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newmicro.F @ 1087

Last change on this file since 1087 was 766, checked in by Laurent Fairhead, 17 years ago
Merge entre la version V3_conv et le HEAD YM, JG, LF
Property svn:eol-style set to `native` Property svn:keywords set to `Author Date Id Revision`
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Line
1	!
2	! $Header$
3	!
4	SUBROUTINE newmicro (paprs, pplay,ok_newmicro,
5	. t, pqlwp, pclc, pcltau, pclemi,
6	. pch, pcl, pcm, pct, pctlwp,
7	s xflwp, xfiwp, xflwc, xfiwc,
8	e ok_aie,
9	e sulfate, sulfate_pi,
10	e bl95_b0, bl95_b1,
11	s cldtaupi, re, fl)
12	USE dimphy
13	IMPLICIT none
14	c======================================================================
15	c Auteur(s): Z.X. Li (LMD/CNRS) date: 19930910
16	c Objet: Calculer epaisseur optique et emmissivite des nuages
17	c======================================================================
18	c Arguments:
19	c t-------input-R-temperature
20	c pqlwp---input-R-eau liquide nuageuse dans l'atmosphere (kg/kg)
21	c pclc----input-R-couverture nuageuse pour le rayonnement (0 a 1)
22	c
23	c ok_aie--input-L-apply aerosol indirect effect or not
24	c sulfate-input-R-sulfate aerosol mass concentration [um/m^3]
25	c sulfate_pi-input-R-dito, pre-industrial value
26	c bl95_b0-input-R-a parameter, may be varied for tests (s-sea, l-land)
27	c bl95_b1-input-R-a parameter, may be varied for tests ( -"- )
28	c
29	c cldtaupi-output-R-pre-industrial value of cloud optical thickness,
30	c needed for the diagnostics of the aerosol indirect
31	c radiative forcing (see radlwsw)
32	c re------output-R-Cloud droplet effective radius multiplied by fl [um]
33	c fl------output-R-Denominator to re, introduced to avoid problems in
34	c the averaging of the output. fl is the fraction of liquid
35	c water clouds within a grid cell
36	c pcltau--output-R-epaisseur optique des nuages
37	c pclemi--output-R-emissivite des nuages (0 a 1)
38	c======================================================================
39	C
40	#include "YOMCST.h"
41	c
42	cym#include "dimensions.h"
43	cym#include "dimphy.h"
44	#include "nuage.h"
45	cIM cf. CR: include pour NOVLP et ZEPSEC
46	#include "radepsi.h"
47	#include "radopt.h"
48	REAL paprs(klon,klev+1), pplay(klon,klev)
49	REAL t(klon,klev)
50	c
51	REAL pclc(klon,klev)
52	REAL pqlwp(klon,klev)
53	REAL pcltau(klon,klev), pclemi(klon,klev)
54	c
55	REAL pct(klon), pctlwp(klon), pch(klon), pcl(klon), pcm(klon)
56	c
57	LOGICAL lo
58	c
59	REAL cetahb, cetamb
60	PARAMETER (cetahb = 0.45, cetamb = 0.80)
61	C
62	INTEGER i, k
63	cIM: 091003 REAL zflwp, zradef, zfice, zmsac
64	REAL zflwp(klon), zradef, zfice, zmsac
65	cIM: 091003 rajout
66	REAL xflwp(klon), xfiwp(klon)
67	REAL xflwc(klon,klev), xfiwc(klon,klev)
68	c
69	REAL radius, rad_chaud
70	cc PARAMETER (rad_chau1=13.0, rad_chau2=9.0, rad_froid=35.0)
71	ccc PARAMETER (rad_chaud=15.0, rad_froid=35.0)
72	c sintex initial PARAMETER (rad_chaud=10.0, rad_froid=30.0)
73	REAL coef, coef_froi, coef_chau
74	PARAMETER (coef_chau=0.13, coef_froi=0.09)
75	REAL seuil_neb, t_glace
76	PARAMETER (seuil_neb=0.001, t_glace=273.0-15.0)
77	INTEGER nexpo ! exponentiel pour glace/eau
78	PARAMETER (nexpo=6)
79	ccc PARAMETER (nexpo=1)
80
81	c -- sb:
82	logical ok_newmicro
83	c parameter (ok_newmicro=.FALSE.)
