[3526] | 1 | ! |
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| 2 | ! $Id: traccoag_mod.F90 4293 2022-10-04 19:42:41Z fhourdin $ |
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| 3 | ! |
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[2690] | 4 | MODULE traccoag_mod |
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| 5 | ! |
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| 6 | ! This module calculates the concentration of aerosol particles in certain size bins |
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| 7 | ! considering coagulation and sedimentation. |
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| 8 | ! |
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| 9 | CONTAINS |
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| 10 | |
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| 11 | SUBROUTINE traccoag(pdtphys, gmtime, debutphy, julien, & |
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| 12 | presnivs, xlat, xlon, pphis, pphi, & |
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[2752] | 13 | t_seri, pplay, paprs, sh, rh, tr_seri) |
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[2690] | 14 | |
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[2752] | 15 | USE phys_local_var_mod, ONLY: mdw, R2SO4, DENSO4, f_r_wet, surf_PM25_sulf, & |
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| 16 | & budg_emi_ocs, budg_emi_so2, budg_emi_h2so4, budg_emi_part |
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[2690] | 17 | |
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| 18 | USE dimphy |
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[4293] | 19 | USE infotrac_phy, ONLY : nbtr_bin, nbtr_sulgas, nbtr, id_SO2_strat |
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[2690] | 20 | USE aerophys |
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[3526] | 21 | USE geometry_mod, ONLY : cell_area, boundslat |
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[2690] | 22 | USE mod_grid_phy_lmdz |
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| 23 | USE mod_phys_lmdz_mpi_data, ONLY : is_mpi_root |
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| 24 | USE mod_phys_lmdz_para, only: gather, scatter |
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[4293] | 25 | USE phys_cal_mod, ONLY : year_len, year_cur,mth_cur, day_cur, hour |
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[2690] | 26 | USE sulfate_aer_mod |
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| 27 | USE phys_local_var_mod, ONLY: stratomask |
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| 28 | USE YOMCST |
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[3526] | 29 | USE print_control_mod, ONLY: lunout |
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| 30 | USE strataer_mod |
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[2690] | 31 | |
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| 32 | IMPLICIT NONE |
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| 33 | |
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| 34 | ! Input argument |
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| 35 | !--------------- |
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| 36 | REAL,INTENT(IN) :: pdtphys ! Pas d'integration pour la physique (seconde) |
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| 37 | REAL,INTENT(IN) :: gmtime ! Heure courante |
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| 38 | LOGICAL,INTENT(IN) :: debutphy ! le flag de l'initialisation de la physique |
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| 39 | INTEGER,INTENT(IN) :: julien ! Jour julien |
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| 40 | |
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| 41 | REAL,DIMENSION(klev),INTENT(IN) :: presnivs! pressions approximat. des milieux couches (en PA) |
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| 42 | REAL,DIMENSION(klon),INTENT(IN) :: xlat ! latitudes pour chaque point |
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| 43 | REAL,DIMENSION(klon),INTENT(IN) :: xlon ! longitudes pour chaque point |
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| 44 | REAL,DIMENSION(klon),INTENT(IN) :: pphis ! geopotentiel du sol |
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| 45 | REAL,DIMENSION(klon,klev),INTENT(IN) :: pphi ! geopotentiel de chaque couche |
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| 46 | |
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| 47 | REAL,DIMENSION(klon,klev),INTENT(IN) :: t_seri ! Temperature |
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| 48 | REAL,DIMENSION(klon,klev),INTENT(IN) :: pplay ! pression pour le mileu de chaque couche (en Pa) |
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| 49 | REAL,DIMENSION(klon,klev+1),INTENT(IN) :: paprs ! pression pour chaque inter-couche (en Pa) |
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| 50 | REAL,DIMENSION(klon,klev),INTENT(IN) :: sh ! humidite specifique |
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| 51 | REAL,DIMENSION(klon,klev),INTENT(IN) :: rh ! humidite relative |
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| 52 | |
