1 | SUBROUTINE GFLUXV(DTDEL,TDEL,TAUCUMIN,WDEL,CDEL,UBAR0,F0PI,RSF, |
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2 | * BTOP,BSURF,FMIDP,FMIDM,DIFFV,FLUXUP,FLUXDN) |
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3 | |
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4 | |
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5 | C THIS SUBROUTINE TAKES THE OPTICAL CONSTANTS AND BOUNDARY CONDITIONS |
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6 | C FOR THE VISIBLE FLUX AT ONE WAVELENGTH AND SOLVES FOR THE FLUXES AT |
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7 | C THE LEVELS. THIS VERSION IS SET UP TO WORK WITH LAYER OPTICAL DEPTHS |
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8 | C MEASURED FROM THE TOP OF EACH LAYER. (DTAU) TOP OF EACH LAYER HAS |
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9 | C OPTICAL DEPTH TAU(N).IN THIS SUB LEVEL N IS ABOVE LAYER N. THAT IS LAYER N |
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10 | C HAS LEVEL N ON TOP AND LEVEL N+1 ON BOTTOM. OPTICAL DEPTH INCREASES |
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11 | C FROM TOP TO BOTTOM. SEE C.P. MCKAY, TGM NOTES. |
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12 | C THIS SUBROUTINE DIFFERS FROM ITS IR COUNTERPART IN THAT HERE WE SOLVE FOR |
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13 | C THE FLUXES DIRECTLY USING THE GENERALIZED NOTATION OF MEADOR AND WEAVOR |
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14 | C J.A.S., 37, 630-642, 1980. |
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15 | C THE TRI-DIAGONAL MATRIX SOLVER IS DSOLVER AND IS DOUBLE PRECISION SO MANY |
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16 | C VARIABLES ARE PASSED AS SINGLE THEN BECOME DOUBLE IN DSOLVER |
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17 | C |
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18 | C NLL = NUMBER OF LEVELS (NAYER + 1) THAT WILL BE SOLVED |
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19 | C NAYER = NUMBER OF LAYERS (NOTE DIFFERENT SPELLING HERE) |
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20 | C WAVEN = WAVELENGTH FOR THE COMPUTATION |
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21 | C DTDEL(NLAYER) = ARRAY OPTICAL DEPTH OF THE LAYERS |
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22 | C TDEL(NLL) = ARRAY COLUMN OPTICAL DEPTH AT THE LEVELS |
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23 | C WDEL(NLEVEL) = SINGLE SCATTERING ALBEDO |
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24 | C CDEL(NLL) = ASYMMETRY FACTORS, 0=ISOTROPIC |
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25 | C UBARV = AVERAGE ANGLE, |
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26 | C UBAR0 = SOLAR ZENITH ANGLE |
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27 | C F0PI = INCIDENT SOLAR DIRECT BEAM FLUX |
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28 | C RSF = SURFACE REFLECTANCE |
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29 | C BTOP = UPPER BOUNDARY CONDITION ON DIFFUSE FLUX |
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30 | C BSURF = REFLECTED DIRECT BEAM = (1-RSFI)*F0PI*EDP-TAU/U |
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31 | C FP(NLEVEL) = UPWARD FLUX AT LEVELS |
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32 | C FM(NLEVEL) = DOWNWARD FLUX AT LEVELS |
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33 | C FMIDP(NLAYER) = UPWARD FLUX AT LAYER MIDPOINTS |
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34 | C FMIDM(NLAYER) = DOWNWARD FLUX AT LAYER MIDPOINTS |
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35 | C added Dec 2002 |
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36 | C DIFFV = downward diffuse solar flux at the surface |
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37 | C |
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38 | !======================================================================! |
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39 | |
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40 | use radinc_h |
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41 | |
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42 | implicit none |
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43 | |
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44 | ! INTEGER NLP |
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45 | ! PARAMETER (NLP=101) ! MUST BE LARGER THAN NLEVEL |
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46 | |
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47 | REAL*8 EM, EP |
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48 | REAL*8 W0(L_NLAYRAD), COSBAR(L_NLAYRAD), DTAU(L_NLAYRAD) |
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49 | REAL*8 TAU(L_NLEVRAD), WDEL(L_NLAYRAD), CDEL(L_NLAYRAD) |
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50 | REAL*8 DTDEL(L_NLAYRAD), TDEL(L_NLEVRAD) |
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51 | REAL*8 FMIDP(L_NLAYRAD), FMIDM(L_NLAYRAD) |
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52 | REAL*8 LAMDA(L_NLAYRAD), ALPHA(L_NLAYRAD), XK1(L_NLAYRAD) |
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53 | REAL*8 XK2(L_NLAYRAD),G1(L_NLAYRAD), G2(L_NLAYRAD) |
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54 | REAL*8 G3(L_NLAYRAD), GAMA(L_NLAYRAD),CP(L_NLAYRAD),CM(L_NLAYRAD) |
