| 1 | MODULE soil_therm_inertia |
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| 2 | !----------------------------------------------------------------------- |
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| 3 | ! NAME |
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| 4 | ! soil_therm_inertia |
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| 5 | ! |
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| 6 | ! DESCRIPTION |
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| 7 | ! Compute and update soil thermal properties based on ice content, |
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| 8 | ! pressure, and cementation state. |
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| 9 | ! |
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| 10 | ! AUTHORS & DATE |
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| 11 | ! L. Lange, 2023 |
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| 12 | ! JB Clement, 2025 |
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| 13 | ! |
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| 14 | ! NOTES |
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| 15 | ! |
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| 16 | !----------------------------------------------------------------------- |
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| 17 | |
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| 18 | ! DEPENDENCIES |
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| 19 | ! ------------ |
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| 20 | use numerics, only: dp, di, k4, minieps |
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| 21 | |
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| 22 | ! DECLARATION |
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| 23 | ! ----------- |
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| 24 | implicit none |
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| 25 | |
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| 26 | ! PARAMETERS |
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| 27 | ! ---------- |
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| 28 | real(dp), parameter :: TI_regolith_avg = 250._dp ! Average of observed thermal inertia for regolith [SI], Mellon et al. 2000 |
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| 29 | real(dp), parameter :: TI_breccia = 750._dp ! Thermal inertia for breccia [SI], Mellon et al. 2000; Wood et al. 2008 |
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| 30 | real(dp), parameter :: TI_bedrock = 2300._dp ! Thermal inertia for bedrock [SI], Mellon et al. 2000; Wood et al. 2008 |
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| 31 | real(dp), parameter, private :: P610 = 610._dp ! Reference mean surface pressure [Pa] |
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| 32 | real(dp), parameter, private :: reg_inertie_thresold = 370._dp ! Above this thermal inertia, the regolith has too much cementation to be dependant on the pressure [J/m^2/K/s^1/2] |
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| 33 | real(dp), parameter, private :: reg_inertie_minvalue = 50._dp ! Minimum value of the Thermal Inertia at low pressure (Piqueux & Christensen 2009) [J/m^2/K/s^1/2] |
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| 34 | real(dp), parameter, private :: reg_inertie_maxvalue = 370._dp ! Maximum value of the Thermal Inertia at low pressure (Piqueux & Christensen 2009) [J/m^2/K/s^1/2] |
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| 35 | real(dp), parameter, private :: C = 0.0015_dp ! Constant to derive TI as a function of P, from Presley and Christensen 1997 [unitless] |
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| 36 | real(dp), parameter, private :: K = 8.1*1e4_dp ! Constant to derive TI as a function of P, from Presley and Christensen 1997 [Torr, or 133.3Pa] |
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| 37 | real(dp), parameter, private :: Pa2Torr = 1./133.3_dp ! Conversion from Pa to tor [Pa/Torr] |
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| 38 | |
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| 39 | contains |
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| 40 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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| 41 | |
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| 42 | !======================================================================= |
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| 43 | SUBROUTINE get_ice_TI(ispureice,pore_filling,surf_thermalinertia,ice_thermalinertia) |
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| 44 | !----------------------------------------------------------------------- |
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| 45 | ! NAME |
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| 46 | ! get_ice_TI |
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| 47 | ! |
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| 48 | ! DESCRIPTION |
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| 49 | ! Compute ice thermal properties based on pore filling and purity. |
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| 50 | ! |
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| 51 | ! AUTHORS & DATE |
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| 52 | ! L. Lange, 2023 |
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| 53 | ! JB Clement, 2025 |
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| 54 | ! |
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| 55 | ! NOTES |
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| 56 | ! Uses Siegler et al. (2012) formula for pore-filling ice; |
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| 57 | ! uses Mellon et al. (2004) value for pure water ice. |
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| 58 | !----------------------------------------------------------------------- |
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| 59 | |
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| 60 | ! DEPENDENCIES |
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| 61 | ! ------------ |
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| 62 | use soil, only: regolith_porosity |
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| 63 | |
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| 64 | ! DECLARATION |
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| 65 | ! ----------- |
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| 66 | implicit none |
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| 67 | |
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| 68 | ! ARGUMENTS |
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| 69 | ! --------- |
