1 | MODULE lmdz_lscp_tools |
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2 | |
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3 | IMPLICIT NONE |
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4 | |
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5 | CONTAINS |
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6 | |
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7 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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8 | SUBROUTINE FALLICE_VELOCITY(klon,iwc,temp,rho,pres,ptconv,velo) |
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9 | |
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10 | ! Ref: |
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11 | ! Stubenrauch, C. J., Bonazzola, M., |
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12 | ! Protopapadaki, S. E., & Musat, I. (2019). |
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13 | ! New cloud system metrics to assess bulk |
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14 | ! ice cloud schemes in a GCM. Journal of |
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15 | ! Advances in Modeling Earth Systems, 11, |
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16 | ! 3212–3234. https://doi.org/10.1029/2019MS001642 |
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17 | |
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18 | use lmdz_lscp_ini, only: iflag_vice, ffallv_con, ffallv_lsc |
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19 | use lmdz_lscp_ini, only: cice_velo, dice_velo |
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20 | |
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21 | IMPLICIT NONE |
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22 | |
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23 | INTEGER, INTENT(IN) :: klon |
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24 | REAL, INTENT(IN), DIMENSION(klon) :: iwc ! specific ice water content [kg/m3] |
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25 | REAL, INTENT(IN), DIMENSION(klon) :: temp ! temperature [K] |
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26 | REAL, INTENT(IN), DIMENSION(klon) :: rho ! dry air density [kg/m3] |
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27 | REAL, INTENT(IN), DIMENSION(klon) :: pres ! air pressure [Pa] |
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28 | LOGICAL, INTENT(IN), DIMENSION(klon) :: ptconv ! convective point [-] |
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29 | |
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30 | REAL, INTENT(OUT), DIMENSION(klon) :: velo ! fallspeed velocity of crystals [m/s] |
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31 | |
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32 | |
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33 | INTEGER i |
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34 | REAL logvm,iwcg,tempc,phpa,fallv_tun |
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35 | REAL m2ice, m2snow, vmice, vmsnow |
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36 | REAL aice, bice, asnow, bsnow |
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37 | |
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38 | |
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39 | DO i=1,klon |
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40 | |
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41 | IF (ptconv(i)) THEN |
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42 | fallv_tun=ffallv_con |
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43 | ELSE |
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44 | fallv_tun=ffallv_lsc |
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45 | ENDIF |
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46 | |
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47 | tempc=temp(i)-273.15 ! celcius temp |
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48 | iwcg=MAX(iwc(i)*1000.,1E-3) ! iwc in g/m3. We set a minimum value to prevent from division by 0 |
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49 | phpa=pres(i)/100. ! pressure in hPa |
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50 | |
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51 | IF (iflag_vice .EQ. 1) THEN |
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52 | ! so-called 'empirical parameterization' in Stubenrauch et al. 2019 |
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53 | if (tempc .GE. -60.0) then |
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54 | |
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55 | logvm= -0.0000414122*tempc*tempc*log(iwcg)-0.00538922*tempc*log(iwcg) & |
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56 | -0.0516344*log(iwcg)+0.00216078*tempc + 1.9714 |
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57 | velo(i)=exp(logvm) |
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58 | else |
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59 | velo(i)=65.0*(iwcg**0.2)*(150./phpa)**0.15 |
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60 | endif |
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61 | |
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62 | velo(i)=fallv_tun*velo(i)/100.0 ! from cm/s to m/s |
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63 | |
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64 | ELSE IF (iflag_vice .EQ. 2) THEN |
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65 | ! so called PSDM empirical coherent bulk ice scheme in Stubenrauch et al. 2019 |
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66 | aice=0.587 |
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67 | bice=2.45 |
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68 | asnow=0.0444 |
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69 | bsnow=2.1 |
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70 | |
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71 | m2ice=((iwcg*0.001/aice)/(exp(13.6-bice*7.76+0.479*bice**2)* & |
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72 | exp((-0.0361+bice*0.0151+0.00149*bice**2)*tempc))) & |
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73 | **(1./(0.807+bice*0.00581+0.0457*bice**2)) |
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74 | |
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75 | vmice=100.*1042.4*exp(13.6-(bice+1)*7.76+0.479*(bice+1.)**2)*exp((-0.0361+ & |
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76 | (bice+1.)*0.0151+0.00149*(bice+1.)**2)*tempc) & |
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77 | *(m2ice**(0.807+(bice+1.)*0.00581+0.0457*(bice+1.)**2))/(iwcg*0.001/aice) |
