! $Header$ SUBROUTINE conflx(dtime, pres_h, pres_f, t, q, con_t, con_q, pqhfl, w, d_t, & d_q, rain, snow, pmfu, pmfd, pen_u, pde_u, pen_d, pde_d, kcbot, kctop, & kdtop, pmflxr, pmflxs) USE dimphy USE yomcst_mod_h USE yoethf_mod_h IMPLICIT NONE ! ====================================================================== ! Auteur(s): Z.X. Li (LMD/CNRS) date: 19941014 ! Objet: Schema flux de masse pour la convection ! (schema de Tiedtke avec qqs modifications mineures) ! Dec.97: Prise en compte des modifications introduites par ! Olivier Boucher et Alexandre Armengaud pour melange ! et lessivage des traceurs passifs. ! ====================================================================== ! Entree: REAL dtime ! pas d'integration (s) REAL pres_h(klon, klev+1) ! pression half-level (Pa) REAL pres_f(klon, klev) ! pression full-level (Pa) REAL t(klon, klev) ! temperature (K) REAL q(klon, klev) ! humidite specifique (g/g) REAL w(klon, klev) ! vitesse verticale (Pa/s) REAL con_t(klon, klev) ! convergence de temperature (K/s) REAL con_q(klon, klev) ! convergence de l'eau vapeur (g/g/s) REAL pqhfl(klon) ! evaporation (negative vers haut) mm/s ! Sortie: REAL d_t(klon, klev) ! incrementation de temperature REAL d_q(klon, klev) ! incrementation d'humidite REAL pmfu(klon, klev) ! flux masse (kg/m2/s) panache ascendant REAL pmfd(klon, klev) ! flux masse (kg/m2/s) panache descendant REAL pen_u(klon, klev) REAL pen_d(klon, klev) REAL pde_u(klon, klev) REAL pde_d(klon, klev) REAL rain(klon) ! pluie (mm/s) REAL snow(klon) ! neige (mm/s) REAL pmflxr(klon, klev+1) REAL pmflxs(klon, klev+1) INTEGER kcbot(klon) ! niveau du bas de la convection INTEGER kctop(klon) ! niveau du haut de la convection INTEGER kdtop(klon) ! niveau du haut des downdrafts ! Local: REAL pt(klon, klev) REAL pq(klon, klev) REAL pqs(klon, klev) REAL pvervel(klon, klev) LOGICAL land(klon) REAL d_t_bis(klon, klev) REAL d_q_bis(klon, klev) REAL paprs(klon, klev+1) REAL paprsf(klon, klev) REAL zgeom(klon, klev) REAL zcvgq(klon, klev) REAL zcvgt(klon, klev) ! AA REAL zmfu(klon, klev) REAL zmfd(klon, klev) REAL zen_u(klon, klev) REAL zen_d(klon, klev) REAL zde_u(klon, klev) REAL zde_d(klon, klev) REAL zmflxr(klon, klev+1) REAL zmflxs(klon, klev+1) ! AA INTEGER i, k REAL zdelta, zqsat include "FCTTRE.h" ! initialiser les variables de sortie (pour securite) DO i = 1, klon rain(i) = 0.0 snow(i) = 0.0 kcbot(i) = 0 kctop(i) = 0 kdtop(i) = 0 END DO DO k = 1, klev DO i = 1, klon d_t(i, k) = 0.0 d_q(i, k) = 0.0 pmfu(i, k) = 0.0 pmfd(i, k) = 0.0 pen_u(i, k) = 0.0 pde_u(i, k) = 0.0 pen_d(i, k) = 0.0 pde_d(i, k) = 0.0 zmfu(i, k) = 0.0 zmfd(i, k) = 0.0 zen_u(i, k) = 0.0 zde_u(i, k) = 0.0 zen_d(i, k) = 0.0 zde_d(i, k) = 0.0 END DO END DO DO k = 1, klev + 1 DO i = 1, klon zmflxr(i, k) = 0.0 zmflxs(i, k) = 0.0 END DO END DO ! calculer la nature du sol (pour l'instant, ocean partout) DO i = 1, klon land(i) = .FALSE. END DO ! preparer les variables d'entree (attention: l'ordre des niveaux ! verticaux augmente du haut vers le bas) DO k = 1, klev DO i = 1, klon pt(i, k) = t(i, klev-k+1) pq(i, k) = q(i, klev-k+1) paprsf(i, k) = pres_f(i, klev-k+1) paprs(i, k) = pres_h(i, klev+1-k+1) pvervel(i, k) = w(i, klev+1-k) zcvgt(i, k) = con_t(i, klev-k+1) zcvgq(i, k) = con_q(i, klev-k+1) zdelta = max(0., sign(1.,rtt-pt(i,k))) zqsat = r2es*foeew(pt(i,k), zdelta)/paprsf(i, k) zqsat = min(0.5, zqsat) zqsat = zqsat/(1.-retv*zqsat) pqs(i, k) = zqsat END DO END DO DO i = 1, klon paprs(i, klev+1) = pres_h(i, 1) zgeom(i, klev) = rd*pt(i, klev)/(0.5*(paprs(i,klev+1)+paprsf(i, & klev)))*(paprs(i,klev+1)-paprsf(i,klev)) END DO DO k = klev - 1, 1, -1 DO i = 1, klon zgeom(i, k) = zgeom(i, k+1) + rd*0.5*(pt(i,k+1)+pt(i,k))/paprs(i, k+1)* & (paprsf(i,k+1)-paprsf(i,k)) END DO END DO ! appeler la routine principale CALL flxmain(dtime, pt, pq, pqs, pqhfl, paprsf, paprs, zgeom, land, zcvgt, & zcvgq, pvervel, rain, snow, kcbot, kctop, kdtop, zmfu, zmfd, zen_u, & zde_u, zen_d, zde_d, d_t_bis, d_q_bis, zmflxr, zmflxs) ! AA-------------------------------------------------------- ! AA rem : De la meme facon que l'on effectue le reindicage ! AA pour la temperature t et le champ q ! AA on reindice les flux necessaires a la convection ! AA des traceurs ! AA-------------------------------------------------------- DO k = 1, klev DO i = 1, klon d_q(i, klev+1-k) = dtime*d_q_bis(i, k) d_t(i, klev+1-k) = dtime*d_t_bis(i, k) END DO END DO DO i = 1, klon pmfu(i, 1) = 0. pmfd(i, 1) = 0. pen_d(i, 1) = 0. pde_d(i, 1) = 0. END DO DO k = 2, klev DO i = 1, klon pmfu(i, klev+2-k) = zmfu(i, k) pmfd(i, klev+2-k) = zmfd(i, k) END DO END DO DO k = 1, klev DO i = 1, klon pen_u(i, klev+1-k) = zen_u(i, k) pde_u(i, klev+1-k) = zde_u(i, k) END DO END DO DO k = 1, klev - 1 DO i = 1, klon pen_d(i, klev+1-k) = -zen_d(i, k+1) pde_d(i, klev+1-k) = -zde_d(i, k+1) END DO END DO DO k = 1, klev + 1 DO i = 1, klon pmflxr(i, klev+2-k) = zmflxr(i, k) pmflxs(i, klev+2-k) = zmflxs(i, k) END DO END DO RETURN END SUBROUTINE conflx ! -------------------------------------------------------------------- SUBROUTINE