| [2888] | 1 | module ice_table_mod |
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| 2 | |
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| 3 | implicit none |
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| 4 | |
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| 5 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 6 | !!! |
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| [2961] | 7 | !!! Purpose: Ice table (pore-filling) variables and methods to compute it (dynamic and static) |
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| [2888] | 8 | !!! Author: LL, 02/2023 |
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| 9 | !!! |
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| 10 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 11 | |
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| [2961] | 12 | LOGICAL,SAVE :: icetable_equilibrium ! Boolean to say if the PEM needs to recompute the icetable depth when at equilibrium |
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| 13 | LOGICAL,SAVE :: icetable_dynamic ! Boolean to say if the PEM needs to recompute the icetable depth (dynamic method) |
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| 14 | real,save,allocatable :: porefillingice_depth(:,:) ! ngrid x nslope: Depth of the ice table [m] |
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| 15 | real,save,allocatable :: porefillingice_thickness(:,:) ! ngrid x nslope: Thickness of the ice table [m] |
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| [2888] | 16 | |
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| [2961] | 17 | contains |
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| [2888] | 18 | |
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| [2961] | 19 | |
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| 20 | subroutine ini_ice_table_porefilling(ngrid,nslope) |
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| 21 | |
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| 22 | implicit none |
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| 23 | integer,intent(in) :: ngrid ! number of atmospheric columns |
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| 24 | integer,intent(in) :: nslope ! number of slope within a mesh |
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| 25 | |
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| 26 | allocate(porefillingice_depth(ngrid,nslope)) |
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| 27 | allocate(porefillingice_thickness(ngrid,nslope)) |
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| 28 | |
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| 29 | end subroutine ini_ice_table_porefilling |
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| 30 | |
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| 31 | subroutine end_ice_table_porefilling |
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| 32 | |
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| 33 | implicit none |
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| 34 | if (allocated(porefillingice_depth)) deallocate(porefillingice_depth) |
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| 35 | if (allocated(porefillingice_thickness)) deallocate(porefillingice_thickness) |
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| 36 | |
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| 37 | end subroutine end_ice_table_porefilling |
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| 38 | |
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| [2980] | 39 | !!! -------------------------------------- |
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| [2961] | 40 | |
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| 41 | SUBROUTINE computeice_table_equilibrium(ngrid,nslope,nsoil_PEM,watercaptag,rhowatersurf_ave,rhowatersoil_ave,regolith_inertia,ice_table_beg,ice_table_thickness) |
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| [2888] | 42 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 43 | !!! |
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| [2961] | 44 | !!! Purpose: Compute the ice table depth (pore-filling) knowing the yearly average water |
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| [2888] | 45 | !!! density at the surface and at depth. |
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| 46 | !!! Computations are made following the methods in Schorgofer et al., 2005 |
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| 47 | !!! This subroutine only gives the ice table at equilibrium and does not consider exchange with the atmosphere |
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| 48 | !!! |
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| 49 | !!! Author: LL |
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| 50 | !!! |
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| 51 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| [2961] | 52 | use math_mod,only: findroot |
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| 53 | USE comsoil_h_PEM, only: mlayer_PEM,layer_PEM ! Depth of the vertical grid |
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| 54 | USE soil_thermalproperties_mod, only: ice_thermal_properties |
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| [2888] | 55 | implicit none |
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| [2961] | 56 | ! inputs |
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| 57 | ! ----------- |
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| [2888] | 58 | integer,intent(in) :: ngrid,nslope,nsoil_PEM ! Size of the physical grid, number of subslope, number of soil layer in the PEM |
