1 | !--------------------------------------------------------------------- |
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2 | ! Interpolation forcing in time and onto model levels |
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3 | !--------------------------------------------------------------------- |
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4 | if (forcing_GCSSold) then |
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5 | |
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6 | call get_uvd(it,timestep,fich_gcssold_ctl,fich_gcssold_dat, & |
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7 | & ht_gcssold,hq_gcssold,hw_gcssold, & |
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8 | & hu_gcssold,hv_gcssold, & |
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9 | & hthturb_gcssold,hqturb_gcssold,Ts_gcssold, & |
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10 | & imp_fcg_gcssold,ts_fcg_gcssold, & |
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11 | & Tp_fcg_gcssold,Turb_fcg_gcssold) |
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12 | if (prt_level.ge.1) then |
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13 | print *,' get_uvd -> hqturb_gcssold ',it,hqturb_gcssold |
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14 | endif |
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15 | ! large-scale forcing : |
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16 | !!! tsurf = ts_gcssold |
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17 | do l = 1, llm |
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18 | ! u(l) = hu_gcssold(l) ! on prescrit le vent |
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19 | ! v(l) = hv_gcssold(l) ! on prescrit le vent |
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20 | ! omega(l) = hw_gcssold(l) |
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21 | ! rho(l) = play(l)/(rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))) |
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22 | ! omega2(l)=-rho(l)*omega(l) |
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23 | omega(l) = hw_gcssold(l) |
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24 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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25 | |
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26 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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27 | d_th_adv(l) = ht_gcssold(l) |
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28 | d_q_adv(l,1) = hq_gcssold(l) |
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29 | dt_cooling(l) = 0.0 |
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30 | enddo |
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31 | |
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32 | endif ! forcing_GCSSold |
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33 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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34 | !--------------------------------------------------------------------- |
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35 | ! Interpolation Toga forcing |
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36 | !--------------------------------------------------------------------- |
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37 | if (forcing_toga) then |
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38 | |
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39 | if (prt_level.ge.1) then |
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40 | print*, & |
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41 | & '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_toga=', & |
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42 | & day,day1,(day-day1)*86400.,(day-day1)*86400/dt_toga |
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43 | endif |
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44 | |
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45 | ! time interpolation: |
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46 | CALL interp_toga_time(daytime,day1,annee_ref & |
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47 | & ,year_ini_toga,day_ju_ini_toga,nt_toga,dt_toga & |
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48 | & ,nlev_toga,ts_toga,plev_toga,t_toga,q_toga,u_toga & |
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49 | & ,v_toga,w_toga,ht_toga,vt_toga,hq_toga,vq_toga & |
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50 | & ,ts_prof,plev_prof,t_prof,q_prof,u_prof,v_prof,w_prof & |
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51 | & ,ht_prof,vt_prof,hq_prof,vq_prof) |
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52 | |
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53 | if (type_ts_forcing.eq.1) ts_cur = ts_prof ! SST used in read_tsurf1d |
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54 | |
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55 | ! vertical interpolation: |
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56 | CALL interp_toga_vertical(play,nlev_toga,plev_prof & |
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57 | & ,t_prof,q_prof,u_prof,v_prof,w_prof & |
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58 | & ,ht_prof,vt_prof,hq_prof,vq_prof & |
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59 | & ,t_mod,q_mod,u_mod,v_mod,w_mod & |