flxmain(pdtime, pten, pqen, pqsen, pqhfl, pap, paph, pgeo, ldland, & ptte, pqte, pvervel, prsfc, pssfc, kcbot, kctop, kdtop, & ! * ! ldcum, ktype, pmfu, pmfd, pen_u, pde_u, pen_d, pde_d, dt_con, dq_con, pmflxr, pmflxs) USE yoecumf_mod_h USE yoethf_mod_h USE dimphy USE yomcst_mod_h IMPLICIT NONE ! ------------------------------------------------------------------ ! ---------------------------------------------------------------- REAL pten(klon, klev), pqen(klon, klev), pqsen(klon, klev) REAL ptte(klon, klev) REAL pqte(klon, klev) REAL pvervel(klon, klev) REAL pgeo(klon, klev), pap(klon, klev), paph(klon, klev+1) REAL pqhfl(klon) REAL ptu(klon, klev), pqu(klon, klev), plu(klon, klev) REAL plude(klon, klev) REAL pmfu(klon, klev) REAL prsfc(klon), pssfc(klon) INTEGER kcbot(klon), kctop(klon), ktype(klon) LOGICAL ldland(klon), ldcum(klon) REAL ztenh(klon, klev), zqenh(klon, klev), zqsenh(klon, klev) REAL zgeoh(klon, klev) REAL zmfub(klon), zmfub1(klon) REAL zmfus(klon, klev), zmfuq(klon, klev), zmful(klon, klev) REAL zdmfup(klon, klev), zdpmel(klon, klev) REAL zentr(klon), zhcbase(klon) REAL zdqpbl(klon), zdqcv(klon), zdhpbl(klon) REAL zrfl(klon) REAL pmflxr(klon, klev+1) REAL pmflxs(klon, klev+1) INTEGER ilab(klon, klev), ictop0(klon) LOGICAL llo1 REAL dt_con(klon, klev), dq_con(klon, klev) REAL zmfmax, zdh REAL pdtime, zqumqe, zdqmin, zalvdcp, zhsat, zzz REAL zhhat, zpbmpt, zgam, zeps, zfac INTEGER i, k, ikb, itopm2, kcum REAL pen_u(klon, klev), pde_u(klon, klev) REAL pen_d(klon, klev), pde_d(klon, klev) REAL ptd(klon, klev), pqd(klon, klev), pmfd(klon, klev) REAL zmfds(klon, klev), zmfdq(klon, klev), zdmfdp(klon, klev) INTEGER kdtop(klon) LOGICAL lddraf(klon) ! --------------------------------------------------------------------- LOGICAL firstcal SAVE firstcal DATA firstcal/.TRUE./ !$OMP THREADPRIVATE(firstcal) ! --------------------------------------------------------------------- IF (firstcal) THEN CALL flxsetup firstcal = .FALSE. END IF ! --------------------------------------------------------------------- DO i = 1, klon ldcum(i) = .FALSE. END DO DO k = 1, klev DO i = 1, klon dt_con(i, k) = 0.0 dq_con(i, k) = 0.0 END DO END DO ! ---------------------------------------------------------------------- ! initialiser les variables et faire l'interpolation verticale ! ---------------------------------------------------------------------- CALL flxini(pten, pqen, pqsen, pgeo, paph, zgeoh, ztenh, zqenh, zqsenh, & ptu, pqu, ptd, pqd, pmfd, zmfds, zmfdq, zdmfdp, pmfu, zmfus, zmfuq, & zdmfup, zdpmel, plu, plude, ilab, pen_u, pde_u, pen_d, pde_d) ! --------------------------------------------------------------------- ! determiner les valeurs au niveau de base de la tour convective ! --------------------------------------------------------------------- CALL flxbase(ztenh, zqenh, zgeoh, paph, ptu, pqu, plu, ldcum, kcbot, ilab) ! --------------------------------------------------------------------- ! calculer la convergence totale de l'humidite et celle en provenance ! de la couche limite, plus precisement, la convergence integree entre ! le sol et la base de la convection. Cette derniere convergence est ! comparee avec l'evaporation obtenue dans la couche limite pour ! determiner le type de la convection ! --------------------------------------------------------------------- k = 1 DO i = 1, klon zdqcv(i) = pqte(i, k)*(paph(i,k+1)-paph(i,k)) zdhpbl(i) = 0.0 zdqpbl(i) = 0.0 END DO DO k = 2, klev DO i = 1, klon zdqcv(i) = zdqcv(i) + pqte(i, k)*(paph(i,k+1)-paph(i,k)) IF (k>=kcbot(i)) THEN zdqpbl(i) = zdqpbl(i) + pqte(i, k)*(paph(i,k+1)-paph(i,k)) zdhpbl(i) = zdhpbl(i) + (rcpd*ptte(i,k)+rlvtt*pqte(i,k))*(paph(i,k+1) & -paph(i,k)) END IF END DO END DO DO i = 1, klon ktype(i) = 2 IF (zdqcv(i)>max(0.,-1.5*pqhfl(i)*rg)) ktype(i) = 1 ! cc if (zdqcv(i).GT.MAX(0.,-1.1*pqhfl(i)*RG)) ktype(i) = 1 END DO ! --------------------------------------------------------------------- ! determiner le flux de masse entrant a travers la base. ! on ignore, pour l'instant, l'effet du panache descendant ! --------------------------------------------------------------------- DO i = 1, klon ikb = kcbot(i) zqumqe = pqu(i, ikb) + plu(i, ikb) - zqenh(i, ikb) zdqmin = max(0.01*zqenh(i,ikb), 1.E-10) IF (zdqpbl(i)>0. .AND. zqumqe>zdqmin .AND. ldcum(i)) THEN zmfub(i) = zdqpbl(i)/(rg*max(zqumqe,zdqmin)) ELSE zmfub(i) = 0.01 ldcum(i) = .FALSE. END IF IF (ktype(i)==2) THEN zdh = rcpd*(ptu(i,ikb)-ztenh(i,ikb)) + rlvtt*zqumqe zdh = rg*max(zdh, 1.0E5*zdqmin) IF (zdhpbl(i)>0. .AND. ldcum(i)) zmfub(i) = zdhpbl(i)/zdh END IF zmfmax = (paph(i,ikb)-paph(i,ikb-1))/(rg*pdtime) zmfub(i) = min(zmfub(i), zmfmax) zentr(i) = entrscv IF (ktype(i)==1) zentr(i) = entrpen END DO ! ----------------------------------------------------------------------- ! DETERMINE CLOUD ASCENT FOR ENTRAINING PLUME ! ----------------------------------------------------------------------- ! (A) calculer d'abord la hauteur "theorique" de la tour convective sans ! considerer l'entrainement ni le detrainement du panache, sachant ! ces derniers peuvent abaisser la hauteur theorique. DO i = 1, klon ikb = kcbot(i) zhcbase(i) = rcpd*ptu(i, ikb) + zgeoh(i, ikb) + rlvtt*pqu(i, ikb) ictop0(i) = kcbot(i) - 1 END DO zalvdcp = rlvtt/rcpd DO k = klev - 1, 3, -1 DO i = 1, klon zhsat = rcpd*ztenh(i, k) + zgeoh(i, k) + rlvtt*zqsenh(i, k) zgam = r5les*zalvdcp*zqsenh(i, k)/((1.