1 |
module pbl_surface_m |
2 |
|
3 |
IMPLICIT NONE |
4 |
|
5 |
contains |
6 |
|
7 |
SUBROUTINE pbl_surface(dtime, pctsrf, t, q, u, v, julien, mu0, ftsol, & |
8 |
cdmmax, cdhmax, ftsoil, qsol, paprs, pplay, fsnow, qsurf, evap, falbe, & |
9 |
fluxlat, rain_fall, snow_f, fsolsw, fsollw, frugs, agesno, rugoro, d_t, & |
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d_q, d_u, d_v, d_ts, flux_t, flux_q, flux_u, flux_v, cdragh, cdragm, & |
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q2, dflux_t, dflux_q, coefh, t2m, q2m, u10m_srf, v10m_srf, pblh, capcl, & |
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oliqcl, cteicl, pblt, therm, plcl, fqcalving, ffonte, run_off_lic_0) |
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|
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! From phylmd/clmain.F, version 1.6, 2005/11/16 14:47:19 |
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! Author: Z. X. Li (LMD/CNRS), date: 1993/08/18 |
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! Objet : interface de couche limite (diffusion verticale) |
17 |
|
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! Tout ce qui a trait aux traceurs est dans "phytrac". Le calcul |
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! de la couche limite pour les traceurs se fait avec "cltrac" et |
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! ne tient pas compte de la diff\'erentiation des sous-fractions |
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! de sol. |
22 |
|
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use cdrag_m, only: cdrag |
24 |
use clqh_m, only: clqh |
25 |
use clvent_m, only: clvent |
26 |
use coef_diff_turb_m, only: coef_diff_turb |
27 |
USE conf_gcm_m, ONLY: lmt_pas |
28 |
USE conf_phys_m, ONLY: iflag_pbl |
29 |
USE dimphy, ONLY: klev, klon, zmasq |
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USE dimsoil, ONLY: nsoilmx |
31 |
use hbtm_m, only: hbtm |
32 |
USE indicesol, ONLY: epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
33 |
USE interfoce_lim_m, ONLY: interfoce_lim |
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use stdlevvar_m, only: stdlevvar |
35 |
USE suphec_m, ONLY: rd, rg |
36 |
use time_phylmdz, only: itap |
37 |
|
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REAL, INTENT(IN):: dtime ! interval du temps (secondes) |
39 |
|
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REAL, INTENT(inout):: pctsrf(klon, nbsrf) |
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! tableau des pourcentages de surface de chaque maille |
42 |
|
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REAL, INTENT(IN):: t(klon, klev) ! temperature (K) |
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REAL, INTENT(IN):: q(klon, klev) ! vapeur d'eau (kg / kg) |
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REAL, INTENT(IN):: u(klon, klev), v(klon, klev) ! vitesse |
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INTEGER, INTENT(IN):: julien ! jour de l'annee en cours |
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REAL, intent(in):: mu0(klon) ! cosinus de l'angle solaire zenithal |
48 |
REAL, INTENT(IN):: ftsol(:, :) ! (klon, nbsrf) temp\'erature du sol (en K) |
49 |
REAL, INTENT(IN):: cdmmax, cdhmax ! seuils cdrm, cdrh |
50 |
|
51 |
REAL, INTENT(inout):: ftsoil(klon, nsoilmx, nbsrf) |
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! soil temperature of surface fraction |
53 |
|
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REAL, INTENT(inout):: qsol(:) ! (klon) |
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! column-density of water in soil, in kg m-2 |
