1 | subroutine vdifc(ngrid,nlay,nq,rnat,ppopsk, |
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2 | & ptimestep,pcapcal,lecrit, |
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3 | & pplay,pplev,pzlay,pzlev,pz0, |
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4 | & pu,pv,ph,pq,ptsrf,pemis,pqsurf, |
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5 | & pdufi,pdvfi,pdhfi,pdqfi,pfluxsrf, |
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6 | & pdudif,pdvdif,pdhdif,pdtsrf,sensibFlux,pq2, |
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7 | & pdqdif,pdqsdif,lastcall) |
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8 | |
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9 | use watercommon_h, only : RLVTT, T_h2O_ice_liq, RCPD, mx_eau_sol |
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10 | use radcommon_h, only : sigma |
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11 | USE surfdat_h |
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12 | USE comgeomfi_h |
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13 | USE tracer_h |
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14 | |
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15 | implicit none |
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16 | |
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17 | !================================================================== |
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18 | ! |
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19 | ! Purpose |
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20 | ! ------- |
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21 | ! Turbulent diffusion (mixing) for pot. T, U, V and tracers |
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22 | ! |
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23 | ! Implicit scheme |
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24 | ! We start by adding to variables x the physical tendencies |
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25 | ! already computed. We resolve the equation: |
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26 | ! |
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27 | ! x(t+1) = x(t) + dt * (dx/dt)phys(t) + dt * (dx/dt)difv(t+1) |
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28 | ! |
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29 | ! Authors |
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30 | ! ------- |
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31 | ! F. Hourdin, F. Forget, R. Fournier (199X) |
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32 | ! R. Wordsworth, B. Charnay (2010) |
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33 | ! |
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34 | !================================================================== |
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35 | |
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36 | !----------------------------------------------------------------------- |
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37 | ! declarations |
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38 | ! ------------ |
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39 | |
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40 | !----------------------------------------------------------------------- |
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41 | ! INCLUDE 'dimensions.h' |
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42 | ! |
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43 | ! dimensions.h contient les dimensions du modele |
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44 | ! ndm est tel que iim=2**ndm |
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45 | !----------------------------------------------------------------------- |
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46 | |
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47 | INTEGER iim,jjm,llm,ndm |
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48 | |
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49 | PARAMETER (iim= 128,jjm=96,llm=64,ndm=1) |
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50 | |
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51 | !----------------------------------------------------------------------- |
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52 | !----------------------------------------------------------------------- |
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53 | ! INCLUDE 'dimphys.h' |
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54 | |
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55 | ! ngridmx : number of horizontal grid points |
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56 | ! note: the -1/jjm term will be 0; unless jj=1 |
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57 | integer, parameter :: ngridmx = (2+(jjm-1)*iim - 1/jjm) |
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58 | ! nlayermx : number of atmospheric layers |
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59 | integer, parameter :: nlayermx = llm |
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60 | ! nsoilmx : number of subterranean layers ! nsoilmx is now in comsoil_h |
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61 | !integer, parameter :: nsoilmx = 4 ! for a test |
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62 | !integer, parameter :: nsoilmx = 18 ! for z1=0.0002 m, depth = 18 m => mars case |
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63 | !integer, parameter :: nsoilmx = 13 ! for z1=0.03 m, depth = 104.8 m => earth case |
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64 | !----------------------------------------------------------------------- |
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65 | |
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66 | !----------------------------------------------------------------------- |
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67 | ! INCLUDE "comcstfi.h" |
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68 | |
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69 | common/comcstfi/pi,rad,g,r,cpp,rcp,dtphys,daysec,mugaz,omeg |
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70 | common/comcstfi/avocado!,molrad,visc |
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71 | |
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72 | real pi,rad,g,r,cpp,rcp,dtphys,daysec,mugaz,omeg |
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73 | real avocado!,molrad,visc |
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74 | |
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75 | ! |
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76 | ! For Fortran 77/Fortran 90 compliance always use line continuation |
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77 | ! symbols '&' in columns 73 and 6 |
