| 1 | ## $Header$ |
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| 2 | # |
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| 3 | ## Planet: |
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| 4 | planet_type=venus |
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| 5 | # |
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| 6 | ## Number of dynamical steps per day (must be a multiple of iperiod) |
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| 7 | day_step=240000 |
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| 8 | ## Apply a Matsuno step every iperiod dynamical step |
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| 9 | iperiod=5 |
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| 10 | ## dissipation is applied every dissip_period dynamical steps |
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| 11 | ## DEFAULT: dissip_period=0 , meaning dissip_period is automatically computed |
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| 12 | ## (in practice it is =>25 in recent runs) |
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| 13 | dissip_period=5 |
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| 14 | ## dissipation operator to use (star or non-star) |
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| 15 | lstardis=y |
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| 16 | ## iterate lateral dissipation operator gradiv nitergdiv times |
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| 17 | nitergdiv=1 |
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| 18 | ## iterate lateral dissipation operator nxgradrot nitergrot times |
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| 19 | nitergrot=2 |
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| 20 | ## iterate lateral dissipation operator divgrad niterh times |
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| 21 | niterh=2 |
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| 22 | ## dissipation time scale (s) for shortest wavelengths for u,v (gradiv) |
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| 23 | tetagdiv=1.e4 |
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| 24 | ## dissipation time scale (s) for shortest wavelengths for u,v (nxgradrot) |
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| 25 | tetagrot=1.e4 |
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| 26 | ## dissipation time scale (s) for shortest wavelengths for u,v (divgrad) |
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| 27 | tetatemp=1.e4 |
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| 28 | ## coefficient for gamdissip |
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| 29 | coefdis=0. |
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| 30 | ## time marching scheme (Matsuno if purmats is y, else Matsuno-Leapfrog) |
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| 31 | purmats=n |
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| 32 | # run with (true) or without (false) physics |
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| 33 | physic=y |
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| 34 | ## Physics package type |
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| 35 | ## 0: no physics (e.g. Shallow Water mode) |
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| 36 | ## 1: with physics (e.g. phyvenus physics package) |
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| 37 | ## 2: with a netwonian relaxation scheme in the dynamics |
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| 38 | iflag_phys=1 |
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| 39 | ## run with or without initial condition files (start.nc, startphy.nc) ? |
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| 40 | ## (in the without case, initialization of fields is done via the iniacademic |
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| 41 | ## routine in the dynamics => not available for Venus |
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| 42 | read_start=y |
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| 43 | ## call physics every iphysiq dynamical steps |
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| 44 | iphysiq=5 |
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| 45 | ## runwith or without tracers |
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| 46 | iflag_trac=0 |
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| 47 | ## run with or without stratosphere // i.e. a sponge layer and secondary |
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| 48 | ## higher altitude level of horizontal dissipation |
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| 49 | ok_strato=y |
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| 50 | ## Horizontal dissipation multipliers along the vertical |
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| 51 | dissip_fac_mid=2. |
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| 52 | dissip_fac_up=50. |
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| 53 | # deltaz et hdelta in km |
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| 54 | dissip_deltaz=30. |
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| 55 | dissip_hdelta=5. |
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| 56 | # pupstart in Pa |
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| 57 | dissip_pupstart=1.e4 |
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| 58 | |
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| 59 | ## Sponge layer |
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| 60 | # 0: LMDZ.GENERIC style |
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| 61 | # 1 and 2: LMDZ.EARTH style |
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| 62 | # 1: in last 4 levels |
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| 63 | # 2: in levels with pressure less than 100 times the last layer pressure |
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| 64 | iflag_top_bound=0 |
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| 65 | |
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| 66 | ## sponge layer parameters LMDZ.EARTH style |
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| 67 | ## Mode |
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| 68 | # mode = 0 : no sponge |
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| 69 | # mode = 1 : u et v -> 0 |
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| 70 | # mode = 2 : u et v -> zonal average |
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| 71 | # mode = 3 : u, v et h -> zonale average |
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| 72 | mode_top_bound=3 |
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| 73 | # Coefficient for the sponge layer (value in topmost layer) |
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| 74 | tau_top_bound=1.e-4 |
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| 75 | |
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| 76 | # sponge layer parameters LMDZ.GENERIC style |
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| 77 | callsponge=y |
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| 78 | # mode_sponge ( 0: h -> h_mean , ucov -> 0 , vcov -> 0 |
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| 79 | # 1: h -> h_mean , ucov -> ucov_mean , vcov -> 0 |
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| 80 | # 2: h -> h_mean , ucov -> ucov_mean , vcov -> vcov_mean ) |
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| 81 | mode_sponge=2 |
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| 82 | # nsponge: number of topmost atmospheric layers over which extends the sponge |
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| 83 | nsponge=10 |
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| 84 | # tetasponge characteristic time scale (seconds) at topmost layer |
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| 85 | # (time scale then doubles with decreasing layer index) |
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| 86 | tetasponge=1.e4 |
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| 87 | |
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| 88 | ############################################### |
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| 89 | ### Zoom parameters |
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| 90 | ############################################### |
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| 91 | ## longitude (degrees) of zoom center |
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| 92 | clon=0. |
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| 93 | ## latitude (degrees) of zoom center |
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| 94 | clat=0. |
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| 95 | ## enhancement factor of zoom, along longitudes |
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| 96 | grossismx=1.0 |
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| 97 | ## enhancement factor of zoom, along latitudes |
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| 98 | grossismy=1.0 |
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| 99 | ## Use an hyperbolic function f(y) if .true., else use a sine |
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| 100 | fxyhypb=y |
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| 101 | ## extention along longitudes of zoom region (fraction of global domain) |
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| 102 | dzoomx=0.0 |
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| 103 | ## extention along latitudes of zoom region (fraction of global domain) |
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| 104 | dzoomy=0.0 |
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| 105 | ## zoom stiffness along longitudes |
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| 106 | taux=3. |
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| 107 | ## zoom stiffness along latitudes |
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| 108 | tauy=3. |
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| 109 | ## Fonction f(y) as y = Sin(latitude) if = .true. , else y = latitude |
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| 110 | ysinus=y |
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