56 |
|
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REAL, INTENT(IN):: paprs(klon, klev + 1) ! pression a intercouche (Pa) |
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REAL, INTENT(IN):: pplay(klon, klev) ! pression au milieu de couche (Pa) |
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REAL, INTENT(inout):: fsnow(:, :) ! (klon, nbsrf) \'epaisseur neigeuse |
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REAL qsurf(klon, nbsrf) |
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REAL evap(klon, nbsrf) |
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REAL, intent(inout):: falbe(klon, nbsrf) |
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REAL, intent(out):: fluxlat(:, :) ! (klon, nbsrf) |
64 |
|
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REAL, intent(in):: rain_fall(klon) |
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! liquid water mass flux (kg / m2 / s), positive down |
67 |
|
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REAL, intent(in):: snow_f(klon) |
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! solid water mass flux (kg / m2 / s), positive down |
70 |
|
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REAL, INTENT(IN):: fsolsw(klon, nbsrf), fsollw(klon, nbsrf) |
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REAL, intent(inout):: frugs(klon, nbsrf) ! longueur de rugosit\'e (en m) |
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real agesno(klon, nbsrf) |
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REAL, INTENT(IN):: rugoro(klon) |
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|
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REAL d_t(klon, klev), d_q(klon, klev) |
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! d_t------output-R- le changement pour "t" |
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! d_q------output-R- le changement pour "q" |
79 |
|
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REAL, intent(out):: d_u(klon, klev), d_v(klon, klev) |
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! changement pour "u" et "v" |
82 |
|
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REAL, intent(out):: d_ts(:, :) ! (klon, nbsrf) variation of ftsol |
84 |
|
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REAL, intent(out):: flux_t(klon, nbsrf) |
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! flux de chaleur sensible (Cp T) (W / m2) (orientation positive vers |
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! le bas) à la surface |
88 |
|
89 |
REAL, intent(out):: flux_q(klon, nbsrf) |
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! flux de vapeur d'eau (kg / m2 / s) à la surface |
91 |
|
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REAL, intent(out):: flux_u(klon, nbsrf), flux_v(klon, nbsrf) |
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! tension du vent (flux turbulent de vent) à la surface, en Pa |
94 |
|
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REAL, INTENT(out):: cdragh(klon), cdragm(klon) |
96 |
real q2(klon, klev + 1, nbsrf) |
97 |
|
98 |
REAL, INTENT(out):: dflux_t(klon), dflux_q(klon) |
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! dflux_t derive du flux sensible |
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! dflux_q derive du flux latent |
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! IM "slab" ocean |
102 |
|
103 |
REAL, intent(out):: coefh(:, 2:) ! (klon, 2:klev) |
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! Pour pouvoir extraire les coefficients d'\'echange, le champ |
