1 | MODULE newsedim_mod |
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2 | |
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3 | IMPLICIT NONE |
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4 | |
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5 | CONTAINS |
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6 | |
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7 | SUBROUTINE newsedim(ngrid,nlay,naersize,ptimestep, |
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8 | & pplev,masse,epaisseur,pt,rd,rho,pqi,wq,iq) |
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9 | |
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10 | use ioipsl_getin_p_mod, only: getin_p |
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11 | use comcstfi_mod, only: r, g |
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12 | use gases_h, only: gfrac, gnom, ngasmx |
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13 | use gases_h, only: igas_CH4, igas_CO2, igas_H2, igas_H2O |
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14 | use gases_h, only: igas_He, igas_N2 |
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15 | use tracer_h, only : igcm_h2o_ice |
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16 | use watercommon_h, only: T_h2O_ice_liq,T_h2O_ice_clouds |
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17 | use radii_mod, only: h2o_cloudrad |
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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 | ! |
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23 | ! Purpose |
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24 | ! ------- |
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25 | ! Calculates sedimentation of 1 tracer |
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26 | ! of radius rd (m) and density rho (kg.m-3) |
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27 | ! |
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28 | !================================================================== |
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29 | |
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30 | !----------------------------------------------------------------------- |
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31 | ! declarations |
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32 | ! ------------ |
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33 | |
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34 | ! arguments |
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35 | ! --------- |
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36 | |
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37 | integer,intent(in) :: ngrid ! number of atmospheric columns |
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38 | integer,intent(in) :: nlay ! number of atmospheric layers |
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39 | integer,intent(in) :: naersize ! number of particle sizes (1 or number |
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40 | ! of grid boxes) |
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41 | real,intent(in) :: ptimestep ! physics time step (s) |
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42 | real,intent(in) :: pplev(ngrid,nlay+1) ! inter-layer pressures (Pa) |
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43 | real,intent(in) :: pt(ngrid,nlay) ! mid-layer temperatures (K) |
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44 | real,intent(in) :: masse (ngrid,nlay) ! atmospheric mass (kg) |
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45 | real,intent(in) :: epaisseur (ngrid,nlay) ! thickness of atm. layers (m) |
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46 | real,intent(in) :: rd(naersize) ! particle radius (m) |
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47 | real,intent(in) :: rho ! particle density (kg.m-3) |
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48 | real,intent(inout) :: pqi(ngrid,nlay) ! tracer (e.g. ?/kg) |
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49 | real,intent(out) :: wq(ngrid,nlay+1) ! flux of tracer during timestep (?/m-2) |
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50 | integer,intent(in) :: iq ! tracer index |
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51 | |
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52 | c local: |
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53 | c ------ |
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54 | |
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55 | INTEGER l,ig, k, i, igas |
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56 | REAL rfall, rsurf, Reynolds, Cd, zfrac |
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57 | REAL reffh2oliq(ngrid,nlay), reffh2oice(ngrid,nlay) |
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58 | |
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59 | LOGICAL,SAVE :: firstcall=.true. |
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60 | !$OMP THREADPRIVATE(firstcall) |
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61 | LOGICAL,SAVE :: crystal_shape |
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62 | !$OMP THREADPRIVATE(crystal_shape) |
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63 | |
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64 | c Traceurs : |
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65 | c ~~~~~~~~ |
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66 | real traversee (ngrid,nlay) |
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67 | real vstokes(ngrid,nlay) |
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68 | real w(ngrid,nlay) |
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69 | real ptop, dztop, Ep, Stra |
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70 | |
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71 | |
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72 | c Physical constant |
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73 | c ~~~~~~~~~~~~~~~~~ |
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74 | c Gas molecular viscosity (N.s.m-2) |
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75 | real, allocatable, save :: visc(:,:) |
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76 | !$OMP THREADPRIVATE(visc) |
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77 | c Effective gas molecular radius (m) |
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78 | real,save :: molrad |
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79 | !$OMP THREADPRIVATE(molrad) |
