1 * inflow_damping_height
[151]	962
[328]	963	ENDIF
[151]	964
[328]	965	ALLOCATE( inflow_damping_factor(nzb:nzt+1) )
[151]	966
[328]	967	DO k = nzb, nzt+1
[151]	968
[328]	969	IF ( zu(k) <= inflow_damping_height ) THEN
	970	inflow_damping_factor(k) = 1.0
	971	ELSEIF ( zu(k) <= inflow_damping_height + &
	972	inflow_damping_width ) THEN
	973	inflow_damping_factor(k) = 1.0 - &
[151]	974	( zu(k) - inflow_damping_height ) / &
	975	inflow_damping_width
[328]	976	ELSE
	977	inflow_damping_factor(k) = 0.0
	978	ENDIF
[151]	979
[328]	980	ENDDO
	981	ENDIF
[151]	982
[147]	983	ENDIF
	984
[152]	985	!
[163]	986	!-- Read binary data from restart file
[667]	987
[559]	988	CALL read_3d_binary
[163]	989
	990	!
[359]	991	!-- Inside buildings set velocities and TKE back to zero
	992	IF ( TRIM( initializing_actions ) == 'cyclic_fill' .AND. &
	993	topography /= 'flat' ) THEN
	994	!
	995	!-- Inside buildings set velocities and TKE back to zero.
	996	!-- Other scalars (pt, q, s, km, kh, p, sa, ...) are ignored at present,
	997	!-- maybe revise later.
	998	IF ( timestep_scheme(1:5) == 'runge' ) THEN
[667]	999	DO i = nxlg, nxrg
	1000	DO j = nysg, nyng
[359]	1001	u (nzb:nzb_u_inner(j,i),j,i) = 0.0
	1002	v (nzb:nzb_v_inner(j,i),j,i) = 0.0
	1003	w (nzb:nzb_w_inner(j,i),j,i) = 0.0
	1004	e (nzb:nzb_w_inner(j,i),j,i) = 0.0
	1005	u_m(nzb:nzb_u_inner(j,i),j,i) = 0.0
	1006	v_m(nzb:nzb_v_inner(j,i),j,i) = 0.0
	1007	w_m(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1008	e_m(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1009	tu_m(nzb:nzb_u_inner(j,i),j,i) = 0.0
	1010	tv_m(nzb:nzb_v_inner(j,i),j,i) = 0.0
	1011	tw_m(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1012	te_m(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1013	tpt_m(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1014	ENDDO
	1015	ENDDO
	1016	ELSE
[667]	1017	DO i = nxlg, nxrg
	1018	DO j = nysg, nyng
[359]	1019	u (nzb:nzb_u_inner(j,i),j,i) = 0.0
	1020	v (nzb:nzb_v_inner(j,i),j,i) = 0.0
	1021	w (nzb:nzb_w_inner(j,i),j,i) = 0.0
	1022	e (nzb:nzb_w_inner(j,i),j,i) = 0.0
	1023	u_m(nzb:nzb_u_inner(j,i),j,i) = 0.0
	1024	v_m(nzb:nzb_v_inner(j,i),j,i) = 0.0
	1025	w_m(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1026	e_m(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1027	u_p(nzb:nzb_u_inner(j,i),j,i) = 0.0
	1028	v_p(nzb:nzb_v_inner(j,i),j,i) = 0.0
	1029	w_p(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1030	e_p(nzb:nzb_w_inner(j,i),j,i) = 0.0
	1031	ENDDO
	1032	ENDDO
	1033	ENDIF
	1034
	1035	ENDIF
	1036
	1037	!
[1]	1038	!-- Calculate initial temperature field and other constants used in case
	1039	!-- of a sloping surface
	1040	IF ( sloping_surface ) CALL init_slope
	1041
	1042	!
	1043	!-- Initialize new time levels (only done in order to set boundary values
	1044	!-- including ghost points)
	1045	e_p = e; pt_p = pt; u_p = u; v_p = v; w_p = w
[75]	1046	IF ( humidity .OR. passive_scalar ) q_p = q
[94]	1047	IF ( ocean ) sa_p = sa
[1]	1048
[181]	1049	!