-retv*zqsenh(i,k))*(ztenh(i, & k)-r4les)**2) zzz = rcpd*ztenh(i, k)*0.608 zhhat = zhsat - (zzz+zgam*zzz)/(1.+zgam*zzz/rlvtt)*max(zqsenh(i,k)- & zqenh(i,k), 0.) IF (kzhhat) ictop0(i) = k END DO END DO ! (B) calculer le panache ascendant CALL flxasc(pdtime, ztenh, zqenh, pten, pqen, pqsen, pgeo, zgeoh, pap, & paph, pqte, pvervel, ldland, ldcum, ktype, ilab, ptu, pqu, plu, pmfu, & zmfub, zentr, zmfus, zmfuq, zmful, plude, zdmfup, kcbot, kctop, ictop0, & kcum, pen_u, pde_u) IF (kcum==0) GO TO 1000 ! verifier l'epaisseur de la convection et changer eventuellement ! le taux d'entrainement/detrainement DO i = 1, klon zpbmpt = paph(i, kcbot(i)) - paph(i, kctop(i)) IF (ldcum(i) .AND. ktype(i)==1 .AND. zpbmpt<2.E4) ktype(i) = 2 IF (ldcum(i)) ictop0(i) = kctop(i) IF (ktype(i)==2) zentr(i) = entrscv END DO IF (lmfdd) THEN ! si l'on considere le panache descendant ! calculer la precipitation issue du panache ascendant pour ! determiner l'existence du panache descendant dans la convection DO i = 1, klon zrfl(i) = zdmfup(i, 1) END DO DO k = 2, klev DO i = 1, klon zrfl(i) = zrfl(i) + zdmfup(i, k) END DO END DO ! determiner le LFS (level of free sinking: niveau de plonge libre) CALL flxdlfs(ztenh, zqenh, zgeoh, paph, ptu, pqu, ldcum, kcbot, kctop, & zmfub, zrfl, ptd, pqd, pmfd, zmfds, zmfdq, zdmfdp, kdtop, lddraf) ! calculer le panache descendant CALL flxddraf(ztenh, zqenh, zgeoh, paph, zrfl, ptd, pqd, pmfd, zmfds, & zmfdq, zdmfdp, lddraf, pen_d, pde_d) ! calculer de nouveau le flux de masse entrant a travers la base ! de la convection, sachant qu'il a ete modifie par le panache ! descendant DO i = 1, klon IF (lddraf(i)) THEN ikb = kcbot(i) llo1 = pmfd(i, ikb) < 0. zeps = 0. IF (llo1) zeps = cmfdeps zqumqe = pqu(i, ikb) + plu(i, ikb) - zeps*pqd(i, ikb) - & (1.-zeps)*zqenh(i, ikb) zdqmin = max(0.01*zqenh(i,ikb), 1.E-10) zmfmax = (paph(i,ikb)-paph(i,ikb-1))/(rg*pdtime) IF (zdqpbl(i)>0. .AND. zqumqe>zdqmin .AND. ldcum(i) .AND. & zmfub(i)0. .AND. ldcum(i)) zmfub1(i) = zdhpbl(i)/zdh END IF IF (.NOT. ((ktype(i)==1 .OR. ktype(i)==2) .AND. abs(zmfub1(i)-zmfub(i & ))<0.2*zmfub(i))) zmfub1(i) = zmfub(i) END IF END DO DO k = 1, klev DO i = 1, klon IF (lddraf(i)) THEN zfac = zmfub1(i)/max(zmfub(i), 1.E-10) pmfd(i, k) = pmfd(i, k)*zfac zmfds(i, k) = zmfds(i, k)*zfac zmfdq(i, k) = zmfdq(i, k)*zfac zdmfdp(i, k) = zdmfdp(i, k)*zfac pen_d(i, k) = pen_d(i, k)*zfac pde_d(i, k) = pde_d(i, k)*zfac END IF END DO END DO DO i = 1, klon IF (lddraf(i)) zmfub(i) = zmfub1(i) END DO END IF ! fin de test sur lmfdd ! ----------------------------------------------------------------------- ! calculer de nouveau le panache ascendant ! ----------------------------------------------------------------------- CALL flxasc(pdtime, ztenh, zqenh, pten, pqen, pqsen, pgeo, zgeoh, pap, & paph, pqte, pvervel, ldland, ldcum, ktype, ilab, ptu, pqu, plu, pmfu, & zmfub, zentr, zmfus, zmfuq, zmful, plude, zdmfup, kcbot, kctop, ictop0, & kcum, pen_u, pde_u) ! ----------------------------------------------------------------------- ! determiner les flux convectifs en forme finale, ainsi que ! la quantite des precipitations ! ----------------------------------------------------------------------- CALL flxflux(pdtime, pqen, pqsen, ztenh, zqenh, pap, paph, ldland, zgeoh, & kcbot, kctop, lddraf, kdtop, ktype, ldcum, pmfu, pmfd, zmfus, zmfds, & zmfuq, zmfdq, zmful, plude, zdmfup, zdmfdp, pten, prsfc, pssfc, zdpmel, & itopm2, pmflxr, pmflxs) ! ---------------------------------------------------------------------- ! calculer les tendances pour T et Q ! ---------------------------------------------------------------------- CALL flxdtdq(pdtime, itopm2, paph, ldcum, pten, zmfus, zmfds, zmfuq, zmfdq, & zmful, zdmfup, zdmfdp, zdpmel, dt_con, dq_con) 1000 CONTINUE RETURN END SUBROUTINE flxmain SUBROUTINE flxini(pten, pqen, pqsen, pgeo, paph, pgeoh, ptenh, pqenh, pqsenh, & ptu, pqu, ptd, pqd, pmfd, pmfds, pmfdq, pdmfdp, pmfu, pmfus, pmfuq, & pdmfup, pdpmel, plu, plude, klab, pen_u, pde_u, pen_d, pde_d) USE dimphy USE yomcst_mod_h USE yoethf_mod_h IMPLICIT NONE ! ---------------------------------------------------------------------- ! THIS ROUTINE INTERPOLATES LARGE-SCALE FIELDS OF T,Q ETC. ! TO HALF LEVELS (I.E. GRID FOR MASSFLUX SCHEME), ! AND INITIALIZES VALUES FOR UPDRAFTS ! ---------------------------------------------------------------------- REAL pten(klon, klev) ! temperature (environnement) REAL pqen(klon, klev) ! humidite (environnement) REAL pqsen(klon, klev) ! humidite saturante (environnement) REAL pgeo(klon, klev) ! geopotentiel (g * metre) REAL pgeoh(klon, klev) ! geopotentiel aux demi-niveaux REAL paph(klon, klev+1) ! pression aux demi-niveaux REAL