| 1 | MODULE compute_soiltemp_mod |
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| 2 | |
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| 3 | implicit none |
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| 4 | !----------------------------------------------------------------------- |
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| 5 | ! Author: LL |
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| 6 | ! Purpose: This module gathers the different routines used in the PEM to compute the soil temperature evolution and initialisation. |
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| 7 | ! |
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| 8 | ! Note: depths of layers and mid-layers, soil thermal inertia and |
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| 9 | ! heat capacity are commons in comsoil_PEM.h |
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| 10 | !----------------------------------------------------------------------- |
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| 11 | contains |
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| 12 | !======================================================================= |
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| 13 | |
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| 14 | SUBROUTINE compute_tsoil_pem(ngrid,nsoil,firstcall,therm_i,timestep,tsurf,tsoil) |
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| 15 | |
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| 16 | use comsoil_h_PEM, only: layer_PEM, mlayer_PEM, mthermdiff_PEM, thermdiff_PEM, coefq_PEM, coefd_PEM, mu_PEM, alph_PEM, beta_PEM, fluxgeo |
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| 17 | use comsoil_h, only: volcapa |
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| 18 | |
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| 19 | implicit none |
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| 20 | |
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| 21 | !----------------------------------------------------------------------- |
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| 22 | ! Author: LL |
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| 23 | ! Purpose: Compute soil temperature using an implict 1st order scheme |
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| 24 | ! |
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| 25 | ! Note: depths of layers and mid-layers, soil thermal inertia and |
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| 26 | ! heat capacity are commons in comsoil_PEM.h |
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| 27 | !----------------------------------------------------------------------- |
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| 28 | |
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| 29 | #include "dimensions.h" |
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| 30 | |
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| 31 | ! Inputs: |
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| 32 | ! ------- |
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| 33 | integer, intent(in) :: ngrid ! number of (horizontal) grid-points |
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| 34 | integer, intent(in) :: nsoil ! number of soil layers |
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| 35 | logical, intent(in) :: firstcall ! identifier for initialization call |
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| 36 | real, dimension(ngrid,nsoil), intent(in) :: therm_i ! thermal inertia [SI] |
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| 37 | real, intent(in) :: timestep ! time step [s] |
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| 38 | real, dimension(ngrid), intent(in) :: tsurf ! surface temperature [K] |
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| 39 | ! Outputs: |
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| 40 | !--------- |
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| 41 | real, dimension(ngrid,nsoil), intent(inout) :: tsoil ! soil (mid-layer) temperature [K] |
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| 42 | ! Local: |
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| 43 | !------- |
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| 44 | integer :: ig, ik |
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| 45 | |
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| 46 | ! 0. Initialisations and preprocessing step |
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| 47 | if (firstcall) then |
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| 48 | ! 0.1 Build mthermdiff_PEM(:), the mid-layer thermal diffusivities |
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| 49 | do ig = 1,ngrid |
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| 50 | do ik = 0,nsoil - 1 |
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| 51 | mthermdiff_PEM(ig,ik) = therm_i(ig,ik + 1)*therm_i(ig,ik + 1)/volcapa |
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| 52 | enddo |
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| 53 | enddo |
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| 54 | |
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| 55 | ! 0.2 Build thermdiff(:), the "interlayer" thermal diffusivities |
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| 56 | do ig = 1,ngrid |
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| 57 | do ik = 1,nsoil - 1 |
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| 58 | thermdiff_PEM(ig,ik) = ((layer_PEM(ik) - mlayer_PEM(ik - 1))*mthermdiff_PEM(ig,ik) & |
