[135] | 1 | subroutine optci(PLEV,TLEV,DTAUI,TAUCUMI, & |
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| 2 | QXIAER,QSIAER,GIAER,COSBI,WBARI,TAUAERO, & |
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[305] | 3 | TMID,PMID,TAUGSURF,QVAR,MUVAR) |
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[135] | 4 | |
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| 5 | use radinc_h |
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[253] | 6 | use radcommon_h, only: gasi, tlimit, wrefVAR, Cmk,tgasref,pfgasref,wnoi,scalep |
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[471] | 7 | use gases_h |
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[135] | 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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[253] | 60 | real*8 DCONT |
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[305] | 61 | double precision wn_cont, p_cont, p_air, T_cont, dtemp |
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[135] | 62 | |
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[305] | 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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[135] | 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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[253] | 72 | real*8 rho, dz(L_LEVELS) |
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[135] | 73 | |
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[253] | 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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[135] | 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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[253] | 93 | taugsurf(:,:) = 0.0 |
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| 94 | dpr(:) = 0.0 |
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| 95 | lkcoef(:,:) = 0.0 |
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[135] | 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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[253] | 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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[135] | 109 | |
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[253] | 110 | ! if we have continuum opacities, we need dz |
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[305] | 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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[135] | 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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[253] | 121 | |
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[135] | 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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[253] | 126 | |
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[135] | 127 | DO NW=1,L_NSPECTI |
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| 128 | do iaer=1,naerkind |
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[253] | 129 | TAEROS(K,NW,IAER) = TAUAERO(K,IAER) * QXIAER(K,NW,IAER) |
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[135] | 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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[253] | 137 | DCONT = 0.0 ! continuum absorption |
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[135] | 138 | |
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[305] | 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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[253] | 142 | do igas=1,ngasmx |
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[135] | 143 | |
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[305] | 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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[135] | 149 | |
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[305] | 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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[135] | 156 | |
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[305] | 157 | endif |
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[253] | 158 | |
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[305] | 159 | DCONT = DCONT + dtemp |
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[253] | 160 | |
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| 161 | enddo |
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| 162 | |
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[305] | 163 | |
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| 164 | DCONT = DCONT*dz(k) |
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| 165 | |
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[253] | 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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[135] | 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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[253] | 181 | if(L_REFVAR.eq.1)then ! added by RW for special no variable case |
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[135] | 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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[253] | 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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[135] | 191 | |
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[253] | 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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[135] | 195 | |
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[253] | 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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[135] | 199 | |
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[253] | 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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[135] | 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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[253] | 207 | ANS = LKCOEF(K,1)*KCOEF(1) + LKCOEF(K,2)*KCOEF(2) + & |
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[135] | 208 | LKCOEF(K,3)*KCOEF(3) + LKCOEF(K,4)*KCOEF(4) |
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[253] | 209 | |
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[135] | 210 | TAUGAS = U(k)*ANS |
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| 211 | |
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[305] | 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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[253] | 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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[135] | 219 | |
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[253] | 220 | DTAUKI(K,nw,ng) = TAUGAS + DCONT ! For parameterized continuum absorption |
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| 221 | |
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[135] | 222 | do iaer=1,naerkind |
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[253] | 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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[135] | 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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[253] | 232 | DTAUKI(K,nw,ng) = 0.0 + DCONT ! For parameterized continuum absorption |
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| 233 | |
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[135] | 234 | do iaer=1,naerkind |
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[253] | 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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[135] | 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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[305] | 333 | end subroutine optci |
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[135] | 334 | |
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| 335 | |
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| 336 | |
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