ptenh(klon, klev) ! temperature aux demi-niveaux REAL pqenh(klon, klev) ! humidite aux demi-niveaux REAL pqsenh(klon, klev) ! humidite saturante aux demi-niveaux REAL ptu(klon, klev) ! temperature du panache ascendant (p-a) REAL pqu(klon, klev) ! humidite du p-a REAL plu(klon, klev) ! eau liquide du p-a REAL pmfu(klon, klev) ! flux de masse du p-a REAL pmfus(klon, klev) ! flux de l'energie seche dans le p-a REAL pmfuq(klon, klev) ! flux de l'humidite dans le p-a REAL pdmfup(klon, klev) ! quantite de l'eau precipitee dans p-a REAL plude(klon, klev) ! quantite de l'eau liquide jetee du ! p-a a l'environnement REAL pdpmel(klon, klev) ! quantite de neige fondue REAL ptd(klon, klev) ! temperature du panache descendant (p-d) REAL pqd(klon, klev) ! humidite du p-d REAL pmfd(klon, klev) ! flux de masse du p-d REAL pmfds(klon, klev) ! flux de l'energie seche dans le p-d REAL pmfdq(klon, klev) ! flux de l'humidite dans le p-d REAL pdmfdp(klon, klev) ! quantite de precipitation dans p-d REAL pen_u(klon, klev) ! quantite de masse entrainee pour p-a REAL pde_u(klon, klev) ! quantite de masse detrainee pour p-a REAL pen_d(klon, klev) ! quantite de masse entrainee pour p-d REAL pde_d(klon, klev) ! quantite de masse detrainee pour p-d INTEGER klab(klon, klev) LOGICAL llflag(klon) INTEGER k, i, icall REAL zzs ! ---------------------------------------------------------------------- ! SPECIFY LARGE SCALE PARAMETERS AT HALF LEVELS ! ADJUST TEMPERATURE FIELDS IF STATICLY UNSTABLE ! ---------------------------------------------------------------------- DO k = 2, klev DO i = 1, klon pgeoh(i, k) = pgeo(i, k) + (pgeo(i,k-1)-pgeo(i,k))*0.5 ptenh(i, k) = (max(rcpd*pten(i,k-1)+pgeo(i,k-1),rcpd*pten(i,k)+pgeo(i, & k))-pgeoh(i,k))/rcpd pqsenh(i, k) = pqsen(i, k-1) llflag(i) = .TRUE. END DO icall = 0 CALL flxadjtq(paph(1,k), ptenh(1,k), pqsenh(1,k), llflag, icall) DO i = 1, klon pqenh(i, k) = min(pqen(i,k-1), pqsen(i,k-1)) + & (pqsenh(i,k)-pqsen(i,k-1)) pqenh(i, k) = max(pqenh(i,k), 0.) END DO END DO DO i = 1, klon ptenh(i, klev) = (rcpd*pten(i,klev)+pgeo(i,klev)-pgeoh(i,klev))/rcpd pqenh(i, klev) = pqen(i, klev) ptenh(i, 1) = pten(i, 1) pqenh(i, 1) = pqen(i, 1) pgeoh(i, 1) = pgeo(i, 1) END DO DO k = klev - 1, 2, -1 DO i = 1, klon zzs = max(rcpd*ptenh(i,k)+pgeoh(i,k), rcpd*ptenh(i,k+1)+pgeoh(i,k+1)) ptenh(i, k) = (zzs-pgeoh(i,k))/rcpd END DO END DO ! ----------------------------------------------------------------------- ! INITIALIZE VALUES FOR UPDRAFTS AND DOWNDRAFTS ! ----------------------------------------------------------------------- DO k = 1, klev DO i = 1, klon ptu(i, k) = ptenh(i, k) pqu(i, k) = pqenh(i, k) plu(i, k) = 0. pmfu(i, k) = 0. pmfus(i, k) = 0. pmfuq(i, k) = 0. pdmfup(i, k) = 0. pdpmel(i, k) = 0. plude(i, k) = 0. klab(i, k) = 0 ptd(i, k) = ptenh(i, k) pqd(i, k) = pqenh(i, k) pmfd(i, k) = 0.0 pmfds(i, k) = 0.0 pmfdq(i, k) = 0.0 pdmfdp(i, k) = 0.0 pen_u(i, k) = 0.0 pde_u(i, k) = 0.0 pen_d(i, k) = 0.0 pde_d(i, k) = 0.0 END DO END DO RETURN END SUBROUTINE flxini SUBROUTINE flxbase(ptenh, pqenh, pgeoh, paph, ptu, pqu, plu, ldcum, kcbot, & klab) USE dimphy USE yomcst_mod_h USE yoethf_mod_h IMPLICIT NONE ! ---------------------------------------------------------------------- ! THIS ROUTINE CALCULATES CLOUD BASE VALUES (T AND Q) ! INPUT ARE ENVIRONM. VALUES OF T,Q,P,PHI AT HALF LEVELS. ! IT RETURNS CLOUD BASE VALUES AND FLAGS AS FOLLOWS; ! klab=1 FOR SUBCLOUD LEVELS ! klab=2 FOR CONDENSATION LEVEL ! LIFT SURFACE AIR DRY-ADIABATICALLY TO CLOUD BASE ! (NON ENTRAINING PLUME,I.E.CONSTANT MASSFLUX) ! ---------------------------------------------------------------------- REAL ptenh(klon, klev), pqenh(klon, klev) REAL pgeoh(klon, klev), paph(klon, klev+1) REAL ptu(klon, klev), pqu(klon, klev), plu(klon, klev) INTEGER klab(klon, klev), kcbot(klon) LOGICAL llflag(klon), ldcum(klon) INTEGER i, k, icall, is REAL zbuo, zqold(klon) ! ---------------------------------------------------------------------- ! INITIALIZE VALUES AT LIFTING LEVEL ! ---------------------------------------------------------------------- DO i = 1, klon klab(i, klev) = 1 kcbot(i) = klev - 1 ldcum(i) = .FALSE. END DO ! ---------------------------------------------------------------------- ! DO ASCENT IN SUBCLOUD LAYER, ! CHECK FOR EXISTENCE OF CONDENSATION LEVEL, ! ADJUST T,Q AND L ACCORDINGLY ! CHECK FOR BUOYANCY AND SET FLAGS ! ---------------------------------------------------------------------- DO k = klev - 1, 2, -1 is = 0 DO i = 1, klon IF (klab(i,k+1)==1) is = is + 1 llflag(i) = .FALSE. IF (klab(i,k+1)==1) llflag(i) = .TRUE. END DO IF (is==0) GO TO 290 DO i = 1, klon IF (llflag(i)) THEN pqu(i, k) = pqu(i, k+1) ptu(i, k) = ptu(i, k+1) + (pgeoh(i,k+1)-pgeoh(i,k))/rcpd zbuo = ptu(i, k)*(1.+retv*pqu(i,k)) - ptenh(i, k)*(1.+retv*pqenh(i,k) & ) + 0.5 IF (zbuo>0.) klab(i, k) = 1 zqold(i) = pqu(i, k) END IF END DO icall = 1 CALL flxadjtq(paph(1,k), ptu(1,k), pqu(1,k), llflag, icall) DO i = 1, klon IF (llflag(i) .AND. pqu(i,k)/=zqold(i)) THEN klab(i, k) = 2 plu(i, k) = plu(i, k) + zqold(i) - pqu(i, k) zbuo = ptu(i, k)*(1.