1 |
cnh |
1.33 |
C $Header: /u/gcmpack/models/MITgcmUV/model/src/dynamics.F,v 1.32 1998/08/23 15:34:40 cnh Exp $ |
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cnh |
1.1 |
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3 |
adcroft |
1.24 |
#include "CPP_OPTIONS.h" |
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cnh |
1.1 |
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5 |
cnh |
1.8 |
SUBROUTINE DYNAMICS(myTime, myIter, myThid) |
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cnh |
1.1 |
C /==========================================================\ |
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C | SUBROUTINE DYNAMICS | |
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C | o Controlling routine for the explicit part of the model | |
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C | dynamics. | |
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C |==========================================================| |
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C | This routine evaluates the "dynamics" terms for each | |
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C | block of ocean in turn. Because the blocks of ocean have | |
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C | overlap regions they are independent of one another. | |
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C | If terms involving lateral integrals are needed in this | |
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C | routine care will be needed. Similarly finite-difference | |
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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 | Notes | |
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C | ===== | |
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C | C*P* comments indicating place holders for which code is | |
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C | presently being developed. | |
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C \==========================================================/ |
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C == Global variables === |
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#include "SIZE.h" |
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#include "EEPARAMS.h" |
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#include "CG2D.h" |
28 |
adcroft |
1.6 |
#include "PARAMS.h" |
29 |
adcroft |
1.3 |
#include "DYNVARS.h" |
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cnh |
1.1 |
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31 |
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C == Routine arguments == |
32 |
cnh |
1.8 |
C myTime - Current time in simulation |
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C myIter - Current iteration number in simulation |
34 |
cnh |
1.1 |
C myThid - Thread number for this instance of the routine. |
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INTEGER myThid |
36 |
cnh |
1.8 |
_RL myTime |
37 |
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INTEGER myIter |
38 |
cnh |
1.1 |
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39 |
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C == Local variables |
40 |
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C xA, yA - Per block temporaries holding face areas |
41 |
cnh |
1.30 |
C uTrans, vTrans, rTrans - Per block temporaries holding flow transport |
42 |
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C rVel o uTrans: Zonal transport |
43 |
cnh |
1.1 |
C o vTrans: Meridional transport |
44 |
cnh |
1.30 |
C o rTrans: Vertical transport |
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C o rVel: Vertical velocity at upper and lower |
46 |
cnh |
1.14 |
C cell faces. |
47 |
cnh |
1.1 |
C maskC,maskUp o maskC: land/water mask for tracer cells |
48 |
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C o maskUp: land/water mask for W points |
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C aTerm, xTerm, cTerm - Work arrays for holding separate terms in |
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C mTerm, pTerm, tendency equations. |
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C fZon, fMer, fVer[STUV] o aTerm: Advection term |
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C o xTerm: Mixing term |
53 |
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C o cTerm: Coriolis term |