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55 | REAL*8 CPM1(L_NLAYRAD),CMM1(L_NLAYRAD), E1(L_NLAYRAD) |
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56 | REAL*8 E2(L_NLAYRAD),E3(L_NLAYRAD),E4(L_NLAYRAD),EXPTRM(L_NLAYRAD) |
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57 | REAL*8 FLUXUP, FLUXDN |
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58 | REAL*8 FACTOR, TAUCUMIN(L_LEVELS), TAUCUM(L_LEVELS) |
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59 | |
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60 | integer NAYER, L, K |
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61 | real*8 ubar0, f0pi, rsf, btop, bsurf, g4, denom, am, ap |
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62 | real*8 taumax, taumid, cpmid, cmmid |
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63 | real*8 diffv |
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64 | |
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65 | C======================================================================C |
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66 | |
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67 | |
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68 | |
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69 | |
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70 | NAYER = L_NLAYRAD |
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71 | TAUMAX = L_TAUMAX !Default is 35.0 |
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72 | |
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73 | ! Delta-Eddington Scaling |
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74 | |
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75 | |
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76 | FACTOR = 1.0D0 - WDEL(1)*CDEL(1)**2 |
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77 | |
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78 | TAU(1) = TDEL(1)*FACTOR |
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79 | TAUCUM(1) = 0.0D0 |
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80 | TAUCUM(2) = TAUCUMIN(2)*FACTOR |
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81 | TAUCUM(3) = TAUCUM(2) +(TAUCUMIN(3)-TAUCUMIN(2))*FACTOR |
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82 | |
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83 | !Print*, 'TBbug wdel= ',WDEL |
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84 | !Print*, 'TBbug cdel= ',CDEL |
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85 | |
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86 | DO L=1,L_NLAYRAD-1 |
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87 | FACTOR = 1.0D0 - WDEL(L)*CDEL(L)**2 |
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88 | W0(L) = WDEL(L)*(1.0D0-CDEL(L)**2)/FACTOR |
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89 | COSBAR(L) = CDEL(L)/(1.0D0+CDEL(L)) |
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90 | DTAU(L) = DTDEL(L)*FACTOR |
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91 | TAU(L+1) = TAU(L)+DTAU(L) |
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92 | K = 2*(L+1) |
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93 | TAUCUM(K) = TAU(L+1) |
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94 | TAUCUM(K+1) = TAUCUM(K) + (TAUCUMIN(K+1)-TAUCUMIN(K))*FACTOR |
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95 | END DO |
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96 | !write(*,*),'gfluxv : cosbar=',COSBAR |
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97 | !write(*,*),'gfluxv : w0, factor=',W0(1),FACTOR |
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98 | !write(*,*),'gfluxv : wdel, cdel',WDEL(1),CDEL(1) |
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99 | |
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100 | |
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101 | ! Bottom layer |
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102 | |
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103 | L = L_NLAYRAD |
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104 | FACTOR = 1.0D0 - WDEL(L)*CDEL(L)**2 |
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105 | W0(L) = WDEL(L)*(1.0D0-CDEL(L)**2)/FACTOR |
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106 | COSBAR(L) = CDEL(L)/(1.0D0+CDEL(L)) |
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107 | DTAU(L) = DTDEL(L)*FACTOR |
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108 | TAU(L+1) = TAU(L)+DTAU(L) |
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109 | TAUCUM(2*L+1) = TAU(L+1) |
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110 | |
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111 | |
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112 | C WE GO WITH THE QUADRATURE APPROACH HERE. THE "SQRT(3)" factors |
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113 | C ARE THE UBARV TERM. |
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114 | |
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115 | DO L=1,L_NLAYRAD |
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116 | |
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117 | |
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118 | ALPHA(L)=SQRT( (1.0-W0(L))/(1.0-W0(L)*COSBAR(L)) ) |