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| 59 | logical,intent(in) :: watercaptag(ngrid) ! Boolean to check the presence of a perennial glacier |
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| 60 | real,intent(in) :: rhowatersurf_ave(ngrid,nslope) ! Water density at the surface, yearly averaged [kg/m^3] |
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| 61 | real,intent(in) :: rhowatersoil_ave(ngrid,nsoil_PEM,nslope) ! Water density at depth, computed from clapeyron law's (Murchy and Koop 2005), yearly averaged [kg/m^3] |
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| [2961] | 62 | real,intent(in) :: regolith_inertia(ngrid,nslope) ! Thermal inertia of the regolith layer [SI] |
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| 63 | ! Ouputs |
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| 64 | ! ----------- |
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| 65 | real,intent(out) :: ice_table_beg(ngrid,nslope) ! ice table depth [m] |
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| 66 | real,intent(out) :: ice_table_thickness(ngrid,nslope) ! ice table thickness [m] |
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| 67 | ! Local |
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| 68 | ! ----------- |
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| [2888] | 69 | real :: z1,z2 ! intermediate variables used when doing a linear interpolation between two depths to find the root |
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| [2961] | 70 | integer ig, islope,isoil,isoilend ! loop variables |
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| [2888] | 71 | real :: diff_rho(nsoil_PEM) ! difference of water vapor density between the surface and at depth [kg/m^3] |
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| [2961] | 72 | real :: ice_table_end ! depth of the end of the ice table [m] |
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| 73 | real :: previous_icetable_depth(ngrid,nslope) ! Ice table computed at previous ice depth [m] |
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| 74 | real :: stretch ! stretch factor to improve the convergence of the ice table |
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| 75 | real :: wice_inertia ! Water Ice thermal Inertia [USI] |
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| 76 | ! Code |
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| 77 | ! ----------- |
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| [2888] | 78 | |
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| [2961] | 79 | previous_icetable_depth(:,:) = ice_table_beg(:,:) |
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| [2888] | 80 | do ig = 1,ngrid |
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| 81 | if(watercaptag(ig)) then |
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| [2961] | 82 | ice_table_beg(ig,:) = 0. |
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| 83 | ice_table_thickness(ig,:) = layer_PEM(nsoil_PEM) ! Let's assume an infinite ice table (true when geothermal flux is set to 0.) |
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| [2888] | 84 | else |
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| 85 | do islope = 1,nslope |
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| [2961] | 86 | ice_table_beg(ig,islope) = -1. |
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| 87 | ice_table_thickness(ig,islope) = 0. |
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| [2888] | 88 | do isoil = 1,nsoil_PEM |
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| 89 | diff_rho(isoil) = rhowatersurf_ave(ig,islope) - rhowatersoil_ave(ig,isoil,islope) |
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| 90 | enddo |
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| 91 | if(diff_rho(1) > 0) then ! ice is at the surface |
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| [2961] | 92 | ice_table_beg(ig,islope) = 0. |
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| 93 | do isoilend = 2,nsoil_PEM-1 |
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| 94 | if((diff_rho(isoilend).gt.0).and.(diff_rho(isoilend+1).lt.0.)) then |
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| 95 | call findroot(diff_rho(isoilend),diff_rho(isoilend+1),mlayer_PEM(isoilend),mlayer_PEM(isoilend+1),ice_table_end) |
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| 96 | ice_table_thickness(ig,islope) = ice_table_end - ice_table_beg(ig,islope) |
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| 97 | exit |
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| 98 | endif |
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| 99 | enddo |
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| [2888] | 100 | else |
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| 101 | do isoil = 1,nsoil_PEM -1 ! general case, we find the ice table depth by doing a linear approximation between the two depth, and then solve the first degree equation to find the root |
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| 102 | if((diff_rho(isoil).lt.0).and.(diff_rho(isoil+1).gt.0.)) then |
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| [2961] | 103 | call findroot(diff_rho(isoil),diff_rho(isoil+1),mlayer_PEM(isoil),mlayer_PEM(isoil+1),ice_table_beg(ig,islope)) |
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| 104 | ! Now let's find the end of the ice table |
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| 105 | ice_table_thickness(ig,islope) = layer_PEM(nsoil_PEM) ! Let's assume an infinite ice table (true when geothermal flux is set to 0.) |
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| 106 | do isoilend = isoil+1,nsoil_PEM-1 |
