1 |
jmc |
1.27 |
C $Header: /u/gcmpack/MITgcm/pkg/seaice/seaice_solve4temp.F,v 1.26 2012/02/05 21:06:54 jmc Exp $ |
2 |
jmc |
1.1 |
C $Name: $ |
3 |
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4 |
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#include "SEAICE_OPTIONS.h" |
5 |
jmc |
1.19 |
#ifdef ALLOW_EXF |
6 |
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# include "EXF_OPTIONS.h" |
7 |
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#endif |
8 |
jmc |
1.1 |
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9 |
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CBOP |
10 |
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C !ROUTINE: SEAICE_SOLVE4TEMP |
11 |
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C !INTERFACE: |
12 |
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SUBROUTINE SEAICE_SOLVE4TEMP( |
13 |
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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 |
jmc |
1.21 |
O F_ia, IcePenetSW, |
19 |
mlosch |
1.10 |
O FWsublim, |
20 |
jmc |
1.1 |
I bi, bj, myTime, myIter, myThid ) |
21 |
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22 |
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C !DESCRIPTION: \bv |
23 |
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C *==========================================================* |
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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 |
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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" |
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" |
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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 |
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 |
jmc |
1.21 |
C !INPUT PARAMETERS: |
53 |
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C UG :: atmospheric wind speed (m/s) |
54 |
jmc |
1.1 |
C HICE_ACTUAL :: actual ice thickness |
55 |
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C HSNOW_ACTUAL :: actual snow thickness |
56 |
jmc |
1.21 |
C TSURF :: surface temperature of ice/snow in Kelvin |
57 |
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C bi,bj :: tile indices |
58 |
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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). |
71 |
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C---------- |
72 |
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) |
75 |
ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
76 |
jmc |
1.21 |
_RL F_lh_max (1:sNx,1:sNy) |
77 |
ifenty |
1.16 |
#endif |
78 |
jmc |
1.21 |
_RL TSURF (1-OLx:sNx+OLx,1-OLy:sNy+OLy,nSx,nSy) |
79 |
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_RL F_ia (1:sNx,1:sNy) |
80 |
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_RL IcePenetSW (1:sNx,1:sNy) |
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_RL FWsublim (1:sNx,1:sNy) |
82 |
jmc |
1.1 |
INTEGER bi, bj |
83 |
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_RL myTime |
84 |
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INTEGER myIter, myThid |
85 |
jmc |
1.19 |
CEOP |
86 |
jmc |
1.1 |
|
87 |
jmc |
1.19 |
#if defined(ALLOW_ATM_TEMP) && defined(ALLOW_DOWNWARD_RADIATION) |
88 |
jmc |
1.1 |
C !LOCAL VARIABLES: |
89 |
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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 |
94 |
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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 |
102 |
jmc |
1.27 |
C SurfMeltTemp :: Temp (K) above which wet-albedo values are used |
103 |
mlosch |
1.5 |
_RL SurfMeltTemp |
104 |
jmc |
1.21 |
C effConduct :: effective conductivity of combined ice and snow |
105 |
mlosch |
1.5 |
_RL effConduct(1:sNx,1:sNy) |
106 |
jmc |
1.21 |
C lhSublim :: latent heat of sublimation (SEAICE_lhEvap + SEAICE_lhFusion) |
107 |
