1 | subroutine largescale(dtime, paprs, pplay, t, pq, |
---|
2 | & pdt, d_t, d_q, d_ql, rneb, reffH2O) |
---|
3 | |
---|
4 | use watercommon_h, only : RLVTT, RCPD, RVTMP2 |
---|
5 | |
---|
6 | IMPLICIT none |
---|
7 | |
---|
8 | !================================================================== |
---|
9 | ! |
---|
10 | ! Purpose |
---|
11 | ! ------- |
---|
12 | ! Calculates large-scale (stratiform) H2O condensation. |
---|
13 | ! |
---|
14 | ! Authors |
---|
15 | ! ------- |
---|
16 | ! Adapted from the LMDTERRE code by R. Wordsworth (2009) |
---|
17 | ! Original author Z. X. Li (1993) |
---|
18 | ! |
---|
19 | !================================================================== |
---|
20 | |
---|
21 | #include "dimensions.h" |
---|
22 | #include "dimphys.h" |
---|
23 | #include "comcstfi.h" |
---|
24 | |
---|
25 | #include "fisice.h" |
---|
26 | #include "callkeys.h" |
---|
27 | #include "tracer.h" |
---|
28 | |
---|
29 | |
---|
30 | ! Pre-arguments (for universal model) |
---|
31 | real pq(ngridmx,nlayermx,nqmx) ! tracer (kg/kg) |
---|
32 | |
---|
33 | ! Arguments |
---|
34 | REAL dtime ! intervalle du temps (s) |
---|
35 | REAL paprs(ngridmx,nlayermx+1) ! pression a inter-couche |
---|
36 | REAL pplay(ngridmx,nlayermx) ! pression au milieu de couche |
---|
37 | REAL t(ngridmx,nlayermx) ! temperature (K) |
---|
38 | REAL q(ngridmx,nlayermx) ! humidite specifique (kg/kg) |
---|
39 | REAL d_t(ngridmx,nlayermx) ! incrementation de la temperature (K) |
---|
40 | REAL d_q(ngridmx,nlayermx) ! incrementation de la vapeur d'eau |
---|
41 | REAL d_ql(ngridmx,nlayermx) ! incrementation de l'eau liquide |
---|
42 | REAL rneb(ngridmx,nlayermx) ! fraction nuageuse |
---|
43 | REAL reffH2O(ngridmx,nlayermx) ! cloud particle mean radius (m) |
---|
44 | |
---|
45 | REAL pdt(ngridmx,nlayermx) ! added by Benjamin! |
---|
46 | |
---|
47 | ! Options du programme |
---|
48 | REAL ratqs ! determine largeur de la distribution de vapeur |
---|
49 | PARAMETER (ratqs=0.2) |
---|
50 | |
---|
51 | ! Variables locales |
---|
52 | REAL CBRT |
---|
53 | EXTERNAL CBRT |
---|
54 | INTEGER i, k |
---|
55 | REAL zt(ngridmx), zq(ngridmx) |
---|
56 | REAL zcond(ngridmx) |
---|
57 | REAL zdelq(ngridmx) |
---|
58 | REAL zqs(ngridmx), zdqs(ngridmx) |
---|
59 | |
---|
60 | REAL zcor(ngridmx), zdelta(ngridmx), zcvm5(ngridmx) |
---|
61 | REAL zx_q(ngridmx) |
---|
62 | |
---|
63 | ! GCM -----> subroutine variables, initialisation of outputs |
---|
64 | DO k = 1, nlayermx |
---|
65 | DO i = 1, ngridmx |
---|
66 | q(i,k) = pq(i,k,igcm_h2o_vap) |
---|
67 | d_t(i,k) = 0.0 |
---|
