1 |
jmc |
1.20 |
C $Header: /u/gcmpack/MITgcm/pkg/seaice/seaice_solve4temp.F,v 1.19 2011/12/24 18:37:18 jmc Exp $ |
2 |
jmc |
1.1 |
C $Name: $ |
3 |
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#include "SEAICE_OPTIONS.h" |
5 |
jmc |
1.19 |
#ifdef ALLOW_EXF |
6 |
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# include "EXF_OPTIONS.h" |
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#endif |
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jmc |
1.1 |
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9 |
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CBOP |
10 |
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C !ROUTINE: SEAICE_SOLVE4TEMP |
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C !INTERFACE: |
12 |
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SUBROUTINE SEAICE_SOLVE4TEMP( |
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I UG, HICE_ACTUAL, HSNOW_ACTUAL, |
14 |
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 |
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O F_ia, IcePenetSWFlux, |
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 *==========================================================* |
24 |
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C | SUBROUTINE SOLVE4TEMP |
25 |
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C | o Calculate ice growth rate, surface fluxes and |
26 |
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C | temperature of ice surface. |
27 |
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C | see Hibler, MWR, 108, 1943-1973, 1980 |
28 |
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C *==========================================================* |
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C \ev |
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C !USES: |
32 |
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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" |
36 |
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#include "EEPARAMS.h" |
37 |
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" |
42 |
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#ifdef SEAICE_VARIABLE_FREEZING_POINT |
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#include "DYNVARS.h" |
44 |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
45 |
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#ifdef ALLOW_EXF |
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# include "EXF_FIELDS.h" |
47 |
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#endif |
48 |
mlosch |
1.8 |
#ifdef ALLOW_AUTODIFF_TAMC |
49 |
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# include "tamc.h" |
50 |
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#endif |
51 |
jmc |
1.1 |
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52 |
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C !INPUT/OUTPUT PARAMETERS |
53 |
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C === Routine arguments === |
54 |
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C INPUT: |
55 |
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C UG :: thermal wind of atmosphere |
56 |
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C HICE_ACTUAL :: actual ice thickness |
57 |
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C HSNOW_ACTUAL :: actual snow thickness |
58 |
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C TSURF :: surface temperature of ice in Kelvin, updated |
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C bi,bj :: loop indices |
60 |
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C OUTPUT: |
61 |
jmc |
1.12 |
C F_io_net :: net upward conductive heat flux through ice at the base |
62 |
mlosch |
1.10 |
C of the ice |
63 |
jmc |
1.1 |
C F_ia_net :: net heat flux divergence at the sea ice/snow surface: |
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C includes ice conductive fluxes and atmospheric fluxes (W/m^2) |
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C F_ia :: upward sea ice/snow surface heat flux to atmosphere (W/m^2) |
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C IcePenetSWFlux :: short wave heat flux under ice |
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jmc |
1.12 |
C FWsublim :: fresh water (mass) flux implied by latent heat of |
68 |
mlosch |
1.10 |
C sublimation (kg/m^2/s) |
69 |
jmc |
1.1 |
_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) |
72 |
ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
73 |
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_RL F_lh_max (1:sNx,1:sNy) |
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#endif |
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jmc |
1.1 |
_RL TSURF (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
76 |
jmc |
1.12 |
c _RL F_io_net (1:sNx,1:sNy) |
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c _RL F_ia_net (1:sNx,1:sNy) |
78 |
jmc |
