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calchim.F90 @ 3667

Last change on this file since 3667 was 3318, checked in by slebonnois, 19 months ago
Titan PCM update : optics + microphysics
File size: 23.0 KB

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1	SUBROUTINE calchim(ngrid,qy_c,declin,dtchim, &
2	ctemp,cpphi,cpphis,cplay,cplev,czlay,czlev,dqyc)
3
4	!---------------------------------------------------------------------------------------------------------
5	!
6	! Purpose : Interface subroutine to photochemical C model for Titan GCM.
7	! -------
8	! The subroutine computes the chemical processes for a single vertical column.
9	!
10	! - Only tendencies are returned.
11	! - With moyzon_ch=.true. and input vectors zonally averaged
12	! the calculation is done only once per lat. band
13	!
14	! Authors: + S. Lebonnois : 01/2000 \| 09/2003
15	! ------- adaptation for Titan 3D : 02/2009
16	! adaptation for // : 04/2013
17	! extension chemistry up to 1300km : 10/2013
18	!
19	! + J. Vatant d'Ollone
20	! + 02/17 - adaptation for the new generic-forked physics
21	! + 01/18 - 03/18 - Major transformations :
22	! - Upper chemistry fields are now stored in startfi
23	! and defined on a pressure grid from Vervack profile
24	! - These modifs enables to run chemistry with others resolution than 32x48x55 !
25	! - Only the actinic fluxes are still read in a 49-lat input but interp. on lat grid
26	! - Chemistry can still be done in 2D
27	! -> Calcul. once per band lat and put same tendency in all longi.
28	! Check for negs in physiq_mod.
29	! -> If procs sharing a lat band, no problem, the calcul will just be done twice.
30	! -> Will not work with Dynamico, where the chemistry will have to be done in 3D.
31	! ( and there'll be work to do to get rid of averaged fields )
32	!
33	! + 02/19 : To always have correct photodissociations rates, altitudes sent here by physiq are always
34	! calculated with effective g - and with reference to the body not the local surface -
35	! even if in physiq we keep altitudes coherent with dynamics !
36	!
37	! + STILL TO DO : + Replug the interaction with haze (cf titan.old) -> to see with JB.
38	! + Use iso_c_binding for the fortran-C exchanges.
39	!---------------------------------------------------------------------------------------------------------
40
41	! --------------------------------------------------------------------
42	! Structure :
