1 | subroutine optci(PLEV,TLEV,DTAUI,TAUCUMI, & |
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2 | QXIAER,QSIAER,GIAER,COSBI,WBARI,TAUAERO, & |
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3 | TMID,PMID,TAUGSURF,QVAR,MUVAR) |
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4 | |
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5 | use radinc_h |
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6 | use radcommon_h, only: gasi, tlimit, wrefVAR, Cmk,tgasref,pfgasref,wnoi,scalep |
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7 | use gases_h |
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8 | implicit none |
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9 | |
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10 | !================================================================== |
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11 | ! |
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12 | ! Purpose |
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13 | ! ------- |
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14 | ! Calculates longwave optical constants at each level. For each |
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15 | ! layer and spectral interval in the IR it calculates WBAR, DTAU |
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16 | ! and COSBAR. For each level it calculates TAU. |
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17 | ! |
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18 | ! TAUI(L,LW) is the cumulative optical depth at level L (or alternatively |
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19 | ! at the *bottom* of layer L), LW is the spectral wavelength interval. |
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20 | ! |
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21 | ! TLEV(L) - Temperature at the layer boundary (i.e., level) |
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22 | ! PLEV(L) - Pressure at the layer boundary (i.e., level) |
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23 | ! |
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24 | ! Authors |
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25 | ! ------- |
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26 | ! Adapted from the NASA Ames code by R. Wordsworth (2009) |
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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 | #include "comcstfi.h" |
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32 | #include "callkeys.h" |
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33 | |
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34 | |
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35 | real*8 DTAUI(L_NLAYRAD,L_NSPECTI,L_NGAUSS) |
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36 | real*8 DTAUKI(L_LEVELS+1,L_NSPECTI,L_NGAUSS) |
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37 | real*8 TAUI(L_NLEVRAD,L_NSPECTI,L_NGAUSS) |
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38 | real*8 TAUCUMI(L_LEVELS,L_NSPECTI,L_NGAUSS) |
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39 | real*8 PLEV(L_LEVELS) |
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40 | real*8 TLEV(L_LEVELS) |
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41 | real*8 TMID(L_LEVELS), PMID(L_LEVELS) |
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42 | real*8 COSBI(L_NLAYRAD,L_NSPECTI,L_NGAUSS) |
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43 | real*8 WBARI(L_NLAYRAD,L_NSPECTI,L_NGAUSS) |
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44 | |
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45 | ! For aerosols |
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46 | real*8 QXIAER(L_LEVELS+1,L_NSPECTI,NAERKIND) |
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47 | real*8 QSIAER(L_LEVELS+1,L_NSPECTI,NAERKIND) |
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48 | real*8 GIAER(L_LEVELS+1,L_NSPECTI,NAERKIND) |
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49 | real*8 TAUAERO(L_LEVELS+1,NAERKIND) |
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50 | real*8 TAUAEROLK(L_LEVELS+1,L_NSPECTI,NAERKIND) |
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51 | real*8 TAEROS(L_LEVELS,L_NSPECTI,NAERKIND) |
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52 | |
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53 | integer L, NW, NG, K, LK, IAER |
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54 | integer MT(L_LEVELS), MP(L_LEVELS), NP(L_LEVELS) |
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55 | real*8 ANS, TAUGAS |
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56 | real*8 DPR(L_LEVELS), U(L_LEVELS) |
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57 | real*8 LCOEF(4), LKCOEF(L_LEVELS,4) |
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58 | |
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59 | real*8 taugsurf(L_NSPECTI,L_NGAUSS-1) |
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60 | real*8 DCONT |
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61 | double precision wn_cont, p_cont, p_air, T_cont, dtemp |
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62 | |
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63 | ! Variable species mixing ratio variables |
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64 | real*8 QVAR(L_LEVELS), WRATIO(L_LEVELS), MUVAR(L_LEVELS) |
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65 | real*8 KCOEF(4) |
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66 | integer NVAR(L_LEVELS) |
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67 | |
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68 | ! temporary variables for multiple aerosol calculation |
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69 | real*8 atemp, btemp |
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70 | |
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71 | ! variables for k in units m^-1 |
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72 | real*8 rho, dz(L_LEVELS) |
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73 | |
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74 | integer igas |
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75 | |
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76 | !--- Kasting's CIA ---------------------------------------- |
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77 | !real*8, parameter :: Ci(L_NSPECTI)=[ & |
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78 | ! 3.8E-5, 1.2E-5, 2.8E-6, 7.6E-7, 4.5E-7, 2.3E-7, & |
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79 | ! 5.4E-7, 1.6E-6, 0.0, & |
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80 | ! 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, & |
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81 | ! 0.0, 4.0E-7, 4.0E-6, 1.4E-5, & |
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82 | ! 1.0E-5, 1.2E-6, 2.0E-7, 5.0E-8, 3.0E-8, 0.0 ] |
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83 | !real*8, parameter :: Ti(L_NSPECTI)=[ -2.2, -1.9, & |
