1 |
jmc |
1.24 |
C $Header: /u/gcmpack/MITgcm/pkg/seaice/seaice_solve4temp.F,v 1.23 2012/01/31 15:57:17 jmc Exp $ |
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jmc |
1.1 |
C $Name: $ |
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#include "SEAICE_OPTIONS.h" |
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jmc |
1.19 |
#ifdef ALLOW_EXF |
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# include "EXF_OPTIONS.h" |
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#endif |
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jmc |
1.1 |
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CBOP |
10 |
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C !ROUTINE: SEAICE_SOLVE4TEMP |
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C !INTERFACE: |
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SUBROUTINE SEAICE_SOLVE4TEMP( |
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I UG, HICE_ACTUAL, HSNOW_ACTUAL, |
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ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
15 |
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I F_lh_max, |
16 |
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#endif |
17 |
jmc |
1.1 |
U TSURF, |
18 |
jmc |
1.21 |
O F_ia, IcePenetSW, |
19 |
mlosch |
1.10 |
O FWsublim, |
20 |
jmc |
1.1 |
I bi, bj, myTime, myIter, myThid ) |
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C !DESCRIPTION: \bv |
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C *==========================================================* |
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C | SUBROUTINE SOLVE4TEMP |
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C | o Calculate ice growth rate, surface fluxes and |
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C | temperature of ice surface. |
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C | see Hibler, MWR, 108, 1943-1973, 1980 |
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C *==========================================================* |
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C \ev |
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C !USES: |
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IMPLICIT NONE |
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C === Global variables === |
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#include "SIZE.h" |
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#include "GRID.h" |
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#include "EEPARAMS.h" |
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jmc |
1.3 |
#include "PARAMS.h" |
38 |
jmc |
1.1 |
#include "FFIELDS.h" |
39 |
heimbach |
1.13 |
#include "SEAICE_SIZE.h" |
40 |
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#include "SEAICE_PARAMS.h" |
41 |
jmc |
1.1 |
#include "SEAICE.h" |
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#ifdef SEAICE_VARIABLE_FREEZING_POINT |
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#include "DYNVARS.h" |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
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#ifdef ALLOW_EXF |
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# include "EXF_FIELDS.h" |
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#endif |
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mlosch |
1.8 |
#ifdef ALLOW_AUTODIFF_TAMC |
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# include "tamc.h" |
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#endif |
51 |
jmc |
1.1 |
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52 |
jmc |
1.21 |
C !INPUT PARAMETERS: |
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C UG :: atmospheric wind speed (m/s) |
54 |
jmc |
1.1 |
C HICE_ACTUAL :: actual ice thickness |
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C HSNOW_ACTUAL :: actual snow thickness |
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jmc |
1.21 |
C TSURF :: surface temperature of ice/snow in Kelvin |
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C bi,bj :: tile indices |
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C myTime :: current time in simulation |
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C myIter :: iteration number in simulation |
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C myThid :: my Thread Id number |
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C !OUTPUT PARAMETERS: |
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C TSURF :: updated surface temperature of ice/snow in Kelvin |
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C F_ia :: upward seaice/snow surface heat flux to atmosphere (W/m^2) |
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C IcePenetSW :: short wave heat flux transmitted through ice (+=upward) |
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C FWsublim :: fresh water (mass) flux due to sublimation (+=up)(kg/m^2/s) |