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| 59 | + (mlayer_PEM(ik) - layer_PEM(ik))*mthermdiff_PEM(ig,ik - 1))/(mlayer_PEM(ik) - mlayer_PEM(ik - 1)) |
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| 60 | enddo |
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| 61 | enddo |
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| 62 | |
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| 63 | ! 0.3 Build coefficients mu_PEM, q_{k+1/2}, d_k, alph_PEM |
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| 64 | ! mu_PEM |
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| 65 | mu_PEM = mlayer_PEM(0)/(mlayer_PEM(1) - mlayer_PEM(0)) |
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| 66 | |
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| 67 | ! q_{1/2} |
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| 68 | coefq_PEM(0) = volcapa*layer_PEM(1)/timestep |
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| 69 | ! q_{k+1/2} |
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| 70 | do ik = 1,nsoil - 1 |
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| 71 | coefq_PEM(ik) = volcapa*(layer_PEM(ik + 1) - layer_PEM(ik))/timestep |
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| 72 | enddo |
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| 73 | |
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| 74 | do ig = 1,ngrid |
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| 75 | ! d_k |
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| 76 | do ik = 1,nsoil - 1 |
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| 77 | coefd_PEM(ig,ik) = thermdiff_PEM(ig,ik)/(mlayer_PEM(ik)-mlayer_PEM(ik - 1)) |
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| 78 | enddo |
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| 79 | |
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| 80 | ! alph_PEM_{N-1} |
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| 81 | alph_PEM(ig,nsoil - 1) = coefd_PEM(ig,nsoil-1)/(coefq_PEM(nsoil - 1) + coefd_PEM(ig,nsoil - 1)) |
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| 82 | ! alph_PEM_k |
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| 83 | do ik = nsoil - 2,1,-1 |
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| 84 | alph_PEM(ig,ik) = coefd_PEM(ig,ik)/(coefq_PEM(ik) + coefd_PEM(ig,ik + 1)*(1. - alph_PEM(ig,ik + 1)) + coefd_PEM(ig,ik)) |
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| 85 | enddo |
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| 86 | enddo ! of do ig=1,ngrid |
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| 87 | endif ! of if (firstcall) |
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| 88 | |
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| 89 | if (.not. firstcall) THEN |
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| 90 | ! 2. Compute soil temperatures |
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| 91 | ! First layer: |
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| 92 | do ig = 1,ngrid |
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| 93 | tsoil(ig,1) = (tsurf(ig) + mu_PEM*beta_PEM(ig,1)*thermdiff_PEM(ig,1)/mthermdiff_PEM(ig,0))/ & |
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| 94 | (1. + mu_PEM*(1. - alph_PEM(ig,1))*thermdiff_PEM(ig,1)/mthermdiff_PEM(ig,0)) |
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| 95 | |
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| 96 | ! Other layers: |
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| 97 | do ik = 1,nsoil - 1 |
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| 98 | tsoil(ig,ik + 1) = alph_PEM(ig,ik)*tsoil(ig,ik) + beta_PEM(ig,ik) |
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| 99 | enddo |
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| 100 | enddo |
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| 101 | endif |
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| 102 | |
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| 103 | ! 2. Compute beta_PEM coefficients (preprocessing for next time step) |
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| 104 | ! Bottom layer, beta_PEM_{N-1} |
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| 105 | do ig = 1,ngrid |
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| 106 | beta_PEM(ig,nsoil - 1) = coefq_PEM(nsoil - 1)*tsoil(ig,nsoil)/(coefq_PEM(nsoil - 1) + coefd_PEM(ig,nsoil - 1)) & |
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| 107 | + fluxgeo/(coefq_PEM(nsoil - 1) + coefd_PEM(ig,nsoil - 1)) |
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| 108 | enddo |
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| 109 | ! Other layers |
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| 110 | do ik = nsoil-2,1,-1 |
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| 111 | do ig = 1,ngrid |
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| 112 | beta_PEM(ig,ik) = (coefq_PEM(ik)*tsoil(ig,ik + 1) + coefd_PEM(ig,ik + 1)*beta_PEM(ig,ik + 1))/ & |
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| 113 | (coefq_PEM(ik) + coefd_PEM(ig,ik + 1)*(1. - alph_PEM(ig,ik + 1)) + coefd_PEM(ig,ik)) |
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| 114 | enddo |
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| 115 | enddo |
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| 116 | |
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| 117 | END SUBROUTINE compute_tsoil_pem |
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| 118 | |
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| 119 | !======================================================================= |
