| 1 |
SUBROUTINE diagetpq(airephy,tit,iprt,idiag,idiag2,dtime |
module diagetpq_m |
| 2 |
e ,t,q,ql,qs,u,v,paprs |
|
| 3 |
s , d_h_vcol, d_qt, d_qw, d_ql, d_qs, d_ec) |
IMPLICIT NONE |
| 4 |
! |
|
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! $Header: /home/cvsroot/LMDZ4/libf/phylmd/diagphy.F,v 1.1.1.1 2004/05/19 12:53:08 lmdzadmin Exp $ |
contains |
| 6 |
! |
|
| 7 |
C====================================================================== |
SUBROUTINE diagetpq(airephy, tit, iprt, idiag, idiag2, dtime, t, q, ql, & |
| 8 |
C |
u, v, paprs, d_h_vcol, d_qt, d_ec) |
| 9 |
C Purpose: |
|
| 10 |
C Calcul la difference d'enthalpie et de masse d'eau entre 2 appels, |
! From LMDZ4/libf/phylmd/diagphy.F, version 1.1.1.1, 2004/05/19 12:53:08 |
| 11 |
C et calcul le flux de chaleur et le flux d'eau necessaire a ces |
|
| 12 |
C changements. Ces valeurs sont moyennees sur la surface de tout |
! Purpose: |
| 13 |
C le globe et sont exprime en W/2 et kg/s/m2 |
|
| 14 |
C Outil pour diagnostiquer la conservation de l'energie |
! Calcule la différence d'enthalpie et de masse d'eau entre deux |
| 15 |
C et de la masse dans la physique. Suppose que les niveau de |
! appels et calcule le flux de chaleur et le flux d'eau |
| 16 |
c pression entre couche ne varie pas entre 2 appels. |
! nécessaires à ces changements. Ces valeurs sont moyennées sur la |
| 17 |
C |
! surface de tout le globe et sont exprimées en W/m2 et |
| 18 |
C Plusieurs de ces diagnostics peuvent etre fait en parallele: les |
! kg/s/m2. Outil pour diagnostiquer la conservation de l'énergie |
| 19 |
c bilans sont sauvegardes dans des tableaux indices. On parlera |
! et de la masse dans la physique. Suppose que les niveaux de |
| 20 |
C "d'indice de diagnostic" |
! pression entre les couches ne varient pas entre deux appels. |
| 21 |
c |
|
| 22 |
C |
! Plusieurs de ces diagnostics peuvent être faits en parallèle : |
| 23 |
c====================================================================== |
! les bilans sont sauvegardés dans des tableaux indices. On |
| 24 |
C Arguments: |
! parlera "d'indice de diagnostic". |
| 25 |
C airephy-------input-R- grid area |
|
| 26 |
C tit-----imput-A15- Comment added in PRINT (CHARACTER*15) |
! Jean-Louis Dufresne, July 2002 |
| 27 |
C iprt----input-I- PRINT level ( <=1 : no PRINT) |
|
| 28 |
C idiag---input-I- indice dans lequel sera range les nouveaux |
USE dimphy, ONLY: klev, klon |
| 29 |
C bilans d' entalpie et de masse |
USE suphec_m, ONLY: rcpd, rcpv, rcw, rg, rlvtt |
| 30 |
C idiag2--input-I-les nouveaux bilans d'entalpie et de masse |
|
| 31 |
C sont compare au bilan de d'enthalpie de masse de |
! Arguments: |
| 32 |
C l'indice numero idiag2 |
|
| 33 |
C Cas parriculier : si idiag2=0, pas de comparaison, on |
