[4664] | 1 | MODULE lmdz_lscp |
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[3999] | 2 | |
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| 3 | IMPLICIT NONE |
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| 4 | |
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| 5 | CONTAINS |
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| 6 | |
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| 7 | !++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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[4380] | 8 | SUBROUTINE lscp(klon,klev,dtime,missing_val, & |
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[5396] | 9 | paprs, pplay, omega, temp, qt, ql_seri, qi_seri, & |
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| 10 | ptconv, ratqs, sigma_qtherm, & |
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[5204] | 11 | d_t, d_q, d_ql, d_qi, rneb, rneblsvol, & |
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[5007] | 12 | pfraclr, pfracld, & |
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| 13 | cldfraliq, sigma2_icefracturb,mean_icefracturb, & |
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[4530] | 14 | radocond, radicefrac, rain, snow, & |
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[3999] | 15 | frac_impa, frac_nucl, beta, & |
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[5007] | 16 | prfl, psfl, rhcl, qta, fraca, & |
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| 17 | tv, pspsk, tla, thl, iflag_cld_th, & |
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[5204] | 18 | iflag_ice_thermo, distcltop, temp_cltop, & |
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| 19 | tke, tke_dissip, & |
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[5575] | 20 | cell_area, stratomask, & |
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[5601] | 21 | cf_seri, qvc_seri, u_seri, v_seri, & |
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[5204] | 22 | qsub, qissr, qcld, subfra, issrfra, gamma_cond, & |
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[5456] | 23 | dcf_sub, dcf_con, dcf_mix, & |
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[5204] | 24 | dqi_adj, dqi_sub, dqi_con, dqi_mix, dqvc_adj, & |
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| 25 | dqvc_sub, dqvc_con, dqvc_mix, qsatl, qsati, & |
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[5601] | 26 | cfa_seri, qta_seri, flight_dist, flight_h2o, & |
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| 27 | qice_cont, Tcritcont, & |
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| 28 | qcritcont, potcontfraP, potcontfraNP, & |
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| 29 | cloudth_sth, & |
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| 30 | cloudth_senv, cloudth_sigmath, cloudth_sigmaenv, & |
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[4830] | 31 | qraindiag, qsnowdiag, dqreva, dqssub, dqrauto, & |
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| 32 | dqrcol, dqrmelt, dqrfreez, dqsauto, dqsagg, dqsrim,& |
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[5589] | 33 | dqsmelt, dqsfreez, dqised, dcfsed, dqvcsed) |
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[3999] | 34 | |
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| 35 | !++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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| 36 | ! Authors: Z.X. Li (LMD), J-L Dufresne (LMD), C. Rio (LMD), J-Y Grandpeix (LMD) |
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| 37 | ! A. JAM (LMD), J-B Madeleine (LMD), E. Vignon (LMD), L. Touzze-Peiffert (LMD) |
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| 38 | !-------------------------------------------------------------------------------- |
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| 39 | ! Date: 01/2021 |
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| 40 | !-------------------------------------------------------------------------------- |
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| 41 | ! Aim: Large Scale Clouds and Precipitation (LSCP) |
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[4226] | 42 | ! |
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[3999] | 43 | ! This code is a new version of the fisrtilp.F90 routine, which is itself a |
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[4072] | 44 | ! merge of 'first' (superrsaturation physics, P. LeVan K. Laval) |
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[3999] | 45 | ! and 'ilp' (il pleut, L. Li) |
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| 46 | ! |
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[4380] | 47 | ! Compared to the original fisrtilp code, lscp |
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[3999] | 48 | ! -> assumes thermcep = .TRUE. all the time (fisrtilp inconsistent when .FALSE.) |
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| 49 | ! -> consider always precipitation thermalisation (fl_cor_ebil>0) |
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| 50 | ! -> option iflag_fisrtilp_qsat<0 no longer possible (qsat does not evolve with T) |
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| 51 | ! -> option "oldbug" by JYG has been removed |
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| 52 | ! -> iflag_t_glace >0 always |
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| 53 | ! -> the 'all or nothing' cloud approach is no longer available (cpartiel=T always) |
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| 54 | ! -> rectangular distribution from L. Li no longer available |
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| 55 | ! -> We always account for the Wegener-Findeisen-Bergeron process (iflag_bergeron = 2 in fisrt) |
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| 56 | !-------------------------------------------------------------------------------- |
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| 57 | ! References: |
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| 58 | ! |
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[4412] | 59 | ! - Bony, S., & Emanuel, K. A. 2001, JAS, doi: 10.1175/1520-0469(2001)058<3158:APOTCA>2.0.CO;2 |
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[3999] | 60 | ! - Hourdin et al. 2013, Clim Dyn, doi:10.1007/s00382-012-1343-y |
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| 61 | ! - Jam et al. 2013, Boundary-Layer Meteorol, doi:10.1007/s10546-012-9789-3 |
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[4412] | 62 | ! - Jouhaud, et al. 2018. JAMES, doi:10.1029/2018MS001379 |
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[3999] | 63 | ! - Madeleine et al. 2020, JAMES, doi:10.1029/2020MS002046 |
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[4412] | 64 | ! - Touzze-Peifert Ludo, PhD thesis, p117-124 |
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[3999] | 65 | ! ------------------------------------------------------------------------------- |
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| 66 | ! Code structure: |
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| 67 | ! |
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[4226] | 68 | ! P0> Thermalization of the precipitation coming from the overlying layer |
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[3999] | 69 | ! P1> Evaporation of the precipitation (falling from the k+1 level) |
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| 70 | ! P2> Cloud formation (at the k level) |
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[4412] | 71 | ! P2.A.1> With the PDFs, calculation of cloud properties using the inital |
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[3999] | 72 | ! values of T and Q |
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| 73 | ! P2.A.2> Coupling between condensed water and temperature |
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| 74 | ! P2.A.3> Calculation of final quantities associated with cloud formation |
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[4412] | 75 | ! P2.B> Release of Latent heat after cloud formation |
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[3999] | 76 | ! P3> Autoconversion to precipitation (k-level) |
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| 77 | ! P4> Wet scavenging |
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| 78 | !------------------------------------------------------------------------------ |
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| 79 | ! Some preliminary comments (JBM) : |
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| 80 | ! |
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| 81 | ! The cloud water that the radiation scheme sees is not the same that the cloud |
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| 82 | ! water used in the physics and the dynamics |
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| 83 | ! |
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[4412] | 84 | ! During the autoconversion to precipitation (P3 step), radocond (cloud water used |
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[3999] | 85 | ! by the radiation scheme) is calculated as an average of the water that remains |
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| 86 | ! in the cloud during the precipitation and not the water remaining at the end |
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| 87 | ! of the time step. The latter is used in the rest of the physics and advected |
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| 88 | ! by the dynamics. |
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| 89 | ! |
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| 90 | ! In summary: |
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| 91 | ! |
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| 92 | ! Radiation: |
