1 | MODULE dynspg_ts |
---|
2 | !!====================================================================== |
---|
3 | !! *** MODULE dynspg_ts *** |
---|
4 | !! Ocean dynamics: surface pressure gradient trend |
---|
5 | !!====================================================================== |
---|
6 | !! History : 9.0 ! 04-12 (L. Bessieres, G. Madec) Original code |
---|
7 | !! " " ! 05-11 (V. Garnier, G. Madec) optimization |
---|
8 | !! 9.0 ! 06-08 (S. Masson) distributed restart using iom |
---|
9 | !! 9.0 ! 08-01 (R. Benshila) change averaging method |
---|
10 | !!--------------------------------------------------------------------- |
---|
11 | #if defined key_dynspg_ts || defined key_esopa |
---|
12 | !!---------------------------------------------------------------------- |
---|
13 | !! 'key_dynspg_ts' free surface cst volume with time splitting |
---|
14 | !!---------------------------------------------------------------------- |
---|
15 | !!---------------------------------------------------------------------- |
---|
16 | !! dyn_spg_ts : compute surface pressure gradient trend using a time- |
---|
17 | !! splitting scheme and add to the general trend |
---|
18 | !! ts_rst : read/write the time-splitting restart fields in the ocean restart file |
---|
19 | !!---------------------------------------------------------------------- |
---|
20 | !! * Modules used |
---|
21 | USE oce ! ocean dynamics and tracers |
---|
22 | USE dom_oce ! ocean space and time domain |
---|
23 | USE sbc_oce ! surface boundary condition: ocean |
---|
24 | USE dynspg_oce ! surface pressure gradient variables |
---|
25 | USE phycst ! physical constants |
---|
26 | USE domvvl ! variable volume |
---|
27 | USE obcdta ! open boundary condition data |
---|
28 | USE obcfla ! Flather open boundary condition |
---|
29 | USE dynvor ! vorticity term |
---|
30 | USE obc_oce ! Lateral open boundary condition |
---|
31 | USE obc_par ! open boundary condition parameters |
---|
32 | USE lib_mpp ! distributed memory computing library |
---|
33 | USE lbclnk ! ocean lateral boundary conditions (or mpp link) |
---|
34 | USE prtctl ! Print control |
---|
35 | USE in_out_manager ! I/O manager |
---|
36 | USE iom |
---|
37 | USE restart ! only for lrst_oce |
---|
38 | |
---|
39 | IMPLICIT NONE |
---|
40 | PRIVATE |
---|
41 | |
---|
42 | PUBLIC dyn_spg_ts ! routine called by step.F90 |
---|
43 | PUBLIC ts_rst ! routine called by istate.F90 |
---|
44 | |
---|
45 | REAL(wp), DIMENSION(jpi,jpj) :: ftnw, ftne, & ! triad of coriolis parameter |
---|
46 | & ftsw, ftse ! (only used with een vorticity scheme) |
---|
47 | |
---|
48 | |
---|
49 | !! * Substitutions |
---|
50 | # include "domzgr_substitute.h90" |
---|
51 | # include "vectopt_loop_substitute.h90" |
---|
52 | !!---------------------------------------------------------------------- |
---|
53 | !! OPA 9.0 , LOCEAN-IPSL (2005) |
---|
54 | !! $Id$ |
---|
55 | !! This software is governed by the CeCILL licence see modipsl/doc/NEMO_CeCILL.txt |
---|
56 | !!---------------------------------------------------------------------- |
---|
57 | |
---|
58 | CONTAINS |
---|
59 | |
---|
60 | SUBROUTINE dyn_spg_ts( kt ) |
---|
61 | !!---------------------------------------------------------------------- |
---|
62 | !! *** routine dyn_spg_ts *** |
---|
63 | !! |
---|
64 | !! ** Purpose : Compute the now trend due to the surface pressure |
---|
65 | !! gradient in case of free surface formulation with time-splitting. |
---|
66 | !! Add it to the general trend of momentum equation. |
---|
67 | !! Compute the free surface. |
---|
68 | !! |
---|
69 | !! ** Method : Free surface formulation with time-splitting |
---|
70 | !! -1- Save the vertically integrated trend. This general trend is |
---|
71 | !! held constant over the barotropic integration. |
---|
72 | !! The Coriolis force is removed from the general trend as the |
---|
73 | !! surface gradient and the Coriolis force are updated within |
---|
74 | !! the barotropic integration. |
---|
75 | !! -2- Barotropic loop : updates of sea surface height (ssha_e) and |
---|
76 | !! barotropic transports (ua_e and va_e) through barotropic |
---|
77 | !! momentum and continuity integration. Barotropic former |
---|
78 | !! variables are time averaging over the full barotropic cycle |
---|