+retv*pqu(i,k)) - ptenh(i, k)*(1.+retv*pqenh(i,k) & ) + 0.5 IF (zbuo>0.) kcbot(i) = k IF (zbuo>0.) ldcum(i) = .TRUE. END IF END DO 290 END DO RETURN END SUBROUTINE flxbase SUBROUTINE flxasc(pdtime, ptenh, pqenh, pten, pqen, pqsen, pgeo, pgeoh, pap, & paph, pqte, pvervel, ldland, ldcum, ktype, klab, ptu, pqu, plu, pmfu, & pmfub, pentr, pmfus, pmfuq, pmful, plude, pdmfup, kcbot, kctop, kctop0, & kcum, pen_u, pde_u) USE yoecumf_mod_h USE yoethf_mod_h USE dimphy USE yomcst_mod_h IMPLICIT NONE ! ---------------------------------------------------------------------- ! THIS ROUTINE DOES THE CALCULATIONS FOR CLOUD ASCENTS ! FOR CUMULUS PARAMETERIZATION ! ---------------------------------------------------------------------- REAL pdtime REAL pten(klon, klev), ptenh(klon, klev) REAL pqen(klon, klev), pqenh(klon, klev), pqsen(klon, klev) REAL pgeo(klon, klev), pgeoh(klon, klev) REAL pap(klon, klev), paph(klon, klev+1) REAL pqte(klon, klev) REAL pvervel(klon, klev) ! vitesse verticale en Pa/s REAL pmfub(klon), pentr(klon) REAL ptu(klon, klev), pqu(klon, klev), plu(klon, klev) REAL plude(klon, klev) REAL pmfu(klon, klev), pmfus(klon, klev) REAL pmfuq(klon, klev), pmful(klon, klev) REAL pdmfup(klon, klev) INTEGER ktype(klon), klab(klon, klev), kcbot(klon), kctop(klon) INTEGER kctop0(klon) LOGICAL ldland(klon), ldcum(klon) REAL pen_u(klon, klev), pde_u(klon, klev) REAL zqold(klon) REAL zdland(klon) LOGICAL llflag(klon) INTEGER k, i, is, icall, kcum REAL ztglace, zdphi, zqeen, zseen, zscde, zqude REAL zmfusk, zmfuqk, zmfulk, zbuo, zdnoprc, zprcon, zlnew REAL zpbot(klon), zptop(klon), zrho(klon) REAL zdprho, zentr, zpmid, zmftest, zmfmax LOGICAL llo1, llo2 REAL zwmax(klon), zzzmb INTEGER klwmin(klon) ! level of maximum vertical velocity REAL fact ! ---------------------------------------------------------------------- ztglace = rtt - 13. ! Chercher le niveau ou la vitesse verticale est maximale: DO i = 1, klon klwmin(i) = klev zwmax(i) = 0.0 END DO DO k = klev, 3, -1 DO i = 1, klon IF (pvervel(i,k)=ztglace) zdland(i) = zdphi zdland(i) = max(3.0E4, zdland(i)) zdland(i) = min(5.0E4, zdland(i)) END IF END DO ! Initialiser les valeurs au niveau d'ascendance DO i = 1, klon kctop(i) = klev - 1 IF (.NOT. ldcum(i)) THEN kcbot(i) = klev - 1 pmfub(i) = 0. pqu(i, klev) = 0. END IF pmfu(i, klev) = pmfub(i) pmfus(i, klev) = pmfub(i)*(rcpd*ptu(i,klev)+pgeoh(i,klev)) pmfuq(i, klev) = pmfub(i)*pqu(i, klev) END DO DO i = 1, klon ldcum(i) = .FALSE. END DO ! ---------------------------------------------------------------------- ! DO ASCENT: SUBCLOUD LAYER (klab=1) ,CLOUDS (klab=2) ! BY DOING FIRST DRY-ADIABATIC ASCENT AND THEN ! BY ADJUSTING T,Q AND L ACCORDINGLY IN *flxadjtq*, ! THEN CHECK FOR BUOYANCY AND SET FLAGS ACCORDINGLY ! ---------------------------------------------------------------------- DO k = klev - 1, 3, -1 IF (lmfmid .AND. k0.9*pqsen(i,k) .AND. pap(i,k)/paph(i,klev+1)>0.4) THEN ptu(i, k+1) = pten(i, k) + (pgeo(i,k)-pgeoh(i,k+1))/rcpd pqu(i, k+1) = pqen(i, k) plu(i, k+1) = 0.0 zzzmb = max(cmfcmin, -pvervel(i,k)/rg) zmfmax = (paph(i,k)-paph(i,k-1))/(rg*pdtime) pmfub(i) = min(zzzmb, zmfmax) pmfu(i, k+1) = pmfub(i) pmfus(i, k+1) = pmfub(i)*(rcpd*ptu(i,k+1)+pgeoh(i,k+1)) pmfuq(i, k+1) = pmfub(i)*pqu(i, k+1) pmful(i, k+1) = 0.0 pdmfup(i, k+1) = 0.0 kcbot(i) = k klab(i, k+1) = 1 ktype(i) = 3 pentr(i) = entrmid END IF END DO END IF is = 0 DO i = 1, klon is = is + klab(i, k+1) IF (klab(i,k+1)==0) klab(i, k) = 0 llflag(i) = .FALSE. IF (klab(i,k+1)>0) llflag(i) = .TRUE. END DO IF (is==0) GO TO 480 ! calculer le taux d'entrainement et de detrainement DO i = 1, klon pen_u(i, k) = 0.0 pde_u(i, k) = 0.0 zrho(i) = paph(i, k+1)/(rd*ptenh(i,k+1)) zpbot(i) = paph(i, kcbot(i)) zptop(i) = paph(i, kctop0(i)) END DO DO i = 1, klon IF (ldcum(i)) THEN zdprho = (paph(i,k+1)-paph(i,k))/(rg*zrho(i)) zentr = pentr(i)*pmfu(i, k+1)*zdprho llo1 = k < kcbot(i) IF (llo1) pde_u(i, k) = zentr zpmid = 0.5*(zpbot(i)+zptop(i)) llo2 = llo1 .AND. ktype(i) == 2 .AND. (zpbot(i)-paph(i,k)<0.2E5 .OR. & paph(i,k)>zpmid) IF (llo2) pen_u(i, k) = zentr llo2 = llo1 .AND. (ktype(i)==1 .OR. ktype(i)==3) .AND. & (k>=max(klwmin(i),kctop0(i)+2) .OR. pap(i,k)>zpmid) IF (llo2) pen_u(i, k) = zentr llo1 = pen_u(i, k) > 0. .AND. (ktype(i)==1 .OR. ktype(i)==2) IF (llo1) THEN fact = 1. + 3.*(1.-min(1.,(zpbot(i)-pap(i,k))/1.5E4)) zentr = zentr*fact pen_u(i, k) = pen_u(i, k)*fact pde_u(i, k) = pde_u(i, k)*fact END IF IF (llo2 .AND. pqenh(i,k+1)>1.E-5) pen_u(i, k) = zentr + & max(pqte(i,k), 0.)