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| 93 | ! xflwc(newmicro)+xfiwc(newmicro) = |
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[4412] | 94 | ! radocond=lwcon(nc)+iwcon(nc) |
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[3999] | 95 | ! |
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| 96 | ! Notetheless, be aware of: |
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| 97 | ! |
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[4412] | 98 | ! radocond .NE. ocond(nc) |
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[3999] | 99 | ! i.e.: |
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| 100 | ! lwcon(nc)+iwcon(nc) .NE. ocond(nc) |
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[4412] | 101 | ! but oliq+(ocond-oliq) .EQ. ocond |
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[3999] | 102 | ! (which is not trivial) |
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| 103 | !++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
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[4226] | 104 | ! |
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[4654] | 105 | |
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| 106 | ! USE de modules contenant des fonctions. |
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[4651] | 107 | USE lmdz_cloudth, ONLY : cloudth, cloudth_v3, cloudth_v6, cloudth_mpc |
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[5007] | 108 | USE lmdz_lscp_tools, ONLY : calc_qsat_ecmwf, calc_gammasat |
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[5413] | 109 | USE lmdz_lscp_tools, ONLY : icefrac_lscp, icefrac_lscp_turb, distance_to_cloud_top |
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[5241] | 110 | USE lmdz_lscp_condensation, ONLY : condensation_lognormal, condensation_ice_supersat |
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[5413] | 111 | USE lmdz_lscp_precip, ONLY : histprecip_precld, histprecip_postcld |
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| 112 | USE lmdz_lscp_precip, ONLY : poprecip_precld, poprecip_postcld |
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[3999] | 113 | |
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[4664] | 114 | ! Use du module lmdz_lscp_ini contenant les constantes |
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[5204] | 115 | USE lmdz_lscp_ini, ONLY : prt_level, lunout, eps |
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[5413] | 116 | USE lmdz_lscp_ini, ONLY : seuil_neb, iflag_evap_prec, DDT0 |
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| 117 | USE lmdz_lscp_ini, ONLY : ok_radocond_snow, a_tr_sca |
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| 118 | USE lmdz_lscp_ini, ONLY : iflag_cloudth_vert, iflag_t_glace, iflag_fisrtilp_qsat |
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| 119 | USE lmdz_lscp_ini, ONLY : t_glace_min, min_frac_th_cld |
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| 120 | USE lmdz_lscp_ini, ONLY : RCPD, RLSTT, RLVTT, RVTMP2, RTT, RD, RG |
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[5412] | 121 | USE lmdz_lscp_ini, ONLY : ok_poprecip, ok_bug_phase_lscp |
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[5211] | 122 | USE lmdz_lscp_ini, ONLY : ok_ice_supersat, ok_unadjusted_clouds, iflag_icefrac |
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[5452] | 123 | USE lmdz_lscp_ini, ONLY : ok_plane_contrail |
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[5204] | 124 | |
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[5575] | 125 | ! Temporary call for Lamquin et al (2012) diagnostics |
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| 126 | USE phys_local_var_mod, ONLY : issrfra100to150, issrfra150to200, issrfra200to250 |
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| 127 | USE phys_local_var_mod, ONLY : issrfra250to300, issrfra300to400, issrfra400to500 |
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[5601] | 128 | USE phys_local_var_mod, ONLY : dcfa_ini, dqia_ini, dqta_ini, dcfa_sub, dqia_sub, dqta_sub |
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| 129 | USE phys_local_var_mod, ONLY : dcfa_cir, dqta_cir, dcfa_mix, dqia_mix, dqta_mix |
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[5573] | 130 | |
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[3999] | 131 | IMPLICIT NONE |
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| 132 | |
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| 133 | !=============================================================================== |
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[4380] | 134 | ! VARIABLES DECLARATION |
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[3999] | 135 | !=============================================================================== |
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| 136 | |
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| 137 | ! INPUT VARIABLES: |
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| 138 | !----------------- |
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| 139 | |
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[4380] | 140 | INTEGER, INTENT(IN) :: klon,klev ! number of horizontal grid points and vertical levels |
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[3999] | 141 | REAL, INTENT(IN) :: dtime ! time step [s] |
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[4380] | 142 | REAL, INTENT(IN) :: missing_val ! missing value for output |
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[4059] | 143 | |
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[3999] | 144 | REAL, DIMENSION(klon,klev+1), INTENT(IN) :: paprs ! inter-layer pressure [Pa] |
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| 145 | REAL, DIMENSION(klon,klev), INTENT(IN) :: pplay ! mid-layer pressure [Pa] |
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[4654] | 146 | REAL, DIMENSION(klon,klev), INTENT(IN) :: temp ! temperature (K) |
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[5383] | 147 | REAL, DIMENSION(klon,klev), INTENT(IN) :: omega ! vertical velocity [Pa/s] |
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[4686] | 148 | REAL, DIMENSION(klon,klev), INTENT(IN) :: qt ! total specific humidity (in vapor phase in input) [kg/kg] |
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[5396] | 149 | REAL, DIMENSION(klon,klev), INTENT(IN) :: ql_seri ! liquid specific content [kg/kg] |
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| 150 | REAL, DIMENSION(klon,klev), INTENT(IN) :: qi_seri ! ice specific content [kg/kg] |
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[3999] | 151 | INTEGER, INTENT(IN) :: iflag_cld_th ! flag that determines the distribution of convective clouds |
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| 152 | INTEGER, INTENT(IN) :: iflag_ice_thermo! flag to activate the ice thermodynamics |
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[4226] | 153 | ! CR: if iflag_ice_thermo=2, only convection is active |
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[3999] | 154 | LOGICAL, DIMENSION(klon,klev), INTENT(IN) :: ptconv ! grid points where deep convection scheme is active |
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| 155 | |
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| 156 | !Inputs associated with thermal plumes |
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[4226] | 157 | |
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[5007] | 158 | REAL, DIMENSION(klon,klev), INTENT(IN) :: tv ! virtual potential temperature [K] |
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| 159 | REAL, DIMENSION(klon,klev), INTENT(IN) :: qta ! specific humidity within thermals [kg/kg] |
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| 160 | REAL, DIMENSION(klon,klev), INTENT(IN) :: fraca ! fraction of thermals within the mesh [-] |
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| 161 | REAL, DIMENSION(klon,klev), INTENT(IN) :: pspsk ! exner potential (p/100000)**(R/cp) |
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| 162 | REAL, DIMENSION(klon,klev), INTENT(IN) :: tla ! liquid temperature within thermals [K] |
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[5413] | 163 | REAL, DIMENSION(klon,klev+1), INTENT(IN) :: tke !--turbulent kinetic energy [m2/s2] |
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| 164 | REAL, DIMENSION(klon,klev+1), INTENT(IN) :: tke_dissip !--TKE dissipation [m2/s3] |
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[3999] | 165 | |
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| 166 | ! INPUT/OUTPUT variables |
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| 167 | !------------------------ |
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[4562] | 168 | |
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[5208] | 169 | REAL, DIMENSION(klon,klev), INTENT(INOUT) :: thl ! liquid potential temperature [K] |
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| 170 | REAL, DIMENSION(klon,klev), INTENT(INOUT) :: ratqs,sigma_qtherm ! function of pressure that sets the large-scale |
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[4059] | 171 | |
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[5208] | 172 | |
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[5204] | 173 | ! INPUT/OUTPUT condensation and ice supersaturation |
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| 174 | !-------------------------------------------------- |
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| 175 | REAL, DIMENSION(klon,klev), INTENT(INOUT):: cf_seri ! cloud fraction [-] |
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[5601] | 176 | REAL, DIMENSION(klon,klev), INTENT(INOUT):: qvc_seri ! cloudy water vapor [kg/kg] |
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[5204] | 177 | REAL, DIMENSION(klon,klev), INTENT(IN) :: u_seri ! eastward wind [m/s] |