105 |
! "coefh" a \'et\'e cr\'e\'e. Nous avons moyenn\'e les valeurs de |
106 |
! ce champ sur les quatre sous-surfaces du mod\`ele. |
107 |
|
108 |
REAL, INTENT(inout):: t2m(klon, nbsrf), q2m(klon, nbsrf) |
109 |
|
110 |
REAL, INTENT(inout):: u10m_srf(:, :), v10m_srf(:, :) ! (klon, nbsrf) |
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! composantes du vent \`a 10m sans spirale d'Ekman |
112 |
|
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! Ionela Musat. Cf. Anne Mathieu : planetary boundary layer, hbtm. |
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! Comme les autres diagnostics on cumule dans physiq ce qui permet |
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! de sortir les grandeurs par sous-surface. |
116 |
REAL pblh(klon, nbsrf) ! height of planetary boundary layer |
117 |
REAL capcl(klon, nbsrf) |
118 |
REAL oliqcl(klon, nbsrf) |
119 |
REAL cteicl(klon, nbsrf) |
120 |
REAL, INTENT(inout):: pblt(klon, nbsrf) ! T au nveau HCL |
121 |
REAL therm(klon, nbsrf) |
122 |
REAL plcl(klon, nbsrf) |
123 |
REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
124 |
! ffonte----Flux thermique utilise pour fondre la neige |
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! fqcalving-Flux d'eau "perdue" par la surface et necessaire pour limiter la |
126 |
! hauteur de neige, en kg / m2 / s |
127 |
REAL run_off_lic_0(klon) |
128 |
|
129 |
! Local: |
130 |
|
131 |
LOGICAL:: firstcal = .true. |
132 |
|
133 |
! la nouvelle repartition des surfaces sortie de l'interface |
134 |
REAL, save:: pctsrf_new_oce(klon) |
135 |
REAL, save:: pctsrf_new_sic(klon) |
136 |
|
137 |
REAL y_fqcalving(klon), y_ffonte(klon) |
138 |
real y_run_off_lic_0(klon) |
139 |
REAL rugmer(klon) |
140 |
REAL ytsoil(klon, nsoilmx) |
141 |
REAL yts(klon), ypct(klon), yz0_new(klon) |
142 |
real yrugos(klon) ! longeur de rugosite (en m) |
143 |
REAL yalb(klon) |
144 |
REAL snow(klon), yqsurf(klon), yagesno(klon) |
145 |
real yqsol(klon) ! column-density of water in soil, in kg m-2 |
146 |
REAL yrain_f(klon) ! liquid water mass flux (kg / m2 / s), positive down |
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REAL ysnow_f(klon) ! solid water mass flux (kg / m2 / s), positive down |
148 |
REAL yrugm(klon), yrads(klon), yrugoro(klon) |
149 |
REAL yfluxlat(klon) |
150 |
REAL y_d_ts(klon) |
151 |
REAL y_d_t(klon, klev), y_d_q(klon, klev) |
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REAL y_d_u(klon, klev), y_d_v(klon, klev) |
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REAL y_flux_t(klon), y_flux_q(klon) |
154 |
REAL y_flux_u(klon), y_flux_v(klon) |
155 |
REAL y_dflux_t(klon), y_dflux_q(klon) |
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REAL ycoefh(klon, 2:klev), ycoefm(klon, 2:klev) |
157 |
real ycdragh(klon), ycdragm(klon) |
158 |
REAL yu(klon, klev), yv(klon, klev) |
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REAL yt(klon, klev), yq(klon, klev) |
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REAL ypaprs(klon, klev + 1), ypplay(klon, klev), ydelp(klon, klev) |
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REAL yq2(klon, klev + 1) |
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REAL delp(klon, klev) |
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INTEGER i, k, nsrf |
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INTEGER ni(klon), knon, j |
165 |
|
166 |
REAL pctsrf_pot(klon, nbsrf) |
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! "pourcentage potentiel" pour tenir compte des \'eventuelles |