	1050	!-- Allthough tendency arrays are set in prognostic_equations, they have
	1051	!-- have to be predefined here because they are used (but multiplied with 0)
	1052	!-- there before they are set.
	1053	IF ( timestep_scheme(1:5) == 'runge' ) THEN
	1054	te_m = 0.0; tpt_m = 0.0; tu_m = 0.0; tv_m = 0.0; tw_m = 0.0
	1055	IF ( humidity .OR. passive_scalar ) tq_m = 0.0
	1056	IF ( ocean ) tsa_m = 0.0
	1057	ENDIF
	1058
[1]	1059	ELSE
	1060	!
	1061	!-- Actually this part of the programm should not be reached
[254]	1062	message_string = 'unknown initializing problem'
	1063	CALL message( 'init_3d_model', 'PA0193', 1, 2, 0, 6, 0 )
[1]	1064	ENDIF
	1065
[151]	1066
	1067	IF ( TRIM( initializing_actions ) /= 'read_restart_data' ) THEN
[1]	1068	!
[151]	1069	!-- Initialize old timelevels needed for radiation boundary conditions
	1070	IF ( outflow_l ) THEN
	1071	u_m_l(:,:,:) = u(:,:,1:2)
	1072	v_m_l(:,:,:) = v(:,:,0:1)
	1073	w_m_l(:,:,:) = w(:,:,0:1)
	1074	ENDIF
	1075	IF ( outflow_r ) THEN
	1076	u_m_r(:,:,:) = u(:,:,nx-1:nx)
	1077	v_m_r(:,:,:) = v(:,:,nx-1:nx)
	1078	w_m_r(:,:,:) = w(:,:,nx-1:nx)
	1079	ENDIF
	1080	IF ( outflow_s ) THEN
	1081	u_m_s(:,:,:) = u(:,0:1,:)
	1082	v_m_s(:,:,:) = v(:,1:2,:)
	1083	w_m_s(:,:,:) = w(:,0:1,:)
	1084	ENDIF
	1085	IF ( outflow_n ) THEN
	1086	u_m_n(:,:,:) = u(:,ny-1:ny,:)
	1087	v_m_n(:,:,:) = v(:,ny-1:ny,:)
	1088	w_m_n(:,:,:) = w(:,ny-1:ny,:)
	1089	ENDIF
[667]	1090
[151]	1091	ENDIF
[667]	1092	!
	1093	!-- Calculate the initial volume flow at the right and north boundary
	1094	IF ( conserve_volume_flow ) THEN
[151]	1095
[667]	1096	volume_flow_initial_l = 0.0
	1097	volume_flow_area_l = 0.0
	1098
	1099	IF ( TRIM( initializing_actions ) == 'cyclic_fill' ) THEN
	1100
	1101	IF ( nxr == nx ) THEN
	1102	DO j = nys, nyn
	1103	DO k = nzb_2d(j,nx) + 1, nzt
	1104	volume_flow_initial_l(1) = volume_flow_initial_l(1) + &
	1105	hom_sum(k,1,0) * dzw(k)
	1106	volume_flow_area_l(1) = volume_flow_area_l(1) + dzw(k)
	1107	ENDDO
	1108	ENDDO
	1109	ENDIF
	1110
	1111	IF ( nyn == ny ) THEN
	1112	DO i = nxl, nxr
	1113	DO k = nzb_2d(ny,i) + 1, nzt
	1114	volume_flow_initial_l(2) = volume_flow_initial_l(2) + &
	1115	hom_sum(k,2,0) * dzw(k)
	1116	volume_flow_area_l(2) = volume_flow_area_l(2) + dzw(k)
	1117	ENDDO
	1118	ENDDO
	1119	ENDIF
	1120
	1121	ELSEIF ( TRIM( initializing_actions ) /= 'read_restart_data' ) THEN
	1122
	1123	IF ( nxr == nx ) THEN
	1124	DO j = nys, nyn
	1125	DO k = nzb_2d(j,nx) + 1, nzt
	1126	volume_flow_initial_l(1) = volume_flow_initial_l(1) + &
	1127	u(k,j,nx) * dzw(k)
