NAM_BU_RSV

NAM_BU_RSV content

Fortran name	Fortran type	Default value
LBU_RSV	LOGICAL	.FALSE.
CBULIST_RSV	CHARACTER(LEN=128)(:)

• LBU_RSV : flag to activate budget for scalar variable

• CBULIST_RSV : list of source terms

Note

Description of the names to be used for the different source terms in the CBULIST_RSV array and the conditions of their availability:

General source terms

Name	Description	Condition(s)
ALL	all available source terms (separated, water microphysics included)	no condition
ASSE	time filter (Asselin)	CUVW_ADV_SCHEME(1:3)=’CEN’ and CTEMP_SCHEME=’LEFR’
NEST	nesting	NMODEL>1
VISC	viscosity	LVISC=T and LVISC_SV=T
ADV	total advection	no condition
FRC	forcing	LFORCING=T
DIF	numerical diffusion	LNUMDIFSV=T
REL	relaxation	LHORELAX_SV(jsv)=T or corresponding LHOREAX_SV*=T or (CELEC/=’NONE’ and LRELAX2FW_ION=T and (jsv=NSV_ELECBEG or jsv=NSV_ELECEND) )
DCONV	KAFR convection	CDCONV=’KAFR’ or CSCONV=’KAFR’
HTURB	horizontal turbulent diffusion	CTURB=’TKEL’ and CTURBDIM=’3DIM’
VTURB	vertical turbulent diffusion	CTURB=’TKEL’
MAFL	mass flux	CSCONV=’EDKF’
NEGA2	negativity correction	no condition

with jsv the scalar variable number.

C2R2 / KHKO source terms

• Common source terms for C2R2 / KHKO :

Name	Description	Condition(s)
NETUR	negativity correction induced by turbulence	CTURB=’TKEL’
NEADV	negativity correction induced by advection	no condition
NEGA	negativity correction	no condition
NECON	negativity correction induced by condensation	no condition

• Concentration of activated nuclei for C2R2 / KHKO :

Name	Description	Condition(s)
HENU	CCN activation	LSUPSAT=F or (CACTCCN=’ABRK’ and (LORILAM=T or LDUST=T or LSALT=T))
CEVA	evaporation	no condition

• Concentration of cloud droplets for C2R2 / KHKO :

Name	Description	Condition(s)
DEPOTR	tree droplet deposition	LDRAGTREE=T and LDEPOTREE=T
HENU	CCN activation	LSUPSAT=F or (CACTCCN=’ABRK’ and (LORILAM=T or LDUST=T or LSALT=T))
SELF	self-collection of cloud droplets	NMOM_R>=1
ACCR	accretion of cloud droplets	NMOM_R>=1
SEDI	sedimentation	LSEDC=T
DEPO	surface droplet deposition	LDEPOC=T
CEVA	evaporation	no condition

• Concentration of raindrops for C2R2 / KHKO :

Name	Description	Condition(s)
AUTO	autoconversion into rain	NMOM_R>=1
SCBU	self collection - coalescence/break-up	CCLOUD/=’KHKO’
REVA	rain evaporation	NMOM_R>=1
BRKU	spontaneous break-up	NMOM_R>=1
SEDI	sedimentation	no condition

• Supersaturation for C2R2 / KHKO :

Name	Description	Condition(s)
CEVA	evaporation	no condition

LIMA source terms

• Common source terms for LIMA :

Name	Description	Condition(s)
NETUR	negativity correction induced by turbulence	CTURB=’TKEL’
NEADV	negativity correction induced by advection	no condition
NEGA	negativity correction	no condition
NECON	negativity correction induced by condensation	no condition

• Concentration of cloud droplets for LIMA :

Name	Description	Condition(s)
DEPOTR	tree droplet deposition	LDRAGTREE=T and LDEPOTREE=T
SEDI	sedimentation of cloud	NMOM_C>=1 and LSEDC=T
DEPO	surface droplet deposition	NMOM_C>=1 and LDEPOC=T
R2C1	rain to cloud change after sedimentation	LPTSPLIT=T and NMOM_C>=1 and NMOM_R>=1
HENU	CCN activation	NMOM_C>=1 and LACTI=T and NMOD_CCN>0 and (LPTSPLIT=F or LSUBG_COND=F)
HINC	heterogeneous nucleation by contact	NMOM_I>=1 and LNUCL=T
SELF	self-collection of cloud droplets	LPTSPLIT=T or (NMOM_C>=1 and NMOM_R>=1)
AUTO	autoconversion into rain	LPTSPLIT=T or (NMOM_C>=1 and NMOM_R>=1)
ACCR	accretion of cloud droplets	LPTSPLIT=T or (NMOM_C>=1 and NMOM_R>=1)
REVA	evaporation of rain drops	LPTSPLIT=T or (NMOM_C>=1 and NMOM_R>=1)
HONC	droplet homogeneous freezing	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and LNUCL=T)
IMLT	melting of ice	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1)
RIM	riming of cloud water	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
WETG	wet growth of graupel	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
DRYG	dry growth of graupel	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
CVRC	rain to cloud change after other microphysical processes	LPTSPLIT=T
WETH	wet growth of hail	LPTSPLIT=T or NMOM_H>=1
CEDS	adjustment to saturation	NMOM_C>=1
CORR2	supplementary correction inside LIMA splitting	LPTSPLIT=T

