! ! $Id: convect2.F 1299 2010-01-20 14:27:21Z crisi $ ! subroutine convect2(ncum,idcum,len,nd,ndp1,nl,minorig, & nk1,icb1, & t1,q1,qs1,u1,v1,gz1,tv1,tp1,tvp1,clw1,h1, & lv1,cpn1,p1,ph1,ft1,fq1,fu1,fv1, & tnk1,qnk1,gznk1,plcl1, & precip1,cbmf1,iflag1, & delt,cpd,cpv,cl,rv,rd,lv0,g, & sigs,sigd,elcrit,tlcrit,omtsnow,dtmax,damp, & alpha,entp,coeffs,coeffr,omtrain,cu,Ma) C.............................START PROLOGUE............................ C C SCCS IDENTIFICATION: @(#)convect2.f 1.2 05/18/00 C 22:06:22 /h/cm/library/nogaps4/src/sub/fcst/convect2.f_v C C CONFIGURATION IDENTIFICATION: None C C MODULE NAME: convect2 C C DESCRIPTION: C C convect1 The Emanuel Cumulus Convection Scheme - compute tendencies C C CONTRACT NUMBER AND TITLE: None C C REFERENCES: Programmers K. Emanuel (MIT), Timothy F. Hogan, M. Peng (NRL) C C CLASSIFICATION: Unclassified C C RESTRICTIONS: None C C COMPILER DEPENDENCIES: FORTRAN 77, FORTRAN 90 C C COMPILE OPTIONS: Fortran 77: -Zu -Wf"-ei -o aggress" C Fortran 90: -O vector3,scalar3,task1,aggress,overindex -ei -r 2 C C LIBRARIES OF RESIDENCE: /a/ops/lib/libfcst159.a C C USAGE: call convect2(ncum,idcum,len,nd,nl,minorig, C & nk1,icb1, C & t1,q1,qs1,u1,v1,gz1,tv1,tp1,tvp1,clw1,h1, C & lv1,cpn1,p1,ph1,ft1,fq1,fu1,fv1, C & tnk1,qnk1,gznk1,plcl1, C & precip1,cbmf1,iflag1, C & delt,cpd,cpv,cl,rv,rd,lv0,g, C & sigs,sigd,elcrit,tlcrit,omtsnow,dtmax,damp, C & alpha,entp,coeffs,coeffr,omtrain,cu) C C PARAMETERS: C Name Type Usage Description C ---------- ---------- ------- ---------------------------- C C ncum Integer Input number of cumulus points C idcum Integer Input index of cumulus point C len Integer Input first dimension C nd Integer Input total vertical dimension C ndp1 Integer Input nd + 1 C nl Integer Input vertical dimension for convection C minorig Integer Input First level where convection is allow to begin C nk1 Integer Input First level of convection C ncb1 Integer Input Level of free convection C t1 Real Input temperature C q1 Real Input specific hum C qs1 Real Input sat specific hum C u1 Real Input u-wind C v1 Real Input v-wind C gz1 Real Inout geop C tv1 Real Input virtual temp C tp1 Real Input C clw1 Real Inout cloud liquid water C h1 Real Inout C lv1 Real Inout C cpn1 Real Inout C p1 Real Input full level pressure C ph1 Real Input half level pressure C ft1 Real Output temp tend C fq1 Real Output spec hum tend C fu1 Real Output u-wind tend C fv1 Real Output v-wind tend C precip1 Real Output prec C cbmf1 Real In/Out cumulus mass flux C iflag1 Integer Output iflag on latitude strip C delt Real Input time step C cpd Integer Input See description below C cpv Integer Input See description below C cl Integer Input See description below C rv Integer Input See description below C rd Integer Input See description below C lv0 Integer Input See description below C g Integer Input See description below C sigs Integer Input See description below C sigd Integer Input See description below C elcrit Integer Input See description below C tlcrit Integer Input See description below C omtsnow Integer Input See description below C dtmax Integer Input See description below C damp Integer Input See description below C alpha Integer Input See description below C ent Integer Input See description below C coeffs Integer Input See description below C coeffr Integer Input See description below C omtrain Integer Input See description below C cu Integer Input See description below C C COMMON BLOCKS: C Block Name Type Usage Notes C -------- -------- ---- ------ ------------------------ C C FILES: None C C DATA BASES: None C C NON-FILE INPUT/OUTPUT: None C C ERROR CONDITIONS: None C C ADDITIONAL COMMENTS: None C C.................MAINTENANCE SECTION................................ C C MODULES CALLED: C Name Description C zilch Zero out an array C ------- ---------------------- C LOCAL VARIABLES AND C STRUCTURES: C Name Type Description C ------- ------ ----------- C See Comments Below C C i Integer loop index C k Integer loop index c C METHOD: C C See Emanuel, K. and M. Zivkovic-Rothman, 2000: Development and evaluation of a C convective scheme for use in climate models. C C FILES: None C C INCLUDE FILES: None C C MAKEFILE: /a/ops/met/nogaps/src/sub/fcst/fcst159lib.mak C C..............................END PROLOGUE............................. c c USE dimphy implicit none c cym#include "dimensions.h" cym#include "dimphy.h" c integer kmax2,imax2,kmin2,imin2 real ftmax2,ftmin2 integer kmax,imax,kmin,imin real ftmax,ftmin c integer ncum integer idcum(len) integer len integer nd integer ndp1 integer nl integer minorig integer nk1(len) integer icb1(len) real t1(len,nd) real q1(len,nd) real qs1(len,nd) real u1(len,nd) real v1(len,nd) real gz1(len,nd) real tv1(len,nd) real tp1(len,nd) real tvp1(len,nd) real clw1(len,nd) real h1(len,nd) real lv1(len,nd) real cpn1(len,nd) real p1(len,nd) real ph1(len,ndp1) real ft1(len,nd) real fq1(len,nd) real fu1(len,nd) real fv1(len,nd) real tnk1(len) real qnk1(len) real gznk1(len) real precip1(len) real cbmf1(len) real plcl1(len) integer iflag1(len) real delt real cpd real cpv real cl real rv real rd real lv0 real g real sigs ! SIGS IS THE FRACTION OF PRECIPITATION FALLING OUTSIDE real sigd ! SIGD IS THE FRACTIONAL AREA COVERED BY UNSATURATED DNDRAFT real elcrit ! ELCRIT IS THE AUTOCONVERSION THERSHOLD WATER CONTENT (gm/gm) real tlcrit ! TLCRIT IS CRITICAL TEMPERATURE BELOW WHICH THE AUTO- c CONVERSION THRESHOLD IS ASSUMED TO BE ZERO real omtsnow ! OMTSNOW IS THE ASSUMED FALL SPEED (P/s) OF SNOW real dtmax ! DTMAX IS THE MAXIMUM NEGATIVE TEMPERATURE PERTURBATION c A LIFTED PARCEL IS ALLOWED TO HAVE BELOW ITS LFC. real damp real alpha real entp ! ENTP IS THE COEFFICIENT OF MIXING IN THE ENTRAINMENT FORMULATION real coeffs ! COEFFS IS A COEFFICIENT GOVERNING THE RATE OF EVAPORATION OF SNOW real coeffr ! COEFFR IS A COEFFICIENT GOVERNING THE RATE OF EVAPORATION OF RAIN real omtrain ! OMTRAIN IS THE ASSUMED FALL SPEED (P/s) OF RAIN real cu ! CU IS THE COEFFICIENT GOVERNING CONVECTIVE MOMENTUM TRANSPORT c real Ma(len,nd) c C C *** ELCRIT IS THE AUTOCONVERSION THERSHOLD WATER CONTENT (gm/gm) *** C *** TLCRIT IS CRITICAL TEMPERATURE BELOW WHICH THE AUTO- *** C *** CONVERSION THRESHOLD IS ASSUMED TO BE ZERO *** C *** (THE AUTOCONVERSION THRESHOLD VARIES LINEARLY *** C *** BETWEEN 0 C AND TLCRIT) *** C *** ENTP IS THE COEFFICIENT OF MIXING IN THE ENTRAINMENT *** C *** FORMULATION *** C *** SIGD IS THE FRACTIONAL AREA COVERED BY UNSATURATED DNDRAFT *** C *** SIGS IS THE FRACTION OF PRECIPITATION FALLING OUTSIDE *** C *** OF CLOUD *** C *** OMTRAIN IS THE ASSUMED FALL SPEED (P/s) OF RAIN *** C *** OMTSNOW IS THE ASSUMED FALL SPEED (P/s) OF SNOW *** C *** COEFFR IS A COEFFICIENT GOVERNING THE RATE OF EVAPORATION *** C *** OF RAIN *** C *** COEFFS IS A COEFFICIENT GOVERNING THE RATE OF EVAPORATION *** C *** OF SNOW *** C *** CU IS THE COEFFICIENT GOVERNING CONVECTIVE MOMENTUM *** C *** TRANSPORT *** C *** DTMAX IS THE MAXIMUM NEGATIVE TEMPERATURE PERTURBATION *** C *** A LIFTED PARCEL IS ALLOWED TO HAVE BELOW ITS LFC *** C *** ALPHA AND DAMP ARE PARAMETERS THAT CONTROL THE RATE OF *** C *** APPROACH TO QUASI-EQUILIBRIUM *** C *** (THEIR STANDARD VALUES ARE 0.20 AND 0.1, RESPECTIVELY) *** C *** (DAMP MUST BE LESS THAN 1) *** c c Local arrays. c real work(ncum) real t(ncum,klev) real q(ncum,klev) real qs(ncum,klev) real u(ncum,klev) real v(ncum,klev) real gz(ncum,klev) real h(ncum,klev) real lv(ncum,klev) real cpn(ncum,klev) real p(ncum,klev) real ph(ncum,klev) real ft(ncum,klev) real fq(ncum,klev) real fu(ncum,klev) real fv(ncum,klev) real precip(ncum) real cbmf(ncum) real plcl(ncum) real tnk(ncum) real qnk(ncum) real gznk(ncum) real tv(ncum,klev) real tp(ncum,klev) real tvp(ncum,klev) real clw(ncum,klev) c real det(ncum,klev) real dph(ncum,klev) c real wd(ncum) c real tprime(ncum) c real qprime(ncum) real ah0(ncum) real ep(ncum,klev) real sigp(ncum,klev) integer nent(ncum,klev) real water(ncum,klev) real evap(ncum,klev) real mp(ncum,klev) real m(ncum,klev) real qti real wt(ncum,klev) real hp(ncum,klev) real lvcp(ncum,klev) real elij(ncum,klev,klev) real ment(ncum,klev,klev) real sij(ncum,klev,klev) real qent(ncum,klev,klev) real uent(ncum,klev,klev) real vent(ncum,klev,klev) real qp(ncum,klev) real up(ncum,klev) real vp(ncum,klev) real cape(ncum) real capem(ncum) real frac(ncum) real dtpbl(ncum) real tvpplcl(ncum) real tvaplcl(ncum) real