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_RL lhSublim |
108 |
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C t1,t2,t3,t4 :: powers of temperature |
109 |
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_RL t1, t2, t3, t4 |
110 |
jmc |
1.1 |
|
111 |
jmc |
1.24 |
C- Constants to calculate Saturation Vapor Pressure |
112 |
jmc |
1.26 |
C Maykut Polynomial Coeff. for Sat. Vapor Press |
113 |
jmc |
1.21 |
_RL C1, C2, C3, C4, C5, QS1 |
114 |
jmc |
1.24 |
C Extended temp-range expon. relation Coeff. for Sat. Vapor Press |
115 |
jmc |
1.21 |
_RL lnTEN |
116 |
jmc |
1.1 |
_RL aa1,aa2,bb1,bb2,Ppascals,cc0,cc1,cc2,cc3t |
117 |
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C specific humidity at ice surface variables |
118 |
jmc |
1.21 |
_RL mm_pi,mm_log10pi |
119 |
jmc |
1.1 |
|
120 |
jmc |
1.22 |
C F_c :: conductive heat flux through seaice+snow (+=upward) |
121 |
jmc |
1.26 |
C F_lwu :: upward long-wave surface heat flux (+=upward) |
122 |
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C F_sens :: sensible surface heat flux (+=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 |
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C dFia_dTs :: derivative of surf heat flux (F_ia) w.r.t surf. temp |
127 |
jmc |
1.26 |
_RL F_c (1:sNx,1:sNy) |
128 |
jmc |
1.21 |
_RL F_lwu (1:sNx,1:sNy) |
129 |
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_RL F_sens (1:sNx,1:sNy) |
130 |
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_RL F_lh (1:sNx,1:sNy) |
131 |
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_RL qhice (1:sNx,1:sNy) |
132 |
jmc |
1.24 |
_RL dqh_dTs (1:sNx,1:sNy) |
133 |
jmc |
1.26 |
_RL dFia_dTs (1:sNx,1:sNy) |
134 |
jmc |
1.21 |
_RL absorbedSW (1:sNx,1:sNy) |
135 |
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_RL penetSWFrac |
136 |
jmc |
1.25 |
_RL delTsurf |
137 |
jmc |
1.21 |
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138 |
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C local copies of global variables |
139 |
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_RL tsurfLoc (1:sNx,1:sNy) |
140 |
jmc |
1.25 |
_RL tsurfPrev (1:sNx,1:sNy) |
141 |
jmc |
1.21 |
_RL atempLoc (1:sNx,1:sNy) |
142 |
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_RL lwdownLoc (1:sNx,1:sNy) |
143 |
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_RL ALB (1:sNx,1:sNy) |
144 |
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_RL ALB_ICE (1:sNx,1:sNy) |
145 |
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_RL ALB_SNOW (1:sNx,1:sNy) |
146 |
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C iceOrNot :: this is HICE_ACTUAL.GT.0. |
147 |
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LOGICAL iceOrNot(1:sNx,1:sNy) |
148 |
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#ifdef SEAICE_DEBUG |
149 |
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C F_io_net :: upward conductive heat flux through seaice+snow |
150 |
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C F_ia_net :: net heat flux divergence at the sea ice/snow surface: |
151 |
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C includes ice conductive fluxes and atmospheric fluxes (W/m^2) |
152 |
jmc |
1.25 |
_RL F_io_net |
153 |
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_RL F_ia_net |
154 |
jmc |
1.21 |
#endif /* SEAICE_DEBUG */ |
155 |
ifenty |
1.14 |
|
156 |
jmc |
1.21 |
C---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
157 |
jmc |
1.1 |
|
158 |
mlosch |
1.8 |
#ifdef ALLOW_AUTODIFF_TAMC |
159 |
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CADJ INIT comlev1_solve4temp = COMMON, sNx*sNy*NMAX_TICE |
160 |
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#endif /* ALLOW_AUTODIFF_TAMC */ |
161 |
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162 |
jmc |
1.24 |
C- MAYKUT CONSTANTS FOR SAT. VAP. PRESSURE TEMP. POLYNOMIAL |
163 |
mlosch |
1.5 |
C1= 2.7798202 _d -06 |
164 |