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| 120 | |
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| 121 | SUBROUTINE ini_tsoil_pem(ngrid,nsoil,therm_i,tsurf,tsoil) |
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| 122 | |
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| 123 | use comsoil_h_PEM, only: layer_PEM, mlayer_PEM, mthermdiff_PEM, thermdiff_PEM, coefq_PEM, coefd_PEM, mu_PEM, alph_PEM, beta_PEM, fluxgeo |
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| 124 | use comsoil_h, only: volcapa |
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| 125 | |
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| 126 | implicit none |
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| 127 | |
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| 128 | !----------------------------------------------------------------------- |
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| 129 | ! Author: LL |
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| 130 | ! Purpose: Initialize the soil with the solution of the stationnary problem of Heat Conduction. Boundarry conditions: Tsurf averaged from the PCM; Geothermal flux at the bottom layer |
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| 131 | ! |
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| 132 | ! Note: depths of layers and mid-layers, soil thermal inertia and |
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| 133 | ! heat capacity are commons in comsoil_PEM.h |
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| 134 | !----------------------------------------------------------------------- |
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| 135 | |
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| 136 | #include "dimensions.h" |
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| 137 | |
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| 138 | ! Inputs: |
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| 139 | !-------- |
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| 140 | integer, intent(in) :: ngrid ! number of (horizontal) grid-points |
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| 141 | integer, intent(in) :: nsoil ! number of soil layers |
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| 142 | real, dimension(ngrid,nsoil), intent(in) :: therm_i ! thermal inertia [SI] |
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| 143 | real, dimension(ngrid), intent(in) :: tsurf ! surface temperature [K] |
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| 144 | ! Outputs: |
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| 145 | !--------- |
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| 146 | real, dimension(ngrid,nsoil), intent(inout) :: tsoil ! soil (mid-layer) temperature [K] |
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| 147 | ! Local: |
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| 148 | !------- |
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| 149 | integer :: ig, ik, iloop |
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| 150 | |
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| 151 | ! 0. Initialisations and preprocessing step |
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| 152 | ! 0.1 Build mthermdiff_PEM(:), the mid-layer thermal diffusivities |
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| 153 | do ig = 1,ngrid |
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| 154 | do ik = 0,nsoil - 1 |
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| 155 | mthermdiff_PEM(ig,ik) = therm_i(ig,ik + 1)*therm_i(ig,ik + 1)/volcapa |
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| 156 | enddo |
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| 157 | enddo |
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| 158 | |
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| 159 | ! 0.2 Build thermdiff(:), the "interlayer" thermal diffusivities |
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| 160 | do ig = 1,ngrid |
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| 161 | do ik = 1,nsoil - 1 |
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| 162 | thermdiff_PEM(ig,ik) = ((layer_PEM(ik) - mlayer_PEM(ik - 1))*mthermdiff_PEM(ig,ik) & |
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| 163 | + (mlayer_PEM(ik) - layer_PEM(ik))*mthermdiff_PEM(ig,ik - 1))/(mlayer_PEM(ik) - mlayer_PEM(ik - 1)) |
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| 164 | enddo |
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| 165 | enddo |
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| 166 | |
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| 167 | ! 0.3 Build coefficients mu_PEM, q_{k+1/2}, d_k, alph_PEM |
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| 168 | ! mu_PEM |
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| 169 | mu_PEM = mlayer_PEM(0)/(mlayer_PEM(1) - mlayer_PEM(0)) |
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| 170 | |
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| 171 | ! q_{1/2} |
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| 172 | coefq_PEM(:) = 0. |
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| 173 | ! q_{k+1/2} |
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| 174 | |
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| 175 | do ig = 1,ngrid |
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| 176 | ! d_k |
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| 177 | do ik = 1,nsoil - 1 |
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| 178 | coefd_PEM(ig,ik) = thermdiff_PEM(ig,ik)/(mlayer_PEM(ik) - mlayer_PEM(ik - 1)) |
