Context Navigation

vdifc_mod.F @ 2350

Last change on this file since 2350 was 2316, checked in by lrossi, 5 years ago
Mars GCM: Fixing some errors in vdifc_mod related to variable watercap. This variable was also integrated to the hdo cycle. Also added watercap output for the 1D model. LR
File size: 33.9 KB

Rev	Line
[1969]	1	MODULE vdifc_mod
	2
	3	IMPLICIT NONE
	4
	5	CONTAINS
	6
[38]	7	SUBROUTINE vdifc(ngrid,nlay,nq,co2ice,ppopsk,
	8	$ ptimestep,pcapcal,lecrit,
	9	$ pplay,pplev,pzlay,pzlev,pz0,
	10	$ pu,pv,ph,pq,ptsrf,pemis,pqsurf,
	11	$ pdufi,pdvfi,pdhfi,pdqfi,pfluxsrf,
	12	$ pdudif,pdvdif,pdhdif,pdtsrf,pq2,
[660]	13	$ pdqdif,pdqsdif,wstar,zcdv_true,zcdh_true,
[1996]	14	$ hfmax,pcondicea_co2microp,sensibFlux,
[2260]	15	$ dustliftday,local_time,watercap, dwatercap_dif)
[1236]	16
[1036]	17	use tracer_mod, only: noms, igcm_dust_mass, igcm_dust_number,
	18	& igcm_dust_submicron, igcm_h2o_vap,
[1974]	19	& igcm_h2o_ice, alpha_lift,
[2312]	20	& igcm_hdo_vap, igcm_hdo_ice,
[1974]	21	& igcm_stormdust_mass, igcm_stormdust_number
[1224]	22	use surfdat_h, only: watercaptag, frost_albedo_threshold, dryness
[1969]	23	USE comcstfi_h, ONLY: cpp, r, rcp, g
[1996]	24	use watersat_mod, only: watersat
[1242]	25	use turb_mod, only: turb_resolved, ustar, tstar
[2160]	26	use compute_dtau_mod, only: ti_injection_sol,tf_injection_sol
[2312]	27	use hdo_surfex_mod, only: hdo_surfex
	28
[38]	29	IMPLICIT NONE
	30
	31	c=======================================================================
	32	c
	33	c subject:
	34	c --------
	35	c Turbulent diffusion (mixing) for potential T, U, V and tracer
	36	c
	37	c Shema implicite
	38	c On commence par rajouter au variables x la tendance physique
	39	c et on resoult en fait:
	40	c x(t+1) = x(t) + dt * (dx/dt)phys(t) + dt * (dx/dt)difv(t+1)
	41	c
	42	c author:
	43	c ------
	44	c Hourdin/Forget/Fournier
	45	c=======================================================================
	46
	47	c-----------------------------------------------------------------------
	48	c declarations:
	49	c -------------
	50
[1944]	51	include "callkeys.h"
	52	include "microphys.h"
[38]	53
	54	c
	55	c arguments:
	56	c ----------
	57
[1036]	58	INTEGER,INTENT(IN) :: ngrid,nlay
	59	REAL,INTENT(IN) :: ptimestep
	60	REAL,INTENT(IN) :: pplay(ngrid,nlay),pplev(ngrid,nlay+1)
	61	REAL,INTENT(IN) :: pzlay(ngrid,nlay),pzlev(ngrid,nlay+1)
	62	REAL,INTENT(IN) :: pu(ngrid,nlay),pv(ngrid,nlay)
	63	REAL,INTENT(IN) :: ph(ngrid,nlay)
	64	REAL,INTENT(IN) :: ptsrf(ngrid),pemis(ngrid)
	65	REAL,INTENT(IN) :: pdufi(ngrid,nlay),pdvfi(ngrid,nlay)
	66	REAL,INTENT(IN) :: pdhfi(ngrid,nlay)
	67	REAL,INTENT(IN) :: pfluxsrf(ngrid)
	68	REAL,INTENT(OUT) :: pdudif(ngrid,nlay),pdvdif(ngrid,nlay)
	69	REAL,INTENT(OUT) :: pdtsrf(ngrid),pdhdif(ngrid,nlay)
[1130]	70	REAL,INTENT(IN) :: pcapcal(ngrid)
	71	REAL,INTENT(INOUT) :: pq2(ngrid,nlay+1)
[38]	72
	73	c Argument added for condensation:
[1036]	74	REAL,INTENT(IN) :: co2ice (ngrid), ppopsk(ngrid,nlay)
	75	logical,INTENT(IN) :: lecrit
[1996]	76	REAL,INTENT(IN) :: pcondicea_co2microp(ngrid,nlay)! tendency due to CO2 condensation (kg/kg.s-1)
	77
[1036]	78	REAL,INTENT(IN) :: pz0(ngrid) ! surface roughness length (m)
[224]	79
[256]	80	c Argument added to account for subgrid gustiness :
	81
[1944]	82	REAL,INTENT(IN) :: wstar(ngrid), hfmax(ngrid)!, zi(ngrid)
[256]	83
[38]	84	c Traceurs :
[1036]	85	integer,intent(in) :: nq
	86	REAL,INTENT(IN) :: pqsurf(ngrid,nq)
	87	real,intent(in) :: pq(ngrid,nlay,nq), pdqfi(ngrid,nlay,nq)
	88	real,intent(out) :: pdqdif(ngrid,nlay,nq)
[1974]	89	real,intent(out) :: pdqsdif(ngrid,nq)
	90	REAL,INTENT(in) :: dustliftday(ngrid)
	91	REAL,INTENT(in) :: local_time(ngrid)
[38]	92
	93	c local:
	94	c ------
	95
[1130]	96	REAL :: pt(ngrid,nlay)
[473]	97
[38]	98	INTEGER ilev,ig,ilay,nlev
	99
[1047]	100	REAL z4st,zdplanck(ngrid)
	101	REAL zkv(ngrid,nlay+1),zkh(ngrid,nlay+1)
	102	REAL zkq(ngrid,nlay+1)
	103	REAL zcdv(ngrid),zcdh(ngrid)
	104	REAL zcdv_true(ngrid),zcdh_true(ngrid) ! drag coeff are used by the LES to recompute u* and hfx
	105	REAL zu(ngrid,nlay),zv(ngrid,nlay)
	106	REAL zh(ngrid,nlay)
	107	REAL ztsrf2(ngrid)
	108	REAL z1(ngrid),z2(ngrid)
	109	REAL za(ngrid,nlay),zb(ngrid,nlay)
	110	REAL zb0(ngrid,nlay)
	111	REAL zc(ngrid,nlay),zd(ngrid,nlay)
[38]	112	REAL zcst1
[1047]	113	REAL zu2(ngrid)
[38]	114
	115	EXTERNAL SSUM,SCOPY
	116	REAL SSUM
[1036]	117	LOGICAL,SAVE :: firstcall=.true.