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jmc |
1.24 |
C---- Notes: |
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C 1) should add IcePenetSW to F_ia to get the net surface heat flux |
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C from the atmosphere (IcePenetSW not currently included in F_ia) |
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C 2) since zero ice/snow heat capacity is assumed, all the absorbed Short |
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C -Wave is used to warm the ice/snow surface (heating profile ignored). |
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C---------- |
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jmc |
1.21 |
_RL UG (1:sNx,1:sNy) |
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_RL HICE_ACTUAL (1:sNx,1:sNy) |
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_RL HSNOW_ACTUAL(1:sNx,1:sNy) |
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ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
76 |
jmc |
1.21 |
_RL F_lh_max (1:sNx,1:sNy) |
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ifenty |
1.16 |
#endif |
78 |
jmc |
1.21 |
_RL TSURF (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
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_RL F_ia (1:sNx,1:sNy) |
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_RL IcePenetSW (1:sNx,1:sNy) |
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_RL FWsublim (1:sNx,1:sNy) |
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jmc |
1.1 |
INTEGER bi, bj |
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_RL myTime |
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INTEGER myIter, myThid |
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jmc |
1.19 |
CEOP |
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jmc |
1.1 |
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jmc |
1.19 |
#if defined(ALLOW_ATM_TEMP) && defined(ALLOW_DOWNWARD_RADIATION) |
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jmc |
1.1 |
C !LOCAL VARIABLES: |
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C === Local variables === |
90 |
jmc |
1.3 |
C i, j :: Loop counters |
91 |
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C kSrf :: vertical index of surface layer |
92 |
jmc |
1.1 |
INTEGER i, j |
93 |
jmc |
1.3 |
#ifdef SEAICE_VARIABLE_FREEZING_POINT |
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INTEGER kSrf |
95 |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
96 |
jmc |
1.1 |
INTEGER ITER |
97 |
jmc |
1.21 |
C TB :: ocean temperature in contact with ice (=seawater freezing point) (K) |
98 |
mlosch |
1.5 |
_RL TB (1:sNx,1:sNy) |
99 |
mlosch |
1.18 |
_RL D1, D1I |
100 |
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_RL D3(1:sNx,1:sNy) |
101 |
mlosch |
1.5 |
_RL TMELT, XKI, XKS, HCUT, XIO |
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_RL SurfMeltTemp |
103 |
jmc |
1.21 |
C effConduct :: effective conductivity of combined ice and snow |
104 |
mlosch |
1.5 |
_RL effConduct(1:sNx,1:sNy) |
105 |
jmc |
1.21 |
C lhSublim :: latent heat of sublimation (SEAICE_lhEvap + SEAICE_lhFusion) |
106 |
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_RL lhSublim |
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C t1,t2,t3,t4 :: powers of temperature |
108 |
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_RL t1, t2, t3, t4 |
109 |
jmc |
1.1 |
|
110 |
jmc |
1.24 |
C- Constants to calculate Saturation Vapor Pressure |
111 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
112 |
jmc |
1.24 |
C Maykut Polynomia Coeff. for Sat. Vapor Press |
113 |
jmc |
1.21 |
_RL C1, C2, C3, C4, C5, QS1 |
114 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
115 |
jmc |
1.24 |
C Extended temp-range expon. relation Coeff. for Sat. Vapor Press |
116 |
jmc |
1.21 |
_RL lnTEN |
117 |
jmc |
1.1 |
_RL aa1,aa2,bb1,bb2,Ppascals,cc0,cc1,cc2,cc3t |
118 |
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C specific humidity at ice surface variables |
119 |
jmc |
1.21 |
_RL mm_pi,mm_log10pi |
120 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
121 |
jmc |
1.1 |
|
122 |
jmc |
1.22 |
C F_c :: conductive heat flux through seaice+snow (+=upward) |
123 |
jmc |
1.21 |
C F_lh :: latent heat flux (sublimation) (+=upward) |
124 |
jmc |
1.24 |
C qhice :: saturation vapor pressure of snow/ice surface |
125 |
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C dqh_dTs :: derivative of qhice w.r.t snow/ice surf. temp |
126 |
jmc |
1.21 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
127 |
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C A1 :: part of atmos surface flux (+=downward) independent of tsurf |
128 |
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C A2 :: part of atmos surface flux (+=upward) which depends on tsurf |
129 |
jmc |
1.24 |
C A3 :: derivative of (A2-F_c) w.r.t tsurf |
130 |
jmc |
1.21 |
_RL A2 (1:sNx,1:sNy) |