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| 178 | REAL, DIMENSION(klon,klev), INTENT(IN) :: v_seri ! northward wind [m/s] |
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| 179 | REAL, DIMENSION(klon), INTENT(IN) :: cell_area ! area of each cell [m2] |
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[5575] | 180 | REAL, DIMENSION(klon,klev), INTENT(IN) :: stratomask ! fraction of stratosphere (0 or 1) |
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[4380] | 181 | |
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[5204] | 182 | ! INPUT/OUTPUT aviation |
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| 183 | !-------------------------------------------------- |
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[5601] | 184 | REAL, DIMENSION(klon,klev), INTENT(INOUT):: cfa_seri ! linear contrails fraction [-] |
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| 185 | REAL, DIMENSION(klon,klev), INTENT(INOUT):: qta_seri ! linear contrails total specific humidity [kg/kg] |
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[5575] | 186 | REAL, DIMENSION(klon,klev), INTENT(IN) :: flight_dist ! aviation distance flown within the mesh [m/s/mesh] |
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| 187 | REAL, DIMENSION(klon,klev), INTENT(IN) :: flight_h2o ! aviation H2O emitted within the mesh [kgH2O/s/mesh] |
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[3999] | 188 | |
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| 189 | ! OUTPUT variables |
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| 190 | !----------------- |
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| 191 | |
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[5204] | 192 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: d_t ! temperature increment [K] |
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| 193 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: d_q ! specific humidity increment [kg/kg] |
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| 194 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: d_ql ! liquid water increment [kg/kg] |
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| 195 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: d_qi ! cloud ice mass increment [kg/kg] |
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| 196 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: rneb ! cloud fraction [-] |
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| 197 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: rneblsvol ! cloud fraction per unit volume [-] |
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| 198 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: pfraclr ! precip fraction clear-sky part [-] |
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| 199 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: pfracld ! precip fraction cloudy part [-] |
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[5007] | 200 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: cldfraliq ! liquid fraction of cloud [-] |
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| 201 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: sigma2_icefracturb ! Variance of the diagnostic supersaturation distribution (icefrac_turb) [-] |
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| 202 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: mean_icefracturb ! Mean of the diagnostic supersaturation distribution (icefrac_turb) [-] |
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[5204] | 203 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: radocond ! condensed water used in the radiation scheme [kg/kg] |
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| 204 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: radicefrac ! ice fraction of condensed water for radiation scheme |
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| 205 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: rhcl ! clear-sky relative humidity [-] |
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| 206 | REAL, DIMENSION(klon), INTENT(OUT) :: rain ! surface large-scale rainfall [kg/s/m2] |
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| 207 | REAL, DIMENSION(klon), INTENT(OUT) :: snow ! surface large-scale snowfall [kg/s/m2] |
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| 208 | REAL, DIMENSION(klon,klev+1), INTENT(OUT) :: prfl ! large-scale rainfall flux in the column [kg/s/m2] |
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| 209 | REAL, DIMENSION(klon,klev+1), INTENT(OUT) :: psfl ! large-scale snowfall flux in the column [kg/s/m2] |
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| 210 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: distcltop ! distance to cloud top [m] |
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| 211 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: temp_cltop ! temperature of cloud top [K] |
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| 212 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: beta ! conversion rate of condensed water |
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[4686] | 213 | |
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[5007] | 214 | ! fraction of aerosol scavenging through impaction and nucleation (for on-line) |
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[3999] | 215 | |
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[5007] | 216 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: frac_impa ! scavenging fraction due tu impaction [-] |
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| 217 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: frac_nucl ! scavenging fraction due tu nucleation [-] |
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[3999] | 218 | |
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[5204] | 219 | ! for condensation and ice supersaturation |
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[3999] | 220 | |
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[5204] | 221 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qsub !--specific total water content in sub-saturated clear sky region [kg/kg] |
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| 222 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qissr !--specific total water content in supersat region [kg/kg] |
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| 223 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qcld !--specific total water content in cloudy region [kg/kg] |
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| 224 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: subfra !--mesh fraction of subsaturated clear sky [-] |
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| 225 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: issrfra !--mesh fraction of ISSR [-] |
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| 226 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: gamma_cond !--coefficient governing the ice nucleation RHi threshold [-] |
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| 227 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dcf_sub !--cloud fraction tendency because of sublimation [s-1] |
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| 228 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dcf_con !--cloud fraction tendency because of condensation [s-1] |
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| 229 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dcf_mix !--cloud fraction tendency because of cloud mixing [s-1] |
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| 230 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqi_adj !--specific ice content tendency because of temperature adjustment [kg/kg/s] |
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| 231 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqi_sub !--specific ice content tendency because of sublimation [kg/kg/s] |
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| 232 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqi_con !--specific ice content tendency because of condensation [kg/kg/s] |
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| 233 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqi_mix !--specific ice content tendency because of cloud mixing [kg/kg/s] |
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| 234 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqvc_adj !--specific cloud water vapor tendency because of temperature adjustment [kg/kg/s] |
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| 235 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqvc_sub !--specific cloud water vapor tendency because of sublimation [kg/kg/s] |
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| 236 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqvc_con !--specific cloud water vapor tendency because of condensation [kg/kg/s] |
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| 237 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqvc_mix !--specific cloud water vapor tendency because of cloud mixing [kg/kg/s] |
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| 238 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qsatl !--saturation specific humidity wrt liquid [kg/kg] |
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| 239 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qsati !--saturation specific humidity wrt ice [kg/kg] |
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| 240 | |
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| 241 | ! for contrails and aviation |
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| 242 | |
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[5601] | 243 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qice_cont !--condensed water in linear contrails used in the radiation scheme [kg/kg] |
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[5456] | 244 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: Tcritcont !--critical temperature for contrail formation [K] |
