| 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 | i ,year_ini_toga,day_ju_ini_toga,nt_toga,dt_toga |
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| 48 | i ,nlev_toga,ts_toga,plev_toga,t_toga,q_toga,u_toga |
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| 49 | i ,v_toga,w_toga,ht_toga,vt_toga,hq_toga,vq_toga |
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| 50 | o ,ts_prof,plev_prof,t_prof,q_prof,u_prof,v_prof,w_prof |
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| 51 | o ,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 | !--------------------------------------------------------------------- |
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| 82 | ! Interpolation forcing TWPice |
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| 83 | !--------------------------------------------------------------------- |
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| 84 | if (forcing_twpice) then |
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| 85 | |
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| 86 | print*, |
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| 87 | : '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_twpi=', |
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| 88 | : daytime,day1,(daytime-day1)*86400., |
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| 89 | : (daytime-day1)*86400/dt_twpi |
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| 90 | |
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| 91 | ! time interpolation: |
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| 92 | CALL interp_toga_time(daytime,day1,annee_ref |
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| 93 | i ,year_ini_twpi,day_ju_ini_twpi,nt_twpi,dt_twpi,nlev_twpi |
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| 94 | i ,ts_twpi,plev_twpi,t_twpi,q_twpi,u_twpi,v_twpi,w_twpi |
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| 95 | i ,ht_twpi,vt_twpi,hq_twpi,vq_twpi |
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| 96 | o ,ts_proftwp,plev_proftwp,t_proftwp,q_proftwp,u_proftwp |
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| 97 | o ,v_proftwp,w_proftwp |
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| 98 | o ,ht_proftwp,vt_proftwp,hq_proftwp,vq_proftwp) |
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| 99 | |
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| 100 | ! vertical interpolation: |
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| 101 | CALL interp_toga_vertical(play,nlev_twpi,plev_proftwp |
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| 102 | : ,t_proftwp,q_proftwp,u_proftwp,v_proftwp,w_proftwp |
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| 103 | : ,ht_proftwp,vt_proftwp,hq_proftwp,vq_proftwp |
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| 104 | : ,t_mod,q_mod,u_mod,v_mod,w_mod |
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| 105 | : ,ht_mod,vt_mod,hq_mod,vq_mod,mxcalc) |
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| 106 | |
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| 107 | |
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| 108 | !calcul de l'advection verticale a partir du omega |
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| 109 | cCalcul des gradients verticaux |
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| 110 | cinitialisation |
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| 111 | d_t_z(:)=0. |
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| 112 | d_q_z(:)=0. |
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| 113 | d_t_dyn_z(:)=0. |
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| 114 | d_q_dyn_z(:)=0. |
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| 115 | DO l=2,llm-1 |
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| 116 | d_t_z(l)=(temp(l+1)-temp(l-1)) |
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| 117 | & /(play(l+1)-play(l-1)) |
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| 118 | d_q_z(l)=(q(l+1,1)-q(l-1,1)) |
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| 119 | & /(play(l+1)-play(l-1)) |
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| 120 | ENDDO |
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| 121 | d_t_z(1)=d_t_z(2) |
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| 122 | d_q_z(1)=d_q_z(2) |
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| 123 | d_t_z(llm)=d_t_z(llm-1) |
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| 124 | d_q_z(llm)=d_q_z(llm-1) |
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| 125 | |
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| 126 | cCalcul de l advection verticale |
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| 127 | d_t_dyn_z(:)=w_mod(:)*d_t_z(:) |
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| 128 | d_q_dyn_z(:)=w_mod(:)*d_q_z(:) |
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| 129 | |
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| 130 | !wind nudging above 500m with a 2h time scale |
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| 131 | do l=1,llm |
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| 132 | if (nudge_wind) then |
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| 133 | ! if (phi(l).gt.5000.) then |
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| 134 | if (phi(l).gt.0.) then |
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| 135 | u(l)=u(l) |
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| 136 | . +timestep*(u_mod(l)-u(l))/(2.*3600.) |
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| 137 | v(l)=v(l) |
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| 138 | . +timestep*(v_mod(l)-v(l))/(2.*3600.) |
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| 139 | endif |
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| 140 | else |
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| 141 | u(l) = u_mod(l) |
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| 142 | v(l) = v_mod(l) |
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| 143 | endif |
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| 144 | enddo |
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| 145 | |
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| 146 | !CR:nudging of q and theta with a 6h time scale above 15km |
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| 147 | if (nudge_thermo) then |
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| 148 | do l=1,llm |
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| 149 | zz(l)=phi(l)/9.8 |