[38]	118
[626]	119
[38]	120	c variable added for CO2 condensation:
	121	c ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
[1047]	122	REAL hh , zhcond(ngrid,nlay)
	123	REAL,PARAMETER :: latcond=5.9e5
	124	REAL,PARAMETER :: tcond1mb=136.27
	125	REAL,SAVE :: acond,bcond
[669]	126
[2179]	127	c For latent heat release from ground water ice sublimation
	128	REAL tsrf_lh(ngrid) ! temporary surface temperature
	129	REAL lh ! latent heat, formulation given in the Technical Document:
	130	! "Modeling water ice sublimation under Phoenix-like conditions", Montmessin et al. 2004
[1047]	131	! REAL tsrf_lw(ngrid)
[1036]	132	! REAL alpha
[2179]	133	! REAL T1,T2
	134	! SAVE T1,T2
	135	! DATA T1,T2/-604.3,1080.7/ ! zeros of latent heat equation for ice
[38]	136
	137	c Tracers :
	138	c ~~~~~~~
	139	INTEGER iq
[1047]	140	REAL zq(ngrid,nlay,nq)
	141	REAL zq1temp(ngrid)
	142	REAL rho(ngrid) ! near surface air density
	143	REAL qsat(ngrid)
[38]	144
[2312]	145	REAL hdoflux(ngrid) ! value of vapour flux of HDO
	146	REAL h2oflux(ngrid) ! value of vapour flux of H2O
	147	REAL old_h2o_vap(ngrid) ! traceur d'eau avant traitement
	148
[38]	149	REAL kmixmin
	150
[2260]	151	c Argument added for surface water ice budget:
	152	REAL,INTENT(IN) :: watercap(ngrid)
	153	REAL,INTENT(OUT) :: dwatercap_dif(ngrid)
	154
[473]	155	c Mass-variation scheme :
	156	c ~~~~~~~
	157
	158	INTEGER j,l
[1047]	159	REAL zcondicea(ngrid,nlay)
	160	REAL zt(ngrid,nlay),ztcond(ngrid,nlay+1)
	161	REAL betam(ngrid,nlay),dmice(ngrid,nlay)
	162	REAL pdtc(ngrid,nlay)
	163	REAL zhs(ngrid,nlay)
	164	REAL,SAVE :: ccond
[473]	165
	166	c Theta_m formulation for mass-variation scheme :
	167	c ~~~~~~~
	168
[1047]	169	INTEGER,SAVE :: ico2
	170	INTEGER llnt(ngrid)
	171	REAL,SAVE :: m_co2, m_noco2, A , B
	172	REAL vmr_co2(ngrid,nlay)
[473]	173	REAL qco2,mmean
	174
[1047]	175	REAL,INTENT(OUT) :: sensibFlux(ngrid)
[660]	176
[2312]	177	!!MARGAUX
	178	REAL DoH_vap(ngrid,nlay)
	179
[38]	180	c ** un petit test de coherence
	181	c --------------------------
	182
[1779]	183	! AS: OK firstcall absolute
[38]	184	IF (firstcall) THEN
	185	c To compute: Tcond= 1./(bcond-acondlog(.0095p)) (p in pascal)
	186	bcond=1./tcond1mb
	187	acond=r/latcond
[473]	188	ccond=cpp/(g*latcond)
[38]	189	PRINT*,'In vdifc: Tcond(P=1mb)=',tcond1mb,' Lcond=',latcond
[473]	190	PRINT*,' acond,bcond,ccond',acond,bcond,ccond
[38]	191
[473]	192
	193	ico2=0
	194
	195	if (tracer) then
	196	c Prepare Special treatment if one of the tracer is CO2 gas
[1036]	197	do iq=1,nq
[473]	198	if (noms(iq).eq."co2") then
	199	ico2=iq
	200	m_co2 = 44.01E-3 ! CO2 molecular mass (kg/mol)
	201	m_noco2 = 33.37E-3 ! Non condensible mol mass (kg/mol)
	202	c Compute A and B coefficient use to compute
	203	c mean molecular mass Mair defined by
	204	c 1/Mair = q(ico2)/m_co2 + (1-q(ico2))/m_noco2
	205	c 1/Mair = A*q(ico2) + B
	206	A =(1/m_co2 - 1/m_noco2)
	207	B=1/m_noco2
	208	endif
	209	enddo
	210	end if
	211
[38]	212	firstcall=.false.
