1 | ! $Id: newmicro.F 1337 2010-04-02 11:31:05Z acozic $ |
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2 | ! |
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3 | SUBROUTINE newmicro (paprs, pplay,ok_newmicro, |
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4 | . t, pqlwp, pclc, pcltau, pclemi, |
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5 | . pch, pcl, pcm, pct, pctlwp, |
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6 | s xflwp, xfiwp, xflwc, xfiwc, |
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7 | e ok_aie, |
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8 | e mass_solu_aero, mass_solu_aero_pi, |
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9 | e bl95_b0, bl95_b1, |
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10 | s cldtaupi, re, fl, reliq, reice) |
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11 | |
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12 | USE dimphy |
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13 | USE phys_local_var_mod, only: scdnc,cldncl,reffclwtop,lcc, |
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14 | . reffclws,reffclwc,cldnvi,lcc3d, |
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15 | . lcc3dcon,lcc3dstra |
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16 | USE phys_state_var_mod, only: rnebcon,clwcon |
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17 | IMPLICIT none |
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18 | c====================================================================== |
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19 | c Auteur(s): Z.X. Li (LMD/CNRS) date: 19930910 |
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20 | c Objet: Calculer epaisseur optique et emmissivite des nuages |
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21 | c====================================================================== |
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22 | c Arguments: |
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23 | c t-------input-R-temperature |
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24 | c pqlwp---input-R-eau liquide nuageuse dans l'atmosphere (kg/kg) |
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25 | c pclc----input-R-couverture nuageuse pour le rayonnement (0 a 1) |
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26 | c |
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27 | c ok_aie--input-L-apply aerosol indirect effect or not |
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28 | c mass_solu_aero-----input-R-total mass concentration for all soluble aerosols[ug/m^3] |
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29 | c mass_solu_aero_pi--input-R-dito, pre-industrial value |
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30 | c bl95_b0-input-R-a parameter, may be varied for tests (s-sea, l-land) |
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31 | c bl95_b1-input-R-a parameter, may be varied for tests ( -"- ) |
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32 | c |
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33 | c cldtaupi-output-R-pre-industrial value of cloud optical thickness, |
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34 | c needed for the diagnostics of the aerosol indirect |
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35 | c radiative forcing (see radlwsw) |
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36 | c re------output-R-Cloud droplet effective radius multiplied by fl [um] |
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37 | c fl------output-R-Denominator to re, introduced to avoid problems in |
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38 | c the averaging of the output. fl is the fraction of liquid |
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39 | c water clouds within a grid cell |
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40 | c pcltau--output-R-epaisseur optique des nuages |
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41 | c pclemi--output-R-emissivite des nuages (0 a 1) |
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42 | c====================================================================== |
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43 | C |
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44 | #include "YOMCST.h" |
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45 | c |
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46 | cym#include "dimensions.h" |
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47 | cym#include "dimphy.h" |
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48 | #include "nuage.h" |
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49 | cIM cf. CR: include pour NOVLP et ZEPSEC |
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50 | #include "radepsi.h" |
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51 | #include "radopt.h" |
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52 | c choix de l'hypothese de recouvrememnt nuageuse |
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53 | LOGICAL RANDOM,MAXIMUM_RANDOM,MAXIMUM,FIRST |
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54 | parameter (RANDOM=.FALSE., MAXIMUM_RANDOM=.TRUE., MAXIMUM=.FALSE.) |
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55 | c Hypoyhese de recouvrement : MAXIMUM_RANDOM |
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56 | INTEGER flag_max |
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57 | REAL phase3d(klon, klev),dh(klon, klev),pdel(klon, klev), |
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58 | . zrho(klon, klev) |
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59 | REAL tcc(klon), ftmp(klon), lcc_integrat(klon), height(klon) |
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60 | REAL thres_tau,thres_neb |
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61 | PARAMETER (thres_tau=0.3, thres_neb=0.001) |
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62 | REAL t_tmp |
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63 | REAL gravit |
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64 | PARAMETER (gravit=9.80616) !m/s2 |
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65 | REAL pqlwpcon(klon, klev), pqlwpstra(klon, klev) |