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C o mTerm: Metric term |
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C o pTerm: Pressure term |
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C o fZon: Zonal flux term |
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C o fMer: Meridional flux term |
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C o fVer: Vertical flux term - note fVer |
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C is "pipelined" in the vertical |
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C so we need an fVer for each |
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C variable. |
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cnh |
1.26 |
C rhoK, rhoKM1 - Density at current level, level above and level below. |
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C rhoKP1 |
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C buoyK, buoyKM1 - Buoyancy at current level and level above. |
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cnh |
1.31 |
C phiHyd - Hydrostatic part of the potential phiHydi. |
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C In z coords phiHydiHyd is the hydrostatic pressure anomaly |
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C In p coords phiHydiHyd is the geopotential surface height |
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cnh |
1.30 |
C anomaly. |
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C etaSurfX, - Holds surface elevation gradient in X and Y. |
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C etaSurfY |
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C K13, K23, K33 - Non-zero elements of small-angle approximation |
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C diffusion tensor. |
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C KapGM - Spatially varying Visbeck et. al mixing coeff. |
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C KappaRT, - Total diffusion in vertical for T and S. |
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C KappaRS ( background + spatially varying, isopycnal term). |
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C iMin, iMax - Ranges and sub-block indices on which calculations |
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C jMin, jMax are applied. |
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cnh |
1.1 |
C bi, bj |
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cnh |
1.30 |
C k, kUp, - Index for layer above and below. kUp and kDown |
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C kDown, kM1 are switched with layer to be the appropriate index |
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C into fVerTerm |
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_RS xA (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RS yA (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL uTrans (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL vTrans (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL rTrans (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL rVel (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
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_RS maskC (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RS maskUp (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL aTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL xTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL cTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL mTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL pTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL fZon (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL fMer (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL fVerT (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
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_RL fVerS (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
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_RL fVerU (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
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_RL fVerV (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
101 |
cnh |
1.31 |
_RL phiHyd (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nr) |
102 |
cnh |
1.30 |
_RL rhokm1 (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
103 |