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78 | ! |
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79 | ! Group commons according to their type for minimal performance impact |
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80 | |
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81 | COMMON/callkeys_l/callrad,corrk,calldifv,UseTurbDiff,calladj & |
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82 | & , co2cond,callsoil & |
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83 | & , season,diurnal,tlocked,rings_shadow,lwrite & |
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84 | & , callstats,calleofdump & |
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85 | & , enertest & |
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86 | & , callgasvis,continuum,H2Ocont_simple,graybody & |
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87 | & , radfixed & |
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88 | & , meanOLR, specOLR & |
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89 | & , kastprof & |
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90 | & , nosurf, oblate & |
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91 | & , newtonian, testradtimes & |
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92 | & , check_cpp_match, force_cpp & |
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93 | & , rayleigh & |
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94 | & , stelbbody & |
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95 | & , nearco2cond & |
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96 | & , tracer, mass_redistrib, varactive, varfixed & |
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97 | & , sedimentation,water,watercond,waterrain & |
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98 | & , aeroco2,aeroh2o,aeroh2so4,aeroback2lay & |
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99 | & , aerofixco2,aerofixh2o & |
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100 | & , hydrology, sourceevol & |
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101 | & , CLFvarying & |
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102 | & , strictboundcorrk & |
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103 | & , ok_slab_ocean & |
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104 | & , ok_slab_sic & |
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105 | & , ok_slab_heat_transp |
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106 | |
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107 | |
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108 | COMMON/callkeys_i/iaervar,iddist,iradia,startype |
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109 | |
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110 | COMMON/callkeys_r/topdustref,Nmix_co2,dusttau,Fat1AU,stelTbb, & |
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111 | & Tstrat,tplanet,obs_tau_col_tropo, & |
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112 | & obs_tau_col_strato,pres_bottom_tropo, & |
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113 | & pres_top_tropo,pres_bottom_strato, & |
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114 | & pres_top_strato,size_tropo,size_strato,satval, & |
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115 | & CLFfixval,n2mixratio,co2supsat,pceil,albedosnow,& |
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116 | & maxicethick,Tsaldiff,tau_relax,cloudlvl, & |
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117 | & icetstep,intheat,flatten,Rmean,J2,MassPlanet |
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118 | |
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119 | logical callrad,corrk,calldifv,UseTurbDiff & |
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120 | & , calladj,co2cond,callsoil & |
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121 | & , season,diurnal,tlocked,rings_shadow,lwrite & |
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122 | & , callstats,calleofdump & |
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123 | & , callgasvis,continuum,H2Ocont_simple,graybody & |
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124 | & , strictboundcorrk |
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125 | |
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126 | logical enertest |
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127 | logical nonideal |
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128 | logical meanOLR |
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129 | logical specOLR |
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130 | logical kastprof |
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131 | logical newtonian |
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132 | logical check_cpp_match |
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133 | logical force_cpp |
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134 | logical testradtimes |
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135 | logical rayleigh |
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136 | logical stelbbody |
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137 | logical ozone |
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138 | logical nearco2cond |
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139 | logical tracer |
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140 | logical mass_redistrib |
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141 | logical varactive |
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142 | logical varfixed |
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143 | logical radfixed |
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144 | logical sedimentation |
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145 | logical water,watercond,waterrain |
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146 | logical aeroco2,aeroh2o,aeroh2so4,aeroback2lay |
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147 | logical aerofixco2,aerofixh2o |
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148 | logical hydrology |
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149 | logical sourceevol |
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150 | logical CLFvarying |
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151 | logical nosurf |
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152 | logical oblate |
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153 | logical ok_slab_ocean |
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154 | logical ok_slab_sic |
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155 | logical ok_slab_heat_transp |
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156 | |
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157 | integer iddist |
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158 | integer iaervar |