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| 107 | if((diff_rho(isoilend).gt.0).and.(diff_rho(isoilend+1).lt.0.)) then |
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| 108 | call findroot(diff_rho(isoilend),diff_rho(isoilend+1),mlayer_PEM(isoilend),mlayer_PEM(isoilend+1),ice_table_end) |
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| 109 | ice_table_thickness(ig,islope) = ice_table_end - ice_table_beg(ig,islope) |
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| 110 | exit |
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| 111 | endif |
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| 112 | enddo |
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| [2888] | 113 | endif !diff_rho(z) <0 & diff_rho(z+1) > 0 |
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| 114 | enddo |
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| 115 | endif ! diff_rho(1) > 0 |
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| 116 | enddo |
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| 117 | endif ! watercaptag |
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| 118 | enddo |
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| [2961] | 119 | |
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| 120 | ! Small trick to speed up the convergence, Oded's idea. |
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| 121 | do islope = 1,nslope |
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| 122 | do ig = 1,ngrid |
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| 123 | if((ice_table_beg(ig,islope).gt.previous_icetable_depth(ig,islope)).and.(previous_icetable_depth(ig,islope).ge.0)) then |
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| 124 | call ice_thermal_properties(.false.,1.,regolith_inertia(ig,islope),wice_inertia) |
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| 125 | stretch = (regolith_inertia(ig,islope)/wice_inertia)**2 |
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| 126 | |
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| 127 | ice_table_thickness(ig,islope) = ice_table_thickness(ig,islope) + (ice_table_beg(ig,islope) - & |
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| 128 | previous_icetable_depth(ig,islope)+(ice_table_beg(ig,islope) - previous_icetable_depth(ig,islope))/stretch) |
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| 129 | ice_table_beg(ig,islope) = previous_icetable_depth(ig,islope)+(ice_table_beg(ig,islope) - previous_icetable_depth(ig,islope))/stretch |
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| 130 | endif |
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| 131 | enddo |
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| 132 | enddo |
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| 133 | |
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| [2888] | 134 | RETURN |
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| 135 | END |
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| 136 | |
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| [2980] | 137 | !!! -------------------------------------- |
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| [2961] | 138 | |
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| [3031] | 139 | |
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| 140 | SUBROUTINE compute_massh2o_exchange_ssi(ngrid,nslope,nsoil_PEM,former_ice_table_thickness,new_ice_table_thickness,ice_table_depth,tsoil,delta_m_h2o) |
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| 141 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 142 | !!! |
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| 143 | !!! Purpose: Compute the mass of H2O that has sublimated from the ice table / condensed |
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| 144 | !!! |
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| 145 | !!! Author: LL |
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| 146 | !!! |
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| 147 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 148 | use comsoil_h_PEM, only: mlayer_PEM |
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| 149 | use comslope_mod, only: subslope_dist,def_slope_mean |
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| 150 | use comconst_mod,only: pi |
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| [3032] | 151 | use constants_marspem_mod,only:porosity |
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| [3031] | 152 | implicit none |
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| 153 | ! inputs |
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| 154 | ! ----------- |
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| 155 | integer,intent(in) :: ngrid,nslope,nsoil_PEM ! Size of the physical grid, number of subslope, number of soil layer in the PEM |
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| 156 | real,intent(in) :: former_ice_table_thickness(ngrid,nslope) ! ice table thickness at the former iteration [m] |
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| 157 | real,intent(in) :: new_ice_table_thickness(ngrid,nslope) ! ice table thickness at the current iteration [m] |
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| 158 | real,intent(out) :: ice_table_depth(ngrid,nslope) ! ice table depth [m] |
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| 159 | real,intent(in) :: tsoil(ngrid,nsoil_PEM,nslope) ! Soil temperature [K] |
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| 160 | ! outputs |
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| 161 | ! ----------- |
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| 162 | real,intent(out) :: delta_m_h2o(ngrid) ! Mass of H2O ice that has been condensed on the ice table / sublimates from the ice table [kg/m^2] |