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| 53 | ! Output argument |
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| 54 | !---------------- |
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| 55 | REAL,DIMENSION(klon,klev,nbtr),INTENT(INOUT) :: tr_seri ! Concentration Traceur [U/KgA] |
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| 56 | |
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| 57 | ! Local variables |
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| 58 | !---------------- |
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[3526] | 59 | REAL :: m_aer_emiss_vol_daily ! daily injection mass emission |
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| 60 | INTEGER :: it, k, i, ilon, ilev, itime, i_int, ieru |
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[2690] | 61 | LOGICAL,DIMENSION(klon,klev) :: is_strato ! true = above tropopause, false = below |
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| 62 | REAL,DIMENSION(klon,klev) :: m_air_gridbox ! mass of air in every grid box [kg] |
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| 63 | REAL,DIMENSION(klon_glo,klev,nbtr) :: tr_seri_glo ! Concentration Traceur [U/KgA] |
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| 64 | REAL,DIMENSION(klev+1) :: altLMDz ! altitude of layer interfaces in m |
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| 65 | REAL,DIMENSION(klev) :: f_lay_emiss ! fraction of emission for every vertical layer |
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| 66 | REAL :: f_lay_sum ! sum of layer emission fractions |
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[2699] | 67 | REAL :: alt ! altitude for integral calculation |
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[2690] | 68 | INTEGER,PARAMETER :: n_int_alt=10 ! number of subintervals for integration over Gaussian emission profile |
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| 69 | REAL,DIMENSION(nbtr_bin) :: r_bin ! particle radius in size bin [m] |
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| 70 | REAL,DIMENSION(nbtr_bin) :: r_lower ! particle radius at lower bin boundary [m] |
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| 71 | REAL,DIMENSION(nbtr_bin) :: r_upper ! particle radius at upper bin boundary [m] |
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| 72 | REAL,DIMENSION(nbtr_bin) :: m_part_dry ! mass of one dry particle in size bin [kg] |
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| 73 | REAL :: zrho ! Density of air [kg/m3] |
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| 74 | REAL :: zdz ! thickness of atm. model layer in m |
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[2752] | 75 | REAL,DIMENSION(klev) :: zdm ! mass of atm. model layer in kg |
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[2690] | 76 | REAL,DIMENSION(klon,klev) :: dens_aer ! density of aerosol particles [kg/m3 aerosol] with default H2SO4 mass fraction |
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[2752] | 77 | REAL :: emission ! emission |
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[3526] | 78 | REAL :: theta_min, theta_max ! for SAI computation between two latitudes |
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| 79 | REAL :: dlat_loc |
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[2690] | 80 | |
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| 81 | IF (is_mpi_root) THEN |
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[3526] | 82 | WRITE(lunout,*) 'in traccoag: date from phys_cal_mod =',year_cur,'-',mth_cur,'-',day_cur,'-',hour |
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| 83 | WRITE(lunout,*) 'IN traccoag flag_sulf_emit: ',flag_sulf_emit |
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[2690] | 84 | ENDIF |
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[3526] | 85 | |
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[2690] | 86 | DO it=1, nbtr_bin |
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| 87 | r_bin(it)=mdw(it)/2. |
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| 88 | ENDDO |
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| 89 | |
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| 90 | !--set boundaries of size bins |
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| 91 | DO it=1, nbtr_bin |
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| 92 | IF (it.EQ.1) THEN |
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| 93 | r_upper(it)=sqrt(r_bin(it+1)*r_bin(it)) |
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| 94 | r_lower(it)=r_bin(it)**2./r_upper(it) |
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| 95 | ELSEIF (it.EQ.nbtr_bin) THEN |
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| 96 | r_lower(it)=sqrt(r_bin(it)*r_bin(it-1)) |
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| 97 | r_upper(it)=r_bin(it)**2./r_lower(it) |
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| 98 | ELSE |
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| 99 | r_lower(it)=sqrt(r_bin(it)*r_bin(it-1)) |
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| 100 | r_upper(it)=sqrt(r_bin(it+1)*r_bin(it)) |
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| 101 | ENDIF |