	1128	volume_flow_area_l(1) = volume_flow_area_l(1) + dzw(k)
	1129	ENDDO
	1130	ENDDO
	1131	ENDIF
	1132
	1133	IF ( nyn == ny ) THEN
	1134	DO i = nxl, nxr
	1135	DO k = nzb_2d(ny,i) + 1, nzt
	1136	volume_flow_initial_l(2) = volume_flow_initial_l(2) + &
	1137	v(k,ny,i) * dzw(k)
	1138	volume_flow_area_l(2) = volume_flow_area_l(2) + dzw(k)
	1139	ENDDO
	1140	ENDDO
	1141	ENDIF
	1142
	1143	ENDIF
	1144
	1145	#if defined( __parallel )
	1146	CALL MPI_ALLREDUCE( volume_flow_initial_l(1), volume_flow_initial(1),&
	1147	2, MPI_REAL, MPI_SUM, comm2d, ierr )
	1148	CALL MPI_ALLREDUCE( volume_flow_area_l(1), volume_flow_area(1), &
	1149	2, MPI_REAL, MPI_SUM, comm2d, ierr )
	1150
	1151	CALL MPI_ALLREDUCE( volume_flow_initial_l(2), volume_flow_initial(2),&
	1152	2, MPI_REAL, MPI_SUM, comm2d, ierr )
	1153	CALL MPI_ALLREDUCE( volume_flow_area_l(2), volume_flow_area(2), &
	1154	2, MPI_REAL, MPI_SUM, comm2d, ierr )
	1155
	1156	#else
	1157	volume_flow_initial = volume_flow_initial_l
	1158	volume_flow_area = volume_flow_area_l
	1159	#endif
	1160
[151]	1161	!
[667]	1162	!-- In case of 'bulk_velocity' mode, volume_flow_initial is overridden
	1163	!-- and calculated from u\|v_bulk instead.
	1164	IF ( TRIM( conserve_volume_flow_mode ) == 'bulk_velocity' ) THEN
	1165	volume_flow_initial(1) = u_bulk * volume_flow_area(1)
	1166	volume_flow_initial(2) = v_bulk * volume_flow_area(2)
	1167	ENDIF
	1168
	1169	ENDIF
	1170	!
[138]	1171	!-- Initialization of the leaf area density
	1172	IF ( plant_canopy ) THEN
	1173
	1174	SELECT CASE ( TRIM( canopy_mode ) )
	1175
	1176	CASE( 'block' )
	1177
[667]	1178	DO i = nxlg, nxrg
	1179	DO j = nysg, nyng
[138]	1180	lad_s(:,j,i) = lad(:)
	1181	cdc(:,j,i) = drag_coefficient
[153]	1182	IF ( passive_scalar ) THEN
	1183	sls(:,j,i) = leaf_surface_concentration
	1184	sec(:,j,i) = scalar_exchange_coefficient
	1185	ENDIF
[138]	1186	ENDDO
	1187	ENDDO
	1188
	1189	CASE DEFAULT
	1190
	1191	!
	1192	!-- The DEFAULT case is reached either if the parameter
	1193	!-- canopy mode contains a wrong character string or if the
	1194	!-- user has coded a special case in the user interface.
	1195	!-- There, the subroutine user_init_plant_canopy checks
	1196	!-- which of these two conditions applies.
	1197	CALL user_init_plant_canopy
	1198
	1199	END SELECT
	1200
[667]	1201	CALL exchange_horiz( lad_s, nbgp )
	1202	CALL exchange_horiz( cdc, nbgp )
[138]	1203
[153]	1204	IF ( passive_scalar ) THEN
[667]	1205	CALL exchange_horiz( sls, nbgp )
	1206	CALL exchange_horiz( sec, nbgp )
[153]	1207	ENDIF
	1208
	1209	!