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_RL rhokp1 (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL rhok (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL buoyKM1 (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL buoyK (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
107 |
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_RL rhotmp (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
108 |
cnh |
1.29 |
_RL etaSurfX(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
109 |
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_RL etaSurfY(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
110 |
cnh |
1.31 |
_RL K13 (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nr) |
111 |
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_RL K23 (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nr) |
112 |
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_RL K33 (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nr) |
113 |
cnh |
1.30 |
_RL KapGM (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
114 |
cnh |
1.31 |
_RL KappaRT (1-Olx:sNx+Olx,1-Oly:sNy+Oly,Nr) |
115 |
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_RL KappaRS (1-Olx:sNx+Olx,1-Oly:sNy+Oly,Nr) |
116 |
adcroft |
1.12 |
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117 |
cnh |
1.1 |
INTEGER iMin, iMax |
118 |
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INTEGER jMin, jMax |
119 |
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INTEGER bi, bj |
120 |
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INTEGER i, j |
121 |
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INTEGER k, kM1, kUp, kDown |
122 |
cnh |
1.19 |
LOGICAL BOTTOM_LAYER |
123 |
cnh |
1.1 |
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adcroft |
1.11 |
C--- The algorithm... |
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C |
126 |
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C "Correction Step" |
127 |
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C ================= |
128 |
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C Here we update the horizontal velocities with the surface |
129 |
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C pressure such that the resulting flow is either consistent |
130 |
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C with the free-surface evolution or the rigid-lid: |
131 |
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C U[n] = U* + dt x d/dx P |
132 |
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C V[n] = V* + dt x d/dy P |
133 |
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C |
134 |
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C "Calculation of Gs" |
135 |
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C =================== |
136 |
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C This is where all the accelerations and tendencies (ie. |
137 |
cnh |
1.31 |
C phiHydysics, parameterizations etc...) are calculated |
138 |
cnh |
1.27 |
C rVel = sum_r ( div. u[n] ) |
139 |
adcroft |
1.11 |
C rho = rho ( theta[n], salt[n] ) |
140 |
cnh |
1.27 |
C b = b(rho, theta) |
141 |
adcroft |
1.11 |
C K31 = K31 ( rho ) |
142 |
cnh |
1.27 |
C Gu[n] = Gu( u[n], v[n], rVel, b, ... ) |
143 |
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C Gv[n] = Gv( u[n], v[n], rVel, b, ... ) |
144 |
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C Gt[n] = Gt( theta[n], u[n], v[n], rVel, K31, ... ) |
145 |
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C Gs[n] = Gs( salt[n], u[n], v[n], rVel, K31, ... ) |
146 |
adcroft |
1.11 |
C |
147 |
adcroft |
1.12 |
C "Time-stepping" or "Prediction" |
148 |
adcroft |
1.11 |
C ================================ |
149 |
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C The models variables are stepped forward with the appropriate |
150 |
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C time-stepping scheme (currently we use Adams-Bashforth II) |
151 |
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C - For momentum, the result is always *only* a "prediction" |
152 |
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C in that the flow may be divergent and will be "corrected" |
153 |
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C later with a surface pressure gradient. |
154 |
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C - Normally for tracers the result is the new field at time |
