!======================================================================= ! THERMCELL_MAIN_MARS !======================================================================= ! This routine is called by calltherm_interface and is inside a sub-timestep ! loop. It computes thermals properties from parametrized entrainment and ! detrainment rate as well as the source profile. ! Mass flux are then computed and temperature and CO2 MMR are transported. !======================================================================= ! Author : A. Colaitis 2011-01-05 (with updates 2011-2013) ! after C. Rio and F. Hourdin ! Institution : Laboratoire de Meteorologie Dynamique (LMD) Paris, France ! ----------------------------------------------------------------------- ! Corresponding author : A. Spiga aymeric.spiga_AT_upmc.fr ! ----------------------------------------------------------------------- ! ASSOCIATED FILES ! --> calltherm_interface.F90 ! --> thermcell_dqup.F90 ! --> comtherm_h.F90 !======================================================================= ! Reference paper: ! A. Colaïtis, A. Spiga, F. Hourdin, C. Rio, F. Forget, and E. Millour. ! A thermal plume model for the Martian convective boundary layer. ! Journal of Geophysical Research (Planets), 118:1468-1487, July 2013. ! http://dx.doi.org/10.1002/jgre.20104 ! http://arxiv.org/abs/1306.6215 ! ----------------------------------------------------------------------- ! Reference paper for terrestrial plume model: ! C. Rio and F. Hourdin. ! A thermal plume model for the convective boundary layer : Representation of cumulus clouds. ! Journal of the Atmospheric Sciences, 65:407-425, 2008. ! ----------------------------------------------------------------------- SUBROUTINE thermcell_main_mars(ngrid,nlayer,nq,igcm_co2 & & ,ptimestep & & ,pplay,pplev,pphi,zlev,zlay & & ,pu,pv,pt,pq,pq2 & & ,pdtadj,pdqadj & & ,fm,entr,detr,lmax,zmax,limz & & ,zw2,fraca & & ,zpopsk,heatFlux,heatFlux_down & & ,buoyancyOut, buoyancyEst) USE comtherm_h #ifndef MESOSCALE use planetwide_mod, only: planetwide_maxval #endif ! SHARED VARIABLES. This needs adaptations in another climate model. ! contains physical constant values such as ! "g" : gravitational acceleration (m.s-2) ! "r" : recuced gas constant (J.K-1.mol-1) USE comcstfi_h IMPLICIT NONE !======================================================================= ! ============== INPUTS ============== INTEGER, INTENT(IN) :: ngrid ! number of horizontal grid points INTEGER, INTENT(IN) :: nlayer ! number of vertical grid points INTEGER, INTENT(IN) :: nq ! number of tracer species INTEGER, INTENT(IN) :: igcm_co2 ! index of the CO2 tracer in mixing ratio array ! --> 0 if no tracer is CO2 (or no tracer at all) ! --> this prepares special treatment for polar night mixing REAL, INTENT(IN) :: ptimestep !subtimestep (s) REAL, INTENT(IN) :: pt(ngrid,nlayer) !temperature (K) REAL, INTENT(IN) :: pu(ngrid,nlayer) !u component of the wind (ms-1) REAL, INTENT(IN) :: pv(ngrid,nlayer) !v component of the wind (ms-1) REAL, INTENT(IN) :: pq(ngrid,nlayer,nq) !tracer concentration (kg/kg) REAL, INTENT(IN) :: pq2(ngrid,nlayer) ! Turbulent Kinetic Energy REAL, INTENT(IN) :: pplay(ngrid,nlayer) !Pressure at the middle of the layers (Pa) REAL, INTENT(IN) :: pplev(ngrid,nlayer+1) !intermediate pressure levels (Pa) REAL, INTENT(IN) :: pphi(ngrid,nlayer) !Geopotential at the middle of the layers (m2s-2) REAL, INTENT(IN) :: zlay(ngrid,nlayer) ! altitude at the middle of the layers REAL, INTENT(IN) :: zlev(ngrid,nlayer+1) ! altitude at layer boundaries ! ============== OUTPUTS ============== ! TEMPERATURE REAL, INTENT(OUT) :: pdtadj(ngrid,nlayer) !temperature change from thermals dT/dt (K/s) ! DIAGNOSTICS REAL, INTENT(OUT) :: zw2(ngrid,nlayer+1) ! vertical velocity (m/s) REAL, INTENT(OUT) :: heatFlux(ngrid,nlayer) ! interface heatflux REAL, INTENT(OUT) :: heatFlux_down(ngrid,nlayer) ! interface heat flux from downdraft INTEGER, INTENT(OUT) :: limz ! limit vertical index for integration ! ============== LOCAL ================ REAL :: pdqadj(ngrid,nlayer,nq) !tracer change from thermals dq/dt, only for CO2 (the rest can be advected outside of the loop) ! dummy variables when output not needed : REAL :: buoyancyOut(ngrid,nlayer) ! interlayer buoyancy term REAL :: buoyancyEst(ngrid,nlayer) ! interlayer estimated buoyancy term ! ============== LOCAL ================ INTEGER ig,k,l,ll,iq INTEGER lmax(ngrid),lmin(ngrid),lalim(ngrid) REAL zmax(ngrid) REAL ztva(ngrid,nlayer),zw_est(ngrid,nlayer+1),ztva_est(ngrid,nlayer) REAL zh(ngrid,nlayer) REAL