Home

Context Navigation

source: palm/trunk/SOURCE/subsidence_mod.f90 @ 4218

Last change on this file since 4218 was 4182, checked in by scharf, 5 years ago
corrected "Former revisions" section minor formatting in "Former revisions" section added "Author" section
Property svn:keywords set to `Id`
File size: 13.8 KB

Line
1	!> @file subsidence_mod.f90
2	!------------------------------------------------------------------------------!
3	! This file is part of the PALM model system.
4	!
5	! PALM is free software: you can redistribute it and/or modify it under the
6	! terms of the GNU General Public License as published by the Free Software
7	! Foundation, either version 3 of the License, or (at your option) any later
8	! version.
9	!
10	! PALM is distributed in the hope that it will be useful, but WITHOUT ANY
11	! WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR
12	! A PARTICULAR PURPOSE. See the GNU General Public License for more details.
13	!
14	! You should have received a copy of the GNU General Public License along with
15	! PALM. If not, see <http://www.gnu.org/licenses/>.
16	!
17	! Copyright 1997-2019 Leibniz Universitaet Hannover
18	!------------------------------------------------------------------------------!
19	!
20	! Current revisions:
21	! -----------------
22	!
23	!
24	! Former revisions:
25	! -----------------
26	! $Id: subsidence_mod.f90 4182 2019-08-22 15:20:23Z knoop $
27	! Corrected "Former revisions" section
28	!
29	! 3655 2019-01-07 16:51:22Z knoop
30	! add subroutine and variable description
31	!
32	! Revision 3.7 2009-12-11 14:15:58Z heinze
33	! Initial revision
34	!
35	! Description:
36	! ------------
37	!> Impact of large-scale subsidence or ascent as tendency term for use
38	!> in the prognostic equation of potential temperature. This enables the
39	!> construction of a constant boundary layer height z_i with time.
40	!-----------------------------------------------------------------------------!
41	MODULE subsidence_mod
42
43
44
45	IMPLICIT NONE
46
47	PRIVATE
48	PUBLIC init_w_subsidence, subsidence
49
50	INTERFACE init_w_subsidence
51	MODULE PROCEDURE init_w_subsidence
52	END INTERFACE init_w_subsidence
53
54	INTERFACE subsidence
55	MODULE PROCEDURE subsidence
56	MODULE PROCEDURE subsidence_ij
57	END INTERFACE subsidence
58
59	CONTAINS
60
61	!------------------------------------------------------------------------------!
62	! Description:
63	! ------------
64	!> Initialize vertical subsidence velocity w_subs.
65	!------------------------------------------------------------------------------!
66	SUBROUTINE init_w_subsidence
67
68	USE arrays_3d, &
69	ONLY: dzu, w_subs, zu
70
71	USE control_parameters, &
72	ONLY: message_string, ocean_mode, subs_vertical_gradient, &
73	subs_vertical_gradient_level, subs_vertical_gradient_level_i
74
75	USE indices, &
76	ONLY: nzb, nzt
77
78	USE kinds
79
80	IMPLICIT NONE
81
82	INTEGER(iwp) :: i !< loop index
83	INTEGER(iwp) :: k !< loop index
84
85	REAL(wp) :: gradient !< vertical gradient of subsidence velocity
86	REAL(wp) :: ws_surface !< subsidence velocity at the surface
87
88	IF ( .NOT. ALLOCATED( w_subs ) ) THEN
89	ALLOCATE( w_subs(nzb:nzt+1) )
90	w_subs = 0.0_wp
91	ENDIF
92
93	IF ( ocean_mode ) THEN
94	message_string = 'applying large scale vertical motion is not ' // &
95	'allowed for ocean mode'
96	CALL message( 'init_w_subsidence', 'PA0324', 2, 2, 0, 6, 0 )
97	ENDIF
98
99	!
100	!-- Compute the profile of the subsidence/ascent velocity
101	!-- using the given gradients
102	i = 1
103	gradient = 0.0_wp
104	ws_surface = 0.0_wp
105
106
107	subs_vertical_gradient_level_i(1) = 0
108	DO k = 1, nzt+1
109	IF ( i < 11 ) THEN
110	IF ( subs_vertical_gradient_level(i) < zu(k) .AND. &
111	subs_vertical_gradient_level(i) >= 0.0_wp ) THEN
112	gradient = subs_vertical_gradient(i) / 100.0_wp
113	subs_vertical_gradient_level_i(i) = k - 1
114	i = i + 1
115	ENDIF
116	ENDIF
117	IF ( gradient /= 0.0_wp ) THEN