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78 | |
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79 | |
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80 | vmice=vmice*((1000./phpa)**0.2) |
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81 | |
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82 | m2snow=((iwcg*0.001/asnow)/(exp(13.6-bsnow*7.76+0.479*bsnow**2)* & |
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83 | exp((-0.0361+bsnow*0.0151+0.00149*bsnow**2)*tempc))) & |
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84 | **(1./(0.807+bsnow*0.00581+0.0457*bsnow**2)) |
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85 | |
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86 | |
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87 | vmsnow=100.*14.3*exp(13.6-(bsnow+.416)*7.76+0.479*(bsnow+.416)**2)& |
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88 | *exp((-0.0361+(bsnow+.416)*0.0151+0.00149*(bsnow+.416)**2)*tempc)& |
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89 | *(m2snow**(0.807+(bsnow+.416)*0.00581+0.0457*(bsnow+.416)**2))/(iwcg*0.001/asnow) |
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90 | |
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91 | vmsnow=vmsnow*((1000./phpa)**0.35) |
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92 | velo(i)=fallv_tun*min(vmsnow,vmice)/100. ! to m/s |
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93 | |
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94 | ELSE |
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95 | ! By default, fallspeed velocity of ice crystals according to Heymsfield & Donner 1990 |
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96 | velo(i) = fallv_tun*cice_velo*((iwcg/1000.)**dice_velo) |
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97 | ENDIF |
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98 | ENDDO |
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99 | |
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100 | END SUBROUTINE FALLICE_VELOCITY |
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101 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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102 | |
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103 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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104 | SUBROUTINE ICEFRAC_LSCP(klon, temp, iflag_ice_thermo, distcltop, temp_cltop, icefrac, dicefracdT) |
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105 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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106 | |
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107 | ! Compute the ice fraction 1-xliq (see e.g. |
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108 | ! Doutriaux-Boucher & Quaas 2004, section 2.2.) |
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109 | ! as a function of temperature |
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110 | ! see also Fig 3 of Madeleine et al. 2020, JAMES |
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111 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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112 | |
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113 | |
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114 | USE print_control_mod, ONLY: lunout, prt_level |
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115 | USE lmdz_lscp_ini, ONLY: t_glace_min, t_glace_max, exposant_glace, iflag_t_glace |
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116 | USE lmdz_lscp_ini, ONLY : RTT, dist_liq, temp_nowater |
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117 | |
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118 | IMPLICIT NONE |
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119 | |
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120 | |
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121 | INTEGER, INTENT(IN) :: klon ! number of horizontal grid points |
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122 | REAL, INTENT(IN), DIMENSION(klon) :: temp ! temperature |
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123 | REAL, INTENT(IN), DIMENSION(klon) :: distcltop ! distance to cloud top |
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124 | REAL, INTENT(IN), DIMENSION(klon) :: temp_cltop ! temperature of cloud top |
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125 | INTEGER, INTENT(IN) :: iflag_ice_thermo |
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126 | REAL, INTENT(OUT), DIMENSION(klon) :: icefrac |
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127 | REAL, INTENT(OUT), DIMENSION(klon) :: dicefracdT |
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128 | |
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129 | |
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130 | INTEGER i |
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131 | REAL liqfrac_tmp, dicefrac_tmp |
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132 | REAL Dv, denomdep,beta,qsi,dqsidt |
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133 | LOGICAL ice_thermo |
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134 | |
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135 | CHARACTER (len = 20) :: modname = 'lscp_tools' |
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136 | CHARACTER (len = 80) :: abort_message |
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137 | |
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138 | IF ((iflag_t_glace.LT.2) .OR. (iflag_t_glace.GT.6)) THEN |
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139 | abort_message = 'lscp cannot be used if iflag_t_glace<2 or >6' |
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140 | CALL abort_physic(modname,abort_message,1) |
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141 | ENDIF |
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142 | |
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143 | IF (.NOT.((iflag_ice_thermo .EQ. 1).OR.(iflag_ice_thermo .GE. 3))) THEN |
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144 | abort_message = 'lscp cannot be used without ice thermodynamics' |
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145 | CALL abort_physic(modname,abort_message,1) |
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146 | ENDIF |
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147 | |
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148 | |
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149 | DO i=1,klon |
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150 | |
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151 | ! old function with sole dependence upon temperature |
