/[MITgcm]/MITgcm/model/src/dynamics.F
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Contents of /MITgcm/model/src/dynamics.F

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Revision 1.5 - (show annotations) (download)
Mon May 4 16:32:10 1998 UTC (26 years ago) by adcroft
Branch: MAIN
CVS Tags: checkpoint1
Changes since 1.4: +33 -27 lines
Changed the descretization of hydrostatic pressure (now barZ(dz)*barZ(rho) )
to conserve potential energy. This was the original discretization but
when I (AJA) made the outer K loop I changed the discretization. Sorry.

1 C $Header: /u/gcmpack/models/MITgcmUV/model/src/dynamics.F,v 1.4 1998/04/30 14:03:28 adcroft Exp $
2
3 #include "CPP_EEOPTIONS.h"
4
5 SUBROUTINE DYNAMICS(myThid)
6 C /==========================================================\
7 C | SUBROUTINE DYNAMICS |
8 C | o Controlling routine for the explicit part of the model |
9 C | dynamics. |
10 C |==========================================================|
11 C | This routine evaluates the "dynamics" terms for each |
12 C | block of ocean in turn. Because the blocks of ocean have |
13 C | overlap regions they are independent of one another. |
14 C | If terms involving lateral integrals are needed in this |
15 C | routine care will be needed. Similarly finite-difference |
16 C | operations with stencils wider than the overlap region |
17 C | require special consideration. |
18 C | Notes |
19 C | ===== |
20 C | C*P* comments indicating place holders for which code is |
21 C | presently being developed. |
22 C \==========================================================/
23
24 C == Global variables ===
25 #include "SIZE.h"
26 #include "EEPARAMS.h"
27 #include "CG2D.h"
28 #include "DYNVARS.h"