79 | !! (= 2 * baroclinic time step) and saved in zsshX_b, zuX_b |
---|
80 | !! and zvX_b (X specifying after, now or before). |
---|
81 | !! -3- Update of sea surface height from time averaged barotropic |
---|
82 | !! variables. |
---|
83 | !! - apply lateral boundary conditions on sshn. |
---|
84 | !! -4- The new general trend becomes : |
---|
85 | !! ua = ua - sum_k(ua)/H + ( zua_b - sum_k(ub) )/H |
---|
86 | !! |
---|
87 | !! ** Action : - Update (ua,va) with the surf. pressure gradient trend |
---|
88 | !! |
---|
89 | !! References : Griffies et al., (2003): A technical guide to MOM4. NOAA/GFDL |
---|
90 | !!--------------------------------------------------------------------- |
---|
91 | INTEGER, INTENT( in ) :: kt ! ocean time-step index |
---|
92 | |
---|
93 | !! * Local declarations |
---|
94 | INTEGER :: ji, jj, jk, jit ! dummy loop indices |
---|
95 | INTEGER :: icycle, ibaro ! temporary scalar |
---|
96 | REAL(wp) :: & |
---|
97 | zraur, zcoef, z2dt_e, z2dt_b, zfac25, & ! temporary scalars |
---|
98 | zfact1, zspgu, zcubt, zx1, zy1, & ! " " |
---|
99 | zfact2, zspgv, zcvbt, zx2, zy2 ! " " |
---|
100 | REAL(wp), DIMENSION(jpi,jpj) :: & |
---|
101 | zcu, zcv, zwx, zwy, zhdiv, & ! temporary arrays |
---|
102 | zua, zva, zub, zvb, & ! " " |
---|
103 | zssha_b, zua_b, zva_b, & ! " " |
---|
104 | zsshb_e, zub_e, zvb_e, & ! " " |
---|
105 | zun_e, zvn_e ! " " |
---|
106 | !! Variable volume |
---|
107 | REAL(wp), DIMENSION(jpi,jpj) :: & |
---|
108 | zspgu_1, zspgv_1, zsshun_e, zsshvn_e, hu_e, hv_e ! 2D workspace |
---|
109 | REAL(wp), DIMENSION(jpi,jpj,jpk) :: zfse3un_e, zfse3vn_e ! 3D workspace |
---|
110 | !!---------------------------------------------------------------------- |
---|
111 | |
---|
112 | ! Arrays initialization |
---|
113 | ! --------------------- |
---|
114 | zua_b(:,:) = 0.e0 ; zub_e(:,:) = 0.e0 ; zun_e(:,:) = 0.e0 |
---|
115 | zva_b(:,:) = 0.e0 ; zvb_e(:,:) = 0.e0 ; zvn_e(:,:) = 0.e0 |
---|
116 | zhdiv(:,:) = 0.e0 |
---|
117 | |
---|
118 | |
---|
119 | IF( kt == nit000 ) THEN |
---|
120 | ! |
---|
121 | IF(lwp) WRITE(numout,*) |
---|
122 | IF(lwp) WRITE(numout,*) 'dyn_spg_ts : surface pressure gradient trend' |
---|
123 | IF(lwp) WRITE(numout,*) '~~~~~~~~~~ free surface with time splitting' |
---|
124 | IF(lwp) WRITE(numout,*) ' Number of sub cycle in 1 time-step (2 rdt) : icycle = ', FLOOR( 2*rdt/rdtbt ) |
---|
125 | |
---|
126 | CALL ts_rst( nit000, 'READ' ) ! read or initialize the following fields: |
---|
127 | ! ! sshb, sshn, sshb_b, sshn_b, un_b, vn_b |
---|
128 | |
---|
129 | ssha_e(:,:) = sshn(:,:) |
---|
130 | ua_e(:,:) = un_b(:,:) |
---|
131 | va_e(:,:) = vn_b(:,:) |
---|
132 | |
---|
133 | IF( ln_dynvor_een ) THEN |
---|
134 | ftne(1,:) = 0.e0 ; ftnw(1,:) = 0.e0 ; ftse(1,:) = 0.e0 ; ftsw(1,:) = 0.e0 |
---|
135 | DO jj = 2, jpj |
---|
136 | DO ji = fs_2, jpi ! vector opt. |
---|
137 | ftne(ji,jj) = ( ff(ji-1,jj ) + ff(ji ,jj ) + ff(ji ,jj-1) ) / 3. |
---|
138 | ftnw(ji,jj) = ( ff(ji-1,jj-1) + ff(ji-1,jj ) + ff(ji ,jj ) ) / 3. |
---|
139 | ftse(ji,jj) = ( ff(ji ,jj ) + ff(ji ,jj-1) + ff(ji-1,jj-1) ) / 3. |
---|
140 | ftsw(ji,jj) = ( ff(ji ,jj-1) + ff(ji-1,jj-1) + ff(ji-1,jj ) ) / 3. |
---|
141 | END DO |
---|
142 | END DO |
---|
143 | ENDIF |
---|
144 | ! |
---|
145 | ENDIF |
---|
146 | |
---|
147 | ! Substract the surface pressure gradient from the momentum |
---|
148 | ! --------------------------------------------------------- |
---|
149 | IF( lk_vvl ) THEN ! Variable volume |
---|
150 | |
---|
151 | ! 0. Local initialization |
---|
152 | ! ----------------------- |
---|
153 | zspgu_1(:,:) = 0.e0 |
---|
154 | zspgv_1(:,:) = 0.e0 |
---|
155 | |
---|
156 | ! 1. Surface pressure gradient (now) |
---|
157 | ! ---------------------------- |
---|
158 | DO jj = 2, jpjm1 |
---|
159 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
160 | zspgu_1(ji,jj) = -grav * ( ( rhd(ji+1,jj ,1) + 1 ) * sshn(ji+1,jj ) & |
---|
161 | & - ( rhd(ji ,jj ,1) + 1 ) * sshn(ji ,jj ) ) / e1u(ji,jj) |
---|
162 | zspgv_1(ji,jj) = -grav * ( ( rhd(ji ,jj+1,1) + 1 ) * sshn(ji ,jj+1) & |
---|
163 | & - ( rhd(ji ,jj ,1) + 1 ) * sshn(ji ,jj ) ) / e2v(ji,jj) |
---|
164 | END DO |
---|
165 | END DO |
---|
166 | |
---|
167 | ! 2. Substract the surface pressure trend from the general trend |
---|
168 | ! ------------------------------------------------------ |
---|