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C level [n+1} *BUT* in the case of implicit diffusion the result |
156 |
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C is also *only* a prediction. |
157 |
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C - We denote "predictors" with an asterisk (*). |
158 |
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C U* = U[n] + dt x ( 3/2 Gu[n] - 1/2 Gu[n-1] ) |
159 |
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C V* = V[n] + dt x ( 3/2 Gv[n] - 1/2 Gv[n-1] ) |
160 |
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C theta[n+1] = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
161 |
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C salt[n+1] = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
162 |
adcroft |
1.12 |
C With implicit diffusion: |
163 |
adcroft |
1.11 |
C theta* = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
164 |
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C salt* = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
165 |
adcroft |
1.12 |
C (1 + dt * K * d_zz) theta[n] = theta* |
166 |
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C (1 + dt * K * d_zz) salt[n] = salt* |
167 |
adcroft |
1.11 |
C--- |
168 |
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169 |
cnh |
1.1 |
C-- Set up work arrays with valid (i.e. not NaN) values |
170 |
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C These inital values do not alter the numerical results. They |
171 |
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C just ensure that all memory references are to valid floating |
172 |
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C point numbers. This prevents spurious hardware signals due to |
173 |
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C uninitialised but inert locations. |
174 |
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DO j=1-OLy,sNy+OLy |
175 |
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DO i=1-OLx,sNx+OLx |
176 |
adcroft |
1.5 |
xA(i,j) = 0. _d 0 |
177 |
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yA(i,j) = 0. _d 0 |
178 |
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uTrans(i,j) = 0. _d 0 |
179 |
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vTrans(i,j) = 0. _d 0 |
180 |
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aTerm(i,j) = 0. _d 0 |
181 |
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xTerm(i,j) = 0. _d 0 |
182 |
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cTerm(i,j) = 0. _d 0 |
183 |
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mTerm(i,j) = 0. _d 0 |
184 |
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pTerm(i,j) = 0. _d 0 |
185 |
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fZon(i,j) = 0. _d 0 |
186 |
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fMer(i,j) = 0. _d 0 |
187 |
cnh |
1.31 |
DO K=1,Nr |
188 |
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phiHyd (i,j,k) = 0. _d 0 |
189 |
cnh |
1.30 |
K13(i,j,k) = 0. _d 0 |
190 |
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K23(i,j,k) = 0. _d 0 |
191 |
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K33(i,j,k) = 0. _d 0 |
192 |
cnh |
1.31 |
KappaRT(i,j,k) = 0. _d 0 |
193 |
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KappaRS(i,j,k) = 0. _d 0 |
194 |
cnh |
1.1 |
ENDDO |
195 |
cnh |
1.30 |
rhoKM1 (i,j) = 0. _d 0 |
196 |
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rhok (i,j) = 0. _d 0 |
197 |
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rhoKP1 (i,j) = 0. _d 0 |
198 |
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rhoTMP (i,j) = 0. _d 0 |
199 |
cnh |
1.26 |
buoyKM1(i,j) = 0. _d 0 |
200 |
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buoyK (i,j) = 0. _d 0 |
201 |
cnh |
1.30 |
maskC (i,j) = 0. _d 0 |
202 |
cnh |
1.1 |
ENDDO |
203 |
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ENDDO |
204 |
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205 |
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DO bj=myByLo(myThid),myByHi(myThid) |
206 |
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DO bi=myBxLo(myThid),myBxHi(myThid) |
207 |
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208 |
cnh |
1.7 |
C-- Set up work arrays that need valid initial values |
209 |
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DO j=1-OLy,sNy+OLy |
210 |