dtmin(ncum) real w3d(ncum,klev) real am(ncum) real ents(ncum) real uav(ncum) real vav(ncum) c integer iflag(ncum) integer nk(ncum) integer icb(ncum) integer inb(ncum) integer inb1(ncum) integer jtt(ncum) c integer nn,i,k,n,icbmax,nlp,j integer ij integer nn2,nn3 real clmcpv real clmcpd real cpdmcp real cpvmcpd real eps real epsi real epsim1 real tg,qg,s,alv,tc,ahg,denom,es,rg,ginv,rowl real delti real tca,elacrit real by,defrac c real byp real byp(ncum) logical lcape(ncum) real dbo real bf2,anum,dei,altem,cwat,stemp real alt,qp1,smid,sjmax,sjmin real delp,delm real awat,coeff,afac,revap,dhdp,fac,qstm,rat real qsm,sigt,b6,c6 real dpinv,cpinv real fqold,ftold,fuold,fvold real wdtrain(ncum),xxx real bsum(ncum,klev) real asij(ncum) real smin(ncum) real scrit(ncum) c real amp1,ad real amp1(ncum),ad(ncum) logical lwork(ncum) integer num1,num2 c c print*,'cpd en entree de convect2 ',cpd nlp=nl+1 c rowl=1000.0 ginv=1.0/g delti=1.0/delt c c Define some thermodynamic variables. c clmcpv=cl-cpv clmcpd=cl-cpd cpdmcp=cpd-cpv cpvmcpd=cpv-cpd eps=rd/rv epsi=1.0/eps epsim1=epsi-1.0 c c Compress the fields. c do 110 k=1,nl+1 nn=0 do 100 i=1,len if(iflag1(i).eq.0)then nn=nn+1 t(nn,k)=t1(i,k) q(nn,k)=q1(i,k) qs(nn,k)=qs1(i,k) u(nn,k)=u1(i,k) v(nn,k)=v1(i,k) gz(nn,k)=gz1(i,k) h(nn,k)=h1(i,k) lv(nn,k)=lv1(i,k) cpn(nn,k)=cpn1(i,k) p(nn,k)=p1(i,k) ph(nn,k)=ph1(i,k) tv(nn,k)=tv1(i,k) tp(nn,k)=tp1(i,k) tvp(nn,k)=tvp1(i,k) clw(nn,k)=clw1(i,k) endif 100 continue c print*,'100 ncum,nn',ncum,nn 110 continue nn=0 do 150 i=1,len if(iflag1(i).eq.0)then nn=nn+1 cbmf(nn)=cbmf1(i) plcl(nn)=plcl1(i) tnk(nn)=tnk1(i) qnk(nn)=qnk1(i) gznk(nn)=gznk1(i) nk(nn)=nk1(i) icb(nn)=icb1(i) iflag(nn)=iflag1(i) endif 150 continue c print*,'150 ncum,nn',ncum,nn c c Initialize the tendencies, det, wd, tprime, qprime. c do 170 k=1,nl do 160 i=1,ncum c det(i,k)=0.0 ft(i,k)=0.0 fu(i,k)=0.0 fv(i,k)=0.0 fq(i,k)=0.0 dph(i,k)=ph(i,k)-ph(i,k+1) ep(i,k)=0.0 sigp(i,k)=sigs 160 continue 170 continue do 180 i=1,ncum c wd(i)=0.0 c tprime(i)=0.0 c qprime(i)=0.0 precip(i)=0.0 ft(i,nl+1)=0.0 fu(i,nl+1)=0.0 fv(i,nl+1)=0.0 fq(i,nl+1)=0.0 180 continue c c Compute icbmax. c icbmax=2 do 230 i=1,ncum icbmax=max(icbmax,icb(i)) 230 continue c c !===================================================================== ! --- FIND THE REST OF THE LIFTED PARCEL TEMPERATURES !===================================================================== c c --- The procedure is to solve the equation. c cp*tp+L*qp+phi=cp*tnk+L*qnk+gznk. c c *** Calculate certain parcel quantities, including static energy *** c c do 240 i=1,ncum ah0(i)=(cpd*(1.-qnk(i))+cl*qnk(i))*tnk(i) & +qnk(i)*(lv0-clmcpv*(tnk(i)-273.15))+gznk(i) 240 continue c c c *** Find lifted parcel quantities above cloud base *** c c do 300 k=minorig+1,nl do 290 i=1,ncum if(k.ge.(icb(i)+1))then tg=t(i,k) qg=qs(i,k) alv=lv0-clmcpv*(t(i,k)-273.15) c c First iteration. c s=cpd+alv*alv*qg/(rv*t(i,k)*t(i,k)) s=1./s ahg=cpd*tg+(cl-cpd)*qnk(i)*t(i,k)+alv*qg+gz(i,k) tg=tg+s*(ah0(i)-ahg) tg=max(tg,35.0) tc=tg-273.15 denom=243.5+tc if(tc.ge.0.0)then es=6.112*exp(17.67*tc/denom) else es=exp(23.33086-6111.72784/tg+0.15215*log(tg)) endif qg=eps*es/(p(i,k)-es*(1.-eps)) c c Second iteration. c s=cpd+alv*alv*qg/(rv*t(i,k)*t(i,k)) s=1./s ahg=cpd*tg+(cl-cpd)*qnk(i)*t(i,k)+alv*qg+gz(i,k) tg=tg+s*(ah0(i)-ahg) tg=max(tg,35.0) tc=tg-273.15 denom=243.5+tc if(tc.ge.0.0)then es=6.112*exp(17.67*tc/denom) else es=exp(23.33086-6111.72784/tg+0.15215*log(tg)) endif qg=eps*es/(p(i,k)-es*(1.-eps)) c alv=lv0-clmcpv*(t(i,k)-273.15) c print*,'cpd dans convect2 ',cpd c print*,'tp(i,k),ah0(i),cl,cpd,qnk(i),t(i,k),gz(i,k),alv,qg,cpd' c print*,tp(i,k),ah0(i),cl,cpd,qnk(i),t(i,k),gz(i,k),alv,qg,cpd tp(i,k)=(ah0(i)-(cl-cpd)*qnk(i)*t(i,k)-gz(i,k)-alv*qg) & /cpd c if (.not.cpd.gt.1000.) then c print*,'CPD=',cpd c stop c endif clw(i,k)=qnk(i)-qg clw(i,k)=max(0.0,clw(i,k)) rg=qg/(1.-qnk(i)) tvp(i,k)=tp(i,k)*(1.+rg*epsi) endif 290 continue 300 continue c !===================================================================== ! --- SET THE PRECIPITATION EFFICIENCIES AND THE FRACTION OF ! --- PRECIPITATION FALLING OUTSIDE OF CLOUD ! --- THESE MAY BE FUNCTIONS OF TP(I), P(I) AND CLW(I) !