1 |
C $Header: /u/gcmpack/MITgcm/model/src/dynamics.F,v 1.98 2003/07/08 15:00:26 heimbach Exp $ |
2 |
C $Name: $ |
3 |
|
4 |
#include "CPP_OPTIONS.h" |
5 |
|
6 |
CBOP |
7 |
C !ROUTINE: DYNAMICS |
8 |
C !INTERFACE: |
9 |
SUBROUTINE DYNAMICS(myTime, myIter, myThid) |
10 |
C !DESCRIPTION: \bv |
11 |
C *==========================================================* |
12 |
C | SUBROUTINE DYNAMICS |
13 |
C | o Controlling routine for the explicit part of the model |
14 |
C | dynamics. |
15 |
C *==========================================================* |
16 |
C | This routine evaluates the "dynamics" terms for each |
17 |
C | block of ocean in turn. Because the blocks of ocean have |
18 |
C | overlap regions they are independent of one another. |
19 |
C | If terms involving lateral integrals are needed in this |
20 |
C | routine care will be needed. Similarly finite-difference |
21 |
C | operations with stencils wider than the overlap region |
22 |
C | require special consideration. |
23 |
C | The algorithm... |
24 |
C | |
25 |
C | "Correction Step" |
26 |
C | ================= |
27 |
C | Here we update the horizontal velocities with the surface |
28 |
C | pressure such that the resulting flow is either consistent |
29 |
C | with the free-surface evolution or the rigid-lid: |
30 |
C | U[n] = U* + dt x d/dx P |
31 |
C | V[n] = V* + dt x d/dy P |
32 |
C | |
33 |
C | "Calculation of Gs" |
34 |
C | =================== |
35 |
C | This is where all the accelerations and tendencies (ie. |
36 |
C | physics, parameterizations etc...) are calculated |
37 |
C | rho = rho ( theta[n], salt[n] ) |
38 |
C | b = b(rho, theta) |
39 |
C | K31 = K31 ( rho ) |
40 |
C | Gu[n] = Gu( u[n], v[n], wVel, b, ... ) |
41 |
C | Gv[n] = Gv( u[n], v[n], wVel, b, ... ) |
42 |
C | Gt[n] = Gt( theta[n], u[n], v[n], wVel, K31, ... ) |
43 |
C | Gs[n] = Gs( salt[n], u[n], v[n], wVel, K31, ... ) |
44 |
C | |
45 |
C | "Time-stepping" or "Prediction" |
46 |
C | ================================ |
47 |
C | The models variables are stepped forward with the appropriate |
48 |
C | time-stepping scheme (currently we use Adams-Bashforth II) |
49 |
C | - For momentum, the result is always *only* a "prediction" |
50 |
C | in that the flow may be divergent and will be "corrected" |
51 |
C | later with a surface pressure gradient. |
52 |
C | - Normally for tracers the result is the new field at time |
53 |
C | level [n+1} *BUT* in the case of implicit diffusion the result |
54 |
C | is also *only* a prediction. |
55 |
C | - We denote "predictors" with an asterisk (*). |
56 |
C | U* = U[n] + dt x ( 3/2 Gu[n] - 1/2 Gu[n-1] ) |
57 |
C | V* = V[n] + dt x ( 3/2 Gv[n] - 1/2 Gv[n-1] ) |
58 |
C | theta[n+1] = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
59 |
C | salt[n+1] = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
60 |
C | With implicit diffusion: |
61 |
C | theta* = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
62 |
C | salt* = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
63 |
C | (1 + dt * K * d_zz) theta[n] = theta* |