! Input variables |
| 34 |
c sort directement les bilans d'enthalpie et de masse |
real, intent(in):: airephy(klon) ! grid area |
| 35 |
C dtime----input-R- time step (s) |
CHARACTER(len=*), intent(in):: tit ! comment added in PRINT |
| 36 |
c t--------input-R- temperature (K) |
INTEGER, intent(in):: iprt ! PRINT level ( <=1 : no PRINT) |
| 37 |
c q--------input-R- vapeur d'eau (kg/kg) |
|
| 38 |
c ql-------input-R- liquid watter (kg/kg) |
INTEGER, intent(in):: idiag |
| 39 |
c qs-------input-R- solid watter (kg/kg) |
! indice dans lequel seront rangés les nouveaux bilans d'enthalpie et |
| 40 |
c u--------input-R- vitesse u |
! de masse |
| 41 |
c v--------input-R- vitesse v |
|
| 42 |
c paprs----input-R- pression a intercouche (Pa) |
INTEGER, intent(in):: idiag2 |
| 43 |
c |
! Les nouveaux bilans d'enthalpie et de masse sont comparés au |
| 44 |
C the following total value are computed by UNIT of earth surface |
! bilan de d'enthalpie de masse de l'indice numéro idiag2. Cas |
| 45 |
C |
! particulier : si idiag2=0, pas de comparaison, on sort |
| 46 |
C d_h_vcol--output-R- Heat flux (W/m2) define as the Enthalpy |
! directement les bilans d'enthalpie et de masse. |
| 47 |
c change (J/m2) during one time step (dtime) for the whole |
|
| 48 |
C atmosphere (air, watter vapour, liquid and solid) |
REAL, intent(in):: dtime ! time step (s) |
| 49 |
C d_qt------output-R- total water mass flux (kg/m2/s) defined as the |
REAL, intent(in):: t(klon, klev) ! temperature (K) |
| 50 |
C total watter (kg/m2) change during one time step (dtime), |
REAL, intent(in):: q(klon, klev) ! vapeur d'eau (kg/kg) |
| 51 |
C d_qw------output-R- same, for the watter vapour only (kg/m2/s) |
REAL, intent(in):: ql(klon, klev) ! liquid water (kg/kg) |
| 52 |
C d_ql------output-R- same, for the liquid watter only (kg/m2/s) |
REAL, intent(in):: u(klon, klev), v(klon, klev) ! vitesse |
| 53 |
C d_qs------output-R- same, for the solid watter only (kg/m2/s) |
REAL, intent(in):: paprs(klon, klev+1) ! pression a intercouche (Pa) |
| 54 |
C d_ec------output-R- Cinetic Energy Budget (W/m2) for vertical air column |
|
| 55 |
C |
! The following total values are computed per UNIT of Earth surface |
| 56 |
C other (COMMON...) |
|
| 57 |
C RCPD, RCPV, .... |
REAL, intent(out):: d_h_vcol |
| 58 |
C |
! heat flux (W/m2) defined as the enthalpy change (J/m2) during |
| 59 |
C J.L. Dufresne, July 2002 |
! one time step (dtime) for the whole atmosphere (air, water |
| 60 |
c====================================================================== |
! vapour, liquid and solid) |
| 61 |
|
|
| 62 |
use dimens_m |
REAL, intent(out):: d_qt |
| 63 |
use dimphy |
! total water mass flux (kg/m2/s) defined as the |
| 64 |
use SUPHEC_M |