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! apparitions ou disparitions de la glace de mer |
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|
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REAL yt2m(klon), yq2m(klon), wind10m(klon) |
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REAL ustar(klon) |
172 |
|
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REAL yt10m(klon), yq10m(klon) |
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REAL ypblh(klon) |
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REAL ylcl(klon) |
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REAL ycapcl(klon) |
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REAL yoliqcl(klon) |
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REAL ycteicl(klon) |
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REAL ypblt(klon) |
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REAL ytherm(klon) |
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REAL u1(klon), v1(klon) |
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REAL tair1(klon), qair1(klon), tairsol(klon) |
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REAL psfce(klon), patm(klon) |
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|
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REAL qairsol(klon), zgeo1(klon) |
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REAL rugo1(klon) |
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REAL zgeop(klon, klev) |
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|
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!------------------------------------------------------------ |
190 |
|
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ytherm = 0. |
192 |
|
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DO k = 1, klev ! epaisseur de couche |
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DO i = 1, klon |
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delp(i, k) = paprs(i, k) - paprs(i, k + 1) |
196 |
END DO |
197 |
END DO |
198 |
|
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! Initialization: |
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rugmer = 0. |
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cdragh = 0. |
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cdragm = 0. |
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dflux_t = 0. |
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dflux_q = 0. |
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ypct = 0. |
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yqsurf = 0. |
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yrain_f = 0. |
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ysnow_f = 0. |
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yrugos = 0. |
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ypaprs = 0. |
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ypplay = 0. |
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ydelp = 0. |
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yu = 0. |
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yv = 0. |
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yt = 0. |
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yq = 0. |
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y_dflux_t = 0. |
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y_dflux_q = 0. |
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yrugoro = 0. |
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d_ts = 0. |
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flux_t = 0. |
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flux_q = 0. |