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66 | c |
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67 | REAL paprs(klon,klev+1), pplay(klon,klev) |
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68 | REAL t(klon,klev) |
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69 | c |
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70 | REAL pclc(klon,klev) |
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71 | REAL pqlwp(klon,klev) |
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72 | REAL pcltau(klon,klev), pclemi(klon,klev) |
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73 | c |
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74 | REAL pct(klon), pctlwp(klon), pch(klon), pcl(klon), pcm(klon) |
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75 | c |
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76 | LOGICAL lo |
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77 | c |
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78 | REAL cetahb, cetamb |
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79 | PARAMETER (cetahb = 0.45, cetamb = 0.80) |
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80 | C |
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81 | INTEGER i, k |
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82 | cIM: 091003 REAL zflwp, zradef, zfice, zmsac |
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83 | REAL zflwp(klon), zradef, zfice, zmsac |
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84 | cIM: 091003 rajout |
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85 | REAL xflwp(klon), xfiwp(klon) |
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86 | REAL xflwc(klon,klev), xfiwc(klon,klev) |
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87 | c |
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88 | REAL radius, rad_chaud |
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89 | cc PARAMETER (rad_chau1=13.0, rad_chau2=9.0, rad_froid=35.0) |
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90 | ccc PARAMETER (rad_chaud=15.0, rad_froid=35.0) |
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91 | c sintex initial PARAMETER (rad_chaud=10.0, rad_froid=30.0) |
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92 | REAL coef, coef_froi, coef_chau |
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93 | PARAMETER (coef_chau=0.13, coef_froi=0.09) |
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94 | REAL seuil_neb |
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95 | PARAMETER (seuil_neb=0.001) |
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96 | INTEGER nexpo ! exponentiel pour glace/eau |
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97 | PARAMETER (nexpo=6) |
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98 | ccc PARAMETER (nexpo=1) |
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99 | |
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100 | c -- sb: |
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101 | logical ok_newmicro |
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102 | c parameter (ok_newmicro=.FALSE.) |
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103 | cIM: 091003 real rel, tc, rei, zfiwp |
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104 | real rel, tc, rei, zfiwp(klon) |
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105 | real k_liq, k_ice0, k_ice, DF |
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106 | parameter (k_liq=0.0903, k_ice0=0.005) ! units=m2/g |
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107 | parameter (DF=1.66) ! diffusivity factor |
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108 | c sb -- |
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109 | cjq for the aerosol indirect effect |
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110 | cjq introduced by Johannes Quaas (quaas@lmd.jussieu.fr), 27/11/2003 |
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111 | cjq |
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112 | LOGICAL ok_aie ! Apply AIE or not? |
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113 | LOGICAL ok_a1lwpdep ! a1 LWP dependent? |
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114 | |
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115 | REAL mass_solu_aero(klon, klev) ! total mass concentration for all soluble aerosols [ug m-3] |
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116 | REAL mass_solu_aero_pi(klon, klev) ! - " - (pre-industrial value) |
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117 | REAL cdnc(klon, klev) ! cloud droplet number concentration [m-3] |
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118 | REAL re(klon, klev) ! cloud droplet effective radius [um] |
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119 | REAL cdnc_pi(klon, klev) ! cloud droplet number concentration [m-3] (pi value) |
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120 | REAL re_pi(klon, klev) ! cloud droplet effective radius [um] (pi value) |
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121 | |
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122 | REAL fl(klon, klev) ! xliq * rneb (denominator to re; fraction of liquid water clouds within the grid cell) |
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123 | |
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124 | REAL bl95_b0, bl95_b1 ! Parameter in B&L 95-Formula |
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125 | |
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126 | REAL cldtaupi(klon, klev) ! pre-industrial cloud opt thickness for diag |
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127 | cjq-end |
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128 | cIM cf. CR:parametres supplementaires |
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129 | REAL zclear(klon) |
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130 | REAL zcloud(klon) |
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131 | |
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132 | c ************************** |
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133 | c * * |
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134 | c * DEBUT PARTIE OPTIMISEE * |
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135 | c * * |