43	! -----------
44	! 0. Declarations
45	! I. Init and firstcall
46	! 1. Read and store Vervack profile
47	! 2. Compute planetar averaged atm. properties
48	! 3. Init compound caracteristics
49	! 4. Init photodissociations rates from actinic fluxes
50	! 5. Init chemical reactions
51	! 6. Init eddy diffusion coeff
52	! II. Loop on latitudes/grid-points
53	! 0. Check on 2D chemistry
54	! 1. Compute atm. properties at grid points
55	! 2. Interpolate photodissociation rates at lat,alt,dec
56	! 3. Read composition
57	! 4. Call main solver gptitan C routine
58	! 5. Calculate output tendencies on advected tracers
59	! 6. Update upper chemistry fields
60	! 0bis. If 2D chemsitry, don't recalculate if needed
61	! -----------------------------------------------------------------
62
63	USE, INTRINSIC :: iso_c_binding
64	use tracer_h
65	USE comchem_h
66	USE dimphy
67	USE datafile_mod, ONLY: datadir
68	USE comcstfi_mod, ONLY: g, rad, pi, r, kbol
69	USE geometry_mod, ONLY: latitude
70	#ifndef MESOSCALE
71	USE logic_mod, ONLY: moyzon_ch
72	USE moyzon_mod, ONLY: tmoy, playmoy
73	#endif
74
75	IMPLICIT NONE
76
77	! ------------------------------------------
78	! ********* 0. Declarations ***********
79	! ------------------------------------------
80
81	! Arguments
82	! ---------
83
84	INTEGER, INTENT(IN) :: ngrid ! Number of atmospheric columns.
85	REAL*8, DIMENSION(ngrid,klev,nkim), INTENT(IN) :: qy_c ! Chemical species on GCM layers after adv.+diss. (mol/mol).
86	REAL*8, INTENT(IN) :: declin ! Solar declination (rad).
87	REAL*8, INTENT(IN) :: dtchim ! Chemistry timsetep (s).
88	REAL*8, DIMENSION(ngrid,klev), INTENT(IN) :: ctemp ! Mid-layer temperature (K).
89	REAL*8, DIMENSION(ngrid,klev), INTENT(IN) :: cpphi ! Mid-layer geopotential (m2.s-2).
90	REAL*8, DIMENSION(ngrid), INTENT(IN) :: cpphis ! Surface geopotential (m2.s-2).
91	REAL*8, DIMENSION(ngrid,klev), INTENT(IN) :: cplay ! Mid-layer pressure (Pa).
92	REAL*8, DIMENSION(ngrid,klev+1), INTENT(IN) :: cplev ! Inter-layer pressure (Pa).
93	REAL*8, DIMENSION(ngrid,klev), INTENT(IN) :: czlay ! Mid-layer effective altitude (m) : ref = geoid.
94	REAL*8, DIMENSION(ngrid,klev+1), INTENT(IN) :: czlev ! Inter-layer effective altitude (m) ref = geoid.
95
96	REAL*8, DIMENSION(ngrid,klev,nkim), INTENT(OUT) :: dqyc ! Chemical species tendencies on GCM layers (mol/mol/s).
97
98	! Local variables :
99	! -----------------
100
101	INTEGER :: i , l, ic, ig, igm1
102
103	INTEGER :: dec, idec, ipres, ialt, klat
104
105	REAL*8 :: declin_c ! Declination (deg).
106	REAL*8 :: factp, factalt, factdec, factlat, krpddec, krpddecp1, krpddecm1
107	REAL*8 :: temp1, logp
108
109	! Variables sent into chemistry module (must be in double precision)
110	! ------------------------------------------------------------------
111
112	REAL*8, DIMENSION(nlaykim_tot) :: temp_c ! Temperature (K).
113	REAL*8, DIMENSION(nlaykim_tot) :: press_c ! Pressure (Pa).
114	REAL*8, DIMENSION(nlaykim_tot) :: phi_c ! Geopotential (m2.s-2) - actually not sent in chem. module but used to compute alts.
115	REAL*8, DIMENSION(nlaykim_tot) :: nb ! Density (cm-3).
116
117	REAL*8, DIMENSION(nlaykim_tot,nkim) :: cqy ! Chemical species in whole column (mol/mol) sent to chem. module.
118	REAL*8, DIMENSION(nlaykim_tot,nkim) :: cqy0 ! " " " " " " before modifs.
119
120	REAL*8 :: surfhaze(nlaykim_tot)
121	REAL*8 :: cprodaer(nlaykim_tot,4), cmaer(nlaykim_tot,4)
122	REAL*8 :: ccsn(nlaykim_tot,4), ccsh(nlaykim_tot,4)
123
124	REAL*8, DIMENSION(nlaykim_tot) :: rmil ! Mid-layer distance (km) to planetographic center.
125	REAL*8, DIMENSION(nlaykim_tot) :: rinter ! Inter-layer distance (km) to planetographic center (RA grid in chem. module).
126	! NB : rinter is on nlaykim_tot too, we don't care of the uppermost layer upper boundary altitude.