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flux_u = 0. |
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flux_v = 0. |
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fluxlat = 0. |
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d_t = 0. |
227 |
d_q = 0. |
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d_u = 0. |
229 |
d_v = 0. |
230 |
coefh = 0. |
231 |
|
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! Initialisation des "pourcentages potentiels". On consid\`ere ici qu'on |
233 |
! peut avoir potentiellement de la glace sur tout le domaine oc\'eanique |
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! (\`a affiner) |
235 |
|
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pctsrf_pot(:, is_ter) = pctsrf(:, is_ter) |
237 |
pctsrf_pot(:, is_lic) = pctsrf(:, is_lic) |
238 |
pctsrf_pot(:, is_oce) = 1. - zmasq |
239 |
pctsrf_pot(:, is_sic) = 1. - zmasq |
240 |
|
241 |
! Tester si c'est le moment de lire le fichier: |
242 |
if (mod(itap - 1, lmt_pas) == 0) then |
243 |
CALL interfoce_lim(julien, pctsrf_new_oce, pctsrf_new_sic) |
244 |
endif |
245 |
|
246 |
! Boucler sur toutes les sous-fractions du sol: |
247 |
|
248 |
loop_surface: DO nsrf = 1, nbsrf |
249 |
! Chercher les indices : |
250 |
ni = 0 |
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knon = 0 |
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DO i = 1, klon |
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! Pour d\'eterminer le domaine \`a traiter, on utilise les surfaces |
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! "potentielles" |
255 |
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
256 |
knon = knon + 1 |
257 |
ni(knon) = i |
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END IF |
259 |
END DO |
260 |
|
261 |
if_knon: IF (knon /= 0) then |
262 |
DO j = 1, knon |
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i = ni(j) |
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ypct(j) = pctsrf(i, nsrf) |
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yts(j) = ftsol(i, nsrf) |
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snow(j) = fsnow(i, nsrf) |
267 |
yqsurf(j) = qsurf(i, nsrf) |
268 |
yalb(j) = falbe(i, nsrf) |
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yrain_f(j) = rain_fall(i) |
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ysnow_f(j) = snow_f(i) |
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yagesno(j) = agesno(i, nsrf) |
272 |
yrugos(j) = frugs(i, nsrf) |
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yrugoro(j) = rugoro(i) |
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yrads(j) = fsolsw(i, nsrf) + fsollw(i, nsrf) |
275 |
ypaprs(j, klev + 1) = paprs(i, klev + 1) |
276 |
y_run_off_lic_0(j) = run_off_lic_0(i) |
277 |
END DO |
278 |
|
279 |
! For continent, copy soil water content |
280 |
IF (nsrf == is_ter) yqsol(:knon) = qsol(ni(:knon)) |
281 |
|
282 |
ytsoil(:knon, :) = ftsoil(ni(:knon), :, nsrf) |
283 |
|
284 |
DO k = 1, klev |
285 |
DO j = 1, knon |
286 |
i = ni(j) |
287 |
ypaprs(j, k) = paprs(i, k) |
288 |
ypplay(j, k) = pplay(i, k) |
289 |
ydelp(j, k) = delp(i, k) |
290 |
yu(j, k) = u(i, k) |
291 |
yv(j, k) = v(i, k) |
292 |
yt(j, k) = t(i, k) |
293 |
yq(j, k) = q(i, k) |
294 |
END DO |
295 |
END DO |
296 |
|
297 |
! Calculer les géopotentiels de chaque couche: |
298 |
|
299 |
zgeop(:knon, 1) = RD * yt(:knon, 1) / (0.5 * (ypaprs(:knon, 1) & |
300 |
+ ypplay(:knon, 1))) * (ypaprs(:knon, 1) - ypplay(:knon, 1)) |
301 |
|
302 |
DO k = 2, klev |
303 |
zgeop(:knon, k) = zgeop(:knon, k - 1) + RD * 0.5 & |