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136 | c ************************** |
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137 | |
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138 | REAL diff_paprs(klon, klev), zfice1, zfice2(klon, klev) |
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139 | REAL rad_chaud_tab(klon, klev), zflwp_var, zfiwp_var |
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140 | |
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141 | ! Abderrahmane oct 2009 |
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142 | Real reliq(klon, klev), reice(klon, klev) |
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143 | |
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144 | c |
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145 | c Calculer l'epaisseur optique et l'emmissivite des nuages |
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146 | c |
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147 | c IM inversion des DO |
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148 | xflwp = 0.d0 |
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149 | xfiwp = 0.d0 |
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150 | xflwc = 0.d0 |
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151 | xfiwc = 0.d0 |
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152 | |
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153 | ! Initialisation |
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154 | reliq=0. |
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155 | reice=0. |
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156 | |
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157 | DO k = 1, klev |
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158 | DO i = 1, klon |
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159 | diff_paprs(i,k) = (paprs(i,k)-paprs(i,k+1))/RG |
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160 | ENDDO |
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161 | ENDDO |
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162 | |
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163 | IF (ok_newmicro) THEN |
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164 | |
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165 | |
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166 | DO k = 1, klev |
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167 | DO i = 1, klon |
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168 | c zfice2(i,k) = 1.0 - (t(i,k)-t_glace) / (273.13-t_glace) |
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169 | zfice2(i,k) = 1.0 - (t(i,k)-t_glace_min) / |
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170 | & (t_glace_max-t_glace_min) |
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171 | zfice2(i,k) = MIN(MAX(zfice2(i,k),0.0),1.0) |
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172 | c IM Total Liquid/Ice water content |
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173 | xflwc(i,k) = (1.-zfice2(i,k))*pqlwp(i,k) |
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174 | xfiwc(i,k) = zfice2(i,k)*pqlwp(i,k) |
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175 | c IM In-Cloud Liquid/Ice water content |
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176 | c xflwc(i,k) = xflwc(i,k)+(1.-zfice)*pqlwp(i,k)/pclc(i,k) |
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177 | c xfiwc(i,k) = xfiwc(i,k)+zfice*pqlwp(i,k)/pclc(i,k) |
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178 | ENDDO |
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179 | ENDDO |
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180 | |
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181 | IF (ok_aie) THEN |
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182 | DO k = 1, klev |
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183 | DO i = 1, klon |
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184 | ! Formula "D" of Boucher and Lohmann, Tellus, 1995 |
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185 | ! |
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186 | cdnc(i,k) = 10.**(bl95_b0+bl95_b1* |
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187 | & log(MAX(mass_solu_aero(i,k),1.e-4))/log(10.))*1.e6 !-m-3 |
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188 | ! Cloud droplet number concentration (CDNC) is restricted |
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189 | ! to be within [20, 1000 cm^3] |
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190 | ! |
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191 | cdnc(i,k)=MIN(1000.e6,MAX(20.e6,cdnc(i,k))) |
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192 | ! |
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193 | ! |
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194 | cdnc_pi(i,k) = 10.**(bl95_b0+bl95_b1* |
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195 | & log(MAX(mass_solu_aero_pi(i,k),1.e-4))/log(10.)) |
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196 | & *1.e6 !-m-3 |
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197 | cdnc_pi(i,k)=MIN(1000.e6,MAX(20.e6,cdnc_pi(i,k))) |
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198 | ENDDO |
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199 | ENDDO |
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200 | DO k = 1, klev |
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201 | DO i = 1, klon |
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202 | ! rad_chaud_tab(i,k) = |
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203 | ! & MAX(1.1e6 |
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204 | ! & *((pqlwp(i,k)*pplay(i,k)/(RD * T(i,k))) |
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205 | ! & /(4./3*RPI*1000.*cdnc(i,k)) )**(1./3.),5.) |
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206 | rad_chaud_tab(i,k) = |
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207 | & 1.1 |
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208 | & *((pqlwp(i,k)*pplay(i,k)/(RD * T(i,k))) |
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209 | & /(4./3*RPI*1000.*cdnc(i,k)) )**(1./3.) |
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210 | rad_chaud_tab(i,k) = MAX(rad_chaud_tab(i,k) * 1e6, 5.) |
