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! version 3; Last Modified: May 7, 2008.
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#if defined (DOC)
*
*
*revision
* v2_10 - Desgagne M. - removed MITH (not used)
* v3_02 - Plante A. - add key Schm_wload_L for water loading
* v3_03 - Pellerin P. - add key Schm_offline_L
* v3_31 - Tanguay M. - Add key Schm_settls_L
*
***comdeck schm.cdk
*
*______________________________________________________________________
* |
* VARIABLES ASSOCIATED WITH CONTROLLING SCHEMES USED IN THE MODEL |
* (set_schm) |
*______________________________________________________________________|
* | |
* NAME | DESCRIPTION |
*--------------------|-------------------------------------------------|
* Schm_adcub_L | .true.-> cubic interpolation for |
* | advection (RU,RV) -> (PHI) |
* | .false. linear interpolotion used instead |
* Schm_chems_L | .true. CHEMISTRY package is used in model run |
* | .false. No CHEMISTRY used |
* Schm_chems_S | Chemical scheme to use ('NIL' if none) |
* Schm_cptop_L | .true.-> model has a const. top pres. (B(1)=0) |
* Schm_difqp_L | .false.=> no diffusion on q' |
* | .true. => indirect diffusion on q' & direct |
* | diffusion on (dp/dpi-1) & (1+d)q' |
* Schm_hdlast_L | .true.-> physics before horizontal diffusion |
* Schm_hydro_L | .true. -> hydrostatic run |
* | .false.-> non-hydrostatic run |
* Schm_itcn | number of iterations for Crank-Nicholson |
* Schm_itnlh | number of iterations to solve non-linear |
* | Helmholtz problem |
* Schm_itraj | number of iterations to compute trjectories |
* Schm_modcn | frequency of Crank-Nicholson procedure |
* Schm_moist_L | .true.-> model has moisture |
* Schm_nith | number of vertical modes treated implicitely |
* Schm_nkbz_L | .true.-> not-a-knot bc for z-spline |
* | .false.-> natural bc for z-spline |
* Schm_nonhy_8 | 0 to 1: from hydrostatic to non-hydrostatic |
* Schm_offline_L | run without the dynamical kernel (GEM) |
* Schm_phyms_L | .true. PHYSICS package is used in model run |
* | .false. No PHYSICS used |
* Schm_psadj_L | .true.-> ps adjust is activated (at every time |
* | step, the integral of ps over the domain|
* | is restored to the value of the previous|
* | time step; afterward, q and s are re- |
* | computed;this can be done in |
* | hydrostatic mode only)|
* Schm_settls_L | .true. -> SETTLS option (Stable extrapolation |
* | for Two-Time level scheme by Hortal M)|
* Schm_sfix_L | .true.-> fix surface values to those of l_nk-1 |
* Schm_theoc_L | .true.-> theoretical case |
* Schm_wload_L | .true.-> Effet of water loading included |
* Schm_xwvt3 | type of extrapolation for wind calculation |
* | at time t-dt/2 (th): |
* | =0 => two time levels (t1, t2) |
* | =1 => two time levels (t1, t2) for u,v |
* | three time levels for vertical wind |
* | =2 => three time levels (t1, t2, t3) |
*----------------------------------------------------------------------
*
#endif
logical Schm_hydro_L, Schm_cptop_L, Schm_moist_L, Schm_nkbz_L ,
$ Schm_phyms_L, Schm_adcub_L, Schm_difqp_L, Schm_psadj_L,
$ Schm_hdlast_L,Schm_wload_L, Schm_pcsty_L, Schm_chems_L,
$ Schm_pheat_L, Schm_theoc_L ,Schm_sfix_L, Schm_offline_L,
$ Schm_settls_L
integer Schm_itcn , Schm_modcn, Schm_xwvt3,
% Schm_itnlh, Schm_itraj, Schm_nith
real*8 Schm_nonhy_8
MARK_COMMON_BEG (schm_l)
common / schm_l /
$ Schm_hydro_L, Schm_cptop_L, Schm_moist_L, Schm_nkbz_L ,
$ Schm_phyms_L, Schm_adcub_L, Schm_difqp_L, Schm_psadj_L,
$ Schm_hdlast_L,Schm_wload_L, Schm_pcsty_L, Schm_chems_L,
$ Schm_pheat_L, Schm_theoc_L ,Schm_sfix_L, Schm_offline_L,
$ Schm_settls_L
MARK_COMMON_END (schm_l)
*
MARK_COMMON_BEG (schm_i)
common / schm_i / Schm_itcn , Schm_modcn, Schm_xwvt3,
% Schm_itnlh, Schm_itraj, Schm_nith
MARK_COMMON_END (schm_i)
*
MARK_COMMON_BEG (schm_r8)
common / schm_r8/ Schm_nonhy_8
MARK_COMMON_END (schm_r8)