	213	ENDIF
	214
	215
	216	c-----------------------------------------------------------------------
	217	c 1. initialisation
	218	c -----------------
	219
	220	nlev=nlay+1
	221
[1035]	222	! initialize output tendencies to zero:
	223	pdudif(1:ngrid,1:nlay)=0
	224	pdvdif(1:ngrid,1:nlay)=0
	225	pdhdif(1:ngrid,1:nlay)=0
	226	pdtsrf(1:ngrid)=0
	227	pdqdif(1:ngrid,1:nlay,1:nq)=0
	228	pdqsdif(1:ngrid,1:nq)=0
[2260]	229	dwatercap_dif(1:ngrid)=0
[1035]	230
[38]	231	c ** calcul de rhodz et dtrho/dz=dtrho*2 g/dp
	232	c avec rho=p/RT=p/ (R Theta) (p/ps)**kappa
	233	c ----------------------------------------
	234
	235	DO ilay=1,nlay
	236	DO ig=1,ngrid
	237	za(ig,ilay)=(pplev(ig,ilay)-pplev(ig,ilay+1))/g
[473]	238	! Mass variation scheme:
	239	betam(ig,ilay)=-za(ig,ilay)latcond/(cppppopsk(ig,ilay))
[38]	240	ENDDO
	241	ENDDO
	242
	243	zcst1=4.gptimestep/(r*r)
	244	DO ilev=2,nlev-1
	245	DO ig=1,ngrid
	246	zb0(ig,ilev)=pplev(ig,ilev)*
	247	s (pplev(ig,1)/pplev(ig,ilev))**rcp /
	248	s (ph(ig,ilev-1)+ph(ig,ilev))
	249	zb0(ig,ilev)=zcst1zb0(ig,ilev)zb0(ig,ilev)/
	250	s (pplay(ig,ilev-1)-pplay(ig,ilev))
	251	ENDDO
	252	ENDDO
	253	DO ig=1,ngrid
[473]	254	zb0(ig,1)=ptimesteppplev(ig,1)/(rptsrf(ig))
[38]	255	ENDDO
	256
	257	c ** diagnostique pour l'initialisation
	258	c ----------------------------------
	259
	260	IF(lecrit) THEN
	261	ig=ngrid/2+1
	262	PRINT*,'Pression (mbar) ,altitude (km),u,v,theta, rho dz'
	263	DO ilay=1,nlay
	264	WRITE(*,'(6f11.5)')
	265	s .01pplay(ig,ilay),.001pzlay(ig,ilay),
	266	s pu(ig,ilay),pv(ig,ilay),ph(ig,ilay),za(ig,ilay)
	267	ENDDO
	268	PRINT*,'Pression (mbar) ,altitude (km),zb'
	269	DO ilev=1,nlay
	270	WRITE(*,'(3f15.7)')
	271	s .01pplev(ig,ilev),.001pzlev(ig,ilev),
	272	s zb0(ig,ilev)
	273	ENDDO
	274	ENDIF
	275
[473]	276	c -----------------------------------
[38]	277	c Potential Condensation temperature:
	278	c -----------------------------------
	279
[473]	280	c Compute CO2 Volume mixing ratio
	281	c -------------------------------
	282	if (callcond.and.(ico2.ne.0)) then
	283	DO ilev=1,nlay
	284	DO ig=1,ngrid
[529]	285	qco2=MAX(1.E-30
	286	& ,pq(ig,ilev,ico2)+pdqfi(ig,ilev,ico2)*ptimestep)
[473]	287	c Mean air molecular mass = 1/(q(ico2)/m_co2 + (1-q(ico2))/m_noco2)
	288	mmean=1/(A*qco2 +B)
	289	vmr_co2(ig,ilev) = qco2*mmean/m_co2
	290	ENDDO
	291	ENDDO
	292	else
	293	DO ilev=1,nlay
	294	DO ig=1,ngrid
	295	vmr_co2(ig,ilev)=0.95
	296	ENDDO
	297	ENDDO
	298	end if
[38]	299
[473]	300	c forecast of atmospheric temperature zt and frost temperature ztcond
	301	c --------------------------------------------------------------------
[38]	302
[473]	303	if (callcond) then
	304	DO ilev=1,nlay
	305	DO ig=1,ngrid
[884]	306	ztcond(ig,ilev)=
	307	& 1./(bcond-acondlog(.01vmr_co2(ig,ilev)*pplay(ig,ilev)))
	308	if (pplay(ig,ilev).lt.1e-4) ztcond(ig,ilev)=0.0 !mars Monica
[473]	309	! zhcond(ig,ilev) =
	310	! & (1./(bcond-acondlog(.0095pplay(ig,ilev))))/ppopsk(ig,ilev)
	311	zhcond(ig,ilev) = ztcond(ig,ilev)/ppopsk(ig,ilev)
	312	END DO
	313	END DO
[884]	314	ztcond(:,nlay+1)=ztcond(:,nlay)
[473]	315	else
[884]	316	zhcond(:,:) = 0
	317	ztcond(:,:) = 0
[473]	318	end if
	319
	320
[38]	321	c-----------------------------------------------------------------------
	322	c 2. ajout des tendances physiques
	323	c -----------------------------
	324
	325	DO ilev=1,nlay
	326	DO ig=1,ngrid
	327	zu(ig,ilev)=pu(ig,ilev)+pdufi(ig,ilev)*ptimestep
	328	zv(ig,ilev)=pv(ig,ilev)+pdvfi(ig,ilev)*ptimestep
	329	zh(ig,ilev)=ph(ig,ilev)+pdhfi(ig,ilev)*ptimestep
[473]	330	! zh(ig,ilev)=max(zh(ig,ilev),zhcond(ig,ilev))
[38]	331	ENDDO
	332	ENDDO
	333	if(tracer) then
	334	DO iq =1, nq
	335	DO ilev=1,nlay
	336	DO ig=1,ngrid
	337	zq(ig,ilev,iq)=pq(ig,ilev,iq)+pdqfi(ig,ilev,iq)*ptimestep
	338	ENDDO
	339	ENDDO
	340	ENDDO
	341	end if
	342
	343	c-----------------------------------------------------------------------
	344	c 3. schema de turbulence
	345	c --------------------
	346
	347	c ** source d'energie cinetique turbulente a la surface
	348	c (condition aux limites du schema de diffusion turbulente
	349	c dans la couche limite
	350	c ---------------------
	351
[499]	352	CALL vdif_cd(ngrid,nlay,pz0,g,pzlay,pu,pv,wstar,ptsrf,ph
[1236]	353	& ,zcdv_true,zcdh_true)
[256]	354
[290]	355	zu2(:)=pu(:,1)pu(:,1)+pv(:,1)pv(:,1)
[256]	356
[291]	357	IF (callrichsl) THEN
[545]	358	zcdv(:)=zcdv_true(:)*sqrt(zu2(:)+
	359	& (log(1.+0.7wstar(:) + 2.3wstar(:)2))2)
	360	zcdh(:)=zcdh_true(:)*sqrt(zu2(:)+
	361	& (log(1.+0.7wstar(:) + 2.3wstar(:)2))2)
[496]	362
[1242]	363	ustar(:)=sqrt(zcdv_true(:))*sqrt(zu2(:)+
[545]	364	& (log(1.+0.7wstar(:) + 2.3wstar(:)2))2)
	365
[1242]	366	tstar(:)=0.