64 |
C | (1 + dt * K * d_zz) salt[n] = salt* |
65 |
C | |
66 |
C *==========================================================* |
67 |
C \ev |
68 |
C !USES: |
69 |
IMPLICIT NONE |
70 |
C == Global variables === |
71 |
#include "SIZE.h" |
72 |
#include "EEPARAMS.h" |
73 |
#include "PARAMS.h" |
74 |
#include "DYNVARS.h" |
75 |
#include "GRID.h" |
76 |
#ifdef ALLOW_PASSIVE_TRACER |
77 |
#include "TR1.h" |
78 |
#endif |
79 |
#ifdef ALLOW_AUTODIFF_TAMC |
80 |
# include "tamc.h" |
81 |
# include "tamc_keys.h" |
82 |
# include "FFIELDS.h" |
83 |
# include "EOS.h" |
84 |
# ifdef ALLOW_KPP |
85 |
# include "KPP.h" |
86 |
# endif |
87 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
88 |
|
89 |
C !CALLING SEQUENCE: |
90 |
C DYNAMICS() |
91 |
C | |
92 |
C |-- CALC_GRAD_PHI_SURF |
93 |
C | |
94 |
C |-- CALC_VISCOSITY |
95 |
C | |
96 |
C |-- CALC_PHI_HYD |
97 |
C | |
98 |
C |-- MOM_FLUXFORM |
99 |
C | |
100 |
C |-- MOM_VECINV |
101 |
C | |
102 |
C |-- TIMESTEP |
103 |
C | |
104 |
C |-- OBCS_APPLY_UV |
105 |
C | |
106 |
C |-- IMPLDIFF |
107 |
C | |
108 |
C |-- OBCS_APPLY_UV |
109 |
C | |
110 |
C |-- CALL TIMEAVE_CUMUL_1T |
111 |
C |-- CALL DEBUG_STATS_RL |
112 |
|
113 |
C !INPUT/OUTPUT PARAMETERS: |
114 |
C == Routine arguments == |
115 |
C myTime - Current time in simulation |
116 |
C myIter - Current iteration number in simulation |
117 |
C myThid - Thread number for this instance of the routine. |
118 |
_RL myTime |
119 |
INTEGER myIter |
120 |
INTEGER myThid |
121 |
|
122 |
C !LOCAL VARIABLES: |
123 |
C == Local variables |
124 |
C fVer[STUV] o fVer: Vertical flux term - note fVer |
125 |
C is "pipelined" in the vertical |
126 |
C so we need an fVer for each |
127 |
C variable. |
128 |
C phiHydC :: hydrostatic potential anomaly at cell center |
129 |
C In z coords phiHyd is the hydrostatic potential |
130 |
C (=pressure/rho0) anomaly |
131 |
C In p coords phiHyd is the geopotential height anomaly. |
132 |
C phiHydF :: hydrostatic potential anomaly at middle between 2 centers |
133 |
C dPhiHydX,Y :: Gradient (X & Y directions) of hydrostatic potential anom. |
134 |
C phiSurfX, :: gradient of Surface potential (Pressure/rho, ocean) |
135 |
C phiSurfY or geopotential (atmos) in X and Y direction |
136 |
C iMin, iMax - Ranges and sub-block indices on which calculations |
137 |
C jMin, jMax are applied. |
138 |
C bi, bj |
139 |
C k, kup, - Index for layer above and below. kup and kDown |
140 |
C kDown, km1 are switched with layer to be the appropriate |
141 |
C index into fVerTerm. |
142 |
_RL fVerU (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
143 |
_RL fVerV (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
144 |
_RL phiHydF (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
145 |
_RL phiHydC (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
146 |
_RL dPhiHydX(1-Olx:sNx+Olx,1-Oly:sNy+Oly) |
147 |
_RL dPhiHydY(1-Olx:sNx+Olx,1-Oly:sNy+Oly) |
148 |
_RL phiSurfX(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
149 |
_RL phiSurfY(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
