1 |
jmc |
1.96 |
C $Header: /u/gcmpack/MITgcm/model/src/dynamics.F,v 1.95 2003/02/28 02:20:52 heimbach Exp $ |
2 |
heimbach |
1.78 |
C $Name: $ |
3 |
cnh |
1.1 |
|
4 |
adcroft |
1.24 |
#include "CPP_OPTIONS.h" |
5 |
cnh |
1.1 |
|
6 |
cnh |
1.82 |
CBOP |
7 |
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C !ROUTINE: DYNAMICS |
8 |
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C !INTERFACE: |
9 |
cnh |
1.8 |
SUBROUTINE DYNAMICS(myTime, myIter, myThid) |
10 |
cnh |
1.82 |
C !DESCRIPTION: \bv |
11 |
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C *==========================================================* |
12 |
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C | SUBROUTINE DYNAMICS |
13 |
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C | o Controlling routine for the explicit part of the model |
14 |
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C | dynamics. |
15 |
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C *==========================================================* |
16 |
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C | This routine evaluates the "dynamics" terms for each |
17 |
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C | block of ocean in turn. Because the blocks of ocean have |
18 |
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C | overlap regions they are independent of one another. |
19 |
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C | If terms involving lateral integrals are needed in this |
20 |
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C | routine care will be needed. Similarly finite-difference |
21 |
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C | operations with stencils wider than the overlap region |
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C | require special consideration. |
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C | The algorithm... |
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C | |
25 |
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C | "Correction Step" |
26 |
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C | ================= |
27 |
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C | Here we update the horizontal velocities with the surface |
28 |
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C | pressure such that the resulting flow is either consistent |
29 |
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C | with the free-surface evolution or the rigid-lid: |
30 |
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C | U[n] = U* + dt x d/dx P |
31 |
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C | V[n] = V* + dt x d/dy P |
32 |
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C | |
33 |
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C | "Calculation of Gs" |
34 |
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C | =================== |
35 |
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C | This is where all the accelerations and tendencies (ie. |
36 |
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C | physics, parameterizations etc...) are calculated |
37 |
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C | rho = rho ( theta[n], salt[n] ) |
38 |
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C | b = b(rho, theta) |
39 |
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C | K31 = K31 ( rho ) |
40 |
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C | Gu[n] = Gu( u[n], v[n], wVel, b, ... ) |
41 |
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C | Gv[n] = Gv( u[n], v[n], wVel, b, ... ) |
42 |
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C | Gt[n] = Gt( theta[n], u[n], v[n], wVel, K31, ... ) |
43 |
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C | Gs[n] = Gs( salt[n], u[n], v[n], wVel, K31, ... ) |
44 |
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C | |
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C | "Time-stepping" or "Prediction" |
46 |
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C | ================================ |
47 |
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C | The models variables are stepped forward with the appropriate |
48 |