131 |
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_RL A3 (1:sNx,1:sNy) |
132 |
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_RL A1 (1:sNx,1:sNy) |
133 |
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#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
134 |
jmc |
1.22 |
C F_lwu :: upward long-wave surface heat flux (+=upward) |
135 |
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C F_sens :: sensible surface heat flux (+=upward) |
136 |
jmc |
1.24 |
C dFia_dTs :: derivative of surf heat flux (F_ia) w.r.t surf. temp |
137 |
jmc |
1.21 |
_RL F_lwu (1:sNx,1:sNy) |
138 |
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_RL F_sens (1:sNx,1:sNy) |
139 |
jmc |
1.24 |
_RL dFia_dTs (1:sNx,1:sNy) |
140 |
jmc |
1.21 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
141 |
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_RL F_lh (1:sNx,1:sNy) |
142 |
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_RL F_c (1:sNx,1:sNy) |
143 |
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_RL qhice (1:sNx,1:sNy) |
144 |
jmc |
1.24 |
_RL dqh_dTs (1:sNx,1:sNy) |
145 |
jmc |
1.21 |
_RL absorbedSW (1:sNx,1:sNy) |
146 |
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_RL penetSWFrac |
147 |
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148 |
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C local copies of global variables |
149 |
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_RL tsurfLoc (1:sNx,1:sNy) |
150 |
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_RL atempLoc (1:sNx,1:sNy) |
151 |
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_RL lwdownLoc (1:sNx,1:sNy) |
152 |
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_RL ALB (1:sNx,1:sNy) |
153 |
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_RL ALB_ICE (1:sNx,1:sNy) |
154 |
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_RL ALB_SNOW (1:sNx,1:sNy) |
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C iceOrNot :: this is HICE_ACTUAL.GT.0. |
156 |
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LOGICAL iceOrNot(1:sNx,1:sNy) |
157 |
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#ifdef SEAICE_DEBUG |
158 |
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C F_io_net :: upward conductive heat flux through seaice+snow |
159 |
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C F_ia_net :: net heat flux divergence at the sea ice/snow surface: |
160 |
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C includes ice conductive fluxes and atmospheric fluxes (W/m^2) |
161 |
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_RL F_io_net (1:sNx,1:sNy) |
162 |
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_RL F_ia_net (1:sNx,1:sNy) |
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#endif /* SEAICE_DEBUG */ |
164 |
ifenty |
1.14 |
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165 |
jmc |
1.21 |
C---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
166 |
jmc |
1.1 |
|
167 |
mlosch |
1.8 |
#ifdef ALLOW_AUTODIFF_TAMC |
168 |
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CADJ INIT comlev1_solve4temp = COMMON, sNx*sNy*NMAX_TICE |
169 |
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#endif /* ALLOW_AUTODIFF_TAMC */ |
170 |
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171 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
172 |
jmc |
1.24 |
C- MAYKUT CONSTANTS FOR SAT. VAP. PRESSURE TEMP. POLYNOMIAL |
173 |
mlosch |
1.5 |
C1= 2.7798202 _d -06 |
174 |
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C2= -2.6913393 _d -03 |
175 |
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C3= 0.97920849 _d +00 |
176 |
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C4= -158.63779 _d +00 |
177 |
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C5= 9653.1925 _d +00 |
178 |
jmc |
1.1 |
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179 |
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QS1=0.622 _d +00/1013.0 _d +00 |
180 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
181 |
jmc |
1.24 |
C- Extended temp-range expon. relation Coeff. for Sat. Vapor Press |
182 |
jmc |
1.21 |
lnTEN = LOG(10.0 _d 0) |
183 |
jmc |
1.1 |
aa1 = 2663.5 _d 0 |
184 |
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aa2 = 12.537 _d 0 |
185 |
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bb1 = 0.622 _d 0 |
186 |
mlosch |
1.5 |
bb2 = 1.0 _d 0 - bb1 |
187 |
jmc |
1.1 |
Ppascals = 100000. _d 0 |
188 |
mlosch |
1.5 |
C cc0 = TEN ** aa2 |
189 |
jmc |
1.21 |
cc0 = EXP(aa2*lnTEN) |
190 |
mlosch |
1.5 |
cc1 = cc0*aa1*bb1*Ppascals*lnTEN |
191 |
jmc |
1.1 |
cc2 = cc0*bb2 |
192 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
193 |
jmc |
1.1 |
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194 |
jmc |
1.4 |
#ifdef SEAICE_VARIABLE_FREEZING_POINT |
195 |
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kSrf = 1 |