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| 70 | logical(k4), intent(in) :: ispureice ! Boolean to check if ice is massive or just pore filling |
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| 71 | real(dp), intent(in) :: pore_filling ! ice pore filling in each layer (1) |
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| 72 | real(dp), intent(in) :: surf_thermalinertia ! surface thermal inertia (J/m^2/K/s^1/2) |
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| 73 | real(dp), intent(out) :: ice_thermalinertia ! Thermal inertia of ice when present in the pore (J/m^2/K/s^1/2) |
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| 74 | |
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| 75 | ! LOCAL VARIABLES |
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| 76 | ! --------------- |
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| 77 | real(dp) :: inertie_purewaterice = 2100._dp ! 2050 is better according to my computations with the formula from Siegler et al., 2012, but let's follow Mellon et al. (2004) |
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| 78 | |
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| 79 | ! CODE |
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| 80 | ! ---- |
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| 81 | if (ispureice) then |
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| 82 | ice_thermalinertia = inertie_purewaterice |
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| 83 | else |
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| 84 | ice_thermalinertia = sqrt(surf_thermalinertia**2 + regolith_porosity*pore_filling*inertie_purewaterice**2) ! Siegler et al., 2012 |
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| 85 | end if |
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| 86 | |
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| 87 | END SUBROUTINE get_ice_TI |
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| 88 | !======================================================================= |
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| 89 | |
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| 90 | !======================================================================= |
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| 91 | SUBROUTINE update_soil_TI(h2o_ice,p_avg_new,icetable_depth,icetable_thickness,ice_porefilling,icetable_equilibrium,icetable_dynamic,TI) |
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| 92 | !----------------------------------------------------------------------- |
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| 93 | ! NAME |
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| 94 | ! update_soil_TI |
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| 95 | ! |
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| 96 | ! DESCRIPTION |
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| 97 | ! Update soil thermal inertia based on ice table, regolith properties, |
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| 98 | ! and pressure-dependent cementation. |
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| 99 | ! |
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| 100 | ! AUTHORS & DATE |
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| 101 | ! L. Lange, 2023 |
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| 102 | ! JB Clement, 2025 |
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| 103 | ! |
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| 104 | ! NOTES |
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| 105 | ! |
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| 106 | !----------------------------------------------------------------------- |
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| 107 | |
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| 108 | ! DEPENDENCIES |
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| 109 | ! ------------ |
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| 110 | use geometry, only: ngrid, nslope, nsoil |
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| 111 | use soil, only: volcapa, layer, inertiedat, depth_breccia, depth_bedrock, index_breccia, index_bedrock, reg_thprop_dependp |
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| 112 | use display, only: print_msg, LVL_NFO |
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| 113 | |
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| 114 | ! DECLARATION |
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| 115 | ! ----------- |
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| 116 | implicit none |
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| 117 | |
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| 118 | ! ARGUMENTS |
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| 119 | ! --------- |
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| 120 | real(dp), intent(in) :: p_avg_new ! Global average surface pressure [Pa] |
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| 121 | real(dp), dimension(:,:), intent(in) :: h2o_ice ! Surface Water ice [kg/m^2] |
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| 122 | real(dp), dimension(:,:), intent(in) :: icetable_depth ! Ice table depth [m] |
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| 123 | real(dp), dimension(:,:), intent(in) :: icetable_thickness ! Ice table thickness [m] |
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| 124 | real(dp), dimension(:,:,:), intent(in) :: ice_porefilling ! Ice porefilling [m^3/m^3] |
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| 125 | logical(k4), intent(in) :: icetable_equilibrium, icetable_dynamic ! Computing method for ice table |
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| 126 | real(dp), dimension(:,:,:), intent(inout) :: TI ! Soil Thermal Inertia [J/m^2/K/s^1/2] |
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| 127 | |
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| 128 | ! LOCAL VARIABLES |
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| 129 | ! --------------- |
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| 130 | integer(di) :: ig, islope, isoil, iref, iend ! Loop variables |
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| 131 | real(dp), dimension(ngrid,nslope) :: regolith_inertia ! Thermal inertia of the regolith (first layer in the GCM) [J/m^2/K/s^1/2] |
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| 132 | real(dp) :: delta ! Difference of depth to compute the thermal inertia in a mixed layer [m] |
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| 133 | real(dp) :: ice_bottom_depth ! Bottom depth of the subsurface ice [m] |
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| 134 | real(dp) :: d_part ! Regolith particle size [micrometer] |
