1 | ## Datagcm path |
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2 | datadir=datadir |
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3 | ## Orbit / general options |
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4 | ## ~~~~~~~~~~~~~~~~~~~~~~~ |
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5 | # Run with or without tracer transport ? |
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6 | tracer = .true. |
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7 | # Diurnal cycle ? if diurnal=false, diurnally averaged solar heating |
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8 | diurnal = .false. |
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9 | # Seasonal cycle ? if season=false, Ls stays constant, to value set in "start" |
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10 | season = .false. |
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11 | noseason_day = 1550 |
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12 | # Fixed zenith angle in 1D |
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13 | global1d = .true. |
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14 | # Run 1D or 3D version (false) / fast version volatile transport (true) |
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15 | fast = .false. |
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16 | # Write some more output on the screen ? |
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17 | lwrite = .false. |
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18 | # Save statistics in file "stats.nc" ? |
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19 | callstats = .false. |
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20 | # Test energy conservation of model physics ? |
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21 | enertest = .false. |
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22 | # run with triton orbit ? |
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23 | triton = .false. |
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24 | # conservation n2 |
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25 | conservn2= .false. |
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26 | # check if cpp and mugaz from start.nc are consistent with values computed by comp_cpp_mugaz with gases.def |
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27 | check_cpp_match = .true. |
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28 | check_physics_inputs = .true. |
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29 | check_physics_outputs = .true. |
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30 | check_ps_min = 0.01 |
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31 | |
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32 | ## Radiative transfer options |
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33 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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34 | # call radiative transfer? |
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35 | callrad = .true. |
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36 | # the rad. transfer is computed every "iradia" physical timestep |
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37 | iradia = 1 |
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38 | # call multilayer correlated-k radiative transfer ? |
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39 | corrk = .true. |
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40 | oldplutocorrk=.true. |
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41 | ch4fix = .true. |
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42 | vmrch4fix = 0.5 |
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43 | nlte=.true. |
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44 | strobel=.false. |
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45 | cooling=.true. |
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46 | pref=.05 |
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47 | alpha_top = 1e-11 |
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48 | deltap = 0.7 |
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49 | # folder in which correlated-k data is stored ? |
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50 | corrkdir = pluton_ch4var_COfix |
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51 | # strictboundcorrk |
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52 | strictboundcorrk = .false. |
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53 | tplanckmin = 30 |
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54 | dtplanck=0.1 |
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55 | # call visible gaseous absorption in radiative transfer ? |
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56 | callgasvis = .true. |
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57 | # call continuum in radiative transfer ? |
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58 | continuum = .false. |
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59 | # Include Rayleigh scattering in the visible ? |
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60 | rayleigh = .false. |
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61 | # Test physics timescale in 1D ? |
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62 | testradtimes = .false. |
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63 | # Output spectral OLR in 1D/3D? |
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64 | specOLR = .true. |
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65 | # Output global radiative balance in file 'rad_bal.out' - slow for 1D!! |
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66 | meanOLR = .false. |
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67 | # Variable gas species: Radiatively active ? |
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68 | varactive = .true. |
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69 | # Variable gas species: Fixed vertical distribution ? |
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70 | # (not to be used in time integration mode) |
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71 | varfixed = .false. |
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72 | # Use fixed vertical profile, 1 step, no iteration ? |
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73 | kastprof = .false. |
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74 | |
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75 | # Star type (inherited from generic model) |
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76 | startype = 1 |
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77 | Fat1AU = 1366.0 |
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78 | |
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79 | |
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80 | ## Other physics options |
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81 | ## ~~~~~~~~~~~~~~~~~~~~~ |
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82 | # call turbulent vertical diffusion ? |
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83 | calldifv = .true. |
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84 | kmixmin=0.001 |
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85 | vertdiff=.true. |
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86 | # use turbdiff instead of vdifc ? (if oldplutovdifc = .false.) |
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87 | UseTurbDiff = .true. |
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88 | oldplutovdifc=.true. |
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89 | # call convective adjustment ? |
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90 | calladj = .true. |
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91 | # call thermal conduction in the soil ? |
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92 | callsoil = .true. |