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152 | IF (iflag_t_glace .EQ. 2) THEN |
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153 | liqfrac_tmp = (temp(i)-t_glace_min) / (t_glace_max-t_glace_min) |
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154 | liqfrac_tmp = MIN(MAX(liqfrac_tmp,0.0),1.0) |
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155 | icefrac(i) = (1.0-liqfrac_tmp)**exposant_glace |
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156 | IF (icefrac(i) .GT.0.) THEN |
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157 | dicefracdT(i)= exposant_glace * (icefrac(i)**(exposant_glace-1.)) & |
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158 | / (t_glace_min - t_glace_max) |
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159 | ENDIF |
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160 | |
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161 | IF ((icefrac(i).EQ.0).OR.(icefrac(i).EQ.1)) THEN |
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162 | dicefracdT(i)=0. |
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163 | ENDIF |
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164 | |
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165 | ENDIF |
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166 | |
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167 | ! function of temperature used in CMIP6 physics |
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168 | IF (iflag_t_glace .EQ. 3) THEN |
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169 | liqfrac_tmp = (temp(i)-t_glace_min) / (t_glace_max-t_glace_min) |
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170 | liqfrac_tmp = MIN(MAX(liqfrac_tmp,0.0),1.0) |
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171 | icefrac(i) = 1.0-liqfrac_tmp**exposant_glace |
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172 | IF ((icefrac(i) .GT.0.) .AND. (liqfrac_tmp .GT. 0.)) THEN |
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173 | dicefracdT(i)= exposant_glace * ((liqfrac_tmp)**(exposant_glace-1.)) & |
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174 | / (t_glace_min - t_glace_max) |
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175 | ELSE |
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176 | dicefracdT(i)=0. |
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177 | ENDIF |
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178 | ENDIF |
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179 | |
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180 | ! for iflag_t_glace .GE. 4, the liquid fraction depends upon temperature at cloud top |
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181 | ! and then decreases with decreasing height |
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182 | |
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183 | !with linear function of temperature at cloud top |
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184 | IF (iflag_t_glace .EQ. 4) THEN |
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185 | liqfrac_tmp = (temp(i)-t_glace_min) / (t_glace_max-t_glace_min) |
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186 | liqfrac_tmp = MIN(MAX(liqfrac_tmp,0.0),1.0) |
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187 | icefrac(i) = MAX(MIN(1.,1.0 - liqfrac_tmp*exp(-distcltop(i)/dist_liq)),0.) |
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188 | dicefrac_tmp = - temp(i)/(t_glace_max-t_glace_min) |
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189 | dicefracdT(i) = dicefrac_tmp*exp(-distcltop(i)/dist_liq) |
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190 | IF ((liqfrac_tmp .LE.0) .OR. (liqfrac_tmp .GE. 1)) THEN |
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191 | dicefracdT(i) = 0. |
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192 | ENDIF |
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193 | ENDIF |
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194 | |
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195 | ! with CMIP6 function of temperature at cloud top |
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196 | IF (iflag_t_glace .EQ. 5) THEN |
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197 | liqfrac_tmp = (temp(i)-t_glace_min) / (t_glace_max-t_glace_min) |
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198 | liqfrac_tmp = MIN(MAX(liqfrac_tmp,0.0),1.0) |
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199 | liqfrac_tmp = liqfrac_tmp**exposant_glace |
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200 | icefrac(i) = MAX(MIN(1.,1.0 - liqfrac_tmp*exp(-distcltop(i)/dist_liq)),0.) |
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201 | IF ((liqfrac_tmp .LE.0) .OR. (liqfrac_tmp .GE. 1)) THEN |
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202 | dicefracdT(i) = 0. |
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203 | ELSE |
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204 | dicefracdT(i) = exposant_glace*((liqfrac_tmp)**(exposant_glace-1.))/(t_glace_min- t_glace_max) & |
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205 | *exp(-distcltop(i)/dist_liq) |
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206 | ENDIF |
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207 | ENDIF |
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208 | |
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209 | ! with modified function of temperature at cloud top |
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210 | ! to get largere values around 260 K, works well with t_glace_min = 241K |
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211 | IF (iflag_t_glace .EQ. 6) THEN |
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212 | IF (temp(i) .GT. t_glace_max) THEN |
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213 | liqfrac_tmp = 1. |
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214 | ELSE |
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215 | liqfrac_tmp = -((temp(i)-t_glace_max) / (t_glace_max-t_glace_min))**2+1. |
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216 | ENDIF |
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217 | liqfrac_tmp = MIN(MAX(liqfrac_tmp,0.0),1.0) |
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218 | icefrac(i) = MAX(MIN(1.,1.0 - liqfrac_tmp*exp(-distcltop(i)/dist_liq)),0.) |
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219 | IF ((liqfrac_tmp .LE.0) .OR. (liqfrac_tmp .GE. 1)) THEN |
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220 | dicefracdT(i) = 0. |
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221 | ELSE |
