| 1 | SUBROUTINE callradite(icount,ngrid,nlayer,nq,zday,ls,pq,albedo, |
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| 2 | $ emis,mu0,pplev,pplay,pt,tsurf,fract,dist_sol,igout, |
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| 3 | $ dtlw,dtsw,fluxsurf_lw,fluxsurf_sw,fluxtop_lw,fluxtop_sw, |
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| 4 | & tauref,tau,aerosol,dsodust,tauscaling,taucloudtes,rdust,rice, |
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| 5 | & nuice,co2ice) |
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| 6 | |
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| 7 | use dimradmars_mod, only: ndomainsz, nflev, nsun, nir |
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| 8 | use dimradmars_mod, only: naerkind, name_iaer, |
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| 9 | & iaer_dust_conrath,iaer_dust_doubleq, |
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| 10 | & iaer_dust_submicron,iaer_h2o_ice |
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| 11 | use yomlw_h, only: gcp, nlaylte |
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| 12 | use comcstfi_h, only: g,cpp |
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| 13 | use time_phylmdz_mod, only: daysec |
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| 14 | IMPLICIT NONE |
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| 15 | c======================================================================= |
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| 16 | c subject: |
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| 17 | c -------- |
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| 18 | c Subroutine designed to call the main canonic |
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| 19 | c radiative transfer subroutine "lwmain" et "swmain" |
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| 20 | c to compute radiative heating and cooling rate and |
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| 21 | c radiative fluxes to the surface. |
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| 22 | c |
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| 23 | c These calculations are only valid on the part of the atmosphere |
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| 24 | c where Local Thermal Equilibrium (NLTE) is verified. In practice |
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| 25 | c The calculations are only performed for the first "nlaylte" |
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| 26 | c parameters (nlaylte is calculated by subroutine "nlthermeq" |
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| 27 | c and stored in module "yomlw_h"). |
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| 28 | c |
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| 29 | c The purpose of this subroutine is to: |
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| 30 | c 1) Make some initial calculation at first call |
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| 31 | c 2) Split the calculation in several sub-grid |
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| 32 | c ("sub-domain") to save memory and |
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| 33 | c be able run on a workstation at high resolution |
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| 34 | c The sub-grid size is defined in dimradmars_mod |
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| 35 | c 3) Compute the 3D scattering parameters depending on the |
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| 36 | c size distribution of the different tracers (added by JBM) |
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| 37 | c 4) call "lwmain" and "swmain" |
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| 38 | c |
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| 39 | c |
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| 40 | c authors: |
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| 41 | c ------ |
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| 42 | c Francois Forget / Christophe Hourdin / J.-B. Madeleine (2009) |
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| 43 | c |
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| 44 | c |
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| 45 | c 3D scattering scheme user's guide (J.-B. Madeleine) |
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| 46 | c --------------------------------- |
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| 47 | c |
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| 48 | c This routine has been modified to take into account 3D, time |
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| 49 | c dependent scattering properties of the aerosols. |
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| 50 | c---- The look-up tables that contain the scattering parameters |
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| 51 | c of a given tracer, for different sizes, are read by SUAER.F90. |
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| 52 | c The names of the corresponding ASCII files have to be set in |
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| 53 | c this subroutine (file_id variable), and files must be in the |
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| 54 | c directory specified in datafile.h. Please make sure that the |
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| 55 | c ASCII files are correctly written, and that the range |
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| 56 | c of particle sizes is consistent with what you would expect. |
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| 57 | c---- SUAER.F90 is in charge of reading the ASCII files and averaging |
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| 58 | c the scattering parameters in each GCM channel, using the three last |
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| 59 | c equations of Forget et al. 1998 (GRL 25, No.7, p.1105-1108). |
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| 60 | c---- These look-up tables, loaded during the firstcall, are then |
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| 61 | c constantly used by the subroutine "aeroptproperties.F" to compute, |