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159 | integer iradia |
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160 | integer startype |
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161 | |
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162 | real topdustref |
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163 | real Nmix_co2 |
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164 | real dusttau |
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165 | real Fat1AU |
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166 | real stelTbb |
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167 | real Tstrat |
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168 | real tplanet |
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169 | real obs_tau_col_tropo |
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170 | real obs_tau_col_strato |
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171 | real pres_bottom_tropo |
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172 | real pres_top_tropo |
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173 | real pres_bottom_strato |
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174 | real pres_top_strato |
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175 | real size_tropo |
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176 | real size_strato |
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177 | real satval |
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178 | real CLFfixval |
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179 | real n2mixratio |
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180 | real co2supsat |
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181 | real pceil |
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182 | real albedosnow |
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183 | real maxicethick |
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184 | real Tsaldiff |
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185 | real tau_relax |
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186 | real cloudlvl |
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187 | real icetstep |
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188 | real intheat |
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189 | real flatten |
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190 | real Rmean |
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191 | real J2 |
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192 | real MassPlanet |
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193 | |
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194 | ! arguments |
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195 | ! --------- |
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196 | INTEGER ngrid,nlay |
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197 | REAL ptimestep |
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198 | REAL pplay(ngrid,nlay),pplev(ngrid,nlay+1) |
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199 | REAL pzlay(ngrid,nlay),pzlev(ngrid,nlay+1) |
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200 | REAL pu(ngrid,nlay),pv(ngrid,nlay),ph(ngrid,nlay) |
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201 | REAL ptsrf(ngrid),pemis(ngrid) |
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202 | REAL pdufi(ngrid,nlay),pdvfi(ngrid,nlay),pdhfi(ngrid,nlay) |
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203 | REAL pfluxsrf(ngrid) |
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204 | REAL pdudif(ngrid,nlay),pdvdif(ngrid,nlay),pdhdif(ngrid,nlay) |
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205 | REAL pdtsrf(ngrid),sensibFlux(ngrid),pcapcal(ngrid) |
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206 | REAL pq2(ngrid,nlay+1) |
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207 | |
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208 | real rnat(ngrid) |
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209 | |
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210 | ! Arguments added for condensation |
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211 | REAL ppopsk(ngrid,nlay) |
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212 | logical lecrit |
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213 | REAL pz0 |
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214 | |
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215 | ! Tracers |
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216 | ! -------- |
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217 | integer nq |
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218 | real pqsurf(ngrid,nq) |
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219 | real pq(ngrid,nlay,nq), pdqfi(ngrid,nlay,nq) |
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220 | real pdqdif(ngrid,nlay,nq) |
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221 | real pdqsdif(ngrid,nq) |
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222 | |
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223 | ! local |
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224 | ! ----- |
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225 | integer ilev,ig,ilay,nlev |
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226 | |
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227 | REAL z4st,zdplanck(ngrid) |
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228 | REAL zkv(ngrid,nlayermx+1),zkh(ngrid,nlayermx+1) |
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229 | REAL zcdv(ngrid),zcdh(ngrid) |
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230 | REAL zcdv_true(ngrid),zcdh_true(ngrid) |
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231 | REAL zu(ngrid,nlayermx),zv(ngrid,nlayermx) |
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232 | REAL zh(ngrid,nlayermx) |
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233 | REAL ztsrf2(ngrid) |
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234 | REAL z1(ngrid),z2(ngrid) |
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235 | REAL za(ngrid,nlayermx),zb(ngrid,nlayermx) |
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236 | REAL zb0(ngrid,nlayermx) |
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237 | REAL zc(ngrid,nlayermx),zd(ngrid,nlayermx) |
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238 | REAL zcst1 |
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239 | REAL zu2!, a |
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240 | REAL zcq(ngrid,nlayermx),zdq(ngrid,nlayermx) |
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241 | REAL evap(ngrid) |
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242 | REAL zcq0(ngrid),zdq0(ngrid) |
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243 | REAL zx_alf1(ngrid),zx_alf2(ngrid) |
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244 | |