304 |
* (yt(:knon, k - 1) + yt(:knon, k)) / ypaprs(:knon, k) & |
305 |
* (ypplay(:knon, k - 1) - ypplay(:knon, k)) |
306 |
ENDDO |
307 |
|
308 |
CALL cdrag(nsrf, sqrt(yu(:knon, 1)**2 + yv(:knon, 1)**2), & |
309 |
yt(:knon, 1), yq(:knon, 1), zgeop(:knon, 1), ypaprs(:knon, 1), & |
310 |
yts(:knon), yqsurf(:knon), yrugos(:knon), ycdragm(:knon), & |
311 |
ycdragh(:knon)) |
312 |
|
313 |
IF (iflag_pbl == 1) THEN |
314 |
ycdragm(:knon) = max(ycdragm(:knon), 0.) |
315 |
ycdragh(:knon) = max(ycdragh(:knon), 0.) |
316 |
end IF |
317 |
|
318 |
! on met un seuil pour ycdragm et ycdragh |
319 |
IF (nsrf == is_oce) THEN |
320 |
ycdragm(:knon) = min(ycdragm(:knon), cdmmax) |
321 |
ycdragh(:knon) = min(ycdragh(:knon), cdhmax) |
322 |
END IF |
323 |
|
324 |
IF (iflag_pbl >= 6) then |
325 |
DO k = 1, klev + 1 |
326 |
DO j = 1, knon |
327 |
i = ni(j) |
328 |
yq2(j, k) = q2(i, k, nsrf) |
329 |
END DO |
330 |
END DO |
331 |
end IF |
332 |
|
333 |
call coef_diff_turb(dtime, nsrf, ni(:knon), ypaprs(:knon, :), & |
334 |
ypplay(:knon, :), yu(:knon, :), yv(:knon, :), yq(:knon, :), & |
335 |
yt(:knon, :), yts(:knon), ycdragm(:knon), zgeop(:knon, :), & |
336 |
ycoefm(:knon, :), ycoefh(:knon, :), yq2(:knon, :)) |
337 |
|
338 |
CALL clvent(dtime, yu(:knon, 1), yv(:knon, 1), ycoefm(:knon, :), & |
339 |
ycdragm(:knon), yt(:knon, :), yu(:knon, :), ypaprs(:knon, :), & |
340 |
ypplay(:knon, :), ydelp(:knon, :), y_d_u(:knon, :), & |
341 |
y_flux_u(:knon)) |
342 |
CALL clvent(dtime, yu(:knon, 1), yv(:knon, 1), ycoefm(:knon, :), & |
343 |
ycdragm(:knon), yt(:knon, :), yv(:knon, :), ypaprs(:knon, :), & |
344 |
ypplay(:knon, :), ydelp(:knon, :), y_d_v(:knon, :), & |
345 |
y_flux_v(:knon)) |
346 |
|
347 |
! calculer la diffusion de "q" et de "h" |
348 |
CALL clqh(dtime, julien, firstcal, nsrf, ni(:knon), & |
349 |
ytsoil(:knon, :), yqsol(:knon), mu0, yrugos, yrugoro, & |
350 |
yu(:knon, 1), yv(:knon, 1), ycoefh(:knon, :), ycdragh(:knon), & |
351 |
yt, yq, yts(:knon), ypaprs, ypplay, ydelp, yrads(:knon), & |
352 |
yalb(:knon), snow(:knon), yqsurf, yrain_f, ysnow_f, & |
353 |
yfluxlat(:knon), pctsrf_new_sic, yagesno(:knon), y_d_t, y_d_q, & |
354 |
y_d_ts(:knon), yz0_new, y_flux_t(:knon), y_flux_q(:knon), & |
355 |
y_dflux_t(:knon), y_dflux_q(:knon), y_fqcalving, y_ffonte, & |
356 |
y_run_off_lic_0) |
357 |
|
358 |
! calculer la longueur de rugosite sur ocean |
359 |
yrugm = 0. |
360 |
IF (nsrf == is_oce) THEN |
361 |
DO j = 1, knon |
362 |
yrugm(j) = 0.018 * ycdragm(j) * (yu(j, 1)**2 + yv(j, 1)**2) & |
363 |
/ rg + 0.11 * 14E-6 & |
364 |
/ sqrt(ycdragm(j) * (yu(j, 1)**2 + yv(j, 1)**2)) |
365 |
yrugm(j) = max(1.5E-05, yrugm(j)) |
366 |
END DO |
367 |
END IF |
368 |
DO j = 1, knon |
369 |
y_dflux_t(j) = y_dflux_t(j) * ypct(j) |
370 |
y_dflux_q(j) = y_dflux_q(j) * ypct(j) |
371 |
END DO |
372 |
|
373 |
DO k = 1, klev |
374 |
DO j = 1, knon |
375 |
i = ni(j) |
376 |
y_d_t(j, k) = y_d_t(j, k) * ypct(j) |
377 |
y_d_q(j, k) = y_d_q(j, k) * ypct(j) |
378 |
y_d_u(j, k) = y_d_u(j, k) * ypct(j) |
379 |
y_d_v(j, k) = y_d_v(j, k) * ypct(j) |
380 |
END DO |
381 |
END DO |
382 |
|
383 |
flux_t(ni(:knon), nsrf) = y_flux_t(:knon) |
384 |
flux_q(ni(:knon), nsrf) = y_flux_q(:knon) |
385 |
flux_u(ni(:knon), nsrf) = y_flux_u(:knon) |
386 |
flux_v(ni(:knon), nsrf) = y_flux_v(:knon) |
387 |
|
388 |
evap(:, nsrf) = -flux_q(:, nsrf) |
389 |
|
390 |
falbe(:, nsrf) = 0. |
391 |
fsnow(:, nsrf) = 0. |
392 |
qsurf(:, nsrf) = 0. |
393 |
frugs(:, nsrf) = 0. |
394 |
DO j = 1, knon |
395 |
i = ni(j) |
396 |
d_ts(i, nsrf) = y_d_ts(j) |
397 |
falbe(i, nsrf) = yalb(j) |
398 |
fsnow(i, nsrf) = snow(j) |