196 |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
197 |
jmc |
1.1 |
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198 |
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C SENSIBLE HEAT CONSTANT |
199 |
mlosch |
1.7 |
D1=SEAICE_dalton*SEAICE_cpAir*SEAICE_rhoAir |
200 |
jmc |
1.1 |
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201 |
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C ICE LATENT HEAT CONSTANT |
202 |
ifenty |
1.14 |
lhSublim = SEAICE_lhEvap + SEAICE_lhFusion |
203 |
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D1I=SEAICE_dalton*lhSublim*SEAICE_rhoAir |
204 |
jmc |
1.1 |
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205 |
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C MELTING TEMPERATURE OF ICE |
206 |
mlosch |
1.5 |
TMELT = celsius2K |
207 |
jmc |
1.1 |
SurfMeltTemp = TMELT |
208 |
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209 |
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C ICE CONDUCTIVITY |
210 |
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XKI=SEAICE_iceConduct |
211 |
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212 |
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C SNOW CONDUCTIVITY |
213 |
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XKS=SEAICE_snowConduct |
214 |
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215 |
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C CUTOFF SNOW THICKNESS |
216 |
jmc |
1.21 |
C Snow-Thickness above HCUT: SW optically thick snow (=> snow-albedo). |
217 |
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C Snow-Thickness below HCUT: linear transition to ice-albedo |
218 |
jmc |
1.24 |
HCUT = SEAICE_snowThick |
219 |
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220 |
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C PENETRATION SHORTWAVE RADIATION FACTOR |
221 |
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XIO=SEAICE_shortwave |
222 |
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223 |
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C-- until these become run-time params, set according to CPP OPTION: |
224 |
jmc |
1.21 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
225 |
jmc |
1.24 |
C old SOLVE4TEMP_LEGACY setting, consistent with former celsius2K value: |
226 |
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c TMELT = 273.16 _d +00 |
227 |
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c SurfMeltTemp = 273.159 _d +00 |
228 |
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SurfMeltTemp = TMELT - 1. _d -3 |
229 |
jmc |
1.21 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
230 |
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HCUT = 0. _d 0 |
231 |
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#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
232 |
jmc |
1.1 |
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233 |
jmc |
1.3 |
C Initialize variables |
234 |
jmc |
1.1 |
DO J=1,sNy |
235 |
mlosch |
1.5 |
DO I=1,sNx |
236 |
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C HICE_ACTUAL is modified in this routine, but at the same time |
237 |
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C used to decided where there is ice, therefore we save this information |
238 |
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C here in a separate array |
239 |
jmc |
1.21 |
iceOrNot (I,J) = HICE_ACTUAL(I,J) .GT. 0. _d 0 |
240 |
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IcePenetSW(I,J) = 0. _d 0 |
241 |
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absorbedSW(I,J) = 0. _d 0 |
242 |
mlosch |
1.5 |
qhice (I,J) = 0. _d 0 |
243 |
jmc |
1.24 |
dqh_dTs (I,J) = 0. _d 0 |
244 |
mlosch |
1.5 |
F_ia (I,J) = 0. _d 0 |
245 |
jmc |
1.21 |
c F_io_net (I,J) = 0. _d 0 |
246 |
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c F_ia_net (I,J) = 0. _d 0 |
247 |
mlosch |
1.10 |
F_lh (I,J) = 0. _d 0 |
248 |
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249 |
mlosch |
1.5 |
C Reset the snow/ice surface to TMELT and bound the atmospheric temperature |
250 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
251 |
mlosch |
1.5 |
A1(I,J) = 0.0 _d 0 |
252 |
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A2(I,J) = 0.0 _d 0 |
253 |
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A3(I,J) = 0.0 _d 0 |
254 |
jmc |
1.23 |
tsurfLoc (I,J) = MIN( celsius2K+MAX_TICE, TSURF(I,J,bi,bj) ) |
255 |
jmc |
1.21 |
lwdownLoc(I,J) = MAX( MIN_LWDOWN, LWDOWN(I,J,bi,bj) ) |
256 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
257 |
mlosch |
1.5 |
F_lwu (I,J) = 0. _d 0 |
258 |
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F_sens (I,J) = 0. _d 0 |
259 |
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tsurfLoc (I,J) = TSURF(I,J,bi,bj) |
260 |
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lwdownLoc(I,J) = LWDOWN(I,J,bi,bj) |
261 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
262 |
jmc |