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C2= -2.6913393 _d -03 |
165 |
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C3= 0.97920849 _d +00 |
166 |
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C4= -158.63779 _d +00 |
167 |
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C5= 9653.1925 _d +00 |
168 |
jmc |
1.1 |
QS1=0.622 _d +00/1013.0 _d +00 |
169 |
jmc |
1.24 |
C- Extended temp-range expon. relation Coeff. for Sat. Vapor Press |
170 |
jmc |
1.21 |
lnTEN = LOG(10.0 _d 0) |
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 |
jmc |
1.21 |
cc0 = EXP(aa2*lnTEN) |
178 |
mlosch |
1.5 |
cc1 = cc0*aa1*bb1*Ppascals*lnTEN |
179 |
jmc |
1.1 |
cc2 = cc0*bb2 |
180 |
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181 |
jmc |
1.4 |
#ifdef SEAICE_VARIABLE_FREEZING_POINT |
182 |
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kSrf = 1 |
183 |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
184 |
jmc |
1.1 |
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185 |
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C SENSIBLE HEAT CONSTANT |
186 |
mlosch |
1.7 |
D1=SEAICE_dalton*SEAICE_cpAir*SEAICE_rhoAir |
187 |
jmc |
1.1 |
|
188 |
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C ICE LATENT HEAT CONSTANT |
189 |
ifenty |
1.14 |
lhSublim = SEAICE_lhEvap + SEAICE_lhFusion |
190 |
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D1I=SEAICE_dalton*lhSublim*SEAICE_rhoAir |
191 |
jmc |
1.1 |
|
192 |
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C MELTING TEMPERATURE OF ICE |
193 |
mlosch |
1.5 |
TMELT = celsius2K |
194 |
jmc |
1.1 |
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195 |
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C ICE CONDUCTIVITY |
196 |
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XKI=SEAICE_iceConduct |
197 |
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198 |
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C SNOW CONDUCTIVITY |
199 |
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XKS=SEAICE_snowConduct |
200 |
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201 |
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C CUTOFF SNOW THICKNESS |
202 |
jmc |
1.21 |
C Snow-Thickness above HCUT: SW optically thick snow (=> snow-albedo). |
203 |
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C Snow-Thickness below HCUT: linear transition to ice-albedo |
204 |
jmc |
1.24 |
HCUT = SEAICE_snowThick |
205 |
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206 |
jmc |
1.26 |
C Wet/dry albebo temperature threshold |
207 |
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SEAICE_wetAlbTemp = - 1. _d -3 |
208 |
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209 |
jmc |
1.24 |
C PENETRATION SHORTWAVE RADIATION FACTOR |
210 |
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XIO=SEAICE_shortwave |
211 |
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212 |
jmc |
1.27 |
C Temperature Threshold for wet-albedo: |
213 |
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SurfMeltTemp = TMELT + SEAICE_wetAlbTemp |
214 |
jmc |
1.24 |
C old SOLVE4TEMP_LEGACY setting, consistent with former celsius2K value: |
215 |
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c TMELT = 273.16 _d +00 |
216 |
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c SurfMeltTemp = 273.159 _d +00 |
217 |
jmc |
1.1 |
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218 |
jmc |
1.3 |
C Initialize variables |
219 |
jmc |
1.1 |
DO J=1,sNy |
220 |
mlosch |
1.5 |
DO I=1,sNx |
221 |
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C HICE_ACTUAL is modified in this routine, but at the same time |
222 |
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C used to decided where there is ice, therefore we save this information |
223 |
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C here in a separate array |
224 |
jmc |
1.21 |
iceOrNot (I,J) = HICE_ACTUAL(I,J) .GT. 0. _d 0 |
225 |