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C | time-stepping scheme (currently we use Adams-Bashforth II) |
49 |
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C | - For momentum, the result is always *only* a "prediction" |
50 |
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C | in that the flow may be divergent and will be "corrected" |
51 |
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C | later with a surface pressure gradient. |
52 |
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C | - Normally for tracers the result is the new field at time |
53 |
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C | level [n+1} *BUT* in the case of implicit diffusion the result |
54 |
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C | is also *only* a prediction. |
55 |
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C | - We denote "predictors" with an asterisk (*). |
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C | U* = U[n] + dt x ( 3/2 Gu[n] - 1/2 Gu[n-1] ) |
57 |
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C | V* = V[n] + dt x ( 3/2 Gv[n] - 1/2 Gv[n-1] ) |
58 |
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C | theta[n+1] = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
59 |
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C | salt[n+1] = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
60 |
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C | With implicit diffusion: |
61 |
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C | theta* = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
62 |
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C | salt* = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
63 |
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C | (1 + dt * K * d_zz) theta[n] = theta* |
64 |
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C | (1 + dt * K * d_zz) salt[n] = salt* |
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C | |
66 |
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C *==========================================================* |
67 |
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C \ev |
68 |
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C !USES: |
69 |
adcroft |
1.40 |
IMPLICIT NONE |
70 |
cnh |
1.1 |
C == Global variables === |
71 |
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#include "SIZE.h" |
72 |
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#include "EEPARAMS.h" |
73 |
adcroft |
1.6 |
#include "PARAMS.h" |
74 |
adcroft |
1.3 |
#include "DYNVARS.h" |
75 |
adcroft |
1.42 |
#include "GRID.h" |
76 |
heimbach |
1.74 |
#ifdef ALLOW_PASSIVE_TRACER |
77 |
heimbach |
1.72 |
#include "TR1.h" |
78 |
heimbach |
1.74 |
#endif |
79 |
heimbach |
1.49 |
#ifdef ALLOW_AUTODIFF_TAMC |
80 |
heimbach |
1.53 |
# include "tamc.h" |
81 |
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# include "tamc_keys.h" |
82 |
heimbach |
1.67 |
# include "FFIELDS.h" |
83 |
heimbach |
1.91 |
# include "EOS.h" |
84 |
heimbach |
1.67 |
# ifdef ALLOW_KPP |
85 |
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# include "KPP.h" |
86 |
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# endif |
87 |
heimbach |
1.53 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
88 |
jmc |
1.62 |
|
89 |
cnh |
1.82 |
C !CALLING SEQUENCE: |
90 |
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C DYNAMICS() |
91 |
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C | |
92 |
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C |-- CALC_GRAD_PHI_SURF |
93 |
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C | |
94 |
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C |-- CALC_VISCOSITY |
95 |
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C | |
96 |
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C |-- CALC_PHI_HYD |
97 |
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C | |
98 |
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C |-- MOM_FLUXFORM |
99 |
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C | |
100 |
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C |-- MOM_VECINV |
101 |
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C | |
102 |
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C |-- TIMESTEP |