[545]	367	DO ig=1,ngrid
	368	IF (zcdh_true(ig) .ne. 0.) THEN ! When Cd=Ch=0, u=t=0
[1242]	369	tstar(ig)=(ph(ig,1)-ptsrf(ig))*zcdh(ig)/ustar(ig)
[545]	370	ENDIF
	371	ENDDO
	372
[284]	373	ELSE
[545]	374	zcdv(:)=zcdv_true(:)*sqrt(zu2(:)) ! 1 / bulk aerodynamic momentum conductance
	375	zcdh(:)=zcdh_true(:)*sqrt(zu2(:)) ! 1 / bulk aerodynamic heat conductance
[1242]	376	ustar(:)=sqrt(zcdv_true(:))*sqrt(zu2(:))
	377	tstar(:)=(ph(:,1)-ptsrf(:))*zcdh_true(:)/sqrt(zcdv_true(:))
[290]	378	ENDIF
[38]	379
[529]	380	! Some usefull diagnostics for the new surface layer parametrization :
[290]	381
[1130]	382	! call WRITEDIAGFI(ngrid,'vdifc_zcdv_true',
[256]	383	! & 'momentum drag','no units',
	384	! & 2,zcdv_true)
[1130]	385	! call WRITEDIAGFI(ngrid,'vdifc_zcdh_true',
[256]	386	! & 'heat drag','no units',
	387	! & 2,zcdh_true)
[1130]	388	! call WRITEDIAGFI(ngrid,'vdifc_ust',
[473]	389	! & 'friction velocity','m/s',2,ust)
[1130]	390	! call WRITEDIAGFI(ngrid,'vdifc_tst',
[473]	391	! & 'friction temperature','K',2,tst)
[1130]	392	! call WRITEDIAGFI(ngrid,'vdifc_zcdv',
[268]	393	! & 'aerodyn momentum conductance','m/s',
[256]	394	! & 2,zcdv)
[1130]	395	! call WRITEDIAGFI(ngrid,'vdifc_zcdh',
[268]	396	! & 'aerodyn heat conductance','m/s',
[256]	397	! & 2,zcdh)
	398
[38]	399	c ** schema de diffusion turbulente dans la couche limite
	400	c ----------------------------------------------------
[1240]	401	IF (.not. callyamada4) THEN
[529]	402
[1130]	403	CALL vdif_kc(ngrid,nlay,nq,ptimestep,g,pzlev,pzlay
[38]	404	& ,pu,pv,ph,zcdv_true
[325]	405	& ,pq2,zkv,zkh,zq)
[529]	406
[544]	407	ELSE
[38]	408
[555]	409	pt(:,:)=ph(:,:)*ppopsk(:,:)
[1036]	410	CALL yamada4(ngrid,nlay,nq,ptimestep,g,r,pplev,pt
[1242]	411	s ,pzlev,pzlay,pu,pv,ph,pq,zcdv_true,pq2,zkv,zkh,zkq,ustar
[652]	412	s ,9)
[544]	413	ENDIF
	414
[38]	415	if ((doubleq).and.(ngrid.eq.1)) then
	416	kmixmin = 80. !80.! minimum eddy mix coeff in 1D
	417	do ilev=1,nlay
	418	do ig=1,ngrid
	419	zkh(ig,ilev) = max(kmixmin,zkh(ig,ilev))
	420	zkv(ig,ilev) = max(kmixmin,zkv(ig,ilev))
	421	end do
	422	end do
	423	end if
	424
	425	c ** diagnostique pour le schema de turbulence
	426	c -----------------------------------------
	427
	428	IF(lecrit) THEN
	429	PRINT*
	430	PRINT*,'Diagnostic for the vertical turbulent mixing'
	431	PRINT*,'Cd for momentum and potential temperature'
	432
	433	PRINT*,zcdv(ngrid/2+1),zcdh(ngrid/2+1)
	434	PRINT*,'Mixing coefficient for momentum and pot.temp.'
	435	DO ilev=1,nlay
	436	PRINT*,zkv(ngrid/2+1,ilev),zkh(ngrid/2+1,ilev)
	437	ENDDO
	438	ENDIF
	439
	440
	441
	442
	443	c-----------------------------------------------------------------------
	444	c 4. inversion pour l'implicite sur u
	445	c --------------------------------
	446
	447	c ** l'equation est
	448	c u(t+1) = u(t) + dt * {(du/dt)phys}(t) + dt * {(du/dt)difv}(t+1)
	449	c avec
	450	c /zu/ = u(t) + dt * {(du/dt)phys}(t) (voir paragraphe 2.)
	451	c et
	452	c dt * {(du/dt)difv}(t+1) = dt * {(d/dz)[ Ku (du/dz) ]}(t+1)
	453	c donc les entrees sont /zcdv/ pour la condition a la limite sol
	454	c et /zkv/ = Ku
[2312]	455
[2274]	456	zb(1:ngrid,2:nlay)=zkv(1:ngrid,2:nlay)*zb0(1:ngrid,2:nlay)
	457	zb(1:ngrid,1)=zcdv(1:ngrid)*zb0(1:ngrid,1)
[38]	458
	459	DO ig=1,ngrid
	460	z1(ig)=1./(za(ig,nlay)+zb(ig,nlay))
	461	zc(ig,nlay)=za(ig,nlay)zu(ig,nlay)z1(ig)
	462	zd(ig,nlay)=zb(ig,nlay)*z1(ig)
	463	ENDDO
	464
	465	DO ilay=nlay-1,1,-1
	466	DO ig=1,ngrid
	467	z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+
	468	$ zb(ig,ilay+1)*(1.-zd(ig,ilay+1)))
	469	zc(ig,ilay)=(za(ig,ilay)*zu(ig,ilay)+
	470	$ zb(ig,ilay+1)zc(ig,ilay+1))z1(ig)
	471	zd(ig,ilay)=zb(ig,ilay)*z1(ig)
	472	ENDDO
	473	ENDDO
	474
	475	DO ig=1,ngrid
	476	zu(ig,1)=zc(ig,1)
	477	ENDDO
	478	DO ilay=2,nlay
	479	DO ig=1,ngrid
	480	zu(ig,ilay)=zc(ig,ilay)+zd(ig,ilay)*zu(ig,ilay-1)
	481	ENDDO
	482	ENDDO
	483
	484
	485
	486
	487
	488	c-----------------------------------------------------------------------
	489	c 5. inversion pour l'implicite sur v
	490	c --------------------------------
	491
	492	c ** l'equation est
	493	c v(t+1) = v(t) + dt * {(dv/dt)phys}(t) + dt * {(dv/dt)difv}(t+1)
	494	c avec
	495	c /zv/ = v(t) + dt * {(dv/dt)phys}(t) (voir paragraphe 2.)