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| 102 | ENDDO |
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| 103 | |
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| 104 | IF (debutphy .and. is_mpi_root) THEN |
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| 105 | DO it=1, nbtr_bin |
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[3526] | 106 | WRITE(lunout,*) 'radius bin', it, ':', r_bin(it), '(from', r_lower(it), 'to', r_upper(it), ')' |
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[2690] | 107 | ENDDO |
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| 108 | ENDIF |
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| 109 | |
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| 110 | !--initialising logical is_strato from stratomask |
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| 111 | is_strato(:,:)=.FALSE. |
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[2695] | 112 | WHERE (stratomask.GT.0.5) is_strato=.TRUE. |
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[2690] | 113 | |
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| 114 | ! STRACOMP (H2O, P, t_seri -> aerosol composition (R2SO4)) |
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| 115 | ! H2SO4 mass fraction in aerosol (%) |
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| 116 | CALL stracomp(sh,t_seri,pplay) |
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| 117 | |
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| 118 | ! aerosol density (gr/cm3) |
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| 119 | CALL denh2sa(t_seri) |
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| 120 | |
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| 121 | ! compute factor for converting dry to wet radius (for every grid box) |
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| 122 | f_r_wet(:,:) = (dens_aer_dry/(DENSO4(:,:)*1000.)/(R2SO4(:,:)/100.))**(1./3.) |
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| 123 | |
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| 124 | !--calculate mass of air in every grid box |
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| 125 | DO ilon=1, klon |
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| 126 | DO ilev=1, klev |
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[2752] | 127 | m_air_gridbox(ilon,ilev)=(paprs(ilon,ilev)-paprs(ilon,ilev+1))/RG*cell_area(ilon) |
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[2690] | 128 | ENDDO |
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| 129 | ENDDO |
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| 130 | |
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[2752] | 131 | ! IF (debutphy) THEN |
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| 132 | ! CALL gather(tr_seri, tr_seri_glo) |
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| 133 | ! IF (MAXVAL(tr_seri_glo).LT.1.e-30) THEN |
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[2690] | 134 | !--initialising tracer concentrations to zero |
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[2752] | 135 | ! DO it=1, nbtr |
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| 136 | ! tr_seri(:,:,it)=0.0 |
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| 137 | ! ENDDO |
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| 138 | ! ENDIF |
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| 139 | ! ENDIF |
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[2690] | 140 | |
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[2752] | 141 | !--initialise emission diagnostics |
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| 142 | budg_emi_ocs(:)=0.0 |
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| 143 | budg_emi_so2(:)=0.0 |
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| 144 | budg_emi_h2so4(:)=0.0 |
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| 145 | budg_emi_part(:)=0.0 |
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| 146 | |
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[2690] | 147 | !--sulfur emission, depending on chosen scenario (flag_sulf_emit) |
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| 148 | SELECT CASE(flag_sulf_emit) |
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| 149 | |
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| 150 | CASE(0) ! background aerosol |
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| 151 | ! do nothing (no emission) |
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| 152 | |
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| 153 | CASE(1) ! volcanic eruption |
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| 154 | !--only emit on day of eruption |
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| 155 | ! stretch emission over one day of Pinatubo eruption |
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[3526] | 156 | DO ieru=1, nErupt |
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| 157 | IF (year_cur==year_emit_vol(ieru).AND.mth_cur==mth_emit_vol(ieru).AND.& |
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| 158 | day_cur>=day_emit_vol(ieru).AND.day_cur<(day_emit_vol(ieru)+injdur)) THEN |
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| 159 | ! |
