1 |
adcroft |
1.13 |
C $Header: /u/gcmpack/models/MITgcmUV/model/src/dynamics.F,v 1.12 1998/06/01 22:27:14 adcroft Exp $ |
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cnh |
1.1 |
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#include "CPP_EEOPTIONS.h" |
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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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C == Routine arguments == |
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cnh |
1.8 |
C myTime - Current time in simulation |
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C myIter - Current iteration number in simulation |
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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 |
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INTEGER myIter |
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cnh |
1.1 |
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C == Local variables |
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C xA, yA - Per block temporaries holding face areas |
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C uTrans, vTrans, wTrans - Per block temporaries holding flow transport |
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C o uTrans: Zonal transport |
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C o vTrans: Meridional transport |
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C o wTrans: Vertical transport |
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C maskC,maskUp o maskC: land/water mask for tracer cells |
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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 |
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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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C iMin, iMax - Ranges and sub-block indices on which calculations |
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C jMin, jMax are applied. |
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C bi, bj |
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C k, kUp, kDown, kM1 - Index for layer above and below. kUp and kDown |
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C 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 wTrans(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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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) |
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_RL pH (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nz) |
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adcroft |
1.3 |
_RL rhokm1(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL rhokp1(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
87 |
adcroft |
1.10 |
_RL rhotmp(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
88 |
adcroft |
1.4 |
_RL pSurfX(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL pSurfY(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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adcroft |
1.6 |
_RL K13 (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nz) |
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_RL K23 (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nz) |
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_RL K33 (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nz) |
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_RL KapGM (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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adcroft |
1.12 |
_RL KappaZT(1-Olx:sNx+Olx,1-Oly:sNy+Oly,Nz) |
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cnh |
1.1 |
INTEGER iMin, iMax |
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INTEGER jMin, jMax |
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INTEGER bi, bj |
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INTEGER i, j |
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INTEGER k, kM1, kUp, kDown |
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adcroft |
1.11 |
C--- The algorithm... |
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C |
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C "Correction Step" |
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C ================= |
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C Here we update the horizontal velocities with the surface |
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C pressure such that the resulting flow is either consistent |