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60 | & ,ht_mod,vt_mod,hq_mod,vq_mod,mxcalc) |
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61 | |
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62 | ! large-scale forcing : |
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63 | tsurf = ts_prof |
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64 | do l = 1, llm |
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65 | u(l) = u_mod(l) ! sb: on prescrit le vent |
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66 | v(l) = v_mod(l) ! sb: on prescrit le vent |
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67 | ! omega(l) = w_prof(l) |
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68 | ! rho(l) = play(l)/(rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))) |
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69 | ! omega2(l)=-rho(l)*omega(l) |
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70 | omega(l) = w_mod(l) |
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71 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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72 | |
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73 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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74 | d_th_adv(l) = alpha*omega(l)/rcpd-(ht_mod(l)+vt_mod(l)) |
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75 | d_q_adv(l,1) = -(hq_mod(l)+vq_mod(l)) |
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76 | dt_cooling(l) = 0.0 |
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77 | enddo |
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78 | |
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79 | endif ! forcing_toga |
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80 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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81 | ! Interpolation DICE forcing |
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82 | !--------------------------------------------------------------------- |
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83 | if (forcing_dice) then |
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84 | |
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85 | if (prt_level.ge.1) then |
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86 | print*,'#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_dice=',& |
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87 | & day,day1,(day-day1)*86400.,(day-day1)*86400/dt_dice |
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88 | endif |
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89 | |
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90 | ! time interpolation: |
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91 | CALL interp_dice_time(daytime,day1,annee_ref & |
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92 | & ,year_ini_dice,day_ju_ini_dice,nt_dice,dt_dice & |
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93 | & ,nlev_dice,shf_dice,lhf_dice,lwup_dice,swup_dice & |
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94 | & ,tg_dice,ustar_dice,psurf_dice,ug_dice,vg_dice & |
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95 | & ,ht_dice,hq_dice,hu_dice,hv_dice,w_dice,omega_dice & |
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96 | & ,shf_prof,lhf_prof,lwup_prof,swup_prof,tg_prof & |
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97 | & ,ustar_prof,psurf_prof,ug_profd,vg_profd & |
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98 | & ,ht_profd,hq_profd,hu_profd,hv_profd,w_profd & |
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99 | & ,omega_profd) |
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100 | ! do l = 1, llm |
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101 | ! print *,'llm l omega_profd',llm,l,omega_profd(l) |
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102 | ! enddo |
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103 | |
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104 | if (type_ts_forcing.eq.1) ts_cur = tg_prof ! SST used in read_tsurf1d |
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105 | |
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106 | ! vertical interpolation: |
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107 | CALL interp_dice_vertical(play,nlev_dice,nt_dice,plev_dice & |
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108 | & ,th_dice,qv_dice,u_dice,v_dice,o3_dice & |
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109 | & ,ht_profd,hq_profd,hu_profd,hv_profd,w_profd,omega_profd & |
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110 | & ,th_mod,qv_mod,u_mod,v_mod,o3_mod & |
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111 | & ,ht_mod,hq_mod,hu_mod,hv_mod,w_mod,omega_mod,mxcalc) |
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112 | ! do l = 1, llm |
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113 | ! print *,'llm l omega_mod',llm,l,omega_mod(l) |
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114 | ! enddo |
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115 | |
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116 | ! Les forcages DICE sont donnes /jour et non /seconde ! |
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117 | ht_mod(:)=ht_mod(:)/86400. |
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118 | hq_mod(:)=hq_mod(:)/86400. |