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222 | dicefracdT(i) = 2*((temp(i)-t_glace_max) / (t_glace_max-t_glace_min))/(t_glace_max-t_glace_min) & |
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223 | *exp(-distcltop(i)/dist_liq) |
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224 | ENDIF |
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225 | ENDIF |
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226 | |
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227 | ! if temperature of cloud top <-40°C, |
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228 | IF (iflag_t_glace .GE. 4) THEN |
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229 | IF ((temp_cltop(i) .LE. temp_nowater) .AND. (temp(i) .LE. t_glace_max)) THEN |
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230 | icefrac(i) = 1. |
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231 | dicefracdT(i) = 0. |
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232 | ENDIF |
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233 | ENDIF |
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234 | |
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235 | |
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236 | ENDDO ! klon |
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237 | |
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238 | RETURN |
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239 | |
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240 | END SUBROUTINE ICEFRAC_LSCP |
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241 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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242 | |
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243 | |
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244 | |
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245 | SUBROUTINE CALC_QSAT_ECMWF(klon,temp,qtot,pressure,tref,phase,flagth,qs,dqs) |
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246 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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247 | ! Calculate qsat following ECMWF method |
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248 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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249 | |
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250 | |
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251 | IMPLICIT NONE |
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252 | |
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253 | include "YOMCST.h" |
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254 | include "YOETHF.h" |
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255 | include "FCTTRE.h" |
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256 | |
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257 | INTEGER, INTENT(IN) :: klon ! number of horizontal grid points |
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258 | REAL, INTENT(IN), DIMENSION(klon) :: temp ! temperature in K |
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259 | REAL, INTENT(IN), DIMENSION(klon) :: qtot ! total specific water in kg/kg |
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260 | REAL, INTENT(IN), DIMENSION(klon) :: pressure ! pressure in Pa |
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261 | REAL, INTENT(IN) :: tref ! reference temperature in K |
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262 | LOGICAL, INTENT(IN) :: flagth ! flag for qsat calculation for thermals |
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263 | INTEGER, INTENT(IN) :: phase |
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264 | ! phase: 0=depend on temperature sign (temp>tref -> liquid, temp<tref, solid) |
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265 | ! 1=liquid |
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266 | ! 2=solid |
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267 | |
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268 | REAL, INTENT(OUT), DIMENSION(klon) :: qs ! saturation specific humidity [kg/kg] |
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269 | REAL, INTENT(OUT), DIMENSION(klon) :: dqs ! derivation of saturation specific humidity wrt T |
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270 | |
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271 | REAL delta, cor, cvm5 |
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272 | INTEGER i |
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273 | |
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274 | DO i=1,klon |
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275 | |
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276 | IF (phase .EQ. 1) THEN |
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277 | delta=0. |
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278 | ELSEIF (phase .EQ. 2) THEN |
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279 | delta=1. |
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280 | ELSE |
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281 | delta=MAX(0.,SIGN(1.,tref-temp(i))) |
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282 | ENDIF |
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283 | |
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284 | IF (flagth) THEN |
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285 | cvm5=R5LES*(1.-delta) + R5IES*delta |
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286 | ELSE |
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287 | cvm5 = R5LES*RLVTT*(1.-delta) + R5IES*RLSTT*delta |
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288 | cvm5 = cvm5 /RCPD/(1.0+RVTMP2*(qtot(i))) |
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289 | ENDIF |
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290 | |
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291 | qs(i)= R2ES*FOEEW(temp(i),delta)/pressure(i) |
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292 | qs(i)=MIN(0.5,qs(i)) |
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293 | cor=1./(1.-RETV*qs(i)) |
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294 | qs(i)=qs(i)*cor |
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295 | dqs(i)= FOEDE(temp(i),delta,cvm5,qs(i),cor) |
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296 | |
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297 | END DO |
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298 | |
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299 | END SUBROUTINE CALC_QSAT_ECMWF |
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300 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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301 | |