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80 | |
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81 | c local and saved variable |
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82 | real,save :: a,b |
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83 | !$OMP THREADPRIVATE(a,b) |
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84 | |
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85 | c ** un petit test de coherence |
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86 | c -------------------------- |
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87 | |
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88 | !print*,'temporary fixed particle rad in newsedim!!' |
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89 | |
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90 | IF (firstcall) THEN |
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91 | firstcall=.false. |
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92 | |
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93 | c Determination of the viscosity a(N.s.m-2) and the mean molecular radius (m) |
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94 | write(*,*) "Calculation of the viscosity and the mean molecular" |
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95 | & ," radius from gases.def" |
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96 | allocate(visc(ngrid,nlay)) |
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97 | visc(:,:)=0.0 |
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98 | molrad=0. |
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99 | do igas=1, ngasmx |
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100 | if(gfrac(igas).ge.0.0) then |
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101 | if(igas.eq.igas_CO2) then |
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102 | molrad = molrad + gfrac(igas)*2.2e-10 ! CO2 |
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103 | visc(:,:) = visc(:,:) + gfrac(igas)*1.0e-5 ! CO2 |
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104 | elseif(igas.eq.igas_N2) then |
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105 | molrad = molrad + gfrac(igas)*1.8e-10 ! N2 (Kunze et al. 2022) |
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106 | visc(:,:) = visc(:,:) + gfrac(igas)*1.0e-5 ! N2 |
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107 | elseif(igas.eq.igas_H2) then |
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108 | molrad = molrad + gfrac(igas)*1.41e-10 ! H2 (Ackerman & Marley 2001) |
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109 | visc(:,:) = visc(:,:) + gfrac(igas)*2.0d-07*pt(:,:)**0.66 ! H2 (from Rosner 2000) |
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110 | elseif(igas.eq.igas_H2O) then |
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111 | molrad = molrad + gfrac(igas)*2.3e-10 ! H2O (Crifo 1989 at 300K) |
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112 | visc(:,:) = visc(:,:) + gfrac(igas)*8e-6 ! H2O (Sengers & Kamgar-Parsi 1984) |
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113 | elseif(igas.eq.igas_He) then |
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114 | molrad = molrad + gfrac(igas)*1.1e-10 ! He (Kunze et al. 2022) |
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115 | visc(:,:) = visc(:,:) + ! He |
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116 | & gfrac(igas)*1.9e-5*(pt(:,:)/273.15)**0.7 ! He (Petersen 1970) |
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117 | elseif(igas.eq.igas_CH4) then |
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118 | molrad = molrad + gfrac(igas)*1.9e-10 ! CH4 (Ismail et al. 2015) |
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119 | visc(:,:) = visc(:,:) + gfrac(igas)*1.0e-5 ! CH4 |
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120 | else |
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121 | molrad = molrad + gfrac(igas)*2.2e-10 ! CO2 by default |
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122 | visc(:,:) = visc(:,:) + gfrac(igas)*1.e-5 ! CO2 by default |
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123 | write(*,*) trim(gnom(igas))," is not included in" |
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124 | & ," newsedim, CO2 is used by default" |
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125 | endif |
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126 | endif |
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127 | enddo |
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128 | write(*,*) "visc(1,1)=",visc(1,1),"N.s.m-2; ", |
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129 | & "molrad=",molrad,"m" |
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130 | |
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131 | c Correction for non-spherical water ice particles |
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132 | write(*,*) "Use non-spherical water ice particles", |
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133 | & " for the sedimentation ?" |
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134 | crystal_shape=.false. !default |
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135 | call getin_p("crystal_shape",crystal_shape) |
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136 | write(*,*) " crystal_shape = ",crystal_shape |
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137 | |
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138 | |
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139 | !======================================================================= |
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140 | ! Preliminary calculations for sedimenation velocity |
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141 | |
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142 | ! - Constant to compute stokes speed simple formulae |
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143 | ! (Vstokes = b / visc * rho* r**2 avec b= (2/9) * rho * g |
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144 | b = 2./9. * g |
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145 | |
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146 | ! - Constant to compute gas mean free path |
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147 | ! l= (T/P)*a, avec a = ( 0.707*8.31/(4*pi*molrad**2 * avogadro)) |
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148 | a = 0.707*8.31/(4*3.1416* molrad**2 * 6.023e23) |
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149 | |