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119 | hu_mod(:)=hu_mod(:)/86400. |
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120 | hv_mod(:)=hv_mod(:)/86400. |
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121 | |
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122 | !calcul de l'advection verticale a partir du omega (repris cas TWPICE, MPL 05082013) |
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123 | !Calcul des gradients verticaux |
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124 | !initialisation |
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125 | d_t_z(:)=0. |
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126 | d_q_z(:)=0. |
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127 | d_u_z(:)=0. |
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128 | d_v_z(:)=0. |
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129 | DO l=2,llm-1 |
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130 | d_t_z(l)=(temp(l+1)-temp(l-1))/(play(l+1)-play(l-1)) |
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131 | d_q_z(l)=(q(l+1,1)-q(l-1,1)) /(play(l+1)-play(l-1)) |
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132 | d_u_z(l)=(u(l+1)-u(l-1))/(play(l+1)-play(l-1)) |
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133 | d_v_z(l)=(v(l+1)-v(l-1))/(play(l+1)-play(l-1)) |
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134 | ENDDO |
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135 | d_t_z(1)=d_t_z(2) |
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136 | d_q_z(1)=d_q_z(2) |
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137 | ! d_u_z(1)=u(2)/(play(2)-psurf)/5. |
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138 | ! d_v_z(1)=v(2)/(play(2)-psurf)/5. |
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139 | d_u_z(1)=0. |
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140 | d_v_z(1)=0. |
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141 | d_t_z(llm)=d_t_z(llm-1) |
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142 | d_q_z(llm)=d_q_z(llm-1) |
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143 | d_u_z(llm)=d_u_z(llm-1) |
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144 | d_v_z(llm)=d_v_z(llm-1) |
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145 | |
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146 | !Calcul de l advection verticale: |
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147 | ! utiliser omega (Pa/s) et non w (m/s) !! MP 20131108 |
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148 | d_t_dyn_z(:)=omega_mod(:)*d_t_z(:) |
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149 | d_q_dyn_z(:)=omega_mod(:)*d_q_z(:) |
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150 | d_u_dyn_z(:)=omega_mod(:)*d_u_z(:) |
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151 | d_v_dyn_z(:)=omega_mod(:)*d_v_z(:) |
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152 | |
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153 | ! large-scale forcing : |
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154 | ! tsurf = tg_prof MPL 20130925 commente |
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155 | psurf = psurf_prof |
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156 | ! For this case, fluxes are imposed |
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157 | fsens=-1*shf_prof |
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158 | flat=-1*lhf_prof |
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159 | ust=ustar_prof |
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160 | tg=tg_prof |
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161 | print *,'ust= ',ust |
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162 | do l = 1, llm |
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163 | ug(l)= ug_profd |
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164 | vg(l)= vg_profd |
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165 | ! omega(l) = w_prof(l) |
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166 | ! rho(l) = play(l)/(rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))) |
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167 | ! omega2(l)=-rho(l)*omega(l) |
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168 | ! omega(l) = w_mod(l)*(-rg*rho(l)) |
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169 | omega(l) = omega_mod(l) |
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170 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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171 | |
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172 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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173 | d_th_adv(l) = alpha*omega(l)/rcpd+ht_mod(l)-d_t_dyn_z(l) |
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174 | d_q_adv(l,1) = hq_mod(l)-d_q_dyn_z(l) |
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175 | d_u_adv(l) = hu_mod(l)-d_u_dyn_z(l) |
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176 | d_v_adv(l) = hv_mod(l)-d_v_dyn_z(l) |
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177 | dt_cooling(l) = 0.0 |
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178 | enddo |
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179 | |
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180 | endif ! forcing_dice |
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181 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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182 | !--------------------------------------------------------------------- |