103 |
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C | |
104 |
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C |-- OBCS_APPLY_UV |
105 |
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C | |
106 |
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C |-- IMPLDIFF |
107 |
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C | |
108 |
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C |-- OBCS_APPLY_UV |
109 |
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C | |
110 |
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C |-- CALL TIMEAVE_CUMUL_1T |
111 |
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C |-- CALL DEBUG_STATS_RL |
112 |
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113 |
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C !INPUT/OUTPUT PARAMETERS: |
114 |
cnh |
1.1 |
C == Routine arguments == |
115 |
cnh |
1.8 |
C myTime - Current time in simulation |
116 |
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C myIter - Current iteration number in simulation |
117 |
cnh |
1.1 |
C myThid - Thread number for this instance of the routine. |
118 |
cnh |
1.8 |
_RL myTime |
119 |
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INTEGER myIter |
120 |
adcroft |
1.47 |
INTEGER myThid |
121 |
cnh |
1.1 |
|
122 |
cnh |
1.82 |
C !LOCAL VARIABLES: |
123 |
cnh |
1.1 |
C == Local variables |
124 |
adcroft |
1.58 |
C fVer[STUV] o fVer: Vertical flux term - note fVer |
125 |
cnh |
1.1 |
C is "pipelined" in the vertical |
126 |
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C so we need an fVer for each |
127 |
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C variable. |
128 |
jmc |
1.94 |
C phiHydC :: hydrostatic potential anomaly at cell center |
129 |
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C In z coords phiHyd is the hydrostatic potential |
130 |
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C (=pressure/rho0) anomaly |
131 |
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C In p coords phiHyd is the geopotential height anomaly. |
132 |
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C phiHydF :: hydrostatic potential anomaly at middle between 2 centers |
133 |
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C dPhiHydX,Y :: Gradient (X & Y directions) of hydrostatic potential anom. |
134 |
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C phiSurfX, :: gradient of Surface potential (Pressure/rho, ocean) |
135 |
jmc |
1.92 |
C phiSurfY or geopotential (atmos) in X and Y direction |
136 |
cnh |
1.30 |
C iMin, iMax - Ranges and sub-block indices on which calculations |
137 |
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C jMin, jMax are applied. |
138 |
cnh |
1.1 |
C bi, bj |
139 |
heimbach |
1.53 |
C k, kup, - Index for layer above and below. kup and kDown |
140 |
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C kDown, km1 are switched with layer to be the appropriate |
141 |
cnh |
1.38 |
C index into fVerTerm. |
142 |
cnh |
1.30 |
_RL fVerU (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
143 |
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_RL fVerV (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
144 |
jmc |
1.94 |
_RL phiHydF (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
145 |
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_RL phiHydC (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
146 |
jmc |
1.92 |
_RL dPhiHydX(1-Olx:sNx+Olx,1-Oly:sNy+Oly) |
147 |
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_RL dPhiHydY(1-Olx:sNx+Olx,1-Oly:sNy+Oly) |
148 |
jmc |
1.63 |
_RL phiSurfX(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
149 |
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_RL phiSurfY(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
150 |
adcroft |
1.42 |
_RL KappaRU (1-Olx:sNx+Olx,1-Oly:sNy+Oly,Nr) |
151 |
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_RL KappaRV (1-Olx:sNx+Olx,1-Oly:sNy+Oly,Nr) |
152 |
adcroft |
1.12 |
|
153 |
cnh |
1.1 |
INTEGER iMin, iMax |
154 |
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INTEGER jMin, jMax |
155 |
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INTEGER bi, bj |
156 |
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INTEGER i, j |