1.1 |
_RL F_ia (1:sNx,1:sNy) |
79 |
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_RL IcePenetSWFlux (1:sNx,1:sNy) |
80 |
mlosch |
1.10 |
_RL FWsublim (1:sNx,1:sNy) |
81 |
jmc |
1.1 |
INTEGER bi, bj |
82 |
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_RL myTime |
83 |
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INTEGER myIter, myThid |
84 |
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 === |
89 |
jmc |
1.12 |
_RL F_io_net (1:sNx,1:sNy) |
90 |
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_RL F_ia_net (1:sNx,1:sNy) |
91 |
jmc |
1.6 |
#ifndef SEAICE_SOLVE4TEMP_LEGACY |
92 |
jmc |
1.1 |
_RL F_swi (1:sNx,1:sNy) |
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_RL F_lwd (1:sNx,1:sNy) |
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_RL F_lwu (1:sNx,1:sNy) |
95 |
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_RL F_sens (1:sNx,1:sNy) |
96 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
97 |
mlosch |
1.10 |
_RL F_lh (1:sNx,1:sNy) |
98 |
jmc |
1.1 |
_RL F_c (1:sNx,1:sNy) |
99 |
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_RL qhice (1:sNx,1:sNy) |
100 |
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101 |
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_RL AbsorbedSWFlux (1:sNx,1:sNy) |
102 |
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_RL IcePenetSWFluxFrac (1:sNx,1:sNy) |
103 |
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104 |
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C local copies of global variables |
105 |
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_RL tsurfLoc (1:sNx,1:sNy) |
106 |
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_RL atempLoc (1:sNx,1:sNy) |
107 |
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_RL lwdownLoc (1:sNx,1:sNy) |
108 |
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_RL ALB (1:sNx,1:sNy) |
109 |
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_RL ALB_ICE (1:sNx,1:sNy) |
110 |
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_RL ALB_SNOW (1:sNx,1:sNy) |
111 |
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112 |
jmc |
1.3 |
C i, j :: Loop counters |
113 |
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C kSrf :: vertical index of surface layer |
114 |
jmc |
1.1 |
INTEGER i, j |
115 |
jmc |
1.3 |
#ifdef SEAICE_VARIABLE_FREEZING_POINT |
116 |
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INTEGER kSrf |
117 |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
118 |
jmc |
1.1 |
INTEGER ITER |
119 |
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120 |
mlosch |
1.5 |
C This is HICE_ACTUAL.GT.0. |
121 |
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LOGICAL iceOrNot(1:sNx,1:sNy) |
122 |
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123 |
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C TB :: temperature in boundary layer (=freezing point temperature) (K) |
124 |
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_RL TB (1:sNx,1:sNy) |
125 |
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C |
126 |
mlosch |
1.18 |
_RL D1, D1I |
127 |
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_RL D3(1:sNx,1:sNy) |
128 |
mlosch |
1.5 |
_RL TMELT, XKI, XKS, HCUT, XIO |
129 |
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_RL SurfMeltTemp |
130 |
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C effective conductivity of combined ice and snow |
131 |
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_RL effConduct(1:sNx,1:sNy) |
132 |
jmc |
1.1 |
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133 |
jmc |
1.3 |
C Constants to calculate Saturation Vapor Pressure |
134 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
135 |
mlosch |
1.5 |
_RL TMELTP, C1, C2, C3, C4, C5, QS1 |
136 |
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_RL A2 (1:sNx,1:sNy) |
137 |
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_RL A3 (1:sNx,1:sNy) |
138 |
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c _RL B (1:sNx,1:sNy) |
139 |
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_RL A1 (1:sNx,1:sNy) |
140 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
141 |
jmc |
1.3 |
_RL dFiDTs1 |
142 |
jmc |
1.1 |
_RL aa1,aa2,bb1,bb2,Ppascals,cc0,cc1,cc2,cc3t |
143 |
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C specific humidity at ice surface variables |
144 |
mlosch |
1.5 |
_RL mm_pi,mm_log10pi,dqhice_dTice |
145 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
146 |
jmc |
1.1 |
|
147 |
ifenty |
1.14 |
C latent heat of sublimation for ice (SEAICE_lhEvap + |
148 |
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C SEAICE_lhFusion) |
149 |
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_RL lhSublim |
150 |
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151 |
jmc |
1.1 |
C powers of temperature |
152 |
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_RL t1, t2, t3, t4 |
153 |
