1 | module co2glaciers_mod |
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2 | implicit none |
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3 | LOGICAL co2glaciersflow ! True by default, to compute co2 ice flow. Read in pem.def |
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4 | |
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5 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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6 | !!! |
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7 | !!! Purpose: Compute CO2 glacier flows |
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8 | !!! |
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9 | !!! Author: LL |
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10 | !!! |
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11 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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12 | |
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13 | contains |
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14 | |
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15 | |
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16 | subroutine co2glaciers_evol(timelen,ngrid,nslope,iflat,subslope_dist,def_slope_mean,vmr_co2_PEM,ps_GCM,global_ave_ps_GCM,global_ave_ps_PEM,co2ice_slope,flag_co2flow,flag_co2flow_mesh) |
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17 | |
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18 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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19 | !!! |
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20 | !!! Purpose: Main for CO2 glaciers evolution: compute maximum thickness, and do |
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21 | !!! the ice transfer |
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22 | !!! |
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23 | !!! |
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24 | !!! Author: LL |
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25 | !!! |
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26 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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27 | |
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28 | |
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29 | IMPLICIT NONE |
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30 | |
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31 | ! arguments |
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32 | ! --------- |
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33 | |
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34 | ! Inputs: |
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35 | INTEGER,INTENT(IN) :: timelen,ngrid,nslope,iflat ! # number of time sample, physical points, subslopes, index of the flat subslope |
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36 | REAL,INTENT(IN) :: subslope_dist(ngrid,nslope), def_slope_mean(ngrid) ! Physical points x SLopes : Distribution of the subgrid slopes; Slopes: values of the sub grid slope angles |
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37 | REAL,INTENT(IN) :: vmr_co2_PEM(ngrid,timelen) ! Physical x Time field : VMR of co2 in the first layer [mol/mol] |
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38 | REAL,INTENT(IN) :: ps_GCM(ngrid,timelen) ! Physical x Time field: surface pressure given by the GCM [Pa] |
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39 | REAL,INTENT(IN) :: global_ave_ps_GCM ! Global averaged surface pressure from the GCM [Pa] |
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40 | REAL,INTENT(IN) :: global_ave_ps_PEM ! global averaged surface pressure during the PEM iteration [Pa] |
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41 | |
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42 | ! Ouputs: |
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43 | REAL,INTENT(INOUT) :: co2ice_slope(ngrid,nslope) ! Physical x Slope field: co2 ice on the subgrid slopes [kg/m^2] |
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44 | REAL,INTENT(INOUT) :: flag_co2flow(ngrid,nslope) ! flag to see if there is flow on the subgrid slopes |
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45 | REAL,INTENT(INOUT) :: flag_co2flow_mesh(ngrid) ! same but within the mesh |
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46 | |
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47 | |
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48 | ! Local |
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49 | REAL :: Tcond(ngrid) ! Physical field: CO2 condensation temperature [K] |
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50 | REAL :: hmax(ngrid,nslope) ! Physical x Slope field: maximum thickness for co2 glacier before flow |
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51 | |
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52 | !----------------------------- |
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53 | call computeTcond(timelen,ngrid,vmr_co2_PEM,ps_GCM,global_ave_ps_GCM,global_ave_ps_PEM,Tcond) |
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54 | |
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55 | call compute_hmaxglaciers_co2(ngrid,nslope,iflat,Tcond,def_slope_mean,hmax) |
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56 | |
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57 | call transfer_co2ice_duringflow(ngrid,nslope,iflat, subslope_dist,def_slope_mean,hmax,Tcond,co2ice_slope,flag_co2flow,flag_co2flow_mesh) |
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58 | RETURN |
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59 | end subroutine |
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60 | |
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61 | |
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62 | |
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63 | subroutine compute_hmaxglaciers_co2(ngrid,nslope,iflat,Tcond,def_slope_mean,hmax) |
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64 | |
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65 | USE comconst_mod, ONLY: pi |