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183 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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184 | !--------------------------------------------------------------------- |
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185 | ! Interpolation forcing TWPice |
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186 | !--------------------------------------------------------------------- |
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187 | if (forcing_twpice) then |
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188 | |
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189 | print*, & |
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190 | & '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_twpi=', & |
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191 | & daytime,day1,(daytime-day1)*86400., & |
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192 | & (daytime-day1)*86400/dt_twpi |
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193 | |
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194 | ! time interpolation: |
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195 | CALL interp_toga_time(daytime,day1,annee_ref & |
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196 | & ,year_ini_twpi,day_ju_ini_twpi,nt_twpi,dt_twpi,nlev_twpi & |
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197 | & ,ts_twpi,plev_twpi,t_twpi,q_twpi,u_twpi,v_twpi,w_twpi & |
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198 | & ,ht_twpi,vt_twpi,hq_twpi,vq_twpi & |
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199 | & ,ts_proftwp,plev_proftwp,t_proftwp,q_proftwp,u_proftwp & |
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200 | & ,v_proftwp,w_proftwp & |
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201 | & ,ht_proftwp,vt_proftwp,hq_proftwp,vq_proftwp) |
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202 | |
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203 | ! vertical interpolation: |
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204 | CALL interp_toga_vertical(play,nlev_twpi,plev_proftwp & |
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205 | & ,t_proftwp,q_proftwp,u_proftwp,v_proftwp,w_proftwp & |
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206 | & ,ht_proftwp,vt_proftwp,hq_proftwp,vq_proftwp & |
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207 | & ,t_mod,q_mod,u_mod,v_mod,w_mod & |
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208 | & ,ht_mod,vt_mod,hq_mod,vq_mod,mxcalc) |
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209 | |
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210 | |
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211 | !calcul de l'advection verticale a partir du omega |
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212 | !Calcul des gradients verticaux |
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213 | !initialisation |
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214 | d_t_z(:)=0. |
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215 | d_q_z(:)=0. |
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216 | d_t_dyn_z(:)=0. |
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217 | d_q_dyn_z(:)=0. |
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218 | DO l=2,llm-1 |
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219 | d_t_z(l)=(temp(l+1)-temp(l-1))/(play(l+1)-play(l-1)) |
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220 | d_q_z(l)=(q(l+1,1)-q(l-1,1))/(play(l+1)-play(l-1)) |
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221 | ENDDO |
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222 | d_t_z(1)=d_t_z(2) |
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223 | d_q_z(1)=d_q_z(2) |
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224 | d_t_z(llm)=d_t_z(llm-1) |
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225 | d_q_z(llm)=d_q_z(llm-1) |
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226 | |
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227 | !Calcul de l advection verticale |
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228 | d_t_dyn_z(:)=w_mod(:)*d_t_z(:) |
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229 | d_q_dyn_z(:)=w_mod(:)*d_q_z(:) |
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230 | |
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231 | !wind nudging above 500m with a 2h time scale |
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232 | do l=1,llm |
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233 | if (nudge_wind) then |
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234 | ! if (phi(l).gt.5000.) then |
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235 | if (phi(l).gt.0.) then |
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236 | u(l)=u(l)+timestep*(u_mod(l)-u(l))/(2.*3600.) |
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237 | v(l)=v(l)+timestep*(v_mod(l)-v(l))/(2.*3600.) |
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238 | endif |
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239 | else |
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240 | u(l) = u_mod(l) |
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241 | v(l) = v_mod(l) |
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242 | endif |
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243 | enddo |