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| 135 | real(dp) :: ice_inertia ! Inertia of water ice [SI] |
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| 136 | |
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| 137 | ! CODE |
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| 138 | ! ---- |
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| 139 | call print_msg("> Updating soil properties",LVL_NFO) |
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| 140 | |
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| 141 | ! 1. Modification of the regolith thermal inertia. |
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| 142 | do islope = 1,nslope |
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| 143 | regolith_inertia(:,islope) = inertiedat(:,1) |
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| 144 | do ig = 1,ngrid |
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| 145 | if (abs(h2o_ice(ig,islope)) < minieps) regolith_inertia(ig,islope) = TI_regolith_avg |
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| 146 | if (reg_thprop_dependp) then |
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| 147 | if (TI(ig,1,islope) < reg_inertie_thresold) then |
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| 148 | d_part = (regolith_inertia(ig,islope)**2/(volcapa*C*(P610*Pa2Torr)**0.6))**(-1./(0.11_dp*log10(P610*Pa2Torr/K))) ! compute particle size, in micrometer |
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| 149 | regolith_inertia(ig,islope) = sqrt(volcapa*C*(p_avg_new*Pa2Torr)**0.6*d_part**(-0.11_dp*log10(p_avg_new*Pa2Torr/K))) |
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| 150 | if (regolith_inertia(ig,islope) > reg_inertie_maxvalue) regolith_inertia(ig,islope) = reg_inertie_maxvalue |
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| 151 | if (regolith_inertia(ig,islope) < reg_inertie_minvalue) regolith_inertia(ig,islope) = reg_inertie_minvalue |
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| 152 | end if |
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| 153 | end if |
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| 154 | end do |
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| 155 | end do |
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| 156 | |
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| 157 | ! 2. Build new thermal inertia |
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| 158 | do islope = 1,nslope |
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| 159 | do ig = 1,ngrid |
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| 160 | do isoil = 1,index_breccia |
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| 161 | TI(ig,isoil,islope) = regolith_inertia(ig,islope) |
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| 162 | end do |
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| 163 | if (regolith_inertia(ig,islope) < TI_breccia) then |
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| 164 | !!! transition |
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| 165 | delta = depth_breccia |
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| 166 | TI(ig,index_breccia + 1,islope) = sqrt((layer(index_breccia + 1) - layer(index_breccia))/ & |
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| 167 | (((delta - layer(index_breccia))/(TI(ig,index_breccia,islope)**2)) + & |
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| 168 | ((layer(index_breccia + 1) - delta)/(TI_breccia**2)))) |
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| 169 | do isoil = index_breccia + 2,index_bedrock |
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| 170 | TI(ig,isoil,islope) = TI_breccia |
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| 171 | end do |
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| 172 | else ! we keep the high ti values |
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| 173 | do isoil = index_breccia + 1,index_bedrock |
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| 174 | TI(ig,isoil,islope) = TI(ig,index_breccia,islope) |
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| 175 | end do |
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| 176 | end if ! TI PEM and breccia comparison |
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| 177 | !!! transition |
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| 178 | delta = depth_bedrock |
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| 179 | TI(ig,index_bedrock + 1,islope) = sqrt((layer(index_bedrock + 1) - layer(index_bedrock))/ & |
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| 180 | (((delta - layer(index_bedrock))/(TI(ig,index_bedrock,islope)**2)) + & |
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| 181 | ((layer(index_bedrock + 1) - delta)/(TI_bedrock**2)))) |
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| 182 | do isoil = index_bedrock + 2,nsoil |
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| 183 | TI(ig,isoil,islope) = TI_bedrock |
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| 184 | end do |
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| 185 | end do ! ig |
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| 186 | end do ! islope |
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| 187 | |
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| 188 | ! 3. Build new TI in case of ice table |
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| 189 | do ig = 1,ngrid |
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| 190 | do islope = 1,nslope |
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| 191 | if (icetable_depth(ig,islope) > -1.e-6_dp) then |
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| 192 | ! 3.0 Case where it is perennial ice |
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| 193 | if (icetable_depth(ig,islope) < minieps) then |
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| 194 | call get_ice_TI(.true.,1._dp,0._dp,ice_inertia) |
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| 195 | do isoil = 1,nsoil |
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| 196 | TI(ig,isoil,islope) = ice_inertia |
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| 197 | end do |
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| 198 | else |
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| 199 | if (icetable_equilibrium) then |
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| 200 | call get_ice_TI(.false.,1._dp,regolith_inertia(ig,islope),ice_inertia) |
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| 201 | ! 3.1.1 find the index of the mixed layer |
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| 202 | iref = 0 ! initialize iref |