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245 | LOGICAL firstcall |
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246 | SAVE firstcall |
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247 | |
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248 | LOGICAL lastcall |
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249 | |
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250 | ! variables added for CO2 condensation |
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251 | ! ------------------------------------ |
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252 | REAL hh !, zhcond(ngrid,nlayermx) |
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253 | ! REAL latcond,tcond1mb |
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254 | ! REAL acond,bcond |
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255 | ! SAVE acond,bcond |
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256 | ! DATA latcond,tcond1mb/5.9e5,136.27/ |
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257 | |
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258 | ! Tracers |
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259 | ! ------- |
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260 | INTEGER iq |
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261 | REAL zq(ngrid,nlayermx,nq) |
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262 | REAL zq1temp(ngrid) |
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263 | REAL rho(ngrid) ! near-surface air density |
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264 | REAL qsat(ngrid) |
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265 | DATA firstcall/.true./ |
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266 | REAL kmixmin |
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267 | |
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268 | ! Variables added for implicit latent heat inclusion |
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269 | ! -------------------------------------------------- |
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270 | real latconst, dqsat(ngrid), qsat_temp1, qsat_temp2 |
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271 | real z1_Tdry(ngrid), z2_Tdry(ngrid) |
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272 | real z1_T(ngrid), z2_T(ngrid) |
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273 | real zb_T(ngrid) |
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274 | real zc_T(ngrid,nlayermx) |
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275 | real zd_T(ngrid,nlayermx) |
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276 | real lat1(ngrid), lat2(ngrid) |
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277 | real surfh2otot |
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278 | logical surffluxdiag |
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279 | integer isub ! sub-loop for precision |
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280 | |
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281 | integer ivap, iice ! also make liq for clarity on surface... |
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282 | save ivap, iice |
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283 | |
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284 | real, parameter :: karman=0.4 |
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285 | real cd0, roughratio |
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286 | |
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287 | logical forceWC |
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288 | real masse, Wtot, Wdiff |
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289 | |
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290 | real dqsdif_total(ngrid) |
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291 | real zq0(ngrid) |
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292 | |
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293 | forceWC=.true. |
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294 | ! forceWC=.false. |
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295 | |
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296 | |
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297 | ! Coherence test |
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298 | ! -------------- |
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299 | |
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300 | IF (firstcall) THEN |
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301 | ! To compute: Tcond= 1./(bcond-acond*log(.0095*p)) (p in pascal) |
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302 | ! bcond=1./tcond1mb |
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303 | ! acond=r/latcond |
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304 | ! PRINT*,'In vdifc: Tcond(P=1mb)=',tcond1mb,' Lcond=',latcond |
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305 | ! PRINT*,' acond,bcond',acond,bcond |
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306 | |
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307 | if(water)then |
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308 | ! iliq=igcm_h2o_vap |
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309 | ivap=igcm_h2o_vap |
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310 | iice=igcm_h2o_ice ! simply to make the code legible |
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311 | ! to be generalised later |
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312 | endif |
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313 | |
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314 | firstcall=.false. |
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315 | ENDIF |
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316 | |
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317 | !----------------------------------------------------------------------- |
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318 | ! 1. Initialisation |
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319 | ! ----------------- |
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320 | |
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321 | nlev=nlay+1 |
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322 | |
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323 | ! Calculate rho*dz and dt*rho/dz=dt*rho**2 g/dp |
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324 | ! with rho=p/RT=p/ (R Theta) (p/ps)**kappa |
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325 | ! --------------------------------------------- |
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326 | |
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327 | DO ilay=1,nlay |
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328 | DO ig=1,ngrid |
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329 | za(ig,ilay)=(pplev(ig,ilay)-pplev(ig,ilay+1))/g |