84	cIM: 091003 real rel, tc, rei, zfiwp
85	real rel, tc, rei, zfiwp(klon)
86	real k_liq, k_ice0, k_ice, DF
87	parameter (k_liq=0.0903, k_ice0=0.005) ! units=m2/g
88	parameter (DF=1.66) ! diffusivity factor
89	c sb --
90	cjq for the aerosol indirect effect
91	cjq introduced by Johannes Quaas (quaas@lmd.jussieu.fr), 27/11/2003
92	cjq
93	LOGICAL ok_aie ! Apply AIE or not?
94	LOGICAL ok_a1lwpdep ! a1 LWP dependent?
95
96	REAL sulfate(klon, klev) ! sulfate aerosol mass concentration [ug m-3]
97	REAL cdnc(klon, klev) ! cloud droplet number concentration [m-3]
98	REAL re(klon, klev) ! cloud droplet effective radius [um]
99	REAL sulfate_pi(klon, klev) ! sulfate aerosol mass concentration [ug m-3] (pre-industrial value)
100	REAL cdnc_pi(klon, klev) ! cloud droplet number concentration [m-3] (pi value)
101	REAL re_pi(klon, klev) ! cloud droplet effective radius [um] (pi value)
102
103	REAL fl(klon, klev) ! xliq * rneb (denominator to re; fraction of liquid water clouds within the grid cell)
104
105	REAL bl95_b0, bl95_b1 ! Parameter in B&L 95-Formula
106
107	REAL cldtaupi(klon, klev) ! pre-industrial cloud opt thickness for diag
108	cjq-end
109	cIM cf. CR:parametres supplementaires
110	REAL zclear(klon)
111	REAL zcloud(klon)
112	c
113	c Calculer l'epaisseur optique et l'emmissivite des nuages
114	c
115	cIM inversion des DO
116	DO i = 1, klon
117	xflwp(i)=0.
118	xfiwp(i)=0.
119	cccccccccccc!CDIR NOVECTOR
120	DO k = 1, klev
121	c
122	xflwc(i,k)=0.
123	xfiwc(i,k)=0.
124	c
125	rad_chaud = rad_chau1
126	IF (k.LE.3) rad_chaud = rad_chau2
127	pclc(i,k) = MAX(pclc(i,k), seuil_neb)
128	zflwp(i) = 1000.*pqlwp(i,k)/RG/pclc(i,k)
129	. *(paprs(i,k)-paprs(i,k+1))
130	zfice = 1.0 - (t(i,k)-t_glace) / (273.13-t_glace)
131	zfice = MIN(MAX(zfice,0.0),1.0)
132	zfice = zfice**nexpo
133	radius = rad_chaud * (1.-zfice) + rad_froid * zfice
134	coef = coef_chau * (1.-zfice) + coef_froi * zfice
135	pcltau(i,k) = 3.0/2.0 * zflwp(i) / radius
136	pclemi(i,k) = 1.0 - EXP( - coef * zflwp(i))
137
138	if (ok_newmicro) then
139
140	c -- liquid/ice cloud water paths:
141
142	zfice = 1.0 - (t(i,k)-t_glace) / (273.13-t_glace)
143	zfice = MIN(MAX(zfice,0.0),1.0)
144
145	zflwp(i) = 1000.(1.-zfice)pqlwp(i,k)/pclc(i,k)
146	: *(paprs(i,k)-paprs(i,k+1))/RG
147	zfiwp(i) = 1000.zficepqlwp(i,k)/pclc(i,k)
148	: *(paprs(i,k)-paprs(i,k+1))/RG
149
150	xflwp(i) = xflwp(i)+ (1.-zfice)*pqlwp(i,k)
151	: *(paprs(i,k)-paprs(i,k+1))/RG
152	xfiwp(i) = xfiwp(i)+ zfice*pqlwp(i,k)
153	: *(paprs(i,k)-paprs(i,k+1))/RG
154
155	cIM Total Liquid/Ice water content
156	xflwc(i,k) = xflwc(i,k)+(1.-zfice)*pqlwp(i,k)
157	xfiwc(i,k) = xfiwc(i,k)+zfice*pqlwp(i,k)
158	cIM In-Cloud Liquid/Ice water content
159	c xflwc(i,k) = xflwc(i,k)+(1.-zfice)*pqlwp(i,k)/pclc(i,k)
160	c xfiwc(i,k) = xfiwc(i,k)+zfice*pqlwp(i,k)/pclc(i,k)
161
162	c -- effective cloud droplet radius (microns):
163
164	c for liquid water clouds:
165	IF (ok_aie) THEN
166	! Formula "D" of Boucher and Lohmann, Tellus, 1995
167	!
168	cdnc(i,k) = 10.*(bl95_b0+bl95_b1
169	. log(MAX(sulfate(i,k),1.e-4))/log(10.))*1.e6 !-m-3
170	! Cloud droplet number concentration (CDNC) is restricted
171	! to be within [20, 1000 cm^3]
172	!
173	cdnc(i,k)=MIN(1000.e6,MAX(20.e6,cdnc(i,k)))
174	!
175	!