169 | DO jk = 1, jpkm1 |
---|
170 | DO jj = 2, jpjm1 |
---|
171 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
172 | ua(ji,jj,jk) = ua(ji,jj,jk) - zspgu_1(ji,jj) |
---|
173 | va(ji,jj,jk) = va(ji,jj,jk) - zspgv_1(ji,jj) |
---|
174 | END DO |
---|
175 | END DO |
---|
176 | END DO |
---|
177 | |
---|
178 | ENDIF |
---|
179 | |
---|
180 | ! Local constant initialization |
---|
181 | ! -------------------------------- |
---|
182 | z2dt_b = 2.0 * rdt ! baroclinic time step |
---|
183 | IF ( neuler == 0 .AND. kt == nit000 ) z2dt_b = rdt |
---|
184 | zfact1 = 0.5 * 0.25 ! coefficient for vorticity estimates |
---|
185 | zfact2 = 0.5 * 0.5 |
---|
186 | zraur = 1. / rauw ! 1 / volumic mass of pure water |
---|
187 | |
---|
188 | ! ----------------------------------------------------------------------------- |
---|
189 | ! Phase 1 : Coupling between general trend and barotropic estimates (1st step) |
---|
190 | ! ----------------------------------------------------------------------------- |
---|
191 | |
---|
192 | ! Vertically integrated quantities |
---|
193 | ! -------------------------------- |
---|
194 | zua(:,:) = 0.e0 |
---|
195 | zva(:,:) = 0.e0 |
---|
196 | zub(:,:) = 0.e0 |
---|
197 | zvb(:,:) = 0.e0 |
---|
198 | zwx(:,:) = 0.e0 |
---|
199 | zwy(:,:) = 0.e0 |
---|
200 | |
---|
201 | ! vertical sum |
---|
202 | IF( lk_vopt_loop ) THEN ! vector opt., forced unroll |
---|
203 | DO jk = 1, jpkm1 |
---|
204 | DO ji = 1, jpij |
---|
205 | ! ! Vertically integrated momentum trends |
---|
206 | zua(ji,1) = zua(ji,1) + fse3u(ji,1,jk) * umask(ji,1,jk) * ua(ji,1,jk) |
---|
207 | zva(ji,1) = zva(ji,1) + fse3v(ji,1,jk) * vmask(ji,1,jk) * va(ji,1,jk) |
---|
208 | ! ! Vertically integrated transports (before) |
---|
209 | zub(ji,1) = zub(ji,1) + fse3u(ji,1,jk) * ub(ji,1,jk) |
---|
210 | zvb(ji,1) = zvb(ji,1) + fse3v(ji,1,jk) * vb(ji,1,jk) |
---|
211 | ! ! Planetary vorticity transport fluxes (now) |
---|
212 | zwx(ji,1) = zwx(ji,1) + e2u(ji,1) * fse3u(ji,1,jk) * un(ji,1,jk) |
---|
213 | zwy(ji,1) = zwy(ji,1) + e1v(ji,1) * fse3v(ji,1,jk) * vn(ji,1,jk) |
---|
214 | END DO |
---|
215 | END DO |
---|
216 | ELSE ! No vector opt. |
---|
217 | DO jk = 1, jpkm1 |
---|
218 | ! ! Vertically integrated momentum trends |
---|
219 | zua(:,:) = zua(:,:) + fse3u(:,:,jk) * umask(:,:,jk) * ua(:,:,jk) |
---|
220 | zva(:,:) = zva(:,:) + fse3v(:,:,jk) * vmask(:,:,jk) * va(:,:,jk) |
---|
221 | ! ! Vertically integrated transports (before) |
---|
222 | zub(:,:) = zub(:,:) + fse3u(:,:,jk) * ub(:,:,jk) |
---|
223 | zvb(:,:) = zvb(:,:) + fse3v(:,:,jk) * vb(:,:,jk) |
---|
224 | ! ! Planetary vorticity (now) |
---|
225 | zwx(:,:) = zwx(:,:) + e2u(:,:) * fse3u(:,:,jk) * un(:,:,jk) |
---|
226 | zwy(:,:) = zwy(:,:) + e1v(:,:) * fse3v(:,:,jk) * vn(:,:,jk) |
---|
227 | END DO |
---|
228 | ENDIF |
---|
229 | |
---|
230 | IF( ln_dynvor_ene .OR. ln_dynvor_mix ) THEN ! energy conserving or mixed scheme |
---|
231 | DO jj = 2, jpjm1 |
---|
232 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
233 | zy1 = ( zwy(ji,jj-1) + zwy(ji+1,jj-1) ) / e1u(ji,jj) |
---|
234 | zy2 = ( zwy(ji,jj ) + zwy(ji+1,jj ) ) / e1u(ji,jj) |
---|
235 | zx1 = ( zwx(ji-1,jj) + zwx(ji-1,jj+1) ) / e2v(ji,jj) |
---|
236 | zx2 = ( zwx(ji ,jj) + zwx(ji ,jj+1) ) / e2v(ji,jj) |
---|
237 | ! energy conserving formulation for planetary vorticity term |
---|
238 | zcu(ji,jj) = zfact2 * ( ff(ji ,jj-1) * zy1 + ff(ji,jj) * zy2 ) |
---|
239 | zcv(ji,jj) =-zfact2 * ( ff(ji-1,jj ) * zx1 + ff(ji,jj) * zx2 ) |
---|
240 | END DO |
---|
241 | END DO |
---|
242 | ! |
---|
243 | ELSEIF ( ln_dynvor_ens ) THEN ! enstrophy conserving scheme |
---|
244 | DO jj = 2, jpjm1 |
---|
245 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
246 | zy1 = zfact1 * ( zwy(ji ,jj-1) + zwy(ji+1,jj-1) & |
---|
247 | + zwy(ji ,jj ) + zwy(ji+1,jj ) ) / e1u(ji,jj) |
---|
248 | zx1 =-zfact1 * ( zwx(ji-1,jj ) + zwx(ji-1,jj+1) & |
---|
249 | + zwx(ji ,jj ) + zwx(ji ,jj+1) ) / e2v(ji,jj) |
---|
250 | zcu(ji,jj) = zy1 * ( ff(ji ,jj-1) + ff(ji,jj) ) |
---|
251 | zcv(ji,jj) = zx1 * ( ff(ji-1,jj ) + ff(ji,jj) ) |
---|
252 | END DO |
---|
253 | END DO |
---|
254 | ! |
---|
255 | ELSEIF ( ln_dynvor_een ) THEN ! enstrophy and energy conserving scheme |
---|
256 | zfac25 = 0.25 |
---|
257 | DO jj = 2, jpjm1 |
---|
258 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
