! $Id: newmicro.F90 3127 2017-12-14 13:27:37Z aborella $ SUBROUTINE newmicro(ok_cdnc, bl95_b0, bl95_b1, paprs, pplay, t, pqlwp, pclc, & pcltau, pclemi, pch, pcl, pcm, pct, pctlwp, xflwp, xfiwp, xflwc, xfiwc, & mass_solu_aero, mass_solu_aero_pi, pcldtaupi, re, fl, reliq, reice, & reliq_pi, reice_pi) USE dimphy USE phys_local_var_mod, ONLY: scdnc, cldncl, reffclwtop, lcc, reffclws, & reffclwc, cldnvi, lcc3d, lcc3dcon, lcc3dstra, icc3dcon, icc3dstra, zfice USE phys_state_var_mod, ONLY: rnebcon, clwcon USE icefrac_lsc_mod ! computes ice fraction (JBM 3/14) IMPLICIT NONE ! ====================================================================== ! Auteur(s): Z.X. Li (LMD/CNRS) date: 19930910 ! O. Boucher (LMD/CNRS) mise a jour en 201212 ! I. Musat (LMD/CNRS) : prise en compte de la meme hypothese de recouvrement ! pour les nuages que pour le rayonnement rrtm via ! le parametre novlp de radopt.h : 20160721 ! Objet: Calculer epaisseur optique et emmissivite des nuages ! ====================================================================== ! Arguments: ! ok_cdnc-input-L-flag pour calculer les rayons a partir des aerosols ! t-------input-R-temperature ! pqlwp---input-R-eau liquide nuageuse dans l'atmosphere dans la partie ! nuageuse (kg/kg) ! pclc----input-R-couverture nuageuse pour le rayonnement (0 a 1) ! mass_solu_aero-----input-R-total mass concentration for all soluble ! aerosols[ug/m^3] ! mass_solu_aero_pi--input-R-ditto, pre-industrial value ! bl95_b0-input-R-a PARAMETER, may be varied for tests (s-sea, l-land) ! bl95_b1-input-R-a PARAMETER, may be varied for tests ( -"- ) ! re------output-R-Cloud droplet effective radius multiplied by fl [um] ! fl------output-R-Denominator to re, introduced to avoid problems in ! the averaging of the output. fl is the fraction of liquid ! water clouds within a grid cell ! pcltau--output-R-epaisseur optique des nuages ! pclemi--output-R-emissivite des nuages (0 a 1) ! pcldtaupi-output-R-pre-industrial value of cloud optical thickness, ! pcl-output-R-2D low-level cloud cover ! pcm-output-R-2D mid-level cloud cover ! pch-output-R-2D high-level cloud cover ! pct-output-R-2D total cloud cover ! ====================================================================== include "YOMCST.h" include "nuage.h" include "radepsi.h" include "radopt.h" ! choix de l'hypothese de recouvrement nuageuse via radopt.h (IM, 19.07.2016) ! !novlp=1: max-random ! !novlp=2: maximum ! !novlp=3: random ! LOGICAL random, maximum_random, maximum ! PARAMETER (random=.FALSE., maximum_random=.TRUE., maximum=.FALSE.) LOGICAL, SAVE :: first = .TRUE. !