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module diagetpq_m |
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guez |
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IMPLICIT NONE |
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guez |
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guez |
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contains |
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SUBROUTINE diagetpq(airephy, tit, iprt, idiag, idiag2, dtime, t, q, ql, qs, & |
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u, v, paprs, d_h_vcol, d_qt, d_qw, d_ql, d_qs, d_ec) |
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! From LMDZ4/libf/phylmd/diagphy.F, version 1.1.1.1 2004/05/19 12:53:08 |
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! Purpose: |
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! Calcule la différence d'enthalpie et de masse d'eau entre deux |
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! appels et calcule le flux de chaleur et le flux d'eau |
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! nécessaires à ces changements. Ces valeurs sont moyennées sur la |
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! surface de tout le globe et sont exprimées en W/m2 et |
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! kg/s/m2. Outil pour diagnostiquer la conservation de l'énergie |
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! et de la masse dans la physique. Suppose que les niveaux de |
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! pression entre les couches ne varient pas entre deux appels. |
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! Plusieurs de ces diagnostics peuvent être faits en parallèle : |
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! les bilans sont sauvegardés dans des tableaux indices. On |
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! parlera "d'indice de diagnostic". |
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! Jean-Louis Dufresne, July 2002 |
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use dimens_m |
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use dimphy |
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use SUPHEC_M |
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use yoethf_m |
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! Arguments: |
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! airephy-------input-R- grid area |
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! tit-----imput-A15- Comment added in PRINT (CHARACTER*15) |
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! iprt----input-I- PRINT level ( <=1 : no PRINT) |
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! idiag---input-I- indice dans lequel sera range les nouveaux |
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! bilans d' entalpie et de masse |
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! idiag2--input-I-les nouveaux bilans d'entalpie et de masse |
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! sont compare au bilan de d'enthalpie de masse de |
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! l'indice numero idiag2 |
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! Cas particulier : si idiag2=0, pas de comparaison, on |
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! sort directement les bilans d'enthalpie et de masse |
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! dtime----input-R- time step (s) |
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! t--------input-R- temperature (K) |
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! q--------input-R- vapeur d'eau (kg/kg) |
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! ql-------input-R- liquid water (kg/kg) |
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! qs-------input-R- solid water (kg/kg) |
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! u--------input-R- vitesse u |
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! v--------input-R- vitesse v |
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! paprs----input-R- pression a intercouche (Pa) |
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! the following total value are computed by UNIT of earth surface |
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! d_h_vcol--output-R- Heat flux (W/m2) define as the Enthalpy |
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! change (J/m2) during one time step (dtime) for the whole |
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! atmosphere (air, water vapour, liquid and solid) |
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! d_qt------output-R- total water mass flux (kg/m2/s) defined as the |
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! total water (kg/m2) change during one time step (dtime), |
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! d_qw------output-R- same, for the water vapour only (kg/m2/s) |
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! d_ql------output-R- same, for the liquid water only (kg/m2/s) |
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! d_qs------output-R- same, for the solid water only (kg/m2/s) |
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! d_ec------output-R- Kinetic Energy Budget (W/m2) for vertical air column |
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! other (COMMON...) |
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! RCPD, RCPV, .... |
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! Input variables |
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real airephy(klon) |
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CHARACTER(len=15) tit |
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INTEGER iprt, idiag, idiag2 |
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REAL, intent(in):: dtime |
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REAL, intent(in):: t(klon, klev) |
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REAL, intent(in):: q(klon, klev), ql(klon, klev), qs(klon, klev) |
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REAL u(klon, klev), v(klon, klev) |
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REAL, intent(in):: paprs(klon, klev+1) |
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! Output variables |
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REAL d_h_vcol, d_qt, d_qw, d_ql, d_qs, d_ec |