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84 | ! -1.7, -1.7, -1.7, -1.7, -1.7, -1.7, & |
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85 | ! 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, & |
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86 | ! -1.7,-1.7,-1.7,-1.7,-1.7,-1.7,-1.7, -1.7,0.0 ] |
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87 | !---------------------------------------------------------- |
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88 | |
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89 | !======================================================================= |
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90 | ! Determine the total gas opacity throughout the column, for each |
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91 | ! spectral interval, NW, and each Gauss point, NG. |
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92 | |
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93 | taugsurf(:,:) = 0.0 |
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94 | dpr(:) = 0.0 |
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95 | lkcoef(:,:) = 0.0 |
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96 | |
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97 | do K=2,L_LEVELS |
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98 | DPR(k) = PLEV(K)-PLEV(K-1) |
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99 | |
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100 | !--- Kasting's CIA ---------------------------------------- |
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101 | !dz(k)=dpr(k)*189.02*TMID(K)/(0.03720*PMID(K)) |
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102 | ! this is CO2 path length (in cm) as written by Francois |
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103 | ! delta_z = delta_p * R_specific * T / (g * P) |
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104 | ! But Kasting states that W is in units of _atmosphere_ cm |
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105 | ! So we do |
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106 | !dz(k)=dz(k)*(PMID(K)/1013.25) |
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107 | !dz(k)=dz(k)/100.0 ! in m for SI calc |
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108 | !---------------------------------------------------------- |
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109 | |
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110 | ! if we have continuum opacities, we need dz |
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111 | if(kastprof)then |
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112 | dz(k) = dpr(k)*(8314.5/muvar(k))*TMID(K)/(g*PMID(K)) |
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113 | U(k) = (Cmk*mugaz/(muvar(k)))*DPR(k) |
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114 | else |
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115 | dz(k) = dpr(k)*R*TMID(K)/(g*PMID(K)) |
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116 | U(k) = Cmk*DPR(k) ! only Cmk line in optci.F |
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117 | endif |
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118 | |
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119 | call tpindex(PMID(K),TMID(K),QVAR(K),pfgasref,tgasref,WREFVAR, & |
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120 | LCOEF,MT(K),MP(K),NVAR(K),WRATIO(K)) |
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121 | |
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122 | do LK=1,4 |
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123 | LKCOEF(K,LK) = LCOEF(LK) |
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124 | end do |
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125 | |
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126 | |
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127 | DO NW=1,L_NSPECTI |
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128 | do iaer=1,naerkind |
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129 | TAEROS(K,NW,IAER) = TAUAERO(K,IAER) * QXIAER(K,NW,IAER) |
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130 | end do |
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131 | END DO |
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132 | end do ! levels |
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133 | |
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134 | do K=2,L_LEVELS |
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135 | do nw=1,L_NSPECTI |
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136 | |
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137 | DCONT = 0.0 ! continuum absorption |
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138 | |
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139 | ! include continua if necessary |
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140 | wn_cont = dble(wnoi(nw)) |
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141 | T_cont = dble(TMID(k)) |
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142 | do igas=1,ngasmx |
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143 | |
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144 | if(gfrac(igas).eq.-1)then ! variable |
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145 | p_cont = dble(PMID(k)*scalep*QVAR(k)) ! qvar = mol/mol |
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146 | else |
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147 | p_cont = dble(PMID(k)*scalep*gfrac(igas)*(1.-QVAR(k))) |
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148 | endif |
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149 | |
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150 | dtemp=0.0 |
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151 | if(gnom(igas).eq.'H2_')then |
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152 | call interpolateH2H2(wn_cont,T_cont,p_cont,dtemp,.false.) |
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153 | elseif(gnom(igas).eq.'H2O'.and.T_cont.gt.200.0)then |
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154 | p_air = dble(PMID(k)*scalep) - p_cont ! note assumes air!! |
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155 | call interpolateH2Ocont(wn_cont,T_cont,p_cont,p_air,dtemp,.false.) |
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156 | |
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157 | endif |
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158 | |
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159 | DCONT = DCONT + dtemp |
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160 | |
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161 | enddo |
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162 | |
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163 | |
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164 | DCONT = DCONT*dz(k) |
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165 | |
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166 | !--- Kasting's CIA ---------------------------------------- |