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DO i=1-OLx,sNx+OLx |
211 |
cnh |
1.27 |
rTrans(i,j) = 0. _d 0 |
212 |
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rVel (i,j,1) = 0. _d 0 |
213 |
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rVel (i,j,2) = 0. _d 0 |
214 |
cnh |
1.30 |
fVerT (i,j,1) = 0. _d 0 |
215 |
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fVerT (i,j,2) = 0. _d 0 |
216 |
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fVerS (i,j,1) = 0. _d 0 |
217 |
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fVerS (i,j,2) = 0. _d 0 |
218 |
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fVerU (i,j,1) = 0. _d 0 |
219 |
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fVerU (i,j,2) = 0. _d 0 |
220 |
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fVerV (i,j,1) = 0. _d 0 |
221 |
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fVerV (i,j,2) = 0. _d 0 |
222 |
cnh |
1.27 |
phiHyd(i,j,1) = 0. _d 0 |
223 |
cnh |
1.30 |
K13 (i,j,1) = 0. _d 0 |
224 |
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K23 (i,j,1) = 0. _d 0 |
225 |
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K33 (i,j,1) = 0. _d 0 |
226 |
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KapGM (i,j) = GMkbackground |
227 |
cnh |
1.7 |
ENDDO |
228 |
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ENDDO |
229 |
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230 |
cnh |
1.1 |
iMin = 1-OLx+1 |
231 |
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iMax = sNx+OLx |
232 |
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jMin = 1-OLy+1 |
233 |
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jMax = sNy+OLy |
234 |
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235 |
cnh |
1.19 |
K = 1 |
236 |
cnh |
1.31 |
BOTTOM_LAYER = K .EQ. Nr |
237 |
cnh |
1.19 |
|
238 |
adcroft |
1.4 |
C-- Calculate gradient of surface pressure |
239 |
cnh |
1.28 |
CALL CALC_GRAD_ETA_SURF( |
240 |
adcroft |
1.4 |
I bi,bj,iMin,iMax,jMin,jMax, |
241 |
cnh |
1.29 |
O etaSurfX,etaSurfY, |
242 |
adcroft |
1.4 |
I myThid) |
243 |
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C-- Update fields in top level according to tendency terms |
244 |
adcroft |
1.11 |
CALL CORRECTION_STEP( |
245 |
cnh |
1.30 |
I bi,bj,iMin,iMax,jMin,jMax,K, |
246 |
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I etaSurfX,etaSurfY,myTime,myThid) |
247 |
adcroft |
1.21 |
IF ( .NOT. BOTTOM_LAYER ) THEN |
248 |
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C-- Update fields in layer below according to tendency terms |
249 |
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CALL CORRECTION_STEP( |
250 |
cnh |
1.30 |
I bi,bj,iMin,iMax,jMin,jMax,K+1, |
251 |
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I etaSurfX,etaSurfY,myTime,myThid) |
252 |
adcroft |
1.21 |
ENDIF |
253 |
cnh |
1.7 |
C-- Density of 1st level (below W(1)) reference to level 1 |
254 |
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CALL FIND_RHO( |
255 |
cnh |
1.19 |
I bi, bj, iMin, iMax, jMin, jMax, K, K, eosType, |
256 |
cnh |
1.7 |
O rhoKm1, |
257 |
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I myThid ) |
258 |
cnh |
1.19 |
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259 |
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IF ( .NOT. BOTTOM_LAYER ) THEN |
260 |
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C-- Check static stability with layer below |
261 |
cnh |
1.30 |
C-- and mix as needed. |
262 |
cnh |
1.19 |
CALL FIND_RHO( |
263 |
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I bi, bj, iMin, iMax, jMin, jMax, K+1, K, eosType, |
264 |
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O rhoKp1, |
265 |
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I myThid ) |
266 |
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CALL CONVECT( |
267 |
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I bi,bj,iMin,iMax,jMin,jMax,K+1,rhoKm1,rhoKp1, |
268 |
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I myTime,myIter,myThid) |
269 |
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C-- Recompute density after mixing |
270 |
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CALL FIND_RHO( |
271 |
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I bi, bj, iMin, iMax, jMin, jMax, K, K, eosType, |
272 |
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O rhoKm1, |
273 |