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| 179 | enddo |
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| 180 | |
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| 181 | ! alph_PEM_{N-1} |
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| 182 | alph_PEM(ig,nsoil - 1) = coefd_PEM(ig,nsoil - 1)/(coefq_PEM(nsoil - 1) + coefd_PEM(ig,nsoil - 1)) |
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| 183 | ! alph_PEM_k |
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| 184 | do ik = nsoil - 2,1,-1 |
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| 185 | alph_PEM(ig,ik) = coefd_PEM(ig,ik)/(coefq_PEM(ik) + coefd_PEM(ig,ik + 1)*(1. - alph_PEM(ig,ik + 1)) + coefd_PEM(ig,ik)) |
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| 186 | enddo |
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| 187 | enddo ! of do ig=1,ngrid |
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| 188 | |
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| 189 | ! 1. Compute beta_PEM coefficients |
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| 190 | ! Bottom layer, beta_PEM_{N-1} |
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| 191 | do ig = 1,ngrid |
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| 192 | beta_PEM(ig,nsoil - 1) = coefq_PEM(nsoil - 1)*tsoil(ig,nsoil)/(coefq_PEM(nsoil - 1) + coefd_PEM(ig,nsoil - 1)) & |
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| 193 | + fluxgeo/(coefq_PEM(nsoil - 1) + coefd_PEM(ig,nsoil - 1)) |
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| 194 | enddo |
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| 195 | ! Other layers |
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| 196 | do ik = nsoil - 2,1,-1 |
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| 197 | do ig = 1,ngrid |
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| 198 | beta_PEM(ig,ik) = (coefq_PEM(ik)*tsoil(ig,ik + 1) + coefd_PEM(ig,ik+1)*beta_PEM(ig,ik + 1))/ & |
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| 199 | (coefq_PEM(ik) + coefd_PEM(ig,ik + 1)*(1. - alph_PEM(ig,ik + 1)) + coefd_PEM(ig,ik)) |
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| 200 | enddo |
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| 201 | enddo |
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| 202 | |
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| 203 | ! 2. Compute soil temperatures |
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| 204 | do iloop = 1,10 !just convergence |
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| 205 | do ig = 1,ngrid |
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| 206 | ! First layer: |
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| 207 | tsoil(ig,1) = (tsurf(ig) + mu_PEM*beta_PEM(ig,1)*thermdiff_PEM(ig,1)/mthermdiff_PEM(ig,0))/ & |
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| 208 | (1. + mu_PEM*(1. - alph_PEM(ig,1))*thermdiff_PEM(ig,1)/mthermdiff_PEM(ig,0)) |
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| 209 | ! Other layers: |
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| 210 | do ik = 1,nsoil - 1 |
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| 211 | tsoil(ig,ik + 1) = alph_PEM(ig,ik)*tsoil(ig,ik) + beta_PEM(ig,ik) |
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| 212 | enddo |
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| 213 | enddo |
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| 214 | enddo ! iloop |
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| 215 | |
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| 216 | END SUBROUTINE ini_tsoil_pem |
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| 217 | |
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| 218 | !======================================================================= |
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| 219 | |
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| 220 | SUBROUTINE shift_tsoil2surf(ngrid,nsoil,nslope,zshift_surf,zlag,tsurf,tsoil) |
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| 221 | |
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| 222 | use comsoil_h_PEM, only: layer_PEM, mlayer_PEM, fluxgeo, thermdiff_PEM, mthermdiff_PEM |
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| 223 | use math_mod, only: solve_steady_heat |
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| 224 | |
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| 225 | implicit none |
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| 226 | |
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| 227 | !----------------------------------------------------------------------- |
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| 228 | ! Author: JBC |
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| 229 | ! Purpose: Shifting the soil temperature profile to follow the surface evolution due to ice condensation/sublimation |
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| 230 | !----------------------------------------------------------------------- |
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| 231 | ! Inputs: |
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| 232 | ! ------- |
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| 233 | integer, intent(in) :: ngrid ! number of (horizontal) grid-points |
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| 234 | integer, intent(in) :: nsoil ! number of soil layers |
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| 235 | integer, intent(in) :: nslope ! number of sub-slopes |