108 |
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C with the free-surface evolution or the rigid-lid: |
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C U[n] = U* + dt x d/dx P |
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C V[n] = V* + dt x d/dy P |
111 |
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C |
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C "Calculation of Gs" |
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C =================== |
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C This is where all the accelerations and tendencies (ie. |
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C physics, parameterizations etc...) are calculated |
116 |
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C w = sum_z ( div. u[n] ) |
117 |
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C rho = rho ( theta[n], salt[n] ) |
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C K31 = K31 ( rho ) |
119 |
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C Gu[n] = Gu( u[n], v[n], w, rho, Ph, ... ) |
120 |
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C Gv[n] = Gv( u[n], v[n], w, rho, Ph, ... ) |
121 |
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C Gt[n] = Gt( theta[n], u[n], v[n], w, K31, ... ) |
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C Gs[n] = Gs( salt[n], u[n], v[n], w, K31, ... ) |
123 |
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C |
124 |
adcroft |
1.12 |
C "Time-stepping" or "Prediction" |
125 |
adcroft |
1.11 |
C ================================ |
126 |
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C The models variables are stepped forward with the appropriate |
127 |
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C time-stepping scheme (currently we use Adams-Bashforth II) |
128 |
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C - For momentum, the result is always *only* a "prediction" |
129 |
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C in that the flow may be divergent and will be "corrected" |
130 |
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C later with a surface pressure gradient. |
131 |
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C - Normally for tracers the result is the new field at time |
132 |
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C level [n+1} *BUT* in the case of implicit diffusion the result |
133 |
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C is also *only* a prediction. |
134 |
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C - We denote "predictors" with an asterisk (*). |
135 |
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C U* = U[n] + dt x ( 3/2 Gu[n] - 1/2 Gu[n-1] ) |
136 |
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C V* = V[n] + dt x ( 3/2 Gv[n] - 1/2 Gv[n-1] ) |
137 |
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C theta[n+1] = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
138 |
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C salt[n+1] = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
139 |
adcroft |
1.12 |
C With implicit diffusion: |
140 |
adcroft |
1.11 |
C theta* = theta[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
141 |
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C salt* = salt[n] + dt x ( 3/2 Gt[n] - 1/2 atG[n-1] ) |
142 |
adcroft |
1.12 |
C (1 + dt * K * d_zz) theta[n] = theta* |
143 |
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C (1 + dt * K * d_zz) salt[n] = salt* |
144 |
adcroft |
1.11 |
C--- |
145 |
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146 |
cnh |
1.1 |
C-- Set up work arrays with valid (i.e. not NaN) values |
147 |
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C These inital values do not alter the numerical results. They |
148 |
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C just ensure that all memory references are to valid floating |
149 |
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C point numbers. This prevents spurious hardware signals due to |
150 |
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C uninitialised but inert locations. |
151 |
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DO j=1-OLy,sNy+OLy |
152 |
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DO i=1-OLx,sNx+OLx |
153 |
adcroft |
1.5 |
xA(i,j) = 0. _d 0 |
154 |
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yA(i,j) = 0. _d 0 |
155 |