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119 | ! write(*,*),'gfluxv : alpha = ',ALPHA(L) |
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120 | |
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121 | |
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122 | C SET OF CONSTANTS DETERMINED BY DOM |
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123 | |
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124 | G1(L) = (SQRT(3.0)*0.5)*(2.0- W0(L)*(1.0+COSBAR(L))) |
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125 | G2(L) = (SQRT(3.0)*W0(L)*0.5)*(1.0-COSBAR(L)) |
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126 | G3(L) = 0.5*(1.0-SQRT(3.0)*COSBAR(L)*UBAR0) |
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127 | |
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128 | |
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129 | c this is Quadrature |
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130 | c but the scaling is Eddington? |
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131 | |
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132 | LAMDA(L) = SQRT(G1(L)**2 - G2(L)**2) |
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133 | GAMA(L) = (G1(L)-LAMDA(L))/G2(L) |
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134 | END DO |
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135 | |
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136 | DO L=1,L_NLAYRAD |
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137 | G4 = 1.0-G3(L) |
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138 | DENOM = LAMDA(L)**2 - 1./UBAR0**2 |
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139 | |
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140 | C THERE IS A POTENTIAL PROBLEM HERE IF W0=0 AND UBARV=UBAR0 |
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141 | C THEN DENOM WILL VANISH. THIS ONLY HAPPENS PHYSICALLY WHEN |
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142 | C THE SCATTERING GOES TO ZERO |
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143 | C PREVENT THIS WITH AN IF STATEMENT |
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144 | |
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145 | IF ( DENOM .EQ. 0.) THEN |
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146 | DENOM=1.E-10 |
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147 | END IF |
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148 | |
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149 | |
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150 | AM = F0PI*W0(L)*(G4 *(G1(L)+1./UBAR0) +G2(L)*G3(L) )/DENOM |
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151 | AP = F0PI*W0(L)*(G3(L)*(G1(L)-1./UBAR0) +G2(L)*G4 )/DENOM |
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152 | |
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153 | C CPM1 AND CMM1 ARE THE CPLUS AND CMINUS TERMS EVALUATED |
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154 | C AT THE TOP OF THE LAYER, THAT IS LOWER OPTICAL DEPTH TAU(L) |
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155 | |
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156 | CPM1(L) = AP*EXP(-TAU(L)/UBAR0) |
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157 | CMM1(L) = AM*EXP(-TAU(L)/UBAR0) |
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158 | |
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159 | C CP AND CM ARE THE CPLUS AND CMINUS TERMS EVALUATED AT THE |
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160 | C BOTTOM OF THE LAYER. THAT IS AT HIGHER OPTICAL DEPTH TAU(L+1) |
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161 | |
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162 | CP(L) = AP*EXP(-TAU(L+1)/UBAR0) |
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163 | CM(L) = AM*EXP(-TAU(L+1)/UBAR0) |
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164 | |
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165 | END DO |
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166 | |
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167 | |
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168 | |
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169 | C NOW CALCULATE THE EXPONENTIAL TERMS NEEDED |
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170 | C FOR THE TRIDIAGONAL ROTATED LAYERED METHOD |
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171 | |
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172 | DO L=1,L_NLAYRAD |
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173 | !print*, 'TBbug=',TAUMAX,LAMDA(L),DTAU(L) |
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174 | EXPTRM(L) = MIN(TAUMAX,LAMDA(L)*DTAU(L)) ! CLIPPED EXPONENTIAL |
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175 | EP = EXP(EXPTRM(L)) |
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176 | |
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177 | EM = 1.0/EP |
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178 | E1(L) = EP+GAMA(L)*EM |
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179 | E2(L) = EP-GAMA(L)*EM |
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180 | E3(L) = GAMA(L)*EP+EM |
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181 | E4(L) = GAMA(L)*EP-EM |
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182 | END DO |
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183 | |