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211 | ENDDO |
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212 | ENDDO |
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213 | ELSE |
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214 | DO k = 1, MIN(3,klev) |
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215 | DO i = 1, klon |
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216 | rad_chaud_tab(i,k) = rad_chau2 |
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217 | ENDDO |
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218 | ENDDO |
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219 | DO k = MIN(3,klev)+1, klev |
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220 | DO i = 1, klon |
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221 | rad_chaud_tab(i,k) = rad_chau1 |
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222 | ENDDO |
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223 | ENDDO |
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224 | |
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225 | ENDIF |
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226 | |
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227 | DO k = 1, klev |
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228 | ! IF(.not.ok_aie) THEN |
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229 | rad_chaud = rad_chau1 |
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230 | IF (k.LE.3) rad_chaud = rad_chau2 |
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231 | ! ENDIF |
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232 | DO i = 1, klon |
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233 | IF (pclc(i,k) .LE. seuil_neb) THEN |
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234 | |
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235 | c -- effective cloud droplet radius (microns): |
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236 | |
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237 | c for liquid water clouds: |
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238 | ! For output diagnostics |
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239 | ! |
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240 | ! Cloud droplet effective radius [um] |
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241 | ! |
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242 | ! we multiply here with f * xl (fraction of liquid water |
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243 | ! clouds in the grid cell) to avoid problems in the |
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244 | ! averaging of the output. |
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245 | ! In the output of IOIPSL, derive the real cloud droplet |
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246 | ! effective radius as re/fl |
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247 | ! |
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248 | |
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249 | fl(i,k) = seuil_neb*(1.-zfice2(i,k)) |
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250 | re(i,k) = rad_chaud_tab(i,k)*fl(i,k) |
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251 | |
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252 | rel = 0. |
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253 | rei = 0. |
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254 | pclc(i,k) = 0.0 |
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255 | pcltau(i,k) = 0.0 |
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256 | pclemi(i,k) = 0.0 |
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257 | cldtaupi(i,k) = 0.0 |
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258 | ELSE |
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259 | |
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260 | c -- liquid/ice cloud water paths: |
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261 | |
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262 | zflwp_var= 1000.*(1.-zfice2(i,k))*pqlwp(i,k)/pclc(i,k) |
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263 | & *diff_paprs(i,k) |
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264 | zfiwp_var= 1000.*zfice2(i,k)*pqlwp(i,k)/pclc(i,k) |
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265 | & *diff_paprs(i,k) |
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266 | |
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267 | c -- effective cloud droplet radius (microns): |
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268 | |
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269 | c for liquid water clouds: |
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270 | |
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271 | IF (ok_aie) THEN |
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272 | radius = |
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273 | & 1.1 |
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274 | & *((pqlwp(i,k)*pplay(i,k)/(RD * T(i,k))) |
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275 | & /(4./3.*RPI*1000.*cdnc_pi(i,k)))**(1./3.) |
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276 | radius = MAX(radius*1e6, 5.) |
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277 | |
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278 | tc = t(i,k)-273.15 |
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279 | rei = 0.71*tc + 61.29 |
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280 | if (tc.le.-81.4) rei = 3.5 |
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281 | if (zflwp_var.eq.0.) radius = 1. |
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282 | if (zfiwp_var.eq.0. .or. rei.le.0.) rei = 1. |
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283 | cldtaupi(i,k) = 3.0/2.0 * zflwp_var / radius |
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284 | & + zfiwp_var * (3.448e-03 + 2.431/rei) |
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285 | |
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286 | ENDIF ! ok_aie |
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287 | ! For output diagnostics |
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288 | ! |
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289 | ! Cloud droplet effective radius [um] |
