[2807] | 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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[3369] | 6 | # Number of outputs per sol for diagfi.nc files |
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| 7 | outputs_per_sol=8 |
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| 8 | |
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[2807] | 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 | #Save statistics in file "stats.nc" ? |
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| 16 | callstats =.true. |
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| 17 | |
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| 18 | #Save EOF profiles in file "profiles" for Climate Database? |
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| 19 | calleofdump = .false. |
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| 20 | |
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| 21 | # check input fields when entering physics? |
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| 22 | check_physics_inputs=.false. |
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| 23 | # check fields at the end of physics? |
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| 24 | check_physics_outputs=.false. |
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| 25 | |
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| 26 | ## Dust scenario. Used to prescribe the dust |
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| 27 | ## ~~~~~~~~~~~~~ |
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| 28 | # =1 Dust opt.deph read in startfi; =2 Viking scenario; =3 MGS scenario, |
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| 29 | # =4 Mars Year 24 from TES assimilation (old version of MY24; dust_tes.nc file) |
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| 30 | # =6 "cold" (low dust) scenario ; =7 "warm" (high dust) scenario |
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| 31 | # =8 "climatology" (our best guess of a typical Mars year) scenario |
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| 32 | # =24 Mars Year 24 from TES assimilation (ie: MCD reference case) |
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| 33 | # =25 Mars Year 25 from TES assimilation (ie: a year with a global dust storm) |
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| 34 | # =26 Mars Year 26 from TES assimilation |
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| 35 | # ... |
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| 36 | # =35 Mars Year 35 from observers assimilation |
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| 37 | iaervar = 8 |
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| 38 | # Dust opacity at 610 Pa (when constant, i.e. for the iaervar=1 case) |
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| 39 | tauvis=0.2 |
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| 40 | # Dust vertical distribution: |
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| 41 | # (=0: old distrib. (Pollack90), =1: top set by "topdustref", |
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| 42 | # =2: Viking scenario; =3 MGS scenario) |
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| 43 | iddist = 3 |
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| 44 | # Dust top altitude (km). (Matters only if iddist=1) |
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| 45 | topdustref = 55. |
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| 46 | # Dust IR opacity ref. wavelength (for dso diagnostics only) |
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| 47 | # "tes" (9.3 microns) [default] or "mcs" (21.6 microns) |
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| 48 | dustiropacity = tes |
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| 49 | # Use an IR to VIS scenario conversion coefficient that is |
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| 50 | # dependent on the GCM dust effective radius, |
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| 51 | # instead of a fixed 2.6 coefficient ? |
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| 52 | #(only if dustiropacity = tes ; default = .false.) |
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| 53 | reff_driven_IRtoVIS_scenario = .true. |
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| 54 | |
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| 55 | ## Physical Parameterizations : |
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| 56 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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| 57 | # call radiative transfer ? |
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| 58 | callrad = .true. |
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| 59 | # call NLTE radiative schemes ? matters only if callrad=T |
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| 60 | callnlte = .true. |
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| 61 | # NLTE 15um scheme to use. |
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| 62 | # 0-> Old scheme, static oxygen |
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| 63 | # 1-> Old scheme, dynamic oxygen |
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| 64 | # 2-> New scheme |
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| 65 | nltemodel = 2 |
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| 66 | # call CO2 NIR absorption ? matters only if callrad=T |
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| 67 | callnirco2 = .true. |
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| 68 | # NIR NLTE correction ? matters only if callnirco2=T |
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| 69 | nircorr=0 |
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| 70 | # call turbulent vertical diffusion ? |
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| 71 | calldifv = .true. |
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| 72 | # call convective adjustment ? |
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| 73 | calladj = .true. |
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| 74 | # Thermals |
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| 75 | calltherm = .true. |
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| 76 | callrichsl = .true. |
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| 77 | # call CO2 condensation ? |
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| 78 | callcond =.true. |
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| 79 | # call thermal conduction in the soil ? |
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| 80 | callsoil = .true. |
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| 81 | |
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| 82 | ##Gravity Waves |
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| 83 | # call Lott's gravity wave/subgrid topography scheme ? |
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| 84 | calllott = .true. |
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| 85 | # call Lott's non-orographic gravity waves scheme? |
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| 86 | calllott_nonoro=.true. |