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| 245 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qcritcont !--critical specific humidity for contrail formation [kg/kg] |
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| 246 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: potcontfraP !--potential persistent contrail fraction [-] |
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| 247 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: potcontfraNP !--potential non-persistent contrail fraction [-] |
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[5204] | 248 | |
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| 249 | |
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[4803] | 250 | ! for POPRECIP |
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[4686] | 251 | |
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[4830] | 252 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qraindiag !--DIAGNOSTIC specific rain content [kg/kg] |
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| 253 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: qsnowdiag !--DIAGNOSTIC specific snow content [kg/kg] |
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[4819] | 254 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqreva !--rain tendendy due to evaporation [kg/kg/s] |
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| 255 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqssub !--snow tendency due to sublimation [kg/kg/s] |
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| 256 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqrcol !--rain tendendy due to collection by rain of liquid cloud droplets [kg/kg/s] |
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| 257 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqsagg !--snow tendency due to collection of lcoud ice by aggregation [kg/kg/s] |
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| 258 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqrauto !--rain tendency due to autoconversion of cloud liquid [kg/kg/s] |
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| 259 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqsauto !--snow tendency due to autoconversion of cloud ice [kg/kg/s] |
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| 260 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqsrim !--snow tendency due to riming [kg/kg/s] |
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| 261 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqsmelt !--snow tendency due to melting [kg/kg/s] |
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| 262 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqrmelt !--rain tendency due to melting [kg/kg/s] |
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| 263 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqsfreez !--snow tendency due to freezing [kg/kg/s] |
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| 264 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqrfreez !--rain tendency due to freezing [kg/kg/s] |
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[5589] | 265 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqised !--ice water content tendency due to sedmentation of ice crystals [kg/kg/s] |
---|
| 266 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dcfsed !--cloud fraction tendency due to sedimentation of ice crystals [kg/kg/s] |
---|
| 267 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: dqvcsed !--cloud water vapor tendency due to sedimentation of ice crystals [kg/kg/s] |
---|
[4686] | 268 | |
---|
[5204] | 269 | ! for thermals |
---|
[4803] | 270 | |
---|
[5204] | 271 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: cloudth_sth !--mean saturation deficit in thermals |
---|
| 272 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: cloudth_senv !--mean saturation deficit in environment |
---|
| 273 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: cloudth_sigmath !--std of saturation deficit in thermals |
---|
| 274 | REAL, DIMENSION(klon,klev), INTENT(OUT) :: cloudth_sigmaenv !--std of saturation deficit in environment |
---|
| 275 | |
---|
| 276 | |
---|
[3999] | 277 | ! LOCAL VARIABLES: |
---|
| 278 | !---------------- |
---|
[5601] | 279 | REAL, DIMENSION(klon) :: qliq_in, qice_in |
---|
[4654] | 280 | REAL, DIMENSION(klon,klev) :: ctot |
---|
| 281 | REAL, DIMENSION(klon,klev) :: ctot_vol |
---|
[5450] | 282 | REAL, DIMENSION(klon) :: zqs, zdqs, zqsl, zdqsl, zqsi, zdqsi |
---|
[5413] | 283 | REAL :: zdelta |
---|
[4654] | 284 | REAL, DIMENSION(klon) :: zdqsdT_raw |
---|
[5007] | 285 | REAL, DIMENSION(klon) :: gammasat,dgammasatdt ! coefficient to make cold condensation at the correct RH and derivative wrt T |
---|
| 286 | REAL, DIMENSION(klon) :: Tbef,qlbef,DT ! temperature, humidity and temp. variation during lognormal iteration |
---|
[4654] | 287 | REAL :: num,denom |
---|
| 288 | REAL :: cste |
---|
[4910] | 289 | REAL, DIMENSION(klon) :: zfice_th |
---|
[4654] | 290 | REAL, DIMENSION(klon) :: qcloud, qincloud_mpc |
---|
[5413] | 291 | REAL, DIMENSION(klon) :: zrfl, zifl |
---|
[5450] | 292 | REAL, DIMENSION(klon) :: zoliq, zcond, zq, zqn, zqnl |
---|
[4654] | 293 | REAL, DIMENSION(klon) :: zoliql, zoliqi |
---|
| 294 | REAL, DIMENSION(klon) :: zt |
---|
[5450] | 295 | REAL, DIMENSION(klon) :: zfice,zneb, znebl |
---|
[4654] | 296 | REAL, DIMENSION(klon) :: dzfice |
---|
[5007] | 297 | REAL, DIMENSION(klon) :: zfice_turb, dzfice_turb |
---|
[4654] | 298 | REAL, DIMENSION(klon) :: qtot, qzero |
---|
[3999] | 299 | ! Variables precipitation energy conservation |
---|
[4654] | 300 | REAL, DIMENSION(klon) :: zmqc |
---|
| 301 | REAL :: zalpha_tr |
---|
| 302 | REAL :: zfrac_lessi |
---|
| 303 | REAL, DIMENSION(klon) :: zprec_cond |
---|
| 304 | REAL, DIMENSION(klon) :: zlh_solid |
---|
[4803] | 305 | REAL, DIMENSION(klon) :: ztupnew |
---|
[4913] | 306 | REAL, DIMENSION(klon) :: zqvapclr, zqupnew ! for poprecip evap / subl |
---|
[5589] | 307 | REAL, DIMENSION(klon) :: zqice_sedim ! for sedimentation of ice crystals |
---|
[4654] | 308 | REAL, DIMENSION(klon) :: zrflclr, zrflcld |
---|
| 309 | REAL, DIMENSION(klon) :: ziflclr, ziflcld |
---|
[5411] | 310 | REAL, DIMENSION(klon) :: znebprecip, znebprecipclr, znebprecipcld |
---|
[5413] | 311 | REAL, DIMENSION(klon) :: tot_zneb |
---|
[4654] | 312 | REAL :: qlmpc, qimpc, rnebmpc |
---|
[5007] | 313 | REAL, DIMENSION(klon) :: zdistcltop, ztemp_cltop |
---|
| 314 | REAL, DIMENSION(klon) :: zqliq, zqice, zqvapcl ! for icefrac_lscp_turb |
---|
[5413] | 315 | |
---|
| 316 | ! for quantity of condensates seen by radiation |
---|
| 317 | REAL, DIMENSION(klon) :: zradocond, zradoice |
---|
| 318 | REAL, DIMENSION(klon) :: zrho_up, zvelo_up |
---|
[5204] | 319 | |
---|
| 320 | ! for condensation and ice supersaturation |
---|
[5450] | 321 | REAL, DIMENSION(klon) :: qvc, qvcl, shear |
---|
[5204] | 322 | REAL :: delta_z |
---|
[5452] | 323 | ! for contrails |
---|
[5601] | 324 | REAL, DIMENSION(klon) :: contfra, qcont |
---|
[5452] | 325 | !--Added for ice supersaturation (ok_ice_supersat) and contrails (ok_plane_contrail) |
---|
[5204] | 326 | ! Constants used for calculating ratios that are advected (using a parent-child |
---|
| 327 | ! formalism). This is not done in the dynamical core because at this moment, |
---|
| 328 | ! only isotopes can use this parent-child formalism. Note that the two constants |
---|
| 329 | ! are the same as the one use in the dynamical core, being also defined in |
---|
| 330 | ! dyn3d_common/infotrac.F90 |
---|
| 331 | REAL :: min_qParent, min_ratio |
---|
[5575] | 332 | !--for Lamquin et al 2012 diagnostics |
---|
| 333 | REAL, DIMENSION(klon) :: issrfra100to150UP, issrfra150to200UP, issrfra200to250UP |
---|
| 334 | REAL, DIMENSION(klon) :: issrfra250to300UP, issrfra300to400UP, issrfra400to500UP |
---|
[3999] | 335 | |
---|
[5413] | 336 | INTEGER i, k, kk, iter |
---|
[4654] | 337 | INTEGER, DIMENSION(klon) :: n_i |
---|
[4226] | 338 | INTEGER ncoreczq |
---|
[4654] | 339 | INTEGER, DIMENSION(klon,klev) :: mpc_bl_points |
---|
[4803] | 340 | LOGICAL iftop |
---|
[3999] | 341 | |
---|
[4654] | 342 | LOGICAL, DIMENSION(klon) :: lognormale |
---|
| 343 | LOGICAL, DIMENSION(klon) :: keepgoing |
---|
[3999] | 344 | |
---|
| 345 | CHARACTER (len = 20) :: modname = 'lscp' |
---|
| 346 | CHARACTER (len = 80) :: abort_message |
---|
| 347 | |
---|
| 348 | |
---|
| 349 | !=============================================================================== |
---|
| 350 | ! INITIALISATION |
---|
| 351 | !=============================================================================== |
---|
| 352 | |
---|
[4226] | 353 | ! Few initial checks |
---|
[3999] | 354 | |
---|
[4654] | 355 | |
---|
[3999] | 356 | IF (iflag_fisrtilp_qsat .LT. 0) THEN |
---|
[4226] | 357 | abort_message = 'lscp cannot be used with iflag_fisrtilp<0' |
---|
| 358 | CALL abort_physic(modname,abort_message,1) |
---|
[3999] | 359 | ENDIF |
---|
| 360 | |
---|
| 361 | ! Few initialisations |
---|
| 362 | |
---|
| 363 | ctot_vol(1:klon,1:klev)=0.0 |
---|
| 364 | rneblsvol(1:klon,1:klev)=0.0 |
---|
[5411] | 365 | znebprecip(:)=0.0 |
---|
[4226] | 366 | znebprecipclr(:)=0.0 |
---|
| 367 | znebprecipcld(:)=0.0 |
---|
[3999] | 368 | mpc_bl_points(:,:)=0 |
---|
| 369 | |
---|
| 370 | IF (prt_level>9) WRITE(lunout,*) 'NUAGES4 A. JAM' |
---|
| 371 | |
---|
| 372 | ! AA for 'safety' reasons |
---|
| 373 | zalpha_tr = 0. |
---|
| 374 | zfrac_lessi = 0. |
---|
[4380] | 375 | beta(:,:)= 0. |
---|
[3999] | 376 | |
---|
[4380] | 377 | ! Initialisation of variables: |
---|
| 378 | |
---|
[3999] | 379 | prfl(:,:) = 0.0 |
---|
| 380 | psfl(:,:) = 0.0 |
---|
| 381 | d_t(:,:) = 0.0 |
---|
| 382 | d_q(:,:) = 0.0 |
---|
| 383 | d_ql(:,:) = 0.0 |
---|
| 384 | d_qi(:,:) = 0.0 |
---|
| 385 | rneb(:,:) = 0.0 |
---|
[4530] | 386 | pfraclr(:,:)=0.0 |
---|