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244 | |
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245 | !CR:nudging of q and theta with a 6h time scale above 15km |
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246 | if (nudge_thermo) then |
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247 | do l=1,llm |
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248 | zz(l)=phi(l)/9.8 |
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249 | if ((zz(l).le.16000.).and.(zz(l).gt.15000.)) then |
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250 | zfact=(zz(l)-15000.)/1000. |
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251 | q(l,1)=q(l,1)+timestep*(q_mod(l)-q(l,1))/(6.*3600.)*zfact |
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252 | temp(l)=temp(l)+timestep*(t_mod(l)-temp(l))/(6.*3600.)*zfact |
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253 | else if (zz(l).gt.16000.) then |
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254 | q(l,1)=q(l,1)+timestep*(q_mod(l)-q(l,1))/(6.*3600.) |
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255 | temp(l)=temp(l)+timestep*(t_mod(l)-temp(l))/(6.*3600.) |
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256 | endif |
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257 | enddo |
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258 | endif |
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259 | |
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260 | do l = 1, llm |
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261 | omega(l) = w_mod(l) |
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262 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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263 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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264 | !calcul de l'advection totale |
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265 | if (cptadvw) then |
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266 | d_th_adv(l) = alpha*omega(l)/rcpd+ht_mod(l)-d_t_dyn_z(l) |
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267 | ! print*,'temp vert adv',l,ht_mod(l),vt_mod(l),-d_t_dyn_z(l) |
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268 | d_q_adv(l,1) = hq_mod(l)-d_q_dyn_z(l) |
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269 | ! print*,'q vert adv',l,hq_mod(l),vq_mod(l),-d_q_dyn_z(l) |
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270 | else |
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271 | d_th_adv(l) = alpha*omega(l)/rcpd+(ht_mod(l)+vt_mod(l)) |
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272 | d_q_adv(l,1) = (hq_mod(l)+vq_mod(l)) |
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273 | endif |
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274 | dt_cooling(l) = 0.0 |
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275 | enddo |
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276 | |
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277 | endif ! forcing_twpice |
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278 | |
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279 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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280 | !--------------------------------------------------------------------- |
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281 | ! Interpolation forcing AMMA |
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282 | !--------------------------------------------------------------------- |
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283 | |
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284 | if (forcing_amma) then |
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285 | |
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286 | print*, & |
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287 | & '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_amma=', & |
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288 | & daytime,day1,(daytime-day1)*86400., & |
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289 | & (daytime-day1)*86400/dt_amma |
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290 | |
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291 | ! time interpolation using TOGA interpolation routine |
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292 | CALL interp_amma_time(daytime,day1,annee_ref & |
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293 | & ,year_ini_amma,day_ju_ini_amma,nt_amma,dt_amma,nlev_amma & |
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294 | & ,vitw_amma,ht_amma,hq_amma,lat_amma,sens_amma & |
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295 | & ,vitw_profamma,ht_profamma,hq_profamma,lat_profamma & |
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296 | & ,sens_profamma) |
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297 | |
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298 | print*,'apres interpolation temporelle AMMA' |
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299 | |
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300 | do k=1,nlev_amma |
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301 | th_profamma(k)=0. |
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302 | q_profamma(k)=0. |
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303 | u_profamma(k)=0. |
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304 | v_profamma(k)=0. |