zdthladj(ngrid,nlayer) REAL zdthladj_down(ngrid,nlayer) REAL ztvd(ngrid,nlayer) REAL ztv(ngrid,nlayer) REAL zu(ngrid,nlayer),zv(ngrid,nlayer),zo(ngrid,nlayer) REAL zva(ngrid,nlayer) REAL zua(ngrid,nlayer) REAL zta(ngrid,nlayer) REAL fraca(ngrid,nlayer+1) REAL q2(ngrid,nlayer) REAL rho(ngrid,nlayer),rhobarz(ngrid,nlayer),masse(ngrid,nlayer) REAL zpopsk(ngrid,nlayer) REAL wmax(ngrid) REAL fm(ngrid,nlayer+1),entr(ngrid,nlayer),detr(ngrid,nlayer) REAL fm_down(ngrid,nlayer+1) REAL ztla(ngrid,nlayer) REAL f_star(ngrid,nlayer+1),entr_star(ngrid,nlayer) REAL detr_star(ngrid,nlayer) REAL alim_star_tot(ngrid) REAL alim_star(ngrid,nlayer) REAL alim_star_clos(ngrid,nlayer) REAL f(ngrid) REAL detrmod(ngrid,nlayer) REAL teta_th_int(ngrid,nlayer) REAL teta_env_int(ngrid,nlayer) REAL teta_down_int(ngrid,nlayer) CHARACTER (LEN=80) :: abort_message INTEGER ndt ! ============= PLUME VARIABLES ============ REAL w_est(ngrid,nlayer+1) REAL wa_moy(ngrid,nlayer+1) REAL wmaxa(ngrid) REAL zdz,zbuoy(ngrid,nlayer),zw2m LOGICAL activecell(ngrid),activetmp(ngrid) INTEGER tic ! ========================================== ! ============= HEIGHT VARIABLES =========== REAL num(ngrid) REAL denom(ngrid) REAL zlevinter(ngrid) ! ========================================= ! ============= CLOSURE VARIABLES ========= REAL zdenom(ngrid) REAL alim_star2(ngrid) REAL alim_star_tot_clos(ngrid) INTEGER llmax ! ========================================= ! ============= FLUX2 VARIABLES =========== INTEGER ncorecfm1,ncorecfm2,ncorecfm3,ncorecalpha INTEGER ncorecfm4,ncorecfm5,ncorecfm6,ncorecfm7,ncorecfm8 REAL zfm REAL f_old,ddd0,eee0,ddd,eee,zzz REAL fomass_max,alphamax ! ========================================= ! ============== Theta_M Variables ======== REAL m_co2, m_noco2, A , B SAVE A, B REAL zhc(ngrid,nlayer) REAL ratiom(ngrid,nlayer) !$OMP THREADPRIVATE(A,B) ! ========================================= !----------------------------------------------------------------------- ! initialization: ! --------------- entr(:,:)=0. ! entrainment mass flux detr(:,:)=0. ! detrainment mass flux fm(:,:)=0. ! upward mass flux zhc(:,:)=pt(:,:)/zpopsk(:,:) ! potential temperature ndt=1 !....................................................................... ! Special treatment for co2: !....................................................................... ! ********************************************************************** ! In order to take into account the effect of vertical molar mass ! gradient on convection, we define modified theta that depends ! on the mass mixing ratio of Co2 in the cell. ! See for details: ! ! Forget, F. and Millour, E. et al. "Non condensable gas enrichment and depletion ! in the martian polar regions", third international workshop on the Mars Atmosphere: ! Modeling and Observations, 1447, 9106. year: 2008 ! ! This is especially important for modelling polar convection. ! ********************************************************************** if (igcm_co2.ne.0) then m_co2 = 44.01E-3 ! CO2 molecular mass (kg/mol) m_noco2 = 33.37E-3 ! Non condensible mol mass (kg/mol) ! Compute A and B coefficient use to compute ! mean molecular mass Mair defined by ! 1/Mair = q(igcm_co2)/m_co2 + (1-q(igcm_co2))/m_noco2 ! 1/Mair = A*q(igcm_co2) + B A =(1/m_co2 - 1/m_noco2) B=1/m_noco2 ! Special case if one of the tracers is CO2 gas DO l=1,nlayer DO ig=1,ngrid ztv(ig,l) = zhc(ig,l)*(A*pq(ig,l,igcm_co2)+B) ENDDO ENDDO else ztv(:,:)=zhc(:,:) end if !------------------------------------------------------------------------ ! where are the different quantities defined ? !------------------------------------------------------------------------ ! -------------------- ! ! ! + + + + + + + + + + + ! ! ! wa, fraca, wd, fracd -------------------- zlev(2), rhobarz ! wh,wt,wo ... ! ! + + + + + + + + + + + zh,zu,zv,zo,rho ! ! ! -------------------- zlev(1) ! \\\\\\\\\\\\\\\\\\\\ ! ! !----------------------------------------------------------------------- ! Densities at layer and layer interface (see above), mass: !----------------------------------------------------------------------- rho(:,:)=pplay(:,:)/(r*pt(:,:)) rhobarz(:,1)=rho(:,1) do l=2,nlayer rhobarz(:,l)=pplev(:,l)/(r*0.5*(pt(:,l)+pt(:,l-1))) enddo ! mass computation do l=1,nlayer masse(:,l)=(pplev(:,l)-pplev(:,l+1))/g enddo !----------------------------------------------------------------- ! Schematic representation of an updraft: !