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SUBROUTINE nuage (paprs, pplay, & |
module nuage_m |
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t, pqlwp, pclc, pcltau, pclemi, & |
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pch, pcl, pcm, pct, pctlwp, & |
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ok_aie, & |
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sulfate, sulfate_pi, & |
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bl95_b0, bl95_b1, & |
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cldtaupi, re, fl) |
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! |
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! From LMDZ4/libf/phylmd/nuage.F, version 1.1.1.1 2004/05/19 12:53:07 |
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! |
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use dimens_m |
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use dimphy |
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use SUPHEC_M |
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IMPLICIT none |
IMPLICIT none |
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!====================================================================== |
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! Auteur(s): Z.X. Li (LMD/CNRS) date: 19930910 |
contains |
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! Objet: Calculer epaisseur optique et emmissivite des nuages |
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!====================================================================== |
SUBROUTINE nuage (paprs, pplay, t, pqlwp, pclc, pcltau, pclemi, pch, pcl, & |
8 |
! Arguments: |
pcm, pct, pctlwp, ok_aie, sulfate, sulfate_pi, bl95_b0, bl95_b1, & |
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! t-------input-R-temperature |
cldtaupi, re, fl) |
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! pqlwp---input-R-eau liquide nuageuse dans l'atmosphere (kg/kg) |
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! pclc----input-R-couverture nuageuse pour le rayonnement (0 a 1) |
! From LMDZ4/libf/phylmd/nuage.F, version 1.1.1.1, 2004/05/19 12:53:07 |
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! ok_aie--input-L-apply aerosol indirect effect or not |
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! sulfate-input-R-sulfate aerosol mass concentration [um/m^3] |
use dimphy, only: klon, klev |
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! sulfate_pi-input-R-dito, pre-industrial value |
use nr_util, only: pi |
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! bl95_b0-input-R-a parameter, may be varied for tests (s-sea, l-land) |
use SUPHEC_M, only: rd, rg |
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! bl95_b1-input-R-a parameter, may be varied for tests ( -"- ) |
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! |
! Author: Z. X. Li (LMD/CNRS) |
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! cldtaupi-output-R-pre-industrial value of cloud optical thickness, |
! Date: 1993/09/10 |
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! needed for the diagnostics of the aerosol indirect |
! Objet: Calculer \'epaisseur optique et \'emissivit\'e des nuages |
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! radiative forcing (see radlwsw) |
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! re------output-R-Cloud droplet effective radius multiplied by fl [um] |
! Arguments: |
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! fl------output-R-Denominator to re, introduced to avoid problems in |
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! the averaging of the output. fl is the fraction of liquid |
REAL, intent(in):: paprs(klon, klev+1) |
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! water clouds within a grid cell |
real, intent(in):: pplay(klon, klev) |
25 |
! |
REAL, intent(in):: t(klon, klev) ! temperature |
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! pcltau--output-R-epaisseur optique des nuages |
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! pclemi--output-R-emissivite des nuages (0 a 1) |
REAL, intent(in):: pqlwp(klon, klev) |