mlosch |
1.5 |
_RL lnTEN |
154 |
jmc |
1.1 |
|
155 |
mlosch |
1.8 |
#ifdef ALLOW_AUTODIFF_TAMC |
156 |
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CADJ INIT comlev1_solve4temp = COMMON, sNx*sNy*NMAX_TICE |
157 |
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#endif /* ALLOW_AUTODIFF_TAMC */ |
158 |
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159 |
mlosch |
1.5 |
lnTEN = log(10.0 _d 0) |
160 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
161 |
jmc |
1.1 |
C MAYKUTS CONSTANTS FOR SAT. VAP. PRESSURE TEMP. POLYNOMIAL |
162 |
mlosch |
1.5 |
C1= 2.7798202 _d -06 |
163 |
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C2= -2.6913393 _d -03 |
164 |
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C3= 0.97920849 _d +00 |
165 |
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C4= -158.63779 _d +00 |
166 |
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C5= 9653.1925 _d +00 |
167 |
jmc |
1.1 |
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168 |
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QS1=0.622 _d +00/1013.0 _d +00 |
169 |
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170 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
171 |
jmc |
1.1 |
aa1 = 2663.5 _d 0 |
172 |
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aa2 = 12.537 _d 0 |
173 |
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bb1 = 0.622 _d 0 |
174 |
mlosch |
1.5 |
bb2 = 1.0 _d 0 - bb1 |
175 |
jmc |
1.1 |
Ppascals = 100000. _d 0 |
176 |
mlosch |
1.5 |
C cc0 = TEN ** aa2 |
177 |
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cc0 = exp(aa2*lnTEN) |
178 |
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cc1 = cc0*aa1*bb1*Ppascals*lnTEN |
179 |
jmc |
1.1 |
cc2 = cc0*bb2 |
180 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
181 |
jmc |
1.1 |
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182 |
jmc |
1.4 |
#ifdef SEAICE_VARIABLE_FREEZING_POINT |
183 |
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kSrf = 1 |
184 |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
185 |
jmc |
1.1 |
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186 |
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C SENSIBLE HEAT CONSTANT |
187 |
mlosch |
1.7 |
D1=SEAICE_dalton*SEAICE_cpAir*SEAICE_rhoAir |
188 |
jmc |
1.1 |
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189 |
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C ICE LATENT HEAT CONSTANT |
190 |
ifenty |
1.14 |
lhSublim = SEAICE_lhEvap + SEAICE_lhFusion |
191 |
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D1I=SEAICE_dalton*lhSublim*SEAICE_rhoAir |
192 |
jmc |
1.1 |
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193 |
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C MELTING TEMPERATURE OF ICE |
194 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
195 |
mlosch |
1.5 |
TMELT = 273.16 _d +00 |
196 |
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TMELTP = 273.159 _d +00 |
197 |
jmc |
1.1 |
SurfMeltTemp = TMELTP |
198 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
199 |
mlosch |
1.5 |
TMELT = celsius2K |
200 |
jmc |
1.1 |
SurfMeltTemp = TMELT |
201 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
202 |
jmc |
1.1 |
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203 |
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C ICE CONDUCTIVITY |
204 |
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XKI=SEAICE_iceConduct |
205 |
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206 |
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C SNOW CONDUCTIVITY |
207 |
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XKS=SEAICE_snowConduct |
208 |
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209 |
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C CUTOFF SNOW THICKNESS |
210 |
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HCUT=SEAICE_snowThick |
211 |
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212 |
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C PENETRATION SHORTWAVE RADIATION FACTOR |
213 |
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XIO=SEAICE_shortwave |
214 |
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215 |
jmc |
1.3 |
C Initialize variables |
216 |
jmc |
1.1 |
DO J=1,sNy |
217 |
mlosch |
1.5 |
DO I=1,sNx |
218 |
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C HICE_ACTUAL is modified in this routine, but at the same time |
219 |
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C used to decided where there is ice, therefore we save this information |
220 |
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C here in a separate array |
221 |
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iceOrNot (I,J) = HICE_ACTUAL(I,J) .GT. 0. _d 0 |
222 |
jmc |
1.6 |
C |
223 |
mlosch |
1.5 |
IcePenetSWFlux (I,J) = 0. _d 0 |
224 |
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IcePenetSWFluxFrac (I,J) = 0. _d 0 |