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| 160 | ! daily injection mass emission - NL |
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| 161 | m_aer_emiss_vol_daily = m_aer_emiss_vol(ieru)/(REAL(injdur)*REAL(ponde_lonlat_vol(ieru))) |
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| 162 | WRITE(lunout,*) 'IN traccoag DD m_aer_emiss_vol(ieru)=',m_aer_emiss_vol(ieru), & |
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| 163 | 'ponde_lonlat_vol(ieru)=',ponde_lonlat_vol(ieru),'(injdur*ponde_lonlat_vol(ieru))', & |
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| 164 | (injdur*ponde_lonlat_vol(ieru)),'m_aer_emiss_vol_daily=',m_aer_emiss_vol_daily,'ieru=',ieru |
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| 165 | WRITE(lunout,*) 'IN traccoag, dlon=',dlon |
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| 166 | DO i=1,klon |
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| 167 | !Pinatubo eruption at 15.14N, 120.35E |
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| 168 | dlat_loc=180./RPI/2.*(boundslat(i,1)-boundslat(i,3)) ! dlat = half difference of boundary latitudes |
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| 169 | WRITE(lunout,*) 'IN traccoag, dlat=',dlat_loc |
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| 170 | IF ( xlat(i).GE.xlat_min_vol(ieru)-dlat_loc .AND. xlat(i).LT.xlat_max_vol(ieru)+dlat_loc .AND. & |
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| 171 | xlon(i).GE.xlon_min_vol(ieru)-dlon .AND. xlon(i).LT.xlon_max_vol(ieru)+dlon ) THEN |
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| 172 | ! |
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| 173 | WRITE(lunout,*) 'coordinates of volcanic injection point=',xlat(i),xlon(i),day_cur,mth_cur,year_cur |
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| 174 | WRITE(lunout,*) 'DD m_aer_emiss_vol_daily=',m_aer_emiss_vol_daily |
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| 175 | ! compute altLMDz |
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| 176 | altLMDz(:)=0.0 |
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| 177 | DO k=1, klev |
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| 178 | zrho=pplay(i,k)/t_seri(i,k)/RD !air density in kg/m3 |
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| 179 | zdm(k)=(paprs(i,k)-paprs(i,k+1))/RG !mass of layer in kg |
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| 180 | zdz=zdm(k)/zrho !thickness of layer in m |
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| 181 | altLMDz(k+1)=altLMDz(k)+zdz !altitude of interface |
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| 182 | ENDDO |
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[2690] | 183 | |
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[3526] | 184 | SELECT CASE(flag_sulf_emit_distrib) |
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| 185 | |
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| 186 | CASE(0) ! Gaussian distribution |
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| 187 | !compute distribution of emission to vertical model layers (based on Gaussian peak in altitude) |
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| 188 | f_lay_sum=0.0 |
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| 189 | DO k=1, klev |
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| 190 | f_lay_emiss(k)=0.0 |
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| 191 | DO i_int=1, n_int_alt |
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| 192 | alt=altLMDz(k)+float(i_int)*(altLMDz(k+1)-altLMDz(k))/float(n_int_alt) |
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| 193 | f_lay_emiss(k)=f_lay_emiss(k)+1./(sqrt(2.*RPI)*sigma_alt_vol(ieru))* & |
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| 194 | & exp(-0.5*((alt-altemiss_vol(ieru))/sigma_alt_vol(ieru))**2.)* & |
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| 195 | & (altLMDz(k+1)-altLMDz(k))/float(n_int_alt) |
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| 196 | ENDDO |
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| 197 | f_lay_sum=f_lay_sum+f_lay_emiss(k) |
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| 198 | ENDDO |
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| 199 | |
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| 200 | CASE(1) ! Uniform distribution |
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| 201 | ! In this case, parameter sigma_alt_vol(ieru) is considered to be half the |
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| 202 | ! height of the injection, centered around altemiss_vol(ieru) |
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| 203 | DO k=1, klev |
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| 204 | f_lay_emiss(k)=max(min(altemiss_vol(ieru)+sigma_alt_vol(ieru),altLMDz(k+1))- & |
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| 205 | & max(altemiss_vol(ieru)-sigma_alt_vol(ieru),altLMDz(k)),0.)/(2.*sigma_alt_vol(ieru)) |
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| 206 | f_lay_sum=f_lay_sum+f_lay_emiss(k) |
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| 207 | ENDDO |
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| 208 | |