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150 | c - Correction to account for non-spherical shape (Murphy et al. 1990) |
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151 | c (correction = 0.85 for irregular particles, 0.5 for disk shaped particles) |
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152 | c a = a * 0.85 |
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153 | |
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154 | |
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155 | ENDIF |
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156 | |
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157 | c----------------------------------------------------------------------- |
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158 | c 1. initialisation |
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159 | c ----------------- |
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160 | |
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161 | c Sedimentation velocity (m/s) |
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162 | c ~~~~~~~~~~~~~~~~~~~~~~ |
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163 | c (stokes law corrected for low pressure by the Cunningham |
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164 | c slip-flow correction according to Rossow (Icarus 36, 1-50, 1978) |
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165 | |
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166 | c Compute liquid and ice particle radii |
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167 | if((iq.eq.igcm_h2o_ice).and.crystal_shape) then |
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168 | call h2o_cloudrad(ngrid,nlay,pqi,reffh2oliq,reffh2oice) |
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169 | endif |
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170 | |
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171 | |
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172 | do l=1,nlay |
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173 | do ig=1, ngrid |
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174 | if (naersize.eq.1) then |
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175 | rfall=rd(1) |
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176 | else |
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177 | i=ngrid*(l-1)+ig |
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178 | rfall=rd(i) ! how can this be correct!!? |
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179 | endif |
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180 | |
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181 | c Correction for non-spherical water ice particles |
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182 | if((iq.eq.igcm_h2o_ice).and.crystal_shape) then |
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183 | zfrac= (pt(ig,l)-T_h2O_ice_clouds) / |
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184 | & (T_h2O_ice_liq-T_h2O_ice_clouds) |
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185 | zfrac= MAX(zfrac, 0.0) |
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186 | zfrac= MIN(zfrac, 1.0) |
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187 | rsurf=max(reffh2oice(ig,l),45.6*reffh2oice(ig,l)**1.3) ! surface radius (formula for rimed dendrites from Hemsfield 1977, transition at around 30 microns) |
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188 | rsurf=1/(zfrac/reffh2oice(ig,l)+(1-zfrac)/rsurf) ! radius giving the mean velocity between liquid and ice particles |
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189 | else |
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190 | rsurf=rfall |
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191 | endif |
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192 | |
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193 | vstokes(ig,l) = b / visc(ig,l) * rho * rfall**3 / rsurf * |
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194 | & (1 + 1.333* ( a*pt(ig,l)/pplev(ig,l) )/rsurf) |
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195 | |
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196 | c Correction for high Reynolds number |
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197 | Reynolds=2. * pplev(ig,l) / r / pt(ig,l) * |
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198 | & rsurf * vstokes(ig,l) / visc(ig,l) |
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199 | if(Reynolds.ge.1.0) then |
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200 | do i=1,5 |
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201 | Cd=24. / Reynolds * (1. + 0.15 * Reynolds**0.687) + |
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202 | & 0.42 / (1. + 42500 / Reynolds**1.16) ! (Formula from Bagheri 2018) |
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203 | vstokes(ig,l) =(8./3.*pplev(ig,l)/r/pt(ig,l)*g*rfall**3 / |
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204 | & rsurf**2/rho/Cd * |
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205 | & (1.+1.333*(a*pt(ig,l)/pplev(ig,l))/rsurf))**0.5 |
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206 | Reynolds=2. * pplev(ig,l) / r / pt(ig,l) * |
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207 | & rsurf * vstokes(ig,l) / visc(ig,l) |
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208 | enddo |
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209 | endif |
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210 | |
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211 | c Layer crossing time (s) : |
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212 | traversee(ig,l)= epaisseur(ig,l)/vstokes(ig,l) |
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213 | end do |
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214 | end do |
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215 | |
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216 | |
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217 | c Calcul de la masse d'atmosphere correspondant a q transferee |
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218 | c ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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219 | c (e.g. on recherche le niveau en dessous de laquelle le traceur |
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220 | c va traverser le niveau intercouche l : "dztop" est sa hauteur |
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221 | c au dessus de l (m), "ptop" est sa pression (Pa)) |
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222 | do l=1,nlay |