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93 | lay1_soil = 2e-4 |
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94 | # geothermal flux at the bottom layer |
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95 | fluxgeo = 0. |
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96 | # call thermal conduction |
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97 | callconduct=.false. |
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98 | # call molecular viscosity 3D only |
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99 | callmolvis=.false. |
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100 | # call molecular diffusion |
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101 | callmoldiff=.false. |
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102 | # flux qui arrive au-dessus de latmosphere |
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103 | phitop=0. |
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104 | |
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105 | |
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106 | ## Tracer and aerosol options |
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107 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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108 | # atm mass update due to tracer evaporation/condensation? |
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109 | mass_redistrib = .false. |
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110 | # Gravitational sedimentation of tracers ? |
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111 | sedimentation = .true. |
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112 | oldsedimpluto= .true. |
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113 | naerkind = 1 |
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114 | ## Condensation |
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115 | ## ~~~~~~~~~~~ |
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116 | generic_condensation = .false. |
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117 | # call N2 condensation ? |
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118 | n2cond = .false. |
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119 | # N2 condensation subtimestep ? |
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120 | nbcond = 20 |
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121 | # Set initial temperature profile to 1 K above N2 condensation everywhere? |
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122 | nearn2cond = .false. |
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123 | # Compute methane cycle ? |
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124 | methane = .true. |
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125 | condmetsurf = .false. |
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126 | # Compute CO cycle ? |
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127 | carbox = .true. |
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128 | condcosurf=.false. |
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129 | # Compute methane clouds ? |
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130 | metcloud = .false. |
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131 | # Compute CO clouds ? |
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132 | monoxcloud = .false. |
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133 | # Haze production ? |
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134 | haze = .true. |
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135 | hazeconservch4 = .true. |
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136 | # haze particule mean radius |
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137 | rad_haze = 10e-9 |
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138 | # number mixing ratio of haze particles for ch4 clouds |
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139 | Nmix_ch4 = 100000. |
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140 | # number mixing ratio of haze particles for co clouds |
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141 | Nmix_co = 100000. |
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142 | # Radiatively active haze ? |
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143 | aerohaze=.false. |
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144 | hazeprop_file=optprop_rannou_r2-200nm_nu003.dat |
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145 | # fractal particle ? |
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146 | fractal=.false. |
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147 | nb_monomer=10 |
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148 | # Fixed haze radius |
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149 | haze_radproffix = .false. |
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150 | hazerad_file = rad_haze.txt |
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151 | # Fixed haze distribution? # t== haze_prof (hazemmr_file) else hazecloud() |
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152 | haze_proffix = .false. |
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153 | hazemmr_file = hazemmr.txt |
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154 | hazedens_file = dens_haze.txt |
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155 | |
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156 | ## Surface properties |
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157 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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158 | mode_n2=0 ! 0=fixed, 1=change w thickness, 2=special for SP |
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159 | deltab=0. ! if mod_n2=1, difference of albedo depending of thickness |
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160 | metlateq=35 ! latitude separating dark/bright methane |
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161 | tholateq=25 ! latitude separating eq/pole tholins |
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162 | mode_ch4=1 |
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163 | specalb=.false. ! Specific treatment for tholins (diff values) |
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164 | |
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165 | alb_n2b=0.7 |
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166 | alb_n2a=0.7 |
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167 | alb_ch4=0.5 |
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168 | alb_ch4_eq=0.5 |
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169 | alb_ch4_s=0.5 |
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170 | alb_co=0.4 |
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171 | alb_tho=0.2 |
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172 | alb_tho_eq=0.2 |
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173 | |
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174 | emis_n2b=0.8 |
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175 | emis_n2a=0.8 |
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176 | emis_ch4=0.8 |
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177 | emis_co=0.8 |
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178 | emis_tho=0.8 |
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179 | emis_tho_eq=0.8 |
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180 | |
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181 | # Change TI with time |
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182 | changeti=.false. |
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183 | changetid=.false. |
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184 | ITCH4=800. |
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185 | ITN2=800 |
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186 | ITH2O=2000. |
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187 | |
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