225 |
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AbsorbedSWFlux (I,J) = 0. _d 0 |
226 |
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227 |
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qhice (I,J) = 0. _d 0 |
228 |
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F_ia (I,J) = 0. _d 0 |
229 |
jmc |
1.6 |
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230 |
mlosch |
1.5 |
F_io_net (I,J) = 0. _d 0 |
231 |
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F_ia_net (I,J) = 0. _d 0 |
232 |
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233 |
mlosch |
1.10 |
F_lh (I,J) = 0. _d 0 |
234 |
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235 |
mlosch |
1.5 |
C Reset the snow/ice surface to TMELT and bound the atmospheric temperature |
236 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
237 |
mlosch |
1.5 |
tsurfLoc (I,J) = MIN(273.16 _d 0 + MAX_TICE,TSURF(I,J,bi,bj)) |
238 |
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atempLoc (I,J) = MAX(273.16 _d 0 + MIN_ATEMP,ATEMP(I,J,bi,bj)) |
239 |
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A1(I,J) = 0.0 _d 0 |
240 |
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A2(I,J) = 0.0 _d 0 |
241 |
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A3(I,J) = 0.0 _d 0 |
242 |
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c B(I,J) = 0.0 _d 0 |
243 |
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lwdownLoc(I,J) = MAX(MIN_LWDOWN,LWDOWN(I,J,bi,bj)) |
244 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
245 |
mlosch |
1.5 |
F_swi (I,J) = 0. _d 0 |
246 |
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F_lwd (I,J) = 0. _d 0 |
247 |
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F_lwu (I,J) = 0. _d 0 |
248 |
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F_sens (I,J) = 0. _d 0 |
249 |
jmc |
1.6 |
|
250 |
mlosch |
1.5 |
tsurfLoc (I,J) = TSURF(I,J,bi,bj) |
251 |
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atempLoc (I,J) = MAX(TMELT + MIN_ATEMP,ATEMP(I,J,bi,bj)) |
252 |
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lwdownLoc(I,J) = LWDOWN(I,J,bi,bj) |
253 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
254 |
jmc |
1.1 |
|
255 |
mlosch |
1.5 |
C FREEZING TEMPERATURE OF SEAWATER |
256 |
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#ifdef SEAICE_VARIABLE_FREEZING_POINT |
257 |
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C Use a variable seawater freezing point |
258 |
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TB(I,J) = -0.0575 _d 0*salt(I,J,kSrf,bi,bj) + 0.0901 _d 0 |
259 |
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& + celsius2K |
260 |
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#else |
261 |
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C Use a constant freezing temperature (SEAICE_VARIABLE_FREEZING_POINT undef) |
262 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
263 |
mlosch |
1.5 |
TB(I,J) = 271.2 _d 0 |
264 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
265 |
mlosch |
1.5 |
TB(I,J) = celsius2K + SEAICE_freeze |
266 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
267 |
mlosch |
1.5 |
#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
268 |
mlosch |
1.18 |
IF(HSNOW_ACTUAL(I,J).GT.0.0) THEN |
269 |
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C Stefan-Boltzman constant times emissivity |
270 |
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D3(I,J)=SEAICE_snow_emiss*SEAICE_boltzmann |
271 |
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#ifdef EXF_LWDOWN_WITH_EMISSIVITY |
272 |
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C This is now [(1-emiss)*lwdown - lwdown] |
273 |
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lwdownloc(I,J) = SEAICE_snow_emiss*lwdownloc(I,J) |
274 |
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#else /* use the old hard wired inconsistent value */ |
275 |
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lwdownloc(I,J) = 0.97 _d 0*lwdownloc(I,J) |
276 |
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#endif /* EXF_LWDOWN_WITH_EMISSIVITY */ |
277 |
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ELSE |
278 |
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C Stefan-Boltzman constant times emissivity |
279 |
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D3(I,J)=SEAICE_ice_emiss*SEAICE_boltzmann |
280 |
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#ifdef EXF_LWDOWN_WITH_EMISSIVITY |
281 |
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C This is now [(1-emiss)*lwdown - lwdown] |
282 |
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lwdownloc(I,J) = SEAICE_ice_emiss*lwdownloc(I,J) |
283 |
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#else /* use the old hard wired inconsistent value */ |
284 |
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lwdownloc(I,J) = 0.97 _d 0*lwdownloc(I,J) |