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| 209 | END SELECT ! End CASE over flag_sulf_emit_distrib) |
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| 210 | |
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| 211 | WRITE(lunout,*) "IN traccoag m_aer_emiss_vol=",m_aer_emiss_vol(ieru) |
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| 212 | WRITE(lunout,*) "IN traccoag f_lay_emiss=",f_lay_emiss |
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| 213 | !correct for step integration error |
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| 214 | f_lay_emiss(:)=f_lay_emiss(:)/f_lay_sum |
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| 215 | !emission as SO2 gas (with m(SO2)=64/32*m_aer_emiss) |
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| 216 | !vertically distributed emission |
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| 217 | DO k=1, klev |
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| 218 | ! stretch emission over one day of Pinatubo eruption |
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| 219 | emission=m_aer_emiss_vol_daily*(mSO2mol/mSatom)/m_air_gridbox(i,k)*f_lay_emiss(k)/1./(86400.-pdtphys) |
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| 220 | tr_seri(i,k,id_SO2_strat)=tr_seri(i,k,id_SO2_strat)+emission*pdtphys |
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| 221 | budg_emi_so2(i)=budg_emi_so2(i)+emission*zdm(k)*mSatom/mSO2mol |
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| 222 | ENDDO |
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| 223 | ENDIF ! emission grid cell |
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| 224 | ENDDO ! klon loop |
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| 225 | WRITE(lunout,*) "IN traccoag (ieru=",ieru,") m_aer_emiss_vol_daily=",m_aer_emiss_vol_daily |
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| 226 | ENDIF ! emission period |
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| 227 | ENDDO ! eruption number |
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| 228 | |
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[2690] | 229 | CASE(2) ! stratospheric aerosol injections (SAI) |
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| 230 | ! |
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| 231 | DO i=1,klon |
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| 232 | ! SAI standard scenario with continuous emission from 1 grid point at the equator |
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| 233 | ! SAI emission on single month |
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| 234 | ! SAI continuous emission o |
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[3526] | 235 | dlat_loc=180./RPI/2.*(boundslat(i,1)-boundslat(i,3)) ! dlat = half difference of boundary latitudes |
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| 236 | IF ( xlat(i).GE.xlat_sai-dlat_loc .AND. xlat(i).LT.xlat_sai+dlat_loc .AND. & |
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[2704] | 237 | & xlon(i).GE.xlon_sai-dlon .AND. xlon(i).LT.xlon_sai+dlon ) THEN |
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[2752] | 238 | ! |
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[2690] | 239 | ! compute altLMDz |
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| 240 | altLMDz(:)=0.0 |
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| 241 | DO k=1, klev |
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[2752] | 242 | zrho=pplay(i,k)/t_seri(i,k)/RD !air density in kg/m3 |
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| 243 | zdm(k)=(paprs(i,k)-paprs(i,k+1))/RG !mass of layer in kg |
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| 244 | zdz=zdm(k)/zrho !thickness of layer in m |
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| 245 | altLMDz(k+1)=altLMDz(k)+zdz !altitude of interface |
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[2690] | 246 | ENDDO |
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[3526] | 247 | |
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| 248 | SELECT CASE(flag_sulf_emit_distrib) |
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| 249 | |
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| 250 | CASE(0) ! Gaussian distribution |
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[2690] | 251 | !compute distribution of emission to vertical model layers (based on Gaussian peak in altitude) |
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| 252 | f_lay_sum=0.0 |
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[3526] | 253 | DO k=1, klev |
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| 254 | f_lay_emiss(k)=0.0 |
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| 255 | DO i_int=1, n_int_alt |
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| 256 | alt=altLMDz(k)+float(i_int)*(altLMDz(k+1)-altLMDz(k))/float(n_int_alt) |
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| 257 | f_lay_emiss(k)=f_lay_emiss(k)+1./(sqrt(2.*RPI)*sigma_alt_sai)* & |
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| 258 | & exp(-0.5*((alt-altemiss_sai)/sigma_alt_sai)**2.)* & |
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| 259 | & (altLMDz(k+1)-altLMDz(k))/float(n_int_alt) |