29
30 C == Routine arguments ==
31 C myThid - Thread number for this instance of the routine.
32 INTEGER myThid
33
34 C == Local variables
35 C xA, yA - Per block temporaries holding face areas
36 C uTrans, vTrans, wTrans - Per block temporaries holding flow transport
37 C o uTrans: Zonal transport
38 C o vTrans: Meridional transport
39 C o wTrans: Vertical transport
40 C maskC,maskUp o maskC: land/water mask for tracer cells
41 C o maskUp: land/water mask for W points
42 C aTerm, xTerm, cTerm - Work arrays for holding separate terms in
43 C mTerm, pTerm, tendency equations.
44 C fZon, fMer, fVer[STUV] o aTerm: Advection term
45 C o xTerm: Mixing term
46 C o cTerm: Coriolis term
47 C o mTerm: Metric term
48 C o pTerm: Pressure term
49 C o fZon: Zonal flux term
50 C o fMer: Meridional flux term
51 C o fVer: Vertical flux term - note fVer
52 C is "pipelined" in the vertical
53 C so we need an fVer for each
54 C variable.
55 C iMin, iMax - Ranges and sub-block indices on which calculations
56 C jMin, jMax are applied.
57 C bi, bj
58 C k, kUp, kDown, kM1 - Index for layer above and below. kUp and kDown
59 C are switched with layer to be the appropriate index
60 C into fVerTerm
61 _RS xA (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
62 _RS yA (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
63 _RL uTrans(1-OLx:sNx+OLx,1-OLy:sNy+OLy)
64 _RL vTrans(1-OLx:sNx+OLx,1-OLy:sNy+OLy)
65 _RL wTrans(1-OLx:sNx+OLx,1-OLy:sNy+OLy)
66 _RS maskC (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
67 _RS maskUp(1-OLx:sNx+OLx,1-OLy:sNy+OLy)
68 _RL aTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
69 _RL xTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
70 _RL cTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
71 _RL mTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
72 _RL pTerm (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
73 _RL fZon (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
74 _RL fMer (1-OLx:sNx+OLx,1-OLy:sNy+OLy)
75 _RL fVerT (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2)
76 _RL fVerS (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2)
77 _RL fVerU (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2)
78 _RL fVerV (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2)
79 _RL pH (1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nz)
80 _RL rhokm1(1-OLx:sNx+OLx,1-OLy:sNy+OLy)
81 _RL rhokp1(1-OLx:sNx+OLx,1-OLy:sNy+OLy)
82 _RL pSurfX(1-OLx:sNx+OLx,1-OLy:sNy+OLy)
83 _RL pSurfY(1-OLx:sNx+OLx,1-OLy:sNy+OLy)
84 INTEGER iMin, iMax
85 INTEGER jMin, jMax
86 INTEGER bi, bj
87 INTEGER i, j
88 INTEGER k, kM1, kUp, kDown
89
90 C-- Set up work arrays with valid (i.e. not NaN) values
91 C These inital values do not alter the numerical results. They
92 C just ensure that all memory references are to valid floating
93 C point numbers. This prevents spurious hardware signals due to
94 C uninitialised but inert locations.
95 DO j=1-OLy,sNy+OLy
96 DO i=1-OLx,sNx+OLx
97 xA(i,j) = 0. _d 0
98 yA(i,j) = 0. _d 0
99 uTrans(i,j) = 0. _d 0
100 vTrans(i,j) = 0. _d 0
101 aTerm(i,j) = 0. _d 0
102 xTerm(i,j) = 0. _d 0
103 cTerm(i,j) = 0. _d 0
104 mTerm(i,j) = 0. _d 0
105 pTerm(i,j) = 0. _d 0
106 fZon(i,j) = 0. _d 0
107 fMer(i,j) = 0. _d 0
108 DO K=1,nZ
109 pH (i,j,k) = 0. _d 0
110 ENDDO
111 rhokm1(i,j) = 0. _d 0
112 rhokp1(i,j) = 0. _d 0
113 ENDDO
114 ENDDO
115 C-- Set up work arrays that need valid initial values
116 DO j=1-OLy,sNy+OLy
117 DO i=1-OLx,sNx+OLx
118 wTrans(i,j) = 0. _d 0
119 fVerT(i,j,1) = 0. _d 0
120 fVerT(i,j,2) = 0. _d 0