285 |
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#endif /* EXF_LWDOWN_WITH_EMISSIVITY */ |
286 |
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ENDIF |
287 |
mlosch |
1.5 |
ENDDO |
288 |
jmc |
1.1 |
ENDDO |
289 |
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290 |
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DO J=1,sNy |
291 |
mlosch |
1.5 |
DO I=1,sNx |
292 |
jmc |
1.1 |
|
293 |
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C DECIDE ON ALBEDO |
294 |
mlosch |
1.5 |
IF ( iceOrNot(I,J) ) THEN |
295 |
jmc |
1.6 |
|
296 |
mlosch |
1.5 |
IF ( YC(I,J,bi,bj) .LT. 0.0 _d 0 ) THEN |
297 |
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IF (tsurfLoc(I,J) .GE. SurfMeltTemp) THEN |
298 |
|
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ALB_ICE (I,J) = SEAICE_wetIceAlb_south |
299 |
|
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ALB_SNOW(I,J) = SEAICE_wetSnowAlb_south |
300 |
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ELSE ! no surface melting |
301 |
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ALB_ICE (I,J) = SEAICE_dryIceAlb_south |
302 |
|
|
ALB_SNOW(I,J) = SEAICE_drySnowAlb_south |
303 |
|
|
ENDIF |
304 |
|
|
ELSE !/ Northern Hemisphere |
305 |
|
|
IF (tsurfLoc(I,J) .GE. SurfMeltTemp) THEN |
306 |
|
|
ALB_ICE (I,J) = SEAICE_wetIceAlb |
307 |
|
|
ALB_SNOW(I,J) = SEAICE_wetSnowAlb |
308 |
|
|
ELSE ! no surface melting |
309 |
|
|
ALB_ICE (I,J) = SEAICE_dryIceAlb |
310 |
|
|
ALB_SNOW(I,J) = SEAICE_drySnowAlb |
311 |
|
|
ENDIF |
312 |
|
|
ENDIF !/ Albedo for snow and ice |
313 |
|
|
|
314 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
315 |
mlosch |
1.5 |
C If actual snow thickness exceeds the cutoff thickness, use the |
316 |
|
|
C snow albedo |
317 |
|
|
IF (HSNOW_ACTUAL(I,J) .GT. HCUT) THEN |
318 |
|
|
ALB(I,J) = ALB_SNOW(I,J) |
319 |
|
|
C otherwise, use some combination of ice and snow albedo |
320 |
|
|
C (What is the source of this formulation ?) |
321 |
|
|
ELSE |
322 |
|
|
ALB(I,J) = MIN(ALB_ICE(I,J) + HSNOW_ACTUAL(I,J)/HCUT* |
323 |
|
|
& (ALB_SNOW(I,J) -ALB_ICE(I,J)), |
324 |
|
|
& ALB_SNOW(I,J)) |
325 |
|
|
ENDIF |
326 |
|
|
|
327 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
328 |
mlosch |
1.5 |
IF (HSNOW_ACTUAL(I,J) .GT. 0.0 _d 0) THEN |
329 |
|
|
ALB(I,J) = ALB_SNOW(I,J) |
330 |
|
|
ELSE |
331 |
|
|
ALB(I,J) = ALB_ICE(I,J) |
332 |
|
|
ENDIF |
333 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
334 |
jmc |
1.1 |
|
335 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
336 |
mlosch |
1.5 |
C NOW DETERMINE FIXED FORCING TERM IN HEAT BUDGET |
337 |
jmc |
1.1 |
|
338 |
mlosch |
1.5 |
IF(HSNOW_ACTUAL(I,J).GT.0.0) THEN |
339 |
|
|
C NO SW PENETRATION WITH SNOW |
340 |
|
|
A1(I,J)=(1.0 _d 0 - ALB(I,J))*SWDOWN(I,J,bi,bj) |
341 |
mlosch |
1.18 |
& +lwdownLoc(I,J) |
342 |
mlosch |
1.5 |
& +D1*UG(I,J)*atempLoc(I,J)+D1I*UG(I,J)*AQH(I,J,bi,bj) |
343 |
|
|
ELSE |
344 |
jmc |
1.1 |
C SW PENETRATION UNDER ICE |
345 |
mlosch |
1.5 |
A1(I,J)=(1.0 _d 0 - ALB(I,J))*SWDOWN(I,J,bi,bj) |
346 |
|
|
& *(1.0 _d 0 - XIO*EXP(-1.5 _d 0*HICE_ACTUAL(I,J))) |
347 |
mlosch |
1.18 |
& +lwdownLoc(I,J) |
348 |
mlosch |
1.5 |
& +D1*UG(I,J)*atempLoc(I,J)+D1I*UG(I,J)*AQH(I,J,bi,bj) |
349 |
|
|
ENDIF |
350 |
jmc |
1.1 |
|
351 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
352 |
jmc |
1.1 |
|
353 |
jmc |
1.3 |
C The longwave radiative flux convergence |
354 |
mlosch |
1.18 |
F_lwd(I,J) = - lwdownLoc(I,J) |
355 |
jmc |
1.1 |
|
356 |
jmc |
1.3 |
C Determine the fraction of shortwave radiative flux |
357 |
|
|
C remaining after scattering through the snow and ice at |
358 |
|
|
C the ocean interface. If snow is present, no radiation |
359 |
|
|
C penetrates to the ocean. |
360 |
mlosch |
1.5 |
IF (HSNOW_ACTUAL(I,J) .GT. 0.0 _d 0) THEN |
361 |
|
|
IcePenetSWFluxFrac(I,J) = 0.0 _d 0 |
362 |
|
|
ELSE |
363 |
|
|
IcePenetSWFluxFrac(I,J) = |
364 |
|
|
& XIO*EXP(-1.5 _d 0 * HICE_ACTUAL(I,J)) |
365 |
|
|
ENDIF |
366 |
jmc |
1.1 |
|
367 |
jmc |
1.3 |
C The shortwave radiative flux convergence in the |
368 |
|
|
C seaice. |
369 |
mlosch |
1.5 |
AbsorbedSWFlux(I,J) = -(1.0 _d 0 - ALB(I,J))* |
370 |
|
|
& (1.0 _d 0 - IcePenetSWFluxFrac(I,J)) |
371 |
|
|
& *SWDOWN(I,J,bi,bj) |
372 |
jmc |
1.6 |
|
373 |
jmc |
1.3 |
C The shortwave radiative flux convergence in the |
374 |
|
|
C ocean beneath ice. |
375 |
mlosch |
1.5 |
IcePenetSWFlux(I,J) = -(1.0 _d 0 - ALB(I,J))* |
376 |
|
|
& IcePenetSWFluxFrac(I,J) |
377 |
|
|
& *SWDOWN(I,J,bi,bj) |
378 |
jmc |
1.1 |
|
379 |
mlosch |
1.5 |
F_swi(I,J) = AbsorbedSWFlux(I,J) |
380 |
jmc |
1.6 |
|
381 |
jmc |
1.3 |
C Set a mininum sea ice thickness of 5 cm to bound |
382 |
|
|
C the magnitude of conductive heat fluxes. |
383 |
ifenty |
1.15 |
cif * now taken care of by SEAICE_hice_reg in seaice_growth |
384 |
|
|
C hice_tmp = max(HICE_ACTUAL(I,J),5. _d -2) |
385 |
jmc |
1.1 |
|
386 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
387 |
