1 | subroutine kcmprof_fn(nlayer,psurf_rcm,qsurf_rcm,Tsurf_rcm,Tstra_rcm,P_rcm,Pl_rcm,z_rcm,T_rcm,q_rcm,m_rcm) |
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2 | |
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3 | use params_h |
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4 | use watercommon_h, only : mH2O |
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5 | use gases_h |
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6 | use comcstfi_mod, only: mugaz, cpp, g |
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7 | use callkeys_mod, only: co2cond |
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8 | implicit none |
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9 | |
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10 | ! ---------------------------------------------------------------- |
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11 | ! Purpose: create profiles of T, rho_v, rho_n, Pv and Pn following |
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12 | ! Kasting 1988 |
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13 | ! Authour: Adapted from a code by E. Marcq by R. Wordsworth (2011) |
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14 | ! ---------------------------------------------------------------- |
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15 | |
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16 | integer ilay, nlay |
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17 | parameter (nlay=10000) ! number of vertical layers |
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18 | |
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19 | ! rcm inputs |
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20 | integer nlayer |
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21 | real Tsurf_rcm,Tstra_rcm |
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22 | |
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23 | ! rcm outputs |
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24 | real psurf_rcm,qsurf_rcm |
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25 | real P_rcm(1:nlayer) |
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26 | real Pl_rcm(1:nlayer+1) |
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27 | real z_rcm(1:nlayer) |
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28 | real T_rcm(1:nlayer),q_rcm(1:nlayer) |
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29 | real m_rcm(1:nlayer+1) |
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30 | |
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31 | ! rcm for interpolation (should really use log coords?) |
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32 | !double precision p1,p2,pnew,ilay_rcm |
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33 | |
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34 | double precision lnp1,lnp2,lnpnew |
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35 | real Dp_rcm, dlogp_rcm |
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36 | integer ilay_rcm,ilev_rcm,ifinal_rcm |
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37 | |
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38 | double precision Dz, Dp |
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39 | double precision Ptop, dlogp, Psat_max |
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40 | parameter (Ptop=1.0) ! Pressure at TOA [Pa] |
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41 | |
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42 | double precision T(1:nlay) ! temperature [K] |
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43 | double precision Ztab(1:nlay) ! altitude [m] |
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44 | double precision Pv(1:nlay),Pn(1:nlay),P(1:nlay) ! pressure [Pa] |
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45 | double precision rho_v(1:nlay), rho_n(1:nlay) ! density [kg m^-3] |
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46 | double precision a_v(1:nlay) ! = rho_v/rho_n [kg/kg] |
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47 | double precision q_v(1:nlay) ! = rho_v/rho_tot [kg/kg] |
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48 | double precision mtot(1:nlay) ! = (rho_v+rho_n)/(n_v+n_n) [g/mol] |
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49 | |
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50 | integer profil_flag(1:nlay) ! 0 = dry, 1 = moist, 2 = isothermal |
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51 | |
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52 | ! inputs |
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53 | double precision Tsurf ! surface temperature [K] |
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54 | double precision Psurf_v ! surface par. pressure (variable species) [Pa] |
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55 | double precision Psurf_n ! surface par. pressure (incondensible species)[Pa] |
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56 | double precision Ttop ! stratospheric temperature [K] |
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57 | |
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58 | double precision dTdp ! [K/Pa] |
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59 | double precision dPvdp,dPndp ! [Pa/Pa] |
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60 | double precision psat_v ! local Psat_H2O value |
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61 | double precision Tcrit ! Critical temperature [K] |
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62 | double precision rho_vTEMP,rho_nTEMP |
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63 | |
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64 | double precision TCO2cond ! for CO2 condensation quasi-hack |
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65 | |
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66 | ! variables necessary for steam.f90 |
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67 | double precision rhol,rhov,nul |
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68 | |
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69 | ! for output |
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70 | double precision vmr |
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71 | |
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72 | logical verbose |
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73 | parameter(verbose=.true.) |