150 |
_RL KappaRU (1-Olx:sNx+Olx,1-Oly:sNy+Oly,Nr) |
151 |
_RL KappaRV (1-Olx:sNx+Olx,1-Oly:sNy+Oly,Nr) |
152 |
|
153 |
INTEGER iMin, iMax |
154 |
INTEGER jMin, jMax |
155 |
INTEGER bi, bj |
156 |
INTEGER i, j |
157 |
INTEGER k, km1, kp1, kup, kDown |
158 |
|
159 |
LOGICAL DIFFERENT_MULTIPLE |
160 |
EXTERNAL DIFFERENT_MULTIPLE |
161 |
|
162 |
C--- The algorithm... |
163 |
C |
164 |
C "Correction Step" |
165 |
C ================= |
166 |
C Here we update the horizontal velocities with the surface |
167 |
C pressure such that the resulting flow is either consistent |
168 |
C with the free-surface evolution or the rigid-lid: |
169 |
C U[n] = U* + dt x d/dx P |
170 |
C V[n] = V* + dt x d/dy P |
171 |
C |
172 |
C "Calculation of Gs" |
173 |
C =================== |
174 |
C This is where all the accelerations and tendencies (ie. |
175 |
C physics, parameterizations etc...) are calculated |
176 |
C rho = rho ( theta[n], salt[n] ) |
177 |
C b = b(rho, theta) |
178 |
C K31 = K31 ( rho ) |
179 |
C Gu[n] = Gu( u[n], v[n], wVel, b, ... ) |
180 |
C Gv[n] = Gv( u[n], v[n], wVel, b, ... ) |
181 |
C Gt[n] = Gt( theta[n], u[n], v[n], wVel, K31, ... ) |
182 |
C Gs[n] = Gs( salt[n], u[n], v[n], wVel, K31, ... ) |
183 |
C |
184 |
C "Time-stepping" or "Prediction" |
185 |
C ================================ |
186 |
C The models variables are stepped forward with the appropriate |
187 |
C time-stepping scheme (currently we use Adams-Bashforth II) |
188 |
C - For momentum, the result is always *only* a "prediction" |
189 |
C in that the flow may be divergent and will be "corrected" |
190 |
C later with a surface pressure gradient. |
191 |
C - Normally for tracers the result is the new field at time |
192 |
C level [n+1} *BUT* in the case of implicit diffusion the result |
193 |
C is also *only* a prediction. |
194 |
C - We denote "predictors" with an asterisk (*). |
195 |
C U* = U[n] + dt x ( 3/2 Gu[n] - 1/2 Gu[n-1] ) |
196 |
C V* = V[n] + dt x ( 3/2 Gv[n] - 1/2 Gv[n-1] ) |
197 |
C theta[n+1] = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
198 |
C salt[n+1] = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
199 |
C With implicit diffusion: |
200 |
C theta* = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
201 |
C salt* = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
202 |
C (1 + dt * K * d_zz) theta[n] = theta* |
203 |
C (1 + dt * K * d_zz) salt[n] = salt* |
204 |
C--- |
205 |
CEOP |
206 |
|
207 |
C-- Call to routine for calculation of |
208 |
C Eliassen-Palm-flux-forced U-tendency, |
209 |
C if desired: |
210 |
#ifdef INCLUDE_EP_FORCING_CODE |
211 |
CALL CALC_EP_FORCING(myThid) |
212 |
#endif |
213 |
|
214 |
#ifdef ALLOW_AUTODIFF_TAMC |
215 |
C-- HPF directive to help TAMC |
216 |
CHPF$ INDEPENDENT |
217 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
218 |
|
219 |
DO bj=myByLo(myThid),myByHi(myThid) |
220 |
|
221 |
#ifdef ALLOW_AUTODIFF_TAMC |
222 |
C-- HPF directive to help TAMC |
223 |
CHPF$ INDEPENDENT, NEW (fVerU,fVerV |
224 |