157 |
heimbach |
1.77 |
INTEGER k, km1, kp1, kup, kDown |
158 |
cnh |
1.1 |
|
159 |
jmc |
1.92 |
LOGICAL DIFFERENT_MULTIPLE |
160 |
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EXTERNAL DIFFERENT_MULTIPLE |
161 |
jmc |
1.62 |
|
162 |
adcroft |
1.11 |
C--- The algorithm... |
163 |
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C |
164 |
|
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C "Correction Step" |
165 |
|
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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 |
|
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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 |
heimbach |
1.53 |
C physics, parameterizations etc...) are calculated |
176 |
adcroft |
1.11 |
C rho = rho ( theta[n], salt[n] ) |
177 |
cnh |
1.27 |
C b = b(rho, theta) |
178 |
adcroft |
1.11 |
C K31 = K31 ( rho ) |
179 |
jmc |
1.61 |
C Gu[n] = Gu( u[n], v[n], wVel, b, ... ) |
180 |
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C Gv[n] = Gv( u[n], v[n], wVel, b, ... ) |
181 |
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C Gt[n] = Gt( theta[n], u[n], v[n], wVel, K31, ... ) |
182 |
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C Gs[n] = Gs( salt[n], u[n], v[n], wVel, K31, ... ) |
183 |
adcroft |
1.11 |
C |
184 |
adcroft |
1.12 |
C "Time-stepping" or "Prediction" |
185 |
adcroft |
1.11 |
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 |
|
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C V* = V[n] + dt x ( 3/2 Gv[n] - 1/2 Gv[n-1] ) |
197 |
|
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C theta[n+1] = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
198 |
|
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C salt[n+1] = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
199 |
adcroft |
1.12 |
C With implicit diffusion: |
200 |
adcroft |
1.11 |
C theta* = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
201 |
|
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C salt* = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
202 |
adcroft |
1.12 |
C (1 + dt * K * d_zz) theta[n] = theta* |
203 |
|
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C (1 + dt * K * d_zz) salt[n] = salt* |
204 |
adcroft |
1.11 |
C--- |
205 |
cnh |
1.82 |
CEOP |
206 |
adcroft |
1.11 |
|
207 |
heimbach |
1.76 |
C-- Set up work arrays with valid (i.e. not NaN) values |
208 |
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C These inital values do not alter the numerical results. They |
209 |
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C just ensure that all memory references are to valid floating |
210 |
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C point numbers. This prevents spurious hardware signals due to |
211 |
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C uninitialised but inert locations. |
212 |
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DO j=1-OLy,sNy+OLy |
213 |
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DO i=1-OLx,sNx+OLx |
214 |
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phiSurfX(i,j) = 0. _d 0 |
215 |
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phiSurfY(i,j) = 0. _d 0 |
216 |
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ENDDO |
217 |
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ENDDO |
218 |
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219 |
heimbach |
1.88 |
C-- Call to routine for calculation of |
220 |
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C Eliassen-Palm-flux-forced U-tendency, |
221 |
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C if desired: |
222 |
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#ifdef INCLUDE_EP_FORCING_CODE |
223 |
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CALL CALC_EP_FORCING(myThid) |
224 |
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#endif |
225 |
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|
226 |
heimbach |
1.76 |
#ifdef ALLOW_AUTODIFF_TAMC |
227 |
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C-- HPF directive to help TAMC |
228 |
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CHPF$ INDEPENDENT |
229 |
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#endif /* ALLOW_AUTODIFF_TAMC */ |