127
128	! Saved variables initialized at firstcall
129	! ----------------------------------------
130
131	LOGICAL, SAVE :: firstcall = .TRUE.
132	!$OMP THREADPRIVATE(firstcall)
133
134	REAL*8, DIMENSION(:), ALLOCATABLE, SAVE :: kedd ! Eddy mixing coefficient for upper chemistry (cm^2.s-1)
135	!$OMP THREADPRIVATE(kedd)
136
137	REAL*8, DIMENSION(:,:), ALLOCATABLE, SAVE :: md ! Mean molecular diffusion coefficients (cm^2.s-1)
138	REAL*8, DIMENSION(:), ALLOCATABLE, SAVE :: mass ! Molar mass of the compounds (g.mol-1)
139	!$OMP THREADPRIVATE(mass,md)
140
141	REAL*8, DIMENSION(:), ALLOCATABLE, SAVE :: r1d, ct1d, p1d, t1d ! Vervack profile
142	! JVO 18 : No threadprivate for those as they'll be read in tcp.ver by master
143
144	REAL*8, DIMENSION(:,:,:,:), ALLOCATABLE, SAVE :: krpd ! Photodissociations rate table
145	REAL*8, DIMENSION(:,:) , ALLOCATABLE, SAVE :: krate ! Reactions rate ( photo + chem )
146	!$OMP THREADPRIVATE(krpd,krate)
147
148	INTEGER, DIMENSION(:), ALLOCATABLE, SAVE :: nom_prod, nom_perte
149	INTEGER, DIMENSION(:,:), ALLOCATABLE, SAVE :: reactif
150	INTEGER, DIMENSION(:,:), ALLOCATABLE, SAVE :: prod
151	INTEGER, DIMENSION(:,:,:), ALLOCATABLE, SAVE :: perte
152	!$OMP THREADPRIVATE(nom_prod,nom_perte,reactif,prod,perte)
153
154	! TEMPORARY : Dummy parameters without microphysics
155	! Here to keep the whole stuff running without modif chem. module
156	! ---------------------------------------------------------------
157
158	INTEGER :: utilaer(16)
159	INTEGER :: aerprod = 0
160	INTEGER :: htoh2 = 0
161
162	! -----------------------------------------------------------------------
163	! *************** I. Initialisations and Firstcall ******************
164	! -----------------------------------------------------------------------
165
166	IF (firstcall) THEN
167
168	PRINT*, 'CHIMIE, premier appel'
169
170	if (ngrid .eq. 1) then ! if 1D no dynamic mixing, we set the kedd in all column
171	call check(nlaykim_tot,0,nlrt_kim,nkim)
172	else
173	call check(nlaykim_tot,klev-15,nlrt_kim,nkim)
174	endif
175
176	ALLOCATE(r1d(131))
177	ALLOCATE(ct1d(131))
178	ALLOCATE(p1d(131))
179	ALLOCATE(t1d(131))
180
181	ALLOCATE(md(nlaykim_tot,nkim))
182	ALLOCATE(mass(nkim))
183
184	ALLOCATE(kedd(nlaykim_tot))
185
186	ALLOCATE(krate(nlaykim_tot,nr_kim))
187	ALLOCATE(krpd(nd_kim+1,nlrt_kim,15,nlat_actfluxes))
188
189	ALLOCATE(nom_prod(nkim))
190	ALLOCATE(nom_perte(nkim))
191	ALLOCATE(reactif(5,nr_kim))
192	ALLOCATE(prod(200,nkim))
193	ALLOCATE(perte(2,200,nkim))
194
195	! 0. Deal with characters for C-interoperability
196	! ----------------------------------------------
197	! NB ( JVO 19 ) : Using iso_c_binding would do things in an even cleaner way !
198	DO ic=1,nkim
199	nomqy_c(ic) = trim(cnames(ic))//char(0) ! Add the C null terminator
200	ENDDO
201	nomqy_c(nkim+1)="HV"//char(0) ! For photodissociations
202
203	! 1. Read Vervack profile "tcp.ver", once for all
204	! -----------------------------------------------
205
206	!$OMP MASTER
207	OPEN(11,FILE=TRIM(datadir)//'/tcp.ver',STATUS='old')
208	READ(11,*)
209	DO i=1,131
210	READ(11,*) r1d(i), t1d(i), ct1d(i), p1d(i)
211	! For debug :
212	! -----------
213	! PRINT*, "tcp.ver", r1d(i), t1d(i), ct1d(i), p1d(i)
214	ENDDO
215	CLOSE(11)
216	!$OMP END MASTER
217	!$OMP BARRIER
218
219	! 2. Calculation of temp_c, densities and altitudes in planetary average
220	! ----------------------------------------------------------------------
221
222	! JVO18 : altitudes are no more calculated in firstcall, as I set kedd in pressure grid
223
224	! a. For GCM layers we just copy-paste ( assuming that physiq always send correct altitudes ! )
225
226	PRINT*,'Init chemistry : pressure, density, temperature ... :'
227	PRINT*,'level, press_c (mbar), nb (cm-3), temp_c (K)'
228
229	#ifndef MESOSCALE
230	!! JVO 20 : I put this CPP key because mesoscale cannot access tmoy and playmoy,
231	! you should fix this when you will propeerly use chemistry !