	1210	!-- Sharp boundaries of the plant canopy in horizontal directions
	1211	!-- In vertical direction the interpolation is retained, as the leaf
	1212	!-- area density is initialised by prescribing a vertical profile
	1213	!-- consisting of piecewise linear segments. The upper boundary
	1214	!-- of the plant canopy is now defined by lad_w(pch_index,:,:) = 0.0.
	1215
[138]	1216	DO i = nxl, nxr
	1217	DO j = nys, nyn
	1218	DO k = nzb, nzt+1
[153]	1219	IF ( lad_s(k,j,i) > 0.0 ) THEN
	1220	lad_u(k,j,i) = lad_s(k,j,i)
	1221	lad_u(k,j,i+1) = lad_s(k,j,i)
	1222	lad_v(k,j,i) = lad_s(k,j,i)
	1223	lad_v(k,j+1,i) = lad_s(k,j,i)
	1224	ENDIF
[138]	1225	ENDDO
	1226	DO k = nzb, nzt
	1227	lad_w(k,j,i) = 0.5 * ( lad_s(k+1,j,i) + lad_s(k,j,i) )
	1228	ENDDO
	1229	ENDDO
	1230	ENDDO
	1231
[153]	1232	lad_w(pch_index,:,:) = 0.0
	1233	lad_w(nzt+1,:,:) = lad_w(nzt,:,:)
[138]	1234
[667]	1235	CALL exchange_horiz( lad_u, nbgp )
	1236	CALL exchange_horiz( lad_v, nbgp )
	1237	CALL exchange_horiz( lad_w, nbgp )
[153]	1238
	1239	!
	1240	!-- Initialisation of the canopy heat source distribution
	1241	IF ( cthf /= 0.0 ) THEN
	1242	!
	1243	!-- Piecewise evaluation of the leaf area index by
	1244	!-- integration of the leaf area density
	1245	lai(:,:,:) = 0.0
[667]	1246	DO i = nxlg, nxrg
	1247	DO j = nysg, nyng
[153]	1248	DO k = pch_index-1, 0, -1
	1249	lai(k,j,i) = lai(k+1,j,i) + &
	1250	( 0.5 * ( lad_w(k+1,j,i) + &
	1251	lad_s(k+1,j,i) ) * &
	1252	( zw(k+1) - zu(k+1) ) ) + &
	1253	( 0.5 * ( lad_w(k,j,i) + &
	1254	lad_s(k+1,j,i) ) * &
	1255	( zu(k+1) - zw(k) ) )
	1256	ENDDO
	1257	ENDDO
	1258	ENDDO
	1259
	1260	!
	1261	!-- Evaluation of the upward kinematic vertical heat flux within the
	1262	!-- canopy
[667]	1263	DO i = nxlg, nxrg
	1264	DO j = nysg, nyng
[153]	1265	DO k = 0, pch_index
	1266	canopy_heat_flux(k,j,i) = cthf * &
	1267	exp( -0.6 * lai(k,j,i) )
	1268	ENDDO
	1269	ENDDO
	1270	ENDDO
	1271
	1272	!
	1273	!-- The near surface heat flux is derived from the heat flux
	1274	!-- distribution within the canopy
	1275	shf(:,:) = canopy_heat_flux(0,:,:)
	1276
	1277	IF ( ASSOCIATED( shf_m ) ) shf_m = shf
	1278
	1279	ENDIF
	1280
[138]	1281	ENDIF
	1282
	1283	!
[1]	1284	!-- If required, initialize dvrp-software
	1285	IF ( dt_dvrp /= 9999999.9 ) CALL init_dvrp
	1286
[96]	1287	IF ( ocean ) THEN
[1]	1288	!
[96]	1289	!-- Initialize quantities needed for the ocean model
	1290	CALL init_ocean
[388]	1291
[96]	1292	ELSE
	1293	!
	1294	!-- Initialize quantities for handling cloud physics
	1295	!-- This routine must be called before init_particles, because
	1296	!-- otherwise, array pt_d_t, needed in data_output_dvrp (called by
	1297	!-- init_particles) is not defined.