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305 | vt_profamma(k)=0. |
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306 | vq_profamma(k)=0. |
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307 | enddo |
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308 | ! vertical interpolation using TOGA interpolation routine: |
---|
309 | ! write(*,*)'avant interp vert', t_proftwp |
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310 | CALL interp_toga_vertical(play,nlev_amma,plev_amma & |
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311 | & ,th_profamma,q_profamma,u_profamma,v_profamma & |
---|
312 | & ,vitw_profamma & |
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313 | & ,ht_profamma,vt_profamma,hq_profamma,vq_profamma & |
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314 | & ,t_mod,q_mod,u_mod,v_mod,w_mod & |
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315 | & ,ht_mod,vt_mod,hq_mod,vq_mod,mxcalc) |
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316 | write(*,*) 'Profil initial forcing AMMA interpole' |
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317 | |
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318 | |
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319 | !calcul de l'advection verticale a partir du omega |
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320 | !Calcul des gradients verticaux |
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321 | !initialisation |
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322 | do l=1,llm |
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323 | d_t_z(l)=0. |
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324 | d_q_z(l)=0. |
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325 | enddo |
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326 | |
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327 | DO l=2,llm-1 |
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328 | d_t_z(l)=(temp(l+1)-temp(l-1))/(play(l+1)-play(l-1)) |
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329 | d_q_z(l)=(q(l+1,1)-q(l-1,1))/(play(l+1)-play(l-1)) |
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330 | ENDDO |
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331 | d_t_z(1)=d_t_z(2) |
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332 | d_q_z(1)=d_q_z(2) |
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333 | d_t_z(llm)=d_t_z(llm-1) |
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334 | d_q_z(llm)=d_q_z(llm-1) |
---|
335 | |
---|
336 | |
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337 | do l = 1, llm |
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338 | rho(l) = play(l)/(rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))) |
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339 | omega(l) = w_mod(l)*(-rg*rho(l)) |
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340 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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341 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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342 | !calcul de l'advection totale |
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343 | ! d_th_adv(l) = alpha*omega(l)/rcpd+ht_mod(l)-omega(l)*d_t_z(l) |
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344 | !attention: on impose dth |
---|
345 | d_th_adv(l) = alpha*omega(l)/rcpd+ & |
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346 | & ht_mod(l)*(play(l)/pzero)**rkappa-omega(l)*d_t_z(l) |
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347 | ! d_th_adv(l) = 0. |
---|
348 | ! print*,'temp vert adv',l,ht_mod(l),vt_mod(l),-d_t_dyn_z(l) |
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349 | d_q_adv(l,1) = hq_mod(l)-omega(l)*d_q_z(l) |
---|
350 | ! d_q_adv(l,1) = 0. |
---|
351 | ! print*,'q vert adv',l,hq_mod(l),vq_mod(l),-d_q_dyn_z(l) |
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352 | |
---|
353 | dt_cooling(l) = 0.0 |
---|
354 | enddo |
---|
355 | |
---|
356 | |
---|
357 | ! ok_flux_surf=.false. |
---|
358 | fsens=-1.*sens_profamma |
---|
359 | flat=-1.*lat_profamma |
---|
360 | |
---|
361 | endif ! forcing_amma |
---|
362 | |
---|
363 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
---|
364 | !--------------------------------------------------------------------- |
---|
365 | ! Interpolation forcing Rico |
---|
366 | !--------------------------------------------------------------------- |
---|
367 | if (forcing_rico) then |
---|
368 | ! call lstendH(llm,omega,dt_dyn,dq_dyn,du_dyn, dv_dyn, |
---|
369 | ! : q,temp,u,v,play) |
---|
370 | call lstendH(llm,nqtot,omega,dt_dyn,dq_dyn,q,temp,u,v,play) |
---|
371 | |
---|
372 | do l=1,llm |
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373 | d_th_adv(l) = (dth_rico(l) + dt_dyn(l)) |
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374 | d_q_adv(l,1) = (dqh_rico(l) + dq_dyn(l,1)) |
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375 | d_q_adv(l,2) = 0. |
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376 | enddo |
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377 | endif ! forcing_rico |
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378 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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379 | !--------------------------------------------------------------------- |
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380 | ! Interpolation forcing Arm_cu |