$OMP THREADPRIVATE(FIRST) INTEGER flag_max ! threshold PARAMETERs REAL thres_tau, thres_neb PARAMETER (thres_tau=0.3, thres_neb=0.001) REAL phase3d(klon, klev) REAL tcc(klon), ftmp(klon), lcc_integrat(klon), height(klon) REAL paprs(klon, klev+1) REAL pplay(klon, klev) REAL t(klon, klev) REAL pclc(klon, klev) REAL pqlwp(klon, klev) REAL pcltau(klon, klev) REAL pclemi(klon, klev) REAL pcldtaupi(klon, klev) REAL pct(klon) REAL pcl(klon) REAL pcm(klon) REAL pch(klon) REAL pctlwp(klon) LOGICAL lo ! !Abderr modif JL mail du 19.01.2011 18:31 ! REAL cetahb, cetamb ! PARAMETER (cetahb = 0.45, cetamb = 0.80) ! Remplacer ! cetahb*paprs(i,1) par prmhc ! cetamb*paprs(i,1) par prlmc REAL prmhc ! Pressure between medium and high level cloud in Pa REAL prlmc ! Pressure between low and medium level cloud in Pa PARAMETER (prmhc=440.*100., prlmc=680.*100.) INTEGER i, k REAL xflwp(klon), xfiwp(klon) REAL xflwc(klon, klev), xfiwc(klon, klev) REAL radius REAL coef_froi, coef_chau PARAMETER (coef_chau=0.13, coef_froi=0.09) REAL seuil_neb PARAMETER (seuil_neb=0.001) ! JBM (3/14) nexpo is replaced by exposant_glace ! INTEGER nexpo ! exponentiel pour glace/eau ! PARAMETER (nexpo=6) ! PARAMETER (nexpo=1) ! if iflag_t_glace=0, the old values are used: REAL, PARAMETER :: t_glace_min_old = 258. REAL, PARAMETER :: t_glace_max_old = 273.13 REAL rel, tc, rei REAL k_ice0, k_ice, df PARAMETER (k_ice0=0.005) ! units=m2/g PARAMETER (df=1.66) ! diffusivity factor ! jq for the aerosol indirect effect ! jq introduced by Johannes Quaas (quaas@lmd.jussieu.fr), 27/11/2003 ! jq REAL mass_solu_aero(klon, klev) ! total mass concentration for all soluble aerosols [ug m-3] REAL mass_solu_aero_pi(klon, klev) ! - " - (pre-industrial value) REAL cdnc(klon, klev) ! cloud droplet number concentration [m-3] REAL re(klon, klev) ! cloud droplet effective radius [um] REAL cdnc_pi(klon, klev) ! cloud droplet number concentration [m-3] (pi value) REAL re_pi(klon, klev) ! cloud droplet effective radius [um] (pi value) REAL fl(klon, klev) ! xliq * rneb (denominator to re; fraction of liquid water clouds ! within the grid cell) LOGICAL ok_cdnc REAL bl95_b0, bl95_b1 ! Parameter in B&L 95-Formula ! jq-end ! IM cf. CR:parametres supplementaires REAL zclear(klon) REAL zcloud(klon) REAL zcloudh(klon) REAL zcloudm(klon) REAL zcloudl(klon) REAL rhodz(klon, klev) !--rho*dz pour la couche REAL zrho(klon, klev) !--rho pour la couche REAL dh(klon, klev) !--dz pour la couche REAL rad_chaud(klon, klev) !--rayon pour les nuages chauds REAL rad_chaud_pi(klon, klev) !--rayon pour les nuages chauds pre-industriels REAL zflwp_var, zfiwp_var REAL d_rei_dt ! Abderrahmane oct 2009 REAL reliq(klon, klev), reice(klon, klev) REAL reliq_pi(klon, klev), reice_pi(klon, klev) ! !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! ! FH : 2011/05/24 ! rei = ( rei_max - rei_min ) * T(°C) / 81.4 + rei_max ! to be used for a temperature in celcius T(°C) < 0 ! rei=rei_min for T(°C) < -81.4 ! Calcul de la pente de la relation entre rayon effective des cristaux ! et la température. ! Pour retrouver les résultats numériques de la version d'origine, ! on impose 0.71 quand on est proche de 0.71 d_rei_dt = (rei_max-rei_min)/81.4 IF (abs(d_rei_dt-0.71)<1.E-4) d_rei_dt = 0.71 ! !