| 387 | pfracld(:,:)=0.0 |
---|
[5007] | 388 | cldfraliq(:,:)=0. |
---|
| 389 | sigma2_icefracturb(:,:)=0. |
---|
| 390 | mean_icefracturb(:,:)=0. |
---|
[4412] | 391 | radocond(:,:) = 0.0 |
---|
[3999] | 392 | radicefrac(:,:) = 0.0 |
---|
[4226] | 393 | frac_nucl(:,:) = 1.0 |
---|
| 394 | frac_impa(:,:) = 1.0 |
---|
[3999] | 395 | rain(:) = 0.0 |
---|
| 396 | snow(:) = 0.0 |
---|
[5450] | 397 | zfice(:)=1.0 ! initialized at 1 as by default we assume mpc to be at ice saturation |
---|
[4114] | 398 | dzfice(:)=0.0 |
---|
[5007] | 399 | zfice_turb(:)=0.0 |
---|
| 400 | dzfice_turb(:)=0.0 |
---|
[3999] | 401 | zrfl(:) = 0.0 |
---|
| 402 | zifl(:) = 0.0 |
---|
| 403 | zneb(:) = seuil_neb |
---|
[4226] | 404 | zrflclr(:) = 0.0 |
---|
| 405 | ziflclr(:) = 0.0 |
---|
| 406 | zrflcld(:) = 0.0 |
---|
| 407 | ziflcld(:) = 0.0 |
---|
| 408 | tot_zneb(:) = 0.0 |
---|
| 409 | qzero(:) = 0.0 |
---|
[5007] | 410 | zdistcltop(:)=0.0 |
---|
| 411 | ztemp_cltop(:) = 0.0 |
---|
[4803] | 412 | ztupnew(:)=0.0 |
---|
[5204] | 413 | |
---|
[4654] | 414 | distcltop(:,:)=0. |
---|
| 415 | temp_cltop(:,:)=0. |
---|
[5007] | 416 | |
---|
[5204] | 417 | !--Ice supersaturation |
---|
| 418 | gamma_cond(:,:) = 1. |
---|
| 419 | qissr(:,:) = 0. |
---|
| 420 | issrfra(:,:) = 0. |
---|
| 421 | dcf_sub(:,:) = 0. |
---|
| 422 | dcf_con(:,:) = 0. |
---|
| 423 | dcf_mix(:,:) = 0. |
---|
| 424 | dqi_adj(:,:) = 0. |
---|
| 425 | dqi_sub(:,:) = 0. |
---|
| 426 | dqi_con(:,:) = 0. |
---|
| 427 | dqi_mix(:,:) = 0. |
---|
| 428 | dqvc_adj(:,:) = 0. |
---|
| 429 | dqvc_sub(:,:) = 0. |
---|
| 430 | dqvc_con(:,:) = 0. |
---|
| 431 | dqvc_mix(:,:) = 0. |
---|
| 432 | qvc(:) = 0. |
---|
| 433 | shear(:) = 0. |
---|
| 434 | min_qParent = 1.e-30 |
---|
| 435 | min_ratio = 1.e-16 |
---|
| 436 | |
---|
[5575] | 437 | !--for Lamquin et al (2012) diagnostics |
---|
| 438 | issrfra100to150(:) = 0. |
---|
| 439 | issrfra100to150UP(:) = 0. |
---|
| 440 | issrfra150to200(:) = 0. |
---|
| 441 | issrfra150to200UP(:) = 0. |
---|
| 442 | issrfra200to250(:) = 0. |
---|
| 443 | issrfra200to250UP(:) = 0. |
---|
| 444 | issrfra250to300(:) = 0. |
---|
| 445 | issrfra250to300UP(:) = 0. |
---|
| 446 | issrfra300to400(:) = 0. |
---|
| 447 | issrfra300to400UP(:) = 0. |
---|
| 448 | issrfra400to500(:) = 0. |
---|
| 449 | issrfra400to500UP(:) = 0. |
---|
| 450 | |
---|
[4803] | 451 | !-- poprecip |
---|
[4830] | 452 | qraindiag(:,:)= 0. |
---|
| 453 | qsnowdiag(:,:)= 0. |
---|
[4819] | 454 | dqreva(:,:) = 0. |
---|
| 455 | dqrauto(:,:) = 0. |
---|
| 456 | dqrmelt(:,:) = 0. |
---|
| 457 | dqrfreez(:,:) = 0. |
---|
| 458 | dqrcol(:,:) = 0. |
---|
| 459 | dqssub(:,:) = 0. |
---|
| 460 | dqsauto(:,:) = 0. |
---|
| 461 | dqsrim(:,:) = 0. |
---|
| 462 | dqsagg(:,:) = 0. |
---|
| 463 | dqsfreez(:,:) = 0. |
---|
| 464 | dqsmelt(:,:) = 0. |
---|
[4913] | 465 | zqupnew(:) = 0. |
---|
| 466 | zqvapclr(:) = 0. |
---|
[5589] | 467 | zqice_sedim(:)= 0. |
---|
[3999] | 468 | |
---|
[4803] | 469 | |
---|
| 470 | |
---|
[4392] | 471 | !c_iso: variable initialisation for iso |
---|
| 472 | |
---|
[3999] | 473 | !=============================================================================== |
---|
| 474 | ! BEGINNING OF VERTICAL LOOP FROM TOP TO BOTTOM |
---|
| 475 | !=============================================================================== |
---|
| 476 | |
---|
| 477 | ncoreczq=0 |
---|
| 478 | |
---|
| 479 | DO k = klev, 1, -1 |
---|
| 480 | |
---|
[4803] | 481 | IF (k.LE.klev-1) THEN |
---|
| 482 | iftop=.false. |
---|
| 483 | ELSE |
---|
| 484 | iftop=.true. |
---|
| 485 | ENDIF |
---|
| 486 | |
---|
[3999] | 487 | ! Initialisation temperature and specific humidity |
---|
[5007] | 488 | ! temp(klon,klev) is not modified by the routine, instead all changes in temperature are made on zt |
---|
| 489 | ! at the end of the klon loop, a temperature incremtent d_t due to all processes |
---|
| 490 | ! (thermalization, evap/sub incoming precip, cloud formation, precipitation processes) is calculated |
---|
| 491 | ! d_t = temperature tendency due to lscp |
---|
| 492 | ! The temperature of the overlying layer is updated here because needed for thermalization |
---|
[3999] | 493 | DO i = 1, klon |
---|
[4654] | 494 | zt(i)=temp(i,k) |
---|
[4686] | 495 | zq(i)=qt(i,k) |
---|
[5601] | 496 | qliq_in(i) = ql_seri(i,k) |
---|
| 497 | qice_in(i) = qi_seri(i,k) |
---|
[4803] | 498 | IF (.not. iftop) THEN |
---|
[4913] | 499 | ztupnew(i) = temp(i,k+1) + d_t(i,k+1) |
---|
| 500 | zqupnew(i) = qt(i,k+1) + d_q(i,k+1) + d_ql(i,k+1) + d_qi(i,k+1) |
---|
| 501 | !--zqs(i) is the saturation specific humidity in the layer above |
---|
| 502 | zqvapclr(i) = MAX(0., qt(i,k+1) + d_q(i,k+1) - rneb(i,k+1) * zqs(i)) |
---|
[4803] | 503 | ENDIF |
---|
[4392] | 504 | !c_iso init of iso |
---|
[3999] | 505 | ENDDO |
---|
[5408] | 506 | |
---|
| 507 | ! -------------------------------------------------------------------- |
---|
| 508 | ! P1> Precipitation processes, before cloud formation: |
---|
| 509 | ! Thermalization of precipitation falling from the overlying layer AND |
---|
| 510 | ! Precipitation evaporation/sublimation/melting |
---|
| 511 | !--------------------------------------------------------------------- |
---|
[4803] | 512 | |
---|
| 513 | !================================================================ |
---|
| 514 | ! Flag for the new and more microphysical treatment of precipitation from Atelier Nuage (R) |
---|
[5431] | 515 | IF ( ok_poprecip ) THEN |
---|
[4803] | 516 | |
---|
[5408] | 517 | CALL poprecip_precld(klon, dtime, iftop, paprs(:,k), paprs(:,k+1), pplay(:,k), & |
---|
| 518 | zt, ztupnew, zq, zmqc, znebprecipclr, znebprecipcld, & |
---|
[5589] | 519 | zqvapclr, zqupnew, zqice_sedim, & |
---|
[5601] | 520 | cf_seri(:,k), qvc_seri(:,k), qliq_in, qice_in, & |
---|
[5408] | 521 | zrfl, zrflclr, zrflcld, & |
---|
| 522 | zifl, ziflclr, ziflcld, & |
---|
[5579] | 523 | dqreva(:,k), dqssub(:,k), & |
---|
[5589] | 524 | dcfsed(:,k), dqvcsed(:,k) & |
---|
[5408] | 525 | ) |
---|
[4803] | 526 | |
---|
| 527 | !================================================================ |
---|
| 528 | ELSE |
---|
| 529 | |
---|
[5408] | 530 | CALL histprecip_precld(klon, dtime, iftop, paprs(:,k), paprs(:,k+1), pplay(:,k), & |
---|
[5411] | 531 | zt, ztupnew, zq, zmqc, zneb, znebprecip, znebprecipclr, & |
---|
[5408] | 532 | zrfl, zrflclr, zrflcld, & |
---|
| 533 | zifl, ziflclr, ziflcld, & |
---|
| 534 | dqreva(:,k), dqssub(:,k) & |
---|
| 535 | ) |
---|
[3999] | 536 | |
---|
[4803] | 537 | ENDIF ! (ok_poprecip) |
---|
[3999] | 538 | |
---|
| 539 | ! Calculation of qsat, L/Cp*dqsat/dT and ncoreczq counter |
---|
| 540 | !------------------------------------------------------- |
---|
[4226] | 541 | |
---|
[4072] | 542 | qtot(:)=zq(:)+zmqc(:) |
---|
[5383] | 543 | CALL calc_qsat_ecmwf(klon,zt,qtot,pplay(:,k),RTT,0,.false.,zqs,zdqs) |
---|
[4072] | 544 | DO i = 1, klon |
---|
[3999] | 545 | zdelta = MAX(0.,SIGN(1.,RTT-zt(i))) |
---|
[4059] | 546 | zdqsdT_raw(i) = zdqs(i)*RCPD*(1.0+RVTMP2*zq(i)) / (RLVTT*(1.-zdelta) + RLSTT*zdelta) |
---|
[3999] | 547 | IF (zq(i) .LT. 1.e-15) THEN |
---|
| 548 | ncoreczq=ncoreczq+1 |
---|
| 549 | zq(i)=1.e-15 |
---|
| 550 | ENDIF |
---|
[4392] | 551 | ! c_iso: do something similar for isotopes |
---|
[3999] | 552 | |
---|
[4072] | 553 | ENDDO |
---|
[3999] | 554 | |
---|
| 555 | ! -------------------------------------------------------------------- |
---|
[5408] | 556 | ! P2> Cloud formation |
---|
[3999] | 557 | !--------------------------------------------------------------------- |
---|
| 558 | ! |
---|
| 559 | ! Unlike fisrtilp, we always assume a 'fractional cloud' approach |
---|
| 560 | ! i.e. clouds occupy only a fraction of the mesh (the subgrid distribution |
---|
| 561 | ! is prescribed and depends on large scale variables and boundary layer |
---|
| 562 | ! properties) |
---|
| 563 | ! The decrease in condensed part due tu latent heating is taken into |
---|
| 564 | ! account |
---|
| 565 | ! ------------------------------------------------------------------- |
---|
| 566 | |
---|
[5408] | 567 | ! P2.1> With the PDFs (log-normal, bigaussian) |
---|
[4424] | 568 | ! cloud properties calculation with the initial values of t and q |
---|
[3999] | 569 | ! ---------------------------------------------------------------- |
---|
| 570 | |
---|
| 571 | ! initialise gammasat and qincloud_mpc |
---|
| 572 | gammasat(:)=1. |
---|
| 573 | qincloud_mpc(:)=0. |
---|
| 574 | |
---|
| 575 | IF (iflag_cld_th.GE.5) THEN |
---|
[4910] | 576 | ! Cloud cover and content in meshes affected by shallow convection, |
---|
| 577 | ! are retrieved from a bi-gaussian distribution of the saturation deficit |
---|
| 578 | ! following Jam et al. 2013 |
---|
[3999] | 579 | |
---|
[4910] | 580 | IF (iflag_cloudth_vert.LE.2) THEN |
---|
| 581 | ! Old version of Arnaud Jam |
---|
[3999] | 582 | |
---|
[4910] | 583 | CALL cloudth(klon,klev,k,tv, & |
---|
| 584 | zq,qta,fraca, & |
---|
| 585 | qcloud,ctot,pspsk,paprs,pplay,tla,thl, & |
---|
[4654] | 586 | ratqs,zqs,temp, & |
---|
[4651] | 587 | cloudth_sth,cloudth_senv,cloudth_sigmath,cloudth_sigmaenv) |
---|
[3999] | 588 | |
---|
[4651] | 589 | |
---|
[3999] | 590 | ELSEIF (iflag_cloudth_vert.GE.3 .AND. iflag_cloudth_vert.LE.5) THEN |
---|
[4910] | 591 | ! Default version of Arnaud Jam |
---|
| 592 | |
---|
| 593 | CALL cloudth_v3(klon,klev,k,tv, & |
---|
| 594 | zq,qta,fraca, & |
---|
| 595 | qcloud,ctot,ctot_vol,pspsk,paprs,pplay,tla,thl, & |
---|
[5208] | 596 | ratqs,sigma_qtherm,zqs,temp, & |
---|
[4651] | 597 | cloudth_sth,cloudth_senv,cloudth_sigmath,cloudth_sigmaenv) |
---|
[3999] | 598 | |
---|
| 599 | |
---|
| 600 | ELSEIF (iflag_cloudth_vert.EQ.6) THEN |
---|
[4910] | 601 | ! Jean Jouhaud's version, with specific separation between surface and volume |
---|
| 602 | ! cloud fraction Decembre 2018 |
---|
[3999] | 603 | |
---|
[4910] | 604 | CALL cloudth_v6(klon,klev,k,tv, & |
---|
| 605 | zq,qta,fraca, & |
---|
| 606 | qcloud,ctot,ctot_vol,pspsk,paprs,pplay,tla,thl, & |