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uTrans(i,j) = 0. _d 0 |
156 |
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vTrans(i,j) = 0. _d 0 |
157 |
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aTerm(i,j) = 0. _d 0 |
158 |
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xTerm(i,j) = 0. _d 0 |
159 |
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cTerm(i,j) = 0. _d 0 |
160 |
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mTerm(i,j) = 0. _d 0 |
161 |
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pTerm(i,j) = 0. _d 0 |
162 |
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fZon(i,j) = 0. _d 0 |
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fMer(i,j) = 0. _d 0 |
164 |
cnh |
1.1 |
DO K=1,nZ |
165 |
adcroft |
1.5 |
pH (i,j,k) = 0. _d 0 |
166 |
adcroft |
1.6 |
K13(i,j,k) = 0. _d 0 |
167 |
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K23(i,j,k) = 0. _d 0 |
168 |
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K33(i,j,k) = 0. _d 0 |
169 |
adcroft |
1.12 |
KappaZT(i,j,k) = 0. _d 0 |
170 |
cnh |
1.1 |
ENDDO |
171 |
adcroft |
1.5 |
rhokm1(i,j) = 0. _d 0 |
172 |
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rhokp1(i,j) = 0. _d 0 |
173 |
adcroft |
1.10 |
rhotmp(i,j) = 0. _d 0 |
174 |
cnh |
1.1 |
ENDDO |
175 |
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ENDDO |
176 |
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177 |
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DO bj=myByLo(myThid),myByHi(myThid) |
178 |
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DO bi=myBxLo(myThid),myBxHi(myThid) |
179 |
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180 |
cnh |
1.7 |
C-- Set up work arrays that need valid initial values |
181 |
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DO j=1-OLy,sNy+OLy |
182 |
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DO i=1-OLx,sNx+OLx |
183 |
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wTrans(i,j) = 0. _d 0 |
184 |
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fVerT(i,j,1) = 0. _d 0 |
185 |
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fVerT(i,j,2) = 0. _d 0 |
186 |
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fVerS(i,j,1) = 0. _d 0 |
187 |
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fVerS(i,j,2) = 0. _d 0 |
188 |
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fVerU(i,j,1) = 0. _d 0 |
189 |
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fVerU(i,j,2) = 0. _d 0 |
190 |
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fVerV(i,j,1) = 0. _d 0 |
191 |
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fVerV(i,j,2) = 0. _d 0 |
192 |
adcroft |
1.11 |
pH(i,j,1) = 0. _d 0 |
193 |
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K13(i,j,1) = 0. _d 0 |
194 |
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K23(i,j,1) = 0. _d 0 |
195 |
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K33(i,j,1) = 0. _d 0 |
196 |
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KapGM(i,j) = 0. _d 0 |
197 |
cnh |
1.7 |
ENDDO |
198 |
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ENDDO |
199 |
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200 |
cnh |
1.1 |
iMin = 1-OLx+1 |
201 |
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iMax = sNx+OLx |
202 |
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jMin = 1-OLy+1 |
203 |
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jMax = sNy+OLy |
204 |
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205 |
adcroft |
1.4 |
C-- Calculate gradient of surface pressure |
206 |
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CALL GRAD_PSURF( |
207 |
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I bi,bj,iMin,iMax,jMin,jMax, |
208 |
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O pSurfX,pSurfY, |
209 |
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I myThid) |
210 |
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211 |
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C-- Update fields in top level according to tendency terms |
212 |
adcroft |
1.11 |
CALL CORRECTION_STEP( |
213 |
adcroft |
1.4 |
I bi,bj,iMin,iMax,jMin,jMax,1,pSurfX,pSurfY,myThid) |
214 |
cnh |
1.1 |
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215 |
cnh |
1.7 |
C-- Density of 1st level (below W(1)) reference to level 1 |
216 |
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CALL FIND_RHO( |
217 |
adcroft |
1.10 |
I bi, bj, iMin, iMax, jMin, jMax, 1, 1, eosType, |
218 |
cnh |