176	cdnc_pi(i,k) = 10.*(bl95_b0+bl95_b1
177	. log(MAX(sulfate_pi(i,k),1.e-4))/log(10.))*1.e6 !-m-3
178	cdnc_pi(i,k)=MIN(1000.e6,MAX(20.e6,cdnc_pi(i,k)))
179	!
180	!
181	! air density: pplay(i,k) / (RD * zT(i,k))
182	! factor 1.1: derive effective radius from volume-mean radius
183	! factor 1000 is the water density
184	! _chaud means that this is the CDR for liquid water clouds
185	!
186	rad_chaud =
187	. 1.1 * ( (pqlwp(i,k) * pplay(i,k) / (RD * T(i,k)) )
188	. / (4./3. * RPI * 1000. * cdnc(i,k)) )**(1./3.)
189	!
190	! Convert to um. CDR shall be at least 3 um.
191	!
192	c rad_chaud = MAX(rad_chaud*1.e6, 3.)
193	rad_chaud = MAX(rad_chaud*1.e6, 5.)
194
195	! Pre-industrial cloud opt thickness
196	!
197	! "radius" is calculated as rad_chaud above (plus the
198	! ice cloud contribution) but using cdnc_pi instead of
199	! cdnc.
200	radius =
201	. 1.1 * ( (pqlwp(i,k) * pplay(i,k) / (RD * T(i,k)) )
202	. / (4./3. * RPI * 1000. * cdnc_pi(i,k)) )**(1./3.)
203	radius = MAX(radius*1.e6, 5.)
204
205	tc = t(i,k)-273.15
206	rei = 0.71*tc + 61.29
207	if (tc.le.-81.4) rei = 3.5
208	if (zflwp(i).eq.0.) radius = 1.
209	if (zfiwp(i).eq.0. .or. rei.le.0.) rei = 1.
210	cldtaupi(i,k) = 3.0/2.0 * zflwp(i) / radius
211	. + zfiwp(i) * (3.448e-03 + 2.431/rei)
212	ENDIF ! ok_aie
213	! For output diagnostics
214	!
215	! Cloud droplet effective radius [um]
216	!
217	! we multiply here with f * xl (fraction of liquid water
218	! clouds in the grid cell) to avoid problems in the
219	! averaging of the output.
220	! In the output of IOIPSL, derive the real cloud droplet
221	! effective radius as re/fl
222	!
223	fl(i,k) = pclc(i,k)*(1.-zfice)
224	re(i,k) = rad_chaud*fl(i,k)
225
226	c-jq end
227
228	rel = rad_chaud
229	c for ice clouds: as a function of the ambiant temperature
230	c [formula used by Iacobellis and Somerville (2000), with an
231	c asymptotical value of 3.5 microns at T<-81.4 C added to be
232	c consistent with observations of Heymsfield et al. 1986]:
233	tc = t(i,k)-273.15
234	rei = 0.71*tc + 61.29
235	if (tc.le.-81.4) rei = 3.5
236
237	c -- cloud optical thickness :
238
239	c [for liquid clouds, traditional formula,
240	c for ice clouds, Ebert & Curry (1992)]
241
242	if (zflwp(i).eq.0.) rel = 1.
243	if (zfiwp(i).eq.0. .or. rei.le.0.) rei = 1.
244	pcltau(i,k) = 3.0/2.0 * ( zflwp(i)/rel )
245	. + zfiwp(i) * (3.448e-03 + 2.431/rei)
246
247	c -- cloud infrared emissivity:
248
249	c [the broadband infrared absorption coefficient is parameterized
250	c as a function of the effective cld droplet radius]
251
252	c Ebert and Curry (1992) formula as used by Kiehl & Zender (1995):
253	k_ice = k_ice0 + 1.0/rei
254
255	pclemi(i,k) = 1.0
256	. - EXP( - coef_chauzflwp(i) - DFk_ice*zfiwp(i) )
257
258	endif ! ok_newmicro
259
260	lo = (pclc(i,k) .LE. seuil_neb)
261	IF (lo) pclc(i,k) = 0.0
262	IF (lo) pcltau(i,k) = 0.0
263	IF (lo) pclemi(i,k) = 0.0
264
265	IF (lo) cldtaupi(i,k) = 0.0
266	IF (.NOT.ok_aie) cldtaupi(i,k)=pcltau(i,k)
267	ENDDO
268	ENDDO
269	ccc DO k = 1, klev
270	ccc DO i = 1, klon
271	ccc t(i,k) = t(i,k)
272	ccc pclc(i,k) = MAX( 1.e-5 , pclc(i,k) )
273	ccc lo = pclc(i,k) .GT. (2.*1.e-5)
274	ccc zflwp = pqlwp(i,k)1000.(paprs(i,k)-paprs(i,k+1))
275	ccc . /(rg*pclc(i,k))
276	ccc zradef = 10.0 + (1.-sigs(k))*45.0
277	ccc pcltau(i,k) = 1.5 * zflwp / zradef
278	ccc zfice=1.0-MIN(MAX((t(i,k)-263.)/(273.-263.),0.0),1.0)
279	ccc zmsac = 0.13(1.0-zfice) + 0.08zfice
280	ccc pclemi(i,k) = 1.-EXP(-zmsac*zflwp)
281	ccc if (.NOT.lo) pclc(i,k) = 0.0
282	ccc if (.NOT.lo) pcltau(i,k) = 0.0
283	ccc if (.NOT.lo) pclemi(i,k) = 0.0
284	ccc ENDDO
285	ccc ENDDO
286	cccccc print*, 'pas de nuage dans le rayonnement'
287	cccccc DO k = 1, klev
288	cccccc DO i = 1, klon
289	cccccc pclc(i,k) = 0.0
290	cccccc pcltau(i,k) = 0.0
291	cccccc pclemi(i,k) = 0.0
292	cccccc ENDDO
293	cccccc ENDDO
294	C
295	C COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS
296	C
297	cIM cf. CR:test: calcul prenant ou non en compte le recouvrement
298	cinitialisations
299	DO i=1,klon
300	zclear(i)=1.