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| 203 | do isoil = 1,nsoil ! loop on layers to find the beginning of the ice table |
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| 204 | if (icetable_depth(ig,islope) >= layer(isoil)) then |
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| 205 | iref = isoil ! pure regolith layer up to here |
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| 206 | else |
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| 207 | exit ! correct iref was obtained in previous cycle |
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| 208 | end if |
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| 209 | end do |
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| 210 | ! 3.1.2 find the index of the end of the ice table |
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| 211 | iend = 0 ! initialize iend |
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| 212 | ice_bottom_depth = icetable_depth(ig,islope) + icetable_thickness(ig,islope) |
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| 213 | do isoil = 1,nsoil ! loop on layers to find the end of the ice table |
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| 214 | if (ice_bottom_depth >= layer(isoil)) then |
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| 215 | iend = isoil ! pure regolith layer up to here |
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| 216 | else |
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| 217 | exit ! correct iref was obtained in previous cycle |
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| 218 | end if |
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| 219 | end do |
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| 220 | ! 3.2 Build the new ti |
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| 221 | if (iref < nsoil) then |
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| 222 | if (iref == iend) then |
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| 223 | ! Ice table begins and end in the same mixture with three components |
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| 224 | if (iref /= 0) then ! mixed layer |
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| 225 | TI(ig,iref + 1,islope) = sqrt((layer(iref + 1) - layer(iref))/ & |
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| 226 | (((icetable_depth(ig,islope) - layer(iref))/(TI(ig,iref,islope)**2)) + & |
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| 227 | ((ice_bottom_depth - icetable_depth(ig,islope))/(ice_inertia**2)) + & |
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| 228 | ((layer(iref + 1) - ice_bottom_depth)/(TI(ig,iref + 1,islope)**2)))) |
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| 229 | else ! first layer is already a mixed layer |
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| 230 | ! (ie: take layer(iref=0)=0) |
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| 231 | TI(ig,1,islope) = sqrt((layer(1))/ & |
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| 232 | (((icetable_depth(ig,islope))/(TI(ig,1,islope)**2)) + & |
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| 233 | ((ice_bottom_depth - icetable_depth(ig,islope))/(ice_inertia**2)) + & |
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| 234 | ((layer(2) - ice_bottom_depth)/(TI(ig,2,islope)**2)))) |
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| 235 | end if ! of if (iref /= 0) |
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| 236 | else |
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| 237 | if (iref /= 0) then ! mixed layer |
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| 238 | TI(ig,iref + 1,islope) = sqrt((layer(iref + 1) - layer(iref))/ & |
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| 239 | (((icetable_depth(ig,islope) - layer(iref))/(TI(ig,iref,islope)**2)) + & |
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| 240 | ((layer(iref + 1) - icetable_depth(ig,islope))/(ice_inertia**2)))) |
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| 241 | else ! first layer is already a mixed layer |
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| 242 | ! (ie: take layer(iref=0)=0) |
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| 243 | TI(ig,1,islope) = sqrt((layer(1))/ & |
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| 244 | (((icetable_depth(ig,islope))/(TI(ig,1,islope)**2)) + & |
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| 245 | ((layer(1) - icetable_depth(ig,islope))/(ice_inertia**2)))) |
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| 246 | end if ! of if (iref /= 0) |
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| 247 | end if ! iref == iend |
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| 248 | |
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| 249 | TI(ig,iref + 2:iend,islope) = ice_inertia |
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| 250 | if (iend < nsoil) then |
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| 251 | TI(ig,iend + 1,islope) = sqrt((layer(iend + 1) - layer(iend))/ & |
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| 252 | (((ice_bottom_depth - layer(iend))/(TI(ig,iend,islope)**2)) + & |
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| 253 | ((layer(iend + 1) - ice_bottom_depth)/(ice_inertia**2)))) |
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| 254 | end if |
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| 255 | end if ! of if (iref < nsoil) |
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| 256 | else if (icetable_dynamic) then |
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| 257 | do isoil = 1,nsoil |
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| 258 | call get_ice_TI(.false.,ice_porefilling(ig,isoil,islope),regolith_inertia(ig,islope),TI(ig,isoil,islope)) |
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| 259 | end do |
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| 260 | end if ! of if icetable_equilibrium |
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| 261 | end if ! permanent glaciers |
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| 262 | end if ! icetable_depth(ig,islope) > 0. |
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| 263 | end do !islope |
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| 264 | end do !ig |
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| 265 | |
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| 266 | END SUBROUTINE update_soil_TI |
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| 267 | !======================================================================= |
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| 268 | |
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| 269 | END MODULE soil_therm_inertia |
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