118	IF ( k /= 1 ) THEN
119	w_subs(k) = w_subs(k-1) + dzu(k) * gradient
120	ELSE
121	w_subs(k) = ws_surface + 0.5_wp * dzu(k) * gradient
122	ENDIF
123	ELSE
124	w_subs(k) = w_subs(k-1)
125	ENDIF
126	ENDDO
127
128	!
129	!-- In case of no given gradients for the subsidence/ascent velocity,
130	!-- choose zero gradient
131	IF ( subs_vertical_gradient_level(1) == -9999999.9_wp ) THEN
132	subs_vertical_gradient_level(1) = 0.0_wp
133	ENDIF
134
135	END SUBROUTINE init_w_subsidence
136
137
138	!------------------------------------------------------------------------------!
139	! Description:
140	! ------------
141	!> Add effect of large-scale subsidence to variable.
142	!------------------------------------------------------------------------------!
143	SUBROUTINE subsidence( tendency, var, var_init, ls_index )
144
145	USE arrays_3d, &
146	ONLY: ddzu, w_subs
147
148	USE control_parameters, &
149	ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing, &
150	scalar_rayleigh_damping
151
152	USE indices, &
153	ONLY: nxl, nxlg, nxr, nxrg, nyn, nyng, nys, nysg, nzb, nzt, &
154	wall_flags_0
155
156	USE kinds
157
158	USE statistics, &
159	ONLY: sums_ls_l, weight_substep
160
161	IMPLICIT NONE
162
163	INTEGER(iwp) :: i !< loop index
164	INTEGER(iwp) :: j !< loop index
165	INTEGER(iwp) :: k !< loop index
166	INTEGER(iwp) :: ls_index !< index of large-scale subsidence in sums_ls_l
167
168	REAL(wp) :: tmp_tend !< temporary tendency
169	REAL(wp) :: tmp_grad !< temporary gradient
170
171	REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !< variable where to add subsidence
172	REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !< tendency of var
173	REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !< initialization profile of var
174	REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !< modified profile of var
175
176	var_mod = var_init
177
178	!
179	!-- Influence of w_subsidence on the current tendency term
180	DO i = nxl, nxr
181	DO j = nys, nyn
182
183	DO k = nzb+1, nzt
184	IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence
185	tmp_tend = - w_subs(k) * &
186	( var(k+1,j,i) - var(k,j,i) ) * ddzu(k+1) * &
187	MERGE( 1.0_wp, 0.0_wp, &
188	BTEST( wall_flags_0(k,j,i), 0 ) )
189	ELSE ! large-scale ascent
190	tmp_tend = - w_subs(k) * &
191	( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) * &
192	MERGE( 1.0_wp, 0.0_wp, &
193	BTEST( wall_flags_0(k,j,i), 0 ) )
194	ENDIF
195
196	tendency(k,j,i) = tendency(k,j,i) + tmp_tend
197
198	IF ( large_scale_forcing ) THEN
199	sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend &
200	* weight_substep(intermediate_timestep_count) &
201	* MERGE( 1.0_wp, 0.0_wp, &
202	BTEST( wall_flags_0(k,j,i), 0 ) )
203	ENDIF
204	ENDDO
205
206	IF ( large_scale_forcing ) THEN
207	sums_ls_l(nzt+1,ls_index) = sums_ls_l(nzt,ls_index)
208	ENDIF
209
210	ENDDO
211	ENDDO
212
213	!
214	!-- Shifting of the initial profile is especially necessary with Rayleigh
215	!-- damping switched on
216	IF ( scalar_rayleigh_damping .AND. &
217	intermediate_timestep_count == 1 ) THEN
218	DO k = nzb, nzt
219	IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence
220	var_mod(k) = var_init(k) - dt_3d * w_subs(k) * &
221	( var_init(k+1) - var_init(k) ) * ddzu(k+1)
222	ENDIF
223	ENDDO
224	!
225	!-- At the upper boundary, the initial profile is shifted with aid of
226	!-- the gradient tmp_grad. (This is ok if the gradients are linear.)
227	IF ( w_subs(nzt) < 0.0_wp ) THEN
228	tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1)
229	var_mod(nzt+1) = var_init(nzt+1) - &
230	dt_3d * w_subs(nzt+1) * tmp_grad
231	ENDIF
232
233
234	DO k = nzt+1, nzb+1, -1
235	IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent
236	var_mod(k) = var_init(k) - dt_3d * w_subs(k) * &
237	( var_init(k) - var_init(k-1) ) * ddzu(k)
238	ENDIF
239	ENDDO
240	!
241	!-- At the lower boundary shifting is not necessary because the
242	!-- subsidence velocity w_subs(nzb) vanishes.