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! Local variables |
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REAL h_vcol_tot, h_dair_tot, h_qw_tot, h_ql_tot, h_qs_tot, qw_tot, ql_tot |
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real qs_tot , ec_tot |
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! h_vcol_tot-- total enthalpy of vertical air column |
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! (air with water vapour, liquid and solid) (J/m2) |
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! h_dair_tot-- total enthalpy of dry air (J/m2) |
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! h_qw_tot---- total enthalpy of water vapour (J/m2) |
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! h_ql_tot---- total enthalpy of liquid water (J/m2) |
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! h_qs_tot---- total enthalpy of solid water (J/m2) |
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! qw_tot------ total mass of water vapour (kg/m2) |
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! ql_tot------ total mass of liquid water (kg/m2) |
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! qs_tot------ total mass of solid water (kg/m2) |
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! ec_tot------ total kinetic energy (kg/m2) |
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REAL zairm(klon, klev) ! layer air mass (kg/m2) |
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REAL zqw_col(klon) |
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REAL zql_col(klon) |
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REAL zqs_col(klon) |
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REAL zec_col(klon) |
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REAL zh_dair_col(klon) |
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REAL zh_qw_col(klon), zh_ql_col(klon), zh_qs_col(klon) |
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REAL d_h_dair, d_h_qw, d_h_ql, d_h_qs |
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REAL airetot, zcpvap, zcwat, zcice |
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INTEGER i, k |
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INTEGER, PARAMETER:: ndiag = 10 ! max number of diagnostic in parallel |
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integer:: pas(ndiag) = 0 |
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REAL, save:: h_vcol_pre(ndiag), h_dair_pre(ndiag), h_qw_pre(ndiag) |
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REAL, save:: h_ql_pre(ndiag), h_qs_pre(ndiag), qw_pre(ndiag), ql_pre(ndiag) |
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REAL, save:: qs_pre(ndiag), ec_pre(ndiag) |
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!------------------------------------------------------------- |
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DO k = 1, klev |
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DO i = 1, klon |
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! layer air mass |
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zairm(i, k) = (paprs(i, k)-paprs(i, k+1))/RG |
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ENDDO |
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END DO |
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! Reset variables |
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DO i = 1, klon |
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zqw_col(i)=0. |
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zql_col(i)=0. |
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zqs_col(i)=0. |
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zec_col(i) = 0. |
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zh_dair_col(i) = 0. |
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zh_qw_col(i) = 0. |
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zh_ql_col(i) = 0. |
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zh_qs_col(i) = 0. |
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ENDDO |
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zcpvap=RCPV |
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zcwat=RCW |
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zcice=RCS |
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! Compute vertical sum for each atmospheric column |
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DO k = 1, klev |
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DO i = 1, klon |
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! Water mass |
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zqw_col(i) = zqw_col(i) + q(i, k)*zairm(i, k) |
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zql_col(i) = zql_col(i) + ql(i, k)*zairm(i, k) |
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zqs_col(i) = zqs_col(i) + qs(i, k)*zairm(i, k) |
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! Kinetic Energy |
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zec_col(i) = zec_col(i) +0.5*(u(i, k)**2+v(i, k)**2)*zairm(i, k) |
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! Air enthalpy |
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zh_dair_col(i) = zh_dair_col(i) & |
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+ RCPD*(1.-q(i, k)-ql(i, k)-qs(i, k))*zairm(i, k)*t(i, k) |
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zh_qw_col(i) = zh_qw_col(i) + zcpvap*q(i, k)*zairm(i, k)*t(i, k) |
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zh_ql_col(i) = zh_ql_col(i) & |
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+ zcwat*ql(i, k)*zairm(i, k)*t(i, k) & |
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- RLVTT*ql(i, k)*zairm(i, k) |
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zh_qs_col(i) = zh_qs_col(i) & |
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+ zcice*qs(i, k)*zairm(i, k)*t(i, k) & |
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- RLSTT*qs(i, k)*zairm(i, k) |
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END DO |
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ENDDO |
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! Mean over the planet surface |
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qw_tot = 0. |
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ql_tot = 0. |
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qs_tot = 0. |