	1298	CALL init_cloud_physics
	1299	ENDIF
[1]	1300
	1301	!
	1302	!-- If required, initialize particles
[63]	1303	IF ( particle_advection ) CALL init_particles
[1]	1304
	1305	!
	1306	!-- Initialize quantities for special advections schemes
	1307	CALL init_advec
[667]	1308	IF ( momentum_advec == 'ws-scheme' .OR. &
	1309	scalar_advec == 'ws-scheme' ) CALL ws_init
[1]	1310
	1311	!
	1312	!-- Initialize Rayleigh damping factors
	1313	rdf = 0.0
	1314	IF ( rayleigh_damping_factor /= 0.0 ) THEN
[108]	1315	IF ( .NOT. ocean ) THEN
	1316	DO k = nzb+1, nzt
	1317	IF ( zu(k) >= rayleigh_damping_height ) THEN
	1318	rdf(k) = rayleigh_damping_factor * &
[1]	1319	( SIN( pi * 0.5 * ( zu(k) - rayleigh_damping_height ) &
	1320	/ ( zu(nzt) - rayleigh_damping_height ) )&
	1321	)**2
[108]	1322	ENDIF
	1323	ENDDO
	1324	ELSE
	1325	DO k = nzt, nzb+1, -1
	1326	IF ( zu(k) <= rayleigh_damping_height ) THEN
	1327	rdf(k) = rayleigh_damping_factor * &
	1328	( SIN( pi * 0.5 * ( rayleigh_damping_height - zu(k) ) &
	1329	/ ( rayleigh_damping_height - zu(nzb+1)))&
	1330	)**2
	1331	ENDIF
	1332	ENDDO
	1333	ENDIF
[1]	1334	ENDIF
	1335
	1336	!
[240]	1337	!-- Initialize the starting level and the vertical smoothing factor used for
	1338	!-- the external pressure gradient
	1339	dp_smooth_factor = 1.0
	1340	IF ( dp_external ) THEN
	1341	!
	1342	!-- Set the starting level dp_level_ind_b only if it has not been set before
	1343	!-- (e.g. in init_grid).
	1344	IF ( dp_level_ind_b == 0 ) THEN
	1345	ind_array = MINLOC( ABS( dp_level_b - zu ) )
	1346	dp_level_ind_b = ind_array(1) - 1 + nzb
	1347	! MINLOC uses lower array bound 1
	1348	ENDIF
	1349	IF ( dp_smooth ) THEN
	1350	dp_smooth_factor(:dp_level_ind_b) = 0.0
	1351	DO k = dp_level_ind_b+1, nzt
	1352	dp_smooth_factor(k) = 0.5 * ( 1.0 + SIN( pi * &
	1353	( REAL( k - dp_level_ind_b ) / &
	1354	REAL( nzt - dp_level_ind_b ) - 0.5 ) ) )
	1355	ENDDO
	1356	ENDIF
	1357	ENDIF
	1358
	1359	!