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| 163 | |
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| 164 | ! local |
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| 165 | real :: rho(ngrid,nslope) ! density of water ice [kg/m^3] |
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| 166 | integer :: ig,islope,ilay,iref ! loop index |
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| 167 | real :: Tice(ngrid,nslope) ! ice temperature [k] |
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| 168 | ! Code |
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| 169 | ! ----------- |
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| 170 | rho(:,:) = 0. |
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| 171 | Tice(:,:) = 0. |
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| 172 | !1. First let's compute Tice using a linear interpolation between the mlayer level |
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| 173 | do ig = 1,ngrid |
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| 174 | do islope = 1,nslope |
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| 175 | if(ice_table_depth(ig,islope).gt.0.) then |
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| 176 | if (ice_table_depth(ig,islope).lt. 1e-10) then |
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| 177 | Tice(ig,islope) = tsoil(ig,1,islope) |
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| 178 | else |
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| 179 | iref=0 ! initialize iref |
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| 180 | do ilay=1,nsoil_PEM ! loop on layers to find the beginning of the ice table |
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| 181 | if (ice_table_depth(ig,islope).ge.mlayer_PEM(ilay)) then |
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| 182 | iref=ilay ! pure regolith layer up to here |
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| 183 | else |
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| 184 | ! correct iref was obtained in previous cycle |
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| 185 | exit |
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| 186 | endif |
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| 187 | enddo |
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| 188 | if(iref.eq.nsoil_PEM) then |
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| 189 | Tice(ig,islope) = tsoil(ig,nsoil_PEM,islope) |
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| 190 | else |
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| 191 | Tice(ig,islope) = (tsoil(ig,iref+1,islope) - tsoil(ig,iref,islope))/(mlayer_PEM(iref+1) - mlayer_PEM(iref))* & |
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| 192 | (ice_table_depth(ig,islope) - mlayer_PEM(iref)) + tsoil(ig,iref,islope) |
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| 193 | endif |
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| 194 | rho(ig,islope) = -3.5353e-4*Tice(ig,islope)**2+ 0.0351* Tice(ig,islope) + 933.5030 ! Rottgers, 2012 |
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| 195 | endif |
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| 196 | endif |
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| 197 | enddo |
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| 198 | enddo |
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| 199 | |
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| 200 | |
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| 201 | !2. Let's compute the amount of ice that has sublimated in each subslope |
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| 202 | do ig = 1,ngrid |
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| 203 | do islope = 1,nslope |
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| [3032] | 204 | delta_m_h2o(ig) = delta_m_h2o(ig) + porosity*rho(ig,islope)*(new_ice_table_thickness(ig,islope) - former_ice_table_thickness(ig,islope)) & ! convention > 0. <=> it condenses |
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| [3031] | 205 | *subslope_dist(ig,islope)/cos(def_slope_mean(islope)*pi/180.) |
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| 206 | enddo |
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| 207 | enddo |
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| 208 | |
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| 209 | return |
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| 210 | end subroutine |
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| 211 | |
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| 212 | !!! -------------------------------------- |
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| 213 | |
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| [2902] | 214 | SUBROUTINE find_layering_icetable(porefill,psat_soil,psat_surf,pwat_surf,psat_bottom,B,index_IS,depth_filling,index_filling,index_geothermal,depth_geothermal,dz_etadz_rho) |
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| 215 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 216 | !!! |
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| 217 | !!! Purpose: Compute layering between dry soil, pore filling ice, and ice sheet based on Schorgofer, Icarus (2010). Adapted from NS MSIM |
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| 218 | !!! |
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| 219 | !!! Author: LL |
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| 220 | !!! |
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| 221 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 222 | use comsoil_h_PEM,only: nsoilmx_PEM,mlayer_PEM |