===================================================================== c do 320 k=minorig+1,nl do 310 i=1,ncum if(k.ge.(nk(i)+1))then tca=tp(i,k)-273.15 if(tca.ge.0.0)then elacrit=elcrit else elacrit=elcrit*(1.0-tca/tlcrit) endif elacrit=max(elacrit,0.0) ep(i,k)=1.0-elacrit/max(clw(i,k),1.0e-8) ep(i,k)=max(ep(i,k),0.0 ) ep(i,k)=min(ep(i,k),1.0 ) sigp(i,k)=sigs endif 310 continue 320 continue c !===================================================================== ! --- CALCULATE VIRTUAL TEMPERATURE AND LIFTED PARCEL ! --- VIRTUAL TEMPERATURE !===================================================================== c do 340 k=minorig+1,nl do 330 i=1,ncum if(k.ge.(icb(i)+1))then tvp(i,k)=tvp(i,k)*(1.0-qnk(i)+ep(i,k)*clw(i,k)) c print*,'i,k,tvp(i,k),qnk(i),ep(i,k),clw(i,k)' c print*, i,k,tvp(i,k),qnk(i),ep(i,k),clw(i,k) endif 330 continue 340 continue do 350 i=1,ncum tvp(i,nlp)=tvp(i,nl)-(gz(i,nlp)-gz(i,nl))/cpd 350 continue c c c===================================================================== c --- NOW INITIALIZE VARIOUS ARRAYS USED IN THE COMPUTATIONS c===================================================================== c do 360 i=1,ncum*nlp nent(i,1)=0 water(i,1)=0.0 evap(i,1)=0.0 mp(i,1)=0.0 m(i,1)=0.0 wt(i,1)=omtsnow hp(i,1)=h(i,1) c if(.not.cpn(i,1).gt.900.) then c print*,'i,lv(i,1),cpn(i,1)' c print*, i,lv(i,1),cpn(i,1) c k=(i-1)/ncum+1 c print*,'i,k',mod(i,ncum),k,' cpn',cpn(mod(i,ncum),k) c stop c endif lvcp(i,1)=lv(i,1)/cpn(i,1) 360 continue c do 380 i=1,ncum*nlp*nlp elij(i,1,1)=0.0 ment(i,1,1)=0.0 sij(i,1,1)=0.0 380 continue c do 400 k=1,nlp do 390 j=1,nlp do 385 i=1,ncum qent(i,k,j)=q(i,j) uent(i,k,j)=u(i,j) vent(i,k,j)=v(i,j) 385 continue 390 continue 400 continue c do 420 i=1,ncum qp(i,1)=q(i,1) up(i,1)=u(i,1) vp(i,1)=v(i,1) 420 continue do 440 k=2,nlp do 430 i=1,ncum qp(i,k)=q(i,k-1) up(i,k)=u(i,k-1) vp(i,k)=v(i,k-1) 430 continue 440 continue c c===================================================================== c --- FIND THE FIRST MODEL LEVEL (INB1) ABOVE THE PARCEL'S c --- HIGHEST LEVEL OF NEUTRAL BUOYANCY c --- AND THE HIGHEST LEVEL OF POSITIVE CAPE (INB) c===================================================================== c do 510 i=1,ncum cape(i)=0.0 capem(i)=0.0 inb(i)=icb(i)+1 inb1(i)=inb(i) 510 continue c c Originial Code c c do 530 k=minorig+1,nl-1 c do 520 i=1,ncum c if(k.ge.(icb(i)+1))then c by=(tvp(i,k)-tv(i,k))*dph(i,k)/p(i,k) c byp=(tvp(i,k+1)-tv(i,k+1))*dph(i,k+1)/p(i,k+1) c cape(i)=cape(i)+by c if(by.ge.0.0)inb1(i)=k+1 c if(cape(i).gt.0.0)then c inb(i)=k+1 c capem(i)=cape(i) c endif c endif c520 continue c530 continue c do 540 i=1,ncum c byp=(tvp(i,nl)-tv(i,nl))*dph(i,nl)/p(i,nl) c cape(i)=capem(i)+byp c defrac=capem(i)-cape(i) c defrac=max(defrac,0.001) c frac(i)=-cape(i)/defrac c frac(i)=min(frac(i),1.0) c frac(i)=max(frac(i),0.0) c540 continue c c K Emanuel fix c c call zilch(byp,ncum) c do 530 k=minorig+1,nl-1 c do 520 i=1,ncum c if(k.ge.(icb(i)+1))then c by=(tvp(i,k)-tv(i,k))*dph(i,k)/p(i,k) c cape(i)=cape(i)+by c if(by.ge.0.0)inb1(i)=k+1 c if(cape(i).gt.0.0)then c inb(i)=k+1 c capem(i)=cape(i) c byp(i)=(tvp(i,k+1)-tv(i,k+1))*dph(i,k+1)/p(i,k+1) c endif c endif c520 continue c530 continue c do 540 i=1,ncum c inb(i)=max(inb(i),inb1(i)) c cape(i)=capem(i)+byp(i) c defrac=capem(i)-cape(i) c defrac=max(defrac,0.001) c frac(i)=-cape(i)/defrac c frac(i)=min(frac(i),1.0) c frac(i)=max(frac(i),0.0) c540 continue c c J Teixeira fix c call zilch(byp,ncum) do 515 i=1,ncum lcape(i)=.true. 515 continue do 530 k=minorig+1,nl-1 do 520 i=1,ncum if(cape(i).lt.0.0)lcape(i)=.false. if((k.ge.(icb(i)+1)).and.lcape(i))then by=(tvp(i,k)-tv(i,k))*dph(i,k)/p(i,k) byp(i)=(tvp(i,k+1)-tv(i,k+1))*dph(i,k+1)/p(i,k+1) cape(i)=cape(i)+by if(by.ge.0.0)inb1(i)=k+1 if(cape(i).gt.0.0)then inb(i)=k+1 capem(i)=cape(i) endif endif 520 continue 530 continue do 540 i=1,ncum cape(i)=capem(i)+byp(i) defrac=capem(i)-cape(i) defrac=max(defrac,0.001) frac(i)=-cape(i)/defrac frac(i)=min(frac(i),1.0) frac(i)=max(frac(i),0.0) 540 continue c c===================================================================== c --- CALCULATE LIQUID WATER STATIC ENERGY OF LIFTED PARCEL c===================================================================== c do 600 k=minorig+1,nl do 590 i=1,ncum if((k.ge.icb(i)).and.