259 | zcu(ji,jj) = + zfac25 / e1u(ji,jj) & |
---|
260 | & * ( ftne(ji,jj ) * zwy(ji ,jj ) + ftnw(ji+1,jj) * zwy(ji+1,jj ) & |
---|
261 | & + ftse(ji,jj ) * zwy(ji ,jj-1) + ftsw(ji+1,jj) * zwy(ji+1,jj-1) ) |
---|
262 | zcv(ji,jj) = - zfac25 / e2v(ji,jj) & |
---|
263 | & * ( ftsw(ji,jj+1) * zwx(ji-1,jj+1) + ftse(ji,jj+1) * zwx(ji ,jj+1) & |
---|
264 | & + ftnw(ji,jj ) * zwx(ji-1,jj ) + ftne(ji,jj ) * zwx(ji ,jj ) ) |
---|
265 | END DO |
---|
266 | END DO |
---|
267 | ! |
---|
268 | ENDIF |
---|
269 | |
---|
270 | |
---|
271 | ! Remove barotropic trend from general momentum trend |
---|
272 | ! --------------------------------------------------- |
---|
273 | DO jk = 1 , jpkm1 |
---|
274 | DO jj = 2, jpjm1 |
---|
275 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
276 | ua(ji,jj,jk) = ua(ji,jj,jk) - zua(ji,jj) * hur(ji,jj) |
---|
277 | va(ji,jj,jk) = va(ji,jj,jk) - zva(ji,jj) * hvr(ji,jj) |
---|
278 | END DO |
---|
279 | END DO |
---|
280 | END DO |
---|
281 | |
---|
282 | ! Remove coriolis term from barotropic trend |
---|
283 | ! ------------------------------------------ |
---|
284 | DO jj = 2, jpjm1 |
---|
285 | DO ji = fs_2, fs_jpim1 |
---|
286 | zua(ji,jj) = zua(ji,jj) - zcu(ji,jj) |
---|
287 | zva(ji,jj) = zva(ji,jj) - zcv(ji,jj) |
---|
288 | END DO |
---|
289 | END DO |
---|
290 | |
---|
291 | ! ----------------------------------------------------------------------- |
---|
292 | ! Phase 2 : Integration of the barotropic equations with time splitting |
---|
293 | ! ----------------------------------------------------------------------- |
---|
294 | |
---|
295 | ! Initialisations |
---|
296 | !---------------- |
---|
297 | ! Number of iteration of the barotropic loop |
---|
298 | ibaro = FLOOR( rdt / rdtbt ) |
---|
299 | icycle = 3 /2 * ibaro |
---|
300 | |
---|
301 | ! variables for the barotropic equations |
---|
302 | zsshb_e(:,:) = sshn_b(:,:) ! (barotropic) sea surface height (before and now) |
---|
303 | sshn_e (:,:) = sshn_b(:,:) |
---|
304 | zub_e (:,:) = un_b (:,:) ! barotropic transports issued from the barotropic equations (before and now) |
---|
305 | zvb_e (:,:) = vn_b (:,:) |
---|
306 | zun_e (:,:) = un_b (:,:) |
---|
307 | zvn_e (:,:) = vn_b (:,:) |
---|
308 | zssha_b(:,:) = 0.e0 |
---|
309 | zua_b (:,:) = 0.e0 |
---|
310 | zva_b (:,:) = 0.e0 |
---|
311 | IF( lk_vvl ) THEN |
---|
312 | zsshun_e(:,:) = sshu (:,:) ! (barotropic) sea surface height (now) at u-point |
---|
313 | zsshvn_e(:,:) = sshv (:,:) ! (barotropic) sea surface height (now) at v-point |
---|
314 | hu_e(:,:) = hu (:,:) ! (barotropic) ocean depth at u-point |
---|
315 | hv_e(:,:) = hv (:,:) ! (barotropic) ocean depth at v-point |
---|
316 | zfse3un_e(:,:,:) = fse3u(:,:,:) ! (barotropic) scale factors at u-point |
---|
317 | zfse3un_e(:,:,:) = fse3v(:,:,:) ! (barotropic) scale factors at v-point |
---|
318 | ENDIF |
---|
319 | |
---|
320 | ! set ssh corrections to 0 |
---|
321 | ! ssh corrections are applied to normal velocities (Flather's algorithm) and averaged over the barotropic loop |
---|
322 | #if defined key_obc |
---|
323 | IF( lp_obc_east ) sshfoe_b(:,:) = 0.e0 |
---|
324 | IF( lp_obc_west ) sshfow_b(:,:) = 0.e0 |
---|
325 | IF( lp_obc_south ) sshfos_b(:,:) = 0.e0 |
---|
326 | IF( lp_obc_north ) sshfon_b(:,:) = 0.e0 |
---|
327 | #endif |
---|
328 | |
---|
329 | ! Barotropic integration over 2 baroclinic time steps |
---|
330 | ! --------------------------------------------------- |
---|
331 | |
---|
332 | ! ! ==================== ! |
---|
333 | DO jit = 1, icycle ! sub-time-step loop ! |
---|
334 | ! ! ==================== ! |
---|
335 | z2dt_e = 2. * rdtbt |
---|
336 | IF ( jit == 1 ) z2dt_e = rdtbt |
---|
337 | |
---|
338 | ! Time interpolation of open boundary condition data |
---|
339 | IF( lk_obc ) CALL obc_dta_bt( kt, jit ) |
---|
340 | |
---|
341 | ! Horizontal divergence of barotropic transports |
---|
342 | !-------------------------------------------------- |
---|
343 | DO jj = 2, jpjm1 |
---|
344 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
345 | zhdiv(ji,jj) = ( e2u(ji ,jj ) * zun_e(ji ,jj) & |
---|
346 | & -e2u(ji-1,jj ) * zun_e(ji-1,jj) & |
---|
347 | & +e1v(ji ,jj ) * zvn_e(ji ,jj) & |
---|
348 | & -e1v(ji ,jj-1) * zvn_e(ji ,jj-1) ) & |
---|
349 | & / (e1t(ji,jj)*e2t(ji,jj)) |
---|
350 | END DO |
---|
351 | END DO |
---|
352 | |