jmc |
1.1 |
|
388 |
jmc |
1.3 |
C The effective conductivity of the two-layer |
389 |
|
|
C snow/ice system. |
390 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
391 |
mlosch |
1.5 |
effConduct(I,J)= |
392 |
|
|
& XKS/(HSNOW_ACTUAL(I,J)/HICE_ACTUAL(I,J) + |
393 |
|
|
& XKS/XKI)/HICE_ACTUAL(I,J) |
394 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
395 |
mlosch |
1.5 |
effConduct(I,J) = XKI * XKS / |
396 |
ifenty |
1.15 |
& (XKS * HICE_ACTUAL(I,j) + XKI * HSNOW_ACTUAL(I,J)) |
397 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
398 |
jmc |
1.1 |
|
399 |
|
|
#ifdef SEAICE_DEBUG |
400 |
ifenty |
1.16 |
IF ( (I .EQ. SEAICE_debugPointI) .and. |
401 |
|
|
& (J .EQ. SEAICE_debugPointJ) ) THEN |
402 |
jmc |
1.1 |
|
403 |
mlosch |
1.5 |
print '(A,i6)','-----------------------------------' |
404 |
|
|
print '(A,i6)','ibi merged initialization ', myIter |
405 |
jmc |
1.6 |
|
406 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
407 |
|
|
& 'ibi iter, TSL, TS ',myIter, |
408 |
|
|
& tsurfLoc(I,J), TSURF(I,J,bi,bj) |
409 |
jmc |
1.6 |
|
410 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
411 |
|
|
& 'ibi iter, TMELT ',myIter,TMELT |
412 |
jmc |
1.6 |
|
413 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
414 |
|
|
& 'ibi iter, HIA, EFKCON ',myIter, |
415 |
|
|
& HICE_ACTUAL(I,J), effConduct(I,J) |
416 |
jmc |
1.6 |
|
417 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
418 |
|
|
& 'ibi iter, HSNOW ',myIter, |
419 |
|
|
& HSNOW_ACTUAL(I,J), ALB(I,J) |
420 |
jmc |
1.6 |
|
421 |
mlosch |
1.5 |
print '(A,i6)','-----------------------------------' |
422 |
|
|
print '(A,i6)','ibi energy balance iterat ', myIter |
423 |
jmc |
1.6 |
|
424 |
mlosch |
1.5 |
ENDIF |
425 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
426 |
jmc |
1.6 |
|
427 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
428 |
|
|
ENDDO !/* i */ |
429 |
|
|
ENDDO !/* j */ |
430 |
jmc |
1.3 |
Ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
431 |
mlosch |
1.5 |
DO ITER=1,IMAX_TICE |
432 |
|
|
DO J=1,sNy |
433 |
|
|
DO I=1,sNx |
434 |
mlosch |
1.8 |
#ifdef ALLOW_AUTODIFF_TAMC |
435 |
|
|
iicekey = I + sNx*(J-1) + (ITER-1)*sNx*sNy |
436 |
|
|
CADJ STORE tsurfloc(i,j) = comlev1_solve4temp, |
437 |
|
|
CADJ & key = iicekey, byte = isbyte |
438 |
|
|
#endif /* ALLOW_AUTODIFF_TAMC */ |
439 |
|
|
|
440 |
mlosch |
1.5 |
IF ( iceOrNot(I,J) ) THEN |
441 |
jmc |
1.1 |
|
442 |
mlosch |
1.5 |
t1 = tsurfLoc(I,J) |
443 |
|
|
t2 = t1*t1 |
444 |
|
|
t3 = t2*t1 |
445 |
|
|
t4 = t2*t2 |
446 |
jmc |
1.1 |
|
447 |
mlosch |
1.5 |
C Calculate the specific humidity in the BL above the snow/ice |
448 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
449 |
mlosch |
1.5 |
C Use the Maykut polynomial |
450 |
|
|
qhice(I,J)=QS1*(C1*t4+C2*t3 +C3*t2+C4*t1+C5) |
451 |
jmc |
1.1 |
|
452 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
453 |
mlosch |
1.5 |
C Use an approximation which is more accurate at low temperatures |
454 |
jmc |
1.1 |
|
455 |
mlosch |
1.5 |
C log 10 of the sat vap pressure |
456 |
|
|
mm_log10pi = -aa1 / t1 + aa2 |
457 |
jmc |
1.1 |
|
458 |
mlosch |
1.5 |
C The saturation vapor pressure (SVP) in the surface |
459 |
|
|
C boundary layer (BL) above the snow/ice. |
460 |
|
|
C mm_pi = TEN **(mm_log10pi) |
461 |
jmc |
1.6 |
C The following form does the same, but is faster |
462 |
mlosch |
1.5 |
mm_pi = exp(mm_log10pi*lnTEN) |
463 |
jmc |
1.1 |
|
464 |
mlosch |
1.5 |
qhice(I,J) = bb1*mm_pi / (Ppascals - (1.0 _d 0 - bb1) * |
465 |
|
|
& mm_pi) |
466 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
467 |
jmc |
1.1 |
|
468 |
mlosch |
1.10 |
C Calculate the flux terms based on the updated tsurfLoc |
469 |
|
|
F_c(I,J) = -effConduct(I,J)*(TB(I,J)-tsurfLoc(I,J)) |
470 |
|
|
F_lh(I,J) = D1I*UG(I,J)*(qhice(I,J)-AQH(I,J,bi,bj)) |
471 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
472 |
mlosch |
1.18 |
A2(I,J)=-D1*UG(I,J)*t1-D1I*UG(I,J)*qhice(I,J)-D3(I,J)*t4 |
473 |
|
|
A3(I,J) = 4.0 _d 0*D3(I,J)*t3 + effConduct(I,J)+D1*UG(I,J) |
474 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
475 |
mlosch |
1.5 |
C A constant for SVP derivative w.r.t TICE |
476 |
|
|
C cc3t = TEN **(aa1 / t1) |
477 |
jmc |
1.6 |
C The following form does the same, but is faster |
478 |
mlosch |
1.5 |
cc3t = exp(aa1 / t1 * lnTEN) |
479 |
|
|
|
480 |
|
|
c d(qh)/d(TICE) |
481 |
|
|
dqhice_dTice = cc1*cc3t/((cc2-cc3t*Ppascals)**2 *t2) |
482 |
|
|
|
483 |
ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
484 |
|
|
c if the latent heat flux implied by tsurfLoc exceeds |
485 |
|
|
c F_lh_max, cap F_lh and decouple the flux magnitude from TICE |
486 |
|
|
if (F_lh(I,J) .GT. F_lh_max(I,J)) THEN |
487 |
|
|
F_lh(I,J) = F_lh_max(I,J) |
488 |
|
|
dqhice_dTice = ZERO |
489 |
|
|
endif |
490 |
|
|
#endif |
491 |
|
|
|
492 |
|
|
|
493 |
mlosch |
1.5 |
c d(F_ia)/d(TICE) |
494 |
mlosch |
1.18 |
dFiDTs1 = 4.0 _d 0*D3(I,J)*t3 + effConduct(I,J) + D1*UG(I,J) |
495 |