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! ! Calculer l'epaisseur optique et l'emmissivite des nuages ! IM inversion des DO xflwp = 0.D0 xfiwp = 0.D0 xflwc = 0.D0 xfiwc = 0.D0 reliq = 0. reice = 0. reliq_pi = 0. reice_pi = 0. IF (iflag_t_glace.EQ.0) THEN DO k = 1, klev DO i = 1, klon ! -layer calculation rhodz(i, k) = (paprs(i,k)-paprs(i,k+1))/rg ! kg/m2 zrho(i, k) = pplay(i, k)/t(i, k)/rd ! kg/m3 dh(i, k) = rhodz(i, k)/zrho(i, k) ! m ! -Fraction of ice in cloud using a linear transition zfice(i, k) = 1.0 - (t(i,k)-t_glace_min_old)/(t_glace_max_old-t_glace_min_old) zfice(i, k) = min(max(zfice(i,k),0.0), 1.0) ! -IM Total Liquid/Ice water content xflwc(i, k) = (1.-zfice(i,k))*pqlwp(i, k) xfiwc(i, k) = zfice(i, k)*pqlwp(i, k) END DO END DO ELSE ! of IF (iflag_t_glace.EQ.0) DO k = 1, klev CALL icefrac_lsc(klon,t(:,k),pplay(:,k)/paprs(:,1),zfice(:,k)) ! JBM: icefrac_lsc is now contained icefrac_lsc_mod ! zfice(i, k) = icefrac_lsc(t(i,k), t_glace_min, & ! t_glace_max, exposant_glace) DO i = 1, klon ! -layer calculation rhodz(i, k) = (paprs(i,k)-paprs(i,k+1))/rg ! kg/m2 zrho(i, k) = pplay(i, k)/t(i, k)/rd ! kg/m3 dh(i, k) = rhodz(i, k)/zrho(i, k) ! m ! -IM Total Liquid/Ice water content xflwc(i, k) = (1.-zfice(i,k))*pqlwp(i, k) xfiwc(i, k) = zfice(i, k)*pqlwp(i, k) END DO END DO ENDIF IF (ok_cdnc) THEN ! --we compute cloud properties as a function of the aerosol load DO k = 1, klev DO i = 1, klon ! Formula "D" of Boucher and Lohmann, Tellus, 1995 ! Cloud droplet number concentration (CDNC) is restricted ! to be within [20, 1000 cm^3] ! --present-day case cdnc(i, k) = 10.**(bl95_b0+bl95_b1*log(max(mass_solu_aero(i,k), & 1.E-4))/log(10.))*1.E6 !-m-3 cdnc(i, k) = min(1000.E6, max(20.E6,cdnc(i,k))) ! --pre-industrial case cdnc_pi(i, k) = 10.**(bl95_b0+bl95_b1*log(max(mass_solu_aero_pi(i,k), & 1.E-4))/log(10.))*1.E6 !-m-3 cdnc_pi(i, k) = min(1000.E6, max(20.E6,cdnc_pi(i,k))) ! --present-day case rad_chaud(i, k) = 1.1*((pqlwp(i,k)*pplay(i, & k)/(rd*t(i,k)))/(4./3*rpi*1000.*cdnc(i,k)))**(1./3.) rad_chaud(i, k) = max(rad_chaud(i,k)*1.E6, 5.) ! --pre-industrial case rad_chaud_pi(i, k) = 1.1*((pqlwp(i,k)*pplay(i, & k)/(rd*t(i,k)))/(4./3.*rpi*1000.*cdnc_pi(i,k)))**(1./3.) rad_chaud_pi(i, k) = max(rad_chaud_pi(i,k)*1.E6, 5.) ! --pre-industrial case ! --liquid/ice cloud water paths: IF (pclc(i,k)<=seuil_neb) THEN pcldtaupi(i, k) = 0.0 ELSE zflwp_var = 1000.*(1.-zfice(i,k))*pqlwp(i, k)/pclc(i, k)* & rhodz(i, k) zfiwp_var = 1000.*zfice(i, k)*pqlwp(i, k)/pclc(i, k)*rhodz(i, k) tc = t(i, k) - 273.15 rei = d_rei_dt*tc + rei_max IF (tc<=-81.4) rei = rei_min ! -- cloud optical thickness : ! [for liquid clouds, traditional formula, ! for ice clouds, Ebert & Curry (1992)] IF (zfiwp_var==0. .OR. rei<=0.) rei = 1. pcldtaupi(i, k) = 3.0/2.0*zflwp_var/rad_chaud_pi(i, k) + & zfiwp_var*(3.448E-03+2.431/rei) END IF END DO END DO ELSE !