/pqenh(i, k+1)*zrho(i)*zdprho END IF END DO ! ---------------------------------------------------------------------- ! DO ADIABATIC ASCENT FOR ENTRAINING/DETRAINING PLUME ! ---------------------------------------------------------------------- DO i = 1, klon IF (llflag(i)) THEN IF (k0. .AND. pmfu(i,k)>=0.1*pmfub(i)) THEN kctop(i) = k ldcum(i) = .TRUE. zdnoprc = 1.5E4 IF (ldland(i)) zdnoprc = zdland(i) zprcon = cprcon IF ((zpbot(i)-paph(i,k))=kctop(i)-1) THEN pmfus(i, k) = pmfus(i, k) - pmfu(i, k)*(rcpd*ptenh(i,k)+pgeoh(i,k)) pmfuq(i, k) = pmfuq(i, k) - pmfu(i, k)*pqenh(i, k) zdp = 1.5E4 IF (ldland(i)) zdp = 3.E4 ! l'eau liquide detrainee est precipitee quand certaines ! conditions sont reunies (sinon, elle est consideree ! evaporee dans l'environnement) IF (paph(i,kcbot(i))-paph(i,kctop(i))>=zdp .AND. pqen(i,k-1)>0.8* & pqsen(i,k-1)) pdmfup(i, k-1) = pdmfup(i, k-1) + plude(i, k-1) IF (lddraf(i) .AND. k>=kdtop(i)) THEN pmfds(i, k) = pmfds(i, k) - pmfd(i, k)*(rcpd*ptenh(i,k)+pgeoh(i,k)) pmfdq(i, k) = pmfdq(i, k) - pmfd(i, k)*pqenh(i, k) ELSE pmfd(i, k) = 0. pmfds(i, k) = 0. pmfdq(i, k) = 0. pdmfdp(i, k-1) = 0. END IF ELSE pmfu(i, k) = 0. pmfus(i, k) = 0. pmfuq(i, k) = 0. pmful(i, k) = 0. pdmfup(i, k-1) = 0. plude(i, k-1) = 0. pmfd(i, k) = 0. pmfds(i, k) = 0. pmfdq(i, k) = 0. pdmfdp(i, k-1) = 0. END IF END DO END DO DO k = ktopm2, klev DO i = 1, klon IF (ldcum(i) .AND. k>kcbot(i)) THEN ikb = kcbot(i) zzp = ((paph(i,klev+1)-paph(i,k))/(paph(i,klev+1)-paph(i,ikb))) IF (ktype(i)==3) zzp = zzp**2 pmfu(i, k) = pmfu(i, ikb)*zzp pmfus(i, k) = pmfus(i, ikb)*zzp pmfuq(i, k) = pmfuq(i, ikb)*zzp pmful(i, k) = pmful(i, ikb)*zzp END IF END DO END DO ! CALCULATE RAIN/SNOW FALL RATES ! CALCULATE MELTING OF SNOW ! CALCULATE EVAPORATION OF PRECIP DO k = 1, klev + 1 DO i = 1, klon pmflxr(i, k) = 0.0 pmflxs(i, k) = 0.0 END DO END DO DO k = ktopm2, klev DO i = 1, klon IF (ldcum(i)) THEN IF (pmflxs(i,k)>0.0 .AND. pten(i,k)>ztmelp2) THEN zfac = zcons1*(paph(i,k+1)-paph(i,k)) zsnmlt = min(pmflxs(i,k), zfac*(pten(i,k)-ztmelp2)) pdpmel(i, k) = zsnmlt ztmsmlt = pten(i, k) - zsnmlt/zfac zdelta = max(0., sign(1.,rtt-ztmsmlt)) zqsat = r2es*foeew(ztmsmlt, zdelta)/pap(i, k) zqsat = min(0.5, zqsat) zqsat = zqsat/(1.-retv*zqsat) pqsen(i, k) = zqsat END IF IF (pten(i,k)>rtt) THEN pmflxr(i, k+1) = pmflxr(i, k) + pdmfup(i, k) + pdmfdp(i, k) + & pdpmel(i, k) pmflxs(i, k+1) = pmflxs(i, k) - pdpmel(i, k) ELSE pmflxs(i, k+1) = pmflxs(i, k) + pdmfup(i, k) + pdmfdp(i, k) pmflxr(i, k+1) = pmflxr(i, k) END IF ! si la precipitation est negative, on ajuste le plux du ! panache descendant pour eliminer la negativite IF ((pmflxr(i,k+1)+pmflxs(i,k+1))<0.0) THEN pdmfdp(i, k) = -pmflxr(i, k) - pmflxs(i, k) - pdmfup(i, k) pmflxr(i, k+1) = 0.0 pmflxs(i, k+1) = 0.0 pdpmel(i, k) = 0.0 END IF END IF END DO END DO ! jq The new variable is initialized here. ! jq It contains the humidity which is fed to the downdraft ! jq by evaporation of precipitation in the column below the base ! jq of convection. ! jq ! jq In the former version, this term has been subtracted from precip ! jq as well as the evaporation. ! jq DO k = 1, klev DO i = 1, klon maxpdmfdp(i, k) = 0.0 END DO END DO DO k = 1, klev DO kp = k, klev DO i = 1, klon maxpdmfdp(i, k) = maxpdmfdp(i, k) + pdmfdp(i, kp) END DO END DO END DO ! jq End of initialization DO k = ktopm2, klev DO i = 1, klon IF (ldcum(i) .AND. k>=kcbot(i)) THEN zrfl = pmflxr(i, k) + pmflxs(i, k) IF (zrfl>1.0E-20) THEN zrnew = (max(0.,sqrt(zrfl/zcucov)-cevapcu(i, & k)*(paph(i,k+1)-paph(i,k))*max(0.,pqsen(i,k)-pqen(i,k))))**2* & zcucov zrmin = zrfl - zcucov*max(0., 0.8*pqsen(i,k)-pqen(i,k))*zcons2*( & paph(i,k+1)-paph(i,k)) zrnew = max(zrnew, zrmin) zrfln = max(zrnew, 0.) zdrfl = min(0., zrfln-zrfl) ! jq At least the amount of precipiation needed to feed the ! downdraft ! jq with humidity below the base of convection has to be left and ! can't ! jq be evaporated (surely the evaporation can't be positive): zdrfl = max(zdrfl, min(-pmflxr(i,k)-pmflxs(i,k)-maxpdmfdp(i, & k),0.0)) ! jq End of insertion zdenom = 1.0/max(1.0E-20, pmflxr(i,k)+pmflxs(i,k)) IF (pten(i,k)>rtt) THEN zpdr = pdmfdp(i, k) zpds = 0.0 ELSE zpdr = 0.0 zpds = pdmfdp(i, k) END IF pmflxr(i, k+1) = pmflxr(i, k) + zpdr + pdpmel(i, k) + & zdrfl*pmflxr(i, k)*zdenom pmflxs(i, k+1) = pmflxs(i, k) + zpds - pdpmel(i, k) + & zdrfl*pmflxs(i, k)*zdenom pdmfup(i, k) = pdmfup(i, k) + zdrfl ELSE pmflxr(i, k+1) = 0.0 pmflxs(i, k+1) = 0.0 pdmfdp(i, k) = 0.0 pdpmel(i, k) = 0.0 END IF IF (pmflxr(i,k)+pmflxs(i,k)<-1.E-26 .AND. prt_level>=1) WRITE (*, *) & 'precip. < 1e-16 ', pmflxr(i, k) + pmflxs(i, k) END IF END DO END DO DO i = 1, klon prfl(i) = pmflxr(i, klev+1) psfl(i) = pmflxs(i, klev+1) END DO RETURN END SUBROUTINE flxflux SUBROUTINE flxdtdq(pdtime, ktopm2, paph, ldcum, pten, pmfus, pmfds, pmfuq, & pmfdq, pmful, pdmfup, pdmfdp, pdpmel, dt_con, dq_con) USE yoecumf_mod_h USE yoethf_mod_h USE dimphy USE yomcst_mod_h IMPLICIT NONE ! ---------------------------------------------------------------------- ! calculer les tendances T et Q ! ---------------------------------------------------------------------- ! ----------------------------------------------------------------- LOGICAL llo1 REAL pten(klon, klev), paph(klon, klev+1) REAL pmfus(klon, klev), pmfuq(klon, klev), pmful(klon, klev) REAL pmfds(klon, klev), pmfdq(klon, klev) REAL pdmfup(klon, klev) REAL pdmfdp(klon, klev) REAL pdpmel(klon, klev) LOGICAL ldcum(klon) REAL dt_con(klon, klev), dq_con(klon, klev) INTEGER ktopm2 REAL pdtime INTEGER i, k REAL zalv, zdtdt, zdqdt