------------------------------------------------------------------ ! ! /|\ ! -------- | F_k+1 ------- ! ----> D_k ! /|\ <---- E_k , A_k ! -------- | F_k --------- ! ----> D_k-1 ! <---- E_k-1 , A_k-1 ! ! ! --------------------------- ! ! ----- F_lmax+1=0 ---------- \ ! lmax (zmax) | ! --------------------------- | ! | ! --------------------------- | ! | ! --------------------------- | ! | ! --------------------------- | ! | ! --------------------------- | ! | E ! --------------------------- | D ! | ! --------------------------- | ! | ! --------------------------- \ | ! lalim | | ! --------------------------- | | ! | | ! --------------------------- | | ! | A | ! --------------------------- | | ! | | ! --------------------------- | | ! lmin (=1 pour le moment) | | ! ----- F_lmin=0 ------------ / / ! ! --------------------------- ! ////////////////////////// ! !============================================================================= ! Mars version: no phase change is considered, we use a "dry" definition ! for the potential temperature. !============================================================================= !------------------------------------------------------------------ ! 1. alim_star is the source layer vertical profile in the lowest layers ! of the thermal plume. Computed from the air buoyancy ! 2. lmin and lalim are the indices of begining and end of source profile !------------------------------------------------------------------ ! entr_star(:,:)=0. ; detr_star(:,:)=0. alim_star(:,:)=0. ; alim_star_tot(:)=0. lmin(:)=1 !----------------------------------------------------------------------------- ! 3. wmax and zmax are maximum vertical velocity and altitude of a ! conservative plume (entrainment = detrainment = 0) using only ! the source layer. This is a CAPE computation used for determining ! the closure mass flux. !----------------------------------------------------------------------------- ! =========================================================================== ! ===================== PLUME =============================================== ! =========================================================================== ! Initialization ztva(:,:)=ztv(:,:) ! temperature in the updraft = temperature of the env. ztva_est(:,:)=ztva(:,:) ! estimated temp. in the updraft ztla(:,:)=0. !intermediary variable zdz=0. !layer thickness zbuoy(:,:)=0. !buoyancy w_est(:,:)=0. !estimated vertical velocity f_star(:,:)=0. !non-dimensional upward mass flux f* wa_moy(:,:)=0. !vertical velocity ! Some more initializations wmaxa(:)=0. lalim(:)=1 !------------------------------------------------------------------------- ! We consider as an activecell columns where the two first layers are ! convectively unstable ! When it is the case, we compute the source layer profile (alim_star) ! see paper appendix 4.1 for details on the source layer !------------------------------------------------------------------------- activecell(:)=ztv(:,1)>ztv(:,2) do ig=1,ngrid if (ztv(ig,1)>=(ztv(ig,2))) then alim_star(ig,1)=MAX((ztv(ig,1)-ztv(ig,2)),0.) & & *sqrt(zlev(ig,2)) lalim(ig)=2 alim_star_tot(ig)=alim_star_tot(ig)+alim_star(ig,1) endif enddo do l=2,nlayer-1 do ig=1,ngrid if (ztv(ig,l)>(ztv(ig,l+1)) .and. ztv(ig,1)>=ztv(ig,l) & & .and. (alim_star(ig,l-1).ne. 0.)) then alim_star(ig,l)=MAX((ztv(ig,l)-ztv(ig,l+1)),0.) & & *sqrt(zlev(ig,l+1)) lalim(ig)=l+1 alim_star_tot(ig)=alim_star_tot(ig)+alim_star(ig,l) endif enddo enddo do l=1,nlayer do ig=1,ngrid if (alim_star_tot(ig) > 1.e-10 ) then alim_star(ig,l)=alim_star(ig,l)/alim_star_tot(ig) endif enddo enddo alim_star_tot(:)=1. ! We compute the initial squared velocity (zw2) and non-dimensional upward mass flux ! (f_star) in the first and second layer from the source profile. do ig=1,ngrid if (activecell(ig)) then ztla(ig,1)=ztv(ig,1) f_star(ig,1)=0. f_star(ig,2)=alim_star(ig,1) zw2(ig,2)=2.*g*(ztv(ig,1)-ztv(ig,2))/ztv(ig,2) & & *(zlev(ig,2)-zlev(ig,1)) & & *0.4*pphi(ig,1)/(pphi(ig,2)-pphi(ig,1)) !0.4=von Karman constant w_est(ig,2)=zw2(ig,2) endif enddo !============================================================================== !============================================================================== !============================================================================== ! LOOP ON VERTICAL LEVELS !============================================================================== do l=2,nlayer-1 !============================================================================== !============================================================================== !