230 |
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|
231 |
cnh |
1.1 |
DO bj=myByLo(myThid),myByHi(myThid) |
232 |
heimbach |
1.76 |
|
233 |
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#ifdef ALLOW_AUTODIFF_TAMC |
234 |
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C-- HPF directive to help TAMC |
235 |
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CHPF$ INDEPENDENT, NEW (fVerU,fVerV |
236 |
jmc |
1.94 |
CHPF$& ,phiHydF |
237 |
heimbach |
1.76 |
CHPF$& ,KappaRU,KappaRV |
238 |
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CHPF$& ) |
239 |
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#endif /* ALLOW_AUTODIFF_TAMC */ |
240 |
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241 |
cnh |
1.1 |
DO bi=myBxLo(myThid),myBxHi(myThid) |
242 |
heimbach |
1.76 |
|
243 |
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#ifdef ALLOW_AUTODIFF_TAMC |
244 |
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act1 = bi - myBxLo(myThid) |
245 |
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max1 = myBxHi(myThid) - myBxLo(myThid) + 1 |
246 |
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act2 = bj - myByLo(myThid) |
247 |
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max2 = myByHi(myThid) - myByLo(myThid) + 1 |
248 |
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act3 = myThid - 1 |
249 |
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max3 = nTx*nTy |
250 |
|
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act4 = ikey_dynamics - 1 |
251 |
heimbach |
1.91 |
idynkey = (act1 + 1) + act2*max1 |
252 |
heimbach |
1.76 |
& + act3*max1*max2 |
253 |
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& + act4*max1*max2*max3 |
254 |
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#endif /* ALLOW_AUTODIFF_TAMC */ |
255 |
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256 |
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C-- Set up work arrays that need valid initial values |
257 |
jmc |
1.94 |
DO k=1,Nr |
258 |
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DO j=1-OLy,sNy+OLy |
259 |
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DO i=1-OLx,sNx+OLx |
260 |
heimbach |
1.87 |
KappaRU(i,j,k) = 0. _d 0 |
261 |
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KappaRV(i,j,k) = 0. _d 0 |
262 |
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ENDDO |
263 |
jmc |
1.94 |
ENDDO |
264 |
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ENDDO |
265 |
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DO j=1-OLy,sNy+OLy |
266 |
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DO i=1-OLx,sNx+OLx |
267 |
heimbach |
1.76 |
fVerU (i,j,1) = 0. _d 0 |
268 |
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fVerU (i,j,2) = 0. _d 0 |
269 |
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fVerV (i,j,1) = 0. _d 0 |
270 |
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fVerV (i,j,2) = 0. _d 0 |
271 |
jmc |
1.94 |
phiHydF (i,j) = 0. _d 0 |
272 |
|
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phiHydC (i,j) = 0. _d 0 |
273 |
jmc |
1.92 |
dPhiHydX(i,j) = 0. _d 0 |
274 |
|
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dPhiHydY(i,j) = 0. _d 0 |
275 |
heimbach |
1.76 |
ENDDO |
276 |
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ENDDO |
277 |
heimbach |
1.49 |
|
278 |
jmc |
1.63 |
C-- Start computation of dynamics |
279 |
jmc |
1.93 |
iMin = 0 |
280 |
|
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iMax = sNx+1 |
281 |
|
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jMin = 0 |
282 |
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jMax = sNy+1 |
283 |
jmc |
1.63 |
|
284 |
heimbach |
1.76 |
#ifdef ALLOW_AUTODIFF_TAMC |
285 |
heimbach |
1.91 |
CADJ STORE wvel (:,:,:,bi,bj) = |
286 |
|
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CADJ & comlev1_bibj, key = idynkey, byte = isbyte |
287 |
heimbach |
1.76 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
288 |
|
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|
289 |
jmc |
1.65 |
C-- Explicit part of the Surface Potentiel Gradient (add in TIMESTEP) |
290 |
jmc |
1.63 |
C (note: this loop will be replaced by CALL CALC_GRAD_ETA) |
291 |
|