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!====================================================================== |
! eau liquide nuageuse dans l'atmosphere (kg/kg) |
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! |
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! |
REAL, intent(inout):: pclc(klon, klev) |
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REAL, intent(in):: paprs(klon,klev+1) |
! couverture nuageuse pour le rayonnement (0 \`a 1) |
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real, intent(in):: pplay(klon,klev) |
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REAL, intent(in):: t(klon,klev) |
REAL pcltau(klon, klev), pclemi(klon, klev) |
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! |
! pcltau--output-R-epaisseur optique des nuages |
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REAL pclc(klon,klev) |
! pclemi--output-R-emissivite des nuages (0 a 1) |
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REAL pqlwp(klon,klev) |
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REAL pcltau(klon,klev), pclemi(klon,klev) |
REAL pch(klon), pcl(klon), pcm(klon), pct(klon), pctlwp(klon) |
38 |
! |
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REAL pct(klon), pctlwp(klon), pch(klon), pcl(klon), pcm(klon) |
!jq for the aerosol indirect effect |
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! |
!jq introduced by Johannes Quaas (quaas@lmd.jussieu.fr), 27/11/2003 |
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LOGICAL lo |
!jq |
42 |
! |
LOGICAL ok_aie ! Apply AIE or not? |
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REAL cetahb, cetamb |
! ok_aie--input-L-apply aerosol indirect effect or not |
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PARAMETER (cetahb = 0.45, cetamb = 0.80) |
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45 |
! |
REAL sulfate(klon, klev) ! sulfate aerosol mass concentration [ug m-3] |
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INTEGER i, k |
! sulfate-input-R-sulfate aerosol mass concentration [um/m^3] |
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REAL zflwp, zradef, zfice, zmsac |
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! |
REAL, intent(in):: sulfate_pi(klon, klev) ! sulfate aerosol mass concentration [ug m-3] (pre-industrial value) |
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REAL radius, rad_froid, rad_chaud, rad_chau1, rad_chau2 |
! sulfate_pi-input-R-dito, pre-industrial value |
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PARAMETER (rad_chau1=13.0, rad_chau2=9.0, rad_froid=35.0) |
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!cc PARAMETER (rad_chaud=15.0, rad_froid=35.0) |
REAL bl95_b0, bl95_b1 ! Parameter in B&L 95-Formula |
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! sintex initial PARAMETER (rad_chaud=10.0, rad_froid=30.0) |
! bl95_b0-input-R-a parameter, may be varied for tests (s-sea, l-land) |
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REAL coef, coef_froi, coef_chau |
! bl95_b1-input-R-a parameter, may be varied for tests (-"-) |
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PARAMETER (coef_chau=0.13, coef_froi=0.09) |
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REAL seuil_neb, t_glace |
REAL cldtaupi(klon, klev) ! pre-industrial cloud opt thickness for diag |
56 |
PARAMETER (seuil_neb=0.001, t_glace=273.0-15.0) |
! cldtaupi-output-R-pre-industrial value of cloud optical thickness, |
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INTEGER nexpo ! exponentiel pour glace/eau |
! needed for the diagnostics of the aerosol indirect |
58 |
PARAMETER (nexpo=6) |
! radiative forcing (see radlwsw) |
59 |
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!jq for the aerosol indirect effect |
REAL re(klon, klev) ! cloud droplet effective radius [um] |
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!jq introduced by Johannes Quaas (quaas@lmd.jussieu.fr), 27/11/2003 |
! re------output-R-Cloud droplet effective radius multiplied by fl [um] |
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!jq |
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LOGICAL ok_aie ! Apply AIE or not? |
REAL fl(klon, klev) ! xliq * rneb (denominator to re ; fraction of liquid water clouds within the grid cell) |
