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module newmicro_m |
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IMPLICIT none |
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|
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contains |
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SUBROUTINE newmicro (paprs, play, t, qlwp, clc, cltau, clemi, cldh, & |
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cldl, cldm, cldt, ctlwp, flwp, fiwp, flwc, fiwc, ok_aie, sulfate, & |
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sulfate_pi, bl95_b0, bl95_b1, cldtaupi, re, fl) |
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|
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! From LMDZ4/libf/phylmd/newmicro.F, version 1.2 2004/06/03 09:22:43 |
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|
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! Authors: Z. X. Li (LMD/CNRS), Johannes Quaas |
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! Date: 1993/09/10 |
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! Objet: calcul de l'épaisseur optique et de l'émissivité des nuages. |
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|
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USE conf_phys_m, ONLY: rad_chau1, rad_chau2 |
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USE dimphy, ONLY: klev, klon |
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USE suphec_m, ONLY: rd, rg |
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use nr_util, only: pi |
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|
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REAL, intent(in):: paprs(:, :) ! (klon, klev+1) |
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real, intent(in):: play(:, :) ! (klon, klev) |
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REAL, intent(in):: t(:, :) ! (klon, klev) temperature |
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|
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REAL, intent(in):: qlwp(:, :) ! (klon, klev) |
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! eau liquide nuageuse dans l'atmosphère (kg/kg) |
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|
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REAL, intent(inout):: clc(:, :) ! (klon, klev) |
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! couverture nuageuse pour le rayonnement (0 à 1) |
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|
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REAL, intent(out):: cltau(:, :) ! (klon, klev) épaisseur optique des nuages |
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REAL, intent(out):: clemi(:, :) ! (klon, klev) émissivité des nuages (0 à 1) |
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|
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REAL, intent(out):: cldh(:), cldl(:), cldm(:), cldt(:) ! (klon) |
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REAL, intent(out):: ctlwp(:) ! (klon) |
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REAL, intent(out):: flwp(:), fiwp(:) ! (klon) |
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REAL, intent(out):: flwc(:, :), fiwc(:, :) ! (klon, klev) |
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LOGICAL, intent(in):: ok_aie ! apply aerosol indirect effect |
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|
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REAL, intent(in):: sulfate(:, :) ! (klon, klev) |
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! sulfate aerosol mass concentration (micro g m-3) |
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|
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REAL, intent(in):: sulfate_pi(:, :) ! (klon, klev) |
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! sulfate aerosol mass concentration (micro g m-3), pre-industrial value |
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|
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REAL, intent(in):: bl95_b0, bl95_b1 |
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! Parameters in equation (D) of Boucher and Lohmann (1995, Tellus |
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! B). They link cloud droplet number concentration to aerosol mass |
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! concentration. |
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|
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REAL, intent(out):: cldtaupi(:, :) ! (klon, klev) |
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! pre-industrial value of cloud optical thickness, needed for the |
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! diagnosis of the aerosol indirect radiative forcing (see |
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! radlwsw) |
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|
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REAL, intent(out):: re(:, :) ! (klon, klev) |
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! cloud droplet effective radius multiplied by fl (micro m) |
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|
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REAL, intent(out):: fl(:, :) ! (klon, klev) |
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! Denominator to re, introduced to avoid problems in the averaging |
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! of the output. fl is the fraction of liquid water clouds within |
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! a grid cell. |
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|
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! Local: |
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|
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REAL, PARAMETER:: cetahb = 0.45, cetamb = 0.8 |
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INTEGER i, k |
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REAL zflwp(klon), fice |
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REAL radius, rad_chaud |
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REAL, PARAMETER:: coef_chau = 0.13 |
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REAL, PARAMETER:: seuil_neb = 0.001, t_glace = 273. - 15. |
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real rel, tc, rei, zfiwp(klon) |
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real k_ice |
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real, parameter:: k_ice0 = 0.005 ! units=m2/g |
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real, parameter:: DF = 1.66 ! diffusivity factor |
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REAL cdnc(klon, klev) ! cloud droplet number concentration (m-3) |
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|
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REAL cdnc_pi(klon, klev) |
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! cloud droplet number concentration, pre-industrial value (m-3) |
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|
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!----------------------------------------------------------------- |
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|
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! Calculer l'épaisseur optique et l'émissivité des nuages |
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|
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loop_horizontal: DO i = 1, klon |
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flwp(i) = 0. |
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fiwp(i) = 0. |
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|
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DO k = 1, klev |
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clc(i, k) = MAX(clc(i, k), seuil_neb) |
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|
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! liquid/ice cloud water paths: |
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|
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fice = 1. - (t(i, k) - t_glace) / (273.13 - t_glace) |
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fice = MIN(MAX(fice, 0.), 1.) |
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|
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zflwp(i) = 1000. * (1. - fice) * qlwp(i, k) / clc(i, k) & |
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* (paprs(i, k) - paprs(i, k + 1)) / RG |
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zfiwp(i) = 1000. * fice * qlwp(i, k) / clc(i, k) & |
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* (paprs(i, k) - paprs(i, k + 1)) / RG |
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|
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flwp(i) = flwp(i) & |
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+ (1. - fice) * qlwp(i, k) * (paprs(i, k) - paprs(i, k + 1)) / RG |
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fiwp(i) = fiwp(i) & |
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+ fice * qlwp(i, k) * (paprs(i, k) - paprs(i, k + 1)) / RG |
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|
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! Total Liquid/Ice water content |
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flwc(i, k) = (1.-fice) * qlwp(i, k) |
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fiwc(i, k) = fice * qlwp(i, k) |
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! In-Cloud Liquid/Ice water content |
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|
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! effective cloud droplet radius (microns): |
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|
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! for liquid water clouds: |
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IF (ok_aie) THEN |
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cdnc(i, k) = 10.**(bl95_b0 + bl95_b1 & |
