[86] | 1 | SUBROUTINE dustlift(ngrid,nlay,nq,rho, |
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| 2 | $ pcdh_true,pcdh,co2ice, |
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[38] | 3 | $ dqslift) |
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[1036] | 4 | |
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[1038] | 5 | #ifndef MESOSCALE |
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[1036] | 6 | use tracer_mod, only: alpha_lift, radius |
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[1038] | 7 | #else |
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| 8 | use tracer_mod, only: alpha_lift, radius, |
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| 9 | & igcm_dust_mass, igcm_dust_number, |
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| 10 | & ref_r0,r3n_q |
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| 11 | #endif |
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[1226] | 12 | USE comcstfi_h |
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[38] | 13 | IMPLICIT NONE |
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| 14 | |
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| 15 | c======================================================================= |
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| 16 | c |
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| 17 | c Dust lifting by surface winds |
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| 18 | c Computing flux to the middle of the first layer |
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| 19 | c (Called by vdifc) |
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| 20 | c |
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| 21 | c======================================================================= |
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| 22 | |
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| 23 | c----------------------------------------------------------------------- |
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| 24 | c declarations: |
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| 25 | c ------------- |
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| 26 | |
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| 27 | c |
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| 28 | c arguments: |
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| 29 | c ---------- |
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| 30 | |
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| 31 | c INPUT |
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| 32 | integer ngrid, nlay, nq |
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| 33 | real rho(ngrid) ! density (kg.m-3) at surface |
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| 34 | real pcdh_true(ngrid) ! Cd |
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| 35 | real pcdh(ngrid) ! Cd * |V| |
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| 36 | real co2ice(ngrid) |
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| 37 | |
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| 38 | c OUTPUT |
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| 39 | real dqslift(ngrid,nq) !surface dust flux to mid-layer (<0 when lifing) |
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| 40 | c real pb(ngrid,nlay) ! diffusion to surface coeff. |
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| 41 | |
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| 42 | c local: |
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| 43 | c ------ |
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| 44 | INTEGER ig,iq |
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[1047] | 45 | REAL fhoriz(ngrid) ! Horizontal dust flux |
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[38] | 46 | REAL ust,us |
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| 47 | REAL stress_seuil |
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| 48 | SAVE stress_seuil |
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| 49 | DATA stress_seuil/0.0225/ ! stress seuil soulevement (N.m2) |
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| 50 | |
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[86] | 51 | #ifdef MESOSCALE |
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| 52 | !!!! AS: In the mesoscale model we'd like to easily set |
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| 53 | !!!! AS: ... stress for lifting |
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| 54 | !!!! AS: you have to compile with -DMESOSCALE to do so |
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| 55 | REAL alpha |
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[310] | 56 | REAL r0_lift |
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[86] | 57 | INTEGER ierr |
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[310] | 58 | REAL ulim |
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[86] | 59 | OPEN(99,file='stress.def',status='old',form='formatted' |
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| 60 | . ,iostat=ierr) |
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| 61 | !!! no file => default values |
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| 62 | IF(ierr.EQ.0) THEN |
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[310] | 63 | READ(99,*) ulim !ulim = sqrt(stress_seuil/rho) avec rho = 0.02. |
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| 64 | !prendre ulim = 1.061 m/s pour avoir stress_seuil = 0.0225 |
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[86] | 65 | READ(99,*) alpha |
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[310] | 66 | stress_seuil = 0.02 * ulim * ulim |
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[86] | 67 | write(*,*) 'USER-DEFINED threshold: ', stress_seuil, alpha |
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| 68 | CLOSE(99) |
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[310] | 69 | alpha_lift(igcm_dust_mass) = alpha |
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| 70 | r0_lift = radius(igcm_dust_mass) / ref_r0 |
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| 71 | alpha_lift(igcm_dust_number)=r3n_q* |
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| 72 | & alpha_lift(igcm_dust_mass)/r0_lift**3 |