---|
[4654] | 607 | ratqs,zqs,temp, & |
---|
[4651] | 608 | cloudth_sth,cloudth_senv,cloudth_sigmath,cloudth_sigmaenv) |
---|
[3999] | 609 | |
---|
[4910] | 610 | ELSEIF (iflag_cloudth_vert .EQ. 7) THEN |
---|
| 611 | ! Updated version of Arnaud Jam (correction by E. Vignon) + adapted treatment |
---|
[5007] | 612 | ! for boundary-layer mixed phase clouds |
---|
[4910] | 613 | CALL cloudth_mpc(klon,klev,k,mpc_bl_points,zt,zq,qta(:,k),fraca(:,k), & |
---|
| 614 | pspsk(:,k),paprs(:,k+1),paprs(:,k),pplay(:,k), tla(:,k), & |
---|
| 615 | ratqs(:,k),qcloud,qincloud_mpc,zfice_th,ctot(:,k),ctot_vol(:,k), & |
---|
| 616 | cloudth_sth(:,k),cloudth_senv(:,k),cloudth_sigmath(:,k),cloudth_sigmaenv(:,k)) |
---|
| 617 | |
---|
[3999] | 618 | ENDIF |
---|
| 619 | |
---|
| 620 | |
---|
| 621 | DO i=1,klon |
---|
| 622 | rneb(i,k)=ctot(i,k) |
---|
| 623 | rneblsvol(i,k)=ctot_vol(i,k) |
---|
| 624 | zqn(i)=qcloud(i) |
---|
[5204] | 625 | !--AB grid-mean vapor in the cloud - we assume saturation adjustment |
---|
| 626 | qvc(i) = rneb(i,k) * zqs(i) |
---|
[3999] | 627 | ENDDO |
---|
| 628 | |
---|
| 629 | ENDIF |
---|
| 630 | |
---|
| 631 | IF (iflag_cld_th .LE. 4) THEN |
---|
| 632 | |
---|
| 633 | ! lognormal |
---|
[5007] | 634 | lognormale(:) = .TRUE. |
---|
[3999] | 635 | |
---|
| 636 | ELSEIF (iflag_cld_th .GE. 6) THEN |
---|
| 637 | |
---|
| 638 | ! lognormal distribution when no thermals |
---|
[5007] | 639 | lognormale(:) = fraca(:,k) < min_frac_th_cld |
---|
[3999] | 640 | |
---|
| 641 | ELSE |
---|
[4226] | 642 | ! When iflag_cld_th=5, we always assume |
---|
[3999] | 643 | ! bi-gaussian distribution |
---|
[5007] | 644 | lognormale(:) = .FALSE. |
---|
[3999] | 645 | |
---|
| 646 | ENDIF |
---|
| 647 | |
---|
| 648 | DT(:) = 0. |
---|
| 649 | n_i(:)=0 |
---|
| 650 | Tbef(:)=zt(:) |
---|
| 651 | qlbef(:)=0. |
---|
| 652 | |
---|
| 653 | ! Treatment of non-boundary layer clouds (lognormale) |
---|
[5383] | 654 | ! We iterate here to take into account the change in qsat(T) and ice fraction |
---|
| 655 | ! during the condensation process |
---|
| 656 | ! the increment in temperature is calculated using the first principle of |
---|
| 657 | ! thermodynamics (enthalpy conservation equation in a mesh composed of a cloud fraction |
---|
| 658 | ! and a clear sky fraction) |
---|
| 659 | ! note that we assume that the vapor in the cloud is at saturation for this calculation |
---|
[4226] | 660 | |
---|
[3999] | 661 | DO iter=1,iflag_fisrtilp_qsat+1 |
---|
[4226] | 662 | |
---|
[5204] | 663 | keepgoing(:) = .FALSE. |
---|
| 664 | |
---|
[3999] | 665 | DO i=1,klon |
---|
| 666 | |
---|
[4424] | 667 | ! keepgoing = .true. while convergence is not satisfied |
---|
[4226] | 668 | |
---|
[5204] | 669 | IF (((ABS(DT(i)).GT.DDT0) .OR. (n_i(i) .EQ. 0)) .AND. lognormale(i)) THEN |
---|
[4226] | 670 | |
---|
[3999] | 671 | ! if not convergence: |
---|
[5204] | 672 | ! we calculate a new iteration |
---|
| 673 | keepgoing(i) = .TRUE. |
---|
[3999] | 674 | |
---|
| 675 | ! P2.2.1> cloud fraction and condensed water mass calculation |
---|
| 676 | ! Calculated variables: |
---|
| 677 | ! rneb : cloud fraction |
---|
| 678 | ! zqn : total water within the cloud |
---|
| 679 | ! zcond: mean condensed water within the mesh |
---|
| 680 | ! rhcl: clear-sky relative humidity |
---|
| 681 | !--------------------------------------------------------------- |
---|
| 682 | |
---|
[4424] | 683 | ! new temperature that only serves in the iteration process: |
---|
[3999] | 684 | Tbef(i)=Tbef(i)+DT(i) |
---|
| 685 | |
---|
| 686 | ! Rneb, qzn and zcond for lognormal PDFs |
---|
[4072] | 687 | qtot(i)=zq(i)+zmqc(i) |
---|
[4226] | 688 | |
---|
[4072] | 689 | ENDIF |
---|
[3999] | 690 | |
---|
[4072] | 691 | ENDDO |
---|
| 692 | |
---|
[4380] | 693 | ! Calculation of saturation specific humidity and ice fraction |
---|
[5383] | 694 | CALL calc_qsat_ecmwf(klon,Tbef,qtot,pplay(:,k),RTT,0,.false.,zqs,zdqs) |
---|
[5450] | 695 | |
---|
| 696 | IF (iflag_icefrac .GE. 3) THEN |
---|
| 697 | ! consider a ice weighted qs to ensure that liquid clouds at T<0 have a consistent cloud fraction |
---|
| 698 | ! and cloud condensed water content. idea following Dietlitcher et al. 2018, GMD |
---|
| 699 | ! we make this option works only for the physically-based and tke-depdenent param (iflag_icefrac>=1) |
---|
| 700 | DO i=1,klon |
---|
| 701 | CALL calc_qsat_ecmwf(klon,Tbef,qtot,pplay(:,k),RTT,1,.false.,zqsl,zdqsl) |
---|
| 702 | CALL calc_qsat_ecmwf(klon,Tbef,qtot,pplay(:,k),RTT,2,.false.,zqsi,zdqsi) |
---|
| 703 | zqs(i)=zfice(i)*zqsi(i)+(1.-zfice(i))*zqsl(i) |
---|
| 704 | zdqs(i)=zfice(i)*zdqsi(i)+zqsi(i)*dzfice(i)+(1.-zfice(i))*zdqsl(i)-zqsl(i)*dzfice(i) |
---|
| 705 | ENDDO |
---|
| 706 | ENDIF |
---|
| 707 | |
---|
[5383] | 708 | CALL calc_gammasat(klon,Tbef,qtot,pplay(:,k),gammasat,dgammasatdt) |
---|
[4072] | 709 | ! saturation may occur at a humidity different from qsat (gamma qsat), so gamma correction for dqs |
---|
| 710 | zdqs(:) = gammasat(:)*zdqs(:)+zqs(:)*dgammasatdt(:) |
---|
| 711 | |
---|
[5450] | 712 | ! Cloud condensation based on subgrid pdf |
---|
[5204] | 713 | !--AB Activates a condensation scheme that allows for |
---|
| 714 | !--ice supersaturation and contrails evolution from aviation |
---|
| 715 | IF (ok_ice_supersat) THEN |
---|
| 716 | |
---|
| 717 | !--Calculate the shear value (input for condensation and ice supersat) |
---|
| 718 | DO i = 1, klon |
---|
| 719 | !--Cell thickness [m] |
---|
| 720 | delta_z = ( paprs(i,k) - paprs(i,k+1) ) / RG / pplay(i,k) * Tbef(i) * RD |
---|
| 721 | IF ( iftop ) THEN |
---|
| 722 | ! top |
---|
| 723 | shear(i) = SQRT( ( (u_seri(i,k) - u_seri(i,k-1)) / delta_z )**2. & |
---|
| 724 | + ( (v_seri(i,k) - v_seri(i,k-1)) / delta_z )**2. ) |
---|
| 725 | ELSEIF ( k .EQ. 1 ) THEN |
---|
| 726 | ! surface |
---|
| 727 | shear(i) = SQRT( ( (u_seri(i,k+1) - u_seri(i,k)) / delta_z )**2. & |
---|
| 728 | + ( (v_seri(i,k+1) - v_seri(i,k)) / delta_z )**2. ) |
---|
| 729 | ELSE |
---|
| 730 | ! other layers |
---|
| 731 | shear(i) = SQRT( ( ( (u_seri(i,k+1) + u_seri(i,k)) / 2. & |
---|
| 732 | - (u_seri(i,k) + u_seri(i,k-1)) / 2. ) / delta_z )**2. & |
---|
| 733 | + ( ( (v_seri(i,k+1) + v_seri(i,k)) / 2. & |
---|
| 734 | - (v_seri(i,k) + v_seri(i,k-1)) / 2. ) / delta_z )**2. ) |
---|
| 735 | ENDIF |
---|
| 736 | ENDDO |
---|
| 737 | |
---|
| 738 | !--------------------------------------------- |
---|
| 739 | !-- CONDENSATION AND ICE SUPERSATURATION -- |
---|
| 740 | !--------------------------------------------- |
---|
| 741 | |
---|
| 742 | CALL condensation_ice_supersat( & |
---|
| 743 | klon, dtime, missing_val, & |
---|
| 744 | pplay(:,k), paprs(:,k), paprs(:,k+1), & |
---|
[5601] | 745 | cf_seri(:,k), qvc_seri(:,k), qliq_in, qice_in, & |
---|
[5575] | 746 | shear, tke_dissip(:,k), cell_area, stratomask(:,k), & |
---|
[5406] | 747 | Tbef, zq, zqs, gammasat, ratqs(:,k), keepgoing, & |
---|
| 748 | rneb(:,k), zqn, qvc, issrfra(:,k), qissr(:,k), & |
---|
[5204] | 749 | dcf_sub(:,k), dcf_con(:,k), dcf_mix(:,k), & |
---|
| 750 | dqi_adj(:,k), dqi_sub(:,k), dqi_con(:,k), dqi_mix(:,k), & |
---|
| 751 | dqvc_adj(:,k), dqvc_sub(:,k), dqvc_con(:,k), dqvc_mix(:,k), & |
---|
[5601] | 752 | cfa_seri(:,k), qta_seri(:,k), flight_dist(:,k), flight_h2o(:,k), & |
---|
| 753 | contfra, qcont, Tcritcont(:,k), qcritcont(:,k), & |
---|
| 754 | potcontfraP(:,k), potcontfraNP(:,k), & |
---|
| 755 | dcfa_ini(:,k), dqia_ini(:,k), dqta_ini(:,k), & |
---|
| 756 | dcfa_sub(:,k), dqia_sub(:,k), dqta_sub(:,k), & |
---|
| 757 | dcfa_cir(:,k), dqta_cir(:,k), & |
---|
| 758 | dcfa_mix(:,k), dqia_mix(:,k), dqta_mix(:,k)) |
---|
[5204] | 759 | |
---|
| 760 | |
---|
[5211] | 761 | ELSE |
---|
| 762 | !--generalised lognormal condensation scheme (Bony and Emanuel 2001) |
---|
| 763 | |
---|
[5241] | 764 | CALL condensation_lognormal( & |
---|
| 765 | klon, Tbef, zq, zqs, gammasat, ratqs(:,k), & |
---|
| 766 | keepgoing, rneb(:,k), zqn, qvc) |
---|
[5204] | 767 | |
---|
| 768 | |
---|
| 769 | ENDIF ! .NOT. ok_ice_supersat |
---|
[4226] | 770 | |
---|
[5450] | 771 | ! cloud phase determination |
---|
| 772 | IF (iflag_icefrac .GE. 2) THEN |
---|
| 773 | ! phase partitioning depending on temperature. activates here in the iteration process if iflag_icefrac > 2 |
---|
[5579] | 774 | CALL icefrac_lscp_turb(klon, dtime, Tbef, pplay(:,k), paprs(:,k), paprs(:,k+1), omega(:,k), qice_in, ziflcld, zqn, & |
---|
[5450] | 775 | rneb(:,k), tke(:,k), tke_dissip(:,k), zqliq, zqvapcl, zqice, zfice, dzfice, cldfraliq(:,k),sigma2_icefracturb(:,k), mean_icefracturb(:,k)) |
---|
| 776 | ELSE |
---|
| 777 | ! phase partitioning depending on temperature and eventually distance to cloud top |
---|
| 778 | IF (iflag_t_glace.GE.4) THEN |
---|
| 779 | ! For iflag_t_glace GE 4 the phase partition function dependends on temperature AND distance to cloud top |
---|
| 780 | CALL distance_to_cloud_top(klon,klev,k,temp,pplay,paprs,rneb,zdistcltop,ztemp_cltop) |
---|
| 781 | ENDIF |
---|
| 782 | CALL icefrac_lscp(klon, zt, iflag_ice_thermo, zdistcltop,ztemp_cltop,zfice,dzfice) |
---|
| 783 | ENDIF |
---|
| 784 | |
---|
| 785 | |
---|
[5204] | 786 | DO i=1,klon |
---|
| 787 | IF (keepgoing(i)) THEN |
---|
[3999] | 788 | |
---|
| 789 | ! If vertical heterogeneity, change fraction by volume as well |
---|
| 790 | IF (iflag_cloudth_vert.GE.3) THEN |
---|
| 791 | ctot_vol(i,k)=rneb(i,k) |
---|
| 792 | rneblsvol(i,k)=ctot_vol(i,k) |
---|
| 793 | ENDIF |
---|
| 794 | |
---|
| 795 | |
---|
[4072] | 796 | ! P2.2.2> Approximative calculation of temperature variation DT |
---|
| 797 | ! due to condensation. |
---|
| 798 | ! Calculated variables: |
---|
| 799 | ! dT : temperature change due to condensation |
---|
| 800 | !--------------------------------------------------------------- |
---|
[3999] | 801 | |
---|
| 802 | |
---|
| 803 | IF (zfice(i).LT.1) THEN |
---|
| 804 | cste=RLVTT |
---|
| 805 | ELSE |
---|
| 806 | cste=RLSTT |
---|
| 807 | ENDIF |
---|