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| 62 | c online, the 3D scattering parameters, based on the size distribution |
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| 63 | c (reffrad and nueffrad) of the different tracers, in each grid box. |
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| 64 | c These 3D size distributions are loaded by the "updatereffrad.F" |
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| 65 | c subroutine. A log-normal distribution is then assumed in |
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| 66 | c "aeroptproperties.F", along with a Gauss-Legendre integration. |
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| 67 | c---- The optical depth at the visible reference wavelength (set in |
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| 68 | c SUAER.F90, after the file_id variable) is then computed by |
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| 69 | c the subroutine "aeropacity.F", by using the size and spatial |
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| 70 | c distribution of the corresponding tracer. This connection has to |
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| 71 | c be implemented in "aeropacity.F" when adding a new tracer. To do so, |
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| 72 | c one can use equation 2 of Forget et al. 1998 (Icarus 131, p.302-316). |
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| 73 | c---- The resulting variables "aerosol", "QVISsQREF3d", "omegaVIS3d" and |
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| 74 | c "gVIS3d" (same in the infrared) are finally used by lwmain.F and |
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| 75 | c swmain.F to solve the radiative transfer equation. |
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| 76 | c |
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| 77 | c changes: |
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| 78 | c ------- |
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| 79 | c |
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| 80 | c > SRL 7/2000 |
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| 81 | c |
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| 82 | c This version has been modified to only calculate radiative tendencies |
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| 83 | c over layers 1..NFLEV (set in dimradmars_mod). Returns zero for higher |
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| 84 | c layers, if any. |
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| 85 | c In other routines, nlayer -> nflev. |
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| 86 | c Routines affected: lwflux, lwi, lwmain, lwxb, lwxd, lwxn. |
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| 87 | c |
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| 88 | c > J.-B. Madeleine 10W12 |
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| 89 | c This version uses the variable's splitting, which can be usefull |
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| 90 | c when performing very high resolution simulation like LES. |
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| 91 | c |
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| 92 | c ---------- |
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| 93 | c Here, solar band#1 is spectral interval between "long1vis" and "long2vis" |
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| 94 | c set in dimradmars_mod |
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| 95 | c Here, solar band#2 is spectral interval between "long2vis" and "long3vis" |
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| 96 | c set in dimradmars_mod |
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| 97 | c |
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| 98 | c input: |
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| 99 | c ----- |
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| 100 | c icount counter of call to subroutine physic by gcm |
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| 101 | c ngrid number of gridpoint of horizontal grid |
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| 102 | c nlayer Number of layer |
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| 103 | c nq Number of tracer |
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| 104 | c ls Solar longitude (Ls) , radian |
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| 105 | c zday Date (time since Ls=0, in martian days) |
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| 106 | c pq(ngrid,nlayer,nq) Advected fields |
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| 107 | c |
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| 108 | c albedo (ngrid,2) hemispheric surface albedo |
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| 109 | c albedo (i,1) : mean albedo for solar band#1 |
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| 110 | c (see below) |
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| 111 | c albedo (i,2) : mean albedo for solar band#2 |
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| 112 | c (see below) |
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| 113 | c emis Thermal IR surface emissivity (no unit) |
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| 114 | c mu0(ngrid) cos of solar zenith angle |
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| 115 | c (=1 when sun at zenith) |
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| 116 | c pplay(ngrid,nlayer) pressure (Pa) in the middle of each layer |
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| 117 | c pplev(ngrid,nlayer+1) pressure (Pa) at boundaries of each layer |
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| 118 | c pt(ngrid,nlayer) atmospheric temperature in each layer (K) |
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| 119 | c tsurf(ngrid) surface temperature (K) |
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| 120 | c fract(ngrid) day fraction of the time interval |
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| 121 | c =1 during the full day ; =0 during the night |