	496	c et
	497	c dt * {(dv/dt)difv}(t+1) = dt * {(d/dz)[ Kv (dv/dz) ]}(t+1)
	498	c donc les entrees sont /zcdv/ pour la condition a la limite sol
	499	c et /zkv/ = Kv
	500
	501	DO ig=1,ngrid
	502	z1(ig)=1./(za(ig,nlay)+zb(ig,nlay))
	503	zc(ig,nlay)=za(ig,nlay)zv(ig,nlay)z1(ig)
	504	zd(ig,nlay)=zb(ig,nlay)*z1(ig)
	505	ENDDO
	506
	507	DO ilay=nlay-1,1,-1
	508	DO ig=1,ngrid
	509	z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+
	510	$ zb(ig,ilay+1)*(1.-zd(ig,ilay+1)))
	511	zc(ig,ilay)=(za(ig,ilay)*zv(ig,ilay)+
	512	$ zb(ig,ilay+1)zc(ig,ilay+1))z1(ig)
	513	zd(ig,ilay)=zb(ig,ilay)*z1(ig)
	514	ENDDO
	515	ENDDO
	516
	517	DO ig=1,ngrid
	518	zv(ig,1)=zc(ig,1)
	519	ENDDO
	520	DO ilay=2,nlay
	521	DO ig=1,ngrid
	522	zv(ig,ilay)=zc(ig,ilay)+zd(ig,ilay)*zv(ig,ilay-1)
	523	ENDDO
	524	ENDDO
	525
	526
	527
	528
	529
	530	c-----------------------------------------------------------------------
	531	c 6. inversion pour l'implicite sur h sans oublier le couplage
	532	c avec le sol (conduction)
	533	c ------------------------
	534
	535	c ** l'equation est
	536	c h(t+1) = h(t) + dt * {(dh/dt)phys}(t) + dt * {(dh/dt)difv}(t+1)
	537	c avec
	538	c /zh/ = h(t) + dt * {(dh/dt)phys}(t) (voir paragraphe 2.)
	539	c et
	540	c dt * {(dh/dt)difv}(t+1) = dt * {(d/dz)[ Kh (dh/dz) ]}(t+1)
	541	c donc les entrees sont /zcdh/ pour la condition de raccord au sol
	542	c et /zkh/ = Kh
	543	c -------------
	544
[473]	545	c Mass variation scheme:
[2274]	546	zb(1:ngrid,2:nlay)=zkh(1:ngrid,2:nlay)*zb0(1:ngrid,2:nlay)
	547	zb(1:ngrid,1)=zcdh(1:ngrid)*zb0(1:ngrid,1)
[38]	548
[473]	549	c on initialise dm c
	550
	551	pdtc(:,:)=0.
	552	zt(:,:)=0.
	553	dmice(:,:)=0.
[38]	554
	555	c ** calcul de (d Planck / dT) a la temperature d'interface
	556	c ------------------------------------------------------
	557
	558	z4st=4.5.67e-8ptimestep
[544]	559	IF (tke_heat_flux .eq. 0.) THEN
[38]	560	DO ig=1,ngrid
	561	zdplanck(ig)=z4stpemis(ig)ptsrf(ig)ptsrf(ig)ptsrf(ig)
	562	ENDDO
[544]	563	ELSE
	564	zdplanck(:)=0.
	565	ENDIF
[38]	566
[473]	567	! calcul de zc et zd pour la couche top en prenant en compte le terme
[2080]	568	! de variation de masse (on fait une boucle pour que \E7a converge)
[473]	569
	570	! Identification des points de grilles qui ont besoin de la correction
	571
	572	llnt(:)=1
[1236]	573	IF (.not.turb_resolved) THEN
[884]	574	IF (callcond) THEN
	575	DO ig=1,ngrid
[473]	576	DO l=1,nlay
	577	if(zh(ig,l) .lt. zhcond(ig,l)) then
	578	llnt(ig)=300
	579	! 200 and 100 do not go beyond month 9 with normal dissipation
	580	goto 5
	581	endif
	582	ENDDO
[884]	583	5 continue
	584	ENDDO
	585	ENDIF
[473]	586
[529]	587	ENDIF
	588
[473]	589	DO ig=1,ngrid
	590
	591	! Initialization of z1 and zd, which do not depend on dmice
	592
	593	z1(ig)=1./(za(ig,nlay)+zb(ig,nlay))
	594	zd(ig,nlay)=zb(ig,nlay)*z1(ig)
	595
	596	DO ilay=nlay-1,1,-1
	597	z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+
	598	$ zb(ig,ilay+1)*(1.-zd(ig,ilay+1)))
	599	zd(ig,ilay)=zb(ig,ilay)*z1(ig)
	600	ENDDO
	601
	602	! Convergence loop
	603
	604	DO j=1,llnt(ig)
	605
	606	z1(ig)=1./(za(ig,nlay)+zb(ig,nlay))
	607	zc(ig,nlay)=za(ig,nlay)*zh(ig,nlay)
	608	& -betam(ig,nlay)*dmice(ig,nlay)
	609	zc(ig,nlay)=zc(ig,nlay)*z1(ig)
	610	! zd(ig,nlay)=zb(ig,nlay)*z1(ig)
	611
	612	! calcul de zc et zd pour les couches du haut vers le bas
	613
	614	DO ilay=nlay-1,1,-1
	615	z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+
	616	$ zb(ig,ilay+1)*(1.-zd(ig,ilay+1)))
	617	zc(ig,ilay)=(za(ig,ilay)*zh(ig,ilay)+
	618	$ zb(ig,ilay+1)*zc(ig,ilay+1)-
	619	$ betam(ig,ilay)dmice(ig,ilay))z1(ig)
	620	! zd(ig,ilay)=zb(ig,ilay)*z1(ig)
	621	ENDDO
	622
[38]	623	c ** calcul de la temperature_d'interface et de sa tendance.
	624	c on ecrit que la somme des flux est nulle a l'interface
	625	c a t + \delta t,
	626	c c'est a dire le flux radiatif a {t + \delta t}
	627	c + le flux turbulent a {t + \delta t}
	628	c qui s'ecrit K (T1-Tsurf) avec T1 = d1 Tsurf + c1
	629	c (notation K dt = /cpp*b/)
	630	c + le flux dans le sol a t
	631	c + l'evolution du flux dans le sol lorsque la temperature d'interface
	632	c passe de sa valeur a t a sa valeur a {t + \delta t}.