--not ok_cdnc ! -prescribed cloud droplet radius DO k = 1, min(3, klev) DO i = 1, klon rad_chaud(i, k) = rad_chau2 rad_chaud_pi(i, k) = rad_chau2 END DO END DO DO k = min(3, klev) + 1, klev DO i = 1, klon rad_chaud(i, k) = rad_chau1 rad_chaud_pi(i, k) = rad_chau1 END DO END DO END IF !--ok_cdnc ! --computation of cloud optical depth and emissivity ! --in the general case DO k = 1, klev DO i = 1, klon IF (pclc(i,k)<=seuil_neb) THEN ! effective cloud droplet radius (microns) for liquid water clouds: ! For output diagnostics cloud droplet effective radius [um] ! we multiply here with f * xl (fraction of liquid water ! clouds in the grid cell) to avoid problems in the averaging of the ! output. ! In the output of IOIPSL, derive the REAL cloud droplet ! effective radius as re/fl fl(i, k) = seuil_neb*(1.-zfice(i,k)) re(i, k) = rad_chaud(i, k)*fl(i, k) rel = 0. rei = 0. pclc(i, k) = 0.0 pcltau(i, k) = 0.0 pclemi(i, k) = 0.0 ELSE ! -- liquid/ice cloud water paths: zflwp_var = 1000.*(1.-zfice(i,k))*pqlwp(i, k)/pclc(i, k)*rhodz(i, k) zfiwp_var = 1000.*zfice(i, k)*pqlwp(i, k)/pclc(i, k)*rhodz(i, k) ! effective cloud droplet radius (microns) for liquid water clouds: ! For output diagnostics cloud droplet effective radius [um] ! we multiply here with f * xl (fraction of liquid water ! clouds in the grid cell) to avoid problems in the averaging of the ! output. ! In the output of IOIPSL, derive the REAL cloud droplet ! effective radius as re/fl fl(i, k) = pclc(i, k)*(1.-zfice(i,k)) re(i, k) = rad_chaud(i, k)*fl(i, k) rel = rad_chaud(i, k) ! for ice clouds: as a function of the ambiant temperature ! [formula used by Iacobellis and Somerville (2000), with an ! asymptotical value of 3.5 microns at T<-81.4 C added to be ! consistent with observations of Heymsfield et al. 1986]: ! 2011/05/24 : rei_min = 3.5 becomes a free PARAMETER as well as ! rei_max=61.29 tc = t(i, k) - 273.15 rei = d_rei_dt*tc + rei_max IF (tc<=-81.4) rei = rei_min ! -- cloud optical thickness : ! [for liquid clouds, traditional formula, ! for ice clouds, Ebert & Curry (1992)] IF (zflwp_var==0.) rel = 1. IF (zfiwp_var==0. .OR. rei<=0.) rei = 1. pcltau(i, k) = 3.0/2.0*(zflwp_var/rel) + zfiwp_var*(3.448E-03+2.431/ & rei) ! -- cloud infrared emissivity: ! [the broadband infrared absorption coefficient is PARAMETERized ! as a function of the effective cld droplet radius] ! Ebert and Curry (1992) formula as used by Kiehl & Zender (1995): k_ice = k_ice0 + 1.0/rei pclemi(i, k) = 1.0 - exp(-coef_chau*zflwp_var-df*k_ice*zfiwp_var) END IF reice(i, k) = rei xflwp(i) = xflwp(i) + xflwc(i, k)*rhodz(i, k) xfiwp(i) = xfiwp(i) + xfiwc(i, k)*rhodz(i, k) END DO END DO ! --if cloud droplet radius is fixed, then pcldtaupi=pcltau IF (.NOT. ok_cdnc) THEN DO k = 1, klev DO i = 1, klon pcldtaupi(i, k) = pcltau(i, k) reice_pi(i, k) = reice(i, k) END DO END DO END IF DO k = 1, klev DO i = 1, klon reliq(i, k) = rad_chaud(i, k) reliq_pi(i, k) = rad_chaud_pi(i, k) reice_pi(i, k) = reice(i, k) END DO END DO ! COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS ! IM cf. CR:test: calcul prenant ou non en compte le recouvrement ! initialisations DO i = 1, klon zclear(i) = 1. zcloud(i) = 0. zcloudh(i) = 0. zcloudm(i) = 0. zcloudl(i) = 0. pch(i) = 1.0 pcm(i) = 1.0 pcl(i) = 1.0 pctlwp(i) = 0.0 END DO ! --calculation of liquid water path DO k = klev, 1, -1 DO i = 1, klon pctlwp(i) = pctlwp(i) + pqlwp(i, k)*rhodz(i, k) END DO END DO ! --calculation of cloud properties with cloud overlap IF (novlp==1) THEN DO k = klev, 1, -1 DO i = 1, klon zclear(i) = zclear(i)*(1.-max(pclc(i,k),zcloud(i)))/(1.-min(real( & zcloud(i),kind=8),1.-zepsec)) pct(i) = 1. - zclear(i) IF (paprs(i,k)=prmhc .AND. paprs(i,k)=prlmc) THEN pcl(i) = pcl(i)*(1.-max(pclc(i,k),zcloudl(i)))/(1.-min(real(zcloudl & (i),kind=8),1.-zepsec)) zcloudl(i) = pclc(i, k) END IF zcloud(i) = pclc(i, k) END DO END DO ELSE IF (novlp==2) THEN DO k = klev, 1, -1 DO i = 1, klon zcloud(i) = max(pclc(i,k), zcloud(i)) pct(i) = zcloud(i) IF (paprs(i,k)=prmhc .AND. paprs(i,k)=prlmc) THEN pcl(i) = min(pclc(i,k), pcl(i)) END IF END DO END DO ELSE IF (novlp==3) THEN DO k = klev, 1, -1 DO i = 1, klon zclear(i) = zclear(i)*(1.-pclc(i,k)) pct(i) = 1 - zclear(i) IF (paprs(i,k)=prmhc .AND. paprs(i,k)=prlmc) THEN pcl(i) = pcl(i)*(1.0-pclc(i,k)) END IF END DO END DO END IF DO i = 1, klon pch(i) = 1. - pch(i) pcm(i) = 1. - pcm(i) pcl(i) = 1. - pcl(i) END DO ! ======================================================== ! DIAGNOSTICS CALCULATION FOR CMIP5 PROTOCOL ! ======================================================== ! change by Nicolas Yan (LSCE) ! Cloud Droplet Number Concentration (CDNC) : 3D variable ! Fractionnal cover by liquid water cloud (LCC3D) : 3D variable ! Cloud Droplet Number Concentration at top of cloud (CLDNCL) : 2D variable ! Droplet effective radius at top of cloud (REFFCLWTOP) : 2D variable ! Fractionnal cover by liquid water at top of clouds (LCC) : 2D variable IF (ok_cdnc) THEN DO k = 1, klev DO i = 1, klon phase3d(i, k) = 1 - zfice(i, k) IF (pclc(i,k)<=seuil_neb) THEN lcc3d(i, k) = seuil_neb*phase3d(i, k) ELSE lcc3d(i, k) = pclc(i, k)*phase3d(i, k) END IF scdnc(i, k) = lcc3d(i, k)*cdnc(i, k) ! m-3 END DO END DO DO i = 1, klon lcc(i) = 0. reffclwtop(i) = 0. cldncl(i) = 0. IF (novlp.EQ.3 .OR. novlp.EQ.1) tcc(i) = 1. IF (novlp.EQ.2) tcc(i) = 0. END DO DO i = 1, klon DO k = klev - 1, 1, -1 !From TOA down ! Test, if the cloud optical depth exceeds the necessary ! threshold: IF (pcltau(i,k)>thres_tau .AND. pclc(i,k)>thres_neb) THEN IF (novlp.EQ.2) THEN IF (first) THEN WRITE (*, *) 'Hypothese de recouvrement: MAXIMUM' first = .FALSE. END IF flag_max = -1. ftmp(i) = max(tcc(i), pclc(i,k)) END IF IF (novlp.EQ.3) THEN IF (first) THEN WRITE (*, *) 'Hypothese de recouvrement: RANDOM' first = .FALSE. END IF flag_max = 1. ftmp(i) = tcc(i)*(1-pclc(i,k)) END IF IF (novlp.EQ.1) THEN IF (first) THEN WRITE (*, *) 'Hypothese de recouvrement: MAXIMUM_ & & & & RANDOM' first = .FALSE. END IF flag_max = 1. ftmp(i) = tcc(i)*(1.