============================================================================== ! is the thermal plume still active ? do ig=1,ngrid activecell(ig)=activecell(ig) & & .and. zw2(ig,l)>1.e-10 & & .and. f_star(ig,l)+alim_star(ig,l)>1.e-10 enddo !--------------------------------------------------------------------------- ! ! .I. INITIALIZATION ! ! Computations of the temperature and buoyancy properties in layer l, ! without accounting for entrainment and detrainment. We are therefore ! assuming constant temperature in the updraft ! ! This computation yields an estimation of the buoyancy (zbuoy) and thereforce ! an estimation of the velocity squared (w_est) !--------------------------------------------------------------------------- do ig=1,ngrid if(activecell(ig)) then ztva_est(ig,l)=ztla(ig,l-1) zdz=zlev(ig,l+1)-zlev(ig,l) zbuoy(ig,l)=g*(ztva_est(ig,l)-ztv(ig,l))/ztv(ig,l) ! Estimated vertical velocity squared ! (discretized version of equation 12 in paragraph 40 of paper) if (((a1*zbuoy(ig,l)/w_est(ig,l)-b1) .gt. 0.) .and. (w_est(ig,l) .ne. 0.)) then w_est(ig,l+1)=Max(0.0001,w_est(ig,l)+2.*zdz*a1*zbuoy(ig,l)-2.*zdz*w_est(ig,l)*b1 & & -2.*(1.-omega)*zdz*w_est(ig,l)*ae*(a1*zbuoy(ig,l)/w_est(ig,l)-b1)**be) else w_est(ig,l+1)=Max(0.0001,w_est(ig,l)+2.*zdz*a1inv*zbuoy(ig,l)-2.*zdz*w_est(ig,l)*b1inv) endif if (w_est(ig,l+1).lt.0.) then w_est(ig,l+1)=zw2(ig,l) endif endif ! of if(activecell(ig)) enddo ! of do ig=1,ngrid !------------------------------------------------- ! Compute corresponding non-dimensional (ND) entrainment and detrainment rates !------------------------------------------------- do ig=1,ngrid if (activecell(ig)) then zw2m=w_est(ig,l+1) zdz=zlev(ig,l+1)-zlev(ig,l) if((a1*(zbuoy(ig,l)/zw2m)-b1).gt.0.) then ! ND entrainment rate, see equation 16 of paper (paragraph 43) entr_star(ig,l)=f_star(ig,l)*zdz* & & MAX(0.,ae*(a1*(zbuoy(ig,l)/zw2m)-b1)**be) else entr_star(ig,l)=0. endif if(zbuoy(ig,l) .gt. 0.) then if(l .lt. lalim(ig)) then detr_star(ig,l)=0. else ! ND detrainment rate, see paragraph 44 of paper detr_star(ig,l) = f_star(ig,l)*zdz*ad endif else detr_star(ig,l)=f_star(ig,l)*zdz* & & MAX(ad,bd*zbuoy(ig,l)/zw2m) endif ! If we are still in the source layer, we define the source layer entr. rate (alim_star) as the ! maximum between the source entrainment rate and the estimated entrainment rate. if (l.lt.lalim(ig)) then alim_star(ig,l)=max(alim_star(ig,l),entr_star(ig,l)) entr_star(ig,l)=0. endif ! Compute the non-dimensional upward mass flux at layer l+1 ! using equation 11 of appendix 4.2 in paper f_star(ig,l+1)=f_star(ig,l)+alim_star(ig,l)+entr_star(ig,l) & & -detr_star(ig,l) endif ! of if (activecell(ig)) enddo ! of do ig=1,ngrid ! ----------------------------------------------------------------------------------- ! ! .II. CONVERGENCE LOOP ! ! We have estimated a vertical velocity profile and refined the source layer profile ! We now conduct iterations to compute: ! ! - the temperature inside the updraft from the estimated entrainment/source, detrainment, ! and upward mass flux. ! - the buoyancy from the new temperature inside the updraft ! - the vertical velocity from the new buoyancy ! - the entr., detr. and upward mass flux from the new buoyancy and vertical velocity ! ! This loop (tic) converges quickly. We have hardcoded 6 iterations from empirical observations. ! Convergence occurs in 1 or 2 iterations in most cases. ! ----------------------------------------------------------------------------------- ! ----------------------------------------------------------------------------------- ! ----------------------------------------------------------------------------------- DO tic=0,5 ! internal convergence loop ! ----------------------------------------------------------------------------------- ! ----------------------------------------------------------------------------------- ! Is the cell still active ? activetmp(:)=activecell(:) .and. f_star(:,l+1)>1.e-10 ! If the cell is active, compute temperature inside updraft do ig=1,ngrid if (activetmp(ig)) then ztla(ig,l)=(f_star(ig,l)*ztla(ig,l-1)+ & & (alim_star(ig,l)+entr_star(ig,l))*ztv(ig,l)) & & /(f_star(ig,l+1)+detr_star(ig,l)) endif enddo ! Is the cell still active with respect to temperature variations ? activetmp(:)=activetmp(:).and.(abs(ztla(:,l)-ztva(:,l)).gt.0.01) ! Compute new buoyancy and vertical velocity do ig=1,ngrid zdz=zlev(ig,l+1)-zlev(ig,l) if (activetmp(ig)) then ztva(ig,l) = ztla(ig,l) zbuoy(ig,l)=g*(ztva(ig,l)-ztv(ig,l))/ztv(ig,l) ! (discretized version of equation 12 in paragraph 40 of paper) if (((a1*zbuoy(ig,l)/zw2(ig,l)-b1) .gt. 0.) .and. & (zw2(ig,l) .ne. 0.) ) then zw2(ig,l+1)=Max(0.,zw2(ig,l)+2.