1 | ##General options |
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2 | ##~~~~~~~~~~~~~~~ |
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3 | #Directory where external input files are: |
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4 | datadir=./datadir |
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5 | |
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6 | #Run with or without tracer transport ? |
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7 | tracer=.true. |
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8 | |
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9 | #Diurnal cycle ? if diurnal=False, diurnal averaged solar heating |
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10 | diurnal=.true. |
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11 | |
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12 | #Seasonal cycle ? if season=False, Ls stays constant, to value set in "start" |
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13 | season = .true. |
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14 | |
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15 | #write some more output on the screen ? |
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16 | lwrite = .false. |
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17 | |
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18 | #Save statistics in file "stats.nc" ? |
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19 | callstats =.true. |
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20 | |
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21 | #Save EOF profiles in file "profiles" for Climate Database? |
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22 | calleofdump = .false. |
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23 | |
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24 | # check input fields when entering physics? |
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25 | check_physics_inputs=.false. |
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26 | # check fields at the end of physics? |
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27 | check_physics_outputs=.false. |
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28 | |
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29 | ## Dust scenario. Used to prescribe the dust |
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30 | ## ~~~~~~~~~~~~~ |
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31 | # =1 Dust opt.deph read in startfi; =2 Viking scenario; =3 MGS scenario, |
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32 | # =4 Mars Year 24 from TES assimilation (old version of MY24; dust_tes.nc file) |
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33 | # =6 "cold" (low dust) scenario ; =7 "warm" (high dust) scenario |
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34 | # =8 "climatology" (our best guess of a typical Mars year) scenario |
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35 | # =24 Mars Year 24 from TES assimilation (ie: MCD reference case) |
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36 | # =25 Mars Year 25 from TES assimilation (ie: a year with a global dust storm) |
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37 | # =26 Mars Year 26 from TES assimilation |
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38 | # ... |
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39 | # =35 Mars Year 35 from observers assimilation |
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40 | iaervar = 8 |
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41 | # Dust opacity at 610 Pa (when constant, i.e. for the iaervar=1 case) |
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42 | tauvis=0.2 |
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43 | # Dust vertical distribution: |
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44 | # (=0: old distrib. (Pollack90), =1: top set by "topdustref", |
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45 | # =2: Viking scenario; =3 MGS scenario) |
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46 | iddist = 3 |
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47 | # Dust top altitude (km). (Matters only if iddist=1) |
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48 | topdustref = 55. |
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49 | # Dust IR opacity ref. wavelength (for dso diagnostics only) |
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50 | # "tes" (9.3 microns) [default] or "mcs" (21.6 microns) |
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51 | dustiropacity = tes |
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52 | # Use an IR to VIS scenario conversion coefficient that is |
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53 | # dependent on the GCM dust effective radius, |
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54 | # instead of a fixed 2.6 coefficient ? |
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55 | #(only if dustiropacity = tes ; default = .false.) |
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56 | reff_driven_IRtoVIS_scenario = .true. |
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57 | |
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58 | ## Physical Parameterizations : |
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59 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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60 | # call radiative transfer ? |
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61 | callrad = .true. |
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62 | # call NLTE radiative schemes ? matters only if callrad=T |
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63 | callnlte = .true. |
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64 | # NLTE 15um scheme to use. |
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65 | # 0-> Old scheme, static oxygen |
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66 | # 1-> Old scheme, dynamic oxygen |
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67 | # 2-> New scheme |
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68 | nltemodel = 2 |
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69 | # call CO2 NIR absorption ? matters only if callrad=T |
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70 | callnirco2 = .true. |
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71 | # NIR NLTE correction ? matters only if callnirco2=T |
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72 | nircorr=0 |
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73 | # call turbulent vertical diffusion ? |
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74 | calldifv = .true. |
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75 | # call convective adjustment ? |
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76 | calladj = .true. |
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77 | # Thermals |
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78 | calltherm = .true. |
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79 | callrichsl = .true. |
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80 | # call CO2 condensation ? |
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81 | callcond =.true. |