1.24 |
atempLoc (I,J) = MAX( celsius2K+MIN_ATEMP, ATEMP(I,J,bi,bj) ) |
263 |
jmc |
1.1 |
|
264 |
mlosch |
1.5 |
C FREEZING TEMPERATURE OF SEAWATER |
265 |
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#ifdef SEAICE_VARIABLE_FREEZING_POINT |
266 |
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C Use a variable seawater freezing point |
267 |
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TB(I,J) = -0.0575 _d 0*salt(I,J,kSrf,bi,bj) + 0.0901 _d 0 |
268 |
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& + celsius2K |
269 |
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#else |
270 |
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C Use a constant freezing temperature (SEAICE_VARIABLE_FREEZING_POINT undef) |
271 |
jmc |
1.23 |
C old SOLVE4TEMP_LEGACY setting (not consistent with seaice_growth value) |
272 |
|
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c TB(I,J) = 271.2 _d 0 |
273 |
mlosch |
1.5 |
TB(I,J) = celsius2K + SEAICE_freeze |
274 |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
275 |
mlosch |
1.18 |
IF(HSNOW_ACTUAL(I,J).GT.0.0) THEN |
276 |
jmc |
1.21 |
C Stefan-Boltzmann constant times emissivity |
277 |
mlosch |
1.18 |
D3(I,J)=SEAICE_snow_emiss*SEAICE_boltzmann |
278 |
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#ifdef EXF_LWDOWN_WITH_EMISSIVITY |
279 |
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C This is now [(1-emiss)*lwdown - lwdown] |
280 |
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lwdownloc(I,J) = SEAICE_snow_emiss*lwdownloc(I,J) |
281 |
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#else /* use the old hard wired inconsistent value */ |
282 |
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lwdownloc(I,J) = 0.97 _d 0*lwdownloc(I,J) |
283 |
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#endif /* EXF_LWDOWN_WITH_EMISSIVITY */ |
284 |
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ELSE |
285 |
jmc |
1.21 |
C Stefan-Boltzmann constant times emissivity |
286 |
mlosch |
1.18 |
D3(I,J)=SEAICE_ice_emiss*SEAICE_boltzmann |
287 |
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#ifdef EXF_LWDOWN_WITH_EMISSIVITY |
288 |
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C This is now [(1-emiss)*lwdown - lwdown] |
289 |
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|
lwdownloc(I,J) = SEAICE_ice_emiss*lwdownloc(I,J) |
290 |
|
|
#else /* use the old hard wired inconsistent value */ |
291 |
|
|
lwdownloc(I,J) = 0.97 _d 0*lwdownloc(I,J) |
292 |
|
|
#endif /* EXF_LWDOWN_WITH_EMISSIVITY */ |
293 |
|
|
ENDIF |
294 |
mlosch |
1.5 |
ENDDO |
295 |
jmc |
1.1 |
ENDDO |
296 |
|
|
|
297 |
|
|
DO J=1,sNy |
298 |
mlosch |
1.5 |
DO I=1,sNx |
299 |
jmc |
1.1 |
|
300 |
|
|
C DECIDE ON ALBEDO |
301 |
mlosch |
1.5 |
IF ( iceOrNot(I,J) ) THEN |
302 |
jmc |
1.6 |
|
303 |
mlosch |
1.5 |
IF ( YC(I,J,bi,bj) .LT. 0.0 _d 0 ) THEN |
304 |
|
|
IF (tsurfLoc(I,J) .GE. SurfMeltTemp) THEN |
305 |
|
|
ALB_ICE (I,J) = SEAICE_wetIceAlb_south |
306 |
|
|
ALB_SNOW(I,J) = SEAICE_wetSnowAlb_south |
307 |
|
|
ELSE ! no surface melting |
308 |
|
|
ALB_ICE (I,J) = SEAICE_dryIceAlb_south |
309 |
|
|
ALB_SNOW(I,J) = SEAICE_drySnowAlb_south |
310 |
|
|
ENDIF |
311 |
|
|
ELSE !/ Northern Hemisphere |
312 |
|
|
IF (tsurfLoc(I,J) .GE. SurfMeltTemp) THEN |
313 |
|
|
ALB_ICE (I,J) = SEAICE_wetIceAlb |
314 |
|
|
ALB_SNOW(I,J) = SEAICE_wetSnowAlb |
315 |
|
|
ELSE ! no surface melting |
316 |
|
|
ALB_ICE (I,J) = SEAICE_dryIceAlb |
317 |
|
|
ALB_SNOW(I,J) = SEAICE_drySnowAlb |
318 |
|
|
ENDIF |
319 |
|
|
ENDIF !/ Albedo for snow and ice |
320 |
|
|
|
321 |
jmc |
1.21 |
C If actual snow thickness exceeds the cutoff thickness, use snow albedo |
322 |
mlosch |
1.5 |
IF (HSNOW_ACTUAL(I,J) .GT. HCUT) THEN |
323 |
|
|
ALB(I,J) = ALB_SNOW(I,J) |
324 |
jmc |
1.21 |
ELSEIF ( HCUT.LE.ZERO ) THEN |
325 |
|
|
ALB(I,J) = ALB_ICE(I,J) |
326 |
mlosch |
1.5 |
ELSE |
327 |
jmc |
1.21 |
C otherwise, use linear transition between ice and snow albedo |
328 |
|
|
ALB(I,J) = MIN( ALB_ICE(I,J) + HSNOW_ACTUAL(I,J)/HCUT |
329 |
|
|
& *(ALB_SNOW(I,J) -ALB_ICE(I,J)) |
330 |
|
|
& , ALB_SNOW(I,J) ) |
331 |
mlosch |
1.5 |
ENDIF |
332 |
|
|
|
333 |
jmc |
1.21 |
C Determine the fraction of shortwave radiative flux remaining |
334 |
|
|
C at ocean interface after scattering through the snow and ice. |
335 |
|
|
C If snow is present, no radiation penetrates through snow+ice |
336 |
mlosch |
1.5 |
IF (HSNOW_ACTUAL(I,J) .GT. 0.0 _d 0) THEN |
337 |
jmc |
1.21 |
penetSWFrac = 0.0 _d 0 |
338 |
mlosch |
1.5 |
ELSE |
339 |
jmc |
1.21 |
penetSWFrac = XIO*EXP(-1.5 _d 0 * HICE_ACTUAL(I,J)) |
340 |
mlosch |
1.5 |
ENDIF |
341 |
jmc |
1.21 |
C The shortwave radiative flux leaving ocean beneath ice (+=up). |
342 |
|
|
IcePenetSW(I,J) = -(1.0 _d 0 - ALB(I,J)) |
343 |
|
|
& *penetSWFrac * SWDOWN(I,J,bi,bj) |
344 |
|
|
C The shortwave radiative flux convergence in the seaice. |
345 |
|
|
absorbedSW(I,J) = (1.0 _d 0 - ALB(I,J)) |