1.7 |
O rhoKm1, |
219 |
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I myThid ) |
220 |
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C-- Integrate hydrostatic balance for pH with BC of pH(z=0)=0 |
221 |
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CALL CALC_PH( |
222 |
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I bi,bj,iMin,iMax,jMin,jMax,1,rhoKm1,rhoKm1, |
223 |
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U pH, |
224 |
adcroft |
1.5 |
I myThid ) |
225 |
adcroft |
1.10 |
DO J=1-Oly,sNy+Oly |
226 |
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DO I=1-Olx,sNx+Olx |
227 |
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rhoKp1(I,J)=rhoKm1(I,J) |
228 |
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ENDDO |
229 |
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ENDDO |
230 |
adcroft |
1.5 |
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231 |
adcroft |
1.3 |
DO K=2,Nz |
232 |
adcroft |
1.4 |
C-- Update fields in Kth level according to tendency terms |
233 |
adcroft |
1.11 |
CALL CORRECTION_STEP( |
234 |
adcroft |
1.4 |
I bi,bj,iMin,iMax,jMin,jMax,K,pSurfX,pSurfY,myThid) |
235 |
adcroft |
1.10 |
C-- Density of K-1 level (above W(K)) reference to K-1 level |
236 |
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copt CALL FIND_RHO( |
237 |
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copt I bi, bj, iMin, iMax, jMin, jMax, K-1, K-1, eosType, |
238 |
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copt O rhoKm1, |
239 |
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copt I myThid ) |
240 |
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C rhoKm1=rhoKp1 |
241 |
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DO J=1-Oly,sNy+Oly |
242 |
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DO I=1-Olx,sNx+Olx |
243 |
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rhoKm1(I,J)=rhoKp1(I,J) |
244 |
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ENDDO |
245 |
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ENDDO |
246 |
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C-- Density of K level (below W(K)) reference to K level |
247 |
cnh |
1.7 |
CALL FIND_RHO( |
248 |
adcroft |
1.10 |
I bi, bj, iMin, iMax, jMin, jMax, K, K, eosType, |
249 |
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O rhoKp1, |
250 |
cnh |
1.7 |
I myThid ) |
251 |
adcroft |
1.10 |
C-- Density of K-1 level (above W(K)) reference to K level |
252 |
cnh |
1.7 |
CALL FIND_RHO( |
253 |
adcroft |
1.10 |
I bi, bj, iMin, iMax, jMin, jMax, K-1, K, eosType, |
254 |
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O rhotmp, |
255 |
cnh |
1.7 |
I myThid ) |
256 |
adcroft |
1.6 |
C-- Calculate iso-neutral slopes for the GM/Redi parameterisation |
257 |
cnh |
1.7 |
CALL CALC_ISOSLOPES( |
258 |
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I bi, bj, iMin, iMax, jMin, jMax, K, |
259 |
adcroft |
1.10 |
I rhoKm1, rhoKp1, rhotmp, |
260 |
cnh |
1.7 |
O K13, K23, K33, KapGM, |
261 |
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I myThid ) |
262 |
cnh |
1.1 |
C-- Calculate static stability and mix where convectively unstable |
263 |
cnh |
1.7 |
CALL CONVECT( |
264 |
adcroft |
1.13 |
I bi,bj,iMin,iMax,jMin,jMax,K,rhotmp,rhoKp1, |
265 |
cnh |
1.8 |
I myTime,myIter,myThid) |
266 |
cnh |
1.7 |
C-- Density of K-1 level (above W(K)) reference to K-1 level |
267 |
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CALL FIND_RHO( |
268 |
adcroft |
1.10 |
I bi, bj, iMin, iMax, jMin, jMax, K-1, K-1, eosType, |
269 |
cnh |
1.7 |
O rhoKm1, |
270 |
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I myThid ) |
271 |
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C-- Density of K level (below W(K)) referenced to K level |
272 |
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CALL FIND_RHO( |
273 |
adcroft |
1.10 |
I bi, bj, iMin, iMax, jMin, jMax, K, K, eosType, |
274 |
cnh |
1.7 |
O rhoKp1, |
275 |
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I myThid ) |
276 |
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C-- Integrate hydrostatic balance for pH with BC of pH(z=0)=0 |
277 |
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CALL CALC_PH( |
278 |
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I bi,bj,iMin,iMax,jMin,jMax,K,rhoKm1,rhoKp1, |
279 |
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U pH, |
280 |
adcroft |
1.3 |
I myThid ) |
281 |
cnh |
1.1 |
|
282 |
adcroft |
1.11 |
ENDDO ! K |
283 |