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! fl------output-R-Denominator to re, introduced to avoid problems in |
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REAL sulfate(klon, klev) ! sulfate aerosol mass concentration [ug m-3] |
! the averaging of the output. fl is the fraction of liquid |
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REAL cdnc(klon, klev) ! cloud droplet number concentration [m-3] |
! water clouds within a grid cell |
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REAL re(klon, klev) ! cloud droplet effective radius [um] |
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REAL sulfate_pi(klon, klev) ! sulfate aerosol mass concentration [ug m-3] (pre-industrial value) |
! Local: |
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REAL cdnc_pi(klon, klev) ! cloud droplet number concentration [m-3] (pi value) |
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REAL re_pi(klon, klev) ! cloud droplet effective radius [um] (pi value) |
LOGICAL lo |
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REAL fl(klon, klev) ! xliq * rneb (denominator to re ; fraction of liquid water clouds within the grid cell) |
REAL cetahb, cetamb |
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PARAMETER (cetahb = 0.45, cetamb = 0.80) |
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REAL bl95_b0, bl95_b1 ! Parameter in B&L 95-Formula |
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INTEGER i, k |
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REAL cldtaupi(klon, klev) ! pre-industrial cloud opt thickness for diag |
REAL zflwp, zfice |
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!cc PARAMETER (nexpo=1) |
REAL radius, rad_froid, rad_chaud, rad_chau1, rad_chau2 |
79 |
! |
PARAMETER (rad_chau1=13.0, rad_chau2=9.0, rad_froid=35.0) |
80 |
! Calculer l'epaisseur optique et l'emmissivite des nuages |
!cc PARAMETER (rad_chaud=15.0, rad_froid=35.0) |
81 |
! |
! sintex initial PARAMETER (rad_chaud=10.0, rad_froid=30.0) |
82 |
DO k = 1, klev |
REAL coef, coef_froi, coef_chau |
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DO i = 1, klon |
PARAMETER (coef_chau=0.13, coef_froi=0.09) |
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rad_chaud = rad_chau1 |
REAL seuil_neb, t_glace |
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IF (k.LE.3) rad_chaud = rad_chau2 |
PARAMETER (seuil_neb=0.001, t_glace=273.0-15.0) |
86 |
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INTEGER nexpo ! exponentiel pour glace/eau |
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pclc(i,k) = MAX(pclc(i,k), seuil_neb) |
PARAMETER (nexpo=6) |
88 |
zflwp = 1000.*pqlwp(i,k)/RG/pclc(i,k) & |
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*(paprs(i,k)-paprs(i,k+1)) |
REAL cdnc(klon, klev) ! cloud droplet number concentration [m-3] |
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zfice = 1.0 - (t(i,k)-t_glace) / (273.13-t_glace) |
REAL cdnc_pi(klon, klev) ! cloud droplet number concentration [m-3] (pi value) |
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zfice = MIN(MAX(zfice,0.0),1.0) |
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zfice = zfice**nexpo |
!-------------------------------------------------------------------- |
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IF (ok_aie) THEN |
! Calculer l'epaisseur optique et l'emmissivite des nuages |
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! Formula "D" of Boucher and Lohmann, Tellus, 1995 |
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! |
DO k = 1, klev |
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cdnc(i,k) = 10.**(bl95_b0+bl95_b1* & |
DO i = 1, klon |
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log(MAX(sulfate(i,k),1.e-4))/log(10.))*1.e6 !-m-3 |
rad_chaud = rad_chau1 |
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! Cloud droplet number concentration (CDNC) is restricted |
IF (k <= 3) rad_chaud = rad_chau2 |
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! to be within [20, 1000 cm^3] |
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! |
pclc(i, k) = MAX(pclc(i, k), seuil_neb) |
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cdnc(i,k)=MIN(1000.e6,MAX(20.e6,cdnc(i,k))) |