DO k = ktopm2, klev - 1 DO i = 1, klon IF (ldcum(i)) THEN llo1 = (pten(i,k)-rtt) > 0. zalv = rlstt IF (llo1) zalv = rlvtt zdtdt = rg/(paph(i,k+1)-paph(i,k))/rcpd*(pmfus(i,k+1)-pmfus(i,k)+ & pmfds(i,k+1)-pmfds(i,k)-rlmlt*pdpmel(i,k)-zalv*(pmful(i, & k+1)-pmful(i,k)-pdmfup(i,k)-pdmfdp(i,k))) dt_con(i, k) = zdtdt zdqdt = rg/(paph(i,k+1)-paph(i,k))*(pmfuq(i,k+1)-pmfuq(i,k)+pmfdq(i,k & +1)-pmfdq(i,k)+pmful(i,k+1)-pmful(i,k)-pdmfup(i,k)-pdmfdp(i,k)) dq_con(i, k) = zdqdt END IF END DO END DO k = klev DO i = 1, klon IF (ldcum(i)) THEN llo1 = (pten(i,k)-rtt) > 0. zalv = rlstt IF (llo1) zalv = rlvtt zdtdt = -rg/(paph(i,k+1)-paph(i,k))/rcpd*(pmfus(i,k)+pmfds(i,k)+rlmlt* & pdpmel(i,k)-zalv*(pmful(i,k)+pdmfup(i,k)+pdmfdp(i,k))) dt_con(i, k) = zdtdt zdqdt = -rg/(paph(i,k+1)-paph(i,k))*(pmfuq(i,k)+pmfdq(i,k)+pmful(i,k)+ & pdmfup(i,k)+pdmfdp(i,k)) dq_con(i, k) = zdqdt END IF END DO RETURN END SUBROUTINE flxdtdq SUBROUTINE flxdlfs(ptenh, pqenh, pgeoh, paph, ptu, pqu, ldcum, kcbot, kctop, & pmfub, prfl, ptd, pqd, pmfd, pmfds, pmfdq, pdmfdp, kdtop, lddraf) USE yoecumf_mod_h USE yoethf_mod_h USE dimphy USE yomcst_mod_h IMPLICIT NONE ! ---------------------------------------------------------------------- ! THIS ROUTINE CALCULATES LEVEL OF FREE SINKING FOR ! CUMULUS DOWNDRAFTS AND SPECIFIES T,Q,U AND V VALUES ! TO PRODUCE LFS-VALUES FOR CUMULUS DOWNDRAFTS ! FOR MASSFLUX CUMULUS PARAMETERIZATION ! INPUT ARE ENVIRONMENTAL VALUES OF T,Q,U,V,P,PHI ! AND UPDRAFT VALUES T,Q,U AND V AND ALSO ! CLOUD BASE MASSFLUX AND CU-PRECIPITATION RATE. ! IT RETURNS T,Q,U AND V VALUES AND MASSFLUX AT LFS. ! CHECK FOR NEGATIVE BUOYANCY OF AIR OF EQUAL PARTS OF ! MOIST ENVIRONMENTAL AIR AND CLOUD AIR. ! ---------------------------------------------------------------------- REAL ptenh(klon, klev) REAL pqenh(klon, klev) REAL pgeoh(klon, klev), paph(klon, klev+1) REAL ptu(klon, klev), pqu(klon, klev) REAL pmfub(klon) REAL prfl(klon) REAL ptd(klon, klev), pqd(klon, klev) REAL pmfd(klon, klev), pmfds(klon, klev), pmfdq(klon, klev) REAL pdmfdp(klon, klev) INTEGER kcbot(klon), kctop(klon), kdtop(klon) LOGICAL ldcum(klon), lddraf(klon) REAL ztenwb(klon, klev), zqenwb(klon, klev), zcond(klon) REAL zttest, zqtest, zbuo, zmftop LOGICAL llo2(klon) INTEGER i, k, is, icall ! ---------------------------------------------------------------------- DO i = 1, klon lddraf(i) = .FALSE. kdtop(i) = klev + 1 END DO ! ---------------------------------------------------------------------- ! DETERMINE LEVEL OF FREE SINKING BY ! DOING A SCAN FROM TOP TO BASE OF CUMULUS CLOUDS ! FOR EVERY POINT AND PROCEED AS FOLLOWS: ! (1) DETEMINE WET BULB ENVIRONMENTAL T AND Q ! (2) DO MIXING WITH CUMULUS CLOUD AIR ! (3) CHECK FOR NEGATIVE BUOYANCY ! THE ASSUMPTION IS THAT AIR OF DOWNDRAFTS IS MIXTURE ! OF 50% CLOUD AIR + 50% ENVIRONMENTAL AIR AT WET BULB ! TEMPERATURE (I.E. WHICH BECAME SATURATED DUE TO ! EVAPORATION OF RAIN AND CLOUD WATER) ! ---------------------------------------------------------------------- DO k = 3, klev - 3 is = 0 DO i = 1, klon ztenwb(i, k) = ptenh(i, k) zqenwb(i, k) = pqenh(i, k) llo2(i) = ldcum(i) .AND. prfl(i) > 0. .AND. .NOT. lddraf(i) .AND. & (kkctop(i)) IF (llo2(i)) is = is + 1 END DO IF (is==0) GO TO 290 icall = 2 CALL flxadjtq(paph(1,k), ztenwb(1,k), zqenwb(1,k), llo2, icall) ! ---------------------------------------------------------------------- ! DO MIXING OF CUMULUS AND ENVIRONMENTAL AIR ! AND CHECK FOR NEGATIVE BUOYANCY. ! THEN SET VALUES FOR DOWNDRAFT AT LFS. ! ---------------------------------------------------------------------- DO i = 1, klon IF (llo2(i)) THEN zttest = 0.5*(ptu(i,k)+ztenwb(i,k)) zqtest = 0.5*(pqu(i,k)+zqenwb(i,k)) zbuo = zttest*(1.+retv*zqtest) - ptenh(i, k)*(1.+retv*pqenh(i,k)) zcond(i) = pqenh(i, k) - zqenwb(i, k) zmftop = -cmfdeps*pmfub(i) IF (zbuo<0. .AND. prfl(i)>10.*zmftop*zcond(i)) THEN kdtop(i) = k lddraf(i) = .TRUE. ptd(i, k) = zttest pqd(i, k) = zqtest pmfd(i, k) = zmftop pmfds(i, k) = pmfd(i, k)*(rcpd*ptd(i,k)+pgeoh(i,k)) pmfdq(i, k) = pmfd(i, k)*pqd(i, k) pdmfdp(i, k-1) = -0.5*pmfd(i, k)*zcond(i) prfl(i) = prfl(i) + pdmfdp(i, k-1) END IF END IF END DO 290 END DO RETURN END SUBROUTINE flxdlfs SUBROUTINE flxddraf(ptenh, pqenh, pgeoh, paph, prfl, ptd, pqd, pmfd, pmfds, & pmfdq, pdmfdp, lddraf, pen_d, pde_d) USE dimphy USE yomcst_mod_h USE yoethf_mod_h USE yoecumf_mod_h IMPLICIT NONE ! ---------------------------------------------------------------------- ! THIS ROUTINE CALCULATES CUMULUS DOWNDRAFT DESCENT ! TO PRODUCE THE VERTICAL PROFILES FOR CUMULUS DOWNDRAFTS ! (I.E. T,Q,U AND V AND FLUXES) ! INPUT IS T,Q,P,PHI,U,V AT HALF LEVELS. ! IT RETURNS FLUXES OF S,Q AND EVAPORATION RATE ! AND U,V AT LEVELS WHERE DOWNDRAFT OCCURS ! CALCULATE MOIST DESCENT FOR ENTRAINING/DETRAINING PLUME BY ! A) MOVING AIR DRY-ADIABATICALLY TO NEXT LEVEL BELOW AND ! B) CORRECTING FOR EVAPORATION TO OBTAIN SATURATED STATE. ! ---------------------------------------------------------------------- REAL ptenh(klon, klev), pqenh(klon, klev) REAL pgeoh(klon, klev), paph(klon, klev+1) REAL