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| 122 | c declin latitude of subsolar point |
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| 123 | c dist_sol sun-Mars distance (AU) |
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| 124 | c igout coordinate of analysed point for debugging |
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| 125 | c reffrad(ngrid,nlayer,naerkind) Aerosol effective radius |
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| 126 | c nueffrad(ngrid,nlayer,naerkind) Aerosol effective variance |
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| 127 | |
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| 128 | c |
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| 129 | c output: |
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| 130 | c ------- |
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| 131 | c dtlw (ngrid,nlayer) longwave (IR) heating rate (K/s) |
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| 132 | c dtsw(ngrid,nlayer) shortwave (Solar) heating rate (K/s) |
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| 133 | c fluxsurf_lw(ngrid) surface downward flux tota LW (thermal IR) (W.m-2) |
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| 134 | c fluxsurf_sw(ngrid,1) surface downward flux SW for solar band#1 (W.m-2) |
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| 135 | c fluxsurf_sw(ngrid,2) surface downward flux SW for solar band#2 (W.m-2) |
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| 136 | c |
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| 137 | c fluxtop_lw(ngrid) outgoing upward flux tota LW (thermal IR) (W.m-2) |
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| 138 | c fluxtop_sw(ngrid,1) outgoing upward flux SW for solar band#1 (W.m-2) |
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| 139 | c fluxtop_sw(ngrid,2) outgoing upward flux SW for solar band#2 (W.m-2) |
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| 140 | |
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| 141 | c tauref Prescribed mean column optical depth at 610 Pa |
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| 142 | c tau Column total visible dust optical depth at each point |
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| 143 | c aerosol(ngrid,nlayer,naerkind) aerosol extinction optical depth |
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| 144 | c at reference wavelength "longrefvis" set |
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| 145 | c in dimradmars_h , in each layer, for one of |
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| 146 | c the "naerkind" kind of aerosol optical |
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| 147 | c properties. |
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| 148 | |
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| 149 | c======================================================================= |
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| 150 | c |
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| 151 | c Declarations : |
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| 152 | c ------------- |
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| 153 | c |
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| 154 | #include "callkeys.h" |
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| 155 | |
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| 156 | c----------------------------------------------------------------------- |
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| 157 | c Input/Output |
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| 158 | c ------------ |
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| 159 | INTEGER,INTENT(IN) :: icount |
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| 160 | INTEGER,INTENT(IN) :: ngrid,nlayer,nq |
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| 161 | INTEGER,INTENT(IN) :: igout |
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| 162 | |
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| 163 | REAL,INTENT(IN) :: pq(ngrid,nlayer,nq) |
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| 164 | REAL,INTENT(IN) :: tauscaling(ngrid) ! Conversion factor for |
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| 165 | ! qdust and Ndust |
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| 166 | REAL,INTENT(IN) :: albedo(ngrid,2),emis(ngrid) |
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| 167 | REAL,INTENT(IN) :: ls,zday |
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| 168 | |
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| 169 | REAL,INTENT(IN) :: pplev(ngrid,nlayer+1),pplay(ngrid,nlayer) |
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| 170 | REAL,INTENT(IN) :: pt(ngrid,nlayer) |
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| 171 | REAL,INTENT(IN) :: tsurf(ngrid) |
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| 172 | REAL,INTENT(IN) :: dist_sol,mu0(ngrid),fract(ngrid) |
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| 173 | REAL,INTENT(OUT) :: dtlw(ngrid,nlayer),dtsw(ngrid,nlayer) |
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| 174 | REAL,INTENT(OUT) :: fluxsurf_lw(ngrid), fluxtop_lw(ngrid) |
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| 175 | REAL,INTENT(OUT) :: fluxsurf_sw(ngrid,2), fluxtop_sw(ngrid,2) |
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| 176 | |
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| 177 | REAL,INTENT(OUT) :: tauref(ngrid), tau(ngrid,naerkind) |
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| 178 | REAL,INTENT(OUT) :: taucloudtes(ngrid)! Cloud opacity at infrared |
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| 179 | ! reference wavelength using |
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| 180 | ! Qabs instead of Qext |
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| 181 | ! (direct comparison with TES) |
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| 182 | REAL,INTENT(OUT) :: aerosol(ngrid,nlayer,naerkind) |
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| 183 | REAL,INTENT(OUT) :: dsodust(ngrid,nlayer) |
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| 184 | REAL,INTENT(OUT) :: rdust(ngrid,nlayer) ! Dust geometric mean radius (m) |