243	IF ( w_subs(nzb+1) >= 0.0_wp ) THEN
244	var_mod(nzb) = var_init(nzb)
245	ENDIF
246
247	var_init = var_mod
248	ENDIF
249
250
251	END SUBROUTINE subsidence
252
253	!------------------------------------------------------------------------------!
254	! Description:
255	! ------------
256	!> Add effect of large-scale subsidence to variable.
257	!------------------------------------------------------------------------------!
258	SUBROUTINE subsidence_ij( i, j, tendency, var, var_init, ls_index )
259
260	USE arrays_3d, &
261	ONLY: ddzu, w_subs
262
263	USE control_parameters, &
264	ONLY: dt_3d, intermediate_timestep_count, large_scale_forcing, &
265	scalar_rayleigh_damping
266
267	USE indices, &
268	ONLY: nxl, nxlg, nxrg, nyng, nys, nysg, nzb, nzt, wall_flags_0
269
270	USE kinds
271
272	USE statistics, &
273	ONLY: sums_ls_l, weight_substep
274
275	IMPLICIT NONE
276
277	INTEGER(iwp) :: i !< loop variable
278	INTEGER(iwp) :: j !< loop variable
279	INTEGER(iwp) :: k !< loop variable
280	INTEGER(iwp) :: ls_index !< index of large-scale subsidence in sums_ls_l
281
282	REAL(wp) :: tmp_tend !< temporary tendency
283	REAL(wp) :: tmp_grad !< temporary gradient
284
285	REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: var !< variable where to add subsidence
286	REAL(wp), DIMENSION(nzb:nzt+1,nysg:nyng,nxlg:nxrg) :: tendency !< tendency of var
287	REAL(wp), DIMENSION(nzb:nzt+1) :: var_init !< initialization profile of var
288	REAL(wp), DIMENSION(nzb:nzt+1) :: var_mod !< modified profile of var
289
290	var_mod = var_init
291
292	!
293	!-- Influence of w_subsidence on the current tendency term
294	DO k = nzb+1, nzt
295	IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence
296	tmp_tend = - w_subs(k) * ( var(k+1,j,i) - var(k,j,i) ) &
297	* ddzu(k+1) &
298	* MERGE( 1.0_wp, 0.0_wp, &
299	BTEST( wall_flags_0(k,j,i), 0 ) )
300	ELSE ! large-scale ascent
301	tmp_tend = - w_subs(k) * ( var(k,j,i) - var(k-1,j,i) ) * ddzu(k) &
302	* MERGE( 1.0_wp, 0.0_wp, &
303	BTEST( wall_flags_0(k,j,i), 0 ) )
304	ENDIF
305
306	tendency(k,j,i) = tendency(k,j,i) + tmp_tend
307
308	IF ( large_scale_forcing ) THEN
309	sums_ls_l(k,ls_index) = sums_ls_l(k,ls_index) + tmp_tend &
310	* weight_substep(intermediate_timestep_count)&
311	* MERGE( 1.0_wp, 0.0_wp, &
312	BTEST( wall_flags_0(k,j,i), 0 ) )
313	ENDIF
314	ENDDO
315
316	IF ( large_scale_forcing ) THEN
317	sums_ls_l(nzt+1,ls_index) = sums_ls_l(nzt,ls_index)
318	ENDIF
319
320	!
321	!-- Shifting of the initial profile is especially necessary with Rayleigh
322	!-- damping switched on
323	IF ( scalar_rayleigh_damping .AND. &
324	intermediate_timestep_count == 1 ) THEN
325	IF ( i == nxl .AND. j == nys ) THEN ! shifting only once per PE
326
327	DO k = nzb, nzt
328	IF ( w_subs(k) < 0.0_wp ) THEN ! large-scale subsidence
329	var_mod(k) = var_init(k) - dt_3d * w_subs(k) * &
330	( var_init(k+1) - var_init(k) ) * ddzu(k+1)
331	ENDIF
332	ENDDO
333	!
334	!-- At the upper boundary, the initial profile is shifted with aid of
335	!-- the gradient tmp_grad. (This is ok if the gradients are linear.)
336	IF ( w_subs(nzt) < 0.0_wp ) THEN
337	tmp_grad = ( var_init(nzt+1) - var_init(nzt) ) * ddzu(nzt+1)
338	var_mod(nzt+1) = var_init(nzt+1) - &
339	dt_3d * w_subs(nzt+1) * tmp_grad
340	ENDIF
341
342
343	DO k = nzt+1, nzb+1, -1
344	IF ( w_subs(k) >= 0.0_wp ) THEN ! large-scale ascent
345	var_mod(k) = var_init(k) - dt_3d * w_subs(k) * &
346	( var_init(k) - var_init(k-1) ) * ddzu(k)
347	ENDIF
348	ENDDO
349	!
350	!-- At the lower boundary shifting is not necessary because the
351	!-- subsidence velocity w_subs(nzb) vanishes.
352	IF ( w_subs(nzb+1) >= 0.0_wp ) THEN
353	var_mod(nzb) = var_init(nzb)
354	ENDIF
355
356	var_init = var_mod
357
358	ENDIF
359	ENDIF
360
361	END SUBROUTINE subsidence_ij
362
363
364	END MODULE subsidence_mod

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

Download in other formats:

| Impressum | ©Leibniz Universität Hannover |