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381 | !--------------------------------------------------------------------- |
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382 | if (forcing_armcu) then |
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383 | |
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384 | print*, & |
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385 | & '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_armcu=', & |
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386 | & day,day1,(day-day1)*86400.,(day-day1)*86400/dt_armcu |
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387 | |
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388 | ! time interpolation: |
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389 | ! ATTENTION, cet appel ne convient pas pour TOGA !! |
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390 | ! revoir 1DUTILS.h et les arguments |
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391 | CALL interp_armcu_time(daytime,day1,annee_ref & |
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392 | & ,year_ini_armcu,day_ju_ini_armcu,nt_armcu,dt_armcu & |
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393 | & ,nlev_armcu,sens_armcu,flat_armcu,adv_theta_armcu & |
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394 | & ,rad_theta_armcu,adv_qt_armcu,sens_prof,flat_prof & |
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395 | & ,adv_theta_prof,rad_theta_prof,adv_qt_prof) |
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396 | |
---|
397 | ! vertical interpolation: |
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398 | ! No vertical interpolation if nlev imposed to 19 or 40 |
---|
399 | |
---|
400 | ! For this case, fluxes are imposed |
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401 | fsens=-1*sens_prof |
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402 | flat=-1*flat_prof |
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403 | |
---|
404 | ! Advective forcings are given in K or g/kg ... BY HOUR |
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405 | do l = 1, llm |
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406 | ug(l)= u_mod(l) |
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407 | vg(l)= v_mod(l) |
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408 | IF((phi(l)/RG).LT.1000) THEN |
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409 | d_th_adv(l) = (adv_theta_prof + rad_theta_prof)/3600. |
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410 | d_q_adv(l,1) = adv_qt_prof/1000./3600. |
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411 | d_q_adv(l,2) = 0.0 |
---|
412 | ! print *,'INF1000: phi dth dq1 dq2', |
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413 | ! : phi(l)/RG,d_th_adv(l),d_q_adv(l,1),d_q_adv(l,2) |
---|
414 | ELSEIF ((phi(l)/RG).GE.1000.AND.(phi(l)/RG).lt.3000) THEN |
---|
415 | fact=((phi(l)/RG)-1000.)/2000. |
---|
416 | fact=1-fact |
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417 | d_th_adv(l) = (adv_theta_prof + rad_theta_prof)*fact/3600. |
---|
418 | d_q_adv(l,1) = adv_qt_prof*fact/1000./3600. |
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419 | d_q_adv(l,2) = 0.0 |
---|
420 | ! print *,'SUP1000: phi fact dth dq1 dq2', |
---|
421 | ! : phi(l)/RG,fact,d_th_adv(l),d_q_adv(l,1),d_q_adv(l,2) |
---|
422 | ELSE |
---|
423 | d_th_adv(l) = 0.0 |
---|
424 | d_q_adv(l,1) = 0.0 |
---|
425 | d_q_adv(l,2) = 0.0 |
---|
426 | ! print *,'SUP3000: phi dth dq1 dq2', |
---|
427 | ! : phi(l)/RG,d_th_adv(l),d_q_adv(l,1),d_q_adv(l,2) |
---|
428 | ENDIF |
---|
429 | dt_cooling(l) = 0.0 |
---|
430 | ! print *,'Interp armcu: phi dth dq1 dq2', |
---|
431 | ! : l,phi(l),d_th_adv(l),d_q_adv(l,1),d_q_adv(l,2) |
---|
432 | enddo |
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433 | endif ! forcing_armcu |
---|
434 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
---|
435 | !--------------------------------------------------------------------- |
---|
436 | ! Interpolation forcing in time and onto model levels |
---|
437 | !--------------------------------------------------------------------- |
---|
438 | if (forcing_sandu) then |
---|
439 | |
---|
440 | print*, & |
---|
441 | & '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_sandu=', & |
---|
442 | & day,day1,(day-day1)*86400.,(day-day1)*86400/dt_sandu |
---|
443 | |
---|
444 | ! time interpolation: |
---|
445 | ! ATTENTION, cet appel ne convient pas pour TOGA !! |
---|
446 | ! revoir 1DUTILS.h et les arguments |
---|
447 | CALL interp_sandu_time(daytime,day1,annee_ref & |
---|
448 | & ,year_ini_sandu,day_ju_ini_sandu,nt_sandu,dt_sandu & |
---|
449 | & ,nlev_sandu & |
---|
450 | & ,ts_sandu,ts_prof) |
---|
451 | |
---|
452 | if (type_ts_forcing.eq.1) ts_cur = ts_prof ! SST used in read_tsurf1d |
---|
453 | |
---|
454 | ! vertical interpolation: |
---|
455 | CALL interp_sandu_vertical(play,nlev_sandu,plev_profs & |
---|
456 | & ,t_profs,thl_profs,q_profs,u_profs,v_profs,w_profs & |
---|
457 | & ,omega_profs,o3mmr_profs & |
---|
458 | & ,t_mod,thl_mod,q_mod,u_mod,v_mod,w_mod & |
---|
459 | & ,omega_mod,o3mmr_mod,mxcalc) |
---|
460 | !calcul de l'advection verticale |
---|
461 | !Calcul des gradients verticaux |
---|
462 | !initialisation |
---|
463 | d_t_z(:)=0. |
---|
464 | d_q_z(:)=0. |
---|
465 | d_t_dyn_z(:)=0. |
---|
466 | d_q_dyn_z(:)=0. |
---|
467 | ! schema centre |
---|
468 | ! DO l=2,llm-1 |
---|
469 | ! d_t_z(l)=(temp(l+1)-temp(l-1)) |
---|
470 | ! & /(play(l+1)-play(l-1)) |