301	zcloud(i)=0.
302	pch(i)=1.0
303	pcm(i) = 1.0
304	pcl(i) = 1.0
305	pctlwp(i) = 0.0
306	ENDDO
307	C
308	cIM cf CR DO k=1,klev
309	DO k = klev, 1, -1
310	DO i = 1, klon
311	pctlwp(i) = pctlwp(i)
312	. + pqlwp(i,k)*(paprs(i,k)-paprs(i,k+1))/RG
313	cIM cf. CR
314	IF (NOVLP.EQ.1) THEN
315	zclear(i)=zclear(i)*(1.-MAX(pclc(i,k),zcloud(i)))
316	s /(1.-MIN(zcloud(i),1.-ZEPSEC))
317	pct(i)=1.-zclear(i)
318	if (pplay(i,k).LE.cetahb*paprs(i,1)) then
319	pch(i) = pch(i)*(1.-MAX(pclc(i,k),zcloud(i)))
320	s /(1.-MIN(zcloud(i),1.-ZEPSEC))
321	else if (pplay(i,k).GT.cetahb*paprs(i,1) .AND.
322	. pplay(i,k).LE.cetamb*paprs(i,1)) then
323	pcm(i) = pcm(i)*(1.-MAX(pclc(i,k),zcloud(i)))
324	s /(1.-MIN(zcloud(i),1.-ZEPSEC))
325	else if (pplay(i,k).GT.cetamb*paprs(i,1)) then
326	pcl(i) = pcl(i)*(1.-MAX(pclc(i,k),zcloud(i)))
327	s /(1.-MIN(zcloud(i),1.-ZEPSEC))
328	endif
329	zcloud(i)=pclc(i,k)
330	ELSE IF (NOVLP.EQ.2) THEN
331	zcloud(i)=MAX(pclc(i,k),zcloud(i))
332	pct(i)=zcloud(i)
333	if (pplay(i,k).LE.cetahb*paprs(i,1)) then
334	pch(i) = MIN(pclc(i,k),pch(i))
335	else if (pplay(i,k).GT.cetahb*paprs(i,1) .AND.
336	. pplay(i,k).LE.cetamb*paprs(i,1)) then
337	pcm(i) = MIN(pclc(i,k),pcm(i))
338	else if (pplay(i,k).GT.cetamb*paprs(i,1)) then
339	pcl(i) = MIN(pclc(i,k),pcl(i))
340	endif
341	ELSE IF (NOVLP.EQ.3) THEN
342	zclear(i)=zclear(i)*(1.-pclc(i,k))
343	pct(i)=1-zclear(i)
344	if (pplay(i,k).LE.cetahb*paprs(i,1)) then
345	pch(i) = pch(i)*(1.0-pclc(i,k))
346	else if (pplay(i,k).GT.cetahb*paprs(i,1) .AND.
347	. pplay(i,k).LE.cetamb*paprs(i,1)) then
348	pcm(i) = pcm(i)*(1.0-pclc(i,k))
349	else if (pplay(i,k).GT.cetamb*paprs(i,1)) then
350	pcl(i) = pcl(i)*(1.0-pclc(i,k))
351	endif
352	ENDIF
353	ENDDO
354	ENDDO
355	C
356	DO i = 1, klon
357	cIM cf. CR pct(i)=1.-pct(i)
358	pch(i)=1.-pch(i)
359	pcm(i)=1.-pcm(i)
360	pcl(i)=1.-pcl(i)
361	ENDDO
362	C
363	RETURN
364	END

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