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66 | |
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67 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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68 | !!! |
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69 | !!! Purpose: Compute the maximum thickness of CO2 glaciers given a slope angle |
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70 | !!! before initating flow |
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71 | !!! |
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72 | !!! Author: LL, based on theoretical work by A.Grau Galofre (LPG) |
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73 | !!! |
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74 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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75 | |
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76 | IMPLICIT NONE |
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77 | |
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78 | ! arguments |
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79 | ! -------- |
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80 | |
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81 | ! Inputs |
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82 | INTEGER,INTENT(IN) :: ngrid,nslope ! # of grid points and subslopes |
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83 | INTEGER,INTENT(IN) :: iflat ! index of the flat subslope |
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84 | REAL,INTENT(IN) :: Tcond(ngrid) ! Physical field: CO2 condensation temperature [K] |
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85 | REAL,INTENT(IN) :: def_slope_mean(nslope) ! Slope field: Values of the subgrid slope angles [deg] |
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86 | ! Outputs |
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87 | REAL,INTENT(OUT) :: hmax(ngrid,nslope) ! Physical grid x Slope field: maximum co2 thickness before flaw [m] |
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88 | ! Local |
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89 | REAL, PARAMETER :: g = 3.71 ! surface gravity [m/s^2] |
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90 | INTEGER,PARAMETER :: n = 7 ! flow law exponent Nye et al., 2000 |
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91 | REAL,PARAMETER :: Rg = 8.3145 ! gas constant [J/K/mol] |
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92 | REAL,PARAMETER :: Q = 59000. ! Activation Energy [J/mol], Nye et al., 2000 |
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93 | DOUBLE PRECISION,PARAMETER :: C = 1.8138e-21 ! Nye et al., 2000 [s/m^n] |
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94 | DOUBLE PRECISION :: Ad = 1.202e11 ! Softness prefactor [MPa^-n] Nye et al., 2000 |
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95 | REAL :: Ro,Ho, S,ratio ! gemoetry from Nye et al., 2000 |
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96 | DOUBLE PRECISION :: A,Ao ! softness parameter [s/m^n] |
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97 | DOUBLE PRECISION :: C1 ! intermediate variable |
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98 | DOUBLE PRECISION :: t_0 ! relaxation time (assuming radial symetry) [s] |
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99 | DOUBLE PRECISION :: u ! characteristic horizontal deformation rate [m/s] |
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100 | DOUBLE PRECISION :: tau_d ! characteristic basal drag, understood as the strest that an ice CO2 mass flowing under its weight balanced by viscosity |
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101 | REAL :: rho_co2(ngrid) ! co2 ice density [kg/m^3] |
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102 | INTEGER :: ig,islope ! loop variables |
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103 | REAL :: slo_angle |
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104 | |
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105 | ! 0. Geometry parameters |
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106 | Ro = 200e3 |
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107 | Ho = 3000. |
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108 | ratio = 2./3. |
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109 | S = Ho/Ro*1/((2+1./n)*(1+1./n))*(1-ratio**(1+1./n))**(1./(2+1./n)-1)*ratio**(1+1./n-1) |
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110 | ! 1. Flow parameters |
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111 | Ao = 3**(1./(2*n+2))*Ad |
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112 | do ig = 1,n |
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113 | Ao = Ao*1e-6 |
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114 | enddo |
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115 | ! 2. Compute rho_co2 |
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116 | DO ig = 1,ngrid |
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117 | rho_co2(ig) = (1.72391 - 2.53e-4*Tcond(ig)-2.87*1e-7*Tcond(ig)**2)*1e3 ! Mangan et al. 2017 |
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118 | ENDDO |
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119 | ! 3. Compute max thickness |
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120 | DO ig = 1,ngrid |
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121 | A = Ao*exp(-Q/(Rg*Tcond(ig))) |
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122 | C1 = A*(rho_co2(ig)*g)**(float(n))/float(n+2) |
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123 | t_0 = Ro/(C1*(5*n+3))*(float(2*n+1)/float(n+1))**n |
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124 | u = Ro/t_0 |
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125 | tau_d = (u*Ho*(rho_co2(ig)*g)**2*S**2/(2*A))**(1./(n+2)) |
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126 | DO islope = 1,nslope |
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127 | if(islope.eq.iflat) then |
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128 | hmax(ig,islope) = 1.e6 |