	633	c ----------------------------------------------------
	634
	635	z1(ig)=pcapcal(ig)ptsrf(ig)+cppzb(ig,1)*zc(ig,1)
	636	s +zdplanck(ig)ptsrf(ig)+ pfluxsrf(ig)ptimestep
	637	z2(ig)= pcapcal(ig)+cppzb(ig,1)(1.-zd(ig,1))+zdplanck(ig)
	638	ztsrf2(ig)=z1(ig)/z2(ig)
[473]	639	! pdtsrf(ig)=(ztsrf2(ig)-ptsrf(ig))/ptimestep !incremented outside loop
	640	zhs(ig,1)=zc(ig,1)+zd(ig,1)*ztsrf2(ig)
[38]	641
	642	c ** et a partir de la temperature au sol on remonte
	643	c -----------------------------------------------
	644
[473]	645	DO ilay=2,nlay
	646	zhs(ig,ilay)=zc(ig,ilay)+zd(ig,ilay)*zhs(ig,ilay-1)
	647	ENDDO
	648	DO ilay=1,nlay
	649	zt(ig,ilay)=zhs(ig,ilay)*ppopsk(ig,ilay)
	650	ENDDO
	651
	652	c Condensation/sublimation in the atmosphere
	653	c ------------------------------------------
	654	c (computation of zcondicea and dmice)
	655
[1996]	656	IF (.NOT. co2clouds) then
	657	DO l=nlay , 1, -1
[473]	658	IF(zt(ig,l).LT.ztcond(ig,l)) THEN
	659	pdtc(ig,l)=(ztcond(ig,l) - zt(ig,l))/ptimestep
	660	zcondicea(ig,l)=(pplev(ig,l)-pplev(ig,l+1))
	661	& ccondpdtc(ig,l)
	662	dmice(ig,l)= dmice(ig,l) + zcondicea(ig,l)*ptimestep
	663	END IF
[1996]	664	ENDDO
	665	ELSE
	666	DO l=nlay , 1, -1
	667	zcondicea(ig,l)= 0.!pcondicea_co2microp(ig,l)*
	668	c & (pplev(ig,l) - pplev(ig,l+1))/g
	669	dmice(ig,l)= 0.!dmice(ig,l) + zcondicea(ig,l)*ptimestep
	670	pdtc(ig,l)=0.
	671	ENDDO
	672	ENDIF
	673
	674	ENDDO!of Do j=1,XXX
[38]	675
[1996]	676	ENDDO !of Do ig=1,ngrid
[38]	677
[473]	678	pdtsrf(:)=(ztsrf2(:)-ptsrf(:))/ptimestep
[669]	679
[660]	680	DO ig=1,ngrid ! computing sensible heat flux (atm => surface)
	681	sensibFlux(ig)=cppzb(ig,1)/ptimestep(zhs(ig,1)-ztsrf2(ig))
	682	ENDDO
[473]	683
[38]	684	c-----------------------------------------------------------------------
	685	c TRACERS
	686	c -------
	687
	688	if(tracer) then
	689
	690	c Using the wind modified by friction for lifting and sublimation
	691	c ----------------------------------------------------------------
	692
[529]	693	! This is computed above and takes into account surface-atmosphere flux
	694	! enhancement by subgrid gustiness and atmospheric-stability related
	695	! variations of transfer coefficients.
	696
	697	! DO ig=1,ngrid
	698	! zu2(ig)=zu(ig,1)zu(ig,1)+zv(ig,1)zv(ig,1)
	699	! zcdv(ig)=zcdv_true(ig)*sqrt(zu2(ig))
	700	! zcdh(ig)=zcdh_true(ig)*sqrt(zu2(ig))
	701	! ENDDO
	702
[38]	703	c Calcul du flux vertical au bas de la premiere couche (dust) :
	704	c -----------------------------------------------------------
[1047]	705	do ig=1,ngrid
[38]	706	rho(ig) = zb0(ig,1) /ptimestep
	707	c zb(ig,1) = 0.
	708	end do
	709	c Dust lifting:
	710	if (lifting) then
[310]	711	#ifndef MESOSCALE
[38]	712	if (doubleq.AND.submicron) then
	713	do ig=1,ngrid
	714	c if(co2ice(ig).lt.1) then
	715	pdqsdif(ig,igcm_dust_mass) =
	716	& -alpha_lift(igcm_dust_mass)
	717	pdqsdif(ig,igcm_dust_number) =
	718	& -alpha_lift(igcm_dust_number)
	719	pdqsdif(ig,igcm_dust_submicron) =
	720	& -alpha_lift(igcm_dust_submicron)
	721	c end if
	722	end do
	723	else if (doubleq) then
[1974]	724	if (dustinjection.eq.0) then !injection scheme 0 (old)
	725	!or 2 (injection in CL)
	726	do ig=1,ngrid
[1455]	727	if(co2ice(ig).lt.1) then ! pas de soulevement si glace CO2
[38]	728	pdqsdif(ig,igcm_dust_mass) =
	729	& -alpha_lift(igcm_dust_mass)
	730	pdqsdif(ig,igcm_dust_number) =
[520]	731	& -alpha_lift(igcm_dust_number)
	732	end if
[1974]	733	end do
	734	elseif(dustinjection.eq.1)then ! dust injection scheme = 1 injection from surface
	735	do ig=1,ngrid
	736	if(co2ice(ig).lt.1) then ! pas de soulevement si glace CO2
[2160]	737	IF((ti_injection_sol.LE.local_time(ig)).and.
	738	& (local_time(ig).LE.tf_injection_sol)) THEN
[1974]	739	if (rdstorm) then !Rocket dust storm scheme
	740	pdqsdif(ig,igcm_stormdust_mass) =
	741	& -alpha_lift(igcm_stormdust_mass)
	742	& *dustliftday(ig)
	743	pdqsdif(ig,igcm_stormdust_number) =
	744	& -alpha_lift(igcm_stormdust_number)
	745	& *dustliftday(ig)
	746	pdqsdif(ig,igcm_dust_mass)= 0.
	747	pdqsdif(ig,igcm_dust_number)= 0.
	748	else
	749	pdqsdif(ig,igcm_dust_mass)=
	750	& -dustliftday(ig)*
	751	& alpha_lift(igcm_dust_mass)
	752	pdqsdif(ig,igcm_dust_number)=
	753	& -dustliftday(ig)*
	754	& alpha_lift(igcm_dust_number)
	755	endif
	756	if (submicron) then
	757	pdqsdif(ig,igcm_dust_submicron) = 0.
	758	endif ! if (submicron)
	759	ELSE ! outside dust injection time frame
[2080]	760	pdqsdif(ig,igcm_dust_mass)= 0.
	761	pdqsdif(ig,igcm_dust_number)= 0.
	762	if (rdstorm) then
[1974]	763	pdqsdif(ig,igcm_stormdust_mass)= 0.
	764	pdqsdif(ig,igcm_stormdust_number)= 0.
[2080]	765	end if
[1974]	766	ENDIF
	767
	768	end if ! of if(co2ice(ig).lt.1)
	769	end do
	770	endif ! end if dustinjection
[38]	771	else if (submicron) then
	772	do ig=1,ngrid
	773	pdqsdif(ig,igcm_dust_submicron) =
	774	& -alpha_lift(igcm_dust_submicron)
	775	end do
	776	else
[1236]	777	#endif
[38]	778	call dustlift(ngrid,nlay,nq,rho,zcdh_true,zcdh,co2ice,
	779	& pdqsdif)
[1236]	780	#ifndef MESOSCALE
[38]	781	endif !doubleq.AND.submicron
[310]	782	#endif
[38]	783	else
	784	pdqsdif(1:ngrid,1:nq) = 0.