! total water (kg/m2) change during one time step (dtime) |
| 65 |
use yoethf_m |
|
| 66 |
IMPLICIT NONE |
REAL, intent(out):: d_ec |
| 67 |
C |
! kinetic energy budget (W/m2) for vertical air column |
| 68 |
C |
|
| 69 |
c Input variables |
! Local: |
| 70 |
real airephy(klon) |
|
| 71 |
CHARACTER*15 tit |
REAL d_qw |
| 72 |
INTEGER iprt,idiag, idiag2 |
! water vapour mass flux (kg/m2/s) defined as the water vapour |
| 73 |
REAL, intent(in):: dtime |
! (kg/m2) change during one time step (dtime) |
| 74 |
REAL t(klon,klev), q(klon,klev), ql(klon,klev), qs(klon,klev) |
|
| 75 |
REAL u(klon,klev), v(klon,klev) |
REAL d_ql ! same, for the liquid water only (kg/m2/s) |
| 76 |
REAL, intent(in):: paprs(klon,klev+1) |
|
| 77 |
c Output variables |
REAL h_vcol_tot |
| 78 |
REAL d_h_vcol, d_qt, d_qw, d_ql, d_qs, d_ec |
! total enthalpy of vertical air column (air with water vapour, |
| 79 |
C |
! liquid and solid) (J/m2) |
| 80 |
C Local variables |
|
| 81 |
c |
REAL h_dair_tot ! total enthalpy of dry air (J/m2) |
| 82 |
REAL h_vcol_tot, h_dair_tot, h_qw_tot, h_ql_tot |
REAL h_qw_tot ! total enthalpy of water vapour (J/m2) |
| 83 |
. , h_qs_tot, qw_tot, ql_tot, qs_tot , ec_tot |
REAL h_ql_tot ! total enthalpy of liquid water (J/m2) |
| 84 |
c h_vcol_tot-- total enthalpy of vertical air column |
REAL qw_tot ! total mass of water vapour (kg/m2) |
| 85 |
C (air with watter vapour, liquid and solid) (J/m2) |
REAL ql_tot ! total mass of liquid water (kg/m2) |
| 86 |
c h_dair_tot-- total enthalpy of dry air (J/m2) |
real ec_tot ! total kinetic energy (kg/m2) |
| 87 |
c h_qw_tot---- total enthalpy of watter vapour (J/m2) |
REAL zairm(klon, klev) ! layer air mass (kg/m2) |
| 88 |
c h_ql_tot---- total enthalpy of liquid watter (J/m2) |
REAL zqw_col(klon) |
| 89 |
c h_qs_tot---- total enthalpy of solid watter (J/m2) |
REAL zql_col(klon) |
| 90 |
c qw_tot------ total mass of watter vapour (kg/m2) |
REAL zec_col(klon) |
| 91 |
c ql_tot------ total mass of liquid watter (kg/m2) |
REAL zh_dair_col(klon) |
| 92 |
c qs_tot------ total mass of solid watter (kg/m2) |
REAL zh_qw_col(klon), zh_ql_col(klon) |
| 93 |
c ec_tot------ total cinetic energy (kg/m2) |
REAL airetot, zcpvap, zcwat |
| 94 |
C |
INTEGER i, k |
| 95 |
REAL zairm(klon,klev) ! layer air mass (kg/m2) |
INTEGER, PARAMETER:: ndiag = 10 ! max number of diagnostic in parallel |
| 96 |
REAL zqw_col(klon) |
integer:: pas(ndiag) = 0 |
| 97 |
REAL zql_col(klon) |
REAL, save:: h_vcol_pre(ndiag) |
| 98 |
REAL zqs_col(klon) |
REAL, save:: qw_pre(ndiag), ql_pre(ndiag) |
| 99 |
REAL zec_col(klon) |
REAL, save:: ec_pre(ndiag) |
| 100 |
REAL zh_dair_col(klon) |
|
| 101 |
REAL zh_qw_col(klon), zh_ql_col(klon), zh_qs_col(klon) |
!------------------------------------------------------------- |