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| 236 | real, dimension(ngrid,nslope), intent(in) :: zshift_surf ! elevation shift for the surface [m] |
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| 237 | real, dimension(ngrid,nslope), intent(in) :: zlag ! newly built lag thickness [m] |
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| 238 | real, dimension(ngrid,nslope), intent(in) :: tsurf ! surface temperature [K] |
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| 239 | ! Outputs: |
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| 240 | ! -------- |
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| 241 | real, dimension(ngrid,nsoil,nslope), intent(inout) :: tsoil ! soil (mid-layer) temperature [K] |
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| 242 | ! Local: |
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| 243 | ! ------ |
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| 244 | integer :: ig, isoil, islope, ishift, ilag, iz |
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| 245 | real :: a, z, zshift_surfloc, tsoil_minus, mlayer_minus |
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| 246 | real, dimension(ngrid,nsoil,nslope) :: tsoil_old |
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| 247 | |
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| 248 | write(*,*) "> Shifting soil temperature profile to match surface evolution" |
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| 249 | tsoil_old = tsoil |
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| 250 | |
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| 251 | do ig = 1,ngrid |
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| 252 | do islope = 1,nslope |
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| 253 | zshift_surfloc = zshift_surf(ig,islope) |
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| 254 | |
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| 255 | if (zshift_surfloc >= 0.) then ! In case of the surface is higher than initially |
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| 256 | if (zshift_surfloc < mlayer_PEM(0)) then ! Surface change is too small to be taken into account |
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| 257 | ! Nothing to do; we keep the soil temperature profile |
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| 258 | else if (zshift_surfloc >= mlayer_PEM(nsoil - 1)) then ! Surface change is much larger than the discretization |
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| 259 | tsoil(ig,:,islope) = tsurf(ig,islope) |
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| 260 | else |
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| 261 | ishift = 0 |
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| 262 | do while (mlayer_PEM(ishift) <= zshift_surfloc) |
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| 263 | ishift = ishift + 1 ! mlayer indices begin at 0 so this the good index for tsoil! |
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| 264 | enddo |
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| 265 | ! The "new soil" temperature is set to tsurf |
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| 266 | tsoil(ig,:ishift,islope) = tsurf(ig,islope) |
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| 267 | do isoil = ishift + 1,nsoil |
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| 268 | ! Position in the old discretization of the depth |
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| 269 | z = mlayer_PEM(isoil - 1) - zshift_surfloc |
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| 270 | ! Interpolation of the temperature profile from the old discretization |
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| 271 | tsoil(ig,isoil,islope) = itp_tsoil(tsoil_old(ig,:,islope),tsurf(ig,islope),z) |
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| 272 | enddo |
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| 273 | endif |
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| 274 | else ! In case of the surface is lower than initially |
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| 275 | if (abs(zshift_surfloc) < mlayer_PEM(0)) then ! Surface change is too small to be taken into account |
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| 276 | ! Nothing to do; we keep the soil temperature profile |
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| 277 | else if (abs(zshift_surfloc) >= mlayer_PEM(nsoil - 1)) then ! Surface change is much larger than the discretization |
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| 278 | call solve_steady_heat(nsoil,mlayer_PEM,layer_PEM,mthermdiff_PEM(ig,:),thermdiff_PEM(ig,:),tsurf(ig,islope),fluxgeo,tsoil(ig,:,islope)) |
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| 279 | else |
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| 280 | if (zlag(ig,islope) < mlayer_PEM(0)) then ! The lag is too thin to be taken into account |
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| 281 | ilag = 0 |
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| 282 | else |
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| 283 | ilag = 0 |
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| 284 | do while (mlayer_PEM(ilag) <= zlag(ig,islope)) |
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| 285 | ilag = ilag + 1 ! mlayer indices begin at 0 so this the good index for tsoil! |
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| 286 | enddo |
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| 287 | ! Position of the lag bottom in the old discretization of the depth |