(k.le.inb(i)))then hp(i,k)=h(i,nk(i))+(lv(i,k)+(cpd-cpv)*t(i,k))*ep(i,k)*clw(i,k) endif 590 continue 600 continue c c===================================================================== c --- CALCULATE CLOUD BASE MASS FLUX AND RATES OF MIXING, M(I), c --- AT EACH MODEL LEVEL c===================================================================== c c tvpplcl = parcel temperature lifted adiabatically from level c icb-1 to the LCL. c tvaplcl = virtual temperature at the LCL. c do 610 i=1,ncum dtpbl(i)=0.0 tvpplcl(i)=tvp(i,icb(i)-1) & -rd*tvp(i,icb(i)-1)*(p(i,icb(i)-1)-plcl(i)) & /(cpn(i,icb(i)-1)*p(i,icb(i)-1)) tvaplcl(i)=tv(i,icb(i)) & +(tvp(i,icb(i))-tvp(i,icb(i)+1))*(plcl(i)-p(i,icb(i))) & /(p(i,icb(i))-p(i,icb(i)+1)) 610 continue c c------------------------------------------------------------------- c --- Interpolate difference between lifted parcel and c --- environmental temperatures to lifted condensation level c------------------------------------------------------------------- c c dtpbl = average of tvp-tv in the PBL (k=nk to icb-1). c do 630 k=minorig,icbmax do 620 i=1,ncum if((k.ge.nk(i)).and.(k.le.(icb(i)-1)))then dtpbl(i)=dtpbl(i)+(tvp(i,k)-tv(i,k))*dph(i,k) endif 620 continue 630 continue do 640 i=1,ncum dtpbl(i)=dtpbl(i)/(ph(i,nk(i))-ph(i,icb(i))) dtmin(i)=tvpplcl(i)-tvaplcl(i)+dtmax+dtpbl(i) 640 continue c c------------------------------------------------------------------- c --- Adjust cloud base mass flux c------------------------------------------------------------------- c do 650 i=1,ncum work(i)=cbmf(i) cbmf(i)=max(0.0,(1.0-damp)*cbmf(i)+0.1*alpha*dtmin(i)) if((work(i).eq.0.0).and.(cbmf(i).eq.0.0))then iflag(i)=3 endif 650 continue c c------------------------------------------------------------------- c --- Calculate rates of mixing, m(i) c------------------------------------------------------------------- c call zilch(work,ncum) c do 670 j=minorig+1,nl do 660 i=1,ncum if((j.ge.(icb(i)+1)).and.(j.le.inb(i)))then k=min(j,inb1(i)) dbo=abs(tv(i,k+1)-tvp(i,k+1)-tv(i,k-1)+tvp(i,k-1)) & +entp*0.04*(ph(i,k)-ph(i,k+1)) work(i)=work(i)+dbo m(i,j)=cbmf(i)*dbo endif 660 continue 670 continue do 690 k=minorig+1,nl do 680 i=1,ncum if((k.ge.(icb(i)+1)).and.(k.le.inb(i)))then m(i,k)=m(i,k)/work(i) endif 680 continue 690 continue c c c===================================================================== c --- CALCULATE ENTRAINED AIR MASS FLUX (ment), TOTAL WATER MIXING c --- RATIO (QENT), TOTAL CONDENSED WATER (elij), AND MIXING c --- FRACTION (sij) c===================================================================== c c do 750 i=minorig+1,nl do 710 j=minorig+1,nl do 700 ij=1,ncum if((i.ge.(icb(ij)+1)).and.(j.ge.icb(ij)) & .and.(i.le.inb(ij)).and.(j.le.inb(ij)))then qti=qnk(ij)-ep(ij,i)*clw(ij,i) bf2=1.+lv(ij,j)*lv(ij,j)*qs(ij,j) & /(rv*t(ij,j)*t(ij,j)*cpd) anum=h(ij,j)-hp(ij,i)+(cpv-cpd)*t(ij,j)*(qti-q(ij,j)) denom=h(ij,i)-hp(ij,i)+(cpd-cpv)*(q(ij,i)-qti)*t(ij,j) dei=denom if(abs(dei).lt.0.01)dei=0.01 sij(ij,i,j)=anum/dei sij(ij,i,i)=1.0 altem=sij(ij,i,j)*q(ij,i)+(1.-sij(ij,i,j))*qti-qs(ij,j) altem=altem/bf2 cwat=clw(ij,j)*(1.-ep(ij,j)) stemp=sij(ij,i,j) if((stemp.lt.0.0.or.stemp.gt.1.0.or. 1 altem.gt.cwat).and.j.gt.i)then anum=anum-lv(ij,j)*(qti-qs(ij,j)-cwat*bf2) denom=denom+lv(ij,j)*(q(ij,i)-qti) if(abs(denom).lt.0.01)denom=0.01 sij(ij,i,j)=anum/denom altem=sij(ij,i,j)*q(ij,i)+(1.-sij(ij,i,j))*qti-qs(ij,j) altem=altem-(bf2-1.)*cwat endif if(sij(ij,i,j).gt.0.0.and.sij(ij,i,j).lt.0.9)then qent(ij,i,j)=sij(ij,i,j)*q(ij,i) & +(1.-sij(ij,i,j))*qti uent(ij,i,j)=sij(ij,i,j)*u(ij,i) & +(1.-sij(ij,i,j))*u(ij,nk(ij)) vent(ij,i,j)=sij(ij,i,j)*v(ij,i) & +(1.-sij(ij,i,j))*v(ij,nk(ij)) elij(ij,i,j)=altem elij(ij,i,j)=max(0.0,elij(ij,i,j)) ment(ij,i,j)=m(ij,i)/(1.-sij(ij,i,j)) nent(ij,i)=nent(ij,i)+1 endif sij(ij,i,j)=max(0.0,sij(ij,i,j)) sij(ij,i,j)=min(1.0,sij(ij,i,j)) endif 700 continue 710 continue c c *** If no air can entrain at level i assume that updraft detrains *** c *** at that level and calculate detrained air flux and properties *** c do 740 ij=1,ncum if((i.ge.(icb(ij)+1)).and.(i.le.inb(ij)) & .and.