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184 | CALL DSOLVER(NAYER,GAMA,CP,CM,CPM1,CMM1,E1,E2,E3,E4,BTOP, |
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185 | * BSURF,RSF,XK1,XK2) |
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186 | |
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187 | C NOW WE CALCULATE THE FLUXES AT THE MIDPOINTS OF THE LAYERS. |
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188 | |
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189 | DO L=1,L_NLAYRAD-1 |
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190 | EXPTRM(L) = MIN(TAUMAX,LAMDA(L)*(TAUCUM(2*L+1)-TAUCUM(2*L))) |
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191 | |
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192 | EP = EXP(EXPTRM(L)) |
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193 | |
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194 | EM = 1.0/EP |
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195 | G4 = 1.0-G3(L) |
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196 | DENOM = LAMDA(L)**2 - 1./UBAR0**2 |
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197 | |
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198 | C THERE IS A POTENTIAL PROBLEM HERE IF W0=0 AND UBARV=UBAR0 |
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199 | C THEN DENOM WILL VANISH. THIS ONLY HAPPENS PHYSICALLY WHEN |
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200 | C THE SCATTERING GOES TO ZERO |
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201 | C PREVENT THIS WITH A IF STATEMENT |
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202 | |
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203 | |
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204 | IF ( DENOM .EQ. 0.) THEN |
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205 | DENOM=1.E-10 |
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206 | END IF |
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207 | |
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208 | AM = F0PI*W0(L)*(G4 *(G1(L)+1./UBAR0) +G2(L)*G3(L) )/DENOM |
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209 | AP = F0PI*W0(L)*(G3(L)*(G1(L)-1./UBAR0) +G2(L)*G4 )/DENOM |
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210 | |
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211 | C CPMID AND CMMID ARE THE CPLUS AND CMINUS TERMS EVALUATED |
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212 | C AT THE MIDDLE OF THE LAYER. |
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213 | |
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214 | TAUMID = TAUCUM(2*L+1) |
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215 | |
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216 | CPMID = AP*EXP(-TAUMID/UBAR0) |
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217 | CMMID = AM*EXP(-TAUMID/UBAR0) |
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218 | |
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219 | FMIDP(L) = XK1(L)*EP + GAMA(L)*XK2(L)*EM + CPMID |
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220 | FMIDM(L) = XK1(L)*EP*GAMA(L) + XK2(L)*EM + CMMID |
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221 | |
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222 | C ADD THE DIRECT FLUX TO THE DOWNWELLING TERM |
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223 | |
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224 | FMIDM(L)= FMIDM(L)+UBAR0*F0PI*EXP(-MIN(TAUMID,TAUMAX)/UBAR0) |
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225 | |
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226 | END DO |
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227 | |
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228 | C FLUX AT THE Ptop layer |
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229 | |
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230 | EP = 1.0 |
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231 | EM = 1.0 |
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232 | G4 = 1.0-G3(1) |
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233 | DENOM = LAMDA(1)**2 - 1./UBAR0**2 |
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234 | |
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235 | C THERE IS A POTENTIAL PROBLEM HERE IF W0=0 AND UBARV=UBAR0 |
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236 | C THEN DENOM WILL VANISH. THIS ONLY HAPPENS PHYSICALLY WHEN |
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237 | C THE SCATTERING GOES TO ZERO |
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238 | C PREVENT THIS WITH A IF STATEMENT |
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239 | |
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240 | IF ( DENOM .EQ. 0.) THEN |
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241 | DENOM=1.E-10 |
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242 | END IF |
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243 | |
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244 | AM = F0PI*W0(1)*(G4 *(G1(1)+1./UBAR0) +G2(1)*G3(1) )/DENOM |
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245 | AP = F0PI*W0(1)*(G3(1)*(G1(1)-1./UBAR0) +G2(1)*G4 )/DENOM |
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246 | |
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247 | C CPMID AND CMMID ARE THE CPLUS AND CMINUS TERMS EVALUATED |