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IcePenetSW(I,J) = 0. _d 0 |
226 |
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absorbedSW(I,J) = 0. _d 0 |
227 |
mlosch |
1.5 |
qhice (I,J) = 0. _d 0 |
228 |
jmc |
1.24 |
dqh_dTs (I,J) = 0. _d 0 |
229 |
mlosch |
1.5 |
F_ia (I,J) = 0. _d 0 |
230 |
mlosch |
1.10 |
F_lh (I,J) = 0. _d 0 |
231 |
mlosch |
1.5 |
F_lwu (I,J) = 0. _d 0 |
232 |
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F_sens (I,J) = 0. _d 0 |
233 |
jmc |
1.26 |
C Make a local copy of LW, surface & atmospheric temperatures |
234 |
mlosch |
1.5 |
tsurfLoc (I,J) = TSURF(I,J,bi,bj) |
235 |
jmc |
1.26 |
c tsurfLoc (I,J) = MIN( celsius2K+MAX_TICE, TSURF(I,J,bi,bj) ) |
236 |
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lwdownLoc(I,J) = MAX( MIN_LWDOWN, LWDOWN(I,J,bi,bj) ) |
237 |
jmc |
1.24 |
atempLoc (I,J) = MAX( celsius2K+MIN_ATEMP, ATEMP(I,J,bi,bj) ) |
238 |
jmc |
1.1 |
|
239 |
mlosch |
1.5 |
C FREEZING TEMPERATURE OF SEAWATER |
240 |
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#ifdef SEAICE_VARIABLE_FREEZING_POINT |
241 |
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C Use a variable seawater freezing point |
242 |
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TB(I,J) = -0.0575 _d 0*salt(I,J,kSrf,bi,bj) + 0.0901 _d 0 |
243 |
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& + celsius2K |
244 |
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#else |
245 |
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C Use a constant freezing temperature (SEAICE_VARIABLE_FREEZING_POINT undef) |
246 |
jmc |
1.23 |
C old SOLVE4TEMP_LEGACY setting (not consistent with seaice_growth value) |
247 |
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c TB(I,J) = 271.2 _d 0 |
248 |
mlosch |
1.5 |
TB(I,J) = celsius2K + SEAICE_freeze |
249 |
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#endif /* SEAICE_VARIABLE_FREEZING_POINT */ |
250 |
jmc |
1.26 |
|
251 |
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C Now determine fixed (relative to tsurf) forcing term in heat budget |
252 |
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253 |
mlosch |
1.18 |
IF(HSNOW_ACTUAL(I,J).GT.0.0) THEN |
254 |
jmc |
1.21 |
C Stefan-Boltzmann constant times emissivity |
255 |
mlosch |
1.18 |
D3(I,J)=SEAICE_snow_emiss*SEAICE_boltzmann |
256 |
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#ifdef EXF_LWDOWN_WITH_EMISSIVITY |
257 |
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C This is now [(1-emiss)*lwdown - lwdown] |
258 |
jmc |
1.26 |
lwdownLoc(I,J) = SEAICE_snow_emiss*lwdownLoc(I,J) |
259 |
mlosch |
1.18 |
#else /* use the old hard wired inconsistent value */ |
260 |
jmc |
1.26 |
lwdownLoc(I,J) = 0.97 _d 0*lwdownLoc(I,J) |
261 |
mlosch |
1.18 |
#endif /* EXF_LWDOWN_WITH_EMISSIVITY */ |
262 |
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ELSE |
263 |
jmc |
1.21 |
C Stefan-Boltzmann constant times emissivity |
264 |
mlosch |
1.18 |
D3(I,J)=SEAICE_ice_emiss*SEAICE_boltzmann |
265 |
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#ifdef EXF_LWDOWN_WITH_EMISSIVITY |
266 |
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C This is now [(1-emiss)*lwdown - lwdown] |
267 |
jmc |
1.26 |
lwdownLoc(I,J) = SEAICE_ice_emiss*lwdownLoc(I,J) |
268 |
mlosch |
1.18 |
#else /* use the old hard wired inconsistent value */ |
269 |
jmc |
1.26 |
lwdownLoc(I,J) = 0.97 _d 0*lwdownLoc(I,J) |
270 |
mlosch |
1.18 |
#endif /* EXF_LWDOWN_WITH_EMISSIVITY */ |
271 |
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ENDIF |
272 |
mlosch |
1.5 |
ENDDO |
273 |
jmc |
1.1 |
ENDDO |
274 |
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275 |
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DO J=1,sNy |
276 |
mlosch |
1.5 |
DO I=1,sNx |
277 |
jmc |
1.1 |
|
278 |
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C DECIDE ON ALBEDO |
279 |
mlosch |
1.5 |
IF ( iceOrNot(I,J) ) THEN |
280 |
jmc |
1.6 |
|
281 |
mlosch |