CHPF$& ,phiHydF |
225 |
CHPF$& ,KappaRU,KappaRV |
226 |
CHPF$& ) |
227 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
228 |
|
229 |
DO bi=myBxLo(myThid),myBxHi(myThid) |
230 |
|
231 |
#ifdef ALLOW_AUTODIFF_TAMC |
232 |
act1 = bi - myBxLo(myThid) |
233 |
max1 = myBxHi(myThid) - myBxLo(myThid) + 1 |
234 |
act2 = bj - myByLo(myThid) |
235 |
max2 = myByHi(myThid) - myByLo(myThid) + 1 |
236 |
act3 = myThid - 1 |
237 |
max3 = nTx*nTy |
238 |
act4 = ikey_dynamics - 1 |
239 |
idynkey = (act1 + 1) + act2*max1 |
240 |
& + act3*max1*max2 |
241 |
& + act4*max1*max2*max3 |
242 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
243 |
|
244 |
C-- Set up work arrays with valid (i.e. not NaN) values |
245 |
C These inital values do not alter the numerical results. They |
246 |
C just ensure that all memory references are to valid floating |
247 |
C point numbers. This prevents spurious hardware signals due to |
248 |
C uninitialised but inert locations. |
249 |
|
250 |
DO k=1,Nr |
251 |
DO j=1-OLy,sNy+OLy |
252 |
DO i=1-OLx,sNx+OLx |
253 |
KappaRU(i,j,k) = 0. _d 0 |
254 |
KappaRV(i,j,k) = 0. _d 0 |
255 |
#ifdef ALLOW_AUTODIFF_TAMC |
256 |
cph( |
257 |
c-- need some re-initialisation here to break dependencies |
258 |
c-- totphihyd is assumed zero from ini_pressure, i.e. |
259 |
c-- avoiding iterate pressure p = integral of (g*rho(p)*dz) |
260 |
cph) |
261 |
totPhiHyd(i,j,k,bi,bj) = 0. _d 0 |
262 |
gu(i,j,k,bi,bj) = 0. _d 0 |
263 |
gv(i,j,k,bi,bj) = 0. _d 0 |
264 |
#endif |
265 |
ENDDO |
266 |
ENDDO |
267 |
ENDDO |
268 |
DO j=1-OLy,sNy+OLy |
269 |
DO i=1-OLx,sNx+OLx |
270 |
fVerU (i,j,1) = 0. _d 0 |
271 |
fVerU (i,j,2) = 0. _d 0 |
272 |
fVerV (i,j,1) = 0. _d 0 |
273 |
fVerV (i,j,2) = 0. _d 0 |
274 |
phiHydF (i,j) = 0. _d 0 |
275 |
phiHydC (i,j) = 0. _d 0 |
276 |
dPhiHydX(i,j) = 0. _d 0 |
277 |
dPhiHydY(i,j) = 0. _d 0 |
278 |
phiSurfX(i,j) = 0. _d 0 |
279 |
phiSurfY(i,j) = 0. _d 0 |
280 |
ENDDO |
281 |
ENDDO |
282 |
|
283 |
C-- Start computation of dynamics |
284 |
iMin = 0 |
285 |
iMax = sNx+1 |
286 |
jMin = 0 |
287 |
jMax = sNy+1 |
288 |
|
289 |
#ifdef ALLOW_AUTODIFF_TAMC |
290 |
CADJ STORE wvel (:,:,:,bi,bj) = |
291 |
CADJ & comlev1_bibj, key = idynkey, byte = isbyte |
292 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
293 |
|
294 |
C-- Explicit part of the Surface Potentiel Gradient (add in TIMESTEP) |
295 |
C (note: this loop will be replaced by CALL CALC_GRAD_ETA) |
296 |
IF (implicSurfPress.NE.1.) THEN |
297 |
CALL CALC_GRAD_PHI_SURF( |
298 |
I bi,bj,iMin,iMax,jMin,jMax, |
299 |
I etaN, |
300 |
O phiSurfX,phiSurfY, |
301 |
I myThid ) |
302 |
ENDIF |
303 |
|
304 |
#ifdef ALLOW_AUTODIFF_TAMC |
305 |
CADJ STORE uvel (:,:,:,bi,bj) = comlev1_bibj, key=idynkey, byte=isbyte |
306 |
CADJ STORE vvel (:,:,:,bi,bj) = comlev1_bibj, key=idynkey, byte=isbyte |
307 |
#ifdef ALLOW_KPP |
308 |
CADJ STORE KPPviscAz (:,:,:,bi,bj) |
309 |
CADJ & = comlev1_bibj, key=idynkey, byte=isbyte |
310 |
#endif /* ALLOW_KPP */ |
311 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
312 |
|
313 |