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82 | # call thermal conduction in the soil ? |
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83 | callsoil = .true. |
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84 | |
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85 | ##Gravity Waves |
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86 | # call Lott's gravity wave/subgrid topography scheme ? |
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87 | calllott = .true. |
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88 | # call Lott's non-orographic gravity waves scheme? |
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89 | calllott_nonoro=.true. |
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90 | #Eliassen-Palm FLux(only if calllott_nonoro=.true.) |
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91 | nonoro_gwd_epflux_max=5.E-4 |
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92 | # saturation parameter non-orographic gravity waves(only if calllott_nonoro=.true.) |
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93 | nonoro_gwd_sat=1.5 |
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94 | # value of the dissaption coefficiet(only if calllott_nonoro=.true.) |
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95 | nonoro_gwd_rdiss=0.15 |
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96 | # value of the max wave number |
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97 | nonoro_gwd_kmax=1.E-4 |
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98 | # value of the min wave number |
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99 | nonoro_gwd_kmin=7.E-6 |
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100 | # value to control the launch altitude |
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101 | nonoro_gwd_xlaunch=0.6 |
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102 | |
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103 | # Impose polar cap surface albedos as observed by TES? |
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104 | TESicealbedo = .true. |
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105 | ## Coefficient for Northern cap albedoes |
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106 | TESice_Ncoef=1.6 |
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107 | ## Coefficient for Southern cap albedoes |
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108 | TESice_Scoef=1.6 |
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109 | |
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110 | |
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111 | ## Radiative transfer options : |
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112 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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113 | # the rad.transfer is computed every "iradia" physical timestep |
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114 | iradia = 1 |
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115 | # Output of the exchange coefficient mattrix ? for diagnostic only |
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116 | callg2d = .false. |
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117 | # Rayleigh scattering : (should be .false. for now) |
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118 | rayleigh = .false. |
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119 | |
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120 | ## Tracer (dust water, ice and/or chemical species) options (used if tracer=T): |
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121 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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122 | # DUST: Transported dust ? (if >0, use 'dustbin' dust bins) |
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123 | dustbin = 2 |
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124 | # DUST: Radiatively active dust ? (matters if dustbin>0) |
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125 | active = .true. |
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126 | # DUST: use mass and number mixing ratios to predict dust size ? |
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127 | doubleq = .true. |
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128 | # DUST: use a small population of dust particules (submicron dust)? |
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129 | submicron = .false. |
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130 | # DUST: lifted by GCM surface winds ? |
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131 | lifting = .true. |
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132 | # DUST: lifted by dust devils ? |
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133 | callddevil = .false. |
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134 | # DUST: Scavenging by H2O snowfall ? |
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135 | scavenging = .true. |
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136 | |
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137 | # DUST: freedust ? |
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138 | freedust=.true. |
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139 | # DUST: dustscaling_mode? |
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140 | # =0 --> freedust, tauscaling=1 |
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141 | # =1 --> GCM5.3-like, tauscaling |
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142 | # =2 --> tauscaling=1,dust_rad_adjust |
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143 | dustscaling_mode=2 |
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144 | # DUST: dust injection scheme (if >0, use 'dustinjection') |
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145 | dustinjection=1 |
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146 | # DUST: dust injection scheme coefficient (default=1.) |
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147 | coeff_injection=0.25 |
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148 | # DUST: dust injection scheme initial local time (def : 10.) |
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149 | ti_injection=0. |
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150 | # DUST: dust injection scheme final local time (def : 12.) |
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151 | tf_injection=24. |
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152 | # DUST: Rocket Dust Storm scheme |
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153 | rdstorm=.true. |
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154 | # DUST: RDS detrainment coefficient (def : 0.05) |
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155 | coeff_detrainment=0.02 |
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156 | # DUST: Dust entrainment by subgrid-scale slope winds |
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157 | topflows=.true. |
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158 | |
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159 | # DUST/WATERICE: Scavenging by CO2 condensation? |
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160 | scavco2cond = .true. |
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161 | # DUST/WATERICE: Gravitationnal sedimentation ? |