*zdz*a1*zbuoy(ig,l)- & 2.*zdz*zw2(ig,l)*b1-2.*(1.-omega)*zdz*zw2(ig,l)* & ae*(a1*zbuoy(ig,l)/zw2(ig,l)-b1)**be) else zw2(ig,l+1)=Max(0.,zw2(ig,l)+2.*zdz*a1inv*zbuoy(ig,l) & -2.*zdz*zw2(ig,l)*b1inv) endif endif enddo ! ================ RECOMPUTE ENTR, DETR, and F FROM NEW W2 =================== ! ND entrainment rate, see equation 16 of paper (paragraph 43) ! ND detrainment rate, see paragraph 44 of paper do ig=1,ngrid if (activetmp(ig)) then zw2m=zw2(ig,l+1) zdz=zlev(ig,l+1)-zlev(ig,l) if(zw2m .gt. 0) then if((a1*(zbuoy(ig,l)/zw2m)-b1) .gt. 0.) then entr_star(ig,l)=f_star(ig,l)*zdz* & & MAX(0.,ae*(a1*(zbuoy(ig,l)/zw2m)-b1)**be) else entr_star(ig,l)=0. endif if(zbuoy(ig,l) .gt. 0.) then if(l .lt. lalim(ig)) then detr_star(ig,l)=0. else detr_star(ig,l) = f_star(ig,l)*zdz*ad endif else detr_star(ig,l)=f_star(ig,l)*zdz* & & MAX(ad,bd*zbuoy(ig,l)/zw2m) endif else entr_star(ig,l)=0. detr_star(ig,l)=0. endif ! of if(zw2m .gt. 0) ! If we are still in the source layer, we define the source layer entr. rate (alim_star) as the ! maximum between the source entrainment rate and the estimated entrainment rate. if (l.lt.lalim(ig)) then alim_star(ig,l)=max(alim_star(ig,l),entr_star(ig,l)) entr_star(ig,l)=0. endif ! Compute the non-dimensional upward mass flux at layer l+1 ! using equation 11 of appendix 4.2 in paper f_star(ig,l+1)=f_star(ig,l)+alim_star(ig,l)+entr_star(ig,l) & & -detr_star(ig,l) endif ! of if (activetmp(ig)) enddo ! of do ig=1,ngrid ! ----------------------------------------------------------------------------------- ! ----------------------------------------------------------------------------------- ENDDO ! of internal convergence loop DO tic=0,5 ! ----------------------------------------------------------------------------------- ! ----------------------------------------------------------------------------------- !--------------------------------------------------------------------------- ! Miscellaneous computations for height !--------------------------------------------------------------------------- do ig=1,ngrid if (zw2(ig,l+1)>0. .and. zw2(ig,l+1).lt.1.e-10) then IF (thermverbose) THEN print*,'thermcell_plume, particular case in velocity profile' ENDIF zw2(ig,l+1)=0. endif if (zw2(ig,l+1).lt.0.) then zw2(ig,l+1)=0. endif wa_moy(ig,l+1)=sqrt(zw2(ig,l+1)) if (wa_moy(ig,l+1).gt.wmaxa(ig)) then wmaxa(ig)=wa_moy(ig,l+1) endif enddo !========================================================================= !========================================================================= !========================================================================= ! END OF THE LOOP ON VERTICAL LEVELS enddo ! of do l=2,nlayer-1 !========================================================================= !========================================================================= !========================================================================= ! Recompute the source layer total entrainment alim_star_tot ! as alim_star may have been modified in the above loop. Renormalization of ! alim_star. do ig=1,ngrid alim_star_tot(ig)=0. enddo do ig=1,ngrid do l=1,lalim(ig)-1 alim_star_tot(ig)=alim_star_tot(ig)+alim_star(ig,l) enddo enddo do l=1,nlayer do ig=1,ngrid if (alim_star_tot(ig) > 1.e-10 ) then alim_star(ig,l)=alim_star(ig,l)/alim_star_tot(ig) endif enddo enddo ! =========================================================================== ! ================= FIN PLUME =============================================== ! =========================================================================== ! =========================================================================== ! ================= HEIGHT ================================================== ! =========================================================================== ! WARNING, W2 (squared velocity) IS TRANSFORMED IN ITS SQUARE ROOT HERE !------------------------------------------------------------------------------- ! Computations of the thermal height zmax and maximum vertical velocity wmax !