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330 | ENDDO |
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331 | ENDDO |
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332 | |
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333 | zcst1=4.*g*ptimestep/(R*R) |
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334 | DO ilev=2,nlev-1 |
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335 | DO ig=1,ngrid |
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336 | zb0(ig,ilev)=pplev(ig,ilev)* |
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337 | s (pplev(ig,1)/pplev(ig,ilev))**rcp / |
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338 | s (ph(ig,ilev-1)+ph(ig,ilev)) |
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339 | zb0(ig,ilev)=zcst1*zb0(ig,ilev)*zb0(ig,ilev)/ |
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340 | s (pplay(ig,ilev-1)-pplay(ig,ilev)) |
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341 | ENDDO |
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342 | ENDDO |
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343 | DO ig=1,ngrid |
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344 | zb0(ig,1)=ptimestep*pplev(ig,1)/(R*ptsrf(ig)) |
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345 | ENDDO |
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346 | |
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347 | dqsdif_total(:)=0.0 |
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348 | |
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349 | !----------------------------------------------------------------------- |
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350 | ! 2. Add the physical tendencies computed so far |
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351 | ! ---------------------------------------------- |
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352 | |
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353 | DO ilev=1,nlay |
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354 | DO ig=1,ngrid |
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355 | zu(ig,ilev)=pu(ig,ilev)+pdufi(ig,ilev)*ptimestep |
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356 | zv(ig,ilev)=pv(ig,ilev)+pdvfi(ig,ilev)*ptimestep |
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357 | zh(ig,ilev)=ph(ig,ilev)+pdhfi(ig,ilev)*ptimestep |
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358 | ENDDO |
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359 | ENDDO |
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360 | if(tracer) then |
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361 | DO iq =1, nq |
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362 | DO ilev=1,nlay |
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363 | DO ig=1,ngrid |
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364 | zq(ig,ilev,iq)=pq(ig,ilev,iq) + |
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365 | & pdqfi(ig,ilev,iq)*ptimestep |
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366 | ENDDO |
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367 | ENDDO |
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368 | ENDDO |
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369 | end if |
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370 | |
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371 | !----------------------------------------------------------------------- |
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372 | ! 3. Turbulence scheme |
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373 | ! -------------------- |
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374 | ! |
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375 | ! Source of turbulent kinetic energy at the surface |
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376 | ! ------------------------------------------------- |
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377 | ! Formula is Cd_0 = (karman / log[1+z1/z0])^2 |
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378 | |
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379 | DO ig=1,ngrid |
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380 | roughratio = 1.E+0 + pzlay(ig,1)/pz0 |
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381 | cd0 = karman/log(roughratio) |
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382 | cd0 = cd0*cd0 |
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383 | zcdv_true(ig) = cd0 |
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384 | zcdh_true(ig) = cd0 |
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385 | if (nosurf) then |
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386 | zcdv_true(ig) = 0. !! disable sensible momentum flux |
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387 | zcdh_true(ig) = 0. !! disable sensible heat flux |
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388 | endif |
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389 | ENDDO |
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390 | |
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391 | DO ig=1,ngrid |
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392 | zu2=pu(ig,1)*pu(ig,1)+pv(ig,1)*pv(ig,1) |
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393 | zcdv(ig)=zcdv_true(ig)*sqrt(zu2) |
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394 | zcdh(ig)=zcdh_true(ig)*sqrt(zu2) |
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395 | ENDDO |
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396 | |
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397 | ! Turbulent diffusion coefficients in the boundary layer |
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398 | ! ------------------------------------------------------ |
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399 | |
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400 | call vdif_kc(ngrid,ptimestep,g,pzlev,pzlay |
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401 | & ,pu,pv,ph,zcdv_true |
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402 | & ,pq2,zkv,zkh) |
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403 | |
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404 | ! Adding eddy mixing to mimic 3D general circulation in 1D |
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405 | ! R. Wordsworth & F. Forget (2010) |
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406 | if ((ngrid.eq.1)) then |
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407 | kmixmin = 1.0e-2 ! minimum eddy mix coeff in 1D |
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408 | do ilev=1,nlay |
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409 | do ig=1,ngrid |
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410 | !zkh(ig,ilev) = 1.0 |
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411 | zkh(ig,ilev) = max(kmixmin,zkh(ig,ilev)) |
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412 | zkv(ig,ilev) = max(kmixmin,zkv(ig,ilev)) |