mlosch |
1.5 |
& + D1I*UG(I,J)*dqhice_dTice |
496 |
|
|
|
497 |
mlosch |
1.18 |
F_lwu(I,J)= t4 * D3(I,J) |
498 |
jmc |
1.6 |
|
499 |
mlosch |
1.5 |
F_sens(I,J)= D1 * UG(I,J) * (t1 - atempLoc(I,J)) |
500 |
jmc |
1.6 |
|
501 |
mlosch |
1.5 |
F_ia(I,J) = F_lwd(I,J) + F_swi(I,J) + F_lwu(I,J) + |
502 |
|
|
& F_c(I,J) + F_sens(I,J) + F_lh(I,J) |
503 |
jmc |
1.1 |
|
504 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
505 |
jmc |
1.1 |
|
506 |
|
|
#ifdef SEAICE_DEBUG |
507 |
ifenty |
1.16 |
IF ( (I .EQ. SEAICE_debugPointI) .and. |
508 |
|
|
& (J .EQ. SEAICE_debugPointJ) ) THEN |
509 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
510 |
|
|
& 'ice-iter qhICE, ', ITER,qhIce(I,J) |
511 |
jmc |
1.1 |
|
512 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
513 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
514 |
|
|
& 'ice-iter A1 A2 B ', ITER,A1(I,J), A2(I,J), |
515 |
|
|
& -F_c(I,J) |
516 |
jmc |
1.1 |
|
517 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
518 |
|
|
& 'ice-iter A3 (-A1+A2) ', ITER, A3(I,J), |
519 |
|
|
& -(A1(I,J) + A2(I,J)) |
520 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
521 |
|
|
|
522 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
523 |
|
|
& 'ice-iter dFiDTs1 F_ia ', ITER, dFiDTs1, |
524 |
|
|
& F_ia(I,J) |
525 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
526 |
jmc |
1.1 |
|
527 |
mlosch |
1.5 |
ENDIF |
528 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
529 |
jmc |
1.1 |
|
530 |
mlosch |
1.5 |
C Update tsurfLoc |
531 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
532 |
mlosch |
1.5 |
tsurfLoc(I,J)=tsurfLoc(I,J) |
533 |
|
|
& +(A1(I,J)+A2(I,J)-F_c(I,J))/A3(I,J) |
534 |
jmc |
1.6 |
|
535 |
mlosch |
1.5 |
tsurfLoc(I,J) =MAX(273.16 _d 0+MIN_TICE,tsurfLoc(I,J)) |
536 |
|
|
tsurfLoc(I,J) =MIN(tsurfLoc(I,J),TMELT) |
537 |
jmc |
1.6 |
|
538 |
|
|
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
539 |
mlosch |
1.5 |
tsurfLoc(I,J) = tsurfLoc(I,J) - F_ia(I,J) / dFiDTs1 |
540 |
jmc |
1.1 |
|
541 |
jmc |
1.3 |
C If the search leads to tsurfLoc < 50 Kelvin, |
542 |
|
|
C restart the search at tsurfLoc = TMELT. Note that one |
543 |
|
|
C solution to the energy balance problem is an |
544 |
|
|
C extremely low temperature - a temperature far below |
545 |
|
|
C realistic values. |
546 |
jmc |
1.1 |
|
547 |
mlosch |
1.5 |
IF (tsurfLoc(I,J) .LT. 50.0 _d 0 ) THEN |
548 |
|
|
tsurfLoc(I,J) = TMELT |
549 |
|
|
ENDIF |
550 |
gforget |
1.11 |
tsurfLoc(I,J) =MIN(tsurfLoc(I,J),TMELT) |
551 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
552 |
jmc |
1.1 |
|
553 |
|
|
#ifdef SEAICE_DEBUG |
554 |
ifenty |
1.16 |
IF ( (I .EQ. SEAICE_debugPointI) .and. |
555 |
|
|
& (J .EQ. SEAICE_debugPointJ) ) THEN |
556 |
jmc |
1.6 |
|
557 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
558 |
|
|
& 'ice-iter tsurfLc,|dif|', ITER, |
559 |
|
|
& tsurfLoc(I,J), |
560 |
|
|
& log10(abs(tsurfLoc(I,J) - t1)) |
561 |
|
|
ENDIF |
562 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
563 |
jmc |
1.1 |
|
564 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
565 |
|
|
ENDDO !/* i */ |
566 |
|
|
ENDDO !/* j */ |
567 |
|
|
ENDDO !/* Iterations */ |
568 |
jmc |
1.3 |
Ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
569 |
mlosch |
1.5 |
DO J=1,sNy |
570 |
|
|
DO I=1,sNx |
571 |
|
|
IF ( iceOrNot(I,J) ) THEN |
572 |
jmc |
1.1 |
|
573 |
jmc |
1.3 |
C Finalize the flux terms |
574 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
575 |
mlosch |
1.5 |
F_ia(I,J)=-A1(I,J)-A2(I,J) |
576 |
|
|
TSURF(I,J,bi,bj)=MIN(tsurfLoc(I,J),TMELT) |
577 |
jmc |
1.6 |
|
578 |
mlosch |
1.5 |
IF (HSNOW_ACTUAL(I,J) .GT. 0.0 _d 0 ) THEN |
579 |
|
|
C NO SW PENETRATION WITH SNOW |
580 |
|
|
IcePenetSWFlux(I,J)=0.0 _d 0 |
581 |
|
|
ELSE |
582 |
|
|
C SW PENETRATION UNDER ICE |
583 |
|
|
IcePenetSWFlux(I,J)=-(1.0 _d 0 -ALB(I,J))*SWDOWN(I,J,bi,bj) |
584 |
|
|
& *XIO*EXP(-1.5 _d 0*HICE_ACTUAL(I,J)) |
585 |
|
|
ENDIF |
586 |
jmc |
1.1 |
|
587 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
588 |
mlosch |
1.5 |
TSURF(I,J,bi,bj) = tsurfLoc(I,J) |
589 |
jmc |
1.1 |
|
590 |
mlosch |
1.5 |
C Recalculate the fluxes based on the (possibly) adjusted TSURF |
591 |
|
|
t1 = tsurfLoc(I,J) |
592 |
|
|
t2 = t1*t1 |
593 |
|
|
t3 = t2*t1 |
594 |
|
|
t4 = t2*t2 |
595 |
jmc |
1.1 |
|
596 |
mlosch |
1.5 |
C log 10 of the sat vap pressure |
597 |
|
|
mm_log10pi = -aa1 / t1 + aa2 |
598 |
jmc |
1.1 |
|
599 |
mlosch |
1.5 |
C saturation vapor pressure |
600 |
|
|
C mm_pi = TEN **(mm_log10pi) |
601 |
jmc |
1.6 |
C The following form does the same, but is faster |
602 |
mlosch |
1.5 |
mm_pi = exp(mm_log10pi*lnTEN) |
603 |
jmc |
1.1 |
|
604 |
jmc |
1.3 |
C over ice specific humidity |
605 |
mlosch |
1.5 |
qhice(I,J) = bb1*mm_pi/(Ppascals- (1.0 _d 0 - bb1) * mm_pi) |
606 |
jmc |
1.1 |
|
607 |
mlosch |
1.5 |
F_lh(I,J) = D1I * UG(I,J)*(qhice(I,J)-AQH(I,J,bi,bj)) |
608 |
ifenty |
1.16 |
|
609 |
|
|