zflwp = 1000.*pqlwp(i, k)/RG/pclc(i, k) & |
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cdnc_pi(i,k) = 10.**(bl95_b0+bl95_b1* & |
*(paprs(i, k)-paprs(i, k+1)) |
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log(MAX(sulfate_pi(i,k),1.e-4))/log(10.))*1.e6 !-m-3 |
zfice = 1.0 - (t(i, k)-t_glace) / (273.13-t_glace) |
105 |
cdnc_pi(i,k)=MIN(1000.e6,MAX(20.e6,cdnc_pi(i,k))) |
zfice = MIN(MAX(zfice, 0.0), 1.0) |
106 |
! |
zfice = zfice**nexpo |
107 |
! |
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! air density: pplay(i,k) / (RD * zT(i,k)) |
IF (ok_aie) THEN |
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! factor 1.1: derive effective radius from volume-mean radius |
! Formula "D" of Boucher and Lohmann, Tellus, 1995 |
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! factor 1000 is the water density |
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! _chaud means that this is the CDR for liquid water clouds |
cdnc(i, k) = 10.**(bl95_b0+bl95_b1* & |
112 |
! |
log(MAX(sulfate(i, k), 1.e-4))/log(10.))*1.e6 !-m-3 |
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rad_chaud = & |
! Cloud droplet number concentration (CDNC) is restricted |
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1.1 * ( (pqlwp(i,k) * pplay(i,k) / (RD * T(i,k)) ) & |
! to be within [20, 1000 cm^3] |
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/ (4./3. * RPI * 1000. * cdnc(i,k)) )**(1./3.) |
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! |
cdnc(i, k)=MIN(1000.e6, MAX(20.e6, cdnc(i, k))) |
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! Convert to um. CDR shall be at least 3 um. |
cdnc_pi(i, k) = 10.**(bl95_b0+bl95_b1* & |
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! |
log(MAX(sulfate_pi(i, k), 1.e-4))/log(10.))*1.e6 !-m-3 |
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rad_chaud = MAX(rad_chaud*1.e6, 3.) |
cdnc_pi(i, k)=MIN(1000.e6, MAX(20.e6, cdnc_pi(i, k))) |
120 |
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! For output diagnostics |
! air density: pplay(i, k) / (RD * zT(i, k)) |
122 |
! |
! factor 1.1: derive effective radius from volume-mean radius |
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! Cloud droplet effective radius [um] |
! factor 1000 is the water density |
124 |
! |
! _chaud means that this is the CDR for liquid water clouds |
125 |
! we multiply here with f * xl (fraction of liquid water |
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! clouds in the grid cell) to avoid problems in the |
rad_chaud = & |
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! averaging of the output. |
1.1 * ((pqlwp(i, k) * pplay(i, k) / (RD * T(i, k))) & |
128 |
! In the output of IOIPSL, derive the real cloud droplet |
/ (4./3. * PI * 1000. * cdnc(i, k)))**(1./3.) |
129 |
! effective radius as re/fl |
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! |
! Convert to um. CDR shall be at least 3 um. |
131 |
fl(i,k) = pclc(i,k)*(1.-zfice) |
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re(i,k) = rad_chaud*fl(i,k) |
rad_chaud = MAX(rad_chaud*1.e6, 3.) |
133 |
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134 |
! Pre-industrial cloud opt thickness |
! For output diagnostics |
135 |
! |
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! "radius" is calculated as rad_chaud above (plus the |
! Cloud droplet effective radius [um] |
137 |
! ice cloud contribution) but using cdnc_pi instead of |
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! cdnc. |
! we multiply here with f * xl (fraction of liquid water |
139 |
radius = MAX(1.1e6 * ( (pqlwp(i,k)*pplay(i,k)/(RD*T(i,k))) & |
! clouds in the grid cell) to avoid problems in the |
140 |
/ (4./3.*RPI*1000.*cdnc_pi(i,k)) )**(1./3.), & |
! averaging of the output. |
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3.) * (1.-zfice) + rad_froid * zfice |
! In the output of IOIPSL, derive the real cloud droplet |
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cldtaupi(i,k) = 3.0/2.0 * zflwp / radius |
! effective radius as re/fl |
143 |
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END IF ! ok_aie |
fl(i, k) = pclc(i, k)*(1.-zfice) |
145 |