---|
471 | ! d_q_z(l)=(q(l+1,1)-q(l-1,1)) |
---|
472 | ! & /(play(l+1)-play(l-1)) |
---|
473 | ! schema amont |
---|
474 | DO l=2,llm-1 |
---|
475 | d_t_z(l)=(temp(l+1)-temp(l))/(play(l+1)-play(l)) |
---|
476 | d_q_z(l)=(q(l+1,1)-q(l,1))/(play(l+1)-play(l)) |
---|
477 | ! print *,'l temp2 temp0 play2 play0 omega_mod', |
---|
478 | ! & temp(l+1),temp(l-1),play(l+1),play(l-1),omega_mod(l) |
---|
479 | ENDDO |
---|
480 | d_t_z(1)=d_t_z(2) |
---|
481 | d_q_z(1)=d_q_z(2) |
---|
482 | d_t_z(llm)=d_t_z(llm-1) |
---|
483 | d_q_z(llm)=d_q_z(llm-1) |
---|
484 | |
---|
485 | ! calcul de l advection verticale |
---|
486 | ! Confusion w (m/s) et omega (Pa/s) !! |
---|
487 | d_t_dyn_z(:)=omega_mod(:)*d_t_z(:) |
---|
488 | d_q_dyn_z(:)=omega_mod(:)*d_q_z(:) |
---|
489 | ! do l=1,llm |
---|
490 | ! print *,'d_t_dyn omega_mod d_t_z d_q_dyn d_q_z', |
---|
491 | ! :l,d_t_dyn_z(l),omega_mod(l),d_t_z(l),d_q_dyn_z(l),d_q_z(l) |
---|
492 | ! enddo |
---|
493 | |
---|
494 | |
---|
495 | ! large-scale forcing : pour le cas Sandu ces forcages sont la SST |
---|
496 | ! et une divergence constante -> profil de omega |
---|
497 | tsurf = ts_prof |
---|
498 | write(*,*) 'SST suivante: ',tsurf |
---|
499 | do l = 1, llm |
---|
500 | omega(l) = omega_mod(l) |
---|
501 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
---|
502 | |
---|
503 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
---|
504 | ! |
---|
505 | ! d_th_adv(l) = 0.0 |
---|
506 | ! d_q_adv(l,1) = 0.0 |
---|
507 | !CR:test advection=0 |
---|
508 | !calcul de l'advection verticale |
---|
509 | d_th_adv(l) = alpha*omega(l)/rcpd-d_t_dyn_z(l) |
---|
510 | ! print*,'temp adv',l,-d_t_dyn_z(l) |
---|
511 | d_q_adv(l,1) = -d_q_dyn_z(l) |
---|
512 | ! print*,'q adv',l,-d_q_dyn_z(l) |
---|
513 | dt_cooling(l) = 0.0 |
---|
514 | enddo |
---|
515 | endif ! forcing_sandu |
---|
516 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
---|
517 | !--------------------------------------------------------------------- |
---|
518 | ! Interpolation forcing in time and onto model levels |
---|
519 | !--------------------------------------------------------------------- |
---|
520 | if (forcing_astex) then |
---|
521 | |
---|
522 | print*, & |
---|
523 | & '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_astex=', & |
---|
524 | & day,day1,(day-day1)*86400.,(day-day1)*86400/dt_astex |
---|
525 | |
---|
526 | ! time interpolation: |
---|
527 | ! ATTENTION, cet appel ne convient pas pour TOGA !! |
---|
528 | ! revoir 1DUTILS.h et les arguments |
---|
529 | CALL interp_astex_time(daytime,day1,annee_ref & |
---|
530 | & ,year_ini_astex,day_ju_ini_astex,nt_astex,dt_astex & |
---|
531 | & ,nlev_astex,div_astex,ts_astex,ug_astex,vg_astex & |
---|
532 | & ,ufa_astex,vfa_astex,div_prof,ts_prof,ug_prof,vg_prof & |
---|
533 | & ,ufa_prof,vfa_prof) |
---|
534 | |
---|
535 | if (type_ts_forcing.eq.1) ts_cur = ts_prof ! SST used in read_tsurf1d |
---|
536 | |
---|
537 | ! vertical interpolation: |
---|
538 | CALL interp_astex_vertical(play,nlev_astex,plev_profa & |
---|
539 | & ,t_profa,thl_profa,qv_profa,ql_profa,qt_profa & |
---|
540 | & ,u_profa,v_profa,w_profa,tke_profa,o3mmr_profa & |
---|
541 | & ,t_mod,thl_mod,qv_mod,ql_mod,qt_mod,u_mod,v_mod,w_mod & |
---|
542 | & ,tke_mod,o3mmr_mod,mxcalc) |
---|
543 | !calcul de l'advection verticale |
---|
544 | !Calcul des gradients verticaux |
---|
545 | !initialisation |
---|
546 | d_t_z(:)=0. |
---|
547 | d_q_z(:)=0. |
---|
548 | d_t_dyn_z(:)=0. |
---|
549 | d_q_dyn_z(:)=0. |
---|
550 | ! schema centre |
---|
551 | ! DO l=2,llm-1 |
---|
552 | ! d_t_z(l)=(temp(l+1)-temp(l-1)) |
---|
553 | ! & /(play(l+1)-play(l-1)) |
---|
554 | ! d_q_z(l)=(q(l+1,1)-q(l-1,1)) |
---|
555 | ! & /(play(l+1)-play(l-1)) |
---|
556 | ! schema amont |
---|
557 | DO l=2,llm-1 |
---|
558 | d_t_z(l)=(temp(l+1)-temp(l))/(play(l+1)-play(l)) |
---|
559 | d_q_z(l)=(q(l+1,1)-q(l,1))/(play(l+1)-play(l)) |
---|
560 | ! print *,'l temp2 temp0 play2 play0 omega_mod', |
---|
561 | ! & temp(l+1),temp(l-1),play(l+1),play(l-1),omega_mod(l) |
---|
562 | ENDDO |
---|
563 | d_t_z(1)=d_t_z(2) |
---|
564 | d_q_z(1)=d_q_z(2) |
---|
565 | d_t_z(llm)=d_t_z(llm-1) |
---|
566 | d_q_z(llm)=d_q_z(llm-1) |
---|
567 | |
---|
568 | ! calcul de l advection verticale |
---|
569 | ! Confusion w (m/s) et omega (Pa/s) !! |
---|
570 | d_t_dyn_z(:)=w_mod(:)*d_t_z(:) |
---|
571 | d_q_dyn_z(:)=w_mod(:)*d_q_z(:) |
---|
572 | ! do l=1,llm |
---|
573 | ! print *,'d_t_dyn omega_mod d_t_z d_q_dyn d_q_z', |
---|
574 | ! :l,d_t_dyn_z(l),omega_mod(l),d_t_z(l),d_q_dyn_z(l),d_q_z(l) |
---|
575 | ! enddo |
---|
576 | |
---|
577 | |
---|
578 | ! large-scale forcing : pour le cas Astex ces forcages sont la SST |
---|
579 | ! la divergence,ug,vg,ufa,vfa |
---|
580 | tsurf = ts_prof |
---|
581 | write(*,*) 'SST suivante: ',tsurf |
---|
582 | do l = 1, llm |
---|
583 | omega(l) = w_mod(l) |
---|
584 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
---|
585 | |
---|
586 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
---|
587 | ! |
---|
588 | ! d_th_adv(l) = 0.0 |
---|
589 | ! d_q_adv(l,1) = 0.0 |
---|
590 | !CR:test advection=0 |
---|
591 | !calcul de l'advection verticale |
---|
592 | d_th_adv(l) = alpha*omega(l)/rcpd-d_t_dyn_z(l) |
---|
593 | ! print*,'temp adv',l,-d_t_dyn_z(l) |
---|
594 | d_q_adv(l,1) = -d_q_dyn_z(l) |
---|
595 | ! print*,'q adv',l,-d_q_dyn_z(l) |
---|
596 | dt_cooling(l) = 0.0 |
---|
597 | enddo |
---|
598 | endif ! forcing_astex |
---|
599 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
---|
600 | |
---|