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I myThid ) |
274 |
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ENDIF |
275 |
cnh |
1.26 |
C-- Calculate buoyancy |
276 |
cnh |
1.32 |
CALL CALC_BUOYANCY( |
277 |
cnh |
1.26 |
I bi,bj,iMin,iMax,jMin,jMax,K,rhoKm1, |
278 |
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O buoyKm1, |
279 |
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I myThid ) |
280 |
cnh |
1.31 |
C-- Integrate hydrostatic balance for phiHyd with BC of phiHyd(z=0)=0 |
281 |
cnh |
1.26 |
CALL CALC_PHI_HYD( |
282 |
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I bi,bj,iMin,iMax,jMin,jMax,K,buoyKm1,buoyKm1, |
283 |
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U phiHyd, |
284 |
adcroft |
1.5 |
I myThid ) |
285 |
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286 |
cnh |
1.31 |
DO K=2,Nr |
287 |
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BOTTOM_LAYER = K .EQ. Nr |
288 |
adcroft |
1.21 |
IF ( .NOT. BOTTOM_LAYER ) THEN |
289 |
|
|
C-- Update fields in layer below according to tendency terms |
290 |
|
|
CALL CORRECTION_STEP( |
291 |
cnh |
1.30 |
I bi,bj,iMin,iMax,jMin,jMax,K+1, |
292 |
|
|
I etaSurfX,etaSurfY,myTime,myThid) |
293 |
adcroft |
1.21 |
ENDIF |
294 |
cnh |
1.19 |
C-- Density of K level (below W(K)) reference to K level |
295 |
|
|
CALL FIND_RHO( |
296 |
|
|
I bi, bj, iMin, iMax, jMin, jMax, K, K, eosType, |
297 |
|
|
O rhoK, |
298 |
|
|
I myThid ) |
299 |
|
|
IF ( .NOT. BOTTOM_LAYER ) THEN |
300 |
cnh |
1.27 |
C-- Check static stability with layer below and mix as needed. |
301 |
|
|
C-- Density of K+1 level (below W(K+1)) reference to K level. |
302 |
cnh |
1.19 |
CALL FIND_RHO( |
303 |
|
|
I bi, bj, iMin, iMax, jMin, jMax, K+1, K, eosType, |
304 |
|
|
O rhoKp1, |
305 |
|
|
I myThid ) |
306 |
|
|
CALL CONVECT( |
307 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,K+1,rhoK,rhoKp1, |
308 |
|
|
I myTime,myIter,myThid) |
309 |
|
|
C-- Recompute density after mixing |
310 |
|
|
CALL FIND_RHO( |
311 |
|
|
I bi, bj, iMin, iMax, jMin, jMax, K, K, eosType, |
312 |
|
|
O rhoK, |
313 |
|
|
I myThid ) |
314 |
|
|
ENDIF |
315 |
cnh |
1.26 |
C-- Calculate buoyancy |
316 |
cnh |
1.32 |
CALL CALC_BUOYANCY( |
317 |
cnh |
1.26 |
I bi,bj,iMin,iMax,jMin,jMax,K,rhoK, |
318 |
|
|
O buoyK, |
319 |
|
|
I myThid ) |
320 |
cnh |
1.31 |
C-- Integrate hydrostatic balance for phiHyd with BC of phiHyd(z=0)=0 |
321 |
cnh |
1.26 |
CALL CALC_PHI_HYD( |
322 |
cnh |
1.30 |
I bi,bj,iMin,iMax,jMin,jMax,K,buoyKm1,buoyK, |
323 |
|
|
U phiHyd, |
324 |
|
|
I myThid ) |
325 |
cnh |
1.19 |
C-- Calculate iso-neutral slopes for the GM/Redi parameterisation |
326 |
|
|
CALL FIND_RHO( |
327 |
cnh |
1.30 |
I bi, bj, iMin, iMax, jMin, jMax, K-1, K, eosType, |
328 |
|
|
O rhoTmp, |
329 |
|
|
I myThid ) |
330 |
cnh |
1.19 |
CALL CALC_ISOSLOPES( |
331 |
cnh |
1.30 |
I bi, bj, iMin, iMax, jMin, jMax, K, |
332 |
|
|
I rhoKm1, rhoK, rhotmp, |
333 |
|
|
O K13, K23, K33, KapGM, |
334 |
|
|
I myThid ) |
335 |
cnh |
1.19 |
DO J=jMin,jMax |
336 |
|
|
DO I=iMin,iMax |
337 |
cnh |
1.27 |
rhoKm1 (I,J) = rhoK(I,J) |
338 |
|
|
buoyKm1(I,J) = buoyK(I,J) |
339 |
cnh |
1.19 |
ENDDO |
340 |
adcroft |
1.10 |
ENDDO |
341 |
adcroft |
1.11 |
ENDDO ! K |
342 |
|
|
|
343 |
cnh |
1.31 |
DO K = Nr, 1, -1 |
344 |
cnh |
1.30 |
|
345 |
cnh |
1.1 |
kM1 =max(1,k-1) ! Points to level above k (=k-1) |
346 |
|
|
kUp =1+MOD(k+1,2) ! Cycles through 1,2 to point to layer above |
347 |
|
|
kDown=1+MOD(k,2) ! Cycles through 2,1 to point to current layer |
348 |
|
|
iMin = 1-OLx+2 |
349 |
|
|
iMax = sNx+OLx-1 |
350 |
|
|
jMin = 1-OLy+2 |
351 |
|
|
jMax = sNy+OLy-1 |
352 |
|
|
|
353 |
|
|
C-- Get temporary terms used by tendency routines |
354 |
|
|
CALL CALC_COMMON_FACTORS ( |
355 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,k,kM1,kUp,kDown, |
356 |
cnh |
1.30 |
O xA,yA,uTrans,vTrans,rTrans,rVel,maskC,maskUp, |
357 |
cnh |
1.1 |
I myThid) |
358 |
cnh |
1.33 |
CcnhDebugStarts |
359 |
|
|
IF ( K .EQ. 1 ) THEN |
360 |
|
|
CALL PLOT_FIELD_XYRL( rVel(1,1,1), 'K=1 Current rVel.1 ' , myIter, myThid ) |
361 |
|
|
CALL PLOT_FIELD_XYRL( rVel(1,1,2), 'K=1 Current rVel.2 ' , myIter, myThid ) |
362 |
|
|
ENDIF |
363 |
|
|
CcnhDebugEnds |
364 |
adcroft |
1.12 |
C-- Calculate the total vertical diffusivity |
365 |
|
|
CALL CALC_DIFFUSIVITY( |
366 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,K, |
367 |
|
|
I maskC,maskUp,KapGM,K33, |
368 |
cnh |
1.31 |