---|
353 | #if defined key_obc |
---|
354 | ! open boundaries (div must be zero behind the open boundary) |
---|
355 | ! mpp remark: The zeroing of hdiv can probably be extended to 1->jpi/jpj for the correct row/column |
---|
356 | IF( lp_obc_east ) zhdiv(nie0p1:nie1p1,nje0 :nje1) = 0.e0 ! east |
---|
357 | IF( lp_obc_west ) zhdiv(niw0 :niw1 ,njw0 :njw1) = 0.e0 ! west |
---|
358 | IF( lp_obc_north ) zhdiv(nin0 :nin1 ,njn0p1:njn1p1) = 0.e0 ! north |
---|
359 | IF( lp_obc_south ) zhdiv(nis0 :nis1 ,njs0 :njs1) = 0.e0 ! south |
---|
360 | #endif |
---|
361 | |
---|
362 | ! Sea surface height from the barotropic system |
---|
363 | !---------------------------------------------- |
---|
364 | DO jj = 2, jpjm1 |
---|
365 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
366 | ssha_e(ji,jj) = ( zsshb_e(ji,jj) - z2dt_e * ( zraur * emp(ji,jj) & |
---|
367 | & + zhdiv(ji,jj) ) ) * tmask(ji,jj,1) |
---|
368 | END DO |
---|
369 | END DO |
---|
370 | |
---|
371 | ! evolution of the barotropic transport ( following the vorticity scheme used) |
---|
372 | ! ---------------------------------------------------------------------------- |
---|
373 | zwx(:,:) = e2u(:,:) * zun_e(:,:) |
---|
374 | zwy(:,:) = e1v(:,:) * zvn_e(:,:) |
---|
375 | |
---|
376 | IF( ln_dynvor_ene .OR. ln_dynvor_mix ) THEN ! energy conserving or mixed scheme |
---|
377 | DO jj = 2, jpjm1 |
---|
378 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
379 | ! surface pressure gradient |
---|
380 | IF( lk_vvl) THEN |
---|
381 | zspgu = -grav * ( ( rhd(ji+1,jj,1) + 1 ) * sshn_e(ji+1,jj) & |
---|
382 | & - ( rhd(ji,jj,1) + 1 ) * sshn_e(ji,jj) ) * hu_e(ji,jj) / e1u(ji,jj) |
---|
383 | zspgv = -grav * ( ( rhd(ji,jj+1,1) + 1 ) * sshn_e(ji,jj+1) & |
---|
384 | & - ( rhd(ji,jj,1) + 1 ) * sshn_e(ji,jj) ) * hv_e(ji,jj) / e2v(ji,jj) |
---|
385 | ELSE |
---|
386 | zspgu = -grav * ( sshn_e(ji+1,jj) - sshn_e(ji,jj) ) * hu(ji,jj) / e1u(ji,jj) |
---|
387 | zspgv = -grav * ( sshn_e(ji,jj+1) - sshn_e(ji,jj) ) * hv(ji,jj) / e2v(ji,jj) |
---|
388 | ENDIF |
---|
389 | ! energy conserving formulation for planetary vorticity term |
---|
390 | zy1 = ( zwy(ji ,jj-1) + zwy(ji+1,jj-1) ) / e1u(ji,jj) |
---|
391 | zy2 = ( zwy(ji ,jj ) + zwy(ji+1,jj ) ) / e1u(ji,jj) |
---|
392 | zx1 = ( zwx(ji-1,jj ) + zwx(ji-1,jj+1) ) / e2v(ji,jj) |
---|
393 | zx2 = ( zwx(ji ,jj ) + zwx(ji ,jj+1) ) / e2v(ji,jj) |
---|
394 | zcubt = zfact2 * ( ff(ji ,jj-1) * zy1 + ff(ji,jj) * zy2 ) |
---|
395 | zcvbt =-zfact2 * ( ff(ji-1,jj ) * zx1 + ff(ji,jj) * zx2 ) |
---|
396 | ! after transports |
---|
397 | ua_e(ji,jj) = ( zub_e(ji,jj) + z2dt_e * ( zcubt + zspgu + zua(ji,jj) ) ) * umask(ji,jj,1) |
---|
398 | va_e(ji,jj) = ( zvb_e(ji,jj) + z2dt_e * ( zcvbt + zspgv + zva(ji,jj) ) ) * vmask(ji,jj,1) |
---|
399 | END DO |
---|
400 | END DO |
---|
401 | ! |
---|
402 | ELSEIF ( ln_dynvor_ens ) THEN ! enstrophy conserving scheme |
---|
403 | DO jj = 2, jpjm1 |
---|
404 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
405 | ! surface pressure gradient |
---|
406 | IF( lk_vvl) THEN |
---|
407 | zspgu = -grav * ( ( rhd(ji+1,jj,1) + 1 ) * sshn_e(ji+1,jj) & |
---|
408 | & - ( rhd(ji,jj,1) + 1 ) * sshn_e(ji,jj) ) * hu_e(ji,jj) / e1u(ji,jj) |
---|
409 | zspgv = -grav * ( ( rhd(ji,jj+1,1) + 1 ) * sshn_e(ji,jj+1) & |
---|
410 | & - ( rhd(ji,jj,1) + 1 ) * sshn_e(ji,jj) ) * hv_e(ji,jj) / e2v(ji,jj) |
---|
411 | ELSE |
---|
412 | zspgu = -grav * ( sshn_e(ji+1,jj) - sshn_e(ji,jj) ) * hu(ji,jj) / e1u(ji,jj) |
---|
413 | zspgv = -grav * ( sshn_e(ji,jj+1) - sshn_e(ji,jj) ) * hv(ji,jj) / e2v(ji,jj) |
---|
414 | ENDIF |
---|
415 | ! enstrophy conserving formulation for planetary vorticity term |
---|
416 | zy1 = zfact1 * ( zwy(ji ,jj-1) + zwy(ji+1,jj-1) & |
---|
417 | + zwy(ji ,jj ) + zwy(ji+1,jj ) ) / e1u(ji,jj) |
---|
418 | zx1 =-zfact1 * ( zwx(ji-1,jj ) + zwx(ji-1,jj+1) & |
---|
419 | + zwx(ji ,jj ) + zwx(ji ,jj+1) ) / e2v(ji,jj) |
---|
420 | zcubt = zy1 * ( ff(ji ,jj-1) + ff(ji,jj) ) |
---|
421 | zcvbt = zx1 * ( ff(ji-1,jj ) + ff(ji,jj) ) |
---|
422 | ! after transports |
---|
423 | ua_e(ji,jj) = ( zub_e(ji,jj) + z2dt_e * ( zcubt + zspgu + zua(ji,jj) ) ) * umask(ji,jj,1) |
---|
424 | va_e(ji,jj) = ( zvb_e(ji,jj) + z2dt_e * ( zcvbt + zspgv + zva(ji,jj) ) ) * vmask(ji,jj,1) |
---|
425 | END DO |
---|
426 | END DO |
---|
427 | ! |
---|