1.5 |
IF ( YC(I,J,bi,bj) .LT. 0.0 _d 0 ) THEN |
282 |
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IF (tsurfLoc(I,J) .GE. SurfMeltTemp) THEN |
283 |
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ALB_ICE (I,J) = SEAICE_wetIceAlb_south |
284 |
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ALB_SNOW(I,J) = SEAICE_wetSnowAlb_south |
285 |
|
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ELSE ! no surface melting |
286 |
|
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ALB_ICE (I,J) = SEAICE_dryIceAlb_south |
287 |
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ALB_SNOW(I,J) = SEAICE_drySnowAlb_south |
288 |
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ENDIF |
289 |
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ELSE !/ Northern Hemisphere |
290 |
|
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IF (tsurfLoc(I,J) .GE. SurfMeltTemp) THEN |
291 |
|
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ALB_ICE (I,J) = SEAICE_wetIceAlb |
292 |
|
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ALB_SNOW(I,J) = SEAICE_wetSnowAlb |
293 |
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ELSE ! no surface melting |
294 |
|
|
ALB_ICE (I,J) = SEAICE_dryIceAlb |
295 |
|
|
ALB_SNOW(I,J) = SEAICE_drySnowAlb |
296 |
|
|
ENDIF |
297 |
|
|
ENDIF !/ Albedo for snow and ice |
298 |
|
|
|
299 |
jmc |
1.21 |
C If actual snow thickness exceeds the cutoff thickness, use snow albedo |
300 |
mlosch |
1.5 |
IF (HSNOW_ACTUAL(I,J) .GT. HCUT) THEN |
301 |
|
|
ALB(I,J) = ALB_SNOW(I,J) |
302 |
jmc |
1.21 |
ELSEIF ( HCUT.LE.ZERO ) THEN |
303 |
|
|
ALB(I,J) = ALB_ICE(I,J) |
304 |
mlosch |
1.5 |
ELSE |
305 |
jmc |
1.21 |
C otherwise, use linear transition between ice and snow albedo |
306 |
|
|
ALB(I,J) = MIN( ALB_ICE(I,J) + HSNOW_ACTUAL(I,J)/HCUT |
307 |
|
|
& *(ALB_SNOW(I,J) -ALB_ICE(I,J)) |
308 |
|
|
& , ALB_SNOW(I,J) ) |
309 |
mlosch |
1.5 |
ENDIF |
310 |
|
|
|
311 |
jmc |
1.21 |
C Determine the fraction of shortwave radiative flux remaining |
312 |
|
|
C at ocean interface after scattering through the snow and ice. |
313 |
|
|
C If snow is present, no radiation penetrates through snow+ice |
314 |
mlosch |
1.5 |
IF (HSNOW_ACTUAL(I,J) .GT. 0.0 _d 0) THEN |
315 |
jmc |
1.21 |
penetSWFrac = 0.0 _d 0 |
316 |
mlosch |
1.5 |
ELSE |
317 |
jmc |
1.21 |
penetSWFrac = XIO*EXP(-1.5 _d 0 * HICE_ACTUAL(I,J)) |
318 |
mlosch |
1.5 |
ENDIF |
319 |
jmc |
1.21 |
C The shortwave radiative flux leaving ocean beneath ice (+=up). |
320 |
|
|
IcePenetSW(I,J) = -(1.0 _d 0 - ALB(I,J)) |
321 |
|
|
& *penetSWFrac * SWDOWN(I,J,bi,bj) |
322 |
|
|
C The shortwave radiative flux convergence in the seaice. |
323 |
|
|
absorbedSW(I,J) = (1.0 _d 0 - ALB(I,J)) |
324 |
|
|
& *(1.0 _d 0 - penetSWFrac)* SWDOWN(I,J,bi,bj) |
325 |
jmc |
1.1 |
|
326 |
jmc |
1.24 |
C The effective conductivity of the two-layer snow/ice system. |
327 |
jmc |
1.26 |
C Set a minimum sea ice thickness of 5 cm to bound |
328 |
jmc |
1.21 |
C the magnitude of conductive heat fluxes. |
329 |
|
|
Cif * now taken care of by SEAICE_hice_reg in seaice_growth |
330 |
|
|
c hice_tmp = max(HICE_ACTUAL(I,J),5. _d -2) |
331 |
mlosch |
1.5 |
effConduct(I,J) = XKI * XKS / |
332 |
jmc |
1.21 |
& (XKS * HICE_ACTUAL(I,J) + XKI * HSNOW_ACTUAL(I,J)) |
333 |
jmc |
1.1 |
|
334 |
|
|
#ifdef SEAICE_DEBUG |
335 |
jmc |
1.21 |
IF ( (I .EQ. SEAICE_debugPointI) .AND. |
336 |
ifenty |
1.16 |
& (J .EQ. SEAICE_debugPointJ) ) THEN |
337 |
mlosch |
1.5 |
print '(A,i6)','-----------------------------------' |
338 |
|
|
print '(A,i6)','ibi merged initialization ', myIter |
339 |
|
|
print '(A,i6,4(1x,D24.15))', |
340 |
|
|
& 'ibi iter, TSL, TS ',myIter, |
341 |
|
|
& tsurfLoc(I,J), TSURF(I,J,bi,bj) |
342 |
|
|
print '(A,i6,4(1x,D24.15))', |
343 |
|
|
& 'ibi iter, TMELT ',myIter,TMELT |
344 |
|
|
print '(A,i6,4(1x,D24.15))', |
345 |
|
|
& 'ibi iter, HIA, EFKCON ',myIter, |
346 |
|
|
& HICE_ACTUAL(I,J), effConduct(I,J) |
347 |
|