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248 | C AT THE MIDDLE OF THE LAYER. |
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249 | |
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250 | CPMID = AP |
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251 | CMMID = AM |
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252 | |
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253 | FLUXUP = XK1(1)*EP + GAMA(1)*XK2(1)*EM + CPMID |
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254 | FLUXDN = XK1(1)*EP*GAMA(1) + XK2(1)*EM + CMMID |
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255 | |
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256 | C ADD THE DIRECT FLUX TO THE DOWNWELLING TERM |
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257 | |
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258 | fluxdn = fluxdn+UBAR0*F0PI*EXP(-MIN(TAUCUM(1),TAUMAX)/UBAR0) |
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259 | |
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260 | C This is for the "special" bottom layer, where we take |
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261 | C DTAU instead of DTAU/2. |
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262 | |
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263 | L = L_NLAYRAD |
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264 | EXPTRM(L) = MIN(TAUMAX,LAMDA(L)*(TAUCUM(L_LEVELS)- |
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265 | * TAUCUM(L_LEVELS-1))) |
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266 | |
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267 | EP = EXP(EXPTRM(L)) |
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268 | EM = 1.0/EP |
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269 | G4 = 1.0-G3(L) |
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270 | DENOM = LAMDA(L)**2 - 1./UBAR0**2 |
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271 | |
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272 | |
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273 | |
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274 | C THERE IS A POTENTIAL PROBLEM HERE IF W0=0 AND UBARV=UBAR0 |
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275 | C THEN DENOM WILL VANISH. THIS ONLY HAPPENS PHYSICALLY WHEN |
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276 | C THE SCATTERING GOES TO ZERO |
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277 | C PREVENT THIS WITH A IF STATEMENT |
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278 | |
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279 | |
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280 | IF ( DENOM .EQ. 0.) THEN |
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281 | DENOM=1.E-10 |
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282 | END IF |
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283 | |
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284 | AM = F0PI*W0(L)*(G4 *(G1(L)+1./UBAR0) +G2(L)*G3(L) )/DENOM |
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285 | AP = F0PI*W0(L)*(G3(L)*(G1(L)-1./UBAR0) +G2(L)*G4 )/DENOM |
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286 | |
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287 | C CPMID AND CMMID ARE THE CPLUS AND CMINUS TERMS EVALUATED |
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288 | C AT THE MIDDLE OF THE LAYER. |
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289 | |
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290 | TAUMID = MIN(TAUCUM(L_LEVELS),TAUMAX) |
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291 | CPMID = AP*EXP(-MIN(TAUMID,TAUMAX)/UBAR0) |
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292 | CMMID = AM*EXP(-MIN(TAUMID,TAUMAX)/UBAR0) |
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293 | |
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294 | |
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295 | FMIDP(L) = XK1(L)*EP + GAMA(L)*XK2(L)*EM + CPMID |
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296 | FMIDM(L) = XK1(L)*EP*GAMA(L) + XK2(L)*EM + CMMID |
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297 | |
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298 | C Save the diffuse downward flux for TEMPGR calculations |
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299 | |
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300 | DIFFV = FMIDM(L) |
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301 | |
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302 | |
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303 | C ADD THE DIRECT FLUX TO THE DOWNWELLING TERM |
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304 | |
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305 | FMIDM(L)= FMIDM(L)+UBAR0*F0PI*EXP(-MIN(TAUMID,TAUMAX)/UBAR0) |
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306 | |
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307 | |
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308 | |
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309 | |
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310 | RETURN |
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311 | |
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312 | |
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313 | END |
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