| 102 |
C |
|
| 103 |
REAL d_h_dair, d_h_qw, d_h_ql, d_h_qs |
DO k = 1, klev |
| 104 |
C |
DO i = 1, klon |
| 105 |
REAL airetot, zcpvap, zcwat, zcice |
zairm(i, k) = (paprs(i, k)-paprs(i, k+1))/RG |
| 106 |
C |
ENDDO |
| 107 |
INTEGER i, k |
END DO |
| 108 |
C |
|
| 109 |
INTEGER ndiag ! max number of diagnostic in parallel |
! Reset variables |
| 110 |
PARAMETER (ndiag=10) |
DO i = 1, klon |
| 111 |
integer pas(ndiag) |
zqw_col(i)=0. |
| 112 |
save pas |
zql_col(i)=0. |
| 113 |
data pas/ndiag*0/ |
zec_col(i) = 0. |
| 114 |
C |
zh_dair_col(i) = 0. |
| 115 |
REAL h_vcol_pre(ndiag), h_dair_pre(ndiag), h_qw_pre(ndiag) |
zh_qw_col(i) = 0. |
| 116 |
$ , h_ql_pre(ndiag), h_qs_pre(ndiag), qw_pre(ndiag) |
zh_ql_col(i) = 0. |
| 117 |
$ , ql_pre(ndiag), qs_pre(ndiag) , ec_pre(ndiag) |
ENDDO |
| 118 |
SAVE h_vcol_pre, h_dair_pre, h_qw_pre, h_ql_pre |
|
| 119 |
$ , h_qs_pre, qw_pre, ql_pre, qs_pre , ec_pre |
zcpvap=RCPV |
| 120 |
|
zcwat=RCW |
| 121 |
c====================================================================== |
|
| 122 |
C |
! Compute vertical sum for each atmospheric column |
| 123 |
DO k = 1, klev |
DO k = 1, klev |
| 124 |
DO i = 1, klon |
DO i = 1, klon |
| 125 |
C layer air mass |
! Water mass |
| 126 |
zairm(i,k) = (paprs(i,k)-paprs(i,k+1))/RG |
zqw_col(i) = zqw_col(i) + q(i, k)*zairm(i, k) |
| 127 |
ENDDO |
zql_col(i) = zql_col(i) + ql(i, k)*zairm(i, k) |
| 128 |
END DO |
! Kinetic Energy |
| 129 |
C |
zec_col(i) = zec_col(i) +0.5*(u(i, k)**2+v(i, k)**2)*zairm(i, k) |
| 130 |
C Reset variables |
! Air enthalpy |
| 131 |
DO i = 1, klon |
zh_dair_col(i) = zh_dair_col(i) & |
| 132 |
zqw_col(i)=0. |
+ RCPD*(1.-q(i, k)-ql(i, k))*zairm(i, k)*t(i, k) |
| 133 |
zql_col(i)=0. |
zh_qw_col(i) = zh_qw_col(i) + zcpvap*q(i, k)*zairm(i, k)*t(i, k) |
| 134 |
zqs_col(i)=0. |
zh_ql_col(i) = zh_ql_col(i) & |
| 135 |
zec_col(i) = 0. |
+ zcwat*ql(i, k)*zairm(i, k)*t(i, k) & |
| 136 |
zh_dair_col(i) = 0. |
- RLVTT*ql(i, k)*zairm(i, k) |
| 137 |
zh_qw_col(i) = 0. |
END DO |
| 138 |
zh_ql_col(i) = 0. |
ENDDO |
| 139 |
zh_qs_col(i) = 0. |
|
| 140 |
ENDDO |
! Mean over the planet surface |
| 141 |
C |
qw_tot = 0. |
| 142 |
zcpvap=RCPV |
ql_tot = 0. |
| 143 |
zcwat=RCW |
ec_tot = 0. |
| 144 |
zcice=RCS |
h_vcol_tot = 0. |
| 145 |
C |
h_dair_tot = 0. |
| 146 |
C Compute vertical sum for each atmospheric column |
h_qw_tot = 0. |
| 147 |
C ================================================ |
h_ql_tot = 0. |
| 148 |
DO k = 1, klev |
airetot=0. |
| 149 |
DO i = 1, klon |
|
| 150 |
C Watter mass |
do i=1, klon |
| 151 |
zqw_col(i) = zqw_col(i) + q(i,k)*zairm(i,k) |
qw_tot = qw_tot + zqw_col(i)*airephy(i) |
| 152 |
zql_col(i) = zql_col(i) + ql(i,k)*zairm(i,k) |
ql_tot = ql_tot + zql_col(i)*airephy(i) |