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284 |
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C-- Initial boundary condition on barotropic divergence integral |
285 |
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DO j=1-OLy,sNy+OLy |
286 |
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DO i=1-OLx,sNx+OLx |
287 |
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cg2d_b(i,j,bi,bj) = 0. _d 0 |
288 |
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ENDDO |
289 |
cnh |
1.7 |
ENDDO |
290 |
adcroft |
1.5 |
|
291 |
cnh |
1.1 |
DO K = Nz, 1, -1 |
292 |
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kM1 =max(1,k-1) ! Points to level above k (=k-1) |
293 |
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kUp =1+MOD(k+1,2) ! Cycles through 1,2 to point to layer above |
294 |
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kDown=1+MOD(k,2) ! Cycles through 2,1 to point to current layer |
295 |
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iMin = 1-OLx+2 |
296 |
|
|
iMax = sNx+OLx-1 |
297 |
|
|
jMin = 1-OLy+2 |
298 |
|
|
jMax = sNy+OLy-1 |
299 |
|
|
|
300 |
|
|
C-- Get temporary terms used by tendency routines |
301 |
|
|
CALL CALC_COMMON_FACTORS ( |
302 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,k,kM1,kUp,kDown, |
303 |
|
|
O xA,yA,uTrans,vTrans,wTrans,maskC,maskUp, |
304 |
|
|
I myThid) |
305 |
|
|
|
306 |
adcroft |
1.12 |
C-- Calculate the total vertical diffusivity |
307 |
|
|
CALL CALC_DIFFUSIVITY( |
308 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,K, |
309 |
|
|
I maskC,maskUp,KapGM,K33, |
310 |
|
|
O KappaZT, |
311 |
|
|
I myThid) |
312 |
|
|
|
313 |
|
|
|
314 |
cnh |
1.1 |
C-- Calculate accelerations in the momentum equations |
315 |
cnh |
1.9 |
IF ( momStepping ) THEN |
316 |
|
|
CALL CALC_MOM_RHS( |
317 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,k,kM1,kUp,kDown, |
318 |
|
|
I xA,yA,uTrans,vTrans,wTrans,maskC, |
319 |
|
|
I pH, |
320 |
|
|
U aTerm,xTerm,cTerm,mTerm,pTerm, |
321 |
|
|
U fZon, fMer, fVerU, fVerV, |
322 |
|
|
I myThid) |
323 |
|
|
ENDIF |
324 |
cnh |
1.1 |
|
325 |
|
|
C-- Calculate active tracer tendencies |
326 |
cnh |
1.9 |
IF ( tempStepping ) THEN |
327 |
|
|
CALL CALC_GT( |
328 |
|
|
I bi,bj,iMin,iMax,jMin,jMax, k,kM1,kUp,kDown, |
329 |
|
|
I xA,yA,uTrans,vTrans,wTrans,maskUp, |
330 |
adcroft |
1.12 |
I K13,K23,KappaZT,KapGM, |
331 |
cnh |
1.9 |
U aTerm,xTerm,fZon,fMer,fVerT, |
332 |
|
|
I myThid) |
333 |
|
|
ENDIF |
334 |
cnh |
1.1 |
Cdbg CALL CALC_GS( |
335 |
|
|
Cdbg I bi,bj,iMin,iMax,jMin,jMax, k,kM1,kUp,kDown, |
336 |
|
|
Cdbg I xA,yA,uTrans,vTrans,wTrans,maskUp, |
337 |
adcroft |
1.6 |
Cdbg I K13,K23,K33,KapGM, |
338 |
cnh |
1.1 |
Cdbg U aTerm,xTerm,fZon,fMer,fVerS, |
339 |
|
|
Cdbg I myThid) |
340 |
|
|
|
341 |
adcroft |
1.11 |
C-- Prediction step (step forward all model variables) |
342 |
|
|
CALL TIMESTEP( |
343 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,K, |
344 |
|
|
I myThid) |
345 |
|
|
|
346 |
|
|
C-- Diagnose barotropic divergence of predicted fields |
347 |
|
|
CALL DIV_G( |
348 |
|
|
I bi,bj,iMin,iMax,jMin,jMax,K, |
349 |
|
|
I xA,yA, |
350 |
|
|
I myThid) |
351 |
|
|
|
352 |
|
|
ENDDO ! K |
353 |
adcroft |
1.12 |
|
354 |
|
|
C-- Implicit diffusion |
355 |
|
|
IF (implicitDiffusion) THEN |
356 |
|
|
CALL IMPLDIFF( bi, bj, iMin, iMax, jMin, jMax, |
357 |
|
|
I KappaZT, |
358 |
|
|
I myThid ) |
359 |
|
|
ENDIF |
360 |
cnh |
1.1 |
|
361 |
|
|
ENDDO |
362 |
|
|
ENDDO |
363 |
adcroft |
1.6 |
|
364 |
adcroft |
1.12 |
write(0,*) 'dynamics: pS',minval(cg2d_x),maxval(cg2d_x) |
365 |
|
|
write(0,*) 'dynamics: U',minval(uVel(1:sNx,1:sNy,:,:,:)), |
366 |
|
|
& maxval(uVel(1:sNx,1:sNy,:,:,:)) |
367 |
|
|
write(0,*) 'dynamics: V',minval(vVel(1:sNx,1:sNy,:,:,:)), |
368 |
|
|
& maxval(vVel(1:sNx,1:sNy,:,:,:)) |
369 |
|
|
write(0,*) 'dynamics: K13',minval(K13(1:sNx,1:sNy,:)), |
370 |
|
|
& maxval(K13(1:sNx,1:sNy,:)) |
371 |
|
|
write(0,*) 'dynamics: K23',minval(K23(1:sNx,1:sNy,:)), |
372 |
|
|
& maxval(K23(1:sNx,1:sNy,:)) |
373 |
|
|
write(0,*) 'dynamics: K33',minval(K33(1:sNx,1:sNy,:)), |
374 |
|
|
& maxval(K33(1:sNx,1:sNy,:)) |
375 |
|
|
write(0,*) 'dynamics: gT',minval(gT(1:sNx,1:sNy,:,:,:)), |
376 |
|
|
& maxval(gT(1:sNx,1:sNy,:,:,:)) |
377 |
|
|
write(0,*) 'dynamics: T',minval(Theta(1:sNx,1:sNy,:,:,:)), |
378 |
|
|
& maxval(Theta(1:sNx,1:sNy,:,:,:)) |
379 |
|
|
write(0,*) 'dynamics: pH',minval(pH/(Gravity*Rhonil)), |
380 |
|
|
& maxval(pH/(Gravity*Rhonil)) |
381 |
cnh |
1.1 |
|
382 |
|
|
RETURN |
383 |
|
|
END |