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129 | else |
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130 | slo_angle = abs(def_slope_mean(islope)*pi/180.) |
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131 | hmax(ig,islope) = tau_d/(rho_co2(ig)*g*slo_angle) |
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132 | endif |
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133 | ENDDO |
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134 | ENDDO |
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135 | RETURN |
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136 | |
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137 | end subroutine |
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138 | |
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139 | subroutine transfer_co2ice_duringflow(ngrid,nslope,iflat, subslope_dist,def_slope_mean,hmax,Tcond,co2ice_slope,flag_co2flow,flag_co2flow_mesh) |
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140 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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141 | !!! |
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142 | !!! Purpose: Transfer the excess of ice from one subslope to another |
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143 | !!! No transfer between mesh at the time |
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144 | !!! Author: LL |
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145 | !!! |
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146 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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147 | |
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148 | USE comconst_mod, ONLY: pi |
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149 | |
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150 | |
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151 | implicit none |
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152 | |
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153 | ! arguments |
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154 | ! -------- |
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155 | |
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156 | ! Inputs |
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157 | INTEGER, INTENT(IN) :: ngrid,nslope !# of physical points and subslope |
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158 | INTEGER, INTENT(IN) :: iflat ! index of the flat subslope |
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159 | REAL, INTENT(IN) :: subslope_dist(ngrid,nslope) ! Distribution of the subgrid slopes within the mesh |
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160 | REAL, INTENT(IN) :: def_slope_mean(nslope) ! values of the subgrid slopes |
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161 | REAL, INTENT(IN) :: hmax(ngrid,nslope) ! maximum height of the CO2 glaciers before initiating flow [m] |
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162 | REAL, INTENT(IN) :: Tcond(ngrid) ! CO2 condensation temperature [K] |
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163 | ! Outputs |
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164 | REAL, INTENT(INOUT) :: co2ice_slope(ngrid,nslope) ! CO2 in the subslope [kg/m^2] |
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165 | REAL, INTENT(INOUT) :: flag_co2flow(ngrid,nslope) ! boolean to check if there is flow on a subgrid slope |
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166 | REAL, INTENT(INOUT) :: flag_co2flow_mesh(ngrid) ! boolean to check if there is flow in the mesh |
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167 | ! Local |
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168 | INTEGER ig,islope ! loop |
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169 | REAL rho_co2(ngrid) ! density of CO2, temperature dependant [kg/m^3] |
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170 | INTEGER iaval ! ice will be transfered here |
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171 | |
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172 | |
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173 | |
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174 | ! 0. Compute rho_co2 |
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175 | DO ig = 1,ngrid |
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176 | rho_co2(ig) = (1.72391 - 2.53e-4*Tcond(ig)-2.87*1e-7*Tcond(ig)**2)*1e3 ! Mangan et al. 2017 |
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177 | ENDDO |
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178 | |
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179 | ! 1. Compute the transfer of ice |
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180 | |
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181 | DO ig = 1,ngrid |
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182 | DO islope = 1,nslope |
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183 | IF(islope.ne.iflat) THEN ! ice can be infinite on flat ground |
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184 | ! First: check that CO2 ice must flow (excess of ice on the slope), ice can accumulate infinitely on flat ground |
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185 | IF(co2ice_slope(ig,islope).ge.rho_co2(ig)*hmax(ig,islope) * & |
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186 | cos(pi*def_slope_mean(islope)/180.)) THEN |
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187 | ! Second: determine the flatest slopes possible: |
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188 | IF(islope.gt.iflat) THEN |
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189 | iaval=islope-1 |
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190 | ELSE |
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191 | iaval=islope+1 |
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192 | ENDIF |
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193 | do while ((iaval.ne.iflat).and. & |
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194 | (subslope_dist(ig,iaval).eq.0)) |