346 |
|
|
& *(1.0 _d 0 - penetSWFrac)* SWDOWN(I,J,bi,bj) |
347 |
jmc |
1.1 |
|
348 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
349 |
jmc |
1.21 |
C Now determine fixed (relative to tsurf) forcing term in heat budget |
350 |
|
|
A1(I,J) = absorbedSW(I,J) + lwdownLoc(I,J) |
351 |
mlosch |
1.5 |
& +D1*UG(I,J)*atempLoc(I,J)+D1I*UG(I,J)*AQH(I,J,bi,bj) |
352 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
353 |
jmc |
1.1 |
|
354 |
jmc |
1.24 |
C The effective conductivity of the two-layer snow/ice system. |
355 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
356 |
mlosch |
1.5 |
effConduct(I,J)= |
357 |
|
|
& XKS/(HSNOW_ACTUAL(I,J)/HICE_ACTUAL(I,J) + |
358 |
|
|
& XKS/XKI)/HICE_ACTUAL(I,J) |
359 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
360 |
jmc |
1.21 |
C Set a mininum sea ice thickness of 5 cm to bound |
361 |
|
|
C the magnitude of conductive heat fluxes. |
362 |
|
|
Cif * now taken care of by SEAICE_hice_reg in seaice_growth |
363 |
|
|
c hice_tmp = max(HICE_ACTUAL(I,J),5. _d -2) |
364 |
mlosch |
1.5 |
effConduct(I,J) = XKI * XKS / |
365 |
jmc |
1.21 |
& (XKS * HICE_ACTUAL(I,J) + XKI * HSNOW_ACTUAL(I,J)) |
366 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
367 |
jmc |
1.1 |
|
368 |
|
|
#ifdef SEAICE_DEBUG |
369 |
jmc |
1.21 |
IF ( (I .EQ. SEAICE_debugPointI) .AND. |
370 |
ifenty |
1.16 |
& (J .EQ. SEAICE_debugPointJ) ) THEN |
371 |
mlosch |
1.5 |
print '(A,i6)','-----------------------------------' |
372 |
|
|
print '(A,i6)','ibi merged initialization ', myIter |
373 |
|
|
print '(A,i6,4(1x,D24.15))', |
374 |
|
|
& 'ibi iter, TSL, TS ',myIter, |
375 |
|
|
& tsurfLoc(I,J), TSURF(I,J,bi,bj) |
376 |
|
|
print '(A,i6,4(1x,D24.15))', |
377 |
|
|
& 'ibi iter, TMELT ',myIter,TMELT |
378 |
|
|
print '(A,i6,4(1x,D24.15))', |
379 |
|
|
& 'ibi iter, HIA, EFKCON ',myIter, |
380 |
|
|
& HICE_ACTUAL(I,J), effConduct(I,J) |
381 |
|
|
print '(A,i6,4(1x,D24.15))', |
382 |
|
|
& 'ibi iter, HSNOW ',myIter, |
383 |
|
|
& HSNOW_ACTUAL(I,J), ALB(I,J) |
384 |
|
|
print '(A,i6)','-----------------------------------' |
385 |
|
|
print '(A,i6)','ibi energy balance iterat ', myIter |
386 |
|
|
ENDIF |
387 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
388 |
jmc |
1.6 |
|
389 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
390 |
|
|
ENDDO !/* i */ |
391 |
|
|
ENDDO !/* j */ |
392 |
jmc |
1.21 |
|
393 |
|
|
C---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
394 |
mlosch |
1.5 |
DO ITER=1,IMAX_TICE |
395 |
|
|
DO J=1,sNy |
396 |
|
|
DO I=1,sNx |
397 |
mlosch |
1.8 |
#ifdef ALLOW_AUTODIFF_TAMC |
398 |
|
|
iicekey = I + sNx*(J-1) + (ITER-1)*sNx*sNy |
399 |
|
|
CADJ STORE tsurfloc(i,j) = comlev1_solve4temp, |
400 |
|
|
CADJ & key = iicekey, byte = isbyte |
401 |
|
|
#endif /* ALLOW_AUTODIFF_TAMC */ |
402 |
|
|
|
403 |
mlosch |
1.5 |
IF ( iceOrNot(I,J) ) THEN |
404 |
jmc |
1.1 |
|
405 |
mlosch |
1.5 |
t1 = tsurfLoc(I,J) |
406 |
|
|
t2 = t1*t1 |
407 |
|
|
t3 = t2*t1 |
408 |
|
|
t4 = t2*t2 |
409 |
jmc |
1.1 |
|
410 |
jmc |
1.24 |
C-- Calculate the specific humidity in the BL above the snow/ice |
411 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
412 |
jmc |
1.24 |
C- Use the Maykut polynomial |
413 |
mlosch |
1.5 |
qhice(I,J)=QS1*(C1*t4+C2*t3 +C3*t2+C4*t1+C5) |
414 |
jmc |
1.24 |
dqh_dTs(I,J) = 0. _d 0 |
415 |
jmc |
1.1 |
|
416 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
417 |
jmc |
1.24 |
C- Use exponential relation approx., more accurate at low temperatures |
418 |
mlosch |
1.5 |
C log 10 of the sat vap pressure |
419 |
|
|
mm_log10pi = -aa1 / t1 + aa2 |
420 |
|
|
C The saturation vapor pressure (SVP) in the surface |
421 |
|
|
C boundary layer (BL) above the snow/ice. |
422 |
jmc |
1.24 |
c mm_pi = TEN **(mm_log10pi) |
423 |
jmc |
1.6 |
C The following form does the same, but is faster |
424 |
jmc |
1.21 |
mm_pi = EXP(mm_log10pi*lnTEN) |
425 |
jmc |
1.24 |
qhice(I,J) = bb1*mm_pi/( Ppascals -(1.0 _d 0 - bb1)*mm_pi ) |
426 |
jmc |
1.21 |
C A constant for SVP derivative w.r.t TICE |
427 |
jmc |
1.24 |
c cc3t = TEN **(aa1 / t1) |
428 |
jmc |
1.21 |
C The following form does the same, but is faster |
429 |
|
|
cc3t = EXP(aa1 / t1 * lnTEN) |
430 |
|
|
C d(qh)/d(TICE) |
431 |
jmc |
1.24 |
dqh_dTs(I,J) = cc1*cc3t/((cc2-cc3t*Ppascals)**2 *t2) |
432 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
433 |
jmc |
1.1 |
|
434 |
mlosch |
1.10 |
C Calculate the flux terms based on the updated tsurfLoc |
435 |
jmc |
1.22 |
F_c(I,J) = effConduct(I,J)*(TB(I,J)-tsurfLoc(I,J)) |
436 |
mlosch |
1.10 |
F_lh(I,J) = D1I*UG(I,J)*(qhice(I,J)-AQH(I,J,bi,bj)) |
437 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
438 |
jmc |
1.21 |
A2(I,J) = D1*UG(I,J)*t1+D1I*UG(I,J)*qhice(I,J)+D3(I,J)*t4 |
439 |
mlosch |
1.18 |
A3(I,J) = 4.0 _d 0*D3(I,J)*t3 + effConduct(I,J)+D1*UG(I,J) |
440 |
jmc |
1.24 |
& + D1I*UG(I,J)*dqh_dTs(I,J) |
441 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
442 |
ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
443 |
jmc |
1.21 |
C if the latent heat flux implied by tsurfLoc exceeds |
444 |
|
|
C F_lh_max, cap F_lh and decouple the flux magnitude from TICE |
445 |
|
|
IF (F_lh(I,J) .GT. F_lh_max(I,J)) THEN |
446 |
ifenty |
1.16 |
F_lh(I,J) = F_lh_max(I,J) |
447 |
jmc |
1.24 |
dqh_dTs(I,J) = ZERO |
448 |
jmc |
1.21 |
ENDIF |
449 |
|
|
#endif /* SEAICE_ADD_SUBLIMATION_TO_FWBUDGET */ |
450 |
ifenty |
1.16 |
|
451 |
jmc |
1.24 |
C d(F_ia)/d(Tsurf) |
452 |
|
|
dFia_dTs(I,J) = 4.0 _d 0*D3(I,J)*t3 + D1*UG(I,J) |
453 |
|
|
& + D1I*UG(I,J)*dqh_dTs(I,J) |
454 |
mlosch |
1.5 |
|
455 |
jmc |
1.21 |
F_lwu(I,J) = t4 * D3(I,J) |
456 |
mlosch |
1.5 |
F_sens(I,J)= D1 * UG(I,J) * (t1 - atempLoc(I,J)) |
457 |
jmc |
1.21 |
F_ia(I,J) = -lwdownLoc(I,J) -absorbedSW(I,J) + F_lwu(I,J) |
458 |
jmc |
1.24 |
& + F_sens(I,J) + F_lh(I,J) |
459 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
460 |
jmc |
1.1 |
|
461 |
|
|
#ifdef SEAICE_DEBUG |
462 |
jmc |
1.21 |
IF ( (I .EQ. SEAICE_debugPointI) .AND. |
463 |
ifenty |
1.16 |
& (J .EQ. SEAICE_debugPointJ) ) THEN |
464 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
465 |
|
|
& 'ice-iter qhICE, ', ITER,qhIce(I,J) |
466 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
467 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
468 |
jmc |
1.22 |
& 'ice-iter A1 A2 B ',ITER,A1(I,J),A2(I,J),F_c(I,J) |
469 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
470 |
jmc |
1.21 |
& 'ice-iter A3 (-A1+A2) ',ITER,A3(I,J),-A1(I,J)+A2(I,J) |
471 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
472 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
473 |
jmc |
1.24 |
& 'ice-iter dFiDTs1 F_ia ', ITER, |
474 |
|
|
& dFia_dTs(I,J)+effConduct(I,J), F_ia(I,J)-F_c(I,J) |
475 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
476 |
mlosch |
1.5 |
ENDIF |
477 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
478 |
jmc |
1.1 |
|
479 |
mlosch |
1.5 |
C Update tsurfLoc |
480 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
481 |
jmc |
1.22 |
C update tsurf as solution of : Fc = A2 - A1 + A3 *delta.tsurf |
482 |
mlosch |
1.5 |
tsurfLoc(I,J)=tsurfLoc(I,J) |
483 |
jmc |
1.22 |
& +(A1(I,J)-A2(I,J)+F_c(I,J))/A3(I,J) |
484 |
jmc |
1.23 |
tsurfLoc(I,J) = MAX( celsius2K+MIN_TICE, tsurfLoc(I,J) ) |
485 |
jmc |
1.6 |
|
486 |
|
|
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
487 |
jmc |
1.24 |
C update tsurf as solution of : Fc = Fia + d/dT(Fia - Fc) *delta.tsurf |
488 |
|
|
tsurfLoc(I,J) = tsurfLoc(I,J) |
489 |
|
|
& + ( F_c(I,J)-F_ia(I,J) ) / ( effConduct(I,J)+dFia_dTs(I,J) ) |
490 |
jmc |
1.1 |
|
491 |
jmc |
1.21 |
C If the search leads to tsurfLoc < 50 Kelvin, restart the search |
492 |
|
|
C at tsurfLoc = TMELT. Note that one solution to the energy balance problem |
493 |
|
|
C is an extremely low temperature - a temperature far below realistic values. |
494 |
mlosch |
1.5 |
IF (tsurfLoc(I,J) .LT. 50.0 _d 0 ) THEN |
495 |
|
|
tsurfLoc(I,J) = TMELT |
496 |
|
|
ENDIF |
497 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
498 |
jmc |
1.21 |
tsurfLoc(I,J) = MIN( tsurfLoc(I,J), TMELT ) |
499 |
jmc |
1.1 |
|
500 |
|
|
#ifdef SEAICE_DEBUG |
501 |
jmc |
1.21 |
IF ( (I .EQ. SEAICE_debugPointI) .AND. |
502 |
ifenty |
1.16 |
& (J .EQ. SEAICE_debugPointJ) ) THEN |
503 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
504 |
|
|
& 'ice-iter tsurfLc,|dif|', ITER, |
505 |
|
|
& tsurfLoc(I,J), |
506 |
jmc |
1.21 |
& LOG10(ABS(tsurfLoc(I,J) - t1)) |
507 |
mlosch |
1.5 |
ENDIF |
508 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
509 |
jmc |
1.1 |
|
510 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
511 |
|
|
ENDDO !/* i */ |
512 |
|
|
ENDDO !/* j */ |
513 |
|
|
ENDDO !/* Iterations */ |
514 |
jmc |
1.21 |
C---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
515 |
|
|
|
516 |
mlosch |
1.5 |
DO J=1,sNy |
517 |
|
|
DO I=1,sNx |
518 |
|
|
IF ( iceOrNot(I,J) ) THEN |
519 |
jmc |
1.1 |
|
520 |
jmc |
1.21 |
C Save updated tsurf and finalize the flux terms |
521 |
|
|
TSURF(I,J,bi,bj) = tsurfLoc(I,J) |
522 |
|
|
|
523 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
524 |
jmc |
1.21 |
F_ia(I,J)=-A1(I,J)+A2(I,J) |
525 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
526 |
mlosch |
1.5 |
C Recalculate the fluxes based on the (possibly) adjusted TSURF |
527 |
|
|
t1 = tsurfLoc(I,J) |
528 |
|
|
t2 = t1*t1 |
529 |
|
|
t3 = t2*t1 |
530 |
|
|
t4 = t2*t2 |
531 |
jmc |
1.1 |
|
532 |
mlosch |
1.5 |
C log 10 of the sat vap pressure |
533 |
|
|
mm_log10pi = -aa1 / t1 + aa2 |
534 |
|
|
C saturation vapor pressure |
535 |
jmc |
1.24 |
c mm_pi = TEN **(mm_log10pi) |
536 |
jmc |
1.6 |
C The following form does the same, but is faster |
537 |
jmc |
1.21 |
mm_pi = EXP(mm_log10pi*lnTEN) |
538 |
|
|
C over ice specific humidity |
539 |
jmc |
1.24 |
qhice(I,J) = bb1*mm_pi/( Ppascals -(1.0 _d 0 - bb1)*mm_pi ) |
540 |
mlosch |
1.5 |
F_lh(I,J) = D1I * UG(I,J)*(qhice(I,J)-AQH(I,J,bi,bj)) |