------------------------------------------------------------------------------- ! Index of the thermal plume height do ig=1,ngrid lmax(ig)=lalim(ig) enddo do ig=1,ngrid do l=nlayer,lalim(ig)+1,-1 if (zw2(ig,l).le.1.e-10) then lmax(ig)=l-1 endif enddo enddo ! Particular case when the thermal reached the model top, which is not a good sign do ig=1,ngrid if ( zw2(ig,nlayer) > 1.e-10 ) then print*,'thermcell_main_mars: WARNING !!!!! W2 non-zero in last layer for ig=',ig lmax(ig)=nlayer endif enddo ! Maximum vertical velocity zw2 do ig=1,ngrid wmax(ig)=0. enddo do l=1,nlayer do ig=1,ngrid if (l.le.lmax(ig)) then if (zw2(ig,l).lt.0.)then ! print*,'pb2 zw2<0',zw2(ig,l) zw2(ig,l)=0. endif zw2(ig,l)=sqrt(zw2(ig,l)) wmax(ig)=max(wmax(ig),zw2(ig,l)) else zw2(ig,l)=0. endif enddo enddo ! Height of the thermal plume, defined as the following: ! zmax=Integral[z*w(z)*dz]/Integral[w(z)*dz] ! do ig=1,ngrid zmax(ig)=0. zlevinter(ig)=zlev(ig,1) enddo num(:)=0. denom(:)=0. do ig=1,ngrid do l=1,nlayer num(ig)=num(ig)+zw2(ig,l)*zlev(ig,l)*(zlev(ig,l+1)-zlev(ig,l)) denom(ig)=denom(ig)+zw2(ig,l)*(zlev(ig,l+1)-zlev(ig,l)) enddo enddo do ig=1,ngrid if (denom(ig).gt.1.e-10) then zmax(ig)=2.*num(ig)/denom(ig) endif enddo ! =========================================================================== ! ================= FIN HEIGHT ============================================== ! =========================================================================== #ifdef MESOSCALE limz= nlayer-5 ! the most important is limz > max(PBLheight)+2 ! nlayer-5 is more than enough! #else call planetwide_maxval(lmax,limz) limz=limz+2 #endif if (limz .ge. nlayer) then print*,'thermals have reached last layer of the model' print*,'this is not good !' limz=nlayer endif ! alim_star_clos is the source profile used for closure. It consists of the ! modified source profile in the source layers, and the entrainment profile ! above it. alim_star_clos(:,:)=entr_star(:,:)+alim_star(:,:) ! =========================================================================== ! ============= CLOSURE ===================================================== ! =========================================================================== !------------------------------------------------------------------------------- ! Closure, determination of the upward mass flux !------------------------------------------------------------------------------- ! Init. alim_star2(:)=0. alim_star_tot_clos(:)=0. f(:)=0. ! llmax is the index of the heighest thermal in the simulation domain #ifdef MESOSCALE !! AS: THIS IS PARALLEL SENSITIVE!!!!! to be corrected? llmax=1 do ig=1,ngrid if (lalim(ig)>llmax) llmax=lalim(ig) enddo #else call planetwide_maxval(lalim,llmax) #endif ! Integral of a**2/(rho* Delta z), see equation 13 of appendix 4.2 in paper do k=1,llmax-1 do ig=1,ngrid if (k1.e-10) then f(ig)=wmax(ig)*alim_star_tot_clos(ig)/ & & (max(500.,zmax(ig))*r_aspect_thermals*alim_star2(ig)) endif enddo ! =========================================================================== ! ============= FIN CLOSURE ================================================= ! =========================================================================== ! =========================================================================== ! ============= FLUX2 ======================================================= ! =========================================================================== !------------------------------------------------------------------------------- ! With the closure mass flux, we can compute the entrainment, detrainment and ! upward mass flux from the non-dimensional ones. !------------------------------------------------------------------------------- fomass_max=0.8 !maximum mass fraction of a cell that can go upward in an ! updraft alphamax=0.5 !maximum updraft coverage in a cell ! these variables allow to follow corrections made to the mass flux when thermverbose=.true. ncorecfm1=0 ncorecfm2=0 ncorecfm3=0 ncorecfm4=0 ncorecfm5=0 ncorecfm6=0 ncorecfm7=0 ncorecfm8=0 ncorecalpha=0 !------------------------------------------------------------------------- ! Multiply by the closure mass flux !------------------------------------------------------------------------- do l=1,limz entr(:,l)=f(:)*(entr_star(:,l)+alim_star(:,l)) detr(:,l)=f(:)*detr_star(:,l) enddo ! Reconstruct the updraft mass flux everywhere do l=1,limz do ig=1,ngrid if (l.lt.lmax(ig)) then fm(ig,l+1)=fm(ig,l)+entr(ig,l)-detr(ig,l) elseif(l.eq.lmax(ig)) then fm(ig,l+1)=0. detr(ig,l)=fm(ig,l)+entr(ig,l) else fm(ig,l+1)=0. endif enddo enddo !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! ! ! Now we will reconstruct once again the upward ! mass flux, but we will apply corrections ! in some cases. We can compare to the ! previously computed mass flux (above) ! ! This verification is done level by level ! !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! do l=1,limz !loop on the levels !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! ! Upward mass flux at level l+1 do ig=1,ngrid if (l.lt.lmax(ig)) then fm(ig,l+1)=fm(ig,l)+entr(ig,l)-detr(ig,l) elseif(l.eq.lmax(ig)) then fm(ig,l+1)=0. detr(ig,l)=fm(ig,l)+entr(ig,l) else fm(ig,l+1)=0. endif enddo !