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| [2961] | 223 | use math_mod, only: deriv1,deriv1_onesided,colint,findroot,deriv2_simple |
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| [2902] | 224 | implicit none |
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| 225 | ! inputs |
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| 226 | ! ------ |
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| [2888] | 227 | |
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| [2902] | 228 | real,intent(in) :: porefill(nsoilmx_PEM) ! Fraction of pore space filled with ice [Unitless] 0 <= f <= 1 for pore ice |
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| 229 | real,intent(in) :: psat_soil(nsoilmx_PEM) ! Soil water pressure at saturation, yearly averaged [Pa] |
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| 230 | real,intent(in) :: psat_surf ! surface water pressure at saturation, yearly averaged [Pa] |
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| 231 | real,intent(in) :: pwat_surf ! Water vapor pressure at the surface, not necesseraly at saturation, yearly averaged [Pa] |
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| 232 | real,intent(in) :: psat_bottom ! Boundary conditions for soil vapor pressure [Pa] |
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| 233 | real,intent(in) :: B ! constant (Eq. 8 from Schorgofer, Icarus (2010).) |
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| 234 | integer, intent(in) :: index_IS ! index of the soil layer where the ice sheet begins [1] |
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| 235 | real, intent(inout) :: depth_filling ! depth where pore filling begins [m] |
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| [2888] | 236 | |
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| [2902] | 237 | ! outputs |
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| 238 | ! ------- |
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| 239 | integer,intent(out) :: index_filling ! index where the pore filling begins [1] |
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| 240 | integer, intent(out) :: index_geothermal ! index where the ice table stops [1] |
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| 241 | real, intent(out) :: depth_geothermal ! depth where the ice table stops [m] |
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| 242 | real, intent(out) :: dz_etadz_rho(nsoilmx_PEM) ! \partial z(eta \partial z rho), eta is the constriction, used later for pore filling increase |
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| 243 | |
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| 244 | ! local |
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| 245 | |
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| 246 | real :: eta(nsoilmx_PEM) ! constriction |
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| 247 | integer :: ilay ! index for loop |
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| 248 | real :: old_depth_filling ! depth_filling saved |
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| 249 | real :: dz_psat(nsoilmx_PEM) ! first derivative of the vapor pressure at saturationn |
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| 250 | integer :: index_tmp ! for loop |
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| 251 | real :: Jdry ! flux trought the dry layer |
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| 252 | real :: Jsat ! flux trought the ice layer |
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| 253 | real :: Jdry_prevlay,Jsat_prevlay ! same but for the previous ice layer |
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| 254 | integer :: index_firstice ! first index where ice appears (i.e., f > 0) |
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| 255 | real :: dz_eta(nsoilmx_PEM) ! \partial z \eta |
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| 256 | real :: dz_eta_low ! same but evaluated at the interface for ice |
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| 257 | real :: dzz_psat(nsoilmx_PEM) ! \partial \partial psat |
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| 258 | real :: massfillabove,massfillafter ! h2O mass above and after index_geothermal |
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| 259 | |
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| 260 | ! constant |
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| 261 | real :: pvap2rho = 18.e-3/8.314 |
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| 262 | ! |
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| 263 | |
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| 264 | ! 0. Compute constriction over the layer |
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| 265 | ! Within the ice sheet, constriction is set to 0. Elsewhere, constriction = (1-porefilling)**2 |
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| 266 | if (index_IS.lt.0) then |
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| 267 | index_tmp = nsoilmx_PEM |
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| 268 | do ilay = 1,nsoilmx_PEM |
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| 269 | call constriction(porefill(ilay),eta(ilay)) |
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| 270 | enddo |
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| 271 | else |
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| 272 | index_tmp = index_IS |
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| 273 | do ilay = 1,index_IS-1 |
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| 274 | call constriction(porefill(ilay),eta(ilay)) |