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| 185 | REAL,INTENT(OUT) :: rice(ngrid,nlayer) ! Ice geometric mean radius (m) |
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| 186 | REAL,INTENT(OUT) :: nuice(ngrid,nlayer) ! Estimated effective variance |
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| 187 | REAL,INTENT(IN) :: co2ice(ngrid) ! co2 ice surface layer (kg.m-2) |
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| 188 | |
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| 189 | c |
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| 190 | c Local variables : |
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| 191 | c ----------------- |
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| 192 | |
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| 193 | INTEGER j,l,ig,n,ich |
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| 194 | INTEGER aer_count,iaer |
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| 195 | INTEGER jd,ig0,nd |
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| 196 | |
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| 197 | real cste_mars ! solar constant on Mars (Wm-2) |
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| 198 | REAL ptlev(ngrid,nlayer+1) |
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| 199 | |
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| 200 | INTEGER,SAVE :: ndomain |
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| 201 | |
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| 202 | c Thermal IR net radiative budget (W m-2) |
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| 203 | |
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| 204 | real znetrad(ndomainsz,nflev) |
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| 205 | |
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| 206 | real zfluxd_sw(ndomainsz,nflev+1,2) |
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| 207 | real zfluxu_sw(ndomainsz,nflev+1,2) |
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| 208 | |
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| 209 | REAL zplev(ndomainsz,nflev+1) |
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| 210 | REAL zztlev(ndomainsz,nflev+1) |
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| 211 | REAL zplay(ndomainsz,nflev) |
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| 212 | REAL zt(ndomainsz,nflev) |
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| 213 | REAL zaerosol(ndomainsz,nflev,naerkind) |
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| 214 | REAL zalbedo(ndomainsz,2) |
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| 215 | REAL zdp(ndomainsz,nflev) |
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| 216 | REAL zdt0(ndomainsz) |
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| 217 | |
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| 218 | REAL zzdtlw(ndomainsz,nflev) |
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| 219 | REAL zzdtsw(ndomainsz,nflev) |
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| 220 | REAL zzflux(ndomainsz,6) |
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| 221 | real zrmuz |
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| 222 | |
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| 223 | REAL :: zQVISsQREF3d(ndomainsz,nflev,nsun,naerkind) |
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| 224 | REAL :: zomegaVIS3d(ndomainsz,nflev,nsun,naerkind) |
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| 225 | REAL :: zgVIS3d(ndomainsz,nflev,nsun,naerkind) |
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| 226 | |
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| 227 | REAL :: zQIRsQREF3d(ndomainsz,nflev,nir,naerkind) |
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| 228 | REAL :: zomegaIR3d(ndomainsz,nflev,nir,naerkind) |
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| 229 | REAL :: zgIR3d(ndomainsz,nflev,nir,naerkind) |
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| 230 | |
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| 231 | c Aerosol size distribution |
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| 232 | REAL :: reffrad(ngrid,nlayer,naerkind) |
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| 233 | REAL :: nueffrad(ngrid,nlayer,naerkind) |
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| 234 | c Aerosol optical properties |
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| 235 | REAL :: QVISsQREF3d(ngrid,nlayer,nsun,naerkind) |
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| 236 | REAL :: omegaVIS3d(ngrid,nlayer,nsun,naerkind) |
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| 237 | REAL :: gVIS3d(ngrid,nlayer,nsun,naerkind) |
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| 238 | |
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| 239 | REAL :: QIRsQREF3d(ngrid,nlayer,nir,naerkind) |
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| 240 | REAL :: omegaIR3d(ngrid,nlayer,nir,naerkind) |
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| 241 | REAL :: gIR3d(ngrid,nlayer,nir,naerkind) |
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| 242 | |
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| 243 | REAL :: QREFvis3d(ngrid,nlayer,naerkind) |
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| 244 | REAL :: QREFir3d(ngrid,nlayer,naerkind) |
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| 245 | |
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| 246 | REAL :: omegaREFvis3d(ngrid,nlayer,naerkind) |
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| 247 | REAL :: omegaREFir3d(ngrid,nlayer,naerkind) |
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| 248 | |
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| 249 | c local saved variables |
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| 250 | c --------------------- |
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| 251 | |
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| 252 | real,save,allocatable :: pview(:) |
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| 253 | |
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| 254 | real zco2 ! volume fraction of CO2 in Mars atmosphere |