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| 150 | if ((zz(l).le.16000.).and.(zz(l).gt.15000.)) then |
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| 151 | zfact=(zz(l)-15000.)/1000. |
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| 152 | q(l,1)=q(l,1) |
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| 153 | . +timestep*(q_mod(l)-q(l,1))/(6.*3600.)*zfact |
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| 154 | temp(l)=temp(l) |
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| 155 | . +timestep*(t_mod(l)-temp(l))/(6.*3600.)*zfact |
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| 156 | else if (zz(l).gt.16000.) then |
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| 157 | q(l,1)=q(l,1) |
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| 158 | . +timestep*(q_mod(l)-q(l,1))/(6.*3600.) |
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| 159 | temp(l)=temp(l) |
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| 160 | . +timestep*(t_mod(l)-temp(l))/(6.*3600.) |
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| 161 | endif |
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| 162 | enddo |
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| 163 | endif |
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| 164 | |
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| 165 | do l = 1, llm |
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| 166 | omega(l) = w_mod(l) |
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| 167 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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| 168 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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| 169 | !calcul de l'advection totale |
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| 170 | if (cptadvw) then |
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| 171 | d_th_adv(l) = alpha*omega(l)/rcpd+ht_mod(l)-d_t_dyn_z(l) |
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| 172 | ! print*,'temp vert adv',l,ht_mod(l),vt_mod(l),-d_t_dyn_z(l) |
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| 173 | d_q_adv(l,1) = hq_mod(l)-d_q_dyn_z(l) |
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| 174 | ! print*,'q vert adv',l,hq_mod(l),vq_mod(l),-d_q_dyn_z(l) |
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| 175 | else |
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| 176 | d_th_adv(l) = alpha*omega(l)/rcpd+(ht_mod(l)+vt_mod(l)) |
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| 177 | d_q_adv(l,1) = (hq_mod(l)+vq_mod(l)) |
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| 178 | endif |
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| 179 | dt_cooling(l) = 0.0 |
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| 180 | enddo |
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| 181 | |
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| 182 | endif ! forcing_twpice |
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| 183 | |
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| 184 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 185 | !--------------------------------------------------------------------- |
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| 186 | ! Interpolation forcing AMMA |
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| 187 | !--------------------------------------------------------------------- |
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| 188 | |
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| 189 | if (forcing_amma) then |
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| 190 | |
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| 191 | print*, |
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| 192 | : '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_amma=', |
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| 193 | : daytime,day1,(daytime-day1)*86400., |
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| 194 | : (daytime-day1)*86400/dt_amma |
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| 195 | |
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| 196 | ! time interpolation using TOGA interpolation routine |
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| 197 | CALL interp_amma_time(daytime,day1,annee_ref |
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| 198 | i ,year_ini_amma,day_ju_ini_amma,nt_amma,dt_amma,nlev_amma |
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| 199 | i ,vitw_amma,ht_amma,hq_amma,lat_amma,sens_amma |
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| 200 | o ,vitw_profamma,ht_profamma,hq_profamma,lat_profamma |
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| 201 | : ,sens_profamma) |
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| 202 | |
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| 203 | print*,'apres interpolation temporelle AMMA' |
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| 204 | |
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| 205 | do k=1,nlev_amma |
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| 206 | th_profamma(k)=0. |
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| 207 | q_profamma(k)=0. |
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| 208 | u_profamma(k)=0. |
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| 209 | v_profamma(k)=0. |
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| 210 | vt_profamma(k)=0. |
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| 211 | vq_profamma(k)=0. |
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| 212 | enddo |
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| 213 | ! vertical interpolation using TOGA interpolation routine: |
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| 214 | ! write(*,*)'avant interp vert', t_proftwp |
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| 215 | CALL interp_toga_vertical(play,nlev_amma,plev_amma |
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| 216 | : ,th_profamma,q_profamma,u_profamma,v_profamma |
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| 217 | : ,vitw_profamma |
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| 218 | : ,ht_profamma,vt_profamma,hq_profamma,vq_profamma |
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| 219 | : ,t_mod,q_mod,u_mod,v_mod,w_mod |
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| 220 | : ,ht_mod,vt_mod,hq_mod,vq_mod,mxcalc) |
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| 221 | write(*,*) 'Profil initial forcing AMMA interpole' |