O KappaRT,KappaRS, |
369 |
adcroft |
1.12 |
I myThid) |
370 |
cnh |
1.1 |
C-- Calculate accelerations in the momentum equations |
371 |
cnh |
1.9 |
IF ( momStepping ) THEN |
372 |
|
|
CALL CALC_MOM_RHS( |
373 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,k,kM1,kUp,kDown, |
374 |
cnh |
1.30 |
I xA,yA,uTrans,vTrans,rTrans,rVel,maskC, |
375 |
cnh |
1.26 |
I phiHyd, |
376 |
cnh |
1.9 |
U aTerm,xTerm,cTerm,mTerm,pTerm, |
377 |
|
|
U fZon, fMer, fVerU, fVerV, |
378 |
|
|
I myThid) |
379 |
|
|
ENDIF |
380 |
cnh |
1.1 |
C-- Calculate active tracer tendencies |
381 |
cnh |
1.9 |
IF ( tempStepping ) THEN |
382 |
|
|
CALL CALC_GT( |
383 |
|
|
I bi,bj,iMin,iMax,jMin,jMax, k,kM1,kUp,kDown, |
384 |
cnh |
1.30 |
I xA,yA,uTrans,vTrans,rTrans,maskUp,maskC, |
385 |
|
|
I K13,K23,KappaRT,KapGM, |
386 |
cnh |
1.9 |
U aTerm,xTerm,fZon,fMer,fVerT, |
387 |
|
|
I myThid) |
388 |
|
|
ENDIF |
389 |
adcroft |
1.18 |
IF ( saltStepping ) THEN |
390 |
|
|
CALL CALC_GS( |
391 |
|
|
I bi,bj,iMin,iMax,jMin,jMax, k,kM1,kUp,kDown, |
392 |
cnh |
1.30 |
I xA,yA,uTrans,vTrans,rTrans,maskUp,maskC, |
393 |
|
|
I K13,K23,KappaRS,KapGM, |
394 |
adcroft |
1.18 |
U aTerm,xTerm,fZon,fMer,fVerS, |
395 |
|
|
I myThid) |
396 |
|
|
ENDIF |
397 |
adcroft |
1.11 |
C-- Prediction step (step forward all model variables) |
398 |
|
|
CALL TIMESTEP( |
399 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,K, |
400 |
|
|
I myThid) |
401 |
|
|
C-- Diagnose barotropic divergence of predicted fields |
402 |
cnh |
1.31 |
CALL CALC_DIV_GHAT( |
403 |
adcroft |
1.11 |
I bi,bj,iMin,iMax,jMin,jMax,K, |
404 |
|
|
I xA,yA, |
405 |
|
|
I myThid) |
406 |
adcroft |
1.23 |
|
407 |
|
|
C-- Cumulative diagnostic calculations (ie. time-averaging) |
408 |
|
|
#ifdef ALLOW_DIAGNOSTICS |
409 |
|
|
IF (taveFreq.GT.0.) THEN |
410 |
|
|
CALL DO_TIME_AVERAGES( |
411 |
|
|
I myTime, myIter, bi, bj, K, kUp, kDown, |
412 |
cnh |
1.30 |
I K13, K23, rVel, KapGM, |
413 |
adcroft |
1.23 |
I myThid ) |
414 |
|
|
ENDIF |
415 |
|
|
#endif |
416 |
adcroft |
1.11 |
|
417 |
|
|
ENDDO ! K |
418 |
adcroft |
1.12 |
|
419 |
|
|
C-- Implicit diffusion |
420 |
|
|
IF (implicitDiffusion) THEN |
421 |
|
|
CALL IMPLDIFF( bi, bj, iMin, iMax, jMin, jMax, |
422 |
cnh |
1.31 |
I KappaRT,KappaRS, |
423 |
adcroft |
1.12 |
I myThid ) |
424 |
|
|
ENDIF |
425 |
cnh |
1.1 |
|
426 |
|
|
ENDDO |
427 |
|
|
ENDDO |
428 |
adcroft |
1.6 |
|
429 |
cnh |
1.19 |
C write(0,*) 'dynamics: pS ',minval(cg2d_x(1:sNx,1:sNy,:,:)), |
430 |
|
|
C & maxval(cg2d_x(1:sNx,1:sNy,:,:)) |
431 |
cnh |
1.20 |
C write(0,*) 'dynamics: U ',minval(uVel(1:sNx,1:sNy,1,:,:),mask=uVel(1:sNx,1:sNy,1,:,:).NE.0.), |
432 |
adcroft |
1.21 |
C & maxval(uVel(1:sNx,1:sNy,1,:,:),mask=uVel(1:sNx,1:sNy,1,:,:).NE.0.) |
433 |
cnh |
1.20 |
C write(0,*) 'dynamics: V ',minval(vVel(1:sNx,1:sNy,1,:,:),mask=vVel(1:sNx,1:sNy,1,:,:).NE.0.), |
434 |
adcroft |
1.21 |
C & maxval(vVel(1:sNx,1:sNy,1,:,:),mask=vVel(1:sNx,1:sNy,1,:,:).NE.0.) |
435 |
cnh |
1.30 |
C write(0,*) 'dynamics: rVel(1) ', |
436 |
|
|
C & minval(rVel(1:sNx,1:sNy,1),mask=rVel(1:sNx,1:sNy,1).NE.0.), |
437 |
|
|
C & maxval(rVel(1:sNx,1:sNy,1),mask=rVel(1:sNx,1:sNy,1).NE.0.) |
438 |
|
|
C write(0,*) 'dynamics: rVel(2) ', |
439 |
|
|
C & minval(rVel(1:sNx,1:sNy,2),mask=rVel(1:sNx,1:sNy,2).NE.0.), |
440 |
|
|
C & maxval(rVel(1:sNx,1:sNy,2),mask=rVel(1:sNx,1:sNy,2).NE.0.) |
441 |
adcroft |
1.15 |
cblk write(0,*) 'dynamics: K13',minval(K13(1:sNx,1:sNy,:)), |
442 |
|
|
cblk & maxval(K13(1:sNx,1:sNy,:)) |
443 |
|
|
cblk write(0,*) 'dynamics: K23',minval(K23(1:sNx,1:sNy,:)), |
444 |
|
|
cblk & maxval(K23(1:sNx,1:sNy,:)) |
445 |
|
|
cblk write(0,*) 'dynamics: K33',minval(K33(1:sNx,1:sNy,:)), |
446 |
|
|
cblk & maxval(K33(1:sNx,1:sNy,:)) |
447 |
cnh |
1.19 |
C write(0,*) 'dynamics: gT ',minval(gT(1:sNx,1:sNy,:,:,:)), |
448 |
|
|
C & maxval(gT(1:sNx,1:sNy,:,:,:)) |
449 |
|
|
C write(0,*) 'dynamics: T ',minval(Theta(1:sNx,1:sNy,:,:,:)), |
450 |
|
|
C & maxval(Theta(1:sNx,1:sNy,:,:,:)) |
451 |
|
|
C write(0,*) 'dynamics: gS ',minval(gS(1:sNx,1:sNy,:,:,:)), |
452 |
|
|
C & maxval(gS(1:sNx,1:sNy,:,:,:)) |
453 |
|
|
C write(0,*) 'dynamics: S ',minval(salt(1:sNx,1:sNy,:,:,:)), |
454 |
|
|
C & maxval(salt(1:sNx,1:sNy,:,:,:)) |
455 |
cnh |
1.31 |
C write(0,*) 'dynamics: phiHyd ',minval(phiHyd/(Gravity*Rhonil),mask=phiHyd.NE.0.), |
456 |
|
|
C & maxval(phiHyd/(Gravity*Rhonil)) |
457 |
cnh |
1.1 |
|
458 |
|
|
RETURN |
459 |
|
|
END |