[1]	1360	!-- Initialize diffusivities used within the outflow damping layer in case of
	1361	!-- non-cyclic lateral boundaries. A linear increase is assumed over the first
	1362	!-- half of the width of the damping layer
[73]	1363	IF ( bc_lr == 'dirichlet/radiation' ) THEN
[1]	1364
[667]	1365	DO i = nxlg, nxrg
[73]	1366	IF ( i >= nx - outflow_damping_width ) THEN
	1367	km_damp_x(i) = km_damp_max * MIN( 1.0, &
	1368	( i - ( nx - outflow_damping_width ) ) / &
	1369	REAL( outflow_damping_width/2 ) &
	1370	)
	1371	ELSE
	1372	km_damp_x(i) = 0.0
	1373	ENDIF
	1374	ENDDO
[1]	1375
[73]	1376	ELSEIF ( bc_lr == 'radiation/dirichlet' ) THEN
[1]	1377
[667]	1378	DO i = nxlg, nxrg
[73]	1379	IF ( i <= outflow_damping_width ) THEN
	1380	km_damp_x(i) = km_damp_max * MIN( 1.0, &
	1381	( outflow_damping_width - i ) / &
	1382	REAL( outflow_damping_width/2 ) &
	1383	)
	1384	ELSE
	1385	km_damp_x(i) = 0.0
	1386	ENDIF
	1387	ENDDO
[1]	1388
[73]	1389	ENDIF
[1]	1390
[73]	1391	IF ( bc_ns == 'dirichlet/radiation' ) THEN
[1]	1392
[667]	1393	DO j = nysg, nyng
[73]	1394	IF ( j >= ny - outflow_damping_width ) THEN
	1395	km_damp_y(j) = km_damp_max * MIN( 1.0, &
	1396	( j - ( ny - outflow_damping_width ) ) / &
	1397	REAL( outflow_damping_width/2 ) &
	1398	)
	1399	ELSE
	1400	km_damp_y(j) = 0.0
[1]	1401	ENDIF
	1402	ENDDO
	1403
[73]	1404	ELSEIF ( bc_ns == 'radiation/dirichlet' ) THEN
[1]	1405
[667]	1406	DO j = nysg, nyng
[73]	1407	IF ( j <= outflow_damping_width ) THEN
	1408	km_damp_y(j) = km_damp_max * MIN( 1.0, &
	1409	( outflow_damping_width - j ) / &
	1410	REAL( outflow_damping_width/2 ) &
	1411	)
	1412	ELSE
	1413	km_damp_y(j) = 0.0
[1]	1414	ENDIF
[73]	1415	ENDDO
[1]	1416
	1417	ENDIF
	1418
	1419	!
	1420	!-- Initialize local summation arrays for UP flow_statistics. This is necessary
	1421	!-- because they may not yet have been initialized when they are called from
	1422	!-- flow_statistics (or - depending on the chosen model run - are never
	1423	!-- initialized)
	1424	sums_divnew_l = 0.0
	1425	sums_divold_l = 0.0
	1426	sums_l_l = 0.0
	1427	sums_up_fraction_l = 0.0
	1428	sums_wsts_bc_l = 0.0
	1429
	1430	!
	1431	!-- Pre-set masks for regional statistics. Default is the total model domain.
	1432	rmask = 1.0
	1433
	1434	!
[51]	1435	!-- User-defined initializing actions. Check afterwards, if maximum number
	1436	!-- of allowed timeseries is not exceeded
[1]	1437	CALL user_init
	1438
[51]	1439	IF ( dots_num > dots_max ) THEN
[254]	1440	WRITE( message_string, * ) 'number of time series quantities exceeds', &
[274]	1441	' its maximum of dots_max = ', dots_max, &
[254]	1442	' &Please increase dots_max in modules.f90.'
	1443	CALL message( 'init_3d_model', 'PA0194', 1, 2, 0, 6, 0 )
[51]	1444	ENDIF
	1445
[1]	1446	!
	1447	!-- Input binary data file is not needed anymore. This line must be placed
	1448	!-- after call of user_init!
	1449	CALL close_file( 13 )
	1450
	1451	!
	1452	!-- Compute total sum of active mask grid points
	1453	!-- ngp_2dh: number of grid points of a horizontal cross section through the
	1454	!-- total domain
	1455	!-- ngp_3d: number of grid points of the total domain
[132]	1456	ngp_2dh_outer_l = 0
	1457	ngp_2dh_outer = 0
	1458	ngp_2dh_s_inner_l = 0
	1459	ngp_2dh_s_inner = 0
	1460	ngp_2dh_l = 0
	1461	ngp_2dh = 0
[485]	1462	ngp_3d_inner_l = 0.0
[132]	1463	ngp_3d_inner = 0
	1464	ngp_3d = 0
	1465	ngp_sums = ( nz + 2 ) * ( pr_palm + max_pr_user )
[1]	1466
	1467	DO sr = 0, statistic_regions
	1468	DO i = nxl, nxr
	1469	DO j = nys, nyn
	1470	IF ( rmask(j,i,sr) == 1.0 ) THEN
	1471	!