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| 222 | |
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| 223 | |
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| 224 | !calcul de l'advection verticale a partir du omega |
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| 225 | cCalcul des gradients verticaux |
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| 226 | cinitialisation |
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| 227 | do l=1,llm |
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| 228 | d_t_z(l)=0. |
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| 229 | d_q_z(l)=0. |
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| 230 | enddo |
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| 231 | |
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| 232 | DO l=2,llm-1 |
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| 233 | d_t_z(l)=(temp(l+1)-temp(l-1)) |
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| 234 | & /(play(l+1)-play(l-1)) |
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| 235 | d_q_z(l)=(q(l+1,1)-q(l-1,1)) |
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| 236 | & /(play(l+1)-play(l-1)) |
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| 237 | ENDDO |
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| 238 | d_t_z(1)=d_t_z(2) |
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| 239 | d_q_z(1)=d_q_z(2) |
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| 240 | d_t_z(llm)=d_t_z(llm-1) |
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| 241 | d_q_z(llm)=d_q_z(llm-1) |
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| 242 | |
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| 243 | |
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| 244 | do l = 1, llm |
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| 245 | rho(l) = play(l)/(rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))) |
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| 246 | omega(l) = w_mod(l)*(-rg*rho(l)) |
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| 247 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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| 248 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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| 249 | !calcul de l'advection totale |
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| 250 | ! d_th_adv(l) = alpha*omega(l)/rcpd+ht_mod(l)-omega(l)*d_t_z(l) |
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| 251 | !attention: on impose dth |
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| 252 | d_th_adv(l) = alpha*omega(l)/rcpd+ |
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| 253 | & ht_mod(l)*(play(l)/pzero)**rkappa-omega(l)*d_t_z(l) |
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| 254 | ! d_th_adv(l) = 0. |
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| 255 | ! print*,'temp vert adv',l,ht_mod(l),vt_mod(l),-d_t_dyn_z(l) |
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| 256 | d_q_adv(l,1) = hq_mod(l)-omega(l)*d_q_z(l) |
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| 257 | ! d_q_adv(l,1) = 0. |
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| 258 | ! print*,'q vert adv',l,hq_mod(l),vq_mod(l),-d_q_dyn_z(l) |
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| 259 | |
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| 260 | dt_cooling(l) = 0.0 |
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| 261 | enddo |
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| 262 | |
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| 263 | |
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| 264 | ! ok_flux_surf=.false. |
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| 265 | fsens=-1.*sens_profamma |
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| 266 | flat=-1.*lat_profamma |
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| 267 | |
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| 268 | endif ! forcing_amma |
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| 269 | |
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| 270 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 271 | !--------------------------------------------------------------------- |
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| 272 | ! Interpolation forcing Rico |
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| 273 | !--------------------------------------------------------------------- |
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| 274 | if (forcing_rico) then |
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| 275 | ! call lstendH(llm,omega,dt_dyn,dq_dyn,du_dyn, dv_dyn, |
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| 276 | ! : q,temp,u,v,play) |
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| 277 | call lstendH(llm,nqtot,omega,dt_dyn,dq_dyn, |
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| 278 | : q,temp,u,v,play) |
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| 279 | |
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| 280 | do l=1,llm |
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| 281 | d_th_adv(l) = (dth_rico(l) + dt_dyn(l)) |
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| 282 | d_q_adv(l,1) = (dqh_rico(l) + dq_dyn(l,1)) |
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| 283 | d_q_adv(l,2) = 0. |
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| 284 | enddo |
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| 285 | endif ! forcing_rico |
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| 286 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 287 | !--------------------------------------------------------------------- |
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| 288 | ! Interpolation forcing Arm_cu |
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| 289 | !--------------------------------------------------------------------- |
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| 290 | if (forcing_armcu) then |
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| 291 | |
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| 292 | print*, |
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| 293 | : '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_armcu=', |
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| 294 | : day,day1,(day-day1)*86400.,(day-day1)*86400/dt_armcu |
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| 295 | |