232
233	IF (ngrid.NE.1) THEN
234	DO l=1,klev
235	temp_c(l) = tmoy(l) ! K
236	press_c(l) = playmoy(l)/100. ! mbar
237	nb(l) = 1.e-4press_c(l) / (kboltemp_c(l)) ! cm-3
238	PRINT*, l, press_c(l), nb(l), temp_c(l)
239	ENDDO
240	ELSE
241	#endif
242	DO l=1,klev
243	temp_c(l) = ctemp(1,l) ! K
244	press_c(l) = cplay(1,l)/100. ! mbar
245	nb(l) = 1.e-4press_c(l) / (kboltemp_c(l)) ! cm-3
246	PRINT*, l, press_c(l), nb(l), temp_c(l)
247	ENDDO
248	#ifndef MESOSCALE
249	ENDIF
250	#endif
251
252	! b. Extension in upper atmosphere with Vervack profile
253	! NB : Maybe the transition klev/klev+1 is harsh if T profile different from Vervack ...
254
255	ipres=1
256	DO l=klev+1,nlaykim_tot
257	press_c(l) = preskim(l-klev) / 100.0
258	DO i=ipres,130
259	IF ( (press_c(l).LE.p1d(i)) .AND. (press_c(l).GT.p1d(i+1)) ) THEN
260	ipres=i
261	ENDIF
262	ENDDO
263	factp = (press_c(l)-p1d(ipres)) / (p1d(ipres+1)-p1d(ipres))
264
265	nb(l) = exp( log(ct1d(ipres))(1-factp) + log(ct1d(ipres+1)) factp )
266	temp_c(l) = t1d(ipres)(1-factp) + t1d(ipres+1)factp
267	PRINT*, l , press_c(l), nb(l), temp_c(l)
268	ENDDO
269
270	! 3. Compounds caracteristics
271	! ---------------------------
272	mass(:) = 0.0
273	call comp(nomqy_c,nb,temp_c,mass,md)
274	PRINT*,' Mass'
275	DO ic=1,nkim
276	PRINT*, nomqy_c(ic), mass(ic)
277	ENDDO
278
279	! 4. Photodissociation rates
280	! --------------------------
281	call disso(krpd,nlat_actfluxes)
282
283	! 5. Init. chemical reactions with planetary average T prof.
