! ! $Id: cond_evap_tstep_mod.F90 3526 2019-05-28 13:00:44Z jyg $ ! MODULE cond_evap_tstep_mod ! based on UPMC aerosol model by Slimane Bekki ! adapted for stratospheric sulfate aerosol in LMDZ by Christoph Kleinschmitt CONTAINS SUBROUTINE condens_evapor_rate(R2SO4G,t_seri,pplay,ACTSO4,R2SO4, & & DENSO4,f_r_wet,RRSI,Vbin,FL,ASO4,DNDR) ! ! INPUT: ! R2SO4: aerosol H2SO4 weight fraction (percent) ! ACTSO4: H2SO4 activity ! R2SO4G: number density of gaseous H2SO4 [molecules/cm3] ! t_seri: temperature (K) ! DENSO4: aerosol density (gr/cm3) USE aerophys USE infotrac USE YOMCST, ONLY : RPI IMPLICIT NONE ! input variables REAL R2SO4G !H2SO4 number density [molecules/cm3] REAL t_seri REAL pplay REAL ACTSO4 REAL R2SO4 REAL DENSO4 REAL f_r_wet REAL RRSI(nbtr_bin) REAL Vbin(nbtr_bin) ! output variables REAL FL(nbtr_bin) REAL ASO4(nbtr_bin) REAL DNDR(nbtr_bin) ! local variables INTEGER IK REAL ALPHA,CST REAL WH2,RP,VTK,AA,FL1,RKNUD REAL DND REAL ATOT,AH2O REAL RRSI_wet(nbtr_bin) REAL Vbin_wet(nbtr_bin) REAL MH2SO4,MH2O,BOLZ,FPATH ! /// MOLEC CONDENSATION GROWTH (DUE TO CHANGES IN H2SO4 AND SO H2O) ! ------------------------------------------------------------------ ! EXCEPT CN ! RK:H2SO4 WEIGHT PERCENT DOESN'T CHANGE ! BE CAREFUL,H2SO4 WEIGHT PERCENTAGE ! WEIGHT OF 1 MOLEC IN G MH2O =1000.*mH2Omol !18.016*1.66E-24 MH2SO4=1000.*mH2SO4mol !98.082*1.66E-24 ! BOLTZMANN CONSTANTE IN DYN.CM/K BOLZ =1.381E-16 ! MOLECULAR ACCOMODATION OF H2SO4 ! raes and van dingen ALPHA =0.1 ! FPLAIR=(2.281238E-5)*TAIR/PAIR ! 1.E2 (m to cm), CST=1.E2*2.281238E-5 ! compute local wet particle radius and volume RRSI_wet(:)=RRSI(:)*f_r_wet Vbin_wet(:)=Vbin(:)*f_r_wet**3 ! Pruppa and Klett FPATH=CST*t_seri/pplay ! H2SO4 mass fraction in aerosol WH2=R2SO4*1.0E-2 IF(WH2.EQ.0.0) RETURN ! ACTIVITY COEFFICIENT(SEE GIAUQUE,1951) ! AYERS ET AL (1980) ! (MU-MU0) RP=-10156.0/t_seri +16.259-(ACTSO4*4.184)/(8.31441*t_seri) ! DROPLET H2SO4 PRESSURE IN DYN.CM-2 RP=EXP(RP)*1.01325E6/0.086 ! RP=EXP(RP)*1.01325E6 ! H2SO4 NUMBER DENSITY NEAR DROPLET ! R=8.31E7 DYN.CM.MOL-1*K-1 ! R/AVOGADRO NUMBER=DYN.CM.MOLEC-1*K-1 DND=RP*6.02E23/(8.31E7*t_seri) ! MEAN KINETIC VELOCITY ! DYN*CM*K/(K*GR)=(CM/SEC2)*CM ! IN CM/SEC VTK=SQRT(8.0*BOLZ*t_seri/(RPI*MH2SO4)) ! KELVIN EFFECT FACTOR !CK 20160613: bug fix, removed factor 250 (from original code by S. Bekki) ! AA =2.0*MH2O*72.0/(DENSO4*BOLZ*t_seri*250.0) AA =2.0*MH2O*72.0/(DENSO4*BOLZ*t_seri) ! Loop on bin radius (RRSI in cm) DO IK=1,nbtr_bin ! KELVIN EFFECT DNDR(IK) =DND*EXP(AA/RRSI_wet(IK)) FL1=RPI*ALPHA*VTK*(R2SO4G-DNDR(IK)) ! TURCO(1979) FOR HNO3:ALH2SO4 CONDENSATION= ALH2SO4 EVAPORATION ! RPI*R2*VTK IS EQUIVALENT TO DIFFUSION COEFFICIENT ! EXTENSION OF THE RELATION FOR DIFFUSION KINETICS ! KNUDSEN NUMBER FPATH/RRSI ! NEW VERSION (SEE NOTES) RKNUD=FPATH/RRSI_wet(IK) ! SENFELD FL(IK)=FL1*RRSI_wet(IK)**2*( 1.0 +RKNUD ) & & /( 1.0 +ALPHA/(2.0*RKNUD) +RKNUD ) ! TURCO ! RL= (4.0/3.0 +0.71/RKNUD)/(1.0+1.0/RKNUD) ! * +4.0*(1.0-ALPHA)/(3.0*ALPHA) ! FL=FL1*RRSI(IK)*RRSI(IK) ! * /( (3.0*ALPHA/4.0)*(1.0/RKNUD+RL*ALPHA) ) ! INITIAL NUMBER OF H2SO4 MOLEC OF 1 DROPLET ATOT=4.0*RPI*DENSO4*(RRSI_wet(IK)**3)/3.0 !attention: g and cm ASO4(IK)=WH2*ATOT/MH2SO4 !attention: g ! ATOT=4.0*RPI*dens_aer(I,J)/1000.*(RRSI(IK)**3)/3.0 ! ASO4=mfrac_H2SO4*ATOT/MH2SO4 ! INITIAL NUMBER OF H2O MOLEC OF 1 DROPLET AH2O=(1.0-WH2)*ATOT/MH2O !attention: g ! CHANGE OF THE NUMBER OF H2SO4 MOLEC OF 1 DROPLET DURING DT ! IT IS FOR KEM BUT THERE ARE OTHER WAYS ENDDO !loop over bins END SUBROUTINE condens_evapor_rate !******************************************************************** SUBROUTINE cond_evap_part(dt,FL,ASO4,f_r_wet,RRSI,Vbin,tr_seri) USE aerophys USE infotrac USE YOMCST, ONLY : RPI IMPLICIT NONE ! input variables REAL dt REAL FL(nbtr_bin) REAL ASO4(nbtr_bin) REAL f_r_wet REAL RRSI(nbtr_bin) REAL Vbin(nbtr_bin) ! output variables REAL tr_seri(nbtr) ! local variables REAL tr_seri_new(nbtr) INTEGER IK,JK,k REAL Vnew REAL RRSI_wet(nbtr_bin) REAL Vbin_wet(nbtr_bin) REAL sum_IK(nbtr_bin) REAL ff(nbtr_bin,nbtr_bin) tr_seri_new(:)=tr_seri(:) ! compute local wet particle radius and volume RRSI_wet(:)=RRSI(:)*f_r_wet Vbin_wet(:)=Vbin(:)*f_r_wet**3 *1.e6 !Vbin_wet in cm3 (as Vnew) ! compute distribution factor for particles of intermediate size (from Jacobson 1994, equation 13) DO IK=1,nbtr_bin Vnew=4.0*RPI*(RRSI_wet(IK)**3)/3.0*(1.+FL(IK)*dt/ASO4(IK)) ff(IK,:)=0.0 DO k=1, nbtr_bin IF (k.LE.(nbtr_bin-1)) THEN IF (Vbin_wet(k).LE.Vnew.AND.Vnew.LT.Vbin_wet(k+1)) THEN ff(IK,k)= Vbin_wet(k)/Vnew*(Vbin_wet(k+1)-Vnew)/(Vbin_wet(k+1)-Vbin_wet(k)) ENDIF ENDIF IF (k.EQ.1.AND.Vnew.LE.Vbin_wet(k)) THEN ff(IK,k)= 1. ENDIF IF (k.GT.1) THEN IF (Vbin_wet(k-1).LT.Vnew.AND.Vnew.LT.Vbin_wet(k)) THEN ff(IK,k)= 1.-ff(IK,k-1) ENDIF ENDIF IF (k.EQ.nbtr_bin.AND.Vnew.GE.Vbin_wet(k)) THEN ff(IK,k)= 1. ENDIF ENDDO ! correction of ff for volume conservation DO k=1, nbtr_bin ff(IK,k)=ff(IK,k)*Vnew/Vbin_wet(k) ENDDO ENDDO !loop over bins DO IK=1, nbtr_bin sum_IK(IK)=0.0 DO JK=1, nbtr_bin sum_IK(IK)=sum_IK(IK)+tr_seri(JK+nbtr_sulgas)*ff(JK,IK) ENDDO ! compute new particle concentrations tr_seri_new(IK+nbtr_sulgas)=sum_IK(IK) ENDDO tr_seri(:)=tr_seri_new(:) END SUBROUTINE cond_evap_part END MODULE cond_evap_tstep_mod