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| 255 | DATA zco2/0.95/ |
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| 256 | SAVE zco2 |
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| 257 | |
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| 258 | LOGICAL firstcall |
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| 259 | DATA firstcall/.true./ |
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| 260 | SAVE firstcall |
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| 261 | |
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| 262 | c---------------------------------------------------------------------- |
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| 263 | |
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| 264 | c Initialisation |
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| 265 | c -------------- |
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| 266 | |
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| 267 | IF (firstcall) THEN |
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| 268 | ! compute ndomain and allocate local saved arrays |
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| 269 | ndomain= (ngrid-1) / ndomainsz + 1 |
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| 270 | allocate(pview(ngrid)) |
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| 271 | |
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| 272 | c Assign a number to the different scatterers |
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| 273 | c ------------------------------------------- |
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| 274 | |
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| 275 | iaer_dust_conrath=0 |
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| 276 | iaer_dust_doubleq=0 |
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| 277 | iaer_dust_submicron=0 |
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| 278 | iaer_h2o_ice=0 |
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| 279 | |
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| 280 | aer_count=0 |
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| 281 | if (.NOT.active) then |
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| 282 | do iaer=1,naerkind |
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| 283 | if (name_iaer(iaer).eq."dust_conrath") then |
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| 284 | iaer_dust_conrath = iaer |
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| 285 | aer_count = aer_count + 1 |
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| 286 | endif |
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| 287 | enddo |
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| 288 | endif |
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| 289 | if (doubleq.AND.active) then |
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| 290 | do iaer=1,naerkind |
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| 291 | if (name_iaer(iaer).eq."dust_doubleq") then |
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| 292 | iaer_dust_doubleq = iaer |
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| 293 | aer_count = aer_count + 1 |
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| 294 | endif |
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| 295 | enddo |
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| 296 | endif |
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| 297 | if (submicron.AND.active) then |
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| 298 | do iaer=1,naerkind |
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| 299 | if (name_iaer(iaer).eq."dust_submicron") then |
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| 300 | iaer_dust_submicron = iaer |
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| 301 | aer_count = aer_count + 1 |
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| 302 | endif |
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| 303 | enddo |
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| 304 | endif |
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| 305 | if (water.AND.activice) then |
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| 306 | do iaer=1,naerkind |
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| 307 | if (name_iaer(iaer).eq."h2o_ice") then |
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| 308 | iaer_h2o_ice = iaer |
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| 309 | aer_count = aer_count + 1 |
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| 310 | endif |
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| 311 | enddo |
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| 312 | endif |
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| 313 | |
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| 314 | c Check that we identified all tracers: |
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| 315 | if (aer_count.ne.naerkind) then |
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| 316 | write(*,*) "callradite: found only ",aer_count," scatterers" |
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| 317 | write(*,*) " expected ",naerkind |
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| 318 | write(*,*) "please make sure that the number of" |
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| 319 | write(*,*) "scatterers in scatterers.h, the names" |
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| 320 | write(*,*) "in callradite.F, and the flags in" |
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| 321 | write(*,*) "callphys.def are all consistent!" |
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| 322 | do iaer=1,naerkind |
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| 323 | write(*,*)' ',iaer,' ',trim(name_iaer(iaer)) |
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| 324 | enddo |
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| 325 | stop |
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| 326 | else |
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| 327 | write(*,*) "callradite: found all scatterers, namely:" |
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| 328 | do iaer=1,naerkind |