541 |
ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
542 |
jmc |
1.21 |
IF (F_lh(I,J) .GT. F_lh_max(I,J)) THEN |
543 |
ifenty |
1.16 |
F_lh(I,J) = F_lh_max(I,J) |
544 |
jmc |
1.21 |
ENDIF |
545 |
|
|
#endif /* SEAICE_ADD_SUBLIMATION_TO_FWBUDGET */ |
546 |
ifenty |
1.16 |
|
547 |
jmc |
1.22 |
F_c(I,J) = effConduct(I,J) * (TB(I,J) - t1) |
548 |
mlosch |
1.18 |
F_lwu(I,J) = t4 * D3(I,J) |
549 |
mlosch |
1.5 |
F_sens(I,J) = D1 * UG(I,J) * (t1 - atempLoc(I,J)) |
550 |
jmc |
1.1 |
|
551 |
jmc |
1.21 |
C The flux between the ice/snow surface and the atmosphere. |
552 |
|
|
F_ia(I,J) = -lwdownLoc(I,J) -absorbedSW(I,J) + F_lwu(I,J) |
553 |
|
|
& + F_sens(I,J) + F_lh(I,J) |
554 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
555 |
jmc |
1.1 |
|
556 |
gforget |
1.9 |
#ifdef SEAICE_MODIFY_GROWTH_ADJ |
557 |
|
|
Cgf no additional dependency through solver, snow, etc. |
558 |
jmc |
1.21 |
IF ( SEAICEadjMODE.GE.2 ) THEN |
559 |
gforget |
1.9 |
CALL ZERO_ADJ_1D( 1, TSURF(I,J,bi,bj), myThid) |
560 |
|
|
t1 = TSURF(I,J,bi,bj) |
561 |
|
|
t2 = t1*t1 |
562 |
|
|
t3 = t2*t1 |
563 |
|
|
t4 = t2*t2 |
564 |
|
|
qhice(I,J)=QS1*(C1*t4+C2*t3 +C3*t2+C4*t1+C5) |
565 |
|
|
|
566 |
mlosch |
1.18 |
A1(I,J)=0.3 _d 0 *SWDOWN(I,J,bi,bj)+lwdownLoc(I,J) |
567 |
gforget |
1.9 |
& +D1*UG(I,J)*atempLoc(I,J)+D1I*UG(I,J)*AQH(I,J,bi,bj) |
568 |
jmc |
1.21 |
A2(I,J)= D1*UG(I,J)*t1+D1I*UG(I,J)*qhice(I,J)+D3(I,J)*t4 |
569 |
gforget |
1.9 |
|
570 |
jmc |
1.21 |
F_ia(I,J)=-A1(I,J)+A2(I,J) |
571 |
|
|
IcePenetSW(I,J)= 0. _d 0 |
572 |
|
|
ENDIF |
573 |
|
|
#endif /* SEAICE_MODIFY_GROWTH_ADJ */ |
574 |
|
|
|
575 |
|
|
C Fresh water flux (kg/m^2/s) from latent heat of sublimation. |
576 |
|
|
C F_lh is positive upward (sea ice looses heat) and FWsublim |
577 |
|
|
C is also positive upward (atmosphere gains freshwater) |
578 |
|
|
FWsublim(I,J) = F_lh(I,J)/lhSublim |
579 |
gforget |
1.9 |
|
580 |
jmc |
1.21 |
#ifdef SEAICE_DEBUG |
581 |
mlosch |
1.5 |
C Caclulate the net ice-ocean and ice-atmosphere fluxes |
582 |
jmc |
1.22 |
IF (F_c(I,J) .GT. 0.0 _d 0) THEN |
583 |
|
|
F_io_net(I,J) = F_c(I,J) |
584 |
mlosch |
1.5 |
F_ia_net(I,J) = 0.0 _d 0 |
585 |
|
|
ELSE |
586 |
|
|
F_io_net(I,J) = 0.0 _d 0 |
587 |
|
|
F_ia_net(I,J) = F_ia(I,J) |
588 |
|
|
ENDIF !/* conductive fluxes up or down */ |
589 |
jmc |
1.1 |
|
590 |
jmc |
1.21 |
IF ( (I .EQ. SEAICE_debugPointI) .AND. |
591 |
ifenty |
1.16 |
& (J .EQ. SEAICE_debugPointJ) ) THEN |
592 |
mlosch |
1.5 |
print '(A)','----------------------------------------' |
593 |
|
|
print '(A,i6)','ibi complete ', myIter |
594 |
|
|
print '(A,4(1x,D24.15))', |
595 |
|
|
& 'ibi T(SURF, surfLoc,atmos) ', |
596 |
|
|
& TSURF(I,J,bi,bj), tsurfLoc(I,J),atempLoc(I,J) |
597 |
|
|
print '(A,4(1x,D24.15))', |
598 |
|
|
& 'ibi LWL ', lwdownLoc(I,J) |
599 |
|
|
print '(A,4(1x,D24.15))', |
600 |
|
|
& 'ibi QSW(Total, Penetrating)', |
601 |
jmc |
1.21 |
& SWDOWN(I,J,bi,bj), IcePenetSW(I,J) |
602 |
mlosch |
1.5 |
print '(A,4(1x,D24.15))', |
603 |
|
|
& 'ibi qh(ATM ICE) ', |
604 |
|
|
& AQH(I,J,bi,bj),qhice(I,J) |
605 |
ifenty |
1.16 |
#ifndef SEAICE_SOLVE4TEMP_LEGACY |
606 |
|
|
print '(A,4(1x,D24.15))', |
607 |
|
|
& 'ibi F(lwd,swi,lwu) ', |
608 |
jmc |
1.21 |
& -lwdownLoc(I,J), -absorbedSW(I,J), F_lwu(I,J) |
609 |
ifenty |
1.16 |
print '(A,4(1x,D24.15))', |
610 |
|
|
& 'ibi F(c,lh,sens) ', |
611 |
|
|
& F_c(I,J), F_lh(I,J), F_sens(I,J) |
612 |
|
|
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
613 |
|
|
IF (F_lh_max(I,J) .GT. ZERO) THEN |
614 |
|
|
print '(A,4(1x,D24.15))', |
615 |
|
|
& 'ibi F_lh_max, F_lh/lhmax) ', |
616 |
|
|
& F_lh_max(I,J), F_lh(I,J)/ F_lh_max(I,J) |
617 |
jmc |
1.19 |
ELSE |
618 |
ifenty |
1.16 |
print '(A,4(1x,D24.15))', |
619 |
|
|
& 'ibi F_lh_max = ZERO! ' |
620 |
|
|
ENDIF |
621 |
|
|
print '(A,4(1x,D24.15))', |
622 |
|
|
& 'ibi FWsub, FWsubm*dT/rhoI ', |
623 |
|
|
& FWsublim(I,J), |
624 |
|
|
& FWsublim(I,J)*SEAICE_deltaTtherm/SEAICE_rhoICE |
625 |
jmc |
1.21 |
#endif /* SEAICE_ADD_SUBLIMATION_TO_FWBUDGET */ |
626 |
|
|
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
627 |
mlosch |
1.5 |
print '(A,4(1x,D24.15))', |
628 |
|
|
& 'ibi F_ia, F_ia_net, F_c ', |
629 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
630 |
jmc |
1.22 |
& -A1(I,J)+A2(I,J), -A1(I,J)+A2(I,J)-F_c(I,J), F_c(I,J) |
631 |
jmc |
1.21 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
632 |
|
|
& F_ia(I,J), F_ia_net(I,J), F_c(I,J) |
633 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
634 |
mlosch |
1.5 |
print '(A)','----------------------------------------' |
635 |
|
|
ENDIF |
636 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
637 |
jmc |
1.6 |
|
638 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
639 |
|
|
ENDDO !/* i */ |
640 |
jmc |
1.1 |
ENDDO !/* j */ |
641 |
|
|
|
642 |
jmc |
1.19 |
#endif /* ALLOW_ATM_TEMP && ALLOW_DOWNWARD_RADIATION */ |
643 |
|
|
RETURN |
644 |
jmc |
1.1 |
END |