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195 | IF(iaval.gt.iflat) THEN |
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196 | iaval=iaval-1 |
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197 | ELSE |
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198 | iaval=iaval+1 |
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199 | ENDIF |
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200 | enddo |
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201 | co2ice_slope(ig,iaval) = co2ice_slope(ig,iaval) + & |
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202 | (co2ice_slope(ig,islope) - rho_co2(ig)*hmax(ig,islope) * & |
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203 | cos(pi*def_slope_mean(islope)/180.)) * & |
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204 | subslope_dist(ig,islope)/subslope_dist(ig,iaval) * & |
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205 | cos(pi*def_slope_mean(iaval)/180.) / & |
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206 | cos(pi*def_slope_mean(islope)/180.) |
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207 | |
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208 | co2ice_slope(ig,islope)=rho_co2(ig)*hmax(ig,islope) * & |
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209 | cos(pi*def_slope_mean(islope)/180.) |
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210 | |
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211 | flag_co2flow(ig,islope) = 1. |
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212 | flag_co2flow_mesh(ig) = 1. |
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213 | ENDIF ! co2ice > hmax |
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214 | ENDIF ! iflat |
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215 | ENDDO !islope |
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216 | ENDDO !ig |
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217 | RETURN |
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218 | end subroutine |
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219 | |
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220 | subroutine computeTcond(timelen,ngrid,vmr_co2_PEM,ps_GCM,global_ave_ps_GCM,global_ave_ps_PEM,Tcond) |
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221 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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222 | !!! |
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223 | !!! Purpose: Compute CO2 condensation temperature |
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224 | !!! |
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225 | !!! Author: LL |
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226 | !!! |
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227 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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228 | implicit none |
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229 | ! arguments: |
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230 | ! ---------- |
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231 | |
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232 | ! INPUT |
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233 | INTEGER,INTENT(IN) :: timelen, ngrid ! # of timesample,physical points, subslopes |
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234 | REAL,INTENT(IN) :: vmr_co2_PEM(ngrid,timelen) ! Physical points x times field: VMR of CO2 in the first layer [mol/mol] |
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235 | REAL,INTENT(IN) :: ps_GCM(ngrid,timelen) ! Physical points x times field: surface pressure in the GCM [Pa] |
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236 | REAL,INTENT(IN) :: global_ave_ps_GCM ! Global averaged surfacepressure in the GCM [Pa] |
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237 | REAL, INTENT(IN) :: global_ave_ps_PEM ! Global averaged surface pressure computed during the PEM iteration |
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238 | ! OUTPUT |
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239 | REAL,INTENT(OUT) :: Tcond(ngrid) ! Physical points : condensation temperature of CO2, yearly averaged |
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240 | |
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241 | ! LOCAL |
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242 | |
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243 | INTEGER :: ig,it ! for loop |
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244 | REAL :: ave ! intermediate to compute average |
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245 | REAL :: alpha_clap, beta_clap ! Clapeyron law for CO2 |
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246 | alpha_clap = 23.3494 ! James et al. 1992 |
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247 | beta_clap = 3182.48 ! James et al. 1992 |
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248 | |
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249 | !!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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250 | |
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251 | |
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252 | DO ig = 1,ngrid |
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253 | ave = 0 |
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254 | DO it = 1,timelen |
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255 | ave = ave + beta_clap/(alpha_clap-log(vmr_co2_PEM(ig,it)*ps_GCM(ig,it)*global_ave_ps_GCM/global_ave_ps_PEM/100)) |
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256 | ENDDO |
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257 | Tcond(ig) = ave/timelen |
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258 | ENDDO |
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259 | RETURN |
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260 | |
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261 | |
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262 | end subroutine |
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263 | end module |
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