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| 329 | write(*,*)' ',iaer,' ',trim(name_iaer(iaer)) |
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| 330 | enddo |
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| 331 | endif |
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| 332 | c ------------------------------------------- |
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| 333 | |
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| 334 | DO ig=1,ngrid |
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| 335 | pview(ig)=1.66 ! cosecant of viewing angle |
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| 336 | ENDDO |
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| 337 | gcp = g/cpp |
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| 338 | |
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| 339 | c Loading the optical properties in external look-up tables: |
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| 340 | CALL SUAER |
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| 341 | ! CALL SULW ! this step is now done in ini_yomlw_h |
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| 342 | |
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| 343 | write(*,*) 'Splitting radiative calculations: ', |
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| 344 | $ ' ngrid,ndomainsz,ndomain', |
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| 345 | $ ngrid,ndomainsz,ndomain |
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| 346 | if (ngrid .EQ. 1) then |
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| 347 | if (ndomainsz .NE. 1) then |
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| 348 | print* |
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| 349 | print*,'ATTENTION !!!' |
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| 350 | print*,'pour tourner en 1D, ' |
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| 351 | print*,'fixer ndomainsz=1 dans phymars/dimradmars_h' |
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| 352 | print* |
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| 353 | call exit(1) |
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| 354 | endif |
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| 355 | endif |
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| 356 | firstcall=.false. |
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| 357 | END IF |
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| 358 | |
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| 359 | c Computing aerosol optical properties and opacity |
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| 360 | c ------------------------------------------------ |
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| 361 | |
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| 362 | c Updating aerosol size distributions: |
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| 363 | CALL updatereffrad(ngrid,nlayer, |
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| 364 | & rdust,rice,nuice, |
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| 365 | & reffrad,nueffrad, |
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| 366 | & pq,tauscaling,tau,pplay) |
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| 367 | |
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| 368 | c Computing 3D scattering parameters: |
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| 369 | CALL aeroptproperties(ngrid,nlayer,reffrad,nueffrad, |
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| 370 | & QVISsQREF3d,omegaVIS3d,gVIS3d, |
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| 371 | & QIRsQREF3d,omegaIR3d,gIR3d, |
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| 372 | & QREFvis3d,QREFir3d, |
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| 373 | & omegaREFvis3d,omegaREFir3d) |
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| 374 | |
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| 375 | c Computing aerosol optical depth in each layer: |
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| 376 | CALL aeropacity(ngrid,nlayer,nq,zday,pplay,pplev,ls, |
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| 377 | & pq,tauscaling,tauref,tau,taucloudtes,aerosol,dsodust,reffrad, |
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| 378 | & nueffrad,QREFvis3d,QREFir3d,omegaREFvis3d,omegaREFir3d) |
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| 379 | |
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| 380 | c Starting loop on sub-domain |
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| 381 | c ---------------------------- |
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| 382 | |
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| 383 | DO jd=1,ndomain |
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| 384 | ig0=(jd-1)*ndomainsz |
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| 385 | if (jd.eq.ndomain) then |
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| 386 | nd=ngrid-ig0 |
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| 387 | else |
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| 388 | nd=ndomainsz |
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| 389 | endif |
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| 390 | |
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| 391 | c Spliting input variable in sub-domain input variables |
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| 392 | c --------------------------------------------------- |
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| 393 | |
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| 394 | do l=1,nlaylte |
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| 395 | do ig = 1,nd |
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| 396 | do iaer = 1, naerkind |
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| 397 | do ich = 1, nsun |
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| 398 | zQVISsQREF3d(ig,l,ich,iaer) = |
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| 399 | & QVISsQREF3d(ig0+ig,l,ich,iaer) |
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| 400 | zomegaVIS3d(ig,l,ich,iaer) = |