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74 | |
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75 | logical add_Pvar_to_total |
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76 | parameter(add_Pvar_to_total=.true.) |
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77 | |
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78 | ! initialise flags |
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79 | profil_flag(:) = 0 |
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80 | |
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81 | !------------------------------- |
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82 | ! assign input variables |
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83 | m_n = dble(mugaz/1000.) |
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84 | cp_n = cpp |
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85 | ! modify/generalise later?? |
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86 | |
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87 | Psat_max = 1000000.0 ! maximum vapour pressure [Pa] |
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88 | ! set huge until further notice |
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89 | |
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90 | if(vgas.lt.1)then |
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91 | if(psat_max.gt.0.0)then |
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92 | print*,'Must have Psat_max=0 if no variable species' |
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93 | psat_max=0.0 |
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94 | !stop |
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95 | endif |
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96 | print*, 'Assuming pure atmosphere' |
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97 | m_v = 1.0 |
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98 | tcrit = 1000.0 |
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99 | elseif(trim(gnom(vgas)).eq.'H2O')then |
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100 | m_v = dble(mH2O/1000.) |
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101 | tcrit = 6.47d2 |
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102 | elseif(trim(gnom(vgas)).eq.'NH3')then |
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103 | m_v = 17.031/1000. |
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104 | tcrit = 4.06d2 |
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105 | elseif(trim(gnom(vgas)).eq.'CH4')then |
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106 | m_v = 16.04/1000. |
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107 | tcrit = 1.91d2 |
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108 | stop |
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109 | else |
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110 | print*,'Variable gas not recognised!' |
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111 | call abort |
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112 | endif |
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113 | |
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114 | rmn = rc/m_n |
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115 | Ttop = dble(Tstra_rcm) |
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116 | Tsurf = dble(Tsurf_rcm) |
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117 | |
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118 | psat_v = psat_max |
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119 | if(vgas.gt.0)then |
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120 | if(trim(gnom(vgas)).eq.'H2O')then |
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121 | call Psat_H2O(tsurf,psat_v) |
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122 | elseif(trim(gnom(vgas)).eq.'NH3')then |
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123 | call Psat_NH3(tsurf,psat_v) |
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124 | endif |
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125 | endif |
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126 | |
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127 | ! Moist adiabat unless greater than or equal to psat_max |
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128 | if(psat_v*1d6.lt.psat_max)then |
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129 | Psurf_v = Psat_v*1d6 |
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130 | profil_flag(1) = 1 |
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131 | else |
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132 | Psurf_v = psat_max |
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133 | profil_flag(1) = 0 |
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134 | endif |
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135 | |
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136 | if(add_Pvar_to_total)then |
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137 | Psurf_n = dble(psurf_rcm) |
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138 | psurf_rcm = real(Psurf_n+Psurf_v) |
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139 | else |
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140 | Psurf_n = dble(psurf_rcm) - Psurf_v |
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141 | endif |
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142 | |
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143 | ! include relative humidity option |
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144 | !if(satval.lt.1.0)then |
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145 | ! Psurf_v = Psurf_v*satval |
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146 | ! profil_flag(1) = 0 |
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147 | !endif |
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148 | |
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149 | if(verbose)then |
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150 | print*,'Psat_v =',psat_v*1d6 |
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151 | print*,'Tsurf =',Tsurf,' K' |
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152 | print*,'Ttop =',Ttop,' K' |
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153 | print*,'Psurf_v =',Psurf_v,' Pa' |
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154 | print*,'Psurf_n =',Psurf_n,' Pa' |