------------------------------------------------------------------------- ! Upward mass flux should be positive !------------------------------------------------------------------------- do ig=1,ngrid if (fm(ig,l+1).lt.0.) then if((l+1) .eq. lmax(ig)) then detr(ig,l)=detr(ig,l)+fm(ig,l+1) fm(ig,l+1)=0. entr(ig,l+1)=0. ncorecfm2=ncorecfm2+1 else IF (thermverbose) THEN print*,'fm(l+1)<0 : ig, l+1,lmax :',ig,l+1,lmax(ig),fm(ig,l+1) ENDIF ncorecfm1=ncorecfm1+1 fm(ig,l+1)=fm(ig,l) detr(ig,l)=entr(ig,l) endif endif enddo !------------------------------------------------------------------------- ! Detrainment should be lower than upward mass flux !------------------------------------------------------------------------- do ig=1,ngrid if (detr(ig,l).gt.fm(ig,l)) then ncorecfm6=ncorecfm6+1 detr(ig,l)=fm(ig,l) entr(ig,l)=fm(ig,l+1) ! When detrainment is stronger than upward mass flux, and we are above the ! thermal last level, the plume is stopped if(l.gt.lmax(ig)) then detr(ig,l)=0. fm(ig,l+1)=0. entr(ig,l)=0. endif endif enddo !------------------------------------------------------------------------- ! Check again for mass flux positivity !------------------------------------------------------------------------- do ig=1,ngrid if (fm(ig,l+1).lt.0.) then detr(ig,l)=detr(ig,l)+fm(ig,l+1) fm(ig,l+1)=0. ncorecfm2=ncorecfm2+1 endif enddo !----------------------------------------------------------------------- ! Fractional coverage should be less than 1 !----------------------------------------------------------------------- do ig=1,ngrid if (zw2(ig,l+1).gt.1.e-10) then zfm=rhobarz(ig,l+1)*zw2(ig,l+1)*alphamax if ( fm(ig,l+1) .gt. zfm) then f_old=fm(ig,l+1) fm(ig,l+1)=zfm detr(ig,l)=detr(ig,l)+f_old-fm(ig,l+1) ncorecalpha=ncorecalpha+1 endif endif enddo enddo ! on vertical levels !----------------------------------------------------------------------- ! ! We limit the total mass going from one level to the next, compared to the ! initial total mass fo the cell ! !----------------------------------------------------------------------- do l=1,limz do ig=1,ngrid eee0=entr(ig,l) ddd0=detr(ig,l) eee=entr(ig,l)-masse(ig,l)*fomass_max/ptimestep ddd=detr(ig,l)-eee if (eee.gt.0.) then ncorecfm3=ncorecfm3+1 entr(ig,l)=entr(ig,l)-eee if ( ddd.gt.0.) then ! The entrainment is too strong but we can compensate the excess by a detrainment decrease detr(ig,l)=ddd else ! The entrainment is too strong and we compensate the excess by a stronger entrainment ! in the layer above if(l.eq.lmax(ig)) then detr(ig,l)=fm(ig,l)+entr(ig,l) else entr(ig,l+1)=entr(ig,l+1)-ddd detr(ig,l)=0. fm(ig,l+1)=fm(ig,l)+entr(ig,l) detr(ig,l)=0. endif endif endif enddo enddo ! Check again that everything cancels at zmax do ig=1,ngrid fm(ig,lmax(ig)+1)=0. entr(ig,lmax(ig))=0. detr(ig,lmax(ig))=fm(ig,lmax(ig))+entr(ig,lmax(ig)) enddo !----------------------------------------------------------------------- ! Summary of the number of modifications that were necessary (if thermverbose=.true. ! and only if there were a lot of them) !----------------------------------------------------------------------- !IM 090508 beg IF (thermverbose) THEN if (ncorecfm1+ncorecfm2+ncorecfm3+ncorecfm4+ncorecfm5+ncorecalpha > ngrid/4. ) then print*,'thermcell warning : large number of corrections' print*,'PB thermcell : on a du coriger ',ncorecfm1,'x fm1',& & ncorecfm2,'x fm2',ncorecfm3,'x fm3 et', & & ncorecfm4,'x fm4',ncorecfm5,'x fm5 et', & & ncorecfm6,'x fm6', & & ncorecfm7,'x fm7', & & ncorecfm8,'x fm8', & & ncorecalpha,'x alpha' endif ENDIF ! =========================================================================== ! ============= FIN FLUX2 =================================================== ! =========================================================================== ! =========================================================================== ! ============= TRANSPORT =================================================== ! =========================================================================== !------------------------------------------------------------------ ! vertical transport computation !