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302 | |
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303 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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304 | SUBROUTINE CALC_GAMMASAT(klon,temp,qtot,pressure,gammasat,dgammasatdt) |
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305 | |
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306 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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307 | ! programme that calculates the gammasat parameter that determines the |
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308 | ! homogeneous condensation thresholds for cold (<0oC) clouds |
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309 | ! condensation at q>gammasat*qsat |
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310 | ! Etienne Vignon, March 2021 |
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311 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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312 | |
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313 | use lmdz_lscp_ini, only: iflag_gammasat, t_glace_min, RTT |
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314 | |
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315 | IMPLICIT NONE |
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316 | |
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317 | |
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318 | INTEGER, INTENT(IN) :: klon ! number of horizontal grid points |
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319 | REAL, INTENT(IN), DIMENSION(klon) :: temp ! temperature in K |
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320 | REAL, INTENT(IN), DIMENSION(klon) :: qtot ! total specific water in kg/kg |
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321 | |
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322 | REAL, INTENT(IN), DIMENSION(klon) :: pressure ! pressure in Pa |
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323 | |
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324 | REAL, INTENT(OUT), DIMENSION(klon) :: gammasat ! coefficient to multiply qsat with to calculate saturation |
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325 | REAL, INTENT(OUT), DIMENSION(klon) :: dgammasatdt ! derivative of gammasat wrt temperature |
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326 | |
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327 | REAL, DIMENSION(klon) :: qsi,qsl,dqsl,dqsi |
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328 | REAL fcirrus, fac |
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329 | REAL, PARAMETER :: acirrus=2.349 |
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330 | REAL, PARAMETER :: bcirrus=259.0 |
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331 | |
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332 | INTEGER i |
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333 | |
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334 | CALL CALC_QSAT_ECMWF(klon,temp,qtot,pressure,RTT,1,.false.,qsl,dqsl) |
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335 | CALL CALC_QSAT_ECMWF(klon,temp,qtot,pressure,RTT,2,.false.,qsi,dqsi) |
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336 | |
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337 | DO i=1,klon |
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338 | |
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339 | IF (temp(i) .GE. RTT) THEN |
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340 | ! warm clouds: condensation at saturation wrt liquid |
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341 | gammasat(i)=1. |
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342 | dgammasatdt(i)=0. |
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343 | |
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344 | ELSEIF ((temp(i) .LT. RTT) .AND. (temp(i) .GT. t_glace_min)) THEN |
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345 | |
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346 | IF (iflag_gammasat .GE. 2) THEN |
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347 | gammasat(i)=qsl(i)/qsi(i) |
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348 | dgammasatdt(i)=(dqsl(i)*qsi(i)-dqsi(i)*qsl(i))/qsi(i)/qsi(i) |
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349 | ELSE |
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350 | gammasat(i)=1. |
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351 | dgammasatdt(i)=0. |
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352 | ENDIF |
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353 | |
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354 | ELSE |
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355 | |
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356 | IF (iflag_gammasat .GE.1) THEN |
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357 | ! homogeneous freezing of aerosols, according to |
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358 | ! Koop, 2000 and Karcher 2008, QJRMS |
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359 | ! 'Cirrus regime' |
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360 | fcirrus=acirrus-temp(i)/bcirrus |
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361 | IF (fcirrus .GT. qsl(i)/qsi(i)) THEN |
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362 | gammasat(i)=qsl(i)/qsi(i) |
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363 | dgammasatdt(i)=(dqsl(i)*qsi(i)-dqsi(i)*qsl(i))/qsi(i)/qsi(i) |
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364 | ELSE |
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365 | gammasat(i)=fcirrus |
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366 | dgammasatdt(i)=-1.0/bcirrus |
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367 | ENDIF |
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368 | |
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369 | ELSE |
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370 | |
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371 | gammasat(i)=1. |
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372 | dgammasatdt(i)=0. |
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373 | |
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374 | ENDIF |
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375 | |
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376 | ENDIF |
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377 | |
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378 | END DO |
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379 | |
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380 | |