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413 | end do |
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414 | end do |
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415 | end if |
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416 | |
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417 | !----------------------------------------------------------------------- |
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418 | ! 4. Implicit inversion of u |
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419 | ! -------------------------- |
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420 | |
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421 | ! u(t+1) = u(t) + dt * {(du/dt)phys}(t) + dt * {(du/dt)difv}(t+1) |
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422 | ! avec |
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423 | ! /zu/ = u(t) + dt * {(du/dt)phys}(t) (voir paragraphe 2.) |
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424 | ! et |
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425 | ! dt * {(du/dt)difv}(t+1) = dt * {(d/dz)[ Ku (du/dz) ]}(t+1) |
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426 | ! donc les entrees sont /zcdv/ pour la condition a la limite sol |
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427 | ! et /zkv/ = Ku |
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428 | |
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429 | CALL multipl((nlay-1)*ngrid,zkv(1,2),zb0(1,2),zb(1,2)) |
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430 | CALL multipl(ngrid,zcdv,zb0,zb) |
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431 | |
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432 | DO ig=1,ngrid |
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433 | z1(ig)=1./(za(ig,nlay)+zb(ig,nlay)) |
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434 | zc(ig,nlay)=za(ig,nlay)*zu(ig,nlay)*z1(ig) |
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435 | zd(ig,nlay)=zb(ig,nlay)*z1(ig) |
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436 | ENDDO |
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437 | |
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438 | DO ilay=nlay-1,1,-1 |
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439 | DO ig=1,ngrid |
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440 | z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+ |
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441 | $ zb(ig,ilay+1)*(1.-zd(ig,ilay+1))) |
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442 | zc(ig,ilay)=(za(ig,ilay)*zu(ig,ilay)+ |
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443 | $ zb(ig,ilay+1)*zc(ig,ilay+1))*z1(ig) |
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444 | zd(ig,ilay)=zb(ig,ilay)*z1(ig) |
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445 | ENDDO |
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446 | ENDDO |
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447 | |
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448 | DO ig=1,ngrid |
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449 | zu(ig,1)=zc(ig,1) |
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450 | ENDDO |
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451 | DO ilay=2,nlay |
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452 | DO ig=1,ngrid |
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453 | zu(ig,ilay)=zc(ig,ilay)+zd(ig,ilay)*zu(ig,ilay-1) |
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454 | ENDDO |
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455 | ENDDO |
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456 | |
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457 | !----------------------------------------------------------------------- |
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458 | ! 5. Implicit inversion of v |
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459 | ! -------------------------- |
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460 | |
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461 | ! v(t+1) = v(t) + dt * {(dv/dt)phys}(t) + dt * {(dv/dt)difv}(t+1) |
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462 | ! avec |
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463 | ! /zv/ = v(t) + dt * {(dv/dt)phys}(t) (voir paragraphe 2.) |
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464 | ! et |
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465 | ! dt * {(dv/dt)difv}(t+1) = dt * {(d/dz)[ Kv (dv/dz) ]}(t+1) |
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466 | ! donc les entrees sont /zcdv/ pour la condition a la limite sol |
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467 | ! et /zkv/ = Kv |
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468 | |
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469 | DO ig=1,ngrid |
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470 | z1(ig)=1./(za(ig,nlay)+zb(ig,nlay)) |
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471 | zc(ig,nlay)=za(ig,nlay)*zv(ig,nlay)*z1(ig) |
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472 | zd(ig,nlay)=zb(ig,nlay)*z1(ig) |
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473 | ENDDO |
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474 | |
---|
475 | DO ilay=nlay-1,1,-1 |
---|
476 | DO ig=1,ngrid |
---|
477 | z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+ |
---|
478 | $ zb(ig,ilay+1)*(1.-zd(ig,ilay+1))) |
---|
479 | zc(ig,ilay)=(za(ig,ilay)*zv(ig,ilay)+ |
---|
480 | $ zb(ig,ilay+1)*zc(ig,ilay+1))*z1(ig) |
---|
481 | zd(ig,ilay)=zb(ig,ilay)*z1(ig) |
---|
482 | ENDDO |
---|
483 | ENDDO |
---|
484 | |
---|
485 | DO ig=1,ngrid |
---|
486 | zv(ig,1)=zc(ig,1) |
---|
487 | ENDDO |
---|
488 | DO ilay=2,nlay |
---|
489 | DO ig=1,ngrid |
---|
490 | zv(ig,ilay)=zc(ig,ilay)+zd(ig,ilay)*zv(ig,ilay-1) |
---|
491 | ENDDO |
---|
492 | ENDDO |
---|
493 | |
---|
494 | !---------------------------------------------------------------------------- |
---|
495 | ! 6. Implicit inversion of h, not forgetting the coupling with the ground |
---|
496 | |
---|
497 | ! h(t+1) = h(t) + dt * {(dh/dt)phys}(t) + dt * {(dh/dt)difv}(t+1) |
---|
498 | ! avec |
---|
499 | ! /zh/ = h(t) + dt * {(dh/dt)phys}(t) (voir paragraphe 2.) |
---|
500 | ! et |
---|
501 | ! dt * {(dh/dt)difv}(t+1) = dt * {(d/dz)[ Kh (dh/dz) ]}(t+1) |
---|
502 | ! donc les entrees sont /zcdh/ pour la condition de raccord au sol |
---|
503 | ! et /zkh/ = Kh |
---|
504 | |
---|
505 | ! Using the wind modified by friction for lifting and sublimation |
---|
506 | ! --------------------------------------------------------------- |
---|
507 | DO ig=1,ngrid |
---|
508 | zu2 = zu(ig,1)*zu(ig,1)+zv(ig,1)*zv(ig,1) |
---|
509 | zcdv(ig) = zcdv_true(ig)*sqrt(zu2) |
---|
510 | zcdh(ig) = zcdh_true(ig)*sqrt(zu2) |
---|
511 | ENDDO |
---|
512 | |
---|
513 | CALL multipl((nlay-1)*ngrid,zkh(1,2),zb0(1,2),zb(1,2)) |