121 fVerS(i,j,1) = 0. _d 0
122 fVerS(i,j,2) = 0. _d 0
123 fVerU(i,j,1) = 0. _d 0
124 fVerU(i,j,2) = 0. _d 0
125 fVerV(i,j,1) = 0. _d 0
126 fVerV(i,j,2) = 0. _d 0
127 ENDDO
128 ENDDO
129
130 DO bj=myByLo(myThid),myByHi(myThid)
131 DO bi=myBxLo(myThid),myBxHi(myThid)
132
133 C-- Boundary condition on hydrostatic pressure is pH(z=0)=0
134 DO j=1-OLy,sNy+OLy
135 DO i=1-OLx,sNx+OLx
136 pH(i,j,1) = 0. _d 0
137 ENDDO
138 ENDDO
139
140 iMin = 1-OLx+1
141 iMax = sNx+OLx
142 jMin = 1-OLy+1
143 jMax = sNy+OLy
144
145 C-- Calculate gradient of surface pressure
146 CALL GRAD_PSURF(
147 I bi,bj,iMin,iMax,jMin,jMax,
148 O pSurfX,pSurfY,
149 I myThid)
150
151 C-- Update fields in top level according to tendency terms
152 CALL TIMESTEP(
153 I bi,bj,iMin,iMax,jMin,jMax,1,pSurfX,pSurfY,myThid)
154
155 C Density of 1st level (below W(1)) reference to level 1
156 CALL FIND_RHO(
157 I bi, bj, iMin, iMax, jMin, jMax, 1, 1, 'LINEAR',
158 O rhoKm1,
159 I myThid )
160 C-- Integrate hydrostatic balance for pH with BC of pH(z=0)=0
161 CALL CALC_PH(
162 I bi,bj,iMin,iMax,jMin,jMax,1,rhoKm1,rhoKm1,
163 U pH,
164 I myThid )
165
166 DO K=2,Nz
167 C-- Update fields in Kth level according to tendency terms
168 CALL TIMESTEP(
169 I bi,bj,iMin,iMax,jMin,jMax,K,pSurfX,pSurfY,myThid)
170 C Density of K-1 level (above W(K)) reference to K level
171 CALL FIND_RHO(
172 I bi, bj, iMin, iMax, jMin, jMax, K-1, K, 'LINEAR',
173 O rhoKm1,
174 I myThid )
175 C Density of K level (below W(K)) reference to K level
176 CALL FIND_RHO(
177 I bi, bj, iMin, iMax, jMin, jMax, K, K, 'LINEAR',
178 O rhoKp1,
179 I myThid )
180 C-- Calculate static stability and mix where convectively unstable
181 CALL CONVECT(
182 I bi,bj,iMin,iMax,jMin,jMax,K,rhoKm1,rhoKp1,myThid)
183 C Density of K-1 level (above W(K)) reference to K-1 level
184 CALL FIND_RHO(
185 I bi, bj, iMin, iMax, jMin, jMax, K-1, K-1, 'LINEAR',
186 O rhoKm1,
187 I myThid )
188 C Density of K level (below W(K)) referenced to K level
189 CALL FIND_RHO(
190 I bi, bj, iMin, iMax, jMin, jMax, K, K, 'LINEAR',
191 O rhoKp1,
192 I myThid )
193 C-- Integrate hydrostatic balance for pH with BC of pH(z=0)=0
194 CALL CALC_PH(
195 I bi,bj,iMin,iMax,jMin,jMax,K,rhoKm1,rhoKp1,
196 U pH,
197 I myThid )
198
199 ENDDO ! K
200
201 DO K = Nz, 1, -1
202 kM1 =max(1,k-1) ! Points to level above k (=k-1)
203 kUp =1+MOD(k+1,2) ! Cycles through 1,2 to point to layer above
204 kDown=1+MOD(k,2) ! Cycles through 2,1 to point to current layer
205 iMin = 1-OLx+2
206 iMax = sNx+OLx-1
207 jMin = 1-OLy+2
208 jMax = sNy+OLy-1
209
210 C-- Get temporary terms used by tendency routines
211 CALL CALC_COMMON_FACTORS (
212 I bi,bj,iMin,iMax,jMin,jMax,k,kM1,kUp,kDown,
213 O xA,yA,uTrans,vTrans,wTrans,maskC,maskUp,
214 I myThid)
215
216 C-- Calculate accelerations in the momentum equations
217 CALL CALC_MOM_RHS(
218 I bi,bj,iMin,iMax,jMin,jMax,k,kM1,kUp,kDown,
219 I xA,yA,uTrans,vTrans,wTrans,maskC,
220 I pH,
221 U aTerm,xTerm,cTerm,mTerm,pTerm,
222 U fZon, fMer, fVerU, fVerV,
223 I myThid)
224
225 C-- Calculate active tracer tendencies
226 CALL CALC_GT(
227 I bi,bj,iMin,iMax,jMin,jMax, k,kM1,kUp,kDown,
228 I xA,yA,uTrans,vTrans,wTrans,maskUp,
229 U aTerm,xTerm,fZon,fMer,fVerT,
230 I myThid)
231 Cdbg CALL CALC_GS(
232 Cdbg I bi,bj,iMin,iMax,jMin,jMax, k,kM1,kUp,kDown,
233 Cdbg I xA,yA,uTrans,vTrans,wTrans,maskUp,
234 Cdbg U aTerm,xTerm,fZon,fMer,fVerS,
235 Cdbg I myThid)
236
237 ENDDO ! K
238
239 ENDDO
240 ENDDO
241
242 RETURN
243 END

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