284	! ----------------------------------------------------------
285
286	! NB : Chemical reactions rate are assumed to be constant within the T range of Titan's atm
287	! so we fill their krate once for all but krate for photodiss will be filled at each timestep
288
289	call chimie(nomqy_c,nb,temp_c,krate,reactif, &
290	nom_perte,nom_prod,perte,prod)
291
292	! 6. Eddy mixing coefficients (constant with time and space)
293	! ----------------------------------------------------------
294
295	kedd(:) = 1.e3 ! Default value =/= zero
296
297	! NB : Eddy coeffs (e.g. Lavvas et al 08, Yelle et al 08) in altitude but they're rather linked to pressure
298	! Below GCM top we have dynamic mixing and for levs < nld=klev-15 the chem. solver ignores diffusion
299
300	!! First calculate kedd for upper chemistry layers
301	!DO l=klev-4,nlaykim_tot
302	! logp=-log10(press_c(l))
303	!! 2E6 at 400 km ~ 10-2 mbar
304	! IF ( logp.ge.2.0 .and. logp.le.3.0 ) THEN
305	! kedd(l) = 2.e6 * 5.0**(logp-2.0)
306	!! 1E7 at 500 km ~ 10-3 mbar
307	! ELSE IF ( logp.ge.3.0 .and. logp.le.4.0 ) THEN
308	! kedd(l) = 1.e7 * 3.0**(logp-3.0)
309	!! 3E7 above 700 km ~ 10-4 mbar
310	! ELSEIF ( logp.gt.4.0 ) THEN
311	! kedd(l) = 3.e7
312	! ENDIF
313	!ENDDO
314
315	! Kedd from (E7) in Vuitton 2019
316	if (ngrid .eq. 1) then ! if 1D no dynamic mixing, we set the kedd in all column
317	DO l=1,nlaykim_tot
318	kedd(l) = 300.0 * ( 1.0E2 / press_c(l) )*1.5 3.0E7 / &
319	( 300.0 * ( 1.0E2 / press_c(l) )**1.5 + 3.0E7 )
320	ENDDO
321	else
322	DO l=klev-4,nlaykim_tot
323	! JVO 18 : We keep the nominal profile in the GCM 5 upper layers
324	! to have a correct vertical mixing in the sponge layer
325	kedd(l) = 300.0 * ( 1.0E2 / press_c(l) )*1.5 3.0E7 / &
326	( 300.0 * ( 1.0E2 / press_c(l) )**1.5 + 3.0E7 )
327	ENDDO
328	endif
329
330	if (ngrid .gt. 1) then ! not in 1D, no dynamic mixing
331	! Then adjust 10 layers profile fading to default value depending on kedd(ptop)
332	DO l=klev-15,klev-5
333	temp1 = ( log10(press_c(l)/press_c(klev-15)) ) / ( log10(press_c(klev-4)/press_c(klev-15)) )
334	kedd(l) = 10.*( 3.0 + log10(kedd(klev-4)/1.e3) temp1 )
335	ENDDO
336	endif
337
338	! [BdBdT : On force la chimie... kedd nul dans le PCM]
339	kedd(:klev) = 1.e3 ! Default value =/= zero
340
341	firstcall = .FALSE.
342	ENDIF ! firstcall
343
344	declin_c = declin*180./pi
345
346	! -----------------------------------------------------------------------
347	! ********************* II. Loop on latitudes ***********************
348	! -----------------------------------------------------------------------
349
350	DO ig=1,ngrid
351
352	IF (ig.eq.1) THEN
353	igm1=1
354	ELSE
355	igm1=ig-1
356	ENDIF
357
358	! If 2D chemistry, trick to do the calculation only once per latitude band within the chunk
359	! NB1 : Will be obsolete with DYNAMICO, the chemistry will necessarly be 3D
360	! NB2 : Test of same latitude with dlat=0.1 : I think that if you run sims better than 1/10th degree then
361	! either it's with Dynamico and doesn't apply OR it is more than enough in terms of "preco / calc time" !
362	! -------------------------------------------------------------------------------------------------------
363
364	#ifndef MESOSCALE
365	IF ( ( moyzon_ch .AND. ( ig.EQ.1 .OR. (ABS(latitude(ig)-latitude(igm1)).GT.0.1*pi/180.0)) ) .OR. (.NOT. moyzon_ch) ) THEN
366	#endif
367	! 1. Compute altitude for the grid point with hydrostat. equilib.
368	! ---------------------------------------------------------------
369
370	! a. For GCM layers we just copy-paste
371	! JVO 19 : Now physiq always sent correct altitudes with effective g for chemistry ( even if it's not the case in physiq )
372
373	DO l=1,klev
374	rinter(l) = (czlev(ig,l)+rad)/1000.0 ! km
375	rmil(l) = (czlay(ig,l)+rad)/1000.0 ! km
376	temp_c(l) = ctemp(ig,l) ! K
377	phi_c(l) = cpphi(ig,l) ! m2.s-2
378	press_c(l) = cplay(ig,l)/100. ! mbar
379	nb(l) = 1.e-4press_c(l) / (kboltemp_c(l)) ! cm-3
380	ENDDO
381	rinter(klev+1)=( (czlay(ig,klev) + ( czlay(ig,klev) - czlev(ig,klev))) +rad )/1000. ! You shall not use czlev(zlev+1) whose value is 1.e7 !