|
print '(A,i6,4(1x,D24.15))', |
348 |
|
|
& 'ibi iter, HSNOW ',myIter, |
349 |
|
|
& HSNOW_ACTUAL(I,J), ALB(I,J) |
350 |
|
|
print '(A,i6)','-----------------------------------' |
351 |
|
|
print '(A,i6)','ibi energy balance iterat ', myIter |
352 |
|
|
ENDIF |
353 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
354 |
jmc |
1.6 |
|
355 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
356 |
|
|
ENDDO !/* i */ |
357 |
|
|
ENDDO !/* j */ |
358 |
jmc |
1.21 |
|
359 |
|
|
C---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
360 |
mlosch |
1.5 |
DO ITER=1,IMAX_TICE |
361 |
|
|
DO J=1,sNy |
362 |
|
|
DO I=1,sNx |
363 |
mlosch |
1.8 |
#ifdef ALLOW_AUTODIFF_TAMC |
364 |
|
|
iicekey = I + sNx*(J-1) + (ITER-1)*sNx*sNy |
365 |
jmc |
1.26 |
CADJ STORE tsurfLoc(i,j) = comlev1_solve4temp, |
366 |
mlosch |
1.8 |
CADJ & key = iicekey, byte = isbyte |
367 |
|
|
#endif /* ALLOW_AUTODIFF_TAMC */ |
368 |
|
|
|
369 |
jmc |
1.25 |
C- save tsurf from previous iter |
370 |
|
|
tsurfPrev(I,J) = tsurfLoc(I,J) |
371 |
mlosch |
1.5 |
IF ( iceOrNot(I,J) ) THEN |
372 |
jmc |
1.1 |
|
373 |
mlosch |
1.5 |
t1 = tsurfLoc(I,J) |
374 |
|
|
t2 = t1*t1 |
375 |
|
|
t3 = t2*t1 |
376 |
|
|
t4 = t2*t2 |
377 |
jmc |
1.1 |
|
378 |
jmc |
1.24 |
C-- Calculate the specific humidity in the BL above the snow/ice |
379 |
jmc |
1.25 |
IF ( useMaykutSatVapPoly ) THEN |
380 |
jmc |
1.24 |
C- Use the Maykut polynomial |
381 |
jmc |
1.25 |
qhice(I,J)=QS1*(C1*t4+C2*t3 +C3*t2+C4*t1+C5) |
382 |
|
|
dqh_dTs(I,J) = 0. _d 0 |
383 |
|
|
ELSE |
384 |
jmc |
1.24 |
C- Use exponential relation approx., more accurate at low temperatures |
385 |
mlosch |
1.5 |
C log 10 of the sat vap pressure |
386 |
jmc |
1.25 |
mm_log10pi = -aa1 / t1 + aa2 |
387 |
mlosch |
1.5 |
C The saturation vapor pressure (SVP) in the surface |
388 |
|
|
C boundary layer (BL) above the snow/ice. |
389 |
jmc |
1.25 |
c mm_pi = TEN **(mm_log10pi) |
390 |
jmc |
1.6 |
C The following form does the same, but is faster |
391 |
jmc |
1.25 |
mm_pi = EXP(mm_log10pi*lnTEN) |
392 |
|
|
qhice(I,J) = bb1*mm_pi/( Ppascals -(1.0 _d 0 - bb1)*mm_pi ) |
393 |
jmc |
1.21 |
C A constant for SVP derivative w.r.t TICE |
394 |
jmc |
1.25 |
c cc3t = TEN **(aa1 / t1) |
395 |
jmc |
1.21 |
C The following form does the same, but is faster |
396 |
jmc |
1.25 |
cc3t = EXP(aa1 / t1 * lnTEN) |
397 |
jmc |
1.21 |
C d(qh)/d(TICE) |
398 |
jmc |
1.25 |
dqh_dTs(I,J) = cc1*cc3t/((cc2-cc3t*Ppascals)**2 *t2) |
399 |
|
|
ENDIF |
400 |
jmc |
1.1 |
|
401 |
mlosch |
1.10 |
C Calculate the flux terms based on the updated tsurfLoc |
402 |
jmc |
1.22 |
F_c(I,J) = effConduct(I,J)*(TB(I,J)-tsurfLoc(I,J)) |
403 |
mlosch |
1.10 |
F_lh(I,J) = D1I*UG(I,J)*(qhice(I,J)-AQH(I,J,bi,bj)) |
404 |
ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
405 |
jmc |
1.21 |
C if the latent heat flux implied by tsurfLoc exceeds |
406 |
|
|
C F_lh_max, cap F_lh and decouple the flux magnitude from TICE |
407 |
|
|
IF (F_lh(I,J) .GT. F_lh_max(I,J)) THEN |
408 |
ifenty |
1.16 |
F_lh(I,J) = F_lh_max(I,J) |
409 |
jmc |
1.24 |
dqh_dTs(I,J) = ZERO |
410 |
jmc |
1.21 |
ENDIF |
411 |
|
|
#endif /* SEAICE_ADD_SUBLIMATION_TO_FWBUDGET */ |
412 |
ifenty |
1.16 |
|
413 |
jmc |
1.21 |
F_lwu(I,J) = t4 * D3(I,J) |
414 |
mlosch |
1.5 |
F_sens(I,J)= D1 * UG(I,J) * (t1 - atempLoc(I,J)) |
415 |
jmc |
1.21 |
F_ia(I,J) = -lwdownLoc(I,J) -absorbedSW(I,J) + F_lwu(I,J) |
416 |
jmc |
1.24 |
& + F_sens(I,J) + F_lh(I,J) |
417 |
jmc |
1.26 |
C d(F_ia)/d(Tsurf) |
418 |
|
|
dFia_dTs(I,J) = 4.0 _d 0*D3(I,J)*t3 + D1*UG(I,J) |
419 |
|
|
& + D1I*UG(I,J)*dqh_dTs(I,J) |
420 |
jmc |
1.1 |
|
421 |
|
|
#ifdef SEAICE_DEBUG |
422 |
jmc |
1.21 |
IF ( (I .EQ. SEAICE_debugPointI) .AND. |
423 |
ifenty |
1.16 |
& (J .EQ. SEAICE_debugPointJ) ) THEN |
424 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
425 |
|
|
& 'ice-iter qhICE, ', ITER,qhIce(I,J) |
426 |
|
|
print '(A,i6,4(1x,D24.15))', |
427 |
jmc |
1.24 |
& 'ice-iter dFiDTs1 F_ia ', ITER, |