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| 296 | ! time interpolation: |
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| 297 | ! ATTENTION, cet appel ne convient pas pour TOGA !! |
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| 298 | ! revoir 1DUTILS.h et les arguments |
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| 299 | CALL interp_armcu_time(daytime,day1,annee_ref |
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| 300 | i ,year_ini_armcu,day_ju_ini_armcu,nt_armcu,dt_armcu |
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| 301 | i ,nlev_armcu,sens_armcu,flat_armcu,adv_theta_armcu |
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| 302 | i ,rad_theta_armcu,adv_qt_armcu,sens_prof,flat_prof |
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| 303 | i ,adv_theta_prof,rad_theta_prof,adv_qt_prof) |
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| 304 | |
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| 305 | ! vertical interpolation: |
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| 306 | ! No vertical interpolation if nlev imposed to 19 or 40 |
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| 307 | |
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| 308 | ! For this case, fluxes are imposed |
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| 309 | fsens=-1*sens_prof |
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| 310 | flat=-1*flat_prof |
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| 311 | |
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| 312 | ! Advective forcings are given in K or g/kg ... BY HOUR |
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| 313 | do l = 1, llm |
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| 314 | ug(l)= u_mod(l) |
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| 315 | vg(l)= v_mod(l) |
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| 316 | IF((phi(l)/RG).LT.1000) THEN |
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| 317 | d_th_adv(l) = (adv_theta_prof + rad_theta_prof)/3600. |
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| 318 | d_q_adv(l,1) = adv_qt_prof/1000./3600. |
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| 319 | d_q_adv(l,2) = 0.0 |
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| 320 | ! print *,'INF1000: phi dth dq1 dq2', |
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| 321 | ! : phi(l)/RG,d_th_adv(l),d_q_adv(l,1),d_q_adv(l,2) |
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| 322 | ELSEIF ((phi(l)/RG).GE.1000.AND.(phi(l)/RG).lt.3000) THEN |
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| 323 | fact=((phi(l)/RG)-1000.)/2000. |
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| 324 | fact=1-fact |
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| 325 | d_th_adv(l) = (adv_theta_prof + rad_theta_prof)*fact/3600. |
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| 326 | d_q_adv(l,1) = adv_qt_prof*fact/1000./3600. |
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| 327 | d_q_adv(l,2) = 0.0 |
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| 328 | ! print *,'SUP1000: phi fact dth dq1 dq2', |
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| 329 | ! : phi(l)/RG,fact,d_th_adv(l),d_q_adv(l,1),d_q_adv(l,2) |
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| 330 | ELSE |
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| 331 | d_th_adv(l) = 0.0 |
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| 332 | d_q_adv(l,1) = 0.0 |
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| 333 | d_q_adv(l,2) = 0.0 |
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| 334 | ! print *,'SUP3000: phi dth dq1 dq2', |
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| 335 | ! : phi(l)/RG,d_th_adv(l),d_q_adv(l,1),d_q_adv(l,2) |
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| 336 | ENDIF |
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| 337 | dt_cooling(l) = 0.0 |
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| 338 | ! print *,'Interp armcu: phi dth dq1 dq2', |
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| 339 | ! : l,phi(l),d_th_adv(l),d_q_adv(l,1),d_q_adv(l,2) |
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| 340 | enddo |
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| 341 | endif ! forcing_armcu |
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| 342 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 343 | !--------------------------------------------------------------------- |
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| 344 | ! Interpolation forcing in time and onto model levels |
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| 345 | !--------------------------------------------------------------------- |
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| 346 | if (forcing_sandu) then |
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| 347 | |
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| 348 | print*, |
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| 349 | : '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_sandu=', |
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| 350 | : day,day1,(day-day1)*86400.,(day-day1)*86400/dt_sandu |
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| 351 | |
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| 352 | ! time interpolation: |
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| 353 | ! ATTENTION, cet appel ne convient pas pour TOGA !! |
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| 354 | ! revoir 1DUTILS.h et les arguments |
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| 355 | CALL interp_sandu_time(daytime,day1,annee_ref |
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| 356 | i ,year_ini_sandu,day_ju_ini_sandu,nt_sandu,dt_sandu |
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| 357 | i ,nlev_sandu |
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| 358 | i ,ts_sandu,ts_prof) |
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| 359 | |
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| 360 | if (type_ts_forcing.eq.1) ts_cur = ts_prof ! SST used in read_tsurf1d |
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| 361 | |
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| 362 | ! vertical interpolation: |
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| 363 | CALL interp_sandu_vertical(play,nlev_sandu,plev_profs |
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| 364 | : ,t_profs,thl_profs,q_profs,u_profs,v_profs,w_profs |