	785	end if
	786
	787	c OU calcul de la valeur de q a la surface (water) :
	788	c ----------------------------------------
	789	if (water) then
[1047]	790	call watersat(ngrid,ptsrf,pplev(1,1),qsat)
[38]	791	end if
	792
	793	c Inversion pour l'implicite sur q
	794	c --------------------------------
[1974]	795	do iq=1,nq !for all tracers including stormdust
[2274]	796	zb(1:ngrid,2:nlay)=zkh(1:ngrid,2:nlay)*zb0(1:ngrid,2:nlay)
[38]	797
[2312]	798	if ((water).and.(iq.eq.igcm_h2o_vap)) then
[38]	799	c This line is required to account for turbulent transport
	800	c from surface (e.g. ice) to mid-layer of atmosphere:
[2274]	801	zb(1:ngrid,1)=zcdv(1:ngrid)*zb0(1:ngrid,1)
	802	zb(1:ngrid,1)=dryness(1:ngrid)*zb(1:ngrid,1)
[38]	803	else ! (re)-initialize zb(:,1)
	804	zb(1:ngrid,1)=0
	805	end if
	806
	807	DO ig=1,ngrid
	808	z1(ig)=1./(za(ig,nlay)+zb(ig,nlay))
	809	zc(ig,nlay)=za(ig,nlay)zq(ig,nlay,iq)z1(ig)
	810	zd(ig,nlay)=zb(ig,nlay)*z1(ig)
	811	ENDDO
	812
	813	DO ilay=nlay-1,2,-1
	814	DO ig=1,ngrid
	815	z1(ig)=1./(za(ig,ilay)+zb(ig,ilay)+
	816	$ zb(ig,ilay+1)*(1.-zd(ig,ilay+1)))
	817	zc(ig,ilay)=(za(ig,ilay)*zq(ig,ilay,iq)+
	818	$ zb(ig,ilay+1)zc(ig,ilay+1))z1(ig)
	819	zd(ig,ilay)=zb(ig,ilay)*z1(ig)
	820	ENDDO
	821	ENDDO
	822
[2312]	823	if ( (water.and.(iq.eq.igcm_h2o_ice))
	824	$ .or. (hdo.and.(iq.eq.igcm_hdo_ice)) ) then
[38]	825	! special case for water ice tracer: do not include
	826	! h2o ice tracer from surface (which is set when handling
[473]	827	! h2o vapour case (see further down).
[38]	828	DO ig=1,ngrid
	829	z1(ig)=1./(za(ig,1)+zb(ig,1)+
	830	$ zb(ig,2)*(1.-zd(ig,2)))
	831	zc(ig,1)=(za(ig,1)*zq(ig,1,iq)+
	832	$ zb(ig,2)zc(ig,2)) z1(ig)
	833	ENDDO
[2312]	834	else if (hdo.and.(iq.eq.igcm_hdo_vap)) then
	835	CALL hdo_surfex(ngrid,nlay,nq,ptimestep,
	836	& zt,zq,pqsurf,
[2316]	837	& old_h2o_vap,pdqsdif,dwatercap_dif,
[2312]	838	& hdoflux)
	839	DO ig=1,ngrid
	840	z1(ig)=1./(za(ig,1)+zb(ig,1)+
	841	$ zb(ig,2)*(1.-zd(ig,2)))
	842	zc(ig,1)=(za(ig,1)*zq(ig,1,iq)+
	843	$ zb(ig,2)*zc(ig,2) +
	844	$ (-hdoflux(ig)) ptimestep) z1(ig) !tracer flux from surface
	845	ENDDO
	846
[38]	847	else ! general case
	848	DO ig=1,ngrid
	849	z1(ig)=1./(za(ig,1)+zb(ig,1)+
	850	$ zb(ig,2)*(1.-zd(ig,2)))
	851	zc(ig,1)=(za(ig,1)*zq(ig,1,iq)+
	852	$ zb(ig,2)*zc(ig,2) +
	853	$ (-pdqsdif(ig,iq)) ptimestep) z1(ig) !tracer flux from surface
	854	ENDDO
[2312]	855
[38]	856	endif ! of if (water.and.(iq.eq.igcm_h2o_ice))
	857
	858	IF ((water).and.(iq.eq.igcm_h2o_vap)) then
	859	c Calculation for turbulent exchange with the surface (for ice)
	860	DO ig=1,ngrid
[2312]	861	old_h2o_vap(ig)=zq(ig,1,igcm_h2o_vap)
[38]	862	zd(ig,1)=zb(ig,1)*z1(ig)
	863	zq1temp(ig)=zc(ig,1)+ zd(ig,1)*qsat(ig)
	864
	865	pdqsdif(ig,igcm_h2o_ice)=rho(ig)dryness(ig)zcdv(ig)
	866	& *(zq1temp(ig)-qsat(ig))
	867	c write(,)'flux vers le sol=',pdqsdif(ig,nq)
	868	END DO
	869
	870	DO ig=1,ngrid
[2312]	871	IF (hdo) then !if hdo, need to treat polar caps differently
	872	h2oflux(ig) = pdqsdif(ig,igcm_h2o_ice) ! h2oflux is
	873	! uncorrected waterflux
	874	ENDIF !hdo
	875
[2260]	876	if ((-pdqsdif(ig,igcm_h2o_ice)*ptimestep)
	877	& .gt.(pqsurf(ig,igcm_h2o_ice))) then
	878	c write(,)'subliming more than available frost: qsurf!'
	879	if(watercaptag(ig)) then
	880	c dwatercap_dif same sign as pdqsdif (pos. toward ground)
[2316]	881	dwatercap_dif(ig) = pdqsdif(ig,igcm_h2o_ice)
	882	& + pqsurf(ig,igcm_h2o_ice)/ptimestep
[2260]	883	pdqsdif(ig,igcm_h2o_ice)=
[38]	884	& -pqsurf(ig,igcm_h2o_ice)/ptimestep
[2260]	885	c write(,) "subliming more than available frost: qsurf!"
