SUBROUTINE dustlift(ngrid,nlay,nq,rho, $ pcdh_true,pcdh,co2ice, $ dqslift) #ifndef MESOSCALE use tracer_mod, only: alpha_lift, radius #else use tracer_mod, only: alpha_lift, radius, & igcm_dust_mass, igcm_dust_number, & ref_r0,r3n_q #endif USE comcstfi_h IMPLICIT NONE c======================================================================= c c Dust lifting by surface winds c Computing flux to the middle of the first layer c (Called by vdifc) c c======================================================================= c----------------------------------------------------------------------- c declarations: c ------------- c c arguments: c ---------- c INPUT integer ngrid, nlay, nq real rho(ngrid) ! density (kg.m-3) at surface real pcdh_true(ngrid) ! Cd real pcdh(ngrid) ! Cd * |V| real co2ice(ngrid) c OUTPUT real dqslift(ngrid,nq) !surface dust flux to mid-layer (<0 when lifing) c real pb(ngrid,nlay) ! diffusion to surface coeff. c local: c ------ INTEGER ig,iq REAL fhoriz(ngrid) ! Horizontal dust flux REAL ust,us REAL stress_seuil SAVE stress_seuil DATA stress_seuil/0.0225/ ! stress seuil soulevement (N.m2) #ifdef MESOSCALE !!!! AS: In the mesoscale model we'd like to easily set !!!! AS: ... stress for lifting !!!! AS: you have to compile with -DMESOSCALE to do so REAL alpha REAL r0_lift INTEGER ierr REAL ulim OPEN(99,file='stress.def',status='old',form='formatted' . ,iostat=ierr) !!! no file => default values IF(ierr.EQ.0) THEN READ(99,*) ulim !ulim = sqrt(stress_seuil/rho) avec rho = 0.02. !prendre ulim = 1.061 m/s pour avoir stress_seuil = 0.0225 READ(99,*) alpha stress_seuil = 0.02 * ulim * ulim write(*,*) 'USER-DEFINED threshold: ', stress_seuil, alpha CLOSE(99) alpha_lift(igcm_dust_mass) = alpha r0_lift = radius(igcm_dust_mass) / ref_r0 alpha_lift(igcm_dust_number)=r3n_q* & alpha_lift(igcm_dust_mass)/r0_lift**3 write(*,*) 'set dust number: ', alpha_lift(igcm_dust_number) ENDIF #endif c --------------------------------- c Computing horizontal flux: fhoriz c --------------------------------- do ig=1,ngrid fhoriz(ig) = 0. ! initialisation c Selection of points where surface dust is available c ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ c if (latid(ig).ge.80.) goto 99 ! N permanent polar caps c if (latid(ig).le.-80.) goto 99 ! S polar deposits c if ((longd(ig).ge.-141. .and. longd(ig).le.-127.) c & .and.(latid(ig).ge.12. .and. latid(ig).le.23.))goto 99 ! olympus c if ((longd(ig).ge.-125. .and. longd(ig).le.-118.) c & .and.(latid(ig).ge.-12. .and. latid(ig).le.-6.))goto 99 ! Arsia c if ((longd(ig).ge.-116. .and. longd(ig).le.-109.) c & .and.(latid(ig).ge.-5. .and. latid(ig).le. 5.))goto 99 ! pavonis c if ((longd(ig).ge.-109. .and. longd(ig).le.-100.) c & .and.(latid(ig).ge. 7. .and. latid(ig).le. 16.))goto 99 ! ascraeus c if ((longd(ig).ge. 61. .and. longd(ig).le. 63.) c & .and.(latid(ig).ge. 63. .and. latid(ig).le. 64.))goto 99 !weird point if (co2ice(ig).gt.0.) goto 99 c Is the wind strong enough ? c ~~~~~~~~~~~~~~~~~~~~~~~~~~~ ust = sqrt(stress_seuil/rho(ig)) us = pcdh(ig) / sqrt(pcdh_true(ig)) ! ustar=cd*v /sqrt(cd) if (us.gt.ust) then c If lifting ? c Calcul du flux suivant Marticorena ( en fait white (1979)) fhoriz(ig) = 2.61*(rho(ig)/g) * & (us -ust) * (us + ust)**2 end if 99 continue end do c ------------------------------------- c Computing vertical flux and diffusion c ------------------------------------- do iq=1,nq do ig=1,ngrid dqslift(ig,iq)= -alpha_lift(iq)* fhoriz(ig) cc le flux vertical remplace le terme de diffusion turb. qui est mis a zero c zb(ig,1) = 0. cc If surface deposition by turbulence diffusion (impaction...) cc if(fhoriz(ig).ne.0) then cc zb(ig,1) = zcdh(ig)*zb0(ig,1) cc AMount of Surface deposition ! cc pdqs_dif(ig,iq)=pdqs_dif(ig,iq) + cc & zb(ig,1)*zq(ig,1,iq)/ptimestep cc write(*,*) 'zb(1) = ' , zb(ig,1),zcdh(ig),zb0(ig,1) cc enddo enddo RETURN END