| 153 |
zqs_col(i) = zqs_col(i) + qs(i,k)*zairm(i,k) |
ec_tot = ec_tot + zec_col(i)*airephy(i) |
| 154 |
C Cinetic Energy |
h_dair_tot = h_dair_tot + zh_dair_col(i)*airephy(i) |
| 155 |
zec_col(i) = zec_col(i) |
h_qw_tot = h_qw_tot + zh_qw_col(i)*airephy(i) |
| 156 |
$ +0.5*(u(i,k)**2+v(i,k)**2)*zairm(i,k) |
h_ql_tot = h_ql_tot + zh_ql_col(i)*airephy(i) |
| 157 |
C Air enthalpy |
airetot=airetot+airephy(i) |
| 158 |
zh_dair_col(i) = zh_dair_col(i) |
END DO |
| 159 |
$ + RCPD*(1.-q(i,k)-ql(i,k)-qs(i,k))*zairm(i,k)*t(i,k) |
|
| 160 |
zh_qw_col(i) = zh_qw_col(i) |
qw_tot = qw_tot/airetot |
| 161 |
$ + zcpvap*q(i,k)*zairm(i,k)*t(i,k) |
ql_tot = ql_tot/airetot |
| 162 |
zh_ql_col(i) = zh_ql_col(i) |
ec_tot = ec_tot/airetot |
| 163 |
$ + zcwat*ql(i,k)*zairm(i,k)*t(i,k) |
h_dair_tot = h_dair_tot/airetot |
| 164 |
$ - RLVTT*ql(i,k)*zairm(i,k) |
h_qw_tot = h_qw_tot/airetot |
| 165 |
zh_qs_col(i) = zh_qs_col(i) |
h_ql_tot = h_ql_tot/airetot |
| 166 |
$ + zcice*qs(i,k)*zairm(i,k)*t(i,k) |
|
| 167 |
$ - RLSTT*qs(i,k)*zairm(i,k) |
h_vcol_tot = h_dair_tot+h_qw_tot+h_ql_tot |
| 168 |
|
|
| 169 |
END DO |
! Compute the change of the atmospheric state compared to the one |
| 170 |
ENDDO |
! stored in "idiag2", and convert it in flux. This computation is |
| 171 |
C |
! performed if idiag2 /= 0 and if it is not the first call for |
| 172 |
C Mean over the planete surface |
! "idiag". |
| 173 |
C ============================= |
|
| 174 |
qw_tot = 0. |
IF (idiag2 > 0 .and. pas(idiag2) /= 0) THEN |
| 175 |
ql_tot = 0. |
d_h_vcol = (h_vcol_tot - h_vcol_pre(idiag2) )/dtime |
| 176 |
qs_tot = 0. |
d_qw = (qw_tot - qw_pre(idiag2) )/dtime |
| 177 |
ec_tot = 0. |
d_ql = (ql_tot - ql_pre(idiag2) )/dtime |
| 178 |
h_vcol_tot = 0. |
d_ec = (ec_tot - ec_pre(idiag2) )/dtime |
| 179 |
h_dair_tot = 0. |
d_qt = d_qw + d_ql |
| 180 |
h_qw_tot = 0. |
ELSE |
| 181 |
h_ql_tot = 0. |
d_h_vcol = 0. |
| 182 |
h_qs_tot = 0. |
d_qw = 0. |
| 183 |
airetot=0. |
d_ql = 0. |
| 184 |
C |
d_ec = 0. |
| 185 |
do i=1,klon |
d_qt = 0. |
| 186 |
qw_tot = qw_tot + zqw_col(i)*airephy(i) |
ENDIF |
| 187 |
ql_tot = ql_tot + zql_col(i)*airephy(i) |
|
| 188 |
qs_tot = qs_tot + zqs_col(i)*airephy(i) |
IF (iprt >= 2) THEN |
| 189 |
ec_tot = ec_tot + zec_col(i)*airephy(i) |
print 9000, tit, pas(idiag), d_qt, d_qw, d_ql |
| 190 |
h_dair_tot = h_dair_tot + zh_dair_col(i)*airephy(i) |
print 9001, tit, pas(idiag), d_h_vcol |
| 191 |
h_qw_tot = h_qw_tot + zh_qw_col(i)*airephy(i) |
print 9002, tit, pas(idiag), d_ec |
| 192 |
h_ql_tot = h_ql_tot + zh_ql_col(i)*airephy(i) |
END IF |
| 193 |
h_qs_tot = h_qs_tot + zh_qs_col(i)*airephy(i) |
|
| 194 |
airetot=airetot+airephy(i) |
! Store the new atmospheric state in "idiag" |
| 195 |
END DO |
pas(idiag)=pas(idiag)+1 |