-max(pclc(i,k),pclc(i,k+1)))/(1.-min(pclc(i, & k+1),1.-thres_neb)) END IF ! Effective radius of cloud droplet at top of cloud (m) reffclwtop(i) = reffclwtop(i) + rad_chaud(i, k)*1.0E-06*phase3d(i, & k)*(tcc(i)-ftmp(i))*flag_max ! CDNC at top of cloud (m-3) cldncl(i) = cldncl(i) + cdnc(i, k)*phase3d(i, k)*(tcc(i)-ftmp(i))* & flag_max ! Liquid Cloud Content at top of cloud lcc(i) = lcc(i) + phase3d(i, k)*(tcc(i)-ftmp(i))*flag_max ! Total Cloud Content at top of cloud tcc(i) = ftmp(i) END IF ! is there a visible, not-too-small cloud? END DO ! loop over k IF (novlp.EQ.3 .OR. novlp.EQ.1) tcc(i) = 1. - tcc(i) END DO ! loop over i ! ! Convective and Stratiform Cloud Droplet Effective Radius (REFFCLWC ! REFFCLWS) DO i = 1, klon DO k = 1, klev ! Weight to be used for outputs: eau_liquide*couverture nuageuse lcc3dcon(i, k) = rnebcon(i, k)*phase3d(i, k)*clwcon(i, k) ! eau liquide convective lcc3dstra(i, k) = pclc(i, k)*pqlwp(i, k)*phase3d(i, k) lcc3dstra(i, k) = lcc3dstra(i, k) - lcc3dcon(i, k) ! eau liquide stratiforme lcc3dstra(i, k) = max(lcc3dstra(i,k), 0.0) !FC pour la glace (CAUSES) icc3dcon(i, k) = rnebcon(i, k)*(1-phase3d(i, k))*clwcon(i, k) ! glace convective icc3dstra(i, k)= pclc(i, k)*pqlwp(i, k)*(1-phase3d(i, k)) icc3dstra(i, k) = icc3dstra(i, k) - icc3dcon(i, k) ! glace stratiforme icc3dstra(i, k) = max( icc3dstra(i, k), 0.0) !FC (CAUSES) ! Compute cloud droplet radius as above in meter radius = 1.1*((pqlwp(i,k)*pplay(i,k)/(rd*t(i,k)))/(4./3*rpi*1000.* & cdnc(i,k)))**(1./3.) radius = max(radius, 5.E-6) ! Convective Cloud Droplet Effective Radius (REFFCLWC) : variable 3D reffclwc(i, k) = radius reffclwc(i, k) = reffclwc(i, k)*lcc3dcon(i, k) ! Stratiform Cloud Droplet Effective Radius (REFFCLWS) : variable 3D reffclws(i, k) = radius reffclws(i, k) = reffclws(i, k)*lcc3dstra(i, k) END DO !klev END DO !klon ! Column Integrated Cloud Droplet Number (CLDNVI) : variable 2D DO i = 1, klon cldnvi(i) = 0. lcc_integrat(i) = 0. height(i) = 0. DO k = 1, klev cldnvi(i) = cldnvi(i) + cdnc(i, k)*lcc3d(i, k)*dh(i, k) lcc_integrat(i) = lcc_integrat(i) + lcc3d(i, k)*dh(i, k) height(i) = height(i) + dh(i, k) END DO ! klev lcc_integrat(i) = lcc_integrat(i)/height(i) IF (lcc_integrat(i)<=1.0E-03) THEN cldnvi(i) = cldnvi(i)*lcc(i)/seuil_neb ELSE cldnvi(i) = cldnvi(i)*lcc(i)/lcc_integrat(i) END IF END DO ! klon DO i = 1, klon DO k = 1, klev IF (scdnc(i,k)<=0.0) scdnc(i, k) = 0.0 IF (reffclws(i,k)<=0.0) reffclws(i, k) = 0.0 IF (reffclwc(i,k)<=0.0) reffclwc(i, k) = 0.0 IF (lcc3d(i,k)<=0.0) lcc3d(i, k) = 0.0 IF (lcc3dcon(i,k)<=0.0) lcc3dcon(i, k) = 0.0 IF (lcc3dstra(i,k)<=0.0) lcc3dstra(i, k) = 0.0 !FC (CAUSES) IF (icc3dcon(i,k)<=0.0) icc3dcon(i, k) = 0.0 IF (icc3dstra(i,k)<=0.0) icc3dstra(i, k) = 0.0 !FC (CAUSES) END DO IF (reffclwtop(i)<=0.0) reffclwtop(i) = 0.0 IF (cldncl(i)<=0.0) cldncl(i) = 0.0 IF (cldnvi(i)<=0.0) cldnvi(i) = 0.0 IF (lcc(i)<=0.0) lcc(i) = 0.0 END DO END IF !ok_cdnc RETURN END SUBROUTINE newmicro