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| 260 | ENDDO |
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| 261 | f_lay_sum=f_lay_sum+f_lay_emiss(k) |
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| 262 | ENDDO |
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| 263 | |
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| 264 | CASE(1) ! Uniform distribution |
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| 265 | f_lay_sum=0.0 |
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| 266 | ! In this case, parameter sigma_alt_vol(ieru) is considered to be half |
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| 267 | ! the height of the injection, centered around altemiss_sai |
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| 268 | DO k=1, klev |
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| 269 | f_lay_emiss(k)=max(min(altemiss_sai+sigma_alt_sai,altLMDz(k+1))- & |
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| 270 | & max(altemiss_sai-sigma_alt_sai,altLMDz(k)),0.)/(2.*sigma_alt_sai) |
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| 271 | f_lay_sum=f_lay_sum+f_lay_emiss(k) |
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| 272 | ENDDO |
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| 273 | |
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| 274 | END SELECT ! Gaussian or uniform distribution |
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| 275 | |
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| 276 | !correct for step integration error |
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| 277 | f_lay_emiss(:)=f_lay_emiss(:)/f_lay_sum |
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| 278 | !emission as SO2 gas (with m(SO2)=64/32*m_aer_emiss) |
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| 279 | !vertically distributed emission |
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[2690] | 280 | DO k=1, klev |
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[3526] | 281 | ! stretch emission over whole year (360d) |
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[3527] | 282 | emission=m_aer_emiss_sai*(mSO2mol/mSatom)/m_air_gridbox(i,k)*f_lay_emiss(k)/FLOAT(year_len)/86400. |
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[3526] | 283 | tr_seri(i,k,id_SO2_strat)=tr_seri(i,k,id_SO2_strat)+emission*pdtphys |
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| 284 | budg_emi_so2(i)=budg_emi_so2(i)+emission*zdm(k)*mSatom/mSO2mol |
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[2690] | 285 | ENDDO |
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[3526] | 286 | |
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| 287 | ! !emission as monodisperse particles with 0.1um dry radius (BIN21) |
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| 288 | ! !vertically distributed emission |
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| 289 | ! DO k=1, klev |
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| 290 | ! ! stretch emission over whole year (360d) |
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[3527] | 291 | ! emission=m_aer_emiss*(mH2SO4mol/mSatom)/m_part_dry(21)/m_air_gridbox(i,k)*f_lay_emiss(k)/FLOAT(year_len)/86400. |
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[3526] | 292 | ! tr_seri(i,k,id_BIN01_strat+20)=tr_seri(i,k,id_BIN01_strat+20)+emission*pdtphys |
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| 293 | ! budg_emi_part(i)=budg_emi_part(i)+emission*zdm(k)*mSatom/mH2SO4mol |
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| 294 | ! ENDDO |
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| 295 | ENDIF ! emission grid cell |
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| 296 | ENDDO ! klon loop |
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| 297 | |
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| 298 | CASE(3) ! --- SAI injection over a single band of longitude and between |
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| 299 | ! lat_min and lat_max |
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| 300 | |
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| 301 | DO i=1,klon |
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| 302 | ! SAI scenario with continuous emission |
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| 303 | dlat_loc=180./RPI/2.*(boundslat(i,1)-boundslat(i,3)) ! dlat = half difference of boundary latitudes |
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| 304 | theta_min = max(xlat(i)-dlat_loc,xlat_min_sai) |
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| 305 | theta_max = min(xlat(i)+dlat_loc,xlat_max_sai) |
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| 306 | IF ( xlat(i).GE.xlat_min_sai-dlat_loc .AND. xlat(i).LT.xlat_max_sai+dlat_loc .AND. & |
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| 307 | & xlon(i).GE.xlon_sai-dlon .AND. xlon(i).LT.xlon_sai+dlon ) THEN |
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| 308 | ! |
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| 309 | ! compute altLMDz |
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| 310 | altLMDz(:)=0.0 |