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ec_tot = 0. |
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h_vcol_tot = 0. |
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h_dair_tot = 0. |
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h_qw_tot = 0. |
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h_ql_tot = 0. |
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h_qs_tot = 0. |
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airetot=0. |
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do i=1, klon |
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qw_tot = qw_tot + zqw_col(i)*airephy(i) |
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ql_tot = ql_tot + zql_col(i)*airephy(i) |
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qs_tot = qs_tot + zqs_col(i)*airephy(i) |
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ec_tot = ec_tot + zec_col(i)*airephy(i) |
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h_dair_tot = h_dair_tot + zh_dair_col(i)*airephy(i) |
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h_qw_tot = h_qw_tot + zh_qw_col(i)*airephy(i) |
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h_ql_tot = h_ql_tot + zh_ql_col(i)*airephy(i) |
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h_qs_tot = h_qs_tot + zh_qs_col(i)*airephy(i) |
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airetot=airetot+airephy(i) |
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END DO |
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qw_tot = qw_tot/airetot |
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ql_tot = ql_tot/airetot |
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qs_tot = qs_tot/airetot |
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ec_tot = ec_tot/airetot |
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h_dair_tot = h_dair_tot/airetot |
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h_qw_tot = h_qw_tot/airetot |
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h_ql_tot = h_ql_tot/airetot |
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h_qs_tot = h_qs_tot/airetot |
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h_vcol_tot = h_dair_tot+h_qw_tot+h_ql_tot+h_qs_tot |
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! Compute the change of the atmospheric state compared to the one |
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! stored in "idiag2", and convert it in flux. This computation is |
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! performed if idiag2 /= 0 and if it is not the first call for |
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! "idiag". |
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IF ((idiag2 > 0) .and. (pas(idiag2) /= 0)) THEN |
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d_h_vcol = (h_vcol_tot - h_vcol_pre(idiag2) )/dtime |
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d_h_dair = (h_dair_tot- h_dair_pre(idiag2))/dtime |
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d_h_qw = (h_qw_tot - h_qw_pre(idiag2) )/dtime |
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d_h_ql = (h_ql_tot - h_ql_pre(idiag2) )/dtime |
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d_h_qs = (h_qs_tot - h_qs_pre(idiag2) )/dtime |
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d_qw = (qw_tot - qw_pre(idiag2) )/dtime |
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d_ql = (ql_tot - ql_pre(idiag2) )/dtime |
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d_qs = (qs_tot - qs_pre(idiag2) )/dtime |
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d_ec = (ec_tot - ec_pre(idiag2) )/dtime |
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d_qt = d_qw + d_ql + d_qs |
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ELSE |
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d_h_vcol = 0. |
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d_h_dair = 0. |
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d_h_qw = 0. |
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d_h_ql = 0. |
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d_h_qs = 0. |
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d_qw = 0. |
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d_ql = 0. |
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d_qs = 0. |
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d_ec = 0. |
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d_qt = 0. |
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ENDIF |
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IF (iprt >= 2) THEN |
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WRITE(6, 9000) tit, pas(idiag), d_qt, d_qw, d_ql, d_qs |
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9000 format('Phys. Water Mass Budget (kg/m2/s)', A15, 1i6, 10(1pE14.6)) |
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WRITE(6, 9001) tit, pas(idiag), d_h_vcol |
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9001 format('Phys. Enthalpy Budget (W/m2) ', A15, 1i6, 10(F8.2)) |
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WRITE(6, 9002) tit, pas(idiag), d_ec |
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9002 format('Phys. Kinetic Energy Budget (W/m2) ', A15, 1i6, 10(F8.2)) |
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END IF |
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! Store the new atmospheric state in "idiag" |
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pas(idiag)=pas(idiag)+1 |
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h_vcol_pre(idiag) = h_vcol_tot |
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h_dair_pre(idiag) = h_dair_tot |
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h_qw_pre(idiag) = h_qw_tot |
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h_ql_pre(idiag) = h_ql_tot |
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h_qs_pre(idiag) = h_qs_tot |
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qw_pre(idiag) = qw_tot |
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ql_pre(idiag) = ql_tot |
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qs_pre(idiag) = qs_tot |
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ec_pre (idiag) = ec_tot |
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END SUBROUTINE diagetpq |
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end module diagetpq_m |
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