---|
514 | CALL multipl(ngrid,zcdh,zb0,zb) |
---|
515 | |
---|
516 | DO ig=1,ngrid |
---|
517 | z1(ig)=1./(za(ig,nlay)+zb(ig,nlay)) |
---|
518 | zc(ig,nlay)=za(ig,nlay)*zh(ig,nlay)*z1(ig) |
---|
519 | zd(ig,nlay)=zb(ig,nlay)*z1(ig) |
---|
520 | ENDDO |
---|
521 | |
---|
522 | DO ilay=nlay-1,2,-1 |
---|
523 | DO ig=1,ngrid |
---|
524 | z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+ |
---|
525 | & zb(ig,ilay+1)*(1.-zd(ig,ilay+1))) |
---|
526 | zc(ig,ilay)=(za(ig,ilay)*zh(ig,ilay)+ |
---|
527 | & zb(ig,ilay+1)*zc(ig,ilay+1))*z1(ig) |
---|
528 | zd(ig,ilay)=zb(ig,ilay)*z1(ig) |
---|
529 | ENDDO |
---|
530 | ENDDO |
---|
531 | |
---|
532 | DO ig=1,ngrid |
---|
533 | z1(ig)=1./(za(ig,1)+zb(ig,1)+ |
---|
534 | & zb(ig,2)*(1.-zd(ig,2))) |
---|
535 | zc(ig,1)=(za(ig,1)*zh(ig,1)+ |
---|
536 | & zb(ig,2)*zc(ig,2))*z1(ig) |
---|
537 | zd(ig,1)=zb(ig,1)*z1(ig) |
---|
538 | ENDDO |
---|
539 | |
---|
540 | ! Calculate (d Planck / dT) at the interface temperature |
---|
541 | ! ------------------------------------------------------ |
---|
542 | |
---|
543 | z4st=4.0*sigma*ptimestep |
---|
544 | DO ig=1,ngrid |
---|
545 | zdplanck(ig)=z4st*pemis(ig)*ptsrf(ig)*ptsrf(ig)*ptsrf(ig) |
---|
546 | ENDDO |
---|
547 | |
---|
548 | ! Calculate temperature tendency at the interface (dry case) |
---|
549 | ! ---------------------------------------------------------- |
---|
550 | ! Sum of fluxes at interface at time t + \delta t gives change in T: |
---|
551 | ! radiative fluxes |
---|
552 | ! turbulent convective (sensible) heat flux |
---|
553 | ! flux (if any) from subsurface |
---|
554 | |
---|
555 | if(.not.water) then |
---|
556 | |
---|
557 | DO ig=1,ngrid |
---|
558 | |
---|
559 | z1(ig) = pcapcal(ig)*ptsrf(ig) + cpp*zb(ig,1)*zc(ig,1) |
---|
560 | & + zdplanck(ig)*ptsrf(ig) + pfluxsrf(ig)*ptimestep |
---|
561 | z2(ig) = pcapcal(ig) + cpp*zb(ig,1)*(1.-zd(ig,1)) |
---|
562 | & +zdplanck(ig) |
---|
563 | ztsrf2(ig) = z1(ig) / z2(ig) |
---|
564 | pdtsrf(ig) = (ztsrf2(ig) - ptsrf(ig))/ptimestep |
---|
565 | zh(ig,1) = zc(ig,1) + zd(ig,1)*ztsrf2(ig) |
---|
566 | ENDDO |
---|
567 | |
---|
568 | ! Recalculate temperature to top of atmosphere, starting from ground |
---|
569 | ! ------------------------------------------------------------------ |
---|
570 | |
---|
571 | DO ilay=2,nlay |
---|
572 | DO ig=1,ngrid |
---|
573 | hh = zh(ig,ilay-1) |
---|
574 | zh(ig,ilay)=zc(ig,ilay)+zd(ig,ilay)*hh |
---|
575 | ENDDO |
---|
576 | ENDDO |
---|
577 | |
---|
578 | endif ! not water |
---|
579 | |
---|
580 | !----------------------------------------------------------------------- |
---|
581 | ! TRACERS (no vapour) |
---|
582 | ! ------- |
---|
583 | |
---|
584 | if(tracer) then |
---|
585 | |
---|
586 | ! Calculate vertical flux from the bottom to the first layer (dust) |
---|
587 | ! ----------------------------------------------------------------- |
---|
588 | do ig=1,ngrid |
---|
589 | rho(ig) = zb0(ig,1) /ptimestep |
---|
590 | end do |
---|
591 | |
---|
592 | call zerophys(ngrid*nq,pdqsdif) |
---|
593 | |
---|
594 | ! Implicit inversion of q |
---|
595 | ! ----------------------- |
---|
596 | do iq=1,nq |
---|
597 | |
---|
598 | if (iq.ne.igcm_h2o_vap) then |
---|
599 | |
---|
600 | DO ig=1,ngrid |
---|
601 | z1(ig)=1./(za(ig,nlay)+zb(ig,nlay)) |
---|
602 | zcq(ig,nlay)=za(ig,nlay)*zq(ig,nlay,iq)*z1(ig) |
---|
603 | zdq(ig,nlay)=zb(ig,nlay)*z1(ig) |
---|
604 | ENDDO |
---|
605 | |
---|
606 | DO ilay=nlay-1,2,-1 |
---|
607 | DO ig=1,ngrid |
---|
608 | z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+ |
---|
609 | & zb(ig,ilay+1)*(1.-zdq(ig,ilay+1))) |
---|
610 | zcq(ig,ilay)=(za(ig,ilay)*zq(ig,ilay,iq)+ |
---|
611 | & zb(ig,ilay+1)*zcq(ig,ilay+1))*z1(ig) |
---|
612 | zdq(ig,ilay)=zb(ig,ilay)*z1(ig) |
---|
613 | ENDDO |
---|
614 | ENDDO |
---|
615 | |
---|
616 | if ((water).and.(iq.eq.iice)) then |
---|
617 | ! special case for water ice tracer: do not include |
---|
618 | ! h2o ice tracer from surface (which is set when handling |
---|
619 | ! h2o vapour case (see further down). |
---|
620 | ! zb(ig,1)=0 if iq ne ivap |
---|
621 | DO ig=1,ngrid |
---|
622 | z1(ig)=1./(za(ig,1)+ |
---|
623 | & zb(ig,2)*(1.-zdq(ig,2))) |
---|
624 | zcq(ig,1)=(za(ig,1)*zq(ig,1,iq)+ |
---|
625 | & zb(ig,2)*zcq(ig,2))*z1(ig) |
---|
626 | ENDDO |
---|
627 | else ! general case |
---|
628 | DO ig=1,ngrid |
---|
629 | z1(ig)=1./(za(ig,1)+ |
---|
630 | & zb(ig,2)*(1.-zdq(ig,2))) |
---|
631 | zcq(ig,1)=(za(ig,1)*zq(ig,1,iq)+ |
---|
632 | & zb(ig,2)*zcq(ig,2) |
---|
633 | & +(-pdqsdif(ig,iq))*ptimestep)*z1(ig) |
---|
634 | ! tracer flux from surface |
---|
635 | ! currently pdqsdif always zero here, |
---|
636 | ! so last line is superfluous |
---|
637 | enddo |
---|
638 | endif ! of if (water.and.(iq.eq.igcm_h2o_ice)) |
---|
639 | |
---|
640 | |
---|
641 | ! Starting upward calculations for simple tracer mixing (e.g., dust) |
---|
642 | do ig=1,ngrid |
---|
643 | zq(ig,1,iq)=zcq(ig,1) |
---|
644 | end do |
---|
645 | |
---|
646 | do ilay=2,nlay |
---|
647 | do ig=1,ngrid |
---|
648 | zq(ig,ilay,iq)=zcq(ig,ilay)+ |
---|
649 | $ zdq(ig,ilay)*zq(ig,ilay-1,iq) |
---|
650 | end do |
---|
651 | end do |
---|
652 | |
---|
653 | endif ! if (iq.ne.igcm_h2o_vap) |
---|
654 | |
---|
655 | ! Calculate temperature tendency including latent heat term |
---|
656 | ! and assuming an infinite source of water on the ground |
---|
657 | ! ------------------------------------------------------------------ |
---|
658 | |
---|
659 | if (water.and.(iq.eq.igcm_h2o_vap)) then |
---|
660 | |
---|
661 | ! compute evaporation efficiency |
---|
662 | do ig = 1, ngrid |
---|
663 | if(nint(rnat(ig)).eq.1)then |
---|
664 | dryness(ig)=pqsurf(ig,ivap)+pqsurf(ig,iice) |
---|
665 | dryness(ig)=MIN(1.,2*dryness(ig)/mx_eau_sol) |
---|
666 | dryness(ig)=MAX(0.,dryness(ig)) |
---|
667 | endif |
---|
668 | enddo |
---|
669 | |
---|
670 | do ig=1,ngrid |
---|
671 | |
---|
672 | ! Calculate the value of qsat at the surface (water) |
---|
673 | call watersat(ptsrf(ig),pplev(ig,1),qsat(ig)) |
---|
674 | call watersat(ptsrf(ig)-0.0001,pplev(ig,1),qsat_temp1) |
---|
675 | call watersat(ptsrf(ig)+0.0001,pplev(ig,1),qsat_temp2) |
---|
676 | dqsat(ig)=(qsat_temp2-qsat_temp1)/0.0002 |
---|
677 | ! calculate dQsat / dT by finite differences |
---|
678 | ! we cannot use the updated temperature value yet... |
---|
679 | |
---|
680 | enddo |
---|
681 | |
---|
682 | ! coefficients for q |
---|
683 | |
---|
684 | do ig=1,ngrid |
---|
685 | z1(ig)=1./(za(ig,nlay)+zb(ig,nlay)) |
---|
686 | zcq(ig,nlay)=za(ig,nlay)*zq(ig,nlay,iq)*z1(ig) |
---|
687 | zdq(ig,nlay)=zb(ig,nlay)*z1(ig) |
---|
688 | enddo |
---|
689 | |
---|
690 | do ilay=nlay-1,2,-1 |
---|
691 | do ig=1,ngrid |
---|
692 | z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+ |
---|
693 | $ zb(ig,ilay+1)*(1.-zdq(ig,ilay+1))) |
---|
694 | zcq(ig,ilay)=(za(ig,ilay)*zq(ig,ilay,iq)+ |
---|
695 | $ zb(ig,ilay+1)*zcq(ig,ilay+1))*z1(ig) |
---|
696 | zdq(ig,ilay)=zb(ig,ilay)*z1(ig) |
---|
697 | enddo |
---|