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| 275 | enddo |
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| 276 | do ilay = index_IS,nsoilmx_PEM |
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| 277 | eta(ilay) = 0. |
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| 278 | enddo |
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| 279 | endif |
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| 280 | |
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| 281 | ! 1. Depth at which pore filling occurs. We solve Eq. 9 from Schorgofer, Icarus (2010) |
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| 282 | |
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| 283 | old_depth_filling = depth_filling |
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| 284 | |
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| 285 | call deriv1(mlayer_PEM,nsoilmx_PEM,psat_soil,psat_surf,psat_bottom,dz_psat) |
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| 286 | |
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| 287 | do ilay = 1,index_tmp |
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| 288 | Jdry = (psat_soil(ilay) - pwat_surf)/mlayer_PEM(ilay) ! left member of Eq. 9 from Schorgofer, Icarus (2010) |
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| 289 | Jsat = eta(ilay)*dz_psat(ilay) !right member of Eq. 9 from Schorgofer, Icarus (2010) |
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| 290 | if((Jdry - Jsat).le.0) then |
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| 291 | index_filling = ilay |
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| 292 | exit |
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| 293 | endif |
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| 294 | enddo |
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| 295 | |
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| 296 | if(index_filling.eq.1) depth_filling = mlayer_PEM(1) |
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| 297 | |
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| 298 | if(index_filling.gt.1) then |
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| 299 | Jdry_prevlay = (psat_soil(index_filling-1) - pwat_surf)/mlayer_PEM(index_filling-1) |
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| 300 | Jsat_prevlay = eta(index_filling-1)*dz_psat(index_filling-1) |
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| 301 | call findroot(Jdry-Jsat,Jdry_prevlay-Jsat_prevlay,mlayer_PEM(index_filling),mlayer_PEM(index_filling-1),depth_filling) |
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| 302 | endif |
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| 303 | |
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| 304 | |
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| 305 | ! 2. Compute d_z (eta* d_z(rho)) (last term in Eq. 13 of Schorgofer, Icarus (2010)) |
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| 306 | |
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| 307 | |
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| 308 | ! 2.0 preliminary: depth to shallowest ice (discontinuity at interface) |
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| 309 | |
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| 310 | index_firstice = -1 |
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| 311 | do ilay = 1,nsoilmx_PEM |
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| 312 | if (porefill(ilay).le.0.) then |
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| 313 | index_firstice = ilay ! first point with ice |
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| 314 | exit |
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| 315 | endif |
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| 316 | enddo |
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| 317 | |
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| 318 | ! 2.1: now we can computeCompute d_z (eta* d_z(rho)) |
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| 319 | |
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| 320 | call deriv1(mlayer_PEM,nsoilmx_PEM,eta,1.,eta(nsoilmx_PEM-1),dz_eta) |
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| 321 | |
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| 322 | if ((index_firstice.gt.0).and.(index_firstice.lt.nsoilmx_PEM-2)) then |
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| 323 | call deriv1_onesided(index_firstice,mlayer_PEM,nsoilmx_PEM,eta,dz_eta(index_firstice)) |
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| 324 | endif |
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| 325 | |
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| 326 | call deriv2_simple(mlayer_PEM,nsoilmx_PEM,psat_soil,psat_surf,psat_bottom,dzz_psat) |
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| 327 | dz_etadz_rho(:) = pvap2rho*(dz_eta(:)*dz_psat(:) + eta(:)*dzz_psat(:)) |
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| 328 | |
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| 329 | ! 3. Ice table boundary due to geothermal heating |
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| 330 | |
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| 331 | if(index_IS.gt.0) index_geothermal = -1 |
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| 332 | if(index_geothermal.lt.0) depth_geothermal = -1. |
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| 333 | if((index_geothermal.gt.0).and.(index_IS.lt.0)) then ! Eq. 21 from Schorfoger, Icarus (2010) |
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| 334 | index_geothermal = -1 |
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| 335 | do ilay=2,nsoilmx_PEM |
