The name of a subdomain can have up to 10 characters

New subdomains with default setup :
CFPDOM         & NLAT & NLON & RLATN & RLATS  & RLONW   & RLONE
'REUNION05' & 61        & 141       & -5.         & -35.        & 30.             & 100.
'OCINDIEN'    & 67        & 89         & 33.         & -66.         & 0.               & 132.

LFPOLE option : removed

Additive variables are at disposal to control the climatology usage :
RFPCSAB : Critical sand percentage difference between source and model climatology for computing relative soil moisture in ISBA ; default is 0.01
RFPCD2 : Critical soil depth difference between source and model climatology for computing relative soil moisture in ISBA ; default is 0.001
LFPMOIS : Month allowed for climatology usage :
    .FALSE. => month of the model (forecast)
     .TRUE. => month of the initial file
Default is .FALSE. ; it is recommended to set LFPMOIS=.TRUE. to enable in-line post-processing

Ozone, cloud fraction and upper air water related variables :
For ozone, cloud fraction, specific humidity, liquid water or ice, it is possible to consider the post-processed fields either as gridpoint or as spectral coefficients,independantly of the state of the model variable (so it is a way to convert these fields from spectral to gridpoint or vice versa) :
LFPGPQ  : .TRUE. to compute gridpoint humidity rather than spectral ; default = LECMWF
LFPGPL  : .TRUE. to compute gridpoint liquid water rather than spectral ; default =.TRUE.
LFPGPI  : .TRUE. to compute gridpoint ice rather than spectral ; default =.TRUE.
LFPGPA  : .TRUE. to compute gridpoint cloud fraction rather than spectral ; default =.TRUE.
LFPGPO3 : .TRUE. to compute gridpoint ozone rather than spectral ; default = LECMWF
These variables are in the namelist NAMFPC.

Adiabatic post-processing :
To run the post-processing in the adiabatic model, you should (not ask for physical fields and) carefully remove the physical fields from the model, by setting the following variables in namelists :
/NAMPHY
        LSOLV=.FALSE.,
        LFGEL=.FALSE.,
        LFGELS=.FALSE.,
        LMPHYS=.FALSE.,
        LNEBN=.FALSE.,
        LREASUR=.TRUE.,
/END
/NAMDPHY
        NVSO=0,
        NVCLIV=0,
        NVRS=0,
        NVSF=0,
        NVSG=0,
        NCSV=0,
        NVCLIN=0,
        NVCLIP=0,
/END
Notice : for technical reasons, it is important to keep LREASUR=.TRUE.

NFPXFLD namelist parameter :is still valid in the distributed memory code ;
the specificity is just that the "extraction" process consists in inter-processors communications.

NFPROMA namelist parameter : has been renamed NFPROMAG

Packing/unpacking :
In the Distributed Memory code, the packing/unpacking of the global fields can be distributed : in namelist NAMPAR1 :

NSTRIN : number of processors used for unpacking ; the best performances are obtained when this variable is set like the total number of processors used in the model (NPROC).
NSTROUT : number of processors used for packing ;  the best performances are obtained for an intermediate value (roughly NPROC/2).

Extension zone for Aladin :
Once you have requested the extension zone, you may set the variable of the namelist NAMFPEZO :
NSTREFP : number of processors used to compute the extension zone ; default is 1 (increasing this parameter seems not to bring benefits).
NFPROMEL : Vector length in the computation of the extension zone ; default is odd and is the maximum possible value.
Notice : the computation of the extension zone is possible only with Aladin library.

Customized complexion of certain fields :
LFPRH100 : .TRUE. to convert relative humidity in percent ; default = LECMWF
LFPLOSP  : is a variable to handle surface pressure (Ps) or its logarithm, taking also into account the value of NLOSP :
    LFPLOSP =.TRUE. =>
        Fill Ps array with Ps or Ln(Ps), according to NLOSP ;
        Fill Ln(Ps) array always with Ln(Ps)
    LFPLOSP =FALSE. =>
        Fill Ps array always with Ps ;
        Fill Ln(Ps) array with Ps or Ln(Ps), according to NLOSP
If (LECMWF) then the default value is .FALSE. ; Else, the default value is .TRUE. except for the configuration 927 where
it is set internally.
These variables are in the namelist NAMFPC.
 