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155 | print*,'m_n =',m_n,' kg/mol' |
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156 | print*,'m_v =',m_v,' kg/mol' |
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157 | print*,'rc =',rc |
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158 | endif |
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159 | |
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160 | ! define fine pressure grid |
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161 | dlogp_rcm = -(log(psurf_rcm)-log(ptop))/nlayer |
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162 | |
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163 | P_rcm(1) = psurf_rcm*exp(dlogp_rcm) |
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164 | do ilay_rcm=1,nlayer-1 |
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165 | P_rcm(ilay_rcm+1) = P_rcm(ilay_rcm)*exp(dlogp_rcm) |
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166 | enddo |
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167 | |
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168 | Pl_rcm(1) = psurf_rcm |
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169 | do ilev_rcm=2,nlayer |
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170 | ! log-linear interpolation |
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171 | Pl_rcm(ilev_rcm) = exp( log( P_rcm(ilev_rcm)*P_rcm(ilev_rcm-1) )/2 ) |
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172 | enddo |
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173 | |
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174 | !------------------------------- |
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175 | ! Layer 1 |
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176 | T(1) = Tsurf |
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177 | Pv(1) = Psurf_v |
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178 | Pn(1) = Psurf_n |
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179 | rho_n(1) = m_n*Pn(1)/(Rc*Tsurf) |
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180 | rho_v(1) = m_v*Pv(1)/(Rc*Tsurf) |
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181 | a_v(1) = rho_v(1)/rho_n(1) |
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182 | |
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183 | ! log pressure grid spacing (constant) |
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184 | dlogp = -(log(Pn(1)+Pv(1))-log(ptop))/(nlay-1) |
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185 | |
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186 | call gradients_kcm(profil_flag(1),rho_v(1),rho_n(1),Tsurf,dTdp,dPvdp,dPndp) |
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187 | if(verbose)then |
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188 | print*, 'dT/dp ground [K/Pa] =',dTdp |
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189 | endif |
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190 | |
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191 | ! initial delta p, delta z |
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192 | Dp = (Pn(1) + Pv(1))*(exp(dlogp) - 1d0) |
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193 | Dz = -Dp/( g*(rho_n(1) + rho_v(1)) ) |
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194 | |
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195 | !------------------------------- |
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196 | ! Layer 2 |
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197 | T(2) = tsurf + dTdp*Dp |
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198 | Pv(2) = Pv(1) + dPvdp*Dp |
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199 | Pn(2) = Pn(1) + dPndp*Dp |
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200 | rho_n(2) = m_n*Pn(2)/(Rc*T(2)) |
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201 | rho_v(2) = m_v*Pv(2)/(Rc*T(2)) |
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202 | a_v(2) = rho_v(2)/rho_n(2) |
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203 | |
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204 | !------------------------------- |
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205 | ! start vertical ascent |
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206 | Ztab(1) = 0. |
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207 | do ilay=2,nlay-1 |
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208 | |
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209 | ! calculate altitude levels (for diagnostic only) |
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210 | Dz = -Dp/( g*(rho_n(ilay) + rho_v(ilay)) ) |
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211 | Ztab(ilay) = Dz + Ztab(ilay-1) |
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212 | |
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213 | ! 1st assume next layer same as last one |
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214 | profil_flag(ilay) = profil_flag(ilay-1) |
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215 | |
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216 | ! update delta p |
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217 | Dp = (Pn(ilay)+Pv(ilay))*(exp(dlogp) - 1d0) |
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218 | |
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219 | ! intial gradients call to calculate temperature at next level |
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220 | call gradients_kcm(profil_flag(ilay),rho_v(ilay),rho_n(ilay),& |
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221 | T(ilay),dTdp,dPvdp,dPndp) |
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222 | |
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223 | T(ilay+1) = T(ilay) + dTdp*Dp |
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224 | |
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225 | ! test for moist adiabat at next level |
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226 | psat_v=psat_max |
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227 | |
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228 | if(vgas.gt.0)then |
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229 | if(trim(gnom(vgas)).eq.'H2O')then |
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230 | call Psat_H2O(T(ilay+1),psat_v) |
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231 | elseif(trim(gnom(vgas)).eq.'NH3')then |