	1472	!-- All xy-grid points
	1473	ngp_2dh_l(sr) = ngp_2dh_l(sr) + 1
	1474	!
	1475	!-- xy-grid points above topography
	1476	DO k = nzb_s_outer(j,i), nz + 1
	1477	ngp_2dh_outer_l(k,sr) = ngp_2dh_outer_l(k,sr) + 1
	1478	ENDDO
[132]	1479	DO k = nzb_s_inner(j,i), nz + 1
	1480	ngp_2dh_s_inner_l(k,sr) = ngp_2dh_s_inner_l(k,sr) + 1
	1481	ENDDO
[1]	1482	!
	1483	!-- All grid points of the total domain above topography
	1484	ngp_3d_inner_l(sr) = ngp_3d_inner_l(sr) + &
	1485	( nz - nzb_s_inner(j,i) + 2 )
	1486	ENDIF
	1487	ENDDO
	1488	ENDDO
	1489	ENDDO
	1490
	1491	sr = statistic_regions + 1
	1492	#if defined( __parallel )
[622]	1493	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
[485]	1494	CALL MPI_ALLREDUCE( ngp_2dh_l(0), ngp_2dh(0), sr, MPI_INTEGER, MPI_SUM, &
[1]	1495	comm2d, ierr )
[622]	1496	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
[485]	1497	CALL MPI_ALLREDUCE( ngp_2dh_outer_l(0,0), ngp_2dh_outer(0,0), (nz+2)*sr, &
[1]	1498	MPI_INTEGER, MPI_SUM, comm2d, ierr )
[622]	1499	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
[485]	1500	CALL MPI_ALLREDUCE( ngp_2dh_s_inner_l(0,0), ngp_2dh_s_inner(0,0), &
[132]	1501	(nz+2)*sr, MPI_INTEGER, MPI_SUM, comm2d, ierr )
[622]	1502	IF ( collective_wait ) CALL MPI_BARRIER( comm2d, ierr )
[485]	1503	CALL MPI_ALLREDUCE( ngp_3d_inner_l(0), ngp_3d_inner_tmp(0), sr, MPI_REAL, &
[1]	1504	MPI_SUM, comm2d, ierr )
[485]	1505	ngp_3d_inner = INT( ngp_3d_inner_tmp, KIND = SELECTED_INT_KIND( 18 ) )
[1]	1506	#else
[132]	1507	ngp_2dh = ngp_2dh_l
	1508	ngp_2dh_outer = ngp_2dh_outer_l
	1509	ngp_2dh_s_inner = ngp_2dh_s_inner_l
[485]	1510	ngp_3d_inner = INT( ngp_3d_inner_l, KIND = SELECTED_INT_KIND( 18 ) )
[1]	1511	#endif
	1512
[560]	1513	ngp_3d = INT ( ngp_2dh, KIND = SELECTED_INT_KIND( 18 ) ) * &
	1514	INT ( (nz + 2 ), KIND = SELECTED_INT_KIND( 18 ) )
[1]	1515
	1516	!
	1517	!-- Set a lower limit of 1 in order to avoid zero divisions in flow_statistics,
	1518	!-- buoyancy, etc. A zero value will occur for cases where all grid points of
	1519	!-- the respective subdomain lie below the surface topography
[667]	1520	ngp_2dh_outer = MAX( 1, ngp_2dh_outer(:,:) )
[631]	1521	ngp_3d_inner = MAX( INT(1, KIND = SELECTED_INT_KIND( 18 )), &
	1522	ngp_3d_inner(:) )
[667]	1523	ngp_2dh_s_inner = MAX( 1, ngp_2dh_s_inner(:,:) )
[1]	1524
[485]	1525	DEALLOCATE( ngp_2dh_l, ngp_2dh_outer_l, ngp_3d_inner_l, ngp_3d_inner_tmp )
[1]	1526
	1527
	1528	END SUBROUTINE init_3d_model

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