There is a new (and post-processable) surface field in historical file : 'SURFRESERV.GLACE',

BOGUSSING :
It is possible to translate a cyclone inside an Aladin file. This procedure will translate the cyclone to a geographical point given in namelist. The following variables should be set in the namelist NAMFPG :
NFPTTYP : set NFPTTYP=2 to activate the translation if the output grid is not global
FPMUCEN : In Aladin : sine of the latitude of the observed cyclone ; default value is sin(ELAT0)
FPLOCEN : In Aladin : longitude of the observed cyclone (in degrees) ; default value is ELON0
Notice : to define the translation vector, the cyclone seen by the model is located through the minimum of surface pressure in the whole model area (C+I).
Usually, this procedure is used to re-build the upper-air fields of an historical file Aladin (using the configuration EE927 in adiabatic mode). In order not to translate the orography, one should first lower the orography to zero, then translate, and finally re-set the original orography.
It is possible to "inject" data out of Aladin post-processing inside a file Arpege : this is called "the bogussing configuration", or
 "the configuration 927E" because it works like the configuration E927 but in a "reverse" way.
To use this configuration, you should use a namelist of configuration 927, but invoking "aladin" instead "arpifs", and set in namelist NAMFPC the new variable NFPINCR=1 (default value is 0). Furthermore, you have to provide 3 input files instead of one :
ICMSH${CNMEXP(1:4)}INIT : Aladin bogussed coupling file
ELSCF${CNMEXP(1:4)}ALBC : Aladin coupling file (before bogussing)
BGPX${CNMEXP(1:4)}${CFPDOM} : Arpege background file
Notice : the Arpege background file should contain all the fields of a normal historical file in gridpoint. Furthermore : in this file surface pressure should be the true surface pressure and not its logarithm.
Important notice : for the time being, this configuration "927E" works only in adiabatic mode (i.e. : it is not yet possible to inject physical surface fields except orography).

New 3D dynamic field available in post-processing :
ozone mixing ratio : name = CNO3MX  ; default value ='OZONE' ; number of bits for packing = N(B/S)O3MX

New surface dynamic field available in post-processing :
Log. of surface pressure : name = CNLNSP ; default value = 'LOG.SURF.PRESS ' ; number of bits for packing = N(B/S)LNSP

New physical surface fields available in post-processing :
Frozen superficial soil wetness : name = CNFSSW ; default value = 'SURFRESERV.GLACE' ;
number of bits for packing = NBFSSW
Frozen deep soil wetness           : name = CNFDSW ; default value = 'PROFRESERV.GLACE' ;
number of bits for packing = NBFDSW

New cumulated fluxes available in post-processing :
Surface downward moon radiation  : name = CNCSMR ; default value = 'SURFRAYT.LUNE.DE' ;
number of bits for packing =NBCSMR

BEWARE of cloudiness CNXC='SURFCUMUL NEBUL ' :
This is the cloudiness out of the subroutine "Araneb", at the level the closest to 550 hPa !

Redundant fields to be removed from post-processing very soon :
U at bottom level                                : CNXUBL='SURFU NIVBAS'
V at bottom level                                : CNXVBL='SURFV NIVBAS'
Temperature at bottom level              : CNXTBL ='SURFT NIVBAS'
Specific humidity at bottom level      : CNXQBL='SURFQ NIVBAS'
Geopotential at bottom level              : CNXGBL='SURFGEOP NIVBAS'
Surface temperature                            : CNXST='SURFTEMPE SURF'
Deep Soil temperature                        : CNXDT='SURFTEMPE PROF'
Surface Water content                        : CNXSW='SURFRESER SURF'
Deep Soil Water content                     : CNXDW='SURFRESER PROF'
Snow mass                                           : CNXSNS='SURFNEIGE'

NAMDYN :
This namelist contains variables related to the dynamics of the model, that may be useful for the post-processing :
NLOSP : To use surface pressure or its logarithm as the primitive variable
NDLNPR : special discretization of delta(Log(P)) for non-hydrostatism.