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
610 |
|
|
if (F_lh(I,J) .GT. F_lh_max(I,J)) THEN |
611 |
|
|
F_lh(I,J) = F_lh_max(I,J) |
612 |
|
|
endif |
613 |
|
|
#endif |
614 |
|
|
|
615 |
mlosch |
1.5 |
F_c(I,J) = -effConduct(I,J) * (TB(I,J) - t1) |
616 |
mlosch |
1.18 |
F_lwu(I,J) = t4 * D3(I,J) |
617 |
mlosch |
1.5 |
F_sens(I,J) = D1 * UG(I,J) * (t1 - atempLoc(I,J)) |
618 |
jmc |
1.1 |
|
619 |
jmc |
1.3 |
C The flux between the ice/snow surface and the atmosphere. |
620 |
|
|
C (excludes upward conductive fluxes) |
621 |
mlosch |
1.5 |
F_ia(I,J) = F_lwd(I,J) + F_swi(I,J) + F_lwu(I,J) + |
622 |
|
|
& F_sens(I,J) + F_lh(I,J) |
623 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
624 |
jmc |
1.1 |
|
625 |
gforget |
1.9 |
#ifdef SEAICE_MODIFY_GROWTH_ADJ |
626 |
|
|
Cgf no additional dependency through solver, snow, etc. |
627 |
|
|
if ( SEAICEadjMODE.GE.2 ) then |
628 |
|
|
CALL ZERO_ADJ_1D( 1, TSURF(I,J,bi,bj), myThid) |
629 |
|
|
t1 = TSURF(I,J,bi,bj) |
630 |
|
|
t2 = t1*t1 |
631 |
|
|
t3 = t2*t1 |
632 |
|
|
t4 = t2*t2 |
633 |
|
|
qhice(I,J)=QS1*(C1*t4+C2*t3 +C3*t2+C4*t1+C5) |
634 |
|
|
|
635 |
mlosch |
1.18 |
A1(I,J)=0.3 _d 0 *SWDOWN(I,J,bi,bj)+lwdownLoc(I,J) |
636 |
gforget |
1.9 |
& +D1*UG(I,J)*atempLoc(I,J)+D1I*UG(I,J)*AQH(I,J,bi,bj) |
637 |
mlosch |
1.18 |
A2(I,J)=-D1*UG(I,J)*t1-D1I*UG(I,J)*qhice(I,J)-D3(I,J)*t4 |
638 |
gforget |
1.9 |
|
639 |
|
|
F_ia(I,J)=-A1(I,J)-A2(I,J) |
640 |
|
|
IcePenetSWFlux(I,J)= 0. _d 0 |
641 |
|
|
endif |
642 |
|
|
#endif |
643 |
|
|
|
644 |
mlosch |
1.5 |
C Caclulate the net ice-ocean and ice-atmosphere fluxes |
645 |
|
|
IF (F_c(I,J) .LT. 0.0 _d 0) THEN |
646 |
|
|
F_io_net(I,J) = -F_c(I,J) |
647 |
|
|
F_ia_net(I,J) = 0.0 _d 0 |
648 |
|
|
ELSE |
649 |
|
|
F_io_net(I,J) = 0.0 _d 0 |
650 |
|
|
F_ia_net(I,J) = F_ia(I,J) |
651 |
|
|
ENDIF !/* conductive fluxes up or down */ |
652 |
mlosch |
1.10 |
C Fresh water flux (kg/m^2/s) from latent heat of sublimation. |
653 |
|
|
C F_lh is positive upward (sea ice looses heat) and FWsublim |
654 |
|
|
C is also positive upward (atmosphere gains freshwater) |
655 |
ifenty |
1.14 |
FWsublim(I,J) = F_lh(I,J)/lhSublim |
656 |
jmc |
1.1 |
|
657 |
|
|
#ifdef SEAICE_DEBUG |
658 |
ifenty |
1.16 |
IF ( (I .EQ. SEAICE_debugPointI) .and. |
659 |
|
|
& (J .EQ. SEAICE_debugPointJ) ) THEN |
660 |
jmc |
1.6 |
|
661 |
mlosch |
1.5 |
print '(A)','----------------------------------------' |
662 |
|
|
print '(A,i6)','ibi complete ', myIter |
663 |
jmc |
1.6 |
|
664 |
mlosch |
1.5 |
print '(A,4(1x,D24.15))', |
665 |
|
|
& 'ibi T(SURF, surfLoc,atmos) ', |
666 |
|
|
& TSURF(I,J,bi,bj), tsurfLoc(I,J),atempLoc(I,J) |
667 |
jmc |
1.6 |
|
668 |
mlosch |
1.5 |
print '(A,4(1x,D24.15))', |
669 |
|
|
& 'ibi LWL ', lwdownLoc(I,J) |
670 |
jmc |
1.6 |
|
671 |
mlosch |
1.5 |
print '(A,4(1x,D24.15))', |
672 |
|
|
& 'ibi QSW(Total, Penetrating)', |
673 |
|
|
& SWDOWN(I,J,bi,bj), IcePenetSWFlux(I,J) |
674 |
jmc |
1.6 |
|
675 |
mlosch |
1.5 |
print '(A,4(1x,D24.15))', |
676 |
|
|
& 'ibi qh(ATM ICE) ', |
677 |
|
|
& AQH(I,J,bi,bj),qhice(I,J) |
678 |
jmc |
1.6 |
|
679 |
ifenty |
1.16 |
#ifndef SEAICE_SOLVE4TEMP_LEGACY |
680 |
|
|
print '(A,4(1x,D24.15))', |
681 |
|
|
& 'ibi F(lwd,swi,lwu) ', |
682 |
|
|
& F_lwd(I,J), F_swi(I,J), F_lwu(I,J) |
683 |
|
|
|
684 |
|
|
print '(A,4(1x,D24.15))', |
685 |
|
|
& 'ibi F(c,lh,sens) ', |
686 |
|
|
& F_c(I,J), F_lh(I,J), F_sens(I,J) |
687 |
|
|
|
688 |
|
|
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
689 |
|
|
IF (F_lh_max(I,J) .GT. ZERO) THEN |
690 |
|
|
print '(A,4(1x,D24.15))', |
691 |
|
|
& 'ibi F_lh_max, F_lh/lhmax) ', |
692 |
|
|
& F_lh_max(I,J), F_lh(I,J)/ F_lh_max(I,J) |
693 |
jmc |
1.19 |
ELSE |
694 |
ifenty |
1.16 |
print '(A,4(1x,D24.15))', |
695 |
|
|
& 'ibi F_lh_max = ZERO! ' |
696 |
|
|
ENDIF |
697 |
|
|
|
698 |
|
|
print '(A,4(1x,D24.15))', |
699 |
|
|
& 'ibi FWsub, FWsubm*dT/rhoI ', |
700 |
|
|
& FWsublim(I,J), |
701 |
|
|
& FWsublim(I,J)*SEAICE_deltaTtherm/SEAICE_rhoICE |
702 |
|
|
#endif |
703 |
|
|
#endif |
704 |
mlosch |
1.5 |
|
705 |
|
|
print '(A,4(1x,D24.15))', |
706 |
|
|
& 'ibi F_ia, F_ia_net, F_c ', |
707 |
jmc |
1.6 |
#ifdef SEAICE_SOLVE4TEMP_LEGACY |
708 |
mlosch |
1.5 |
& -(A1(I,J)+A2(I,J)), |
709 |
|
|
& -(A1(I,J)+A2(I,J)-F_c(I,J)), |
710 |
|
|
& F_c(I,J) |
711 |
jmc |
1.6 |
#else /* SEAICE_SOLVE4TEMP_LEGACY */ |
712 |
mlosch |
1.5 |
& F_ia(I,J), |
713 |
|
|
& F_ia_net(I,J), |
714 |
|
|
& F_c(I,J) |
715 |
jmc |
1.6 |
#endif /* SEAICE_SOLVE4TEMP_LEGACY */ |
716 |
jmc |
1.1 |
|
717 |
mlosch |
1.5 |
print '(A)','----------------------------------------' |
718 |
jmc |
1.1 |
|
719 |
mlosch |
1.5 |
ENDIF |
720 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
721 |
jmc |
1.6 |
|
722 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
723 |
|
|
ENDDO !/* i */ |
724 |
jmc |
1.1 |
ENDDO !/* j */ |
725 |
|
|
|
726 |
jmc |
1.19 |
#endif /* ALLOW_ATM_TEMP && ALLOW_DOWNWARD_RADIATION */ |
727 |
|
|
RETURN |
728 |
jmc |
1.1 |
END |