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290 | ! |
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291 | ! we multiply here with f * xl (fraction of liquid water |
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292 | ! clouds in the grid cell) to avoid problems in the |
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293 | ! averaging of the output. |
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294 | ! In the output of IOIPSL, derive the real cloud droplet |
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295 | ! effective radius as re/fl |
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296 | ! |
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297 | |
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298 | fl(i,k) = pclc(i,k)*(1.-zfice2(i,k)) |
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299 | re(i,k) = rad_chaud_tab(i,k)*fl(i,k) |
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300 | |
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301 | rel = rad_chaud_tab(i,k) |
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302 | c for ice clouds: as a function of the ambiant temperature |
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303 | c [formula used by Iacobellis and Somerville (2000), with an |
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304 | c asymptotical value of 3.5 microns at T<-81.4 C added to be |
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305 | c consistent with observations of Heymsfield et al. 1986]: |
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306 | tc = t(i,k)-273.15 |
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307 | rei = 0.71*tc + 61.29 |
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308 | if (tc.le.-81.4) rei = 3.5 |
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309 | c -- cloud optical thickness : |
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310 | |
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311 | c [for liquid clouds, traditional formula, |
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312 | c for ice clouds, Ebert & Curry (1992)] |
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313 | |
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314 | if (zflwp_var.eq.0.) rel = 1. |
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315 | if (zfiwp_var.eq.0. .or. rei.le.0.) rei = 1. |
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316 | pcltau(i,k) = 3.0/2.0 * ( zflwp_var/rel ) |
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317 | & + zfiwp_var * (3.448e-03 + 2.431/rei) |
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318 | c -- cloud infrared emissivity: |
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319 | |
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320 | c [the broadband infrared absorption coefficient is parameterized |
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321 | c as a function of the effective cld droplet radius] |
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322 | |
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323 | c Ebert and Curry (1992) formula as used by Kiehl & Zender (1995): |
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324 | k_ice = k_ice0 + 1.0/rei |
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325 | |
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326 | pclemi(i,k) = 1.0 |
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327 | & - EXP( -coef_chau*zflwp_var - DF*k_ice*zfiwp_var) |
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328 | |
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329 | ENDIF |
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330 | reliq(i,k)=rel |
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331 | reice(i,k)=rei |
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332 | ! if (i.eq.1) then |
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333 | ! print*,'Dans newmicro rel, rei :',rel, rei |
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334 | ! print*,'Dans newmicro reliq, reice :', |
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335 | ! $ reliq(i,k),reice(i,k) |
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336 | ! endif |
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337 | |
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338 | ENDDO |
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339 | ENDDO |
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340 | |
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341 | DO k = 1, klev |
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342 | DO i = 1, klon |
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343 | xflwp(i) = xflwp(i)+ xflwc(i,k) * diff_paprs(i,k) |
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344 | xfiwp(i) = xfiwp(i)+ xfiwc(i,k) * diff_paprs(i,k) |
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345 | ENDDO |
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346 | ENDDO |
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347 | |
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348 | ELSE |
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349 | DO k = 1, klev |
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350 | rad_chaud = rad_chau1 |
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351 | IF (k.LE.3) rad_chaud = rad_chau2 |
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352 | DO i = 1, klon |
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353 | |
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354 | IF (pclc(i,k) .LE. seuil_neb) THEN |
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355 | |
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356 | pclc(i,k) = 0.0 |
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357 | pcltau(i,k) = 0.0 |
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358 | pclemi(i,k) = 0.0 |
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359 | cldtaupi(i,k) = 0.0 |
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360 | |
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361 | ELSE |
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362 | |
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363 | zflwp_var = 1000.*pqlwp(i,k)*diff_paprs(i,k) |
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364 | & /pclc(i,k) |