428 | ELSEIF ( ln_dynvor_een ) THEN ! energy and enstrophy conserving scheme |
---|
429 | zfac25 = 0.25 |
---|
430 | DO jj = 2, jpjm1 |
---|
431 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
432 | ! surface pressure gradient |
---|
433 | IF( lk_vvl) THEN |
---|
434 | zspgu = -grav * ( ( rhd(ji+1,jj,1) + 1 ) * sshn_e(ji+1,jj) & |
---|
435 | & - ( rhd(ji,jj,1) + 1 ) * sshn_e(ji,jj) ) * hu_e(ji,jj) / e1u(ji,jj) |
---|
436 | zspgv = -grav * ( ( rhd(ji,jj+1,1) + 1 ) * sshn_e(ji,jj+1) & |
---|
437 | & - ( rhd(ji,jj,1) + 1 ) * sshn_e(ji,jj) ) * hv_e(ji,jj) / e2v(ji,jj) |
---|
438 | ELSE |
---|
439 | zspgu = -grav * ( sshn_e(ji+1,jj) - sshn_e(ji,jj) ) * hu(ji,jj) / e1u(ji,jj) |
---|
440 | zspgv = -grav * ( sshn_e(ji,jj+1) - sshn_e(ji,jj) ) * hv(ji,jj) / e2v(ji,jj) |
---|
441 | ENDIF |
---|
442 | ! energy/enstrophy conserving formulation for planetary vorticity term |
---|
443 | zcubt = + zfac25 / e1u(ji,jj) * ( ftne(ji,jj ) * zwy(ji ,jj ) + ftnw(ji+1,jj) * zwy(ji+1,jj ) & |
---|
444 | & + ftse(ji,jj ) * zwy(ji ,jj-1) + ftsw(ji+1,jj) * zwy(ji+1,jj-1) ) |
---|
445 | zcvbt = - zfac25 / e2v(ji,jj) * ( ftsw(ji,jj+1) * zwx(ji-1,jj+1) + ftse(ji,jj+1) * zwx(ji ,jj+1) & |
---|
446 | & + ftnw(ji,jj ) * zwx(ji-1,jj ) + ftne(ji,jj ) * zwx(ji ,jj ) ) |
---|
447 | ! after transports |
---|
448 | ua_e(ji,jj) = ( zub_e(ji,jj) + z2dt_e * ( zcubt + zspgu + zua(ji,jj) ) ) * umask(ji,jj,1) |
---|
449 | va_e(ji,jj) = ( zvb_e(ji,jj) + z2dt_e * ( zcvbt + zspgv + zva(ji,jj) ) ) * vmask(ji,jj,1) |
---|
450 | END DO |
---|
451 | END DO |
---|
452 | ! |
---|
453 | ENDIF |
---|
454 | |
---|
455 | ! Flather's boundary condition for the barotropic loop : |
---|
456 | ! - Update sea surface height on each open boundary |
---|
457 | ! - Correct the barotropic transports |
---|
458 | IF( lk_obc ) CALL obc_fla_ts |
---|
459 | |
---|
460 | |
---|
461 | ! ... Boundary conditions on ua_e, va_e, ssha_e |
---|
462 | CALL lbc_lnk( ua_e , 'U', -1. ) |
---|
463 | CALL lbc_lnk( va_e , 'V', -1. ) |
---|
464 | CALL lbc_lnk( ssha_e, 'T', 1. ) |
---|
465 | |
---|
466 | ! temporal sum |
---|
467 | !------------- |
---|
468 | IF( jit >= ibaro/2 ) THEN |
---|
469 | zssha_b(:,:) = zssha_b(:,:) + ssha_e(:,:) |
---|
470 | zua_b (:,:) = zua_b (:,:) + ua_e (:,:) |
---|
471 | zva_b (:,:) = zva_b (:,:) + va_e (:,:) |
---|
472 | ENDIF |
---|
473 | |
---|
474 | ! Time filter and swap of dynamics arrays |
---|
475 | ! --------------------------------------- |
---|
476 | IF( neuler == 0 .AND. jit == 1 ) THEN ! Euler (forward) time stepping |
---|
477 | zsshb_e(:,:) = sshn_e(:,:) |
---|
478 | zub_e (:,:) = zun_e (:,:) |
---|
479 | zvb_e (:,:) = zvn_e (:,:) |
---|
480 | sshn_e (:,:) = ssha_e(:,:) |
---|
481 | zun_e (:,:) = ua_e (:,:) |
---|
482 | zvn_e (:,:) = va_e (:,:) |
---|
483 | ELSE ! Asselin filtering |
---|
484 | zsshb_e(:,:) = atfp * ( zsshb_e(:,:) + ssha_e(:,:) ) + atfp1 * sshn_e(:,:) |
---|
485 | zub_e (:,:) = atfp * ( zub_e (:,:) + ua_e (:,:) ) + atfp1 * zun_e (:,:) |
---|
486 | zvb_e (:,:) = atfp * ( zvb_e (:,:) + va_e (:,:) ) + atfp1 * zvn_e (:,:) |
---|
487 | sshn_e (:,:) = ssha_e(:,:) |
---|
488 | zun_e (:,:) = ua_e (:,:) |
---|
489 | zvn_e (:,:) = va_e (:,:) |
---|
490 | ENDIF |
---|
491 | |
---|
492 | IF( lk_vvl ) THEN ! Variable volume |
---|
493 | |
---|
494 | ! Sea surface elevation |
---|
495 | ! --------------------- |
---|
496 | DO jj = 1, jpjm1 |
---|
497 | DO ji = 1,jpim1 |
---|
498 | |
---|
499 | ! Sea Surface Height at u-point before |
---|
500 | zsshun_e(ji,jj) = 0.5 * umask(ji,jj,1) / ( e1u(ji,jj) * e2u(ji,jj) ) & |
---|
501 | & * ( e1t(ji ,jj) * e2t(ji ,jj) * sshn_e(ji ,jj) & |
---|
502 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * sshn_e(ji+1,jj) ) |
---|
503 | |
---|
504 | ! Sea Surface Height at v-point before |
---|
505 | zsshvn_e(ji,jj) = 0.5 * vmask(ji,jj,1) / ( e1v(ji,jj) * e2v(ji,jj) ) & |
---|
506 | & * ( e1t(ji,jj ) * e2t(ji,jj ) * sshn_e(ji,jj ) & |
---|
507 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * sshn_e(ji,jj+1) ) |
---|
508 | |
---|
509 | END DO |
---|
510 | END DO |
---|
511 | |
---|
512 | ! Boundaries conditions |
---|
513 | CALL lbc_lnk( zsshun_e, 'U', 1. ) ; CALL lbc_lnk( zsshvn_e, 'V', 1. ) |
---|
514 | |
---|
515 | ! Scale factors at before and after time step |
---|
516 | ! ------------------------------------------- |
---|