------------------------------------------------------------------ ! ------------------------------------------------------------------ ! IN THE UPDRAFT ! ------------------------------------------------------------------ zdthladj(:,:)=0. ! Based on equation 14 in appendix 4.2 do ig=1,ngrid if(lmax(ig) .gt. 1) then do k=1,lmax(ig) zdthladj(ig,k)=(1./masse(ig,k))*(fm(ig,k+1)*ztv(ig,k+1)- & & fm(ig,k)*ztv(ig,k)+fm(ig,k)*ztva(ig,k)-fm(ig,k+1)*ztva(ig,k+1)) if (ztv(ig,k) + ptimestep*zdthladj(ig,k) .le. 0.) then IF (thermverbose) THEN print*,'Teta<0 in thermcell_dTeta up: qenv .. dq : ', ztv(ig,k),ptimestep*zdthladj(ig,k) ENDIF if(ztv(ig,k) .gt. 0.) then zdthladj(ig,k)=0. endif endif enddo endif enddo ! ------------------------------------------------------------------ ! DOWNDRAFT PARAMETERIZATION ! ------------------------------------------------------------------ ztvd(:,:)=ztv(:,:) fm_down(:,:)=0. do ig=1,ngrid if (lmax(ig) .gt. 1) then do l=1,lmax(ig) if(zlay(ig,l) .le. zmax(ig)) then ! see equation 18 of paragraph 48 in paper fm_down(ig,l) =fm(ig,l)* & & max(fdfu,-4*max(0.,(zlay(ig,l)/zmax(ig)))-0.6) endif if(zlay(ig,l) .le. zmax(ig)) then ! see equation 19 of paragraph 49 in paper ztvd(ig,l)=min(ztv(ig,l),ztv(ig,l)*((zlay(ig,l)/zmax(ig))/400. + 0.997832)) else ztvd(ig,l)=ztv(ig,l) endif enddo endif enddo ! ------------------------------------------------------------------ ! TRANSPORT IN DOWNDRAFT ! ------------------------------------------------------------------ zdthladj_down(:,:)=0. do ig=1,ngrid if(lmax(ig) .gt. 1) then ! No downdraft in the very-near surface layer, we begin at k=3 ! Based on equation 14 in appendix 4.2 do k=3,lmax(ig) zdthladj_down(ig,k)=(1./masse(ig,k))*(fm_down(ig,k+1)*ztv(ig,k+1)- & & fm_down(ig,k)*ztv(ig,k)+fm_down(ig,k)*ztvd(ig,k)-fm_down(ig,k+1)*ztvd(ig,k+1)) if (ztv(ig,k) + ptimestep*zdthladj_down(ig,k) .le. 0.) then IF (thermverbose) THEN print*,'q<0 in thermcell_dTeta down: qenv .. dq : ', ztv(ig,k),ptimestep*zdthladj_down(ig,k) ENDIF if(ztv(ig,k) .gt. 0.) then zdthladj(ig,k)=0. endif endif enddo endif enddo !------------------------------------------------------------------ ! Final fraction coverage with the clean upward mass flux, computed at interfaces !------------------------------------------------------------------ fraca(:,:)=0. do l=2,limz do ig=1,ngrid if (zw2(ig,l).gt.1.e-10) then fraca(ig,l)=fm(ig,l)/(rhobarz(ig,l)*zw2(ig,l)) else fraca(ig,l)=0. endif enddo enddo !------------------------------------------------------------------ ! Transport of C02 Tracer !------------------------------------------------------------------ ! We only transport co2 tracer because it is coupled to the scheme through theta_m ! The rest is transported outside the sub-timestep loop ratiom(:,:)=1. if (igcm_co2.ne.0) then detrmod(:,:)=0. do k=1,limz do ig=1,ngrid detrmod(ig,k)=fm(ig,k)-fm(ig,k+1) & & +entr(ig,k) if (detrmod(ig,k).lt.0.) then entr(ig,k)=entr(ig,k)-detrmod(ig,k) detrmod(ig,k)=0. endif enddo enddo call thermcell_dqup(ngrid,nlayer,ptimestep & & ,fm,entr,detrmod, & & masse,pq(:,:,igcm_co2),pdqadj(:,:,igcm_co2),ndt,limz) ! Compute the ratio between theta and theta_m do l=1,limz do ig=1,ngrid ratiom(ig,l)=1./(A*(pq(ig,l,igcm_co2)+pdqadj(ig,l,igcm_co2)*ptimestep)+B) enddo enddo endif !------------------------------------------------------------------ ! incrementation dt !------------------------------------------------------------------ pdtadj(:,:)=0. do l=1,limz do ig=1,ngrid pdtadj(ig,l)=(zdthladj(ig,l)+zdthladj_down(ig,l))*zpopsk(ig,l)*ratiom(ig,l) enddo enddo ! =========================================================================== ! ============= FIN TRANSPORT =============================================== ! =========================================================================== !------------------------------------------------------------------ ! Diagnostics for outputs !------------------------------------------------------------------ ! We compute interface values for teta env and th. The last interface ! value does not matter, as the mass flux is 0 there. do l=1,nlayer-1 do ig=1,ngrid teta_th_int(ig,l)=0.5*(ztva(ig,l+1)+ztva(ig,l))*ratiom(ig,l) teta_down_int(ig,l) = 0.5*(ztvd(ig,l+1)+ztvd(ig,l))*ratiom(ig,l) teta_env_int(ig,l)=0.5*(ztv(ig,l+1)+ztv(ig,l))*ratiom(ig,l) enddo enddo do ig=1,ngrid teta_th_int(ig,nlayer)=teta_th_int(ig,nlayer-1) teta_env_int(ig,nlayer)=teta_env_int(ig,nlayer-1) teta_down_int(ig,nlayer)=teta_down_int(ig,nlayer-1) enddo heatFlux(:,:)=0. buoyancyOut(:,:)=0. buoyancyEst(:,:)=0. heatFlux_down(:,:)=0. do l=1,limz do ig=1,ngrid heatFlux(ig,l)=fm(ig,l)*(teta_th_int(ig,l)-teta_env_int(ig,l))/(rhobarz(ig,l)) buoyancyOut(ig,l)=g*(ztva(ig,l)-ztv(ig,l))/ztv(ig,l) buoyancyEst(ig,l)=g*(ztva_est(ig,l)-ztv(ig,l))/ztv(ig,l) heatFlux_down(ig,l)=fm_down(ig,l)*(teta_down_int(ig,l)-teta_env_int(ig,l))/rhobarz(ig,l) enddo enddo return end