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167 | !DCO2 = dz(k)*Ci(nw)*(1.2859*PMID(k)/1000.0)*(TMID(k)/300.)**Ti(nw) |
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168 | !DCO2 = 130*Ci(nw)*(pmid(k)/1013.25)**2*(tmid(k)/300.)**Ti(nw) * dz(k) |
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169 | ! these two have been verified to give the same results |
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170 | !---------------------------------------------------------- |
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171 | |
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172 | |
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173 | do ng=1,L_NGAUSS-1 |
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174 | |
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175 | ! Now compute TAUGAS |
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176 | |
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177 | ! Interpolate between water mixing ratios |
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178 | ! WRATIO = 0.0 if the requested water amount is equal to, or outside the |
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179 | ! the water data range |
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180 | |
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181 | if(L_REFVAR.eq.1)then ! added by RW for special no variable case |
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182 | KCOEF(1) = GASI(MT(K),MP(K),1,NW,NG) |
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183 | KCOEF(2) = GASI(MT(K),MP(K)+1,1,NW,NG) |
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184 | KCOEF(3) = GASI(MT(K)+1,MP(K)+1,1,NW,NG) |
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185 | KCOEF(4) = GASI(MT(K)+1,MP(K),1,NW,NG) |
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186 | else |
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187 | |
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188 | KCOEF(1) = GASI(MT(K),MP(K),NVAR(K),NW,NG) + WRATIO(K)* & |
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189 | (GASI(MT(K),MP(K),NVAR(K)+1,NW,NG) - & |
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190 | GASI(MT(K),MP(K),NVAR(K),NW,NG)) |
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191 | |
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192 | KCOEF(2) = GASI(MT(K),MP(K)+1,NVAR(K),NW,NG) + WRATIO(K)* & |
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193 | (GASI(MT(K),MP(K)+1,NVAR(K)+1,NW,NG) - & |
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194 | GASI(MT(K),MP(K)+1,NVAR(K),NW,NG)) |
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195 | |
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196 | KCOEF(3) = GASI(MT(K)+1,MP(K)+1,NVAR(K),NW,NG) + WRATIO(K)* & |
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197 | (GASI(MT(K)+1,MP(K)+1,NVAR(K)+1,NW,NG) - & |
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198 | GASI(MT(K)+1,MP(K)+1,NVAR(K),NW,NG)) |
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199 | |
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200 | KCOEF(4) = GASI(MT(K)+1,MP(K),NVAR(K),NW,NG) + WRATIO(K)* & |
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201 | (GASI(MT(K)+1,MP(K),NVAR(K)+1,NW,NG) - & |
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202 | GASI(MT(K)+1,MP(K),NVAR(K),NW,NG)) |
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203 | endif |
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204 | |
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205 | ! Interpolate the gaseous k-coefficients to the requested T,P values |
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206 | |
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207 | ANS = LKCOEF(K,1)*KCOEF(1) + LKCOEF(K,2)*KCOEF(2) + & |
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208 | LKCOEF(K,3)*KCOEF(3) + LKCOEF(K,4)*KCOEF(4) |
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209 | |
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210 | TAUGAS = U(k)*ANS |
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211 | |
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212 | if(graybody)then |
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213 | TAUGAS = 0.0 |
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214 | DCONT = U(k)*3.3e-26 |
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215 | endif |
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216 | |
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217 | TAUGSURF(NW,NG) = TAUGSURF(NW,NG) + TAUGAS + DCONT |
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218 | !TAUGSURF(NW,NG) = TAUGSURF(NW,NG) + TAUGAS |
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219 | |
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220 | DTAUKI(K,nw,ng) = TAUGAS + DCONT ! For parameterized continuum absorption |
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221 | |
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222 | do iaer=1,naerkind |
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223 | DTAUKI(K,nw,ng) = DTAUKI(K,nw,ng) + TAEROS(K,NW,IAER) |
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224 | end do ! a bug was here! |
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225 | |
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226 | end do |
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227 | |
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228 | ! Now fill in the "clear" part of the spectrum (NG = L_NGAUSS), |
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229 | ! which holds continuum opacity only |
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230 | |
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231 | NG = L_NGAUSS |
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232 | DTAUKI(K,nw,ng) = 0.0 + DCONT ! For parameterized continuum absorption |
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233 | |
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234 | do iaer=1,naerkind |
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235 | DTAUKI(K,nw,ng) = DTAUKI(K,nw,ng) + TAEROS(K,NW,IAER) |
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236 | end do ! a bug was here! |
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237 | |
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238 | end do |
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239 | end do |
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240 | |
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241 | |
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242 | !======================================================================= |
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243 | ! Now the full treatment for the layers, where besides the opacity |
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244 | ! we need to calculate the scattering albedo and asymmetry factors |
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245 | |
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246 | DO NW=1,L_NSPECTI |