(nent(ij,i).eq.0))then ment(ij,i,i)=m(ij,i) qent(ij,i,i)=q(ij,nk(ij))-ep(ij,i)*clw(ij,i) uent(ij,i,i)=u(ij,nk(ij)) vent(ij,i,i)=v(ij,nk(ij)) elij(ij,i,i)=clw(ij,i) sij(ij,i,i)=1.0 endif 740 continue 750 continue c do 770 i=1,ncum sij(i,inb(i),inb(i))=1.0 770 continue c c===================================================================== c --- NORMALIZE ENTRAINED AIR MASS FLUXES c --- TO REPRESENT EQUAL PROBABILITIES OF MIXING c===================================================================== c c call zilch(bsum,ncum*nlp) do 780 ij=1,ncum lwork(ij)=.false. 780 continue do 789 i=minorig+1,nl c num1=0 do 779 ij=1,ncum if((i.ge.icb(ij)+1).and.(i.le.inb(ij)))num1=num1+1 779 continue if(num1.le.0)go to 789 c do 781 ij=1,ncum if((i.ge.icb(ij)+1).and.(i.le.inb(ij)))then lwork(ij)=(nent(ij,i).ne.0) qp1=q(ij,nk(ij))-ep(ij,i)*clw(ij,i) anum=h(ij,i)-hp(ij,i)-lv(ij,i)*(qp1-qs(ij,i)) denom=h(ij,i)-hp(ij,i)+lv(ij,i)*(q(ij,i)-qp1) if(abs(denom).lt.0.01)denom=0.01 scrit(ij)=anum/denom alt=qp1-qs(ij,i)+scrit(ij)*(q(ij,i)-qp1) if(scrit(ij).lt.0.0.or.alt.lt.0.0)scrit(ij)=1.0 asij(ij)=0.0 smin(ij)=1.0 endif 781 continue do 783 j=minorig,nl c num2=0 do 778 ij=1,ncum if((i.ge.icb(ij)+1).and.(i.le.inb(ij)) & .and.(j.ge.icb(ij)).and.(j.le.inb(ij)) & .and.lwork(ij))num2=num2+1 778 continue if(num2.le.0)go to 783 c do 782 ij=1,ncum if((i.ge.icb(ij)+1).and.(i.le.inb(ij)) & .and.(j.ge.icb(ij)).and.(j.le.inb(ij)).and.lwork(ij))then if(sij(ij,i,j).gt.0.0.and.sij(ij,i,j).lt.0.9)then if(j.gt.i)then smid=min(sij(ij,i,j),scrit(ij)) sjmax=smid sjmin=smid if(smid.lt.smin(ij) & .and.sij(ij,i,j+1).lt.smid)then smin(ij)=smid sjmax=min(sij(ij,i,j+1),sij(ij,i,j),scrit(ij)) sjmin=max(sij(ij,i,j-1),sij(ij,i,j)) sjmin=min(sjmin,scrit(ij)) endif else sjmax=max(sij(ij,i,j+1),scrit(ij)) smid=max(sij(ij,i,j),scrit(ij)) sjmin=0.0 if(j.gt.1)sjmin=sij(ij,i,j-1) sjmin=max(sjmin,scrit(ij)) endif delp=abs(sjmax-smid) delm=abs(sjmin-smid) asij(ij)=asij(ij)+(delp+delm) & *(ph(ij,j)-ph(ij,j+1)) ment(ij,i,j)=ment(ij,i,j)*(delp+delm) & *(ph(ij,j)-ph(ij,j+1)) endif endif 782 continue 783 continue do 784 ij=1,ncum if((i.ge.icb(ij)+1).and.(i.le.inb(ij)).and.lwork(ij))then asij(ij)=max(1.0e-21,asij(ij)) asij(ij)=1.0/asij(ij) bsum(ij,i)=0.0 endif 784 continue do 786 j=minorig,nl+1 do 785 ij=1,ncum if((i.ge.icb(ij)+1).and.(i.le.inb(ij)) & .and.(j.ge.icb(ij)).and.(j.le.inb(ij)) & .and.lwork(ij))then ment(ij,i,j)=ment(ij,i,j)*asij(ij) bsum(ij,i)=bsum(ij,i)+ment(ij,i,j) endif 785 continue 786 continue do 787 ij=1,ncum if((i.ge.icb(ij)+1).and.(i.le.inb(ij)) & .and.(bsum(ij,i).lt.1.0e-18).and.lwork(ij))then nent(ij,i)=0 ment(ij,i,i)=m(ij,i) qent(ij,i,i)=q(ij,nk(ij))-ep(ij,i)*clw(ij,i) uent(ij,i,i)=u(ij,nk(ij)) vent(ij,i,i)=v(ij,nk(ij)) elij(ij,i,i)=clw(ij,i) sij(ij,i,i)=1.0 endif 787 continue 789 continue c c===================================================================== c --- PRECIPITATING DOWNDRAFT CALCULATION c===================================================================== c c *** Check whether ep(inb)=0, if so, skip precipitating *** c *** downdraft calculation *** c c c *** Integrate liquid water equation to find condensed water *** c *** and condensed water flux *** c c do 890 i=1,ncum jtt(i)=2 if(ep(i,inb(i)).le.0.0001)iflag(i)=2 if(iflag(i).eq.0)then lwork(i)=.true. else lwork(i)=.false. endif 890 continue c c *** Begin downdraft loop *** c c call zilch(wdtrain,ncum) do 899 i=nl+1,1,-1 c num1=0 do 879 ij=1,ncum if((i.le.inb(ij)).and.lwork(ij))num1=num1+1 879 continue if(num1.le.0)go to 899 c c c *** Calculate detrained precipitation *** c do 891 ij=1,ncum if((i.le.inb(ij)).and.(lwork(ij)))then wdtrain(ij)=g*ep(ij,i)*m(ij,i)*clw(ij,i) endif 891 continue c if(i.gt.1)then do 893 j=1,i-1 do 892 ij=1,ncum if((i.le.inb(ij)).and.(lwork(ij)))then awat=elij(ij,j,i)-(1.-ep(ij,i))*clw(ij,i) awat=max(0.0,awat) wdtrain(ij)=wdtrain(ij)+g*awat*ment(ij,j,i) endif 892 continue 893 continue endif c c *** Find rain water and evaporation using provisional *** c *** estimates of qp(i)and qp(i-1) *** c c c *** Value of terminal velocity and coeffecient of evaporation for snow *** c do 894 ij=1,ncum if((i.le.inb(ij)).and.