| 196 |
C |
h_vcol_pre(idiag) = h_vcol_tot |
| 197 |
qw_tot = qw_tot/airetot |
qw_pre(idiag) = qw_tot |
| 198 |
ql_tot = ql_tot/airetot |
ql_pre(idiag) = ql_tot |
| 199 |
qs_tot = qs_tot/airetot |
ec_pre (idiag) = ec_tot |
| 200 |
ec_tot = ec_tot/airetot |
|
| 201 |
h_dair_tot = h_dair_tot/airetot |
9000 format('Physics water mass budget (kg/m2/s)', A15, 1i6, 10(1pE14.6)) |
| 202 |
h_qw_tot = h_qw_tot/airetot |
9001 format('Physics enthalpy budget (W/m2) ', A15, 1i6, 10(F8.2)) |
| 203 |
h_ql_tot = h_ql_tot/airetot |
9002 format('Physics kinetic energy budget (W/m2) ', A15, 1i6, 10(F8.2)) |
| 204 |
h_qs_tot = h_qs_tot/airetot |
|
| 205 |
C |
END SUBROUTINE diagetpq |
| 206 |
h_vcol_tot = h_dair_tot+h_qw_tot+h_ql_tot+h_qs_tot |
|
| 207 |
C |
end module diagetpq_m |
|
C Compute the change of the atmospheric state compare to the one |
|
|
C stored in "idiag2", and convert it in flux. THis computation |
|
|
C is performed IF idiag2 /= 0 and IF it is not the first CALL |
|
|
c for "idiag" |
|
|
C =================================== |
|
|
C |
|
|
IF ( (idiag2.gt.0) .and. (pas(idiag2) .ne. 0) ) THEN |
|
|
d_h_vcol = (h_vcol_tot - h_vcol_pre(idiag2) )/dtime |
|
|
d_h_dair = (h_dair_tot- h_dair_pre(idiag2))/dtime |
|
|
d_h_qw = (h_qw_tot - h_qw_pre(idiag2) )/dtime |
|
|
d_h_ql = (h_ql_tot - h_ql_pre(idiag2) )/dtime |
|
|
d_h_qs = (h_qs_tot - h_qs_pre(idiag2) )/dtime |
|
|
d_qw = (qw_tot - qw_pre(idiag2) )/dtime |
|
|
d_ql = (ql_tot - ql_pre(idiag2) )/dtime |
|
|
d_qs = (qs_tot - qs_pre(idiag2) )/dtime |
|
|
d_ec = (ec_tot - ec_pre(idiag2) )/dtime |
|
|
d_qt = d_qw + d_ql + d_qs |
|
|
ELSE |
|
|
d_h_vcol = 0. |
|
|
d_h_dair = 0. |
|
|
d_h_qw = 0. |
|
|
d_h_ql = 0. |
|
|
d_h_qs = 0. |
|
|
d_qw = 0. |
|
|
d_ql = 0. |
|
|
d_qs = 0. |
|
|
d_ec = 0. |
|
|
d_qt = 0. |
|
|
ENDIF |
|
|
C |
|
|
IF (iprt.ge.2) THEN |
|
|
WRITE(6,9000) tit,pas(idiag),d_qt,d_qw,d_ql,d_qs |
|
|
9000 format('Phys. Watter Mass Budget (kg/m2/s)',A15 |
|
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$ ,1i6,10(1pE14.6)) |
|
|
WRITE(6,9001) tit,pas(idiag), d_h_vcol |
|
|
9001 format('Phys. Enthalpy Budget (W/m2) ',A15,1i6,10(F8.2)) |
|
|
WRITE(6,9002) tit,pas(idiag), d_ec |
|
|
9002 format('Phys. Cinetic Energy Budget (W/m2) ',A15,1i6,10(F8.2)) |
|
|
END IF |
|
|
C |
|
|
C Store the new atmospheric state in "idiag" |
|
|
C |
|
|
pas(idiag)=pas(idiag)+1 |
|
|
h_vcol_pre(idiag) = h_vcol_tot |
|
|
h_dair_pre(idiag) = h_dair_tot |
|
|
h_qw_pre(idiag) = h_qw_tot |
|
|
h_ql_pre(idiag) = h_ql_tot |
|
|
h_qs_pre(idiag) = h_qs_tot |
|
|
qw_pre(idiag) = qw_tot |
|
|
ql_pre(idiag) = ql_tot |
|
|
qs_pre(idiag) = qs_tot |
|
|
ec_pre (idiag) = ec_tot |
|
|
C |
|
|
RETURN |
|
|
END |
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