382
383	! b. Extension in upper atmosphere with Vervack profile
384
385	ipres=1
386	DO l=klev+1,nlaykim_tot
387	press_c(l) = preskim(l-klev) / 100.0
388	DO i=ipres,130
389	IF ( (press_c(l).LE.p1d(i)) .AND. (press_c(l).GT.p1d(i+1)) ) THEN
390	ipres=i
391	ENDIF
392	ENDDO
393	factp = (press_c(l)-p1d(ipres)) / (p1d(ipres+1)-p1d(ipres))
394
395	nb(l) = exp( log(ct1d(ipres))(1-factp) + log(ct1d(ipres+1)) factp )
396	temp_c(l) = t1d(ipres)(1-factp) + t1d(ipres+1)factp
397	ENDDO
398
399	! We build altitude with hydrostatic equilibrium on preskim grid with Vervack profile
400	! ( keeping in mind that preskim is built based on Vervack profile with dz=10km )
401
402	DO l=klev+1,nlaykim_tot
403
404	! Compute geopotential on the upper grid with effective g to have correct altitudes
405	! ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
406
407	temp1 = 0.5*(temp_c(l-1)+temp_c(l)) ! interlayer temp
408	phi_c(l) = phi_c(l-1) + rtemp1log(press_c(l-1)/press_c(l)) ! Geopotential assuming hydrostatic equilibrium
409
410	rmil(l) = ( gradrad / (g*rad - ( phi_c(l) + cpphis(ig) ) ) ) / 1000.0 ! z(phi) with g varying with altitude with reference to the geoid
411	ENDDO
412
413	DO l=klev+2,nlaykim_tot
414	rinter(l) = 0.5*(rmil(l-1) + rmil(l)) ! should be balanced with the intermediate pressure rather than 0.5
415	ENDDO
416
417	! 2. From krpd, compute krate for dissociations (declination-latitude-altitude interpolation)
418	! -------------------------------------------------------------------------------------------
419
420	! a. Calculate declination dependence
421
422	if ((declin_c*10+267).lt.14.) then
423	idec = 0
424	dec = 0
425	else
426	if ((declin_c*10+267).gt.520.) then
427	idec = 14
428	dec = 534
429	else
430	idec = 1
431	dec = 27
432	do while( (declin_c*10+267).ge.real(dec+20) )
433	dec = dec+40
434	idec = idec+1
435	enddo
436	endif
437	endif
438	if ((declin_c.ge.-24.).and.(declin_c.le.24.)) then
439	factdec = ( declin_c - (dec-267)/10. ) / 4.
440	else
441	factdec = ( declin_c - (dec-267)/10. ) / 2.7
442	endif
443
444	! b. Calculate klat for interpolation on fixed latitudes of actinic fluxes input
445
446	klat=1
447	DO i=1,nlat_actfluxes
448	IF (latitude(ig).LT.lat_actfluxes(i)) klat=i
449	ENDDO
450	IF (klat==nlat_actfluxes) THEN ! avoid rounding problems
451	klat = nlat_actfluxes-1
452	factlat = 1.0
453	ELSE
454	factlat = (latitude(ig)-lat_actfluxes(klat))/(lat_actfluxes(klat+1)-lat_actfluxes(klat))
455	ENDIF
456
457	! c. Altitude loop
458
459	DO l=1,nlaykim_tot
460
461	! Calculate ialt for interpolation in altitude (krpd every 2 km)
462	ialt = int((rmil(l)-rad/1000.)/2.)+1
463	factalt = (rmil(l)-rad/1000.)/2.-(ialt-1)
464
465	! Altitude can go above top limit of UV levels - in this case we keep the 1310km top fluxes
466	IF (ialt.GT.nlrt_kim-1) THEN
467	ialt = nlrt_kim-1 ! avoid out-of-bound array