428 |
|
|
& dFia_dTs(I,J)+effConduct(I,J), F_ia(I,J)-F_c(I,J) |
429 |
mlosch |
1.5 |
ENDIF |
430 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
431 |
jmc |
1.1 |
|
432 |
jmc |
1.26 |
C- Update tsurf as solution of : Fc = Fia + d/dT(Fia - Fc) *delta.tsurf |
433 |
jmc |
1.24 |
tsurfLoc(I,J) = tsurfLoc(I,J) |
434 |
|
|
& + ( F_c(I,J)-F_ia(I,J) ) / ( effConduct(I,J)+dFia_dTs(I,J) ) |
435 |
jmc |
1.1 |
|
436 |
jmc |
1.26 |
IF ( useMaykutSatVapPoly ) THEN |
437 |
|
|
tsurfLoc(I,J) = MAX( celsius2K+MIN_TICE, tsurfLoc(I,J) ) |
438 |
|
|
ENDIF |
439 |
jmc |
1.21 |
C If the search leads to tsurfLoc < 50 Kelvin, restart the search |
440 |
|
|
C at tsurfLoc = TMELT. Note that one solution to the energy balance problem |
441 |
|
|
C is an extremely low temperature - a temperature far below realistic values. |
442 |
jmc |
1.26 |
c IF (tsurfLoc(I,J) .LT. 50.0 _d 0 ) tsurfLoc(I,J) = TMELT |
443 |
|
|
C Comments & code above not relevant anymore (from older version, when |
444 |
|
|
C trying Maykut-Polynomial & dqh_dTs > 0 ?): commented out |
445 |
jmc |
1.21 |
tsurfLoc(I,J) = MIN( tsurfLoc(I,J), TMELT ) |
446 |
jmc |
1.1 |
|
447 |
|
|
#ifdef SEAICE_DEBUG |
448 |
jmc |
1.21 |
IF ( (I .EQ. SEAICE_debugPointI) .AND. |
449 |
ifenty |
1.16 |
& (J .EQ. SEAICE_debugPointJ) ) THEN |
450 |
mlosch |
1.5 |
print '(A,i6,4(1x,D24.15))', |
451 |
|
|
& 'ice-iter tsurfLc,|dif|', ITER, |
452 |
|
|
& tsurfLoc(I,J), |
453 |
jmc |
1.21 |
& LOG10(ABS(tsurfLoc(I,J) - t1)) |
454 |
mlosch |
1.5 |
ENDIF |
455 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
456 |
jmc |
1.1 |
|
457 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
458 |
|
|
ENDDO !/* i */ |
459 |
|
|
ENDDO !/* j */ |
460 |
|
|
ENDDO !/* Iterations */ |
461 |
jmc |
1.21 |
C---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
462 |
|
|
|
463 |
mlosch |
1.5 |
DO J=1,sNy |
464 |
|
|
DO I=1,sNx |
465 |
|
|
IF ( iceOrNot(I,J) ) THEN |
466 |
jmc |
1.1 |
|
467 |
jmc |
1.21 |
C Save updated tsurf and finalize the flux terms |
468 |
|
|
TSURF(I,J,bi,bj) = tsurfLoc(I,J) |
469 |
|
|
|
470 |
jmc |
1.25 |
#ifdef SEAICE_MODIFY_GROWTH_ADJ |
471 |
|
|
Cgf no additional dependency through solver, snow, etc. |
472 |
|
|
IF ( SEAICEadjMODE.GE.2 ) THEN |
473 |
|
|
CALL ZERO_ADJ_1D( 1, TSURF(I,J,bi,bj), myThid) |
474 |
jmc |
1.26 |
absorbedSW(I,J) = 0.3 _d 0 *SWDOWN(I,J,bi,bj) |
475 |
|
|
IcePenetSW(I,J)= 0. _d 0 |
476 |
|
|
ENDIF |
477 |
|
|
IF ( postSolvTempIter.EQ.2 .OR. SEAICEadjMODE.GE.2 ) THEN |
478 |
jmc |
1.25 |
t1 = TSURF(I,J,bi,bj) |
479 |
|
|
#else /* SEAICE_MODIFY_GROWTH_ADJ */ |
480 |
|
|
|
481 |
|
|
IF ( postSolvTempIter.EQ.2 ) THEN |
482 |
mlosch |
1.5 |
C Recalculate the fluxes based on the (possibly) adjusted TSURF |
483 |
jmc |
1.25 |
t1 = tsurfLoc(I,J) |
484 |
jmc |
1.26 |
#endif /* SEAICE_MODIFY_GROWTH_ADJ */ |
485 |
jmc |
1.25 |
t2 = t1*t1 |
486 |
|
|
t3 = t2*t1 |
487 |
|
|
t4 = t2*t2 |
488 |
jmc |
1.1 |
|
489 |
jmc |
1.25 |
IF ( useMaykutSatVapPoly ) THEN |
490 |
|
|
qhice(I,J)=QS1*(C1*t4+C2*t3 +C3*t2+C4*t1+C5) |
491 |
|
|
ELSE |
492 |
mlosch |
1.5 |
C log 10 of the sat vap pressure |
493 |
jmc |
1.25 |
mm_log10pi = -aa1 / t1 + aa2 |
494 |
mlosch |
1.5 |
C saturation vapor pressure |
495 |
jmc |
1.25 |
c mm_pi = TEN **(mm_log10pi) |
496 |
jmc |
1.6 |
C The following form does the same, but is faster |
497 |
jmc |
1.25 |
mm_pi = EXP(mm_log10pi*lnTEN) |
498 |
jmc |
1.21 |
C over ice specific humidity |
499 |
jmc |
1.25 |
qhice(I,J) = bb1*mm_pi/( Ppascals -(1.0 _d 0 - bb1)*mm_pi ) |
500 |
|
|
ENDIF |
501 |
jmc |
1.26 |
F_c(I,J) = effConduct(I,J) * (TB(I,J) - t1) |
502 |
jmc |
1.25 |
F_lh(I,J) = D1I * UG(I,J)*(qhice(I,J)-AQH(I,J,bi,bj)) |
503 |
ifenty |
1.16 |
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
504 |
jmc |
1.25 |
IF (F_lh(I,J) .GT. F_lh_max(I,J)) THEN |
505 |
ifenty |
1.16 |
F_lh(I,J) = F_lh_max(I,J) |
506 |
jmc |
1.25 |
ENDIF |
507 |
jmc |
1.21 |
#endif /* SEAICE_ADD_SUBLIMATION_TO_FWBUDGET */ |