#ifdef INCLUDE_CALC_DIFFUSIVITY_CALL |
314 |
C-- Calculate the total vertical diffusivity |
315 |
DO k=1,Nr |
316 |
CALL CALC_VISCOSITY( |
317 |
I bi,bj,iMin,iMax,jMin,jMax,k, |
318 |
O KappaRU,KappaRV, |
319 |
I myThid) |
320 |
ENDDO |
321 |
#endif |
322 |
|
323 |
C-- Start of dynamics loop |
324 |
DO k=1,Nr |
325 |
|
326 |
C-- km1 Points to level above k (=k-1) |
327 |
C-- kup Cycles through 1,2 to point to layer above |
328 |
C-- kDown Cycles through 2,1 to point to current layer |
329 |
|
330 |
km1 = MAX(1,k-1) |
331 |
kp1 = MIN(k+1,Nr) |
332 |
kup = 1+MOD(k+1,2) |
333 |
kDown= 1+MOD(k,2) |
334 |
|
335 |
#ifdef ALLOW_AUTODIFF_TAMC |
336 |
kkey = (idynkey-1)*Nr + k |
337 |
c |
338 |
CADJ STORE totphihyd (:,:,k,bi,bj) |
339 |
CADJ & = comlev1_bibj_k, key=kkey, byte=isbyte |
340 |
CADJ STORE gt (:,:,k,bi,bj) |
341 |
CADJ & = comlev1_bibj_k, key=kkey, byte=isbyte |
342 |
CADJ STORE gs (:,:,k,bi,bj) |
343 |
CADJ & = comlev1_bibj_k, key=kkey, byte=isbyte |
344 |
CADJ STORE theta (:,:,k,bi,bj) |
345 |
CADJ & = comlev1_bibj_k, key=kkey, byte=isbyte |
346 |
CADJ STORE salt (:,:,k,bi,bj) |
347 |
CADJ & = comlev1_bibj_k, key=kkey, byte=isbyte |
348 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
349 |
|
350 |
C-- Integrate hydrostatic balance for phiHyd with BC of |
351 |
C phiHyd(z=0)=0 |
352 |
C distinguishe between Stagger and Non Stagger time stepping |
353 |
IF (staggerTimeStep) THEN |
354 |
CALL CALC_PHI_HYD( |
355 |
I bi,bj,iMin,iMax,jMin,jMax,k, |
356 |
I gT, gS, |
357 |
U phiHydF, |
358 |
O phiHydC, dPhiHydX, dPhiHydY, |
359 |
I myTime, myIter, myThid ) |
360 |
ELSE |
361 |
CALL CALC_PHI_HYD( |
362 |
I bi,bj,iMin,iMax,jMin,jMax,k, |
363 |
I theta, salt, |
364 |
U phiHydF, |
365 |
O phiHydC, dPhiHydX, dPhiHydY, |
366 |
I myTime, myIter, myThid ) |
367 |
ENDIF |
368 |
|
369 |
C-- Calculate accelerations in the momentum equations (gU, gV, ...) |
370 |
C and step forward storing the result in gU, gV, etc... |
371 |
IF ( momStepping ) THEN |
372 |
#ifndef DISABLE_MOM_FLUXFORM |
373 |
IF (.NOT. vectorInvariantMomentum) CALL MOM_FLUXFORM( |
374 |
I bi,bj,iMin,iMax,jMin,jMax,k,kup,kDown, |
375 |
I dPhiHydX,dPhiHydY,KappaRU,KappaRV, |
376 |
U fVerU, fVerV, |
377 |
I myTime, myIter, myThid) |
378 |
#endif |
379 |
#ifndef DISABLE_MOM_VECINV |
380 |
IF (vectorInvariantMomentum) CALL MOM_VECINV( |
381 |
I bi,bj,iMin,iMax,jMin,jMax,k,kup,kDown, |
382 |
I dPhiHydX,dPhiHydY,KappaRU,KappaRV, |
383 |
U fVerU, fVerV, |
384 |
I myTime, myIter, myThid) |
385 |
#endif |
386 |
CALL TIMESTEP( |
387 |
I bi,bj,iMin,iMax,jMin,jMax,k, |
388 |
I dPhiHydX,dPhiHydY, phiSurfX, phiSurfY, |
389 |
I myTime, myIter, myThid) |
390 |
|
391 |
#ifdef ALLOW_OBCS |
392 |
C-- Apply open boundary conditions |
393 |
IF (useOBCS) THEN |
394 |
CALL OBCS_APPLY_UV( bi, bj, k, gU, gV, myThid ) |
395 |
ENDIF |
396 |
#endif /* ALLOW_OBCS */ |
397 |
|
398 |
ENDIF |
399 |
|
400 |
|
401 |
C-- end of dynamics k loop (1:Nr) |
402 |
ENDDO |
403 |
|
404 |
C-- Implicit viscosity |
405 |
IF (implicitViscosity.AND.momStepping) THEN |
406 |