468	factalt = 1.0
469	ENDIF
470
471	DO i=1,nd_kim+1 ! nd_kim+1 is dissociation of N2 by GCR
472
473	krpddec = ( krpd(i,ialt ,idec+1,klat) * (1.0-factalt) &
474	+ krpd(i,ialt+1,idec+1,klat) * factalt ) * (1.0-factlat) &
475	+ ( krpd(i,ialt ,idec+1,klat+1) * (1.0-factalt) &
476	+ krpd(i,ialt+1,idec+1,klat+1) * factalt ) * factlat
477
478	if ( factdec.lt.0. ) then
479	krpddecm1 = ( krpd(i,ialt ,idec ,klat) * (1.0-factalt) &
480	+ krpd(i,ialt+1,idec ,klat) * factalt ) * (1.0-factlat) &
481	+ ( krpd(i,ialt ,idec ,klat+1) * (1.0-factalt) &
482	+ krpd(i,ialt+1,idec ,klat+1) * factalt ) * factlat
483	krate(l,i) = krpddecm1 * abs(factdec) + krpddec * ( 1.0 + factdec)
484	else if ( factdec.gt.0. ) then
485	krpddecp1 = ( krpd(i,ialt ,idec+2,klat) * (1.0-factalt) &
486	+ krpd(i,ialt+1,idec+2,klat) * factalt ) * (1.0-factlat) &
487	+ ( krpd(i,ialt ,idec+2,klat+1) * (1.0-factalt) &
488	+ krpd(i,ialt+1,idec+2,klat+1) * factalt ) * factlat
489	krate(l,i) = krpddecp1 * factdec + krpddec * ( 1.0 - factdec)
490	else if ( factdec.eq.0. ) then
491	krate(l,i) = krpddec
492	endif
493
494	ENDDO ! i=1,nd_kim+1
495	ENDDO ! l=1,nlaykim_tot
496
497	! 3. Read composition
498	! -------------------
499
500	DO ic=1,nkim
501	DO l=1,klev
502	cqy(l,ic) = qy_c(ig,l,ic) ! advected tracers for the GCM part converted to molar frac.
503	ENDDO
504
505	DO l=1,nlaykim_up
506	cqy(klev+l,ic) = ykim_up(ic,ig,l) ! ykim_up for the upper atm.
507	ENDDO
508	ENDDO
509
510	cqy0(:,:) = cqy(:,:) ! Stores compo. before modifs
511
512	! 4. Call main Titan chemistry C routine
513	! --------------------------------------
514
515	call gptitan(rinter,temp_c,nb, &
516	nomqy_c,cqy, &
517	dtchim,latitude(ig)*180./pi,mass,md, &
518	kedd,krate,reactif, &
519	nom_prod,nom_perte,prod,perte, &
520	aerprod,utilaer,cmaer,cprodaer,ccsn,ccsh, &
521	htoh2,surfhaze)
522
523	! 5. Calculates tendencies on composition for advected tracers
524	! ------------------------------------------------------------
525	DO ic=1,nkim
526	DO l=1,klev
527	dqyc(ig,l,ic) = (cqy(l,ic) - cqy0(l,ic))/dtchim ! (mol/mol/s)
528	ENDDO
529	ENDDO
530
531	! 6. Update ykim_up
532	! -----------------
533	DO ic=1,nkim
534	DO l=1,nlaykim_up
535	ykim_up(ic,ig,l) = cqy(klev+l,ic)
536	ENDDO
537	ENDDO
538	! NB: The full vertical composition grid will be created only for the outputs
539
540	#ifndef MESOSCALE
541	ELSE ! In 2D chemistry, if following grid point at same latitude, same zonal mean so don't do calculations again !
542	dqyc(ig,:,:) = dqyc(igm1,:,:) ! will be put back in 3D with longitudinal variations assuming same relative tendencies within a lat band
543	ykim_up(:,ig,:) = ykim_up(:,igm1,:) ! no horizontal mixing in upper layers -> no longitudinal variations
544	ENDIF
545	#endif
546
547	ENDDO
548
549	END SUBROUTINE calchim

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