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232 | call Psat_NH3(T(ilay+1),psat_v) |
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233 | endif |
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234 | endif |
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235 | |
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236 | if (psat_v*1d6 .lt. Pv(ilay)+dPvdp*Dp) then |
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237 | profil_flag(ilay)=1 |
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238 | call gradients_kcm(profil_flag(ilay),rho_v(ilay),rho_n(ilay),& |
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239 | T(ilay),dTdp,dPvdp,dPndp) |
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240 | endif |
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241 | |
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242 | ! test for stratosphere at next level |
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243 | if (T(ilay+1) .le. Ttop) then |
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244 | profil_flag(ilay)=2 |
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245 | T(ilay+1)=Ttop |
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246 | endif |
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247 | |
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248 | ! calculate pressures at next level |
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249 | Pn(ilay+1) = Pn(ilay) + dPndp*Dp |
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250 | Pv(ilay+1) = Pv(ilay) + dPvdp*Dp |
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251 | |
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252 | if(profil_flag(ilay) .eq. 1)then |
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253 | |
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254 | psat_v=psat_max |
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255 | |
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256 | if(vgas.gt.0)then |
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257 | if(trim(gnom(vgas)).eq.'H2O')then |
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258 | call Psat_H2O(T(ilay+1),psat_v) |
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259 | elseif(trim(gnom(vgas)).eq.'NH3')then |
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260 | call Psat_NH3(T(ilay+1),psat_v) |
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261 | endif |
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262 | endif |
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263 | |
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264 | if(Pv(ilay+1) .lt. psat_v*1e6)then |
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265 | Pv(ilay+1)=psat_v*1d6 |
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266 | endif |
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267 | |
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268 | endif |
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269 | |
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270 | ! calculate gas densities at next level (assume ideal) |
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271 | rho_n(ilay+1) = m_n*Pn(ilay+1)/(rc*T(ilay+1)) |
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272 | select case(profil_flag(ilay)) |
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273 | case(2) ! isothermal |
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274 | rho_v(ilay+1) = rho_v(ilay)/rho_n(ilay)*rho_n(ilay+1) |
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275 | case(1) ! moist |
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276 | |
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277 | ! dont think this is necessary |
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278 | !call psat_est(T(ilay+1),psat_v) |
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279 | ! modify for ammonia!!! |
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280 | |
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281 | rho_v(ilay+1) = m_v*psat_v*1d6/(rc*T(ilay+1)) |
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282 | case(0) ! dry |
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283 | rho_v(ilay+1) = m_v*Pv(ilay+1)/(rc*T(ilay+1)) |
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284 | end select |
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285 | |
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286 | enddo |
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287 | |
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288 | Ztab(nlay)=Ztab(nlay-1)+Dz |
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289 | |
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290 | !------------------------------- |
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291 | ! save to kcm1d variables |
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292 | |
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293 | ! surface quantities |
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294 | psurf_rcm = Pn(1) + Pv(1) |
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295 | qsurf_rcm = rho_v(1)/(rho_v(1) + rho_n(1)) |
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296 | |
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297 | ! create q_v, mtot for saving |
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298 | do ilay=1,nlay |
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299 | mtot(ilay) = 1d3*(rho_v(ilay) + rho_n(ilay)) / & |
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300 | (rho_v(ilay)/m_v + rho_n(ilay)/m_n) |
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301 | q_v(ilay) = rho_v(ilay)/(rho_v(ilay) + rho_n(ilay)) |
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302 | ! CHECK THIS |
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303 | enddo |
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304 | |
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305 | |
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306 | ! convert to rcm lower-res grid |
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307 | z_rcm(:) = 0.0 |
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308 | T_rcm(:) = 0.0 |
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309 | q_rcm(:) = 0.0 |
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310 | m_rcm(:) = 0.0 |
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311 | |
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312 | m_rcm(1) = real( 1d3*(rho_v(1) + rho_n(1)) / & |