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162 | sedimentation = .true. |
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163 | |
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164 | # WATERICE: Radiatively active transported atmospheric water ice ? |
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165 | activice = .true. |
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166 | # WATER: Compute water cycle |
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167 | water = .true. |
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168 | # WATER: Microphysical scheme for water-ice clouds? |
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169 | microphys = .true. |
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170 | # WATER: Effective variance for sedimentation for the log-normal |
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171 | # distribution of ice particles ? |
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172 | nuice_sed=0.1 |
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173 | # WATER: contact parameter (only if temp_dependant_m = .false.) |
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174 | ##mteta = 0.95 |
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175 | # Temperature-dependant water contact parameter |
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176 | temp_dependant_m = .true. |
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177 | # WATER: current permanent caps at both poles. True IS RECOMMENDED |
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178 | # (with .true., North cap is a source of water and South pole |
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179 | # is a cold trap) |
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180 | caps = .true. |
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181 | # WATER: Water ice albedos (old ice/fresh frost)? |
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182 | # Perennial ice albedo |
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183 | albedo_h2o_ice = 0.30 |
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184 | # Account for fresh frost ice albedo if cst_cap_albedo = .false. |
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185 | cst_cap_albedo = .false. |
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186 | # Fresh frost albedo (only used if cst_cap_albedo = .false.) |
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187 | albedo_h2o_frost = 0.35 |
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188 | # Frost thickness threshold for albedo |
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189 | frost_albedo_threshold = 0.005 |
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190 | # Frost metamorphism into old ice |
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191 | refill_watercap = .true. |
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192 | frost_metam_threshold = 0.05 |
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193 | # WATER: Water ice thermal inertia (old ice and fresh frost) |
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194 | inert_h2o_ice = 800 |
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195 | # Sublimation latent heat (def = T) |
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196 | latentheat_surfwater = .true. |
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197 | #WATER: subgrid clouds |
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198 | CLFvarying=.false. |
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199 | #WATER: subgrid clouds |
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200 | CLFfixval=1 |
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201 | |
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202 | # PHOTOCHEMISTRY: include chemical species |
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203 | photochem = .true. |
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204 | |
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205 | # SCATTERERS: set number of scatterers. must be compliant with preceding options. |
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206 | naerkind = 4 |
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207 | |
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208 | |
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209 | ## Thermospheric options (relevant if tracer=T) : |
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210 | ##~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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211 | # call thermosphere ? |
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212 | callthermos = .true. |
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213 | # WATER: included without cycle (only if water=.false.) |
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214 | thermoswater = .false. |
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215 | # call thermal conduction ? (only if callthermos=.true.) |
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216 | callconduct = .true |
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217 | # call molecular viscosity ? (only if callthermos=.true.) |
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218 | callmolvis = .true. |
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219 | # call molecular diffusion ? (only if callthermos=.true.) |
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220 | callmoldiff = .true. |
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221 | # call thermospheric photochemistry ? (only if callthermos=.true.) |
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222 | thermochem = .true. |
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223 | # call EUV heating ? (only if callthermos=.true.) |
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224 | calleuv=.true. |
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225 | #Method to include solar variability? |
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226 | #0-> Fixed EUV input 1-> Variability with E10.7 as observed |
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227 | solvarmod=0 |
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228 | # fixed E10.7 value (for solvarmod=0) |
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229 | # (min=80 , ave=140, max=320) |
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230 | fixed_euv_value=140 |
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231 | #Solar variability as observed for MY? (must be between MY23 and MY32) |
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232 | # (only matters if solvarmod=1) |
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233 | solvaryear=24 |
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234 | # value for the UV heating efficiency |
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235 | ##(experimental values between 0.19 and 0.23, lower values may |
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236 | ## be used to compensate for low 15 um cooling) |
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237 | euveff = 0.21 |
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238 | |
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239 | |
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