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381 | END SUBROUTINE CALC_GAMMASAT |
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382 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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383 | |
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384 | |
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385 | !++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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386 | SUBROUTINE DISTANCE_TO_CLOUD_TOP(klon,klev,k,temp,pplay,paprs,rneb,distcltop1D,temp_cltop) |
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387 | !++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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388 | |
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389 | USE lmdz_lscp_ini, ONLY : rd,rg,tresh_cl |
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390 | |
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391 | IMPLICIT NONE |
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392 | |
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393 | INTEGER, INTENT(IN) :: klon,klev !number of horizontal and vertical grid points |
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394 | INTEGER, INTENT(IN) :: k ! vertical index |
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395 | REAL, INTENT(IN), DIMENSION(klon,klev) :: temp ! temperature in K |
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396 | REAL, INTENT(IN), DIMENSION(klon,klev) :: pplay ! pressure middle layer in Pa |
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397 | REAL, INTENT(IN), DIMENSION(klon,klev+1) :: paprs ! pressure interfaces in Pa |
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398 | REAL, INTENT(IN), DIMENSION(klon,klev) :: rneb ! cloud fraction |
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399 | |
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400 | REAL, INTENT(OUT), DIMENSION(klon) :: distcltop1D ! distance from cloud top |
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401 | REAL, INTENT(OUT), DIMENSION(klon) :: temp_cltop ! temperature of cloud top |
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402 | |
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403 | REAL dzlay(klon,klev) |
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404 | REAL zlay(klon,klev) |
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405 | REAL dzinterf |
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406 | INTEGER i,k_top, kvert |
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407 | LOGICAL bool_cl |
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408 | |
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409 | |
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410 | DO i=1,klon |
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411 | ! Initialization height middle of first layer |
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412 | dzlay(i,1) = Rd * temp(i,1) / rg * log(paprs(i,1)/paprs(i,2)) |
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413 | zlay(i,1) = dzlay(i,1)/2 |
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414 | |
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415 | DO kvert=2,klev |
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416 | IF (kvert.EQ.klev) THEN |
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417 | dzlay(i,kvert) = 2*(rd * temp(i,kvert) / rg * log(paprs(i,kvert)/pplay(i,kvert))) |
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418 | ELSE |
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419 | dzlay(i,kvert) = rd * temp(i,kvert) / rg * log(paprs(i,kvert)/paprs(i,kvert+1)) |
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420 | ENDIF |
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421 | dzinterf = rd * temp(i,kvert) / rg * log(pplay(i,kvert-1)/pplay(i,kvert)) |
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422 | zlay(i,kvert) = zlay(i,kvert-1) + dzinterf |
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423 | ENDDO |
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424 | ENDDO |
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425 | |
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426 | DO i=1,klon |
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427 | k_top = k |
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428 | IF (rneb(i,k) .LE. tresh_cl) THEN |
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429 | bool_cl = .FALSE. |
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430 | ELSE |
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431 | bool_cl = .TRUE. |
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432 | ENDIF |
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433 | |
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434 | DO WHILE ((bool_cl) .AND. (k_top .LE. klev)) |
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435 | ! find cloud top |
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436 | IF (rneb(i,k_top) .GT. tresh_cl) THEN |
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437 | k_top = k_top + 1 |
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438 | ELSE |
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439 | bool_cl = .FALSE. |
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440 | k_top = k_top - 1 |
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441 | ENDIF |
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442 | ENDDO |
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443 | k_top=min(k_top,klev) |
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444 | |
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445 | !dist to top is dist between current layer and layer of cloud top (from middle to middle) + dist middle to |
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446 | !interf for layer of cloud top |
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447 | distcltop1D(i) = zlay(i,k_top) - zlay(i,k) + dzlay(i,k_top)/2 |
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448 | temp_cltop(i) = temp(i,k_top) |
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449 | ENDDO ! klon |
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450 | |
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451 | END SUBROUTINE DISTANCE_TO_CLOUD_TOP |
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452 | !++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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453 | |
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454 | END MODULE lmdz_lscp_tools |
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455 | |
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456 | |
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