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| 311 | DO k=1, klev |
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| 312 | zrho=pplay(i,k)/t_seri(i,k)/RD !air density in kg/m3 |
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| 313 | zdm(k)=(paprs(i,k)-paprs(i,k+1))/RG !mass of layer in kg |
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| 314 | zdz=zdm(k)/zrho !thickness of layer in m |
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| 315 | altLMDz(k+1)=altLMDz(k)+zdz !altitude of interface |
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| 316 | ENDDO |
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| 317 | |
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| 318 | SELECT CASE(flag_sulf_emit_distrib) |
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| 319 | |
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| 320 | CASE(0) ! Gaussian distribution |
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| 321 | !compute distribution of emission to vertical model layers (based on |
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| 322 | !Gaussian peak in altitude) |
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| 323 | f_lay_sum=0.0 |
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| 324 | DO k=1, klev |
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| 325 | f_lay_emiss(k)=0.0 |
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| 326 | DO i_int=1, n_int_alt |
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| 327 | alt=altLMDz(k)+float(i_int)*(altLMDz(k+1)-altLMDz(k))/float(n_int_alt) |
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| 328 | f_lay_emiss(k)=f_lay_emiss(k)+1./(sqrt(2.*RPI)*sigma_alt_sai)* & |
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| 329 | & exp(-0.5*((alt-altemiss_sai)/sigma_alt_sai)**2.)* & |
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| 330 | & (altLMDz(k+1)-altLMDz(k))/float(n_int_alt) |
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| 331 | ENDDO |
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| 332 | f_lay_sum=f_lay_sum+f_lay_emiss(k) |
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| 333 | ENDDO |
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| 334 | |
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| 335 | CASE(1) ! Uniform distribution |
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| 336 | f_lay_sum=0.0 |
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| 337 | ! In this case, parameter sigma_alt_vol(ieru) is considered to be half |
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| 338 | ! the height of the injection, centered around altemiss_sai |
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| 339 | DO k=1, klev |
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| 340 | f_lay_emiss(k)=max(min(altemiss_sai+sigma_alt_sai,altLMDz(k+1))- & |
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| 341 | & max(altemiss_sai-sigma_alt_sai,altLMDz(k)),0.)/(2.*sigma_alt_sai) |
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| 342 | f_lay_sum=f_lay_sum+f_lay_emiss(k) |
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| 343 | ENDDO |
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| 344 | |
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| 345 | END SELECT ! Gaussian or uniform distribution |
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| 346 | |
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[2690] | 347 | !correct for step integration error |
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| 348 | f_lay_emiss(:)=f_lay_emiss(:)/f_lay_sum |
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| 349 | !emission as SO2 gas (with m(SO2)=64/32*m_aer_emiss) |
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| 350 | !vertically distributed emission |
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| 351 | DO k=1, klev |
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[2752] | 352 | ! stretch emission over whole year (360d) |
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[3526] | 353 | emission=m_aer_emiss_sai*(mSO2mol/mSatom)/m_air_gridbox(i,k)*f_lay_emiss(k)/ & |
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[3527] | 354 | & FLOAT(year_len)/86400.*(sin(theta_max/180.*RPI)-sin(theta_min/180.*RPI))/ & |
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[3526] | 355 | & (sin(xlat_max_sai/180.*RPI)-sin(xlat_min_sai/180.*RPI)) |
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[2752] | 356 | tr_seri(i,k,id_SO2_strat)=tr_seri(i,k,id_SO2_strat)+emission*pdtphys |
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| 357 | budg_emi_so2(i)=budg_emi_so2(i)+emission*zdm(k)*mSatom/mSO2mol |
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[2690] | 358 | ENDDO |
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[3526] | 359 | |
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[2690] | 360 | ! !emission as monodisperse particles with 0.1um dry radius (BIN21) |
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| 361 | ! !vertically distributed emission |
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| 362 | ! DO k=1, klev |
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[2752] | 363 | ! ! stretch emission over whole year (360d) |