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| 401 | & omegaVIS3d(ig0+ig,l,ich,iaer) |
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| 402 | zgVIS3d(ig,l,ich,iaer) = |
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| 403 | & gVIS3d(ig0+ig,l,ich,iaer) |
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| 404 | enddo |
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| 405 | do ich = 1, nir |
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| 406 | zQIRsQREF3d(ig,l,ich,iaer) = |
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| 407 | & QIRsQREF3d(ig0+ig,l,ich,iaer) |
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| 408 | zomegaIR3d(ig,l,ich,iaer) = |
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| 409 | & omegaIR3d(ig0+ig,l,ich,iaer) |
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| 410 | zgIR3d(ig,l,ich,iaer) = |
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| 411 | & gIR3d(ig0+ig,l,ich,iaer) |
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| 412 | enddo |
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| 413 | enddo |
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| 414 | enddo |
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| 415 | enddo |
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| 416 | |
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| 417 | do l=1,nlaylte+1 |
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| 418 | do ig = 1,nd |
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| 419 | zplev(ig,l) = pplev(ig0+ig,l) |
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| 420 | enddo |
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| 421 | enddo |
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| 422 | |
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| 423 | do l=1,nlaylte |
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| 424 | do ig = 1,nd |
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| 425 | zplay(ig,l) = pplay(ig0+ig,l) |
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| 426 | zt(ig,l) = pt(ig0+ig,l) |
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| 427 | c Thickness of each layer (Pa) : |
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| 428 | zdp(ig,l)= pplev(ig0+ig,l) - pplev(ig0+ig,l+1) |
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| 429 | enddo |
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| 430 | enddo |
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| 431 | |
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| 432 | do n=1,naerkind |
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| 433 | do l=1,nlaylte |
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| 434 | do ig=1,nd |
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| 435 | zaerosol(ig,l,n) = aerosol(ig0+ig,l,n) |
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| 436 | enddo |
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| 437 | enddo |
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| 438 | enddo |
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| 439 | |
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| 440 | do j=1,2 |
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| 441 | do ig = 1,nd |
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| 442 | zalbedo(ig,j) = albedo(ig0+ig,j) |
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| 443 | enddo |
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| 444 | enddo |
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| 445 | |
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| 446 | c Intermediate levels: (computing tlev) |
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| 447 | c --------------------------------------- |
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| 448 | c Extrapolation for the air temperature above the surface |
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| 449 | DO ig=1,nd |
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| 450 | zztlev(ig,1)=zt(ig,1)+ |
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| 451 | s (zplev(ig,1)-zplay(ig,1))* |
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| 452 | s (zt(ig,1)-zt(ig,2))/(zplay(ig,1)-zplay(ig,2)) |
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| 453 | |
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| 454 | zdt0(ig) = tsurf(ig0+ig) - zztlev(ig,1) |
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| 455 | ENDDO |
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| 456 | |
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| 457 | DO l=2,nlaylte |
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| 458 | DO ig=1, nd |
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| 459 | zztlev(ig,l)=0.5*(zt(ig,l-1)+zt(ig,l)) |
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| 460 | ENDDO |
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| 461 | ENDDO |
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| 462 | |
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| 463 | DO ig=1, nd |
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| 464 | zztlev(ig,nlaylte+1)=zt(ig,nlaylte) |
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| 465 | ENDDO |
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| 466 | |
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| 467 | |
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| 468 | c Longwave ("lw") radiative transfer (= thermal infrared) |
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| 469 | c ------------------------------------------------------- |
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| 470 | call lwmain (ig0,icount,nd,nflev |
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| 471 | . ,zdp,zdt0,emis(ig0+1),zplev,zztlev,zt |
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| 472 | . ,zaerosol,zzdtlw |
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| 473 | . ,fluxsurf_lw(ig0+1),fluxtop_lw(ig0+1) |
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| 474 | . ,znetrad |
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| 475 | & ,zQIRsQREF3d,zomegaIR3d,zgIR3d |
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| 476 | & ,co2ice(ig0+1)) |
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| 477 | |