508 |
jmc |
1.25 |
F_lwu(I,J) = t4 * D3(I,J) |
509 |
|
|
F_sens(I,J) = D1 * UG(I,J) * (t1 - atempLoc(I,J)) |
510 |
jmc |
1.21 |
C The flux between the ice/snow surface and the atmosphere. |
511 |
jmc |
1.25 |
F_ia(I,J) = -lwdownLoc(I,J) -absorbedSW(I,J) + F_lwu(I,J) |
512 |
|
|
& + F_sens(I,J) + F_lh(I,J) |
513 |
jmc |
1.1 |
|
514 |
jmc |
1.25 |
ELSEIF ( postSolvTempIter.EQ.1 ) THEN |
515 |
|
|
C Update fluxes (consistent with the linearized formulation) |
516 |
|
|
delTsurf = tsurfLoc(I,J)-tsurfPrev(I,J) |
517 |
|
|
F_c(I,J) = effConduct(I,J)*(TB(I,J)-tsurfLoc(I,J)) |
518 |
|
|
F_ia(I,J) = F_ia(I,J) + dFia_dTs(I,J)*delTsurf |
519 |
|
|
F_lh(I,J) = F_lh(I,J) |
520 |
|
|
& + D1I*UG(I,J)*dqh_dTs(I,J)*delTsurf |
521 |
jmc |
1.26 |
|
522 |
|
|
c ELSEIF ( postSolvTempIter.EQ.0 ) THEN |
523 |
jmc |
1.25 |
C Take fluxes from last iteration |
524 |
jmc |
1.26 |
|
525 |
jmc |
1.25 |
ELSEIF ( postSolvTempIter.NE.0 ) THEN |
526 |
jmc |
1.26 |
STOP 'SEAICE_SOLVE4TEMP: invalid postSolvTempIter' |
527 |
jmc |
1.21 |
ENDIF |
528 |
|
|
|
529 |
|
|
C Fresh water flux (kg/m^2/s) from latent heat of sublimation. |
530 |
|
|
C F_lh is positive upward (sea ice looses heat) and FWsublim |
531 |
|
|
C is also positive upward (atmosphere gains freshwater) |
532 |
|
|
FWsublim(I,J) = F_lh(I,J)/lhSublim |
533 |
gforget |
1.9 |
|
534 |
jmc |
1.21 |
#ifdef SEAICE_DEBUG |
535 |
jmc |
1.26 |
C Calculate the net ice-ocean and ice-atmosphere fluxes |
536 |
jmc |
1.22 |
IF (F_c(I,J) .GT. 0.0 _d 0) THEN |
537 |
jmc |
1.25 |
F_io_net = F_c(I,J) |
538 |
|
|
F_ia_net = 0.0 _d 0 |
539 |
mlosch |
1.5 |
ELSE |
540 |
jmc |
1.25 |
F_io_net = 0.0 _d 0 |
541 |
|
|
F_ia_net = F_ia(I,J) |
542 |
mlosch |
1.5 |
ENDIF !/* conductive fluxes up or down */ |
543 |
jmc |
1.1 |
|
544 |
jmc |
1.21 |
IF ( (I .EQ. SEAICE_debugPointI) .AND. |
545 |
ifenty |
1.16 |
& (J .EQ. SEAICE_debugPointJ) ) THEN |
546 |
mlosch |
1.5 |
print '(A)','----------------------------------------' |
547 |
|
|
print '(A,i6)','ibi complete ', myIter |
548 |
|
|
print '(A,4(1x,D24.15))', |
549 |
|
|
& 'ibi T(SURF, surfLoc,atmos) ', |
550 |
|
|
& TSURF(I,J,bi,bj), tsurfLoc(I,J),atempLoc(I,J) |
551 |
|
|
print '(A,4(1x,D24.15))', |
552 |
|
|
& 'ibi LWL ', lwdownLoc(I,J) |
553 |
|
|
print '(A,4(1x,D24.15))', |
554 |
|
|
& 'ibi QSW(Total, Penetrating)', |
555 |
jmc |
1.21 |
& SWDOWN(I,J,bi,bj), IcePenetSW(I,J) |
556 |
mlosch |
1.5 |
print '(A,4(1x,D24.15))', |
557 |
|
|
& 'ibi qh(ATM ICE) ', |
558 |
|
|
& AQH(I,J,bi,bj),qhice(I,J) |
559 |
ifenty |
1.16 |
print '(A,4(1x,D24.15))', |
560 |
|
|
& 'ibi F(lwd,swi,lwu) ', |
561 |
jmc |
1.21 |
& -lwdownLoc(I,J), -absorbedSW(I,J), F_lwu(I,J) |
562 |
ifenty |
1.16 |
print '(A,4(1x,D24.15))', |
563 |
|
|
& 'ibi F(c,lh,sens) ', |
564 |
|
|
& F_c(I,J), F_lh(I,J), F_sens(I,J) |
565 |
|
|
#ifdef SEAICE_ADD_SUBLIMATION_TO_FWBUDGET |
566 |
|
|
IF (F_lh_max(I,J) .GT. ZERO) THEN |
567 |
|
|
print '(A,4(1x,D24.15))', |
568 |
|
|
& 'ibi F_lh_max, F_lh/lhmax) ', |
569 |
|
|
& F_lh_max(I,J), F_lh(I,J)/ F_lh_max(I,J) |
570 |
jmc |
1.19 |
ELSE |
571 |
ifenty |
1.16 |
print '(A,4(1x,D24.15))', |
572 |
|
|
& 'ibi F_lh_max = ZERO! ' |
573 |
|
|
ENDIF |
574 |
|
|
print '(A,4(1x,D24.15))', |
575 |
|
|
& 'ibi FWsub, FWsubm*dT/rhoI ', |
576 |
|
|
& FWsublim(I,J), |
577 |
|
|
& FWsublim(I,J)*SEAICE_deltaTtherm/SEAICE_rhoICE |
578 |
jmc |
1.21 |
#endif /* SEAICE_ADD_SUBLIMATION_TO_FWBUDGET */ |
579 |
mlosch |
1.5 |
print '(A,4(1x,D24.15))', |
580 |
|
|
& 'ibi F_ia, F_ia_net, F_c ', |
581 |
jmc |
1.25 |
& F_ia(I,J), F_ia_net, F_c(I,J) |
582 |
mlosch |
1.5 |
print '(A)','----------------------------------------' |
583 |
|
|
ENDIF |
584 |
jmc |
1.2 |
#endif /* SEAICE_DEBUG */ |
585 |
jmc |
1.6 |
|
586 |
mlosch |
1.5 |
ENDIF !/* iceOrNot */ |
587 |
|
|
ENDDO !/* i */ |
588 |
jmc |
1.1 |
ENDDO !/* j */ |
589 |
|
|
|
590 |
jmc |
1.19 |
#endif /* ALLOW_ATM_TEMP && ALLOW_DOWNWARD_RADIATION */ |
591 |
|
|
RETURN |
592 |
jmc |
1.1 |
END |