[5007] | 808 | |
---|
[5204] | 809 | IF ( ok_unadjusted_clouds ) THEN |
---|
| 810 | !--AB We relax the saturation adjustment assumption |
---|
| 811 | !-- qvc (grid-mean vapor in cloud) is calculated by the condensation scheme |
---|
| 812 | IF ( rneb(i,k) .GT. eps ) THEN |
---|
| 813 | qlbef(i) = MAX(0., zqn(i) - qvc(i) / rneb(i,k)) |
---|
| 814 | ELSE |
---|
| 815 | qlbef(i) = 0. |
---|
| 816 | ENDIF |
---|
| 817 | ELSE |
---|
| 818 | qlbef(i)=max(0.,zqn(i)-zqs(i)) |
---|
| 819 | ENDIF |
---|
| 820 | |
---|
[3999] | 821 | num = -Tbef(i)+zt(i)+rneb(i,k)*((1-zfice(i))*RLVTT & |
---|
[4226] | 822 | +zfice(i)*RLSTT)/RCPD/(1.0+RVTMP2*(zq(i)+zmqc(i)))*qlbef(i) |
---|
[3999] | 823 | denom = 1.+rneb(i,k)*((1-zfice(i))*RLVTT+zfice(i)*RLSTT)/cste*zdqs(i) & |
---|
| 824 | -(RLSTT-RLVTT)/RCPD/(1.0+RVTMP2*(zq(i)+zmqc(i)))*rneb(i,k) & |
---|
[4226] | 825 | *qlbef(i)*dzfice(i) |
---|
[4424] | 826 | ! here we update a provisory temperature variable that only serves in the iteration |
---|
| 827 | ! process |
---|
[3999] | 828 | DT(i)=num/denom |
---|
| 829 | n_i(i)=n_i(i)+1 |
---|
| 830 | |
---|
[4424] | 831 | ENDIF ! end keepgoing |
---|
[3999] | 832 | |
---|
| 833 | ENDDO ! end loop on i |
---|
| 834 | |
---|
| 835 | ENDDO ! iter=1,iflag_fisrtilp_qsat+1 |
---|
| 836 | |
---|
[5408] | 837 | ! P2.2> Final quantities calculation |
---|
[3999] | 838 | ! Calculated variables: |
---|
| 839 | ! rneb : cloud fraction |
---|
| 840 | ! zcond: mean condensed water in the mesh |
---|
| 841 | ! zqn : mean water vapor in the mesh |
---|
[4562] | 842 | ! zfice: ice fraction in clouds |
---|
[3999] | 843 | ! zt : temperature |
---|
| 844 | ! rhcl : clear-sky relative humidity |
---|
| 845 | ! ---------------------------------------------------------------- |
---|
| 846 | |
---|
| 847 | |
---|
[5450] | 848 | ! Cloud phase final determination |
---|
| 849 | !-------------------------------- |
---|
[4562] | 850 | ! For iflag_t_glace GE 4 the phase partition function dependends on temperature AND distance to cloud top |
---|
| 851 | IF (iflag_t_glace.GE.4) THEN |
---|
[5007] | 852 | CALL distance_to_cloud_top(klon,klev,k,temp,pplay,paprs,rneb,zdistcltop,ztemp_cltop) |
---|
| 853 | distcltop(:,k)=zdistcltop(:) |
---|
| 854 | temp_cltop(:,k)=ztemp_cltop(:) |
---|
| 855 | ENDIF |
---|
[5450] | 856 | ! Partition function depending on temperature for all clouds (shallow convective and stratiform) |
---|
[5204] | 857 | CALL icefrac_lscp(klon, zt, iflag_ice_thermo, zdistcltop, ztemp_cltop, zfice, dzfice) |
---|
[4562] | 858 | |
---|
[5450] | 859 | ! Partition function depending on tke for non shallow-convective clouds, erase previous estimation |
---|
[5007] | 860 | IF (iflag_icefrac .GE. 1) THEN |
---|
[5579] | 861 | CALL icefrac_lscp_turb(klon, dtime, Tbef, pplay(:,k), paprs(:,k), paprs(:,k+1), omega(:,k), qice_in, ziflcld, zqn, & |
---|
[5007] | 862 | rneb(:,k), tke(:,k), tke_dissip(:,k), zqliq, zqvapcl, zqice, zfice_turb, dzfice_turb, cldfraliq(:,k),sigma2_icefracturb(:,k), mean_icefracturb(:,k)) |
---|
| 863 | ENDIF |
---|
| 864 | |
---|
[5450] | 865 | ! Water vapor update, subsequent latent heat exchange for each cloud type |
---|
| 866 | !------------------------------------------------------------------------ |
---|
[3999] | 867 | DO i=1, klon |
---|
[5007] | 868 | ! Overwrite phase partitioning in boundary layer mixed phase clouds when the |
---|
| 869 | ! iflag_cloudth_vert=7 and specific param is activated |
---|
[3999] | 870 | IF (mpc_bl_points(i,k) .GT. 0) THEN |
---|
| 871 | zcond(i) = MAX(0.0,qincloud_mpc(i))*rneb(i,k) |
---|
| 872 | ! following line is very strange and probably wrong |
---|
| 873 | rhcl(i,k)= (zqs(i)+zq(i))/2./zqs(i) |
---|
| 874 | ! water vapor update and partition function if thermals |
---|
| 875 | zq(i) = zq(i) - zcond(i) |
---|
[4910] | 876 | zfice(i)=zfice_th(i) |
---|
[3999] | 877 | ELSE |
---|
| 878 | ! Checks on rneb, rhcl and zqn |
---|
| 879 | IF (rneb(i,k) .LE. 0.0) THEN |
---|
| 880 | zqn(i) = 0.0 |
---|
| 881 | rneb(i,k) = 0.0 |
---|
| 882 | zcond(i) = 0.0 |
---|
| 883 | rhcl(i,k)=zq(i)/zqs(i) |
---|
| 884 | ELSE IF (rneb(i,k) .GE. 1.0) THEN |
---|
| 885 | zqn(i) = zq(i) |
---|
| 886 | rneb(i,k) = 1.0 |
---|
[5204] | 887 | IF ( ok_unadjusted_clouds ) THEN |
---|
| 888 | !--AB We relax the saturation adjustment assumption |
---|
| 889 | !-- qvc (grid-mean vapor in cloud) is calculated by the condensation scheme |
---|
| 890 | zcond(i) = MAX(0., zqn(i) - qvc(i)) |
---|
| 891 | ELSE |
---|
| 892 | zcond(i) = MAX(0.0,zqn(i)-zqs(i)) |
---|
| 893 | ENDIF |
---|
[3999] | 894 | rhcl(i,k)=1.0 |
---|
| 895 | ELSE |
---|
[5204] | 896 | IF ( ok_unadjusted_clouds ) THEN |
---|
| 897 | !--AB We relax the saturation adjustment assumption |
---|
| 898 | !-- qvc (grid-mean vapor in cloud) is calculated by the condensation scheme |
---|
| 899 | zcond(i) = MAX(0., zqn(i) * rneb(i,k) - qvc(i)) |
---|
| 900 | ELSE |
---|
| 901 | zcond(i) = MAX(0.0,zqn(i)-zqs(i))*rneb(i,k) |
---|
| 902 | ENDIF |
---|
[3999] | 903 | ! following line is very strange and probably wrong: |
---|
| 904 | rhcl(i,k)=(zqs(i)+zq(i))/2./zqs(i) |
---|
[5007] | 905 | ! Overwrite partitioning for non shallow-convective clouds if iflag_icefrac>1 (icefrac turb param) |
---|
| 906 | IF (iflag_icefrac .GE. 1) THEN |
---|
| 907 | IF (lognormale(i)) THEN |
---|
| 908 | zcond(i) = zqliq(i) + zqice(i) |
---|
[5450] | 909 | zfice(i) = zfice_turb(i) |
---|
[5007] | 910 | rhcl(i,k) = zqvapcl(i) * rneb(i,k) + (zq(i) - zqn(i)) * (1.-rneb(i,k)) |
---|
| 911 | ENDIF |
---|
| 912 | ENDIF |
---|
[3999] | 913 | ENDIF |
---|
| 914 | |
---|
[4226] | 915 | ! water vapor update |
---|
| 916 | zq(i) = zq(i) - zcond(i) |
---|
[3999] | 917 | |
---|
| 918 | ENDIF |
---|
[5450] | 919 | |
---|
| 920 | |
---|
[3999] | 921 | ! temperature update due to phase change |
---|
| 922 | zt(i) = zt(i) + (1.-zfice(i))*zcond(i) & |
---|
| 923 | & * RLVTT/RCPD/(1.0+RVTMP2*(zq(i)+zmqc(i)+zcond(i))) & |
---|
| 924 | +zfice(i)*zcond(i) * RLSTT/RCPD/(1.0+RVTMP2*(zq(i)+zmqc(i)+zcond(i))) |
---|
| 925 | ENDDO |
---|
| 926 | |
---|
| 927 | ! If vertical heterogeneity, change volume fraction |
---|
| 928 | IF (iflag_cloudth_vert .GE. 3) THEN |
---|
| 929 | ctot_vol(1:klon,k)=min(max(ctot_vol(1:klon,k),0.),1.) |
---|
| 930 | rneblsvol(1:klon,k)=ctot_vol(1:klon,k) |
---|
| 931 | ENDIF |
---|
| 932 | |
---|
[5204] | 933 | |
---|
[3999] | 934 | ! ---------------------------------------------------------------- |
---|
[5408] | 935 | ! P3> Precipitation processes, after cloud formation |
---|
| 936 | ! - precipitation formation, melting/freezing |
---|
[3999] | 937 | ! ---------------------------------------------------------------- |
---|
[4226] | 938 | |
---|
[5413] | 939 | ! Initiate the quantity of liquid and solid condensates |
---|
| 940 | ! Note that in the following, zcond is the total amount of condensates |
---|
| 941 | ! including newly formed precipitations (i.e., condensates formed by the |
---|
| 942 | ! condensation process), while zoliq is the total amount of condensates in |
---|
| 943 | ! the cloud (i.e., on which precipitation processes have applied) |
---|
| 944 | DO i = 1, klon |
---|
| 945 | zoliq(i) = zcond(i) |
---|
| 946 | zoliql(i) = zcond(i) * ( 1. - zfice(i) ) |
---|
| 947 | zoliqi(i) = zcond(i) * zfice(i) |
---|
| 948 | ENDDO |
---|
| 949 | |
---|
[5579] | 950 | IF (ok_plane_contrail) THEN |
---|
| 951 | !--Contrails do not precipitate. We remove then from the variables temporarily |
---|
[5593] | 952 | DO i = 1, klon |
---|
[5601] | 953 | rneb(i,k) = rneb(i,k) - contfra(i) |
---|
| 954 | zoliqi(i) = zoliqi(i) - ( qcont(i) - zqs(i) * contfra(i) ) |
---|
[5593] | 955 | ENDDO |
---|
[5579] | 956 | ENDIF |
---|
| 957 | |
---|
[4803] | 958 | !================================================================ |
---|
[5408] | 959 | ! Flag for the new and more microphysical treatment of precipitation from Atelier Nuage (R) |
---|
[4803] | 960 | IF (ok_poprecip) THEN |
---|
| 961 | |
---|
| 962 | CALL poprecip_postcld(klon, dtime, paprs(:,k), paprs(:,k+1), pplay(:,k), & |
---|
| 963 | ctot_vol(:,k), ptconv(:,k), & |
---|
| 964 | zt, zq, zoliql, zoliqi, zfice, & |
---|
[5589] | 965 | rneb(:,k), zqice_sedim, znebprecipclr, znebprecipcld, & |
---|
[4803] | 966 | zrfl, zrflclr, zrflcld, & |
---|
| 967 | zifl, ziflclr, ziflcld, & |
---|
[4830] | 968 | qraindiag(:,k), qsnowdiag(:,k), dqrauto(:,k), & |
---|
[4819] | 969 | dqrcol(:,k), dqrmelt(:,k), dqrfreez(:,k), & |
---|
| 970 | dqsauto(:,k), dqsagg(:,k), dqsrim(:,k), & |
---|
[5589] | 971 | dqsmelt(:,k), dqsfreez(:,k), dqised(:,k) & |
---|
[4803] | 972 | ) |
---|
[5431] | 973 | DO i = 1, klon |
---|
| 974 | zoliq(i) = zoliql(i) + zoliqi(i) |
---|
| 975 | ENDDO |
---|
[4803] | 976 | |
---|
| 977 | !================================================================ |
---|
| 978 | ELSE |
---|
| 979 | |
---|
[5413] | 980 | CALL histprecip_postcld(klon, dtime, iftop, paprs(:,k), paprs(:,k+1), pplay(:,k), & |
---|
| 981 | ctot_vol(:,k), ptconv(:,k), zdqsdT_raw, & |
---|
| 982 | zt, zq, zoliq, zoliql, zoliqi, zcond, zfice, zmqc, & |
---|
| 983 | rneb(:,k), znebprecipclr, znebprecipcld, & |
---|
| 984 | zneb, tot_zneb, zrho_up, zvelo_up, & |
---|
| 985 | zrfl, zrflclr, zrflcld, zifl, ziflclr, ziflcld, & |
---|
| 986 | zradocond, zradoice, dqrauto(:,k), dqsauto(:,k) & |
---|
| 987 | ) |
---|
[3999] | 988 | |
---|
[4803] | 989 | ENDIF ! ok_poprecip |
---|
[5579] | 990 | |
---|
| 991 | IF (ok_plane_contrail) THEN |
---|
| 992 | !--Contrails are reintroduced in the variables |
---|
[5593] | 993 | DO i = 1, klon |
---|
[5601] | 994 | rneb(i,k) = rneb(i,k) + contfra(i) |
---|
| 995 | zoliqi(i) = zoliqi(i) + ( qcont(i) - zqs(i) * contfra(i) ) |
---|
[5593] | 996 | ENDDO |
---|
[5579] | 997 | ENDIF |
---|
[4803] | 998 | |
---|
[5408] | 999 | ! End of precipitation processes after cloud formation |
---|
| 1000 | ! ---------------------------------------------------- |
---|
[3999] | 1001 | |
---|
[5406] | 1002 | !---------------------------------------------------------------------- |