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IF (implicSurfPress.NE.1.) THEN |
292 |
jmc |
1.65 |
CALL CALC_GRAD_PHI_SURF( |
293 |
|
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I bi,bj,iMin,iMax,jMin,jMax, |
294 |
|
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I etaN, |
295 |
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O phiSurfX,phiSurfY, |
296 |
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I myThid ) |
297 |
jmc |
1.63 |
ENDIF |
298 |
heimbach |
1.83 |
|
299 |
|
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#ifdef ALLOW_AUTODIFF_TAMC |
300 |
heimbach |
1.91 |
CADJ STORE uvel (:,:,:,bi,bj) = comlev1_bibj, key=idynkey, byte=isbyte |
301 |
|
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CADJ STORE vvel (:,:,:,bi,bj) = comlev1_bibj, key=idynkey, byte=isbyte |
302 |
heimbach |
1.83 |
#ifdef ALLOW_KPP |
303 |
|
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CADJ STORE KPPviscAz (:,:,:,bi,bj) |
304 |
heimbach |
1.91 |
CADJ & = comlev1_bibj, key=idynkey, byte=isbyte |
305 |
heimbach |
1.83 |
#endif /* ALLOW_KPP */ |
306 |
|
|
#endif /* ALLOW_AUTODIFF_TAMC */ |
307 |
adcroft |
1.58 |
|
308 |
heimbach |
1.77 |
#ifdef INCLUDE_CALC_DIFFUSIVITY_CALL |
309 |
|
|
C-- Calculate the total vertical diffusivity |
310 |
|
|
DO k=1,Nr |
311 |
|
|
CALL CALC_VISCOSITY( |
312 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,k, |
313 |
|
|
O KappaRU,KappaRV, |
314 |
|
|
I myThid) |
315 |
|
|
ENDDO |
316 |
|
|
#endif |
317 |
|
|
|
318 |
adcroft |
1.58 |
C-- Start of dynamics loop |
319 |
|
|
DO k=1,Nr |
320 |
|
|
|
321 |
|
|
C-- km1 Points to level above k (=k-1) |
322 |
|
|
C-- kup Cycles through 1,2 to point to layer above |
323 |
|
|
C-- kDown Cycles through 2,1 to point to current layer |
324 |
|
|
|
325 |
|
|
km1 = MAX(1,k-1) |
326 |
heimbach |
1.77 |
kp1 = MIN(k+1,Nr) |
327 |
adcroft |
1.58 |
kup = 1+MOD(k+1,2) |
328 |
|
|
kDown= 1+MOD(k,2) |
329 |
|
|
|
330 |
heimbach |
1.76 |
#ifdef ALLOW_AUTODIFF_TAMC |
331 |
heimbach |
1.91 |
kkey = (idynkey-1)*Nr + k |
332 |
heimbach |
1.95 |
CADJ STORE totphihyd (:,:,k,bi,bj) |
333 |
|
|
CADJ & = comlev1_bibj_k, key=kkey, byte=isbyte |
334 |
heimbach |
1.76 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
335 |
|
|
|
336 |
adcroft |
1.58 |
C-- Integrate hydrostatic balance for phiHyd with BC of |
337 |
|
|
C phiHyd(z=0)=0 |
338 |
|
|
C distinguishe between Stagger and Non Stagger time stepping |
339 |
|
|
IF (staggerTimeStep) THEN |
340 |
|
|
CALL CALC_PHI_HYD( |
341 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,k, |
342 |
adcroft |
1.81 |
I gT, gS, |
343 |
jmc |
1.94 |
U phiHydF, |
344 |
|
|
O phiHydC, dPhiHydX, dPhiHydY, |
345 |
jmc |
1.92 |
I myTime, myIter, myThid ) |
346 |
adcroft |
1.58 |
ELSE |
347 |
|
|
CALL CALC_PHI_HYD( |
348 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,k, |
349 |
|
|
I theta, salt, |
350 |
jmc |
1.94 |
U phiHydF, |
351 |
|
|
O phiHydC, dPhiHydX, dPhiHydY, |
352 |
jmc |
1.92 |
I myTime, myIter, myThid ) |
353 |
adcroft |
1.58 |
ENDIF |
354 |
mlosch |
1.89 |
|
355 |
adcroft |
1.58 |
C-- Calculate accelerations in the momentum equations (gU, gV, ...) |
356 |
jmc |
1.96 |
C and step forward storing the result in gU, gV, etc... |
357 |
adcroft |
1.58 |
IF ( momStepping ) THEN |
358 |
adcroft |
1.79 |
#ifndef DISABLE_MOM_FLUXFORM |
359 |
|
|
IF (.NOT. vectorInvariantMomentum) CALL MOM_FLUXFORM( |
360 |
adcroft |
1.58 |
I bi,bj,iMin,iMax,jMin,jMax,k,kup,kDown, |
361 |
jmc |
1.94 |
I dPhiHydX,dPhiHydY,KappaRU,KappaRV, |
362 |
adcroft |
1.58 |
U fVerU, fVerV, |
363 |
adcroft |
1.80 |
I myTime, myIter, myThid) |
364 |
adcroft |
1.79 |
#endif |
365 |
|
|
#ifndef DISABLE_MOM_VECINV |
366 |
|
|
IF (vectorInvariantMomentum) CALL MOM_VECINV( |
367 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,k,kup,kDown, |
368 |
jmc |
1.92 |
I dPhiHydX,dPhiHydY,KappaRU,KappaRV, |
369 |
adcroft |
1.79 |
U fVerU, fVerV, |
370 |
adcroft |
1.80 |
I myTime, myIter, myThid) |
371 |
adcroft |
1.79 |
#endif |
372 |
adcroft |
1.58 |
CALL TIMESTEP( |
373 |
jmc |
1.63 |
I bi,bj,iMin,iMax,jMin,jMax,k, |
374 |
jmc |
1.94 |
I dPhiHydX,dPhiHydY, phiSurfX, phiSurfY, |
375 |
jmc |
1.96 |
I myTime, myIter, myThid) |
376 |
adcroft |
1.58 |
|
377 |
|
|
#ifdef ALLOW_OBCS |
378 |
|
|