517 | CALL dom_vvl_sf( zsshun_e, 'U', zfse3un_e ) ; CALL dom_vvl_sf( zsshvn_e, 'V', zfse3vn_e ) |
---|
518 | |
---|
519 | ! Ocean depth at U- and V-points |
---|
520 | hu_e(:,:) = 0.e0 |
---|
521 | hv_e(:,:) = 0.e0 |
---|
522 | |
---|
523 | DO jk = 1, jpk |
---|
524 | hu_e(:,:) = hu_e(:,:) + zfse3un_e(:,:,jk) * umask(:,:,jk) |
---|
525 | hv_e(:,:) = hv_e(:,:) + zfse3vn_e(:,:,jk) * vmask(:,:,jk) |
---|
526 | END DO |
---|
527 | |
---|
528 | ENDIF ! End variable volume case |
---|
529 | |
---|
530 | ! ! ==================== ! |
---|
531 | END DO ! end loop ! |
---|
532 | ! ! ==================== ! |
---|
533 | |
---|
534 | |
---|
535 | ! Time average of after barotropic variables |
---|
536 | zcoef = 1.e0 / ( ibaro + 1 ) |
---|
537 | zssha_b(:,:) = zcoef * zssha_b(:,:) |
---|
538 | zua_b (:,:) = zcoef * zua_b (:,:) |
---|
539 | zva_b (:,:) = zcoef * zva_b (:,:) |
---|
540 | #if defined key_obc |
---|
541 | IF( lp_obc_east ) sshfoe_b(:,:) = zcoef * sshfoe_b(:,:) |
---|
542 | IF( lp_obc_west ) sshfow_b(:,:) = zcoef * sshfow_b(:,:) |
---|
543 | IF( lp_obc_north ) sshfon_b(:,:) = zcoef * sshfon_b(:,:) |
---|
544 | IF( lp_obc_south ) sshfos_b(:,:) = zcoef * sshfos_b(:,:) |
---|
545 | #endif |
---|
546 | |
---|
547 | |
---|
548 | ! --------------------------------------------------------------------------- |
---|
549 | ! Phase 3 : Update sea surface height from time averaged barotropic variables |
---|
550 | ! --------------------------------------------------------------------------- |
---|
551 | |
---|
552 | |
---|
553 | ! Horizontal divergence of time averaged barotropic transports |
---|
554 | !------------------------------------------------------------- |
---|
555 | IF( .NOT. lk_vvl ) THEN |
---|
556 | DO jj = 2, jpjm1 |
---|
557 | DO ji = fs_2, fs_jpim1 ! vector opt. |
---|
558 | zhdiv(ji,jj) = ( e2u(ji,jj) * un_b(ji,jj) - e2u(ji-1,jj ) * un_b(ji-1,jj ) & |
---|
559 | & +e1v(ji,jj) * vn_b(ji,jj) - e1v(ji ,jj-1) * vn_b(ji ,jj-1) ) & |
---|
560 | & / ( e1t(ji,jj) * e2t(ji,jj) ) |
---|
561 | END DO |
---|
562 | END DO |
---|
563 | ENDIF |
---|
564 | |
---|
565 | #if defined key_obc && ! defined key_vvl |
---|
566 | ! open boundaries (div must be zero behind the open boundary) |
---|
567 | ! mpp remark: The zeroing of hdiv can probably be extended to 1->jpi/jpj for the correct row/column |
---|
568 | IF( lp_obc_east ) zhdiv(nie0p1:nie1p1,nje0 :nje1) = 0.e0 ! east |
---|
569 | IF( lp_obc_west ) zhdiv(niw0 :niw1 ,njw0 :njw1) = 0.e0 ! west |
---|
570 | IF( lp_obc_north ) zhdiv(nin0 :nin1 ,njn0p1:njn1p1) = 0.e0 ! north |
---|
571 | IF( lp_obc_south ) zhdiv(nis0 :nis1 ,njs0 :njs1) = 0.e0 ! south |
---|
572 | #endif |
---|
573 | |
---|
574 | ! sea surface height |
---|
575 | !------------------- |
---|
576 | IF( lk_vvl ) THEN |
---|
577 | sshbb(:,:) = sshb(:,:) |
---|
578 | sshb (:,:) = sshn(:,:) |
---|
579 | sshn (:,:) = ssha(:,:) |
---|
580 | ELSE |
---|
581 | sshb (:,:) = sshn(:,:) |
---|
582 | sshn(:,:) = ( sshb_b(:,:) - z2dt_b * ( zraur * emp(:,:) + zhdiv(:,:) ) ) * tmask(:,:,1) |
---|
583 | ENDIF |
---|
584 | |
---|
585 | ! ... Boundary conditions on sshn |
---|
586 | IF( .NOT. lk_obc ) CALL lbc_lnk( sshn, 'T', 1. ) |
---|
587 | |
---|
588 | |
---|
589 | ! ----------------------------------------------------------------------------- |
---|
590 | ! Phase 4. Coupling between general trend and barotropic estimates - (2nd step) |
---|
591 | ! ----------------------------------------------------------------------------- |
---|
592 | |
---|
593 | ! Swap on time averaged barotropic variables |
---|
594 | ! ------------------------------------------ |
---|
595 | sshb_b(:,:) = sshn_b (:,:) |
---|
596 | IF ( kt == nit000 ) zssha_b(:,:) = sshn(:,:) |
---|
597 | sshn_b(:,:) = zssha_b(:,:) |
---|
598 | un_b (:,:) = zua_b (:,:) |
---|
599 | vn_b (:,:) = zva_b (:,:) |
---|
600 | |
---|
601 | ! add time averaged barotropic coriolis and surface pressure gradient |
---|
602 | ! terms to the general momentum trend |
---|
603 | ! -------------------------------------------------------------------- |
---|
604 | DO jk=1,jpkm1 |
---|
605 | ua(:,:,jk) = ua(:,:,jk) + hur(:,:) * ( zua_b(:,:) - zub(:,:) ) / z2dt_b |
---|
606 | va(:,:,jk) = va(:,:,jk) + hvr(:,:) * ( zva_b(:,:) - zvb(:,:) ) / z2dt_b |
---|
607 | END DO |
---|
608 | |
---|
609 | ! write filtered free surface arrays in restart file |
---|