68 | d_q(i,k) = 0.0 |
---|
69 | d_ql(i,k) = 0.0 |
---|
70 | rneb(i,k) = 0.0 |
---|
71 | ENDDO |
---|
72 | ENDDO |
---|
73 | |
---|
74 | ! Boucle verticale (du haut vers le bas) |
---|
75 | DO 9999 k = nlayermx, 1, -1 |
---|
76 | |
---|
77 | DO i = 1, ngridmx |
---|
78 | zt(i)=t(i,k)+pdt(i,k)*dtime |
---|
79 | zq(i)=q(i,k) ! no need to add tendency as we're already dealing with qevap |
---|
80 | ENDDO |
---|
81 | |
---|
82 | ! Calculer la vapeur d'eau saturante et |
---|
83 | ! determiner la condensation partielle |
---|
84 | DO i = 1, ngridmx |
---|
85 | |
---|
86 | call watersat(zt(i),pplay(i,k),zqs(i)) |
---|
87 | call watersat_grad(zt(i),zqs(i),zdqs(i)) |
---|
88 | |
---|
89 | !IF (zt(i).LT.t_coup) THEN |
---|
90 | ! zqs(i) = qsats(zt(i))/pplay(i,k) |
---|
91 | ! zdqs(i) = dqsats(zt(i),zqs(i)) |
---|
92 | !ELSE |
---|
93 | ! zqs(i) = qsatl(zt(i))/pplay(i,k) |
---|
94 | ! zdqs(i) = dqsatl(zt(i),zqs(i)) |
---|
95 | !ENDIF |
---|
96 | |
---|
97 | zdelq(i) = ratqs * zq(i) |
---|
98 | rneb(i,k) = (zq(i)+zdelq(i)-zqs(i)) / (2.0*zdelq(i)) |
---|
99 | zcond(i) = 0.0 |
---|
100 | zx_q(i) = (zq(i)+zdelq(i)+zqs(i))/2.0 |
---|
101 | if (rneb(i,k) .LE. 0.0) zx_q(i) = 0.0 |
---|
102 | if (rneb(i,k) .GE. 1.0) zx_q(i) = zq(i) |
---|
103 | rneb(i,k) = MAX(0.0,MIN(1.0,rneb(i,k))) |
---|
104 | !zcond(i) = MAX(0.0,(zx_q(i)-zqs(i)*rneb(i,k)/(1.+zdqs(i)))) |
---|
105 | zcond(i) = MAX(0.0,(zx_q(i)-zqs(i))*rneb(i,k)/(1.+zdqs(i))) |
---|
106 | ! zcond always postive! cannot evaporate clouds! |
---|
107 | ! this is why we must reevaporate before largescale |
---|
108 | |
---|
109 | |
---|
110 | zcond(i) = zcond(i)/dtime ! added by RDW |
---|
111 | |
---|
112 | ! for varying particle size in rad tran and (possibly) sedimentation |
---|
113 | if(.not.aerofixed)then |
---|
114 | reffH2O(i,k) = CBRT( 3*zcond(i)/( 4*Nmix_h2o*pi*rho_ice)) |
---|
115 | reffH2O(i,k) = max(reffH2O(i,k),1.e-8) |
---|
116 | endif |
---|
117 | |
---|
118 | ENDDO |
---|
119 | |
---|
120 | ! Tendances de t et q |
---|
121 | DO i = 1, ngridmx |
---|
122 | d_q(i,k) = - zcond(i) |
---|
123 | d_ql(i,k) = zcond(i) |
---|
124 | !d_t(i,k) = zcond(i)*RLVTT/cpp |
---|
125 | d_t(i,k) = zcond(i)*RLVTT/RCPD!/(1.0+RVTMP2*q(i,k)) |
---|
126 | ! this one is FAR TOO BIG |
---|
127 | ENDDO |
---|
128 | |
---|
129 | 9999 CONTINUE |
---|
130 | |
---|
131 | !print*,'qsat=',zqs |
---|
132 | !print*,'q=',q |
---|
133 | !print*,'dq=',d_q*dtime |
---|
134 | !print*,'dT in LS=',d_t*dtime |
---|
135 | |
---|
136 | !print*,'rice=',rice |
---|
137 | !print*,'rneb=',rneb |
---|
138 | |
---|
139 | return |
---|
140 | end |
---|