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313 | (rho_v(1)/m_v + rho_n(1)/m_n) ) |
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314 | |
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315 | ilay_rcm=1 |
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316 | do ilay=2,nlay |
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317 | |
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318 | if(ilay_rcm.le.nlayer)then |
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319 | ! interpolate rcm variables |
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320 | |
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321 | if(Pn(ilay)+Pv(ilay) .lt. P_rcm(ilay_rcm))then |
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322 | |
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323 | if(ilay.eq.1)then |
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324 | print*,'Error in create_profils: Psurf here less than Psurf in RCM!' |
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325 | call abort |
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326 | endif |
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327 | |
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328 | lnp1 = log(Pn(ilay-1)+Pv(ilay-1)) |
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329 | lnp2 = log(Pn(ilay)+Pv(ilay)) |
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330 | lnpnew = dble(log(P_rcm(ilay_rcm))) |
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331 | |
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332 | z_rcm(ilay_rcm) = real(Ztab(ilay-1)*(lnp2-lnpnew)/(lnp2-lnp1) & |
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333 | + Ztab(ilay)*(lnpnew-lnp1)/(lnp2-lnp1)) |
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334 | T_rcm(ilay_rcm) = real(T(ilay-1)*(lnp2-lnpnew)/(lnp2-lnp1) & |
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335 | + T(ilay)*(lnpnew-lnp1)/(lnp2-lnp1)) |
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336 | q_rcm(ilay_rcm) = real(q_v(ilay-1)*(lnp2-lnpnew)/(lnp2-lnp1) & |
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337 | + q_v(ilay)*(lnpnew-lnp1)/(lnp2-lnp1)) |
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338 | |
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339 | m_rcm(ilay_rcm+1) = real(mtot(ilay-1)*(lnp2-lnpnew)/(lnp2-lnp1) & |
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340 | + mtot(ilay)*(lnpnew-lnp1)/(lnp2-lnp1)) |
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341 | |
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342 | ilay_rcm = ilay_rcm+1 |
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343 | endif |
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344 | |
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345 | endif |
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346 | enddo |
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347 | |
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348 | ifinal_rcm=ilay_rcm-1 |
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349 | if(ifinal_rcm.lt.nlayer)then |
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350 | if(verbose)then |
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351 | print*,'Interpolation in kcmprof stopped at layer',ilay_rcm,'!' |
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352 | endif |
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353 | |
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354 | do ilay_rcm=ifinal_rcm+1,nlayer |
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355 | |
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356 | z_rcm(ilay_rcm) = z_rcm(ilay_rcm-1) |
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357 | T_rcm(ilay_rcm) = T_rcm(ilay_rcm-1) |
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358 | q_rcm(ilay_rcm) = q_rcm(ilay_rcm-1) |
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359 | m_rcm(ilay_rcm+1) = m_rcm(ilay_rcm) |
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360 | |
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361 | enddo |
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362 | endif |
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363 | |
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364 | do ilay=2,nlayer |
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365 | if(T_rcm(ilay).lt.Ttop)then |
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366 | T_rcm(ilay)=Ttop |
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367 | endif |
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368 | enddo |
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369 | |
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370 | ! CO2 condensation 'haircut' of temperature profile if necessary |
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371 | if(co2cond)then |
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372 | print*,'CO2 condensation haircut - assumes CO2-dominated atmosphere!' |
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373 | do ilay=2,nlayer |
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374 | if(P_rcm(ilay).lt.518000.)then |
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375 | TCO2cond = (-3167.8)/(log(.01*P_rcm(ilay))-23.23) ! Fanale's formula |
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376 | else |
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377 | TCO2cond = 684.2-92.3*log(P_rcm(ilay))+4.32*log(P_rcm(ilay))**2 |
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378 | ! liquid-vapour transition (based on CRC handbook 2003 data) |
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379 | endif |
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380 | |
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381 | print*,'p=',P_rcm(ilay),', T=',T_rcm(ilay),' Tcond=',TCO2cond |
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382 | if(T_rcm(ilay).lt.TCO2cond)then |
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383 | T_rcm(ilay)=TCO2cond |
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384 | endif |
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385 | enddo |
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386 | endif |
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387 | |
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388 | return |
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389 | end subroutine kcmprof_fn |
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