ptd(klon, klev), pqd(klon, klev) REAL pmfd(klon, klev), pmfds(klon, klev), pmfdq(klon, klev) REAL pdmfdp(klon, klev) REAL prfl(klon) LOGICAL lddraf(klon) REAL pen_d(klon, klev), pde_d(klon, klev), zcond(klon) LOGICAL llo2(klon), llo1 INTEGER i, k, is, icall, itopde REAL zentr, zseen, zqeen, zsdde, zqdde, zmfdsk, zmfdqk, zdmfdp REAL zbuo ! ---------------------------------------------------------------------- ! CALCULATE MOIST DESCENT FOR CUMULUS DOWNDRAFT BY ! (A) CALCULATING ENTRAINMENT RATES, ASSUMING ! LINEAR DECREASE OF MASSFLUX IN PBL ! (B) DOING MOIST DESCENT - EVAPORATIVE COOLING ! AND MOISTENING IS CALCULATED IN *flxadjtq* ! (C) CHECKING FOR NEGATIVE BUOYANCY AND ! SPECIFYING FINAL T,Q,U,V AND DOWNWARD FLUXES DO k = 3, klev is = 0 DO i = 1, klon llo2(i) = lddraf(i) .AND. pmfd(i, k-1) < 0. IF (llo2(i)) is = is + 1 END DO IF (is==0) GO TO 180 DO i = 1, klon IF (llo2(i)) THEN zentr = entrdd*pmfd(i, k-1)*rd*ptenh(i, k-1)/(rg*paph(i,k-1))* & (paph(i,k)-paph(i,k-1)) pen_d(i, k) = zentr pde_d(i, k) = zentr END IF END DO itopde = klev - 2 IF (k>itopde) THEN DO i = 1, klon IF (llo2(i)) THEN pen_d(i, k) = 0. pde_d(i, k) = pmfd(i, itopde)*(paph(i,k)-paph(i,k-1))/ & (paph(i,klev+1)-paph(i,itopde)) END IF END DO END IF DO i = 1, klon IF (llo2(i)) THEN pmfd(i, k) = pmfd(i, k-1) + pen_d(i, k) - pde_d(i, k) zseen = (rcpd*ptenh(i,k-1)+pgeoh(i,k-1))*pen_d(i, k) zqeen = pqenh(i, k-1)*pen_d(i, k) zsdde = (rcpd*ptd(i,k-1)+pgeoh(i,k-1))*pde_d(i, k) zqdde = pqd(i, k-1)*pde_d(i, k) zmfdsk = pmfds(i, k-1) + zseen - zsdde zmfdqk = pmfdq(i, k-1) + zqeen - zqdde pqd(i, k) = zmfdqk*(1./min(-cmfcmin,pmfd(i,k))) ptd(i, k) = (zmfdsk*(1./min(-cmfcmin,pmfd(i,k)))-pgeoh(i,k))/rcpd ptd(i, k) = min(400., ptd(i,k)) ptd(i, k) = max(100., ptd(i,k)) zcond(i) = pqd(i, k) END IF END DO icall = 2 CALL flxadjtq(paph(1,k), ptd(1,k), pqd(1,k), llo2, icall) DO i = 1, klon IF (llo2(i)) THEN zcond(i) = zcond(i) - pqd(i, k) zbuo = ptd(i, k)*(1.+retv*pqd(i,k)) - ptenh(i, k)*(1.+retv*pqenh(i,k) & ) llo1 = zbuo < 0. .AND. (prfl(i)-pmfd(i,k)*zcond(i)>0.) IF (.NOT. llo1) pmfd(i, k) = 0.0 pmfds(i, k) = (rcpd*ptd(i,k)+pgeoh(i,k))*pmfd(i, k) pmfdq(i, k) = pqd(i, k)*pmfd(i, k) zdmfdp = -pmfd(i, k)*zcond(i) pdmfdp(i, k-1) = zdmfdp prfl(i) = prfl(i) + zdmfdp END IF END DO 180 END DO RETURN END SUBROUTINE flxddraf SUBROUTINE flxadjtq(pp, pt, pq, ldflag, kcall) USE dimphy USE yomcst_mod_h USE yoethf_mod_h IMPLICIT NONE ! ====================================================================== ! Objet: ajustement entre T et Q ! ====================================================================== ! NOTE: INPUT PARAMETER kcall DEFINES CALCULATION AS ! kcall=0 ENV. T AND QS IN*CUINI* ! kcall=1 CONDENSATION IN UPDRAFTS (E.G. CUBASE, CUASC) ! kcall=2 EVAPORATION IN DOWNDRAFTS (E.G. CUDLFS,CUDDRAF) REAL pt(klon), pq(klon), pp(klon) LOGICAL ldflag(klon) INTEGER kcall REAL zcond(klon), zcond1 REAL z5alvcp, z5alscp, zalvdcp, zalsdcp REAL zdelta, zcvm5, zldcp, zqsat, zcor INTEGER is, i include "FCTTRE.h" z5alvcp = r5les*rlvtt/rcpd z5alscp = r5ies*rlstt/rcpd zalvdcp = rlvtt/rcpd zalsdcp = rlstt/rcpd DO i = 1, klon zcond(i) = 0.0 END DO DO i = 1, klon IF (ldflag(i)) THEN zdelta = max(0., sign(1.,rtt-pt(i))) zcvm5 = z5alvcp*(1.-zdelta) + zdelta*z5alscp zldcp = zalvdcp*(1.-zdelta) + zdelta*zalsdcp zqsat = r2es*foeew(pt(i), zdelta)/pp(i) zqsat = min(0.5, zqsat) zcor = 1./(1.-retv*zqsat) zqsat = zqsat*zcor zcond(i) = (pq(i)-zqsat)/(1.+foede(pt(i),zdelta,zcvm5,zqsat,zcor)) IF (kcall==1) zcond(i) = max(zcond(i), 0.) IF (kcall==2) zcond(i) = min(zcond(i), 0.) pt(i) = pt(i) + zldcp*zcond(i) pq(i) = pq(i) - zcond(i) END IF END DO is = 0 DO i = 1, klon IF (zcond(i)/=0.) is = is + 1 END DO IF (is==0) GO TO 230 DO i = 1, klon IF (ldflag(i) .AND. zcond(i)/=0.) THEN zdelta = max(0., sign(1.,rtt-pt(i))) zcvm5 = z5alvcp*(1.-zdelta) + zdelta*z5alscp zldcp = zalvdcp*(1.-zdelta) + zdelta*zalsdcp zqsat = r2es*foeew(pt(i), zdelta)/pp(i) zqsat = min(0.5, zqsat) zcor = 1./(1.-retv*zqsat) zqsat = zqsat*zcor zcond1 = (pq(i)-zqsat)/(1.+foede(pt(i),zdelta,zcvm5,zqsat,zcor)) pt(i) = pt(i) + zldcp*zcond1 pq(i) = pq(i) - zcond1 END IF END DO 230 CONTINUE RETURN END SUBROUTINE flxadjtq SUBROUTINE flxsetup USE yoecumf_mod_h IMPLICIT NONE ! THIS ROUTINE DEFINES DISPOSABLE PARAMETERS FOR MASSFLUX SCHEME entrpen = 1.0E-4 ! ENTRAINMENT RATE FOR PENETRATIVE CONVECTION entrscv = 3.0E-4 ! ENTRAINMENT RATE FOR SHALLOW CONVECTION entrmid = 1.0E-4 ! ENTRAINMENT RATE FOR MIDLEVEL CONVECTION entrdd = 2.0E-4 ! ENTRAINMENT RATE FOR DOWNDRAFTS cmfctop = 0.33 ! RELATIVE CLOUD MASSFLUX AT LEVEL ABOVE NONBUO LEVEL cmfcmax = 1.0 ! MAXIMUM MASSFLUX VALUE ALLOWED FOR UPDRAFTS ETC cmfcmin = 1.E-10 ! MINIMUM MASSFLUX VALUE (FOR SAFETY) cmfdeps = 0.3 ! FRACTIONAL MASSFLUX FOR DOWNDRAFTS AT LFS cprcon = 2.0E-4 ! CONVERSION FROM CLOUD WATER TO RAIN rhcdd = 1. ! RELATIVE SATURATION IN DOWNDRAFRS (NO LONGER USED) ! (FORMULATION IMPLIES SATURATION) lmfpen = .TRUE. lmfscv = .TRUE. lmfmid = .TRUE. lmfdd = .TRUE. lmfdudv = .TRUE. RETURN END SUBROUTINE flxsetup