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re(i, k) = rad_chaud*fl(i, k) |
146 |
radius = rad_chaud * (1.-zfice) + rad_froid * zfice |
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coef = coef_chau * (1.-zfice) + coef_froi * zfice |
! Pre-industrial cloud opt thickness |
148 |
pcltau(i,k) = 3.0/2.0 * zflwp / radius |
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pclemi(i,k) = 1.0 - EXP( - coef * zflwp) |
! "radius" is calculated as rad_chaud above (plus the |
150 |
lo = (pclc(i,k) .LE. seuil_neb) |
! ice cloud contribution) but using cdnc_pi instead of |
151 |
IF (lo) pclc(i,k) = 0.0 |
! cdnc. |
152 |
IF (lo) pcltau(i,k) = 0.0 |
radius = MAX(1.1e6 * ((pqlwp(i, k)*pplay(i, k)/(RD*T(i, k))) & |
153 |
IF (lo) pclemi(i,k) = 0.0 |
/ (4./3.*PI*1000.*cdnc_pi(i, k)))**(1./3.), & |
154 |
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3.) * (1.-zfice) + rad_froid * zfice |
155 |
IF (.NOT.ok_aie) cldtaupi(i,k)=pcltau(i,k) |
cldtaupi(i, k) = 3.0/2.0 * zflwp / radius |
156 |
END DO |
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END DO |
END IF ! ok_aie |
158 |
! |
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! COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS |
radius = rad_chaud * (1.-zfice) + rad_froid * zfice |
160 |
! |
coef = coef_chau * (1.-zfice) + coef_froi * zfice |
161 |
DO i = 1, klon |
pcltau(i, k) = 3.0/2.0 * zflwp / radius |
162 |
pct(i)=1.0 |
pclemi(i, k) = 1.0 - EXP(- coef * zflwp) |
163 |
pch(i)=1.0 |
lo = (pclc(i, k) <= seuil_neb) |
164 |
pcm(i) = 1.0 |
IF (lo) pclc(i, k) = 0.0 |
165 |
pcl(i) = 1.0 |
IF (lo) pcltau(i, k) = 0.0 |
166 |
pctlwp(i) = 0.0 |
IF (lo) pclemi(i, k) = 0.0 |
167 |
END DO |
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168 |
! |
IF (.NOT.ok_aie) cldtaupi(i, k)=pcltau(i, k) |
169 |
DO k = klev, 1, -1 |
END DO |
170 |
DO i = 1, klon |
END DO |
171 |
pctlwp(i) = pctlwp(i) & |
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+ pqlwp(i,k)*(paprs(i,k)-paprs(i,k+1))/RG |
! COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS |
173 |
pct(i) = pct(i)*(1.0-pclc(i,k)) |
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174 |
if (pplay(i,k).LE.cetahb*paprs(i,1)) & |
DO i = 1, klon |
175 |
pch(i) = pch(i)*(1.0-pclc(i,k)) |
pct(i)=1.0 |
176 |
if (pplay(i,k).GT.cetahb*paprs(i,1) .AND. & |
pch(i)=1.0 |
177 |
pplay(i,k).LE.cetamb*paprs(i,1)) & |
pcm(i) = 1.0 |
178 |
pcm(i) = pcm(i)*(1.0-pclc(i,k)) |
pcl(i) = 1.0 |
179 |
if (pplay(i,k).GT.cetamb*paprs(i,1)) & |
pctlwp(i) = 0.0 |
180 |
pcl(i) = pcl(i)*(1.0-pclc(i,k)) |
END DO |
181 |
END DO |
|
182 |
END DO |
DO k = klev, 1, -1 |
183 |
! |
DO i = 1, klon |
184 |
DO i = 1, klon |
pctlwp(i) = pctlwp(i) & |
185 |
pct(i)=1.-pct(i) |
+ pqlwp(i, k)*(paprs(i, k)-paprs(i, k+1))/RG |
186 |
pch(i)=1.-pch(i) |
pct(i) = pct(i)*(1.0-pclc(i, k)) |
187 |
pcm(i)=1.-pcm(i) |
if (pplay(i, k) <= cetahb*paprs(i, 1)) & |
188 |
pcl(i)=1.-pcl(i) |
pch(i) = pch(i)*(1.0-pclc(i, k)) |
189 |
END DO |
if (pplay(i, k) > cetahb*paprs(i, 1) .AND. & |
190 |
! |
pplay(i, k) <= cetamb*paprs(i, 1)) & |
191 |
END SUBROUTINE nuage |
pcm(i) = pcm(i)*(1.0-pclc(i, k)) |
192 |
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if (pplay(i, k) > cetamb*paprs(i, 1)) & |
193 |
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pcl(i) = pcl(i)*(1.0-pclc(i, k)) |
194 |
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END DO |
195 |
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END DO |
196 |
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197 |
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DO i = 1, klon |
198 |
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pct(i)=1.-pct(i) |
199 |
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pch(i)=1.-pch(i) |
200 |
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pcm(i)=1.-pcm(i) |
201 |
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pcl(i)=1.-pcl(i) |
202 |
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END DO |
203 |
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204 |
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END SUBROUTINE nuage |
205 |
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206 |
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end module nuage_m |