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365 | |
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366 | zfice1 = MIN( |
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367 | & MAX( 1.0 - (t(i,k)-t_glace_min) / |
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368 | & (t_glace_max-t_glace_min),0.0),1.0)**nexpo |
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369 | |
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370 | radius = rad_chaud * (1.-zfice1) + rad_froid * zfice1 |
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371 | coef = coef_chau * (1.-zfice1) + coef_froi * zfice1 |
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372 | |
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373 | pcltau(i,k) = 3.0 * zflwp_var / (2.0 * radius) |
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374 | pclemi(i,k) = 1.0 - EXP( - coef * zflwp_var) |
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375 | |
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376 | ENDIF |
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377 | |
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378 | ENDDO |
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379 | ENDDO |
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380 | ENDIF |
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381 | |
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382 | IF (.NOT.ok_aie) THEN |
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383 | DO k = 1, klev |
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384 | DO i = 1, klon |
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385 | cldtaupi(i,k)=pcltau(i,k) |
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386 | ENDDO |
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387 | ENDDO |
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388 | ENDIF |
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389 | |
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390 | ccc DO k = 1, klev |
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391 | ccc DO i = 1, klon |
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392 | ccc t(i,k) = t(i,k) |
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393 | ccc pclc(i,k) = MAX( 1.e-5 , pclc(i,k) ) |
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394 | ccc lo = pclc(i,k) .GT. (2.*1.e-5) |
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395 | ccc zflwp = pqlwp(i,k)*1000.*(paprs(i,k)-paprs(i,k+1)) |
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396 | ccc . /(rg*pclc(i,k)) |
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397 | ccc zradef = 10.0 + (1.-sigs(k))*45.0 |
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398 | ccc pcltau(i,k) = 1.5 * zflwp / zradef |
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399 | ccc zfice=1.0-MIN(MAX((t(i,k)-263.)/(273.-263.),0.0),1.0) |
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400 | ccc zmsac = 0.13*(1.0-zfice) + 0.08*zfice |
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401 | ccc pclemi(i,k) = 1.-EXP(-zmsac*zflwp) |
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402 | ccc if (.NOT.lo) pclc(i,k) = 0.0 |
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403 | ccc if (.NOT.lo) pcltau(i,k) = 0.0 |
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404 | ccc if (.NOT.lo) pclemi(i,k) = 0.0 |
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405 | ccc ENDDO |
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406 | ccc ENDDO |
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407 | ccccc print*, 'pas de nuage dans le rayonnement' |
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408 | ccccc DO k = 1, klev |
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409 | ccccc DO i = 1, klon |
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410 | ccccc pclc(i,k) = 0.0 |
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411 | ccccc pcltau(i,k) = 0.0 |
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412 | ccccc pclemi(i,k) = 0.0 |
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413 | ccccc ENDDO |
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414 | ccccc ENDDO |
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415 | C |
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416 | C COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS |
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417 | C |
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418 | c IM cf. CR:test: calcul prenant ou non en compte le recouvrement |
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419 | c initialisations |
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420 | DO i=1,klon |
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421 | zclear(i)=1. |
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422 | zcloud(i)=0. |
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423 | pch(i)=1.0 |
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424 | pcm(i) = 1.0 |
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425 | pcl(i) = 1.0 |
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426 | pctlwp(i) = 0.0 |
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427 | ENDDO |
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428 | C |
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429 | cIM cf CR DO k=1,klev |
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430 | DO k = klev, 1, -1 |
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431 | DO i = 1, klon |
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432 | pctlwp(i) = pctlwp(i) |
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433 | & + pqlwp(i,k)*diff_paprs(i,k) |
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434 | ENDDO |
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435 | ENDDO |
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436 | c IM cf. CR |
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437 | IF (NOVLP.EQ.1) THEN |
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438 | DO k = klev, 1, -1 |
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439 | DO i = 1, klon |
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440 | zclear(i)=zclear(i)*(1.-MAX(pclc(i,k),zcloud(i))) |
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441 | & /(1.-MIN(real(zcloud(i), kind=8),1.-ZEPSEC)) |