	886	else ! (case not.watercaptag(ig))
	887	pdqsdif(ig,igcm_h2o_ice)=
	888	& -pqsurf(ig,igcm_h2o_ice)/ptimestep
	889	dwatercap_dif(ig) = 0.0
[2312]	890	if (hdo) then
	891	h2oflux(ig) = pdqsdif(ig,igcm_h2o_ice)
	892	endif
[2260]	893
[38]	894	c write(,)'flux vers le sol=',pdqsdif(ig,nq)
	895	z1(ig)=1./(za(ig,1)+ zb(ig,2)*(1.-zd(ig,2)))
	896	zc(ig,1)=(za(ig,1)*zq(ig,1,igcm_h2o_vap)+
[2316]	897	$ zb(ig,2)*zc(ig,2) +
	898	$ (-pdqsdif(ig,igcm_h2o_ice)) ptimestep) z1(ig)
[38]	899	zq1temp(ig)=zc(ig,1)
[2316]	900	endif !if .not.watercaptag(ig)
	901	endif ! if sublim more than surface
	902
[38]	903	c Starting upward calculations for water :
[669]	904	zq(ig,1,igcm_h2o_vap)=zq1temp(ig)
	905
[742]	906	!c Take into account H2O latent heat in surface energy budget
	907	!c We solve dT/dt = (2834.3-0.28(T-To)-0.004(T-To)^2)1e3iceflux/cpp
	908	! tsrf_lw(ig) = ptsrf(ig) + pdtsrf(ig) *ptimestep
	909	!
	910	! alpha = exp(-4abs(T1-T2)pdqsdif(ig,igcm_h2o_ice)
	911	! & *ptimestep/pcapcal(ig))
	912	!
	913	! tsrf_lw(ig) = (tsrf_lw(ig)(T2-alphaT1)+T1T2(alpha-1))
	914	! & /(tsrf_lw(ig)(1-alpha)+alphaT2-T1) ! surface temperature at t+1
	915	!
	916	! pdtsrf(ig) = (tsrf_lw(ig)-ptsrf(ig))/ptimestep
[2179]	917	c Take into account the H2O latent heat impact on the surface temperature
[2218]	918	if (latentheat_surfwater) then
[2179]	919	tsrf_lh(ig) = ptsrf(ig) + pdtsrf(ig) *ptimestep
	920	lh=(2834.3-0.28*(tsrf_lh(ig)-To)-
	921	& 0.004(tsrf_lh(ig)-To)(tsrf_lh(ig)-To))*1.e+3
[2260]	922	pdtsrf(ig)= pdtsrf(ig) + (dwatercap_dif(ig)+
	923	& pdqsdif(ig,igcm_h2o_ice))*lh /pcapcal(ig)
[2179]	924	endif
[669]	925
	926	if(pqsurf(ig,igcm_h2o_ice)
[2316]	927	& +pdqsdif(ig,igcm_h2o_ice)*ptimestep
[669]	928	& .gt.frost_albedo_threshold) ! if there is still ice, T cannot exceed To
	929	& pdtsrf(ig) = min(pdtsrf(ig),(To-ptsrf(ig))/ptimestep) ! ice melt case
	930
[38]	931	ENDDO ! of DO ig=1,ngrid
	932	ELSE
	933	c Starting upward calculations for simple mixing of tracer (dust)
	934	DO ig=1,ngrid
	935	zq(ig,1,iq)=zc(ig,1)
	936	ENDDO
	937	END IF ! of IF ((water).and.(iq.eq.igcm_h2o_vap))
	938
	939	DO ilay=2,nlay
	940	DO ig=1,ngrid
[626]	941	zq(ig,ilay,iq)=zc(ig,ilay)+zd(ig,ilay)*zq(ig,ilay-1,iq)
[38]	942	ENDDO
	943	ENDDO
	944	enddo ! of do iq=1,nq
	945	end if ! of if(tracer)
	946
[2312]	947	C Diagnostic output for HDO
	948	if (hdo) then
	949	CALL WRITEDIAGFI(ngrid,'hdoflux',
	950	& 'hdoflux',
	951	& ' ',2,hdoflux)
	952	CALL WRITEDIAGFI(ngrid,'h2oflux',
	953	& 'h2oflux',
	954	& ' ',2,h2oflux)
	955	endif
	956
[38]	957	c-----------------------------------------------------------------------
	958	c 8. calcul final des tendances de la diffusion verticale
	959	c ----------------------------------------------------
	960
	961	DO ilev = 1, nlay
	962	DO ig=1,ngrid
	963	pdudif(ig,ilev)=( zu(ig,ilev)-
	964	$ (pu(ig,ilev)+pdufi(ig,ilev)*ptimestep) )/ptimestep
	965	pdvdif(ig,ilev)=( zv(ig,ilev)-
	966	$ (pv(ig,ilev)+pdvfi(ig,ilev)*ptimestep) )/ptimestep
[473]	967	hh = ph(ig,ilev)+pdhfi(ig,ilev)*ptimestep
	968	$ + (latcond*dmice(ig,ilev)/cpp)/ppopsk(ig,ilev)
	969	pdhdif(ig,ilev)=( zhs(ig,ilev)- hh )/ptimestep
[38]	970	ENDDO
	971	ENDDO
	972
	973	if (tracer) then
	974	DO iq = 1, nq
	975	DO ilev = 1, nlay
	976	DO ig=1,ngrid
	977	pdqdif(ig,ilev,iq)=(zq(ig,ilev,iq)-
	978	$ (pq(ig,ilev,iq) + pdqfi(ig,ilev,iq)*ptimestep))/ptimestep
	979	ENDDO
	980	ENDDO
	981	ENDDO
	982	end if
	983
	984	c ** diagnostique final
	985	c ------------------
	986
	987	IF(lecrit) THEN
	988	PRINT*,'In vdif'
	989	PRINT*,'Ts (t) and Ts (t+st)'
	990	WRITE(*,'(a10,3a15)')
	991	s 'theta(t)','theta(t+dt)','u(t)','u(t+dt)'
	992	PRINT*,ptsrf(ngrid/2+1),ztsrf2(ngrid/2+1)
	993	DO ilev=1,nlay
	994	WRITE(*,'(4f15.7)')
[473]	995	s ph(ngrid/2+1,ilev),zhs(ngrid/2+1,ilev),
[38]	996	s pu(ngrid/2+1,ilev),zu(ngrid/2+1,ilev)
	997
	998	ENDDO
	999	ENDIF
	1000
[1036]	1001	END SUBROUTINE vdifc
[1969]	1002
[2312]	1003	c====================================
	1004
	1005
[1969]	1006	END MODULE vdifc_mod

Note: See TracBrowser for help on using the repository browser.

Download in other formats:

Original Format