(lwork(ij)))then coeff=coeffs wt(ij,i)=omtsnow c c *** Value of terminal velocity and coeffecient of evaporation for rain *** c if(t(ij,i).gt.273.0)then coeff=coeffr wt(ij,i)=omtrain endif qsm=0.5*(q(ij,i)+qp(ij,i+1)) afac=coeff*ph(ij,i)*(qs(ij,i)-qsm) & /(1.0e4+2.0e3*ph(ij,i)*qs(ij,i)) afac=max(afac,0.0) sigt=sigp(ij,i) sigt=max(0.0,sigt) sigt=min(1.0,sigt) b6=100.*(ph(ij,i)-ph(ij,i+1))*sigt*afac/wt(ij,i) c6=(water(ij,i+1)*wt(ij,i+1)+wdtrain(ij)/sigd)/wt(ij,i) revap=0.5*(-b6+sqrt(b6*b6+4.*c6)) evap(ij,i)=sigt*afac*revap water(ij,i)=revap*revap c c *** Calculate precipitating downdraft mass flux under *** c *** hydrostatic approximation *** c if(i.gt.1)then dhdp=(h(ij,i)-h(ij,i-1))/(p(ij,i-1)-p(ij,i)) dhdp=max(dhdp,10.0) mp(ij,i)=100.*ginv*lv(ij,i)*sigd*evap(ij,i)/dhdp mp(ij,i)=max(mp(ij,i),0.0) c c *** Add small amount of inertia to downdraft *** c fac=20.0/(ph(ij,i-1)-ph(ij,i)) mp(ij,i)=(fac*mp(ij,i+1)+mp(ij,i))/(1.+fac) c c *** Force mp to decrease linearly to zero *** c *** between about 950 mb and the surface *** c if(p(ij,i).gt.(0.949*p(ij,1)))then jtt(ij)=max(jtt(ij),i) mp(ij,i)=mp(ij,jtt(ij))*(p(ij,1)-p(ij,i)) & /(p(ij,1)-p(ij,jtt(ij))) endif endif c c *** Find mixing ratio of precipitating downdraft *** c if(i.ne.inb(ij))then if(i.eq.1)then qstm=qs(ij,1) else qstm=qs(ij,i-1) endif if(mp(ij,i).gt.mp(ij,i+1))then rat=mp(ij,i+1)/mp(ij,i) qp(ij,i)=qp(ij,i+1)*rat+q(ij,i)*(1.0-rat)+100.*ginv* & sigd*(ph(ij,i)-ph(ij,i+1))*(evap(ij,i)/mp(ij,i)) up(ij,i)=up(ij,i+1)*rat+u(ij,i)*(1.-rat) vp(ij,i)=vp(ij,i+1)*rat+v(ij,i)*(1.-rat) else if(mp(ij,i+1).gt.0.0)then qp(ij,i)=(gz(ij,i+1)-gz(ij,i) & +qp(ij,i+1)*(lv(ij,i+1)+t(ij,i+1) & *(cl-cpd))+cpd*(t(ij,i+1)-t(ij,i))) & /(lv(ij,i)+t(ij,i)*(cl-cpd)) up(ij,i)=up(ij,i+1) vp(ij,i)=vp(ij,i+1) endif endif qp(ij,i)=min(qp(ij,i),qstm) qp(ij,i)=max(qp(ij,i),0.0) endif endif 894 continue 899 continue c c *** Calculate surface precipitation in mm/day *** c do 1190 i=1,ncum if(iflag(i).le.1)then cc precip(i)=precip(i)+wt(i,1)*sigd*water(i,1)*3600.*24000. cc & /(rowl*g) cc precip(i)=precip(i)*delt/86400. precip(i) = wt(i,1)*sigd*water(i,1)*86400/g endif 1190 continue c c c *** Calculate downdraft velocity scale and surface temperature and *** c *** water vapor fluctuations *** c c wd=beta*abs(mp(icb))*0.01*rd*t(icb)/(sigd*p(icb)) c qprime=0.5*(qp(1)-q(1)) c tprime=lv0*qprime/cpd c c *** Calculate tendencies of lowest level potential temperature *** c *** and mixing ratio *** c do 1200 i=1,ncum work(i)=0.01/(ph(i,1)-ph(i,2)) am(i)=0.0 1200 continue do 1220 k=2,nl do 1210 i=1,ncum if((nk(i).eq.1).and.(k.le.inb(i)).and.(nk(i).eq.1))then am(i)=am(i)+m(i,k) endif 1210 continue 1220 continue do 1240 i=1,ncum if((g*work(i)*am(i)).ge.delti)iflag(i)=1 ft(i,1)=ft(i,1)+g*work(i)*am(i)*(t(i,2)-t(i,1) & +(gz(i,2)-gz(i,1))/cpn(i,1)) ft(i,1)=ft(i,1)-lvcp(i,1)*sigd*evap(i,1) ft(i,1)=ft(i,1)+sigd*wt(i,2)*(cl-cpd)*water(i,2)*(t(i,2) & -t(i,1))*work(i)/cpn(i,1) fq(i,1)=fq(i,1)+g*mp(i,2)*(qp(i,2)-q(i,1))* & work(i)+sigd*evap(i,1) fq(i,1)=fq(i,1)+g*am(i)*(q(i,2)-q(i,1))*work(i) fu(i,1)=fu(i,1)+g*work(i)*(mp(i,2)*(up(i,2)-u(i,1)) & +am(i)*(u(i,2)-u(i,1))) fv(i,1)=fv(i,1)+g*work(i)*(mp(i,2)*(vp(i,2)-v(i,1)) & +am(i)*(v(i,2)-v(i,1))) 1240 continue do 1260 j=2,nl do 1250 i=1,ncum if(j.le.inb(i))then fq(i,1)=fq(i,1) & +g*work(i)*ment(i,j,1)*(qent(i,j,1)-q(i,1)) fu(i,1)=fu(i,1) & +g*work(i)*ment(i,j,1)*(uent(i,j,1)-u(i,1)) fv(i,1)=fv(i,1) & +g*work(i)*ment(i,j,1)*(vent(i,j,1)-v(i,1)) endif 1250 continue 1260 continue c c *** Calculate tendencies of potential temperature and mixing ratio *** c *** at levels above the lowest level *** c c *** First find the net saturated updraft and downdraft mass fluxes *** c *** through each level *** c do 1500 i=2,nl+1 c num1=0 do 1265 ij=1,ncum if(i.le.inb(ij))num1=num1+1 1265 continue if(num1.le.0)go to 1500 c call zilch(amp1,ncum) call zilch(ad,ncum) c do 1280 k=i+1,nl+1 do 1270 ij=1,ncum if((i.ge.nk(ij)).and.(i.le.inb(ij)) & .and.(k.le.(inb(ij)+1)))then amp1(ij)=amp1(ij)+m(ij,k) endif 1270 continue 1280 continue c do 1310 k=1,i do 1300 j=i+1,nl+1 do 1290 ij=1,ncum if((j.le.(inb(ij)+1)).and.(i.le.inb(ij)))then amp1(ij)=amp1(ij)+ment(ij,k,j) endif 1290 continue 1300 continue 1310 continue do 1340 k=1,i-1 do 1330 j=i,nl+1 do 1320 ij=1,ncum if((i.le.inb(ij)).and.