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247 | DO K=2,L_LEVELS+1 |
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248 | do iaer=1,naerkind |
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249 | TAUAEROLK(K,NW,IAER) = TAUAERO(K,IAER)*QSIAER(K,NW,IAER) |
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250 | end do |
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251 | ENDDO |
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252 | ENDDO |
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253 | |
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254 | DO NW=1,L_NSPECTI |
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255 | NG = L_NGAUSS |
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256 | DO L=1,L_NLAYRAD |
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257 | |
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258 | K = 2*L+1 |
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259 | DTAUI(L,nw,ng) = DTAUKI(K,NW,NG) + DTAUKI(K+1,NW,NG)! + 1.e-50 |
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260 | |
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261 | atemp = 0. |
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262 | btemp = 0. |
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263 | if(DTAUI(L,NW,NG) .GT. 1.0E-9) then |
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264 | do iaer=1,naerkind |
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265 | atemp = atemp + & |
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266 | GIAER(K,NW,IAER) * TAUAEROLK(K,NW,IAER) + & |
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267 | GIAER(K+1,NW,IAER) * TAUAEROLK(K+1,NW,IAER) |
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268 | btemp = btemp + TAUAEROLK(K,NW,IAER) + TAUAEROLK(K+1,NW,IAER) |
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269 | ! * + 1.e-10 |
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270 | end do |
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271 | WBARI(L,nw,ng) = btemp / DTAUI(L,NW,NG) |
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272 | else |
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273 | WBARI(L,nw,ng) = 0.0D0 |
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274 | DTAUI(L,NW,NG) = 1.0E-9 |
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275 | endif |
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276 | |
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277 | if(btemp .GT. 0.0) then |
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278 | cosbi(L,NW,NG) = atemp/btemp |
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279 | else |
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280 | cosbi(L,NW,NG) = 0.0D0 |
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281 | end if |
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282 | |
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283 | END DO ! L vertical loop |
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284 | |
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285 | ! Now the other Gauss points, if needed. |
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286 | |
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287 | DO NG=1,L_NGAUSS-1 |
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288 | IF(TAUGSURF(NW,NG) .gt. TLIMIT) THEN |
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289 | |
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290 | DO L=1,L_NLAYRAD |
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291 | K = 2*L+1 |
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292 | DTAUI(L,nw,ng) = DTAUKI(K,NW,NG)+DTAUKI(K+1,NW,NG)! + 1.e-50 |
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293 | |
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294 | btemp = 0. |
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295 | if(DTAUI(L,NW,NG) .GT. 1.0E-9) then |
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296 | |
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297 | do iaer=1,naerkind |
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298 | btemp = btemp + TAUAEROLK(K,NW,IAER) + TAUAEROLK(K+1,NW,IAER) |
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299 | end do |
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300 | WBARI(L,nw,ng) = btemp / DTAUI(L,NW,NG) |
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301 | |
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302 | else |
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303 | WBARI(L,nw,ng) = 0.0D0 |
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304 | DTAUI(L,NW,NG) = 1.0E-9 |
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305 | endif |
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306 | |
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307 | cosbi(L,NW,NG) = cosbi(L,NW,L_NGAUSS) |
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308 | END DO ! L vertical loop |
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309 | END IF |
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310 | |
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311 | END DO ! NG Gauss loop |
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312 | END DO ! NW spectral loop |
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313 | |
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314 | ! Total extinction optical depths |
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315 | |
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316 | DO NW=1,L_NSPECTI |
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317 | DO NG=1,L_NGAUSS ! full gauss loop |
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318 | TAUI(1,NW,NG)=0.0D0 |
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319 | DO L=1,L_NLAYRAD |
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320 | TAUI(L+1,NW,NG)=TAUI(L,NW,NG)+DTAUI(L,NW,NG) |
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321 | END DO |
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322 | |
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323 | TAUCUMI(1,NW,NG)=0.0D0 |
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324 | DO K=2,L_LEVELS |
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325 | TAUCUMI(K,NW,NG)=TAUCUMI(K-1,NW,NG)+DTAUKI(K,NW,NG) |
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326 | END DO |
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327 | END DO ! end full gauss loop |
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328 | END DO |
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329 | |
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330 | return |
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331 | |
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332 | |
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333 | end subroutine optci |
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334 | |
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335 | |
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336 | |
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