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| 288 | z = zlag(ig,islope) - zshift_surfloc |
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| 289 | ! The "new lag" temperature is set to the ice temperature just below |
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| 290 | tsoil(ig,:ilag,islope) = itp_tsoil(tsoil_old(ig,:,islope),tsurf(ig,islope),z) |
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| 291 | endif |
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| 292 | |
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| 293 | ishift = nsoil - 1 |
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| 294 | z = mlayer_PEM(nsoil - 1) + zshift_surfloc |
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| 295 | do while (mlayer_PEM(ishift) >= z) |
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| 296 | ishift = ishift - 1 |
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| 297 | enddo |
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| 298 | ishift = ishift + 1 ! Adding 1 is needed to match the good index for tsoil! |
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| 299 | do isoil = ilag + 1,ishift |
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| 300 | ! Position in the old discretization of the depth |
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| 301 | z = mlayer_PEM(isoil - 1) - zshift_surfloc |
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| 302 | ! Interpolation of the temperature profile from the old discretization |
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| 303 | tsoil(ig,isoil,islope) = itp_tsoil(tsoil_old(ig,:,islope),tsurf(ig,islope),z) |
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| 304 | enddo |
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| 305 | |
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| 306 | ! The "new deepest layers" temperature is set by solving the steady heat equation |
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| 307 | call solve_steady_heat(nsoil - ishift + 1,mlayer_PEM(ishift - 1:),layer_PEM(ishift:),mthermdiff_PEM(ig,ishift - 1:),thermdiff_PEM(ig,ishift:),tsoil(ig,ishift,islope),fluxgeo,tsoil(ig,ishift:,islope)) |
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| 308 | endif |
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| 309 | endif |
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| 310 | enddo |
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| 311 | enddo |
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| 312 | |
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| 313 | END SUBROUTINE shift_tsoil2surf |
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| 314 | |
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| 315 | !======================================================================= |
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| 316 | |
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| 317 | FUNCTION itp_tsoil(tsoil,tsurf,z) RESULT(tsoil_z) |
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| 318 | |
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| 319 | use comsoil_h_PEM, only: mlayer_PEM |
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| 320 | |
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| 321 | implicit none |
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| 322 | |
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| 323 | real, dimension(:), intent(in) :: tsoil |
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| 324 | real, intent(in) :: z, tsurf |
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| 325 | |
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| 326 | real :: tsoil_z, tsoil_minus, mlayer_minus, a |
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| 327 | integer :: iz |
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| 328 | |
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| 329 | ! Find the interval [mlayer_PEM(iz - 1),mlayer_PEM(iz)[ where the position z belongs |
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| 330 | iz = 0 |
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| 331 | do while (mlayer_PEM(iz) <= z) |
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| 332 | iz = iz + 1 |
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| 333 | enddo |
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| 334 | if (iz == 0) then |
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| 335 | tsoil_minus = tsurf |
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| 336 | mlayer_minus = 0. |
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| 337 | else |
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| 338 | tsoil_minus = tsoil(iz) |
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| 339 | mlayer_minus = mlayer_PEM(iz - 1) |
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| 340 | endif |
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| 341 | ! Interpolation of the temperature profile from the old discretization |
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| 342 | a = (tsoil(iz + 1) - tsoil_minus)/(mlayer_PEM(iz) - mlayer_minus) |
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| 343 | tsoil_z = a*(z - mlayer_minus) + tsoil_minus |
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| 344 | |
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| 345 | END FUNCTION itp_tsoil |
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| 346 | |
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| 347 | END MODULE compute_soiltemp_mod |
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