---|
[5408] | 1003 | ! P4> Calculation of cloud condensates amount seen by radiative scheme |
---|
[5406] | 1004 | !---------------------------------------------------------------------- |
---|
[4803] | 1005 | |
---|
[5413] | 1006 | DO i=1,klon |
---|
[3999] | 1007 | |
---|
[5413] | 1008 | IF (ok_poprecip) THEN |
---|
| 1009 | IF (ok_radocond_snow) THEN |
---|
| 1010 | radocond(i,k) = zoliq(i) |
---|
| 1011 | zradoice(i) = zoliqi(i) + qsnowdiag(i,k) |
---|
| 1012 | ELSE |
---|
| 1013 | radocond(i,k) = zoliq(i) |
---|
| 1014 | zradoice(i) = zoliqi(i) |
---|
| 1015 | ENDIF |
---|
| 1016 | ELSE |
---|
| 1017 | radocond(i,k) = zradocond(i) |
---|
| 1018 | ENDIF |
---|
[4114] | 1019 | |
---|
[5413] | 1020 | ! calculate the percentage of ice in "radocond" so cloud+precip seen |
---|
| 1021 | ! by the radiation scheme |
---|
| 1022 | IF (radocond(i,k) .GT. 0.) THEN |
---|
| 1023 | radicefrac(i,k)=MIN(MAX(zradoice(i)/radocond(i,k),0.),1.) |
---|
| 1024 | ENDIF |
---|
[4114] | 1025 | ENDDO |
---|
| 1026 | |
---|
[3999] | 1027 | ! ---------------------------------------------------------------- |
---|
[5408] | 1028 | ! P5> Wet scavenging |
---|
[3999] | 1029 | ! ---------------------------------------------------------------- |
---|
| 1030 | |
---|
| 1031 | !Scavenging through nucleation in the layer |
---|
| 1032 | |
---|
| 1033 | DO i = 1,klon |
---|
| 1034 | |
---|
| 1035 | IF(zcond(i).GT.zoliq(i)+1.e-10) THEN |
---|
| 1036 | beta(i,k) = (zcond(i)-zoliq(i))/zcond(i)/dtime |
---|
| 1037 | ELSE |
---|
| 1038 | beta(i,k) = 0. |
---|
| 1039 | ENDIF |
---|
| 1040 | |
---|
[4059] | 1041 | zprec_cond(i) = MAX(zcond(i)-zoliq(i),0.0)*(paprs(i,k)-paprs(i,k+1))/RG |
---|
[3999] | 1042 | |
---|
| 1043 | IF (rneb(i,k).GT.0.0.AND.zprec_cond(i).GT.0.) THEN |
---|
| 1044 | |
---|
[4654] | 1045 | IF (temp(i,k) .GE. t_glace_min) THEN |
---|
[3999] | 1046 | zalpha_tr = a_tr_sca(3) |
---|
| 1047 | ELSE |
---|
| 1048 | zalpha_tr = a_tr_sca(4) |
---|
| 1049 | ENDIF |
---|
| 1050 | |
---|
[5450] | 1051 | zfrac_lessi = 1. - EXP(zalpha_tr*zprec_cond(i)/MAX(rneb(i,k),seuil_neb)) |
---|
| 1052 | frac_nucl(i,k)= 1.-MAX(rneb(i,k),seuil_neb)*zfrac_lessi |
---|
[4226] | 1053 | |
---|
[3999] | 1054 | ! Nucleation with a factor of -1 instead of -0.5 |
---|
[5450] | 1055 | zfrac_lessi = 1. - EXP(-zprec_cond(i)/MAX(rneb(i,k),seuil_neb)) |
---|
[3999] | 1056 | |
---|
| 1057 | ENDIF |
---|
| 1058 | |
---|
[4226] | 1059 | ENDDO |
---|
| 1060 | |
---|
[3999] | 1061 | ! Scavenging through impaction in the underlying layer |
---|
| 1062 | |
---|
| 1063 | DO kk = k-1, 1, -1 |
---|
| 1064 | |
---|
| 1065 | DO i = 1, klon |
---|
| 1066 | |
---|
| 1067 | IF (rneb(i,k).GT.0.0.AND.zprec_cond(i).GT.0.) THEN |
---|
| 1068 | |
---|
[4654] | 1069 | IF (temp(i,kk) .GE. t_glace_min) THEN |
---|
[3999] | 1070 | zalpha_tr = a_tr_sca(1) |
---|
| 1071 | ELSE |
---|
| 1072 | zalpha_tr = a_tr_sca(2) |
---|
| 1073 | ENDIF |
---|
| 1074 | |
---|
[5450] | 1075 | zfrac_lessi = 1. - EXP(zalpha_tr*zprec_cond(i)/MAX(rneb(i,k),seuil_neb)) |
---|
| 1076 | frac_impa(i,kk)= 1.-MAX(rneb(i,k),seuil_neb)*zfrac_lessi |
---|
[3999] | 1077 | |
---|
| 1078 | ENDIF |
---|
| 1079 | |
---|
| 1080 | ENDDO |
---|
| 1081 | |
---|
| 1082 | ENDDO |
---|
[5406] | 1083 | |
---|
| 1084 | !------------------------------------------------------------ |
---|
[5408] | 1085 | ! P6 > write diagnostics and outputs |
---|
[5406] | 1086 | !------------------------------------------------------------ |
---|
| 1087 | |
---|
| 1088 | !--AB Write diagnostics and tracers for ice supersaturation |
---|
[5601] | 1089 | IF ( ok_plane_contrail ) THEN |
---|
| 1090 | cfa_seri(:,k) = contfra(:) |
---|
| 1091 | qta_seri(:,k) = qcont(:) |
---|
| 1092 | qice_cont(:,k) = qcont(:) - zqs(:) * contfra(:) |
---|
| 1093 | ENDIF |
---|
| 1094 | |
---|
| 1095 | IF ( ok_ice_supersat .AND. .NOT. ok_unadjusted_clouds) qvc(:) = zqs(:) * rneb(:,k) |
---|
| 1096 | |
---|
[5406] | 1097 | IF ( ok_ice_supersat ) THEN |
---|
| 1098 | CALL calc_qsat_ecmwf(klon,zt,qzero,pplay(:,k),RTT,1,.false.,qsatl(:,k),zdqs) |
---|
| 1099 | CALL calc_qsat_ecmwf(klon,zt,qzero,pplay(:,k),RTT,2,.false.,qsati(:,k),zdqs) |
---|
[4226] | 1100 | |
---|
[5406] | 1101 | DO i = 1, klon |
---|
| 1102 | |
---|
[5545] | 1103 | cf_seri(i,k) = rneb(i,k) |
---|
| 1104 | |
---|
[5406] | 1105 | IF ( zoliq(i) .LE. 0. ) THEN |
---|
| 1106 | !--If everything was precipitated, the remaining empty cloud is dissipated |
---|
| 1107 | !--and everything is transfered to the subsaturated clear sky region |
---|
[5545] | 1108 | !--NB. we do not change rneb, as it is a diagnostic only |
---|
| 1109 | cf_seri(i,k) = 0. |
---|
[5406] | 1110 | qvc(i) = 0. |
---|
| 1111 | ENDIF |
---|
| 1112 | |
---|
[5601] | 1113 | qvc_seri(i,k) = qvc(i) |
---|
[5406] | 1114 | |
---|
| 1115 | !--Diagnostics |
---|
| 1116 | gamma_cond(i,k) = gammasat(i) |
---|
| 1117 | subfra(i,k) = 1. - cf_seri(i,k) - issrfra(i,k) |
---|
| 1118 | qsub(i,k) = zq(i) - qvc(i) - qissr(i,k) |
---|
[5412] | 1119 | qcld(i,k) = qvc(i) + zoliq(i) |
---|
[5575] | 1120 | |
---|
| 1121 | !--Calculation of the ice supersaturated fraction following Lamquin et al (2012) |
---|
| 1122 | !--methodology: in each layer, we make a maximum random overlap assumption for |
---|
| 1123 | !--ice supersaturation |
---|
| 1124 | IF ( ( paprs(i,k) .GT. 10000. ) .AND. ( paprs(i,k) .LE. 15000. ) ) THEN |
---|
| 1125 | IF ( issrfra100to150UP(i) .GT. ( 1. - eps ) ) THEN |
---|
| 1126 | issrfra100to150(i) = 1. |
---|
| 1127 | ELSE |
---|
| 1128 | issrfra100to150(i) = 1. - ( 1. - issrfra100to150(i) ) * & |
---|
| 1129 | ( 1. - MAX( issrfra(i,k), issrfra100to150UP(i) ) ) & |
---|
| 1130 | / ( 1. - issrfra100to150UP(i) ) |
---|
| 1131 | issrfra100to150UP(i) = issrfra(i,k) |
---|
| 1132 | ENDIF |
---|
| 1133 | ELSEIF ( ( paprs(i,k) .GT. 15000. ) .AND. ( paprs(i,k) .LE. 20000. ) ) THEN |
---|
| 1134 | IF ( issrfra150to200UP(i) .GT. ( 1. - eps ) ) THEN |
---|
| 1135 | issrfra150to200(i) = 1. |
---|
| 1136 | ELSE |
---|
| 1137 | issrfra150to200(i) = 1. - ( 1. - issrfra150to200(i) ) * & |
---|
| 1138 | ( 1. - MAX( issrfra(i,k), issrfra150to200UP(i) ) ) & |
---|
| 1139 | / ( 1. - issrfra150to200UP(i) ) |
---|
| 1140 | issrfra150to200UP(i) = issrfra(i,k) |
---|
| 1141 | ENDIF |
---|
| 1142 | ELSEIF ( ( paprs(i,k) .GT. 20000. ) .AND. ( paprs(i,k) .LE. 25000. ) ) THEN |
---|
| 1143 | IF ( issrfra200to250UP(i) .GT. ( 1. - eps ) ) THEN |
---|
| 1144 | issrfra200to250(i) = 1. |
---|
| 1145 | ELSE |
---|
| 1146 | issrfra200to250(i) = 1. - ( 1. - issrfra200to250(i) ) * & |
---|
| 1147 | ( 1. - MAX( issrfra(i,k), issrfra200to250UP(i) ) ) & |
---|
| 1148 | / ( 1. - issrfra200to250UP(i) ) |
---|
| 1149 | issrfra200to250UP(i) = issrfra(i,k) |
---|
| 1150 | ENDIF |
---|
| 1151 | ELSEIF ( ( paprs(i,k) .GT. 25000. ) .AND. ( paprs(i,k) .LE. 30000. ) ) THEN |
---|
| 1152 | IF ( issrfra250to300UP(i) .GT. ( 1. - eps ) ) THEN |
---|
| 1153 | issrfra250to300(i) = 1. |
---|
| 1154 | ELSE |
---|
| 1155 | issrfra250to300(i) = 1. - ( 1. - issrfra250to300(i) ) * & |
---|
| 1156 | ( 1. - MAX( issrfra(i,k), issrfra250to300UP(i) ) ) & |
---|
| 1157 | / ( 1. - issrfra250to300UP(i) ) |
---|
| 1158 | issrfra250to300UP(i) = issrfra(i,k) |
---|
| 1159 | ENDIF |
---|
| 1160 | ELSEIF ( ( paprs(i,k) .GT. 30000. ) .AND. ( paprs(i,k) .LE. 40000. ) ) THEN |
---|
| 1161 | IF ( issrfra300to400UP(i) .GT. ( 1. - eps ) ) THEN |
---|
| 1162 | issrfra300to400(i) = 1. |
---|
| 1163 | ELSE |
---|
| 1164 | issrfra300to400(i) = 1. - ( 1. - issrfra300to400(i) ) * & |
---|
| 1165 | ( 1. - MAX( issrfra(i,k), issrfra300to400UP(i) ) ) & |
---|
| 1166 | / ( 1. - issrfra300to400UP(i) ) |
---|
| 1167 | issrfra300to400UP(i) = issrfra(i,k) |
---|
| 1168 | ENDIF |
---|
| 1169 | ELSEIF ( ( paprs(i,k) .GT. 40000. ) .AND. ( paprs(i,k) .LE. 50000. ) ) THEN |
---|
| 1170 | IF ( issrfra400to500UP(i) .GT. ( 1. - eps ) ) THEN |
---|
| 1171 | issrfra400to500(i) = 1. |
---|
| 1172 | ELSE |
---|
| 1173 | issrfra400to500(i) = 1. - ( 1. - issrfra400to500(i) ) * & |
---|
| 1174 | ( 1. - MAX( issrfra(i,k), issrfra400to500UP(i) ) ) & |
---|
| 1175 | / ( 1. - issrfra400to500UP(i) ) |
---|
| 1176 | issrfra400to500UP(i) = issrfra(i,k) |
---|
| 1177 | ENDIF |
---|
| 1178 | ENDIF |
---|
| 1179 | |
---|
[5406] | 1180 | ENDDO |
---|
| 1181 | ENDIF |
---|
| 1182 | |
---|
[4803] | 1183 | ! Outputs: |
---|
| 1184 | !------------------------------- |
---|
| 1185 | ! Precipitation fluxes at layer interfaces |
---|
| 1186 | ! + precipitation fractions + |
---|
| 1187 | ! temperature and water species tendencies |
---|
| 1188 | DO i = 1, klon |
---|
| 1189 | psfl(i,k)=zifl(i) |
---|
| 1190 | prfl(i,k)=zrfl(i) |
---|
| 1191 | pfraclr(i,k)=znebprecipclr(i) |
---|
| 1192 | pfracld(i,k)=znebprecipcld(i) |
---|
| 1193 | d_q(i,k) = zq(i) - qt(i,k) |
---|
| 1194 | d_t(i,k) = zt(i) - temp(i,k) |
---|
[5412] | 1195 | |
---|
| 1196 | IF (ok_bug_phase_lscp) THEN |
---|
| 1197 | d_ql(i,k) = (1-zfice(i))*zoliq(i) |
---|
| 1198 | d_qi(i,k) = zfice(i)*zoliq(i) |
---|
| 1199 | ELSE |
---|
| 1200 | d_ql(i,k) = zoliql(i) |
---|
| 1201 | d_qi(i,k) = zoliqi(i) |
---|
| 1202 | ENDIF |
---|
| 1203 | |
---|
[4803] | 1204 | ENDDO |
---|
| 1205 | |
---|
| 1206 | |
---|
[5413] | 1207 | ENDDO ! loop on k from top to bottom |
---|
[4059] | 1208 | |
---|
[3999] | 1209 | |
---|
| 1210 | ! Rain or snow at the surface (depending on the first layer temperature) |
---|
| 1211 | DO i = 1, klon |
---|
| 1212 | snow(i) = zifl(i) |
---|
| 1213 | rain(i) = zrfl(i) |
---|
[4392] | 1214 | ! c_iso final output |
---|
[3999] | 1215 | ENDDO |
---|
| 1216 | |
---|
| 1217 | IF (ncoreczq>0) THEN |
---|
| 1218 | WRITE(lunout,*)'WARNING : ZQ in LSCP ',ncoreczq,' val < 1.e-15.' |
---|
| 1219 | ENDIF |
---|
| 1220 | |
---|
[4654] | 1221 | |
---|
| 1222 | RETURN |
---|
| 1223 | |
---|
[4380] | 1224 | END SUBROUTINE lscp |
---|
[3999] | 1225 | !+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++ |
---|
| 1226 | |
---|
[4664] | 1227 | END MODULE lmdz_lscp |
---|