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| 336 | if (dz_psat(ilay).gt.0.) then ! first point with reversed flux |
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| 337 | index_geothermal=ilay |
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| 338 | call findroot(dz_psat(ilay-1),dz_psat(ilay),mlayer_PEM(ilay-1),mlayer_PEM(ilay),depth_geothermal) |
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| 339 | exit |
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| 340 | endif |
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| 341 | enddo |
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| 342 | else |
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| 343 | index_geothermal = -1 |
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| 344 | endif |
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| 345 | if ((index_geothermal.gt.0).and.(index_IS.lt.0)) then ! Eq. 24 from Schorgofer, Icarus (2010) |
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| 346 | call colint(porefill(:)/eta(:),mlayer_PEM,nsoilmx_PEM,index_geothermal-1,nsoilmx_PEM,massfillabove) |
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| 347 | index_tmp = -1 |
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| 348 | do ilay=index_geothermal,nsoilmx_PEM |
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| 349 | if (minval(eta(ilay:nsoilmx_PEM)).le.0.) cycle ! eta=0 means completely full |
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| 350 | call colint(porefill(:)/eta(:),mlayer_PEM,nsoilmx_PEM,ilay,nsoilmx_PEM,massfillafter) |
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| 351 | if (massfillafter<dz_psat(ilay)*pvap2rho*B) then ! usually executes on i=typeG |
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| 352 | if (ilay>index_geothermal) then |
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| 353 | ! write(34,*) '# adjustment to geotherm depth by',ilay-index_geothermal |
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| 354 | call findroot(dz_psat(ilay-1)*pvap2rho*B-massfillabove, & |
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| 355 | dz_psat(ilay)*pvap2rho*B-massfillafter,mlayer_PEM(ilay-1),mlayer_PEM(ilay),depth_geothermal) |
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| 356 | ! if (depth_geothermal.gt.mlayer_PEM(ilay) .or. depth_geothermal.lt.<mlayer_PEM(ilay-1)) write(34,*) |
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| 357 | ! '# WARNING: zdepthG interpolation failed',ilay,mlayer_PEM(ilay-1),depth_geothermal,mlayer_PEM(ilay) |
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| 358 | index_tmp=ilay |
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| 359 | endif |
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| 360 | ! otherwise leave depth_geothermal unchanged |
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| 361 | exit |
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| 362 | endif |
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| 363 | massfillabove = massfillafter |
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| 364 | enddo |
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| 365 | if (index_tmp.gt.0) index_geothermal = index_tmp |
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| 366 | end if |
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| 367 | return |
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| 368 | end subroutine |
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| 369 | |
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| [2980] | 370 | !!! -------------------------------------- |
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| [2902] | 371 | |
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| 372 | SUBROUTINE constriction(porefill,eta) |
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| 373 | |
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| 374 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 375 | !!! |
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| 376 | !!! Purpose: Compute the constriction of vapor flux by pore ice |
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| 377 | !!! |
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| 378 | !!! Author: LL |
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| 379 | !!! |
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| 380 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 381 | implicit none |
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| 382 | real,intent(in) :: porefill ! pore filling fraction |
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| 383 | real,intent(out) :: eta ! constriction |
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| 384 | |
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| 385 | !!! |
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| 386 | |
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| 387 | if (porefill.le.0.) eta = 1. |
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| 388 | if ((porefill.gt.0.) .and.(porefill.lt.1.)) then |
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| 389 | eta = (1-porefill)**2 ! Hudson et al., JGR, 2009 |
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| 390 | endif |
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| 391 | if (porefill.le.1.) eta = 0. |
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| 392 | return |
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| [2961] | 393 | end subroutine |
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| [2902] | 394 | |
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| [2961] | 395 | end module |
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