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| 365 | : ,omega_profs,o3mmr_profs |
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| 366 | : ,t_mod,thl_mod,q_mod,u_mod,v_mod,w_mod |
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| 367 | : ,omega_mod,o3mmr_mod,mxcalc) |
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| 368 | !calcul de l'advection verticale |
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| 369 | cCalcul des gradients verticaux |
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| 370 | cinitialisation |
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| 371 | d_t_z(:)=0. |
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| 372 | d_q_z(:)=0. |
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| 373 | d_t_dyn_z(:)=0. |
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| 374 | d_q_dyn_z(:)=0. |
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| 375 | ! schema centre |
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| 376 | ! DO l=2,llm-1 |
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| 377 | ! d_t_z(l)=(temp(l+1)-temp(l-1)) |
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| 378 | ! & /(play(l+1)-play(l-1)) |
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| 379 | ! d_q_z(l)=(q(l+1,1)-q(l-1,1)) |
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| 380 | ! & /(play(l+1)-play(l-1)) |
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| 381 | ! schema amont |
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| 382 | DO l=2,llm-1 |
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| 383 | d_t_z(l)=(temp(l+1)-temp(l))/(play(l+1)-play(l)) |
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| 384 | d_q_z(l)=(q(l+1,1)-q(l,1))/(play(l+1)-play(l)) |
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| 385 | ! print *,'l temp2 temp0 play2 play0 omega_mod', |
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| 386 | ! & temp(l+1),temp(l-1),play(l+1),play(l-1),omega_mod(l) |
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| 387 | ENDDO |
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| 388 | d_t_z(1)=d_t_z(2) |
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| 389 | d_q_z(1)=d_q_z(2) |
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| 390 | d_t_z(llm)=d_t_z(llm-1) |
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| 391 | d_q_z(llm)=d_q_z(llm-1) |
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| 392 | |
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| 393 | ! calcul de l advection verticale |
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| 394 | ! Confusion w (m/s) et omega (Pa/s) !! |
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| 395 | d_t_dyn_z(:)=omega_mod(:)*d_t_z(:) |
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| 396 | d_q_dyn_z(:)=omega_mod(:)*d_q_z(:) |
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| 397 | ! do l=1,llm |
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| 398 | ! print *,'d_t_dyn omega_mod d_t_z d_q_dyn d_q_z', |
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| 399 | ! :l,d_t_dyn_z(l),omega_mod(l),d_t_z(l),d_q_dyn_z(l),d_q_z(l) |
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| 400 | ! enddo |
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| 401 | |
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| 402 | |
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| 403 | ! large-scale forcing : pour le cas Sandu ces forcages sont la SST |
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| 404 | ! et une divergence constante -> profil de omega |
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| 405 | tsurf = ts_prof |
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| 406 | write(*,*) 'SST suivante: ',tsurf |
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| 407 | do l = 1, llm |
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| 408 | omega(l) = omega_mod(l) |
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| 409 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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| 410 | |
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| 411 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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| 412 | ! |
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| 413 | ! d_th_adv(l) = 0.0 |
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| 414 | ! d_q_adv(l,1) = 0.0 |
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| 415 | !CR:test advection=0 |
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| 416 | !calcul de l'advection verticale |
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| 417 | d_th_adv(l) = alpha*omega(l)/rcpd-d_t_dyn_z(l) |
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| 418 | ! print*,'temp adv',l,-d_t_dyn_z(l) |
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| 419 | d_q_adv(l,1) = -d_q_dyn_z(l) |
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| 420 | ! print*,'q adv',l,-d_q_dyn_z(l) |
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| 421 | dt_cooling(l) = 0.0 |
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| 422 | enddo |
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| 423 | endif ! forcing_sandu |
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| 424 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 425 | !--------------------------------------------------------------------- |
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| 426 | ! Interpolation forcing in time and onto model levels |
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| 427 | !--------------------------------------------------------------------- |
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| 428 | if (forcing_astex) then |
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| 429 | |
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| 430 | print*, |
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| 431 | : '#### ITAP,day,day1,(day-day1)*86400,(day-day1)*86400/dt_astex=', |
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| 432 | : day,day1,(day-day1)*86400.,(day-day1)*86400/dt_astex |
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| 433 | |
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| 434 | ! time interpolation: |
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| 435 | ! ATTENTION, cet appel ne convient pas pour TOGA !! |
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| 436 | ! revoir 1DUTILS.h et les arguments |
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| 437 | CALL interp_astex_time(daytime,day1,annee_ref |