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442 | pct(i)=1.-zclear(i) |
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443 | IF (pplay(i,k).LE.cetahb*paprs(i,1)) THEN |
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444 | pch(i) = pch(i)*(1.-MAX(pclc(i,k),zcloud(i))) |
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445 | & /(1.-MIN(real(zcloud(i), kind=8),1.-ZEPSEC)) |
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446 | ELSE IF (pplay(i,k).GT.cetahb*paprs(i,1) .AND. |
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447 | & pplay(i,k).LE.cetamb*paprs(i,1)) THEN |
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448 | pcm(i) = pcm(i)*(1.-MAX(pclc(i,k),zcloud(i))) |
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449 | & /(1.-MIN(real(zcloud(i), kind=8),1.-ZEPSEC)) |
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450 | ELSE IF (pplay(i,k).GT.cetamb*paprs(i,1)) THEN |
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451 | pcl(i) = pcl(i)*(1.-MAX(pclc(i,k),zcloud(i))) |
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452 | & /(1.-MIN(real(zcloud(i), kind=8),1.-ZEPSEC)) |
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453 | endif |
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454 | zcloud(i)=pclc(i,k) |
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455 | ENDDO |
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456 | ENDDO |
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457 | ELSE IF (NOVLP.EQ.2) THEN |
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458 | DO k = klev, 1, -1 |
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459 | DO i = 1, klon |
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460 | zcloud(i)=MAX(pclc(i,k),zcloud(i)) |
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461 | pct(i)=zcloud(i) |
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462 | IF (pplay(i,k).LE.cetahb*paprs(i,1)) THEN |
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463 | pch(i) = MIN(pclc(i,k),pch(i)) |
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464 | ELSE IF (pplay(i,k).GT.cetahb*paprs(i,1) .AND. |
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465 | & pplay(i,k).LE.cetamb*paprs(i,1)) THEN |
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466 | pcm(i) = MIN(pclc(i,k),pcm(i)) |
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467 | ELSE IF (pplay(i,k).GT.cetamb*paprs(i,1)) THEN |
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468 | pcl(i) = MIN(pclc(i,k),pcl(i)) |
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469 | endif |
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470 | ENDDO |
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471 | ENDDO |
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472 | ELSE IF (NOVLP.EQ.3) THEN |
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473 | DO k = klev, 1, -1 |
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474 | DO i = 1, klon |
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475 | zclear(i)=zclear(i)*(1.-pclc(i,k)) |
---|
476 | pct(i)=1-zclear(i) |
---|
477 | IF (pplay(i,k).LE.cetahb*paprs(i,1)) THEN |
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478 | pch(i) = pch(i)*(1.0-pclc(i,k)) |
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479 | ELSE IF (pplay(i,k).GT.cetahb*paprs(i,1) .AND. |
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480 | & pplay(i,k).LE.cetamb*paprs(i,1)) THEN |
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481 | pcm(i) = pcm(i)*(1.0-pclc(i,k)) |
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482 | ELSE IF (pplay(i,k).GT.cetamb*paprs(i,1)) THEN |
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483 | pcl(i) = pcl(i)*(1.0-pclc(i,k)) |
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484 | endif |
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485 | ENDDO |
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486 | ENDDO |
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487 | ENDIF |
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488 | |
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489 | C |
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490 | DO i = 1, klon |
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491 | c IM cf. CR pct(i)=1.-pct(i) |
---|
492 | pch(i)=1.-pch(i) |
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493 | pcm(i)=1.-pcm(i) |
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494 | pcl(i)=1.-pcl(i) |
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495 | ENDDO |
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496 | |
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497 | c ======================================================== |
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498 | ! DIAGNOSTICS CALCULATION FOR CMIP5 PROTOCOL |
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499 | c ======================================================== |
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500 | !! change by Nicolas Yan (LSCE) |
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501 | !! Cloud Droplet Number Concentration (CDNC) : 3D variable |
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502 | !! Fractionnal cover by liquid water cloud (LCC3D) : 3D variable |
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503 | !! Cloud Droplet Number Concentration at top of cloud (CLDNCL) : 2D variable |
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504 | !! Droplet effective radius at top of cloud (REFFCLWTOP) : 2D variable |
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505 | !! Fractionnal cover by liquid water at top of clouds (LCC) : 2D variable |
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506 | IF (ok_newmicro) THEN |
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507 | IF (ok_aie) THEN |
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508 | DO k = 1, klev |
---|
509 | DO i = 1, klon |
---|
510 | phase3d(i,k)=1-zfice2(i,k) |
---|
511 | IF (pclc(i,k) .LE. seuil_neb) THEN |
---|
512 | lcc3d(i,k)=seuil_neb*phase3d(i,k) |
---|
513 | ELSE |
---|
514 | lcc3d(i,k)=pclc(i,k)*phase3d(i,k) |
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515 | ENDIF |
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516 | scdnc(i,k)=lcc3d(i,k)*cdnc(i,k) ! m-3 |
