|
MATCH Aerosol Transport Model |
|
OUTINST, OUTTIMAV = 'ALL'
CALC_ADV_FLUX bug
CONVTRAN on by default in params.h
precision_mode in GNUmakefileETDOTR vertical velocity in eta coord before correctionMCA Mass convergence aboveMCAR Mass convergence above before correctionO3INT integrated ozone in Dobson unitsnf90 instead of nf conventions, requires atleast netcdf3.5
syscall, fileUtils.Fcldprp() which
has the effect of a trigger function.Q (specific humidity) to be initialized from the same file as
the other trace species. By default Q is initialized from the input
meteorology.useAltConv=.true..nhtfrq=0.fixmas=.true..Q in the X, Y, and
Z directions. This option is turned on by adding "#define
CALC_ADV_FLUX" to the params.h configuration file.msread and mswrite (except in the NCEP GRIB
reader). Set up reads from the NCAR MSS to use msrcp via issuing
system commands. Set up writes to the NCAR MSS to use the perl
script rdsp.cmfadj() in archived convection mode.QRELAX is provided to nudge Q towards the input
meteorology, but by default this option is off.Q due to total precip.ncaru library installed.fmalloc.c for SGI compilation with -64 option.oro, phis,
and sflx from plon to plond
for consistency with the CCM.filtedot. The default is on.esice so that the option to either account for an
ice phase or not in the saturation water vapor calcs can be turned on
or off without code modification. The default is to account for an ice
phase (esice=.true.).limqin to enable the limiting of the input Q
field to have a maximum value equal to the saturation Q. By default
limqin=.false..Q field to have a minimum value
of 2.e-12. shneg so that it doesn't issue messages when it fixes the Q field
after adjusting it in vdiff().physlic() or in
routines called by physlic()).INCORE in the params.h file. In large memory machines, the
incore version can result in a substantially more efficient
execution.| - |