C-- Apply open boundary conditions |
379 |
jmc |
1.96 |
IF (useOBCS) THEN |
380 |
|
|
CALL OBCS_APPLY_UV( bi, bj, k, gU, gV, myThid ) |
381 |
|
|
ENDIF |
382 |
adcroft |
1.58 |
#endif /* ALLOW_OBCS */ |
383 |
|
|
|
384 |
|
|
ENDIF |
385 |
|
|
|
386 |
|
|
|
387 |
|
|
C-- end of dynamics k loop (1:Nr) |
388 |
|
|
ENDDO |
389 |
|
|
|
390 |
adcroft |
1.44 |
C-- Implicit viscosity |
391 |
adcroft |
1.58 |
IF (implicitViscosity.AND.momStepping) THEN |
392 |
|
|
#ifdef ALLOW_AUTODIFF_TAMC |
393 |
jmc |
1.96 |
CADJ STORE gU(:,:,:,bi,bj) = comlev1_bibj , key=idynkey, byte=isbyte |
394 |
adcroft |
1.58 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
395 |
adcroft |
1.42 |
CALL IMPLDIFF( |
396 |
|
|
I bi, bj, iMin, iMax, jMin, jMax, |
397 |
|
|
I deltaTmom, KappaRU,recip_HFacW, |
398 |
jmc |
1.96 |
U gU, |
399 |
adcroft |
1.42 |
I myThid ) |
400 |
adcroft |
1.58 |
#ifdef ALLOW_AUTODIFF_TAMC |
401 |
heimbach |
1.91 |
CADJ STORE gVNm1(:,:,:,bi,bj) = comlev1_bibj , key=idynkey, byte=isbyte |
402 |
adcroft |
1.58 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
403 |
adcroft |
1.42 |
CALL IMPLDIFF( |
404 |
|
|
I bi, bj, iMin, iMax, jMin, jMax, |
405 |
|
|
I deltaTmom, KappaRV,recip_HFacS, |
406 |
jmc |
1.96 |
U gV, |
407 |
adcroft |
1.42 |
I myThid ) |
408 |
heimbach |
1.49 |
|
409 |
adcroft |
1.58 |
#ifdef ALLOW_OBCS |
410 |
|
|
C-- Apply open boundary conditions |
411 |
|
|
IF (useOBCS) THEN |
412 |
|
|
DO K=1,Nr |
413 |
jmc |
1.96 |
CALL OBCS_APPLY_UV( bi, bj, k, gU, gV, myThid ) |
414 |
adcroft |
1.58 |
ENDDO |
415 |
|
|
END IF |
416 |
|
|
#endif /* ALLOW_OBCS */ |
417 |
heimbach |
1.49 |
|
418 |
adcroft |
1.58 |
#ifdef INCLUDE_CD_CODE |
419 |
|
|
#ifdef ALLOW_AUTODIFF_TAMC |
420 |
heimbach |
1.91 |
CADJ STORE vVelD(:,:,:,bi,bj) = comlev1_bibj , key=idynkey, byte=isbyte |
421 |
adcroft |
1.58 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
422 |
adcroft |
1.42 |
CALL IMPLDIFF( |
423 |
|
|
I bi, bj, iMin, iMax, jMin, jMax, |
424 |
|
|
I deltaTmom, KappaRU,recip_HFacW, |
425 |
|
|
U vVelD, |
426 |
|
|
I myThid ) |
427 |
adcroft |
1.58 |
#ifdef ALLOW_AUTODIFF_TAMC |
428 |
heimbach |
1.91 |
CADJ STORE uVelD(:,:,:,bi,bj) = comlev1_bibj , key=idynkey, byte=isbyte |
429 |
adcroft |
1.58 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
430 |
adcroft |
1.42 |
CALL IMPLDIFF( |
431 |
|
|
I bi, bj, iMin, iMax, jMin, jMax, |
432 |
|
|
I deltaTmom, KappaRV,recip_HFacS, |
433 |
|
|
U uVelD, |
434 |
|
|
I myThid ) |
435 |
adcroft |
1.58 |
#endif /* INCLUDE_CD_CODE */ |
436 |
|
|
C-- End If implicitViscosity.AND.momStepping |
437 |
heimbach |
1.53 |
ENDIF |
438 |
cnh |
1.1 |
|
439 |
|
|
ENDDO |
440 |
|
|
ENDDO |
441 |
mlosch |
1.90 |
|
442 |
|
|
Cml( |
443 |
|
|
C In order to compare the variance of phiHydLow of a p/z-coordinate |
444 |
|
|
C run with etaH of a z/p-coordinate run the drift of phiHydLow |
445 |
|
|
C has to be removed by something like the following subroutine: |
446 |
|
|
C CALL REMOVE_MEAN_RL( 1, phiHydLow, maskH, maskH, rA, drF, |
447 |
|
|
C & 'phiHydLow', myThid ) |
448 |
|
|
Cml) |
449 |
adcroft |
1.69 |
|
450 |
adcroft |
1.79 |
#ifndef DISABLE_DEBUGMODE |
451 |
adcroft |
1.70 |
If (debugMode) THEN |
452 |
adcroft |
1.69 |
CALL DEBUG_STATS_RL(1,EtaN,'EtaN (DYNAMICS)',myThid) |
453 |
adcroft |
1.73 |
CALL DEBUG_STATS_RL(Nr,uVel,'Uvel (DYNAMICS)',myThid) |
454 |
adcroft |
1.69 |
CALL DEBUG_STATS_RL(Nr,vVel,'Vvel (DYNAMICS)',myThid) |
455 |
|
|
CALL DEBUG_STATS_RL(Nr,wVel,'Wvel (DYNAMICS)',myThid) |
456 |
|
|
CALL DEBUG_STATS_RL(Nr,theta,'Theta (DYNAMICS)',myThid) |
457 |
|
|
CALL DEBUG_STATS_RL(Nr,salt,'Salt (DYNAMICS)',myThid) |
458 |
|
|
CALL DEBUG_STATS_RL(Nr,Gu,'Gu (DYNAMICS)',myThid) |
459 |
|
|
CALL DEBUG_STATS_RL(Nr,Gv,'Gv (DYNAMICS)',myThid) |
460 |
|
|
CALL DEBUG_STATS_RL(Nr,Gt,'Gt (DYNAMICS)',myThid) |
461 |
|
|
CALL DEBUG_STATS_RL(Nr,Gs,'Gs (DYNAMICS)',myThid) |
462 |
|
|
CALL DEBUG_STATS_RL(Nr,GuNm1,'GuNm1 (DYNAMICS)',myThid) |
463 |
|
|
CALL DEBUG_STATS_RL(Nr,GvNm1,'GvNm1 (DYNAMICS)',myThid) |
464 |
|
|
CALL DEBUG_STATS_RL(Nr,GtNm1,'GtNm1 (DYNAMICS)',myThid) |
465 |
|
|
CALL DEBUG_STATS_RL(Nr,GsNm1,'GsNm1 (DYNAMICS)',myThid) |
466 |
adcroft |
1.70 |
ENDIF |
467 |
adcroft |
1.69 |
#endif |
468 |
cnh |
1.1 |
|
469 |
|
|
RETURN |
470 |
|
|
END |