399 |
qsurf(i, nsrf) = yqsurf(j) |
400 |
frugs(i, nsrf) = yz0_new(j) |
401 |
fluxlat(i, nsrf) = yfluxlat(j) |
402 |
IF (nsrf == is_oce) THEN |
403 |
rugmer(i) = yrugm(j) |
404 |
frugs(i, nsrf) = yrugm(j) |
405 |
END IF |
406 |
agesno(i, nsrf) = yagesno(j) |
407 |
fqcalving(i, nsrf) = y_fqcalving(j) |
408 |
ffonte(i, nsrf) = y_ffonte(j) |
409 |
cdragh(i) = cdragh(i) + ycdragh(j) * ypct(j) |
410 |
cdragm(i) = cdragm(i) + ycdragm(j) * ypct(j) |
411 |
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
412 |
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
413 |
END DO |
414 |
IF (nsrf == is_ter) THEN |
415 |
qsol(ni(:knon)) = yqsol(:knon) |
416 |
else IF (nsrf == is_lic) THEN |
417 |
DO j = 1, knon |
418 |
i = ni(j) |
419 |
run_off_lic_0(i) = y_run_off_lic_0(j) |
420 |
END DO |
421 |
END IF |
422 |
|
423 |
ftsoil(:, :, nsrf) = 0. |
424 |
ftsoil(ni(:knon), :, nsrf) = ytsoil(:knon, :) |
425 |
|
426 |
DO j = 1, knon |
427 |
i = ni(j) |
428 |
DO k = 1, klev |
429 |
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
430 |
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
431 |
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
432 |
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
433 |
END DO |
434 |
END DO |
435 |
|
436 |
forall (k = 2:klev) coefh(ni(:knon), k) & |
437 |
= coefh(ni(:knon), k) + ycoefh(:knon, k) * ypct(:knon) |
438 |
|
439 |
! diagnostic t, q a 2m et u, v a 10m |
440 |
|
441 |
DO j = 1, knon |
442 |
i = ni(j) |
443 |
u1(j) = yu(j, 1) + y_d_u(j, 1) |
444 |
v1(j) = yv(j, 1) + y_d_v(j, 1) |
445 |
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
446 |
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
447 |
zgeo1(j) = rd * tair1(j) / (0.5 * (ypaprs(j, 1) + ypplay(j, & |
448 |
1))) * (ypaprs(j, 1)-ypplay(j, 1)) |
449 |
tairsol(j) = yts(j) + y_d_ts(j) |
450 |
rugo1(j) = yrugos(j) |
451 |
IF (nsrf == is_oce) THEN |
452 |
rugo1(j) = frugs(i, nsrf) |
453 |
END IF |
454 |
psfce(j) = ypaprs(j, 1) |
455 |
patm(j) = ypplay(j, 1) |
456 |
|
457 |
qairsol(j) = yqsurf(j) |
458 |
END DO |
459 |
|
460 |
CALL stdlevvar(nsrf, u1(:knon), v1(:knon), tair1(:knon), qair1, & |
461 |
zgeo1, tairsol, qairsol, rugo1, psfce, patm, yt2m, yq2m, yt10m, & |
462 |
yq10m, wind10m(:knon), ustar(:knon)) |
463 |
|
464 |
DO j = 1, knon |
465 |
i = ni(j) |
466 |
t2m(i, nsrf) = yt2m(j) |
467 |
q2m(i, nsrf) = yq2m(j) |
468 |
|
469 |
u10m_srf(i, nsrf) = (wind10m(j) * u1(j)) & |
470 |
/ sqrt(u1(j)**2 + v1(j)**2) |
471 |
v10m_srf(i, nsrf) = (wind10m(j) * v1(j)) & |
472 |
/ sqrt(u1(j)**2 + v1(j)**2) |
473 |
END DO |
474 |
|
475 |
CALL hbtm(ypaprs, ypplay, yt2m, yq2m, ustar(:knon), y_flux_t(:knon), & |
476 |
y_flux_q(:knon), yu, yv, yt, yq, ypblh(:knon), ycapcl, & |
477 |
yoliqcl, ycteicl, ypblt, ytherm, ylcl) |
478 |
|
479 |
DO j = 1, knon |
480 |
i = ni(j) |
481 |
pblh(i, nsrf) = ypblh(j) |
482 |
plcl(i, nsrf) = ylcl(j) |
483 |
capcl(i, nsrf) = ycapcl(j) |
484 |
oliqcl(i, nsrf) = yoliqcl(j) |
485 |
cteicl(i, nsrf) = ycteicl(j) |
486 |
pblt(i, nsrf) = ypblt(j) |
487 |
therm(i, nsrf) = ytherm(j) |
488 |
END DO |
489 |
|
490 |
DO j = 1, knon |
491 |
DO k = 1, klev + 1 |
492 |
i = ni(j) |
493 |
q2(i, k, nsrf) = yq2(j, k) |
494 |
END DO |
495 |
END DO |
496 |
else |
497 |
fsnow(:, nsrf) = 0. |
498 |
end IF if_knon |
499 |
END DO loop_surface |
500 |
|
501 |
! On utilise les nouvelles surfaces |
502 |
frugs(:, is_oce) = rugmer |
503 |
pctsrf(:, is_oce) = pctsrf_new_oce |
504 |
pctsrf(:, is_sic) = pctsrf_new_sic |
505 |
|
506 |
firstcal = .false. |
507 |
|
508 |
END SUBROUTINE pbl_surface |
509 |
|
510 |
end module pbl_surface_m |