#ifdef ALLOW_AUTODIFF_TAMC |
407 |
CADJ STORE gU(:,:,:,bi,bj) = comlev1_bibj , key=idynkey, byte=isbyte |
408 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
409 |
CALL IMPLDIFF( |
410 |
I bi, bj, iMin, iMax, jMin, jMax, |
411 |
I deltaTmom, KappaRU,recip_HFacW, |
412 |
U gU, |
413 |
I myThid ) |
414 |
#ifdef ALLOW_AUTODIFF_TAMC |
415 |
CADJ STORE gV(:,:,:,bi,bj) = comlev1_bibj , key=idynkey, byte=isbyte |
416 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
417 |
CALL IMPLDIFF( |
418 |
I bi, bj, iMin, iMax, jMin, jMax, |
419 |
I deltaTmom, KappaRV,recip_HFacS, |
420 |
U gV, |
421 |
I myThid ) |
422 |
|
423 |
#ifdef ALLOW_OBCS |
424 |
C-- Apply open boundary conditions |
425 |
IF (useOBCS) THEN |
426 |
DO K=1,Nr |
427 |
CALL OBCS_APPLY_UV( bi, bj, k, gU, gV, myThid ) |
428 |
ENDDO |
429 |
END IF |
430 |
#endif /* ALLOW_OBCS */ |
431 |
|
432 |
#ifdef INCLUDE_CD_CODE |
433 |
#ifdef ALLOW_AUTODIFF_TAMC |
434 |
CADJ STORE vVelD(:,:,:,bi,bj) = comlev1_bibj , key=idynkey, byte=isbyte |
435 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
436 |
CALL IMPLDIFF( |
437 |
I bi, bj, iMin, iMax, jMin, jMax, |
438 |
I deltaTmom, KappaRU,recip_HFacW, |
439 |
U vVelD, |
440 |
I myThid ) |
441 |
#ifdef ALLOW_AUTODIFF_TAMC |
442 |
CADJ STORE uVelD(:,:,:,bi,bj) = comlev1_bibj , key=idynkey, byte=isbyte |
443 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
444 |
CALL IMPLDIFF( |
445 |
I bi, bj, iMin, iMax, jMin, jMax, |
446 |
I deltaTmom, KappaRV,recip_HFacS, |
447 |
U uVelD, |
448 |
I myThid ) |
449 |
#endif /* INCLUDE_CD_CODE */ |
450 |
C-- End If implicitViscosity.AND.momStepping |
451 |
ENDIF |
452 |
|
453 |
ENDDO |
454 |
ENDDO |
455 |
|
456 |
Cml( |
457 |
C In order to compare the variance of phiHydLow of a p/z-coordinate |
458 |
C run with etaH of a z/p-coordinate run the drift of phiHydLow |
459 |
C has to be removed by something like the following subroutine: |
460 |
C CALL REMOVE_MEAN_RL( 1, phiHydLow, maskH, maskH, rA, drF, |
461 |
C & 'phiHydLow', myThid ) |
462 |
Cml) |
463 |
|
464 |
#ifndef DISABLE_DEBUGMODE |
465 |
If ( debugLevel .GE. debLevB ) THEN |
466 |
CALL DEBUG_STATS_RL(1,EtaN,'EtaN (DYNAMICS)',myThid) |
467 |
CALL DEBUG_STATS_RL(Nr,uVel,'Uvel (DYNAMICS)',myThid) |
468 |
CALL DEBUG_STATS_RL(Nr,vVel,'Vvel (DYNAMICS)',myThid) |
469 |
CALL DEBUG_STATS_RL(Nr,wVel,'Wvel (DYNAMICS)',myThid) |
470 |
CALL DEBUG_STATS_RL(Nr,theta,'Theta (DYNAMICS)',myThid) |
471 |
CALL DEBUG_STATS_RL(Nr,salt,'Salt (DYNAMICS)',myThid) |
472 |
CALL DEBUG_STATS_RL(Nr,Gu,'Gu (DYNAMICS)',myThid) |
473 |
CALL DEBUG_STATS_RL(Nr,Gv,'Gv (DYNAMICS)',myThid) |
474 |
CALL DEBUG_STATS_RL(Nr,Gt,'Gt (DYNAMICS)',myThid) |
475 |
CALL DEBUG_STATS_RL(Nr,Gs,'Gs (DYNAMICS)',myThid) |
476 |
CALL DEBUG_STATS_RL(Nr,GuNm1,'GuNm1 (DYNAMICS)',myThid) |
477 |
CALL DEBUG_STATS_RL(Nr,GvNm1,'GvNm1 (DYNAMICS)',myThid) |
478 |
CALL DEBUG_STATS_RL(Nr,GtNm1,'GtNm1 (DYNAMICS)',myThid) |
479 |
CALL DEBUG_STATS_RL(Nr,GsNm1,'GsNm1 (DYNAMICS)',myThid) |
480 |
ENDIF |
481 |
#endif |
482 |
|
483 |
RETURN |
484 |
END |