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517 | ENDDO |
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518 | ENDDO |
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519 | |
---|
520 | DO i=1,klon |
---|
521 | lcc(i)=0. |
---|
522 | reffclwtop(i)=0. |
---|
523 | cldncl(i)=0. |
---|
524 | IF(RANDOM .OR. MAXIMUM_RANDOM) tcc(i) = 1. |
---|
525 | IF(MAXIMUM) tcc(i) = 0. |
---|
526 | ENDDO |
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527 | |
---|
528 | FIRST=.TRUE. |
---|
529 | |
---|
530 | DO i=1,klon |
---|
531 | DO k=klev-1,1,-1 !From TOA down |
---|
532 | |
---|
533 | |
---|
534 | ! Test, if the cloud optical depth exceeds the necessary |
---|
535 | ! threshold: |
---|
536 | |
---|
537 | IF (pcltau(i,k).GT.thres_tau .AND. pclc(i,k).GT.thres_neb) |
---|
538 | . THEN |
---|
539 | ! To calculate the right Temperature at cloud top, |
---|
540 | ! interpolate it between layers: |
---|
541 | t_tmp = t(i,k) + |
---|
542 | . (paprs(i,k+1)-pplay(i,k))/(pplay(i,k+1)-pplay(i,k)) |
---|
543 | . * ( t(i,k+1) - t(i,k) ) |
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544 | |
---|
545 | IF(MAXIMUM) THEN |
---|
546 | IF(FIRST) THEN |
---|
547 | write(*,*)'Hypothese de recouvrement: MAXIMUM' |
---|
548 | FIRST=.FALSE. |
---|
549 | ENDIF |
---|
550 | flag_max= -1. |
---|
551 | ftmp(i) = MAX(tcc(i),pclc(i,k)) |
---|
552 | ENDIF |
---|
553 | |
---|
554 | IF(RANDOM) THEN |
---|
555 | IF(FIRST) THEN |
---|
556 | write(*,*)'Hypothese de recouvrement: RANDOM' |
---|
557 | FIRST=.FALSE. |
---|
558 | ENDIF |
---|
559 | flag_max= 1. |
---|
560 | ftmp(i) = tcc(i) * (1-pclc(i,k)) |
---|
561 | ENDIF |
---|
562 | |
---|
563 | IF(MAXIMUM_RANDOM) THEN |
---|
564 | IF(FIRST) THEN |
---|
565 | write(*,*)'Hypothese de recouvrement: MAXIMUM_ |
---|
566 | . RANDOM' |
---|
567 | FIRST=.FALSE. |
---|
568 | ENDIF |
---|
569 | flag_max= 1. |
---|
570 | ftmp(i) = tcc(i) * |
---|
571 | . (1. - MAX(pclc(i,k),pclc(i,k+1))) / |
---|
572 | . (1. - MIN(pclc(i,k+1),1.-thres_neb)) |
---|
573 | ENDIF |
---|
574 | c Effective radius of cloud droplet at top of cloud (m) |
---|
575 | reffclwtop(i) = reffclwtop(i) + rad_chaud_tab(i,k) * |
---|
576 | . 1.0E-06 * phase3d(i,k) * ( tcc(i) - ftmp(i))*flag_max |
---|
577 | c CDNC at top of cloud (m-3) |
---|
578 | cldncl(i) = cldncl(i) + cdnc(i,k) * phase3d(i,k) * |
---|
579 | . (tcc(i) - ftmp(i))*flag_max |
---|
580 | c Liquid Cloud Content at top of cloud |
---|
581 | lcc(i) = lcc(i) + phase3d(i,k) * (tcc(i)-ftmp(i))* |
---|
582 | . flag_max |
---|
583 | c Total Cloud Content at top of cloud |
---|
584 | tcc(i)=ftmp(i) |
---|
585 | |
---|
586 | ENDIF ! is there a visible, not-too-small cloud? |
---|
587 | ENDDO ! loop over k |
---|
588 | |
---|
589 | IF(RANDOM .OR. MAXIMUM_RANDOM) tcc(i)=1.-tcc(i) |
---|
590 | ENDDO ! loop over i |
---|
591 | |
---|
592 | !! Convective and Stratiform Cloud Droplet Effective Radius (REFFCLWC REFFCLWS) |
---|
593 | DO i = 1, klon |
---|
594 | DO k = 1, klev |
---|
595 | pqlwpcon(i,k)=rnebcon(i,k)*clwcon(i,k) ! fraction eau liquide convective |
---|
596 | pqlwpstra(i,k)=pclc(i,k)*phase3d(i,k)-pqlwpcon(i,k) ! fraction eau liquide stratiforme |
---|
597 | IF (pqlwpstra(i,k) .LE. 0.0) pqlwpstra(i,k)=0.0 |
---|
598 | ! Convective Cloud Droplet Effective Radius (REFFCLWC) : variable 3D |
---|
599 | reffclwc(i,k)=1.1 |
---|
600 | & *((pqlwpcon(i,k)*pplay(i,k)/(RD * T(i,k))) |
---|
601 | & /(4./3*RPI*1000.*cdnc(i,k)) )**(1./3.) |
---|
602 | reffclwc(i,k) = MAX(reffclwc(i,k) * 1e6, 5.) |
---|
603 | |
---|
604 | ! Stratiform Cloud Droplet Effective Radius (REFFCLWS) : variable 3D |
---|
605 | IF ((pclc(i,k)-rnebcon(i,k)) .LE. seuil_neb) THEN ! tout sous la forme convective |
---|
606 | reffclws(i,k)=0.0 |
---|
607 | lcc3dstra(i,k)= 0.0 |
---|
608 | ELSE |
---|
609 | reffclws(i,k) = (pclc(i,k)*phase3d(i,k)* |
---|
610 | & rad_chaud_tab(i,k)- |
---|
611 | & pqlwpcon(i,k)*reffclwc(i,k)) |
---|
612 | IF(reffclws(i,k) .LE. 0.0) reffclws(i,k)=0.0 |
---|
613 | lcc3dstra(i,k)=pqlwpstra(i,k) |
---|
614 | ENDIF |
---|
615 | !Convertion from um to m |
---|
616 | IF(rnebcon(i,k). LE. seuil_neb) THEN |
---|
617 | reffclwc(i,k) = reffclwc(i,k)*seuil_neb*clwcon(i,k) |
---|
618 | & *1.0E-06 |
---|
619 | lcc3dcon(i,k)= seuil_neb*clwcon(i,k) |
---|
620 | ELSE |
---|
621 | reffclwc(i,k) = reffclwc(i,k)*pqlwpcon(i,k) |
---|
622 | & *1.0E-06 |
---|
623 | lcc3dcon(i,k) = pqlwpcon(i,k) |
---|
624 | ENDIF |
---|
625 | |
---|
626 | reffclws(i,k) = reffclws(i,k)*1.0E-06 |
---|
627 | |
---|
628 | ENDDO !klev |
---|
629 | ENDDO !klon |
---|
630 | |
---|
631 | !! Column Integrated Cloud Droplet Number (CLDNVI) : variable 2D |
---|
632 | DO k = 1, klev |
---|
633 | DO i = 1, klon |
---|
634 | pdel(i,k) = paprs(i,k)-paprs(i,k+1) |
---|
635 | zrho(i,k)=pplay(i,k)/t(i,k)/RD ! kg/m3 |
---|
636 | dh(i,k)=pdel(i,k)/(gravit*zrho(i,k)) ! hauteur de chaque boite (m) |
---|
637 | ENDDO |
---|
638 | ENDDO |
---|
639 | c |
---|
640 | DO i = 1, klon |
---|
641 | cldnvi(i)=0. |
---|
642 | lcc_integrat(i)=0. |
---|
643 | height(i)=0. |
---|
644 | DO k = 1, klev |
---|
645 | cldnvi(i)=cldnvi(i)+cdnc(i,k)*lcc3d(i,k)*dh(i,k) |
---|
646 | lcc_integrat(i)=lcc_integrat(i)+lcc3d(i,k)*dh(i,k) |
---|
647 | height(i)=height(i)+dh(i,k) |
---|
648 | ENDDO ! klev |
---|
649 | lcc_integrat(i)=lcc_integrat(i)/height(i) |
---|
650 | IF (lcc_integrat(i) .LE. 1.0E-03) THEN |
---|
651 | cldnvi(i)=cldnvi(i)*lcc(i)/seuil_neb |
---|
652 | ELSE |
---|
653 | cldnvi(i)=cldnvi(i)*lcc(i)/lcc_integrat(i) |
---|
654 | ENDIF |
---|
655 | ENDDO ! klon |
---|
656 | |
---|
657 | DO i = 1, klon |
---|
658 | DO k = 1, klev |
---|
659 | IF (scdnc(i,k) .LE. 0.0) scdnc(i,k)=0.0 |
---|
660 | IF (reffclws(i,k) .LE. 0.0) reffclws(i,k)=0.0 |
---|
661 | IF (reffclwc(i,k) .LE. 0.0) reffclwc(i,k)=0.0 |
---|
662 | IF (lcc3d(i,k) .LE. 0.0) lcc3d(i,k)=0.0 |
---|
663 | IF (lcc3dcon(i,k) .LE. 0.0) lcc3dcon(i,k)=0.0 |
---|
664 | IF (lcc3dstra(i,k) .LE. 0.0) lcc3dstra(i,k)=0.0 |
---|
665 | ENDDO |
---|
666 | IF (reffclwtop(i) .LE. 0.0) reffclwtop(i)=0.0 |
---|
667 | IF (cldncl(i) .LE. 0.0) cldncl(i)=0.0 |
---|
668 | IF (cldnvi(i) .LE. 0.0) cldnvi(i)=0.0 |
---|
669 | IF (lcc(i) .LE. 0.0) lcc(i)=0.0 |
---|
670 | ENDDO |
---|
671 | |
---|
672 | ENDIF !ok_aie |
---|
673 | ENDIF !ok newmicro |
---|
674 | c |
---|
675 | C |
---|
676 | RETURN |
---|
677 | END |
---|