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| 73 | write(*,*) 'set dust number: ', alpha_lift(igcm_dust_number) |
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[86] | 74 | ENDIF |
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| 75 | #endif |
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[38] | 76 | |
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| 77 | c --------------------------------- |
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| 78 | c Computing horizontal flux: fhoriz |
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| 79 | c --------------------------------- |
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| 80 | |
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| 81 | do ig=1,ngrid |
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| 82 | fhoriz(ig) = 0. ! initialisation |
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| 83 | |
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| 84 | c Selection of points where surface dust is available |
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| 85 | c ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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| 86 | c if (latid(ig).ge.80.) goto 99 ! N permanent polar caps |
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| 87 | c if (latid(ig).le.-80.) goto 99 ! S polar deposits |
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| 88 | c if ((longd(ig).ge.-141. .and. longd(ig).le.-127.) |
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| 89 | c & .and.(latid(ig).ge.12. .and. latid(ig).le.23.))goto 99 ! olympus |
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| 90 | c if ((longd(ig).ge.-125. .and. longd(ig).le.-118.) |
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| 91 | c & .and.(latid(ig).ge.-12. .and. latid(ig).le.-6.))goto 99 ! Arsia |
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| 92 | c if ((longd(ig).ge.-116. .and. longd(ig).le.-109.) |
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| 93 | c & .and.(latid(ig).ge.-5. .and. latid(ig).le. 5.))goto 99 ! pavonis |
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| 94 | c if ((longd(ig).ge.-109. .and. longd(ig).le.-100.) |
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| 95 | c & .and.(latid(ig).ge. 7. .and. latid(ig).le. 16.))goto 99 ! ascraeus |
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| 96 | c if ((longd(ig).ge. 61. .and. longd(ig).le. 63.) |
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| 97 | c & .and.(latid(ig).ge. 63. .and. latid(ig).le. 64.))goto 99 !weird point |
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| 98 | if (co2ice(ig).gt.0.) goto 99 |
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| 99 | |
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| 100 | |
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| 101 | c Is the wind strong enough ? |
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| 102 | c ~~~~~~~~~~~~~~~~~~~~~~~~~~~ |
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| 103 | ust = sqrt(stress_seuil/rho(ig)) |
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| 104 | us = pcdh(ig) / sqrt(pcdh_true(ig)) ! ustar=cd*v /sqrt(cd) |
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| 105 | if (us.gt.ust) then |
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| 106 | c If lifting ? |
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| 107 | c Calcul du flux suivant Marticorena ( en fait white (1979)) |
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| 108 | |
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| 109 | fhoriz(ig) = 2.61*(rho(ig)/g) * |
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| 110 | & (us -ust) * (us + ust)**2 |
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| 111 | end if |
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| 112 | 99 continue |
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| 113 | end do |
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| 114 | |
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| 115 | c ------------------------------------- |
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| 116 | c Computing vertical flux and diffusion |
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| 117 | c ------------------------------------- |
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| 118 | |
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| 119 | do iq=1,nq |
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| 120 | do ig=1,ngrid |
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| 121 | dqslift(ig,iq)= -alpha_lift(iq)* fhoriz(ig) |
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| 122 | |
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| 123 | |
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| 124 | cc le flux vertical remplace le terme de diffusion turb. qui est mis a zero |
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| 125 | c zb(ig,1) = 0. |
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| 126 | cc If surface deposition by turbulence diffusion (impaction...) |
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| 127 | cc if(fhoriz(ig).ne.0) then |
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| 128 | cc zb(ig,1) = zcdh(ig)*zb0(ig,1) |
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| 129 | cc AMount of Surface deposition ! |
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| 130 | cc pdqs_dif(ig,iq)=pdqs_dif(ig,iq) + |
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| 131 | cc & zb(ig,1)*zq(ig,1,iq)/ptimestep |
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| 132 | cc write(*,*) 'zb(1) = ' , zb(ig,1),zcdh(ig),zb0(ig,1) |
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| 133 | cc |
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| 134 | |
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| 135 | enddo |
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| 136 | enddo |
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| 137 | |
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| 138 | RETURN |
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| 139 | END |
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| 140 | |
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