698 | enddo |
---|
699 | |
---|
700 | do ig=1,ngrid |
---|
701 | z1(ig)=1./(za(ig,1)+zb(ig,1)*dryness(ig)+ |
---|
702 | $ zb(ig,2)*(1.-zdq(ig,2))) |
---|
703 | zcq(ig,1)=(za(ig,1)*zq(ig,1,iq)+ |
---|
704 | $ zb(ig,2)*zcq(ig,2))*z1(ig) |
---|
705 | zdq(ig,1)=dryness(ig)*zb(ig,1)*z1(ig) |
---|
706 | enddo |
---|
707 | |
---|
708 | ! calculation of h0 and h1 |
---|
709 | do ig=1,ngrid |
---|
710 | zdq0(ig) = dqsat(ig) |
---|
711 | zcq0(ig) = qsat(ig)-dqsat(ig)*ptsrf(ig) |
---|
712 | |
---|
713 | z1(ig) = pcapcal(ig)*ptsrf(ig) +cpp*zb(ig,1)*zc(ig,1) |
---|
714 | & + zdplanck(ig)*ptsrf(ig) + pfluxsrf(ig)*ptimestep |
---|
715 | & + zb(ig,1)*dryness(ig)*RLVTT* |
---|
716 | & ((zdq(ig,1)-1.0)*zcq0(ig)+zcq(ig,1)) |
---|
717 | |
---|
718 | z2(ig) = pcapcal(ig) + cpp*zb(ig,1)*(1.-zd(ig,1)) |
---|
719 | & +zdplanck(ig) |
---|
720 | & +zb(ig,1)*dryness(ig)*RLVTT*zdq0(ig)* |
---|
721 | & (1.0-zdq(ig,1)) |
---|
722 | |
---|
723 | ztsrf2(ig) = z1(ig) / z2(ig) |
---|
724 | pdtsrf(ig) = (ztsrf2(ig) - ptsrf(ig))/ptimestep |
---|
725 | zh(ig,1) = zc(ig,1) + zd(ig,1)*ztsrf2(ig) |
---|
726 | enddo |
---|
727 | |
---|
728 | ! calculation of qs and q1 |
---|
729 | do ig=1,ngrid |
---|
730 | zq0(ig) = zcq0(ig)+zdq0(ig)*ztsrf2(ig) |
---|
731 | zq(ig,1,iq) = zcq(ig,1)+zdq(ig,1)*zq0(ig) |
---|
732 | enddo |
---|
733 | |
---|
734 | ! calculation of evaporation |
---|
735 | do ig=1,ngrid |
---|
736 | evap(ig)= zb(ig,1)*dryness(ig)*(zq(ig,1,ivap)-zq0(ig)) |
---|
737 | dqsdif_total(ig)=evap(ig) |
---|
738 | enddo |
---|
739 | |
---|
740 | ! recalculate temperature and q(vap) to top of atmosphere, starting from ground |
---|
741 | do ilay=2,nlay |
---|
742 | do ig=1,ngrid |
---|
743 | zq(ig,ilay,iq)=zcq(ig,ilay) |
---|
744 | & +zdq(ig,ilay)*zq(ig,ilay-1,iq) |
---|
745 | zh(ig,ilay)=zc(ig,ilay)+zd(ig,ilay)*zh(ig,ilay-1) |
---|
746 | end do |
---|
747 | end do |
---|
748 | |
---|
749 | do ig=1,ngrid |
---|
750 | |
---|
751 | ! -------------------------------------------------------------------------- |
---|
752 | ! On the ocean, if T > 0 C then the vapour tendency must replace the ice one |
---|
753 | ! The surface vapour tracer is actually liquid. To make things difficult. |
---|
754 | |
---|
755 | if (nint(rnat(ig)).eq.0) then ! unfrozen ocean |
---|
756 | |
---|
757 | pdqsdif(ig,ivap)=dqsdif_total(ig)/ptimestep |
---|
758 | pdqsdif(ig,iice)=0.0 |
---|
759 | |
---|
760 | |
---|
761 | elseif (nint(rnat(ig)).eq.1) then ! (continent) |
---|
762 | |
---|
763 | ! -------------------------------------------------------- |
---|
764 | ! Now check if we've taken too much water from the surface |
---|
765 | ! This can only occur on the continent |
---|
766 | |
---|
767 | ! If water is evaporating / subliming, we take it from ice before liquid |
---|
768 | ! -- is this valid?? |
---|
769 | if(dqsdif_total(ig).lt.0)then |
---|
770 | pdqsdif(ig,iice)=dqsdif_total(ig)/ptimestep |
---|
771 | pdqsdif(ig,iice)=max(-pqsurf(ig,iice)/ptimestep |
---|
772 | & ,pdqsdif(ig,iice)) |
---|
773 | endif |
---|
774 | ! sublimation only greater than qsurf(ice) |
---|
775 | ! ---------------------------------------- |
---|
776 | ! we just convert some liquid to vapour too |
---|
777 | ! if latent heats are the same, no big deal |
---|
778 | if (-dqsdif_total(ig).gt.pqsurf(ig,iice))then |
---|
779 | pdqsdif(ig,iice) = -pqsurf(ig,iice)/ptimestep ! removes all the ice! |
---|
780 | pdqsdif(ig,ivap) = dqsdif_total(ig)/ptimestep |
---|
781 | & - pdqsdif(ig,iice) ! take the remainder from the liquid instead |
---|
782 | pdqsdif(ig,ivap) = max(-pqsurf(ig,ivap)/ptimestep |
---|
783 | & ,pdqsdif(ig,ivap)) |
---|
784 | endif |
---|
785 | |
---|
786 | endif ! if (rnat.ne.1) |
---|
787 | |
---|
788 | ! If water vapour is condensing, we must decide whether it forms ice or liquid. |
---|
789 | if(dqsdif_total(ig).gt.0)then ! a bug was here! |
---|
790 | if(ztsrf2(ig).gt.T_h2O_ice_liq)then |
---|
791 | pdqsdif(ig,iice)=0.0 |
---|
792 | pdqsdif(ig,ivap)=dqsdif_total(ig)/ptimestep |
---|
793 | else |
---|
794 | pdqsdif(ig,iice)=dqsdif_total(ig)/ptimestep |
---|
795 | pdqsdif(ig,ivap)=0.0 |
---|
796 | endif |
---|
797 | endif |
---|
798 | |
---|
799 | end do ! of DO ig=1,ngrid |
---|
800 | endif ! if (water et iq=ivap) |
---|
801 | end do ! of do iq=1,nq |
---|
802 | endif ! traceur |
---|
803 | |
---|
804 | |
---|
805 | !----------------------------------------------------------------------- |
---|
806 | ! 8. Final calculation of the vertical diffusion tendencies |
---|
807 | ! ----------------------------------------------------------------- |
---|
808 | |
---|
809 | do ilev = 1, nlay |
---|
810 | do ig=1,ngrid |
---|
811 | pdudif(ig,ilev)=(zu(ig,ilev)- |
---|
812 | & (pu(ig,ilev)+pdufi(ig,ilev)*ptimestep))/ptimestep |
---|
813 | pdvdif(ig,ilev)=(zv(ig,ilev)- |
---|
814 | & (pv(ig,ilev)+pdvfi(ig,ilev)*ptimestep))/ptimestep |
---|
815 | hh = ph(ig,ilev)+pdhfi(ig,ilev)*ptimestep |
---|
816 | |
---|
817 | pdhdif(ig,ilev)=( zh(ig,ilev)- hh )/ptimestep |
---|
818 | enddo |
---|
819 | enddo |
---|
820 | |
---|
821 | DO ig=1,ngrid ! computing sensible heat flux (atm => surface) |
---|
822 | sensibFlux(ig)=cpp*zb(ig,1)/ptimestep*(zh(ig,1)-ztsrf2(ig)) |
---|
823 | ENDDO |
---|
824 | |
---|
825 | if (tracer) then |
---|
826 | do iq = 1, nq |
---|
827 | do ilev = 1, nlay |
---|
828 | do ig=1,ngrid |
---|
829 | pdqdif(ig,ilev,iq)=(zq(ig,ilev,iq)- |
---|
830 | & (pq(ig,ilev,iq)+pdqfi(ig,ilev,iq)*ptimestep))/ |
---|
831 | & ptimestep |
---|
832 | enddo |
---|
833 | enddo |
---|
834 | enddo |
---|
835 | |
---|
836 | if(water.and.forceWC)then ! force water conservation in model |
---|
837 | ! we calculate the difference and add it to the ground |
---|
838 | ! this is ugly and should be improved in the future |
---|
839 | do ig=1,ngrid |
---|
840 | Wtot=0.0 |
---|
841 | do ilay=1,nlay |
---|
842 | masse = (pplev(ig,ilay) - pplev(ig,ilay+1))/g |
---|
843 | ! Wtot=Wtot+masse*(zq(ig,ilay,iice)- |
---|
844 | ! & (pq(ig,ilay,iice)+pdqfi(ig,ilay,iice)*ptimestep)) |
---|
845 | Wtot=Wtot+masse*(zq(ig,ilay,ivap)- |
---|
846 | & (pq(ig,ilay,ivap)+pdqfi(ig,ilay,ivap)*ptimestep)) |
---|
847 | enddo |
---|
848 | Wdiff=Wtot/ptimestep+pdqsdif(ig,ivap)+pdqsdif(ig,iice) |
---|
849 | |
---|
850 | if(ztsrf2(ig).gt.T_h2O_ice_liq)then |
---|
851 | pdqsdif(ig,ivap)=pdqsdif(ig,ivap)-Wdiff |
---|
852 | else |
---|
853 | pdqsdif(ig,iice)=pdqsdif(ig,iice)-Wdiff |
---|
854 | endif |
---|
855 | enddo |
---|
856 | |
---|
857 | endif |
---|
858 | |
---|
859 | endif |
---|
860 | |
---|
861 | if(water)then |
---|
862 | call writediagfi(ngrid,'beta','Dryness coefficient',' ',2,dryness) |
---|
863 | endif |
---|
864 | |
---|
865 | ! if(lastcall)then |
---|
866 | ! if(ngrid.eq.1)then |
---|
867 | ! print*,'Saving k.out...' |
---|
868 | ! OPEN(12,file='k.out',form='formatted') |
---|
869 | ! DO ilay=1,nlay |
---|
870 | ! write(12,*) zkh(1,ilay), pplay(1,ilay) |
---|
871 | ! ENDDO |
---|
872 | ! CLOSE(12) |
---|
873 | ! endif |
---|
874 | ! endif |
---|
875 | |
---|
876 | |
---|
877 | return |
---|
878 | end |
---|