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223 | do ig=1, ngrid |
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224 | |
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225 | dztop = vstokes(ig,l)* ptimestep |
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226 | Ep=0 |
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227 | k=0 |
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228 | w(ig,l) = 0. !! JF+AS ajout initialisation (LK MARS) |
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229 | c ************************************************************** |
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230 | c Simple Method |
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231 | cc w(ig,l) = |
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232 | cc & (1- exp(-dztop*g/(r*pt(ig,l))))*pplev(ig,l) / g |
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233 | cc write(*,*) 'OK simple method l,w =', l, w(ig,l) |
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234 | cc write(*,*) 'OK simple method dztop =', dztop |
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235 | w(ig,l) = 1. - exp(-dztop*g/(r*pt(ig,l))) |
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236 | !!! Diagnostic: JF. Fix: AS. Date: 05/11 |
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237 | !!! Probleme arrondi avec la quantite ci-dessus |
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238 | !!! ---> vaut 0 pour -dztop*g/(r*pt(ig,l)) trop petit |
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239 | !!! ---> dans ce cas on utilise le developpement limite ! |
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240 | !!! ---> exp(-x) = 1 - x lorsque x --> 0 avec une erreur de x^2 / 2 |
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241 | |
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242 | IF ( w(ig,l) .eq. 0. ) THEN |
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243 | w(ig,l) = ( dztop*g/(r*pt(ig,l)) ) * pplev(ig,l) / g |
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244 | ELSE |
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245 | w(ig,l) = w(ig,l) * pplev(ig,l) / g |
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246 | ENDIF |
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247 | ! LK borrowed simple method from Mars model (AS/JF) |
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248 | |
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249 | !************************************************************** |
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250 | cccc Complex method : |
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251 | if (dztop.gt.epaisseur(ig,l)) then |
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252 | cccc Cas ou on "epuise" la couche l : On calcule le flux |
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253 | cccc Venant de dessus en tenant compte de la variation de Vstokes |
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254 | |
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255 | Ep= epaisseur(ig,l) |
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256 | Stra= traversee(ig,l) |
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257 | do while(dztop.gt.Ep.and.l+k+1.le.nlay) |
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258 | k=k+1 |
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259 | dztop= Ep + vstokes(ig,l+k)*(ptimestep -Stra) |
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260 | Ep = Ep + epaisseur(ig,l+k) |
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261 | Stra = Stra + traversee(ig,l+k) |
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262 | enddo |
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263 | Ep = Ep - epaisseur(ig,l+k) |
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264 | ! ptop=pplev(ig,l+k)*exp(-(dztop-Ep)*g/(r*pt(ig,l+k))) |
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265 | ptop=exp(-(dztop-Ep)*g/(r*pt(ig,l+k))) |
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266 | IF ( ptop .eq. 1. ) THEN |
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267 | !PRINT*, 'newsedim: exposant trop petit ', ig, l |
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268 | ptop=pplev(ig,l+k) * ( 1. - (dztop-Ep)*g/(r*pt(ig,l+k))) |
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269 | ELSE |
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270 | ptop=pplev(ig,l+k) * ptop |
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271 | ENDIF |
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272 | |
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273 | w(ig,l) = (pplev(ig,l) - ptop)/g |
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274 | |
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275 | endif !!! complex method |
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276 | c |
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277 | cc write(*,*) 'OK new method l,w =', l, w(ig,l) |
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278 | cc write(*,*) 'OK new method dztop =', dztop |
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279 | cc if(l.eq.7)write(*,*)'l=7,k,pplev,Ptop',pplev(ig,l),Ptop |
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280 | cc if(l.eq.7)write(*,*)'l=7,dztop,Ep',dztop,Ep |
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281 | cc if(l.eq.6)write(*,*)'l=6,k, w',k, w(1,l) |
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282 | cc if(l.eq.7)write(*,*)'l=7,k, w',k, w(1,l) |
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283 | cc if(l.eq.8)write(*,*)'l=8,k, w',k, w(1,l) |
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284 | c ************************************************************** |
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285 | |
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286 | end do |
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287 | end do |
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288 | |
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289 | call vlz_fi(ngrid,nlay,pqi,2.,masse,w,wq) |
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290 | c write(*,*) ' newsed: wq(6), wq(7), q(6)', |
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291 | c & wq(1,6),wq(1,7),pqi(1,6) |
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292 | |
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293 | END SUBROUTINE newsedim |
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294 | |
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295 | END MODULE newsedim_mod |
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