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* log10(MAX(sulfate(i, k), 1e-4))) * 1.e6 |
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cdnc_pi(i, k) = 10.**(bl95_b0 + bl95_b1 & |
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* log10(MAX(sulfate_pi(i, k), 1e-4))) * 1e6 |
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|
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! Restrict to interval [20, 1000] cm^3: |
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cdnc(i, k) = MIN(1000e6, MAX(20e6, cdnc(i, k))) |
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cdnc_pi(i, k) = MIN(1000e6, MAX(20e6, cdnc_pi(i, k))) |
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|
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! air density: play(i, k) / (RD * T(i, k)) |
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! factor 1.1: derive effective radius from volume-mean radius |
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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 |
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|
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rad_chaud = 1.1 * ((qlwp(i, k) * play(i, k) / (RD * T(i, k))) & |
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/ (4./3. * PI * 1000. * cdnc(i, k)))**(1./3.) |
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|
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! Convert to micro m and set a lower limit: |
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rad_chaud = MAX(rad_chaud * 1e6, 5.) |
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|
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! Pre-industrial cloud optical thickness |
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! "radius" is calculated as rad_chaud above (plus the |
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! ice cloud contribution) but using cdnc_pi instead of |
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! cdnc. |
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radius = 1.1 * ((qlwp(i, k) * play(i, k) / (RD * T(i, k))) & |
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/ (4./3. * PI * 1000. * cdnc_pi(i, k)))**(1./3.) |
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radius = MAX(radius * 1e6, 5.) |
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|
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tc = t(i, k)-273.15 |
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rei = merge(3.5, 0.71 * tc + 61.29, tc <= -81.4) |
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if (zflwp(i) == 0.) radius = 1. |
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if (zfiwp(i) == 0. .or. rei <= 0.) rei = 1. |
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cldtaupi(i, k) = 3. / 2. * zflwp(i) / radius & |
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+ zfiwp(i) * (3.448e-03 + 2.431 / rei) |
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else |
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rad_chaud = merge(rad_chau2, rad_chau1, k <= 3) |
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ENDIF |
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! For output diagnostics |
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|
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! Cloud droplet effective radius (micro m) |
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|
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! we multiply here with f * xl (fraction of liquid water |
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! clouds in the grid cell) to avoid problems in the |
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! averaging of the output. |
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! In the output of IOIPSL, derive the real cloud droplet |
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! effective radius as re/fl |
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|
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fl(i, k) = clc(i, k) * (1.-fice) |
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re(i, k) = rad_chaud * fl(i, k) |
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|
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rel = rad_chaud |
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! for ice clouds: as a function of the ambiant temperature |
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! (formula used by Iacobellis and Somerville (2000), with an |
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! asymptotical value of 3.5 microns at T<-81.4 C added to be |
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! consistent with observations of Heymsfield et al. 1986): |
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tc = t(i, k)-273.15 |
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rei = merge(3.5, 0.71 * tc + 61.29, tc <= -81.4) |
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|
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! cloud optical thickness: |
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|
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! (for liquid clouds, traditional formula, |
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! for ice clouds, Ebert & Curry (1992)) |
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|
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if (zflwp(i) == 0.) rel = 1. |
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if (zfiwp(i) == 0. .or. rei <= 0.) rei = 1. |
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cltau(i, k) = 3./2. * (zflwp(i)/rel) & |
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+ zfiwp(i) * (3.448e-03 + 2.431/rei) |
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|
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! cloud infrared emissivity: |
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|
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! (the broadband infrared absorption coefficient is parameterized |
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! as a function of the effective cld droplet radius) |
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|
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! Ebert and Curry (1992) formula as used by Kiehl & Zender (1995): |
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k_ice = k_ice0 + 1. / rei |
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|
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clemi(i, k) = 1. - EXP(- coef_chau * zflwp(i) - DF * k_ice * zfiwp(i)) |
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|
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if (clc(i, k) <= seuil_neb) then |
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clc(i, k) = 0. |
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cltau(i, k) = 0. |
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clemi(i, k) = 0. |
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cldtaupi(i, k) = 0. |
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end if |
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|
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IF (.NOT. ok_aie) cldtaupi(i, k) = cltau(i, k) |
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ENDDO |
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ENDDO loop_horizontal |
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! COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS |
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|
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DO i = 1, klon |
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cldt(i)=1. |
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cldh(i)=1. |
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cldm(i) = 1. |
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cldl(i) = 1. |
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ctlwp(i) = 0. |
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ENDDO |
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|
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DO k = klev, 1, -1 |
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DO i = 1, klon |
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ctlwp(i) = ctlwp(i) & |
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+ qlwp(i, k) * (paprs(i, k) - paprs(i, k + 1)) / RG |
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cldt(i) = cldt(i) * (1.-clc(i, k)) |
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if (play(i, k) <= cetahb * paprs(i, 1)) & |
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cldh(i) = cldh(i) * (1. - clc(i, k)) |
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if (play(i, k) > cetahb * paprs(i, 1) .AND. & |
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play(i, k) <= cetamb * paprs(i, 1)) & |
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cldm(i) = cldm(i) * (1.-clc(i, k)) |
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if (play(i, k) > cetamb * paprs(i, 1)) & |
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cldl(i) = cldl(i) * (1. - clc(i, k)) |
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ENDDO |
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ENDDO |
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|
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DO i = 1, klon |
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cldt(i)=1.-cldt(i) |
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cldh(i)=1.-cldh(i) |
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cldm(i)=1.-cldm(i) |
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cldl(i)=1.-cldl(i) |
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ENDDO |
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|
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END SUBROUTINE newmicro |
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|
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end module newmicro_m |
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