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| 478 | c Shortwave ("sw") radiative transfer (= solar radiation) |
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| 479 | c ------------------------------------------------------- |
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| 480 | c Mars solar constant (W m-2) |
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| 481 | c 1370 W.m-2 is the solar constant at 1 AU. |
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| 482 | cste_mars=1370./(dist_sol*dist_sol) |
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| 483 | |
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| 484 | call swmain ( nd, nflev, |
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| 485 | S cste_mars, zalbedo, |
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| 486 | S mu0(ig0+1), zdp, zplev, zaerosol, fract(ig0+1), |
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| 487 | S zzdtsw, zfluxd_sw, zfluxu_sw, |
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| 488 | & zQVISsQREF3d,zomegaVIS3d,zgVIS3d) |
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| 489 | |
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| 490 | c ------------------------------------------------------------ |
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| 491 | c Un-spliting output variable from sub-domain input variables |
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| 492 | c ------------------------------------------------------------ |
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| 493 | |
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| 494 | do l=1,nlaylte |
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| 495 | do ig = 1,nd |
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| 496 | dtlw(ig0+ig,l) = zzdtlw(ig,l) |
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| 497 | dtsw(ig0+ig,l) = zzdtsw(ig,l) |
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| 498 | enddo |
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| 499 | enddo |
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| 500 | |
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| 501 | do l=1,nlaylte+1 |
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| 502 | do ig = 1,nd |
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| 503 | ptlev(ig0+ig,l) = zztlev(ig,l) |
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| 504 | enddo |
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| 505 | enddo |
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| 506 | |
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| 507 | do ig = 1,nd |
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| 508 | fluxsurf_sw(ig0+ig,1) = zfluxd_sw(ig,1,1) |
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| 509 | fluxsurf_sw(ig0+ig,2) = zfluxd_sw(ig,1,2) |
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| 510 | fluxtop_sw(ig0+ig,1) = zfluxu_sw(ig,nlaylte+1,1) |
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| 511 | fluxtop_sw(ig0+ig,2) = zfluxu_sw(ig,nlaylte+1,2) |
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| 512 | enddo |
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| 513 | |
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| 514 | ENDDO ! (boucle jd=1, ndomain) |
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| 515 | |
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| 516 | c Zero tendencies for any remaining layers between nlaylte and nlayer |
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| 517 | if (nlayer.gt.nlaylte) then |
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| 518 | do l = nlaylte+1, nlayer |
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| 519 | do ig = 1, ngrid |
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| 520 | dtlw(ig, l) = 0. |
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| 521 | dtsw(ig, l) = 0. |
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| 522 | enddo |
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| 523 | enddo |
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| 524 | endif |
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| 525 | |
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| 526 | c Output for debugging if lwrite=T |
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| 527 | c -------------------------------- |
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| 528 | c Write all nlayer layers, even though only nlaylte layers may have |
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| 529 | c non-zero tendencies. |
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| 530 | |
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| 531 | IF(lwrite) THEN |
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| 532 | PRINT*,'Diagnotique for the radiation' |
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| 533 | PRINT*,'albedo, emissiv, mu0,fract,fluxsurf_lw,fluxsurf_sw' |
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| 534 | PRINT*,albedo(igout,1),emis(igout),mu0(igout), |
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| 535 | s fract(igout), fluxsurf_lw(igout), |
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| 536 | $ fluxsurf_sw(igout,1)+fluxsurf_sw(igout,2) |
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| 537 | PRINT*,'Tlay Tlev Play Plev dT/dt SW dT/dt LW (K/s)' |
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| 538 | PRINT*,'daysec',daysec |
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| 539 | DO l=1,nlayer |
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| 540 | PRINT*,pt(igout,l),ptlev(igout,l), |
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| 541 | s pplay(igout,l),pplev(igout,l), |
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| 542 | s dtsw(igout,l),dtlw(igout,l) |
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| 543 | ENDDO |
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| 544 | ENDIF |
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| 545 | |
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| 546 | |
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| 547 | return |
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| 548 | end |
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