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| 87 | #Eliassen-Palm FLux(only if calllott_nonoro=.true.) |
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| 88 | nonoro_gwd_epflux_max=5.E-4 |
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| 89 | # saturation parameter non-orographic gravity waves(only if calllott_nonoro=.true.) |
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| 90 | nonoro_gwd_sat=1.5 |
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| 91 | # value of the dissaption coefficiet(only if calllott_nonoro=.true.) |
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| 92 | nonoro_gwd_rdiss=0.15 |
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| 93 | # value of the max wave number |
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| 94 | nonoro_gwd_kmax=1.E-4 |
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| 95 | # value of the min wave number |
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| 96 | nonoro_gwd_kmin=7.E-6 |
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| 97 | # value to control the launch altitude |
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| 98 | nonoro_gwd_xlaunch=0.6 |
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| 99 | |
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| 100 | # Impose polar cap surface albedos as observed by TES? |
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| 101 | TESicealbedo = .true. |
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| 102 | ## Coefficient for Northern cap albedoes |
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| 103 | TESice_Ncoef=1.6 |
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| 104 | ## Coefficient for Southern cap albedoes |
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| 105 | TESice_Scoef=1.6 |
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| 106 | |
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| 107 | |
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| 108 | ## Radiative transfer options : |
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| 109 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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| 110 | # the rad.transfer is computed every "iradia" physical timestep |
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| 111 | iradia = 1 |
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| 112 | # Output of the exchange coefficient mattrix ? for diagnostic only |
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| 113 | callg2d = .false. |
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| 114 | # Rayleigh scattering : (should be .false. for now) |
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| 115 | rayleigh = .false. |
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| 116 | |
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[3448] | 117 | ## Tracer (dust water, ice and/or chemical species) options : |
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| 118 | ## ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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[2807] | 119 | # DUST: Transported dust ? (if >0, use 'dustbin' dust bins) |
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| 120 | dustbin = 2 |
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| 121 | # DUST: Radiatively active dust ? (matters if dustbin>0) |
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| 122 | active = .true. |
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| 123 | # DUST: use mass and number mixing ratios to predict dust size ? |
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| 124 | doubleq = .true. |
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| 125 | # DUST: use a small population of dust particules (submicron dust)? |
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| 126 | submicron = .false. |
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| 127 | # DUST: lifted by GCM surface winds ? |
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| 128 | lifting = .true. |
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| 129 | # DUST: lifted by dust devils ? |
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| 130 | callddevil = .false. |
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| 131 | # DUST: Scavenging by H2O snowfall ? |
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| 132 | scavenging = .true. |
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| 133 | |
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| 134 | # DUST: freedust ? |
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| 135 | freedust=.true. |
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| 136 | # DUST: dustscaling_mode? |
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| 137 | # =0 --> freedust, tauscaling=1 |
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| 138 | # =1 --> GCM5.3-like, tauscaling |
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| 139 | # =2 --> tauscaling=1,dust_rad_adjust |
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| 140 | dustscaling_mode=2 |
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| 141 | # DUST: dust injection scheme (if >0, use 'dustinjection') |
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| 142 | dustinjection=1 |
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[3192] | 143 | # DUST: dust injection scheme coefficient (default = 0.25) |
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[2807] | 144 | coeff_injection=0.25 |
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[3192] | 145 | # DUST: dust injection scheme initial local time (default = 0.) |
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[2807] | 146 | ti_injection=0. |
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[3192] | 147 | # DUST: dust injection scheme final local time (default = 24.) |
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[2807] | 148 | tf_injection=24. |
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| 149 | # DUST: Rocket Dust Storm scheme |
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| 150 | rdstorm=.true. |
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[3192] | 151 | # DUST: RDS detrainment coefficient (default = 0.02) |
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[2807] | 152 | coeff_detrainment=0.02 |
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| 153 | # DUST: Dust entrainment by subgrid-scale slope winds |
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| 154 | topflows=.true. |
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| 155 | |
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| 156 | # DUST/WATERICE: Scavenging by CO2 condensation? |
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| 157 | scavco2cond = .true. |
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| 158 | # DUST/WATERICE: Gravitationnal sedimentation ? |
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| 159 | sedimentation = .true. |
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| 160 | |
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| 161 | # WATERICE: Radiatively active transported atmospheric water ice ? |