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[3526] | 364 | ! emission=m_aer_emiss*(mH2SO4mol/mSatom)/m_part_dry(21)/m_air_gridbox(i,k)*f_lay_emiss(k)/year_len/86400 |
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[2752] | 365 | ! tr_seri(i,k,id_BIN01_strat+20)=tr_seri(i,k,id_BIN01_strat+20)+emission*pdtphys |
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| 366 | ! budg_emi_part(i)=budg_emi_part(i)+emission*zdm(k)*mSatom/mH2SO4mol |
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[2690] | 367 | ! ENDDO |
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| 368 | ENDIF ! emission grid cell |
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| 369 | ENDDO ! klon loop |
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| 370 | |
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| 371 | END SELECT ! emission scenario (flag_sulf_emit) |
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| 372 | |
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| 373 | !--read background concentrations of OCS and SO2 and lifetimes from input file |
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[2695] | 374 | !--update the variables defined in phys_local_var_mod |
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| 375 | CALL interp_sulf_input(debutphy,pdtphys,paprs,tr_seri) |
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[2690] | 376 | |
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| 377 | !--convert OCS to SO2 in the stratosphere |
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[2752] | 378 | CALL ocs_to_so2(pdtphys,tr_seri,t_seri,pplay,paprs,is_strato) |
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[2690] | 379 | |
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| 380 | !--convert SO2 to H2SO4 |
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[2752] | 381 | CALL so2_to_h2so4(pdtphys,tr_seri,t_seri,pplay,paprs,is_strato) |
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[2690] | 382 | |
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| 383 | !--common routine for nucleation and condensation/evaporation with adaptive timestep |
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| 384 | CALL micphy_tstep(pdtphys,tr_seri,t_seri,pplay,paprs,rh,is_strato) |
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| 385 | |
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| 386 | !--call coagulation routine |
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| 387 | CALL coagulate(pdtphys,mdw,tr_seri,t_seri,pplay,dens_aer,is_strato) |
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| 388 | |
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| 389 | !--call sedimentation routine |
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| 390 | CALL aer_sedimnt(pdtphys, t_seri, pplay, paprs, tr_seri, dens_aer) |
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| 391 | |
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| 392 | !--compute mass concentration of PM2.5 sulfate particles (wet diameter and mass) at the surface for health studies |
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| 393 | surf_PM25_sulf(:)=0.0 |
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| 394 | DO i=1,klon |
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| 395 | DO it=1, nbtr_bin |
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| 396 | IF (mdw(it) .LT. 2.5e-6) THEN |
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| 397 | !surf_PM25_sulf(i)=surf_PM25_sulf(i)+tr_seri(i,1,it+nbtr_sulgas)*m_part(i,1,it) & |
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[3526] | 398 | !assume that particles consist of ammonium sulfate at the surface (132g/mol) |
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| 399 | !and are dry at T = 20 deg. C and 50 perc. humidity |
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[2690] | 400 | surf_PM25_sulf(i)=surf_PM25_sulf(i)+tr_seri(i,1,it+nbtr_sulgas) & |
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| 401 | & *132./98.*dens_aer_dry*4./3.*RPI*(mdw(it)/2.)**3 & |
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[2752] | 402 | & *pplay(i,1)/t_seri(i,1)/RD*1.e9 |
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[2690] | 403 | ENDIF |
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| 404 | ENDDO |
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| 405 | ENDDO |
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| 406 | |
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[2695] | 407 | ! CALL minmaxsimple(tr_seri(:,:,id_SO2_strat),0.0,0.0,'fin SO2') |
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| 408 | ! DO it=1, nbtr_bin |
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| 409 | ! CALL minmaxsimple(tr_seri(:,:,nbtr_sulgas+it),0.0,0.0,'fin bin ') |
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| 410 | ! ENDDO |
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| 411 | |
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[2690] | 412 | END SUBROUTINE traccoag |
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| 413 | |
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| 414 | END MODULE traccoag_mod |
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