610 | ! -------------------------------------------------- |
---|
611 | IF( lrst_oce ) CALL ts_rst( kt, 'WRITE' ) |
---|
612 | |
---|
613 | ! print sum trends (used for debugging) |
---|
614 | IF( ln_ctl ) CALL prt_ctl( tab2d_1=sshn, clinfo1=' ssh : ', mask1=tmask ) |
---|
615 | ! |
---|
616 | END SUBROUTINE dyn_spg_ts |
---|
617 | |
---|
618 | |
---|
619 | SUBROUTINE ts_rst( kt, cdrw ) |
---|
620 | !!--------------------------------------------------------------------- |
---|
621 | !! *** ROUTINE ts_rst *** |
---|
622 | !! |
---|
623 | !! ** Purpose : Read or write time-splitting arrays in restart file |
---|
624 | !!---------------------------------------------------------------------- |
---|
625 | INTEGER , INTENT(in) :: kt ! ocean time-step |
---|
626 | CHARACTER(len=*), INTENT(in) :: cdrw ! "READ"/"WRITE" flag |
---|
627 | ! |
---|
628 | INTEGER :: ji, jk ! dummy loop indices |
---|
629 | !!---------------------------------------------------------------------- |
---|
630 | ! |
---|
631 | IF( TRIM(cdrw) == 'READ' ) THEN |
---|
632 | IF( iom_varid( numror, 'sshn', ldstop = .FALSE. ) > 0 ) THEN |
---|
633 | CALL iom_get( numror, jpdom_autoglo, 'sshb' , sshb(:,:) ) |
---|
634 | CALL iom_get( numror, jpdom_autoglo, 'sshn' , sshn(:,:) ) |
---|
635 | IF( neuler == 0 ) sshb(:,:) = sshn(:,:) |
---|
636 | ELSE |
---|
637 | IF( nn_rstssh == 1 ) THEN |
---|
638 | sshb(:,:) = 0.e0 |
---|
639 | sshn(:,:) = 0.e0 |
---|
640 | ENDIF |
---|
641 | ENDIF |
---|
642 | IF( iom_varid( numror, 'sshn_b', ldstop = .FALSE. ) > 0 ) THEN |
---|
643 | CALL iom_get( numror, jpdom_autoglo, 'sshb_b', sshb_b(:,:) ) ! free surface issued |
---|
644 | CALL iom_get( numror, jpdom_autoglo, 'sshn_b', sshn_b(:,:) ) ! from time-splitting loop |
---|
645 | CALL iom_get( numror, jpdom_autoglo, 'un_b' , un_b (:,:) ) ! horizontal transports issued |
---|
646 | CALL iom_get( numror, jpdom_autoglo, 'vn_b' , vn_b (:,:) ) ! from barotropic loop |
---|
647 | IF( neuler == 0 ) sshb_b(:,:) = sshn_b(:,:) |
---|
648 | ELSE |
---|
649 | sshb_b(:,:) = sshb(:,:) |
---|
650 | sshn_b(:,:) = sshn(:,:) |
---|
651 | un_b (:,:) = 0.e0 |
---|
652 | vn_b (:,:) = 0.e0 |
---|
653 | ! vertical sum |
---|
654 | IF( lk_vopt_loop ) THEN ! vector opt., forced unroll |
---|
655 | DO jk = 1, jpkm1 |
---|
656 | DO ji = 1, jpij |
---|
657 | un_b(ji,1) = un_b(ji,1) + fse3u(ji,1,jk) * un(ji,1,jk) |
---|
658 | vn_b(ji,1) = vn_b(ji,1) + fse3v(ji,1,jk) * vn(ji,1,jk) |
---|
659 | END DO |
---|
660 | END DO |
---|
661 | ELSE ! No vector opt. |
---|
662 | DO jk = 1, jpkm1 |
---|
663 | un_b(:,:) = un_b(:,:) + fse3u(:,:,jk) * un(:,:,jk) |
---|
664 | vn_b(:,:) = vn_b(:,:) + fse3v(:,:,jk) * vn(:,:,jk) |
---|
665 | END DO |
---|
666 | ENDIF |
---|
667 | ENDIF |
---|
668 | ELSEIF( TRIM(cdrw) == 'WRITE' ) THEN |
---|
669 | CALL iom_rstput( kt, nitrst, numrow, 'sshb' , sshb (:,:) ) |
---|
670 | CALL iom_rstput( kt, nitrst, numrow, 'sshn' , sshn (:,:) ) |
---|
671 | CALL iom_rstput( kt, nitrst, numrow, 'sshb_b', sshb_b(:,:) ) ! free surface issued |
---|
672 | CALL iom_rstput( kt, nitrst, numrow, 'sshn_b', sshn_b(:,:) ) ! from barotropic loop |
---|
673 | CALL iom_rstput( kt, nitrst, numrow, 'un_b' , un_b (:,:) ) ! horizontal transports issued |
---|
674 | CALL iom_rstput( kt, nitrst, numrow, 'vn_b' , vn_b (:,:) ) ! from barotropic loop |
---|
675 | ENDIF |
---|
676 | ! |
---|
677 | END SUBROUTINE ts_rst |
---|
678 | |
---|
679 | #else |
---|
680 | !!---------------------------------------------------------------------- |
---|
681 | !! Default case : Empty module No standart free surface cst volume |
---|
682 | !!---------------------------------------------------------------------- |
---|
683 | CONTAINS |
---|
684 | SUBROUTINE dyn_spg_ts( kt ) ! Empty routine |
---|
685 | WRITE(*,*) 'dyn_spg_ts: You should not have seen this print! error?', kt |
---|
686 | END SUBROUTINE dyn_spg_ts |
---|
687 | SUBROUTINE ts_rst( kt, cdrw ) ! Empty routine |
---|
688 | INTEGER , INTENT(in) :: kt ! ocean time-step |
---|
689 | CHARACTER(len=*), INTENT(in) :: cdrw ! "READ"/"WRITE" flag |
---|
690 | WRITE(*,*) 'ts_rst : You should not have seen this print! error?', kt, cdrw |
---|
691 | END SUBROUTINE ts_rst |
---|
692 | #endif |
---|
693 | |
---|
694 | !!====================================================================== |
---|
695 | END MODULE dynspg_ts |
---|