(j.le.inb(ij)))then ad(ij)=ad(ij)+ment(ij,j,k) endif 1320 continue 1330 continue 1340 continue c do 1350 ij=1,ncum if(i.le.inb(ij))then dpinv=0.01/(ph(ij,i)-ph(ij,i+1)) cpinv=1.0/cpn(ij,i) c ft(ij,i)=ft(ij,i) & +g*dpinv*(amp1(ij)*(t(ij,i+1)-t(ij,i) & +(gz(ij,i+1)-gz(ij,i))*cpinv) & -ad(ij)*(t(ij,i)-t(ij,i-1)+(gz(ij,i)-gz(ij,i-1))*cpinv)) & -sigd*lvcp(ij,i)*evap(ij,i) ft(ij,i)=ft(ij,i)+g*dpinv*ment(ij,i,i)*(hp(ij,i)-h(ij,i)+ & t(ij,i)*(cpv-cpd)*(q(ij,i)-qent(ij,i,i)))*cpinv ft(ij,i)=ft(ij,i)+sigd*wt(ij,i+1)*(cl-cpd)*water(ij,i+1)* & (t(ij,i+1)-t(ij,i))*dpinv*cpinv fq(ij,i)=fq(ij,i)+g*dpinv*(amp1(ij)*(q(ij,i+1)-q(ij,i))- & ad(ij)*(q(ij,i)-q(ij,i-1))) fu(ij,i)=fu(ij,i)+g*dpinv*(amp1(ij)*(u(ij,i+1)-u(ij,i))- & ad(ij)*(u(ij,i)-u(ij,i-1))) fv(ij,i)=fv(ij,i)+g*dpinv*(amp1(ij)*(v(ij,i+1)-v(ij,i))- & ad(ij)*(v(ij,i)-v(ij,i-1))) endif 1350 continue do 1370 k=1,i-1 do 1360 ij=1,ncum if(i.le.inb(ij))then awat=elij(ij,k,i)-(1.-ep(ij,i))*clw(ij,i) awat=max(awat,0.0) fq(ij,i)=fq(ij,i) & +g*dpinv*ment(ij,k,i)*(qent(ij,k,i)-awat-q(ij,i)) fu(ij,i)=fu(ij,i) & +g*dpinv*ment(ij,k,i)*(uent(ij,k,i)-u(ij,i)) fv(ij,i)=fv(ij,i) & +g*dpinv*ment(ij,k,i)*(vent(ij,k,i)-v(ij,i)) endif 1360 continue 1370 continue do 1390 k=i,nl+1 do 1380 ij=1,ncum if((i.le.inb(ij)).and.(k.le.inb(ij)))then fq(ij,i)=fq(ij,i) & +g*dpinv*ment(ij,k,i)*(qent(ij,k,i)-q(ij,i)) fu(ij,i)=fu(ij,i) & +g*dpinv*ment(ij,k,i)*(uent(ij,k,i)-u(ij,i)) fv(ij,i)=fv(ij,i) & +g*dpinv*ment(ij,k,i)*(vent(ij,k,i)-v(ij,i)) endif 1380 continue 1390 continue do 1400 ij=1,ncum if(i.le.inb(ij))then fq(ij,i)=fq(ij,i) & +sigd*evap(ij,i)+g*(mp(ij,i+1)* & (qp(ij,i+1)-q(ij,i)) & -mp(ij,i)*(qp(ij,i)-q(ij,i-1)))*dpinv fu(ij,i)=fu(ij,i) & +g*(mp(ij,i+1)*(up(ij,i+1)-u(ij,i))-mp(ij,i)* & (up(ij,i)-u(ij,i-1)))*dpinv fv(ij,i)=fv(ij,i) & +g*(mp(ij,i+1)*(vp(ij,i+1)-v(ij,i))-mp(ij,i)* & (vp(ij,i)-v(ij,i-1)))*dpinv endif 1400 continue 1500 continue c c *** Adjust tendencies at top of convection layer to reflect *** c *** actual position of the level zero cape *** c do 503 ij=1,ncum fqold=fq(ij,inb(ij)) fq(ij,inb(ij))=fq(ij,inb(ij))*(1.-frac(ij)) fq(ij,inb(ij)-1)=fq(ij,inb(ij)-1) & +frac(ij)*fqold*((ph(ij,inb(ij))-ph(ij,inb(ij)+1))/ 1 (ph(ij,inb(ij)-1)-ph(ij,inb(ij))))*lv(ij,inb(ij)) & /lv(ij,inb(ij)-1) ftold=ft(ij,inb(ij)) ft(ij,inb(ij))=ft(ij,inb(ij))*(1.-frac(ij)) ft(ij,inb(ij)-1)=ft(ij,inb(ij)-1) & +frac(ij)*ftold*((ph(ij,inb(ij))-ph(ij,inb(ij)+1))/ 1 (ph(ij,inb(ij)-1)-ph(ij,inb(ij))))*cpn(ij,inb(ij)) & /cpn(ij,inb(ij)-1) fuold=fu(ij,inb(ij)) fu(ij,inb(ij))=fu(ij,inb(ij))*(1.-frac(ij)) fu(ij,inb(ij)-1)=fu(ij,inb(ij)-1) & +frac(ij)*fuold*((ph(ij,inb(ij))-ph(ij,inb(ij)+1))/ 1 (ph(ij,inb(ij)-1)-ph(ij,inb(ij)))) fvold=fv(ij,inb(ij)) fv(ij,inb(ij))=fv(ij,inb(ij))*(1.-frac(ij)) fv(ij,inb(ij)-1)=fv(ij,inb(ij)-1) & +frac(ij)*fvold*((ph(ij,inb(ij))-ph(ij,inb(ij)+1))/ 1 (ph(ij,inb(ij)-1)-ph(ij,inb(ij)))) 503 continue c c *** Very slightly adjust tendencies to force exact *** c *** enthalpy, momentum and tracer conservation *** c do 682 ij=1,ncum ents(ij)=0.0 uav(ij)=0.0 vav(ij)=0.0 do 681 i=1,inb(ij) ents(ij)=ents(ij) & +(cpn(ij,i)*ft(ij,i)+lv(ij,i)*fq(ij,i))*(ph(ij,i)-ph(ij,i+1)) uav(ij)=uav(ij)+fu(ij,i)*(ph(ij,i)-ph(ij,i+1)) vav(ij)=vav(ij)+fv(ij,i)*(ph(ij,i)-ph(ij,i+1)) 681 continue 682 continue do 683 ij=1,ncum ents(ij)=ents(ij)/(ph(ij,1)-ph(ij,inb(ij)+1)) uav(ij)=uav(ij)/(ph(ij,1)-ph(ij,inb(ij)+1)) vav(ij)=vav(ij)/(ph(ij,1)-ph(ij,inb(ij)+1)) 683 continue do 642 ij=1,ncum do 641 i=1,inb(ij) ft(ij,i)=ft(ij,i)-ents(ij)/cpn(ij,i) fu(ij,i)=(1.-cu)*(fu(ij,i)-uav(ij)) fv(ij,i)=(1.-cu)*(fv(ij,i)-vav(ij)) 641 continue 642 continue c do 1810 k=1,nl+1 do 1800 i=1,ncum if((q(i,k)+delt*fq(i,k)).lt.0.0)iflag(i)=10 1800 continue 1810 continue c c do 1900 i=1,ncum if(iflag(i).gt.2)then precip(i)=0.0 cbmf(i)=0.0 endif 1900 continue do 1920 k=1,nl do 1910 i=1,ncum if(iflag(i).gt.2)then ft(i,k)=0.0 fq(i,k)=0.0 fu(i,k)=0.0 fv(i,k)=0.0 endif 1910 continue 1920 continue do 2000 i=1,ncum precip1(idcum(i))=precip(i) cbmf1(idcum(i))=cbmf(i) iflag1(idcum(i))=iflag(i) 2000 continue do 2020 k=1,nl do 2010 i=1,ncum ft1(idcum(i),k)=ft(i,k) fq1(idcum(i),k)=fq(i,k) fu1(idcum(i),k)=fu(i,k) fv1(idcum(i),k)=fv(i,k) 2010 continue 2020 continue c DO k=1,nd DO i=1,len Ma(i,k) = 0. ENDDO ENDDO DO k=nl,1,-1 DO i=1,ncum Ma(i,k) = Ma(i,k+1)+m(i,k) ENDDO ENDDO c return end