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| 438 | i ,year_ini_astex,day_ju_ini_astex,nt_astex,dt_astex |
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| 439 | i ,nlev_astex,div_astex,ts_astex,ug_astex,vg_astex |
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| 440 | i ,ufa_astex,vfa_astex,div_prof,ts_prof,ug_prof,vg_prof |
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| 441 | i ,ufa_prof,vfa_prof) |
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| 442 | |
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| 443 | if (type_ts_forcing.eq.1) ts_cur = ts_prof ! SST used in read_tsurf1d |
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| 444 | |
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| 445 | ! vertical interpolation: |
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| 446 | CALL interp_astex_vertical(play,nlev_astex,plev_profa |
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| 447 | : ,t_profa,thl_profa,qv_profa,ql_profa,qt_profa |
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| 448 | : ,u_profa,v_profa,w_profa,tke_profa,o3mmr_profa |
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| 449 | : ,t_mod,thl_mod,qv_mod,ql_mod,qt_mod,u_mod,v_mod,w_mod |
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| 450 | : ,tke_mod,o3mmr_mod,mxcalc) |
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| 451 | !calcul de l'advection verticale |
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| 452 | !Calcul des gradients verticaux |
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| 453 | !initialisation |
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| 454 | d_t_z(:)=0. |
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| 455 | d_q_z(:)=0. |
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| 456 | d_t_dyn_z(:)=0. |
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| 457 | d_q_dyn_z(:)=0. |
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| 458 | ! schema centre |
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| 459 | ! DO l=2,llm-1 |
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| 460 | ! d_t_z(l)=(temp(l+1)-temp(l-1)) |
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| 461 | ! & /(play(l+1)-play(l-1)) |
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| 462 | ! d_q_z(l)=(q(l+1,1)-q(l-1,1)) |
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| 463 | ! & /(play(l+1)-play(l-1)) |
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| 464 | ! schema amont |
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| 465 | DO l=2,llm-1 |
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| 466 | d_t_z(l)=(temp(l+1)-temp(l))/(play(l+1)-play(l)) |
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| 467 | d_q_z(l)=(q(l+1,1)-q(l,1))/(play(l+1)-play(l)) |
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| 468 | ! print *,'l temp2 temp0 play2 play0 omega_mod', |
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| 469 | ! & temp(l+1),temp(l-1),play(l+1),play(l-1),omega_mod(l) |
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| 470 | ENDDO |
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| 471 | d_t_z(1)=d_t_z(2) |
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| 472 | d_q_z(1)=d_q_z(2) |
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| 473 | d_t_z(llm)=d_t_z(llm-1) |
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| 474 | d_q_z(llm)=d_q_z(llm-1) |
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| 475 | |
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| 476 | ! calcul de l advection verticale |
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| 477 | ! Confusion w (m/s) et omega (Pa/s) !! |
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| 478 | d_t_dyn_z(:)=w_mod(:)*d_t_z(:) |
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| 479 | d_q_dyn_z(:)=w_mod(:)*d_q_z(:) |
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| 480 | ! do l=1,llm |
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| 481 | ! print *,'d_t_dyn omega_mod d_t_z d_q_dyn d_q_z', |
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| 482 | ! :l,d_t_dyn_z(l),omega_mod(l),d_t_z(l),d_q_dyn_z(l),d_q_z(l) |
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| 483 | ! enddo |
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| 484 | |
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| 485 | |
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| 486 | ! large-scale forcing : pour le cas Astex ces forcages sont la SST |
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| 487 | ! la divergence,ug,vg,ufa,vfa |
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| 488 | tsurf = ts_prof |
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| 489 | write(*,*) 'SST suivante: ',tsurf |
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| 490 | do l = 1, llm |
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| 491 | omega(l) = w_mod(l) |
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| 492 | omega2(l)= omega(l)/rg*airefi ! flxmass_w calcule comme ds physiq |
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| 493 | |
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| 494 | alpha = rd*temp(l)*(1.+(rv/rd-1.)*q(l,1))/play(l) |
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| 495 | ! |
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| 496 | ! d_th_adv(l) = 0.0 |
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| 497 | ! d_q_adv(l,1) = 0.0 |
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| 498 | !CR:test advection=0 |
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| 499 | !calcul de l'advection verticale |
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| 500 | d_th_adv(l) = alpha*omega(l)/rcpd-d_t_dyn_z(l) |
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| 501 | ! print*,'temp adv',l,-d_t_dyn_z(l) |
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| 502 | d_q_adv(l,1) = -d_q_dyn_z(l) |
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| 503 | ! print*,'q adv',l,-d_q_dyn_z(l) |
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| 504 | dt_cooling(l) = 0.0 |
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| 505 | enddo |
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| 506 | endif ! forcing_astex |
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| 507 | !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! |
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| 508 | |
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