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| 162 | activice = .true. |
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| 163 | # WATER: Compute water cycle |
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| 164 | water = .true. |
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| 165 | # WATER: Microphysical scheme for water-ice clouds? |
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| 166 | microphys = .true. |
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| 167 | # WATER: Effective variance for sedimentation for the log-normal |
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| 168 | # distribution of ice particles ? |
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| 169 | nuice_sed=0.1 |
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[3064] | 170 | # WATER: contact parameter (only if temp_dependent_m = .false.) |
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[2807] | 171 | ##mteta = 0.95 |
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[3064] | 172 | # Temperature-dependent water contact parameter |
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| 173 | temp_dependent_m = .true. |
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[2807] | 174 | # WATER: current permanent caps at both poles. True IS RECOMMENDED |
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| 175 | # (with .true., North cap is a source of water and South pole |
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| 176 | # is a cold trap) |
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| 177 | caps = .true. |
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| 178 | # WATER: Water ice albedos (old ice/fresh frost)? |
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| 179 | # Perennial ice albedo |
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| 180 | albedo_h2o_ice = 0.30 |
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| 181 | # Account for fresh frost ice albedo if cst_cap_albedo = .false. |
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| 182 | cst_cap_albedo = .false. |
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| 183 | # Fresh frost albedo (only used if cst_cap_albedo = .false.) |
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| 184 | albedo_h2o_frost = 0.35 |
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| 185 | # Frost thickness threshold for albedo |
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| 186 | frost_albedo_threshold = 0.005 |
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| 187 | # Frost metamorphism into old ice |
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[3058] | 188 | refill_watercap = .false. |
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[2807] | 189 | frost_metam_threshold = 0.05 |
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| 190 | # WATER: Water ice thermal inertia (old ice and fresh frost) |
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| 191 | inert_h2o_ice = 800 |
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| 192 | # Sublimation latent heat (def = T) |
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| 193 | latentheat_surfwater = .true. |
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| 194 | #WATER: subgrid clouds |
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| 195 | CLFvarying=.false. |
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| 196 | #WATER: subgrid clouds |
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| 197 | CLFfixval=1 |
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| 198 | |
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| 199 | # PHOTOCHEMISTRY: include chemical species |
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| 200 | photochem = .true. |
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| 201 | |
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| 202 | # SCATTERERS: set number of scatterers. must be compliant with preceding options. |
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| 203 | naerkind = 4 |
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| 204 | |
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| 205 | |
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[3448] | 206 | ## Thermospheric options : |
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| 207 | ##~~~~~~~~~~~~~~~~~~~~~~ |
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[2807] | 208 | # call thermosphere ? |
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| 209 | callthermos = .true. |
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| 210 | # WATER: included without cycle (only if water=.false.) |
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| 211 | thermoswater = .false. |
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| 212 | # call thermal conduction ? (only if callthermos=.true.) |
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| 213 | callconduct = .true |
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| 214 | # call molecular viscosity ? (only if callthermos=.true.) |
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| 215 | callmolvis = .true. |
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| 216 | # call molecular diffusion ? (only if callthermos=.true.) |
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| 217 | callmoldiff = .true. |
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| 218 | # call thermospheric photochemistry ? (only if callthermos=.true.) |
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| 219 | thermochem = .true. |
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| 220 | # call EUV heating ? (only if callthermos=.true.) |
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| 221 | calleuv=.true. |
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| 222 | #Method to include solar variability? |
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| 223 | #0-> Fixed EUV input 1-> Variability with E10.7 as observed |
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| 224 | solvarmod=0 |
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| 225 | # fixed E10.7 value (for solvarmod=0) |
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| 226 | # (min=80 , ave=140, max=320) |
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| 227 | fixed_euv_value=140 |
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| 228 | #Solar variability as observed for MY? (must be between MY23 and MY32) |
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| 229 | # (only matters if solvarmod=1) |
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| 230 | solvaryear=24 |
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| 231 | # value for the UV heating efficiency |
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| 232 | ##(experimental values between 0.19 and 0.23, lower values may |
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| 233 | ## be used to compensate for low 15 um cooling) |
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| 234 | euveff = 0.21 |
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| 235 | |
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| 236 | |
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