• Concentration of raindrops for LIMA :

Name	Description	Condition(s)
SEDI	sedimentation	NMOM_C>=1 and NMOM_R>=1
R2C1	rain to cloud change after sedimentation	LPTSPLIT=T and NMOM_C>=1 and NMOM_R>=1
AUTO	autoconversion into rain	LPTSPLIT=T or (NMOM_C>=1 and NMOM_R>=1)
SCBU	self collection - coalescence/break-up	LPTSPLIT=T or (NMOM_C>=1 and NMOM_R>=1)
REVA	rain evaporation	LPTSPLIT=T or (NMOM_C>=1 and NMOM_R>=1)
BRKU	spontaneous break-up	LPTSPLIT=T or (NMOM_C>=1 and NMOM_R>=1)
HONR	rain homogeneous freezing	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_R>=1 and LNUCL=T)
ACC	accretion of rain on aggregates	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1 and NMOM_R>=1)
CFRZ	conversion freezing of rain	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
WETG	wet growth of graupel	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
DRYG	dry growth of graupel	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
GMLT	graupel melting	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
CVRC	rain to cloud change after other microphysical processes	LPTSPLIT=T
WETH	wet growth of hail	LPTSPLIT=T or NMOM_H>=1
HMLT	melting of hail	LPTSPLIT=T or NMOM_H>=1
CORR2	supplementary correction inside LIMA splitting	LPTSPLIT=T

• Concentration of free CCN for LIMA :

Name	Description	Condition(s)
HENU	CCN activation	NMOM_C>=1 and LACTI=T and NMOD_CCN>0 and (LPTSPLIT=F or LSUBG_COND=F)
HONH	haze homogeneous nucleation	NMOM_I>=1 and LNUCL=T and LHHONI=T and NMOD_CCN>0
CEDS	adjustment to saturation	NMOM_C>=1
SCAV	scavenging	LSCAV=T

• Concentration of activated CCN for LIMA :

Name	Description	Condition(s)
HENU	CCN activation	NMOM_C>=1 and LACTI=T and NMOD_CCN>0 and (LPTSPLIT=F or LSUBG_COND=F)
HINC	heterogeneous nucleation by contact	NMOM_I>=1 and LNUCL=T and LMEYERS=F
CEDS	adjustment to saturation	NMOM_C>=1

• Scavenged mass variable for LIMA :

Name	Description	Condition(s)
SCAV	scavenging	LSCAV=T and LAERO_MASS=T
CEDS	adjustment to saturation	LSCAV=T and LAERO_MASS=T and LSPRO=F

• Concentration of pristine ice crystals for LIMA :

Name	Description	Condition(s)
SEDI	sedimentation	NMOM_I>=1 and LSEDI=T
HIND	heterogeneous nucleation by deposition	NMOM_I>=1 and LNUCL=T
HINC	heterogeneous nucleation by contact	NMOM_I>=1 and LNUCL=T
HONH	haze homogeneous nucleation	NMOM_I>=1 and LNUCL=T and LHHONI=T and NMOD_CCN>0
HONC	droplet homogeneous freezing	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and LNUCL=T)
CNVI	conversion of snow to cloud ice	LPTSPLIT=T or (NMOM_I>=1 and NMOM_S>=1)
CNVS	conversion of pristine ice to snow	LPTSPLIT=T or (NMOM_I>=1 and NMOM_S>=1)
AGGS	aggregation of snow	LPTSPLIT=T or (NMOM_I>=1 and NMOM_S>=1)
IMLT	melting of ice	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1)
HMS	Hallett-Mossop ice multiplication process due to snow riming	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
CIBU	ice multiplication process due to ice collisional breakup	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1 and LCIBU=T)
CFRZ	conversion freezing of rain	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
RDSF	ice multiplication process following rain contact freezing	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1 and LRDSF=T)
WETG	wet growth of graupel	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
DRYG	dry growth of graupel	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
HMG	Hallett-Mossop ice multiplication process due to graupel riming	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)
WETH	wet growth of hail	LPTSPLIT=T or NMOM_H>=1
CEDS	adjustment to saturation	LPTSPLIT=F and LSPRO=F
CORR2	supplementary correction inside LIMA splitting	LPTSPLIT=T

• Concentration of snow for LIMA :

Name	Description	Condition(s)
SEDI	sedimentation	NMOM_S>=2
CNVI	conversion of snow to cloud ice	NMOM_S>=2
CNVS	conversion of pristine ice to snow	NMOM_S>=2
BRKU	break up of snow	NMOM_S>=2
RIM	heavy riming of cloud droplet on snow	NMOM_S>=2
ACC	accretion of rain on snow	NMOM_S>=2
CMEL	conversion melting of snow	NMOM_S>=2
WETG	wet growth of graupel	NMOM_S>=2
DRYG	dry growth of graupel	NMOM_S>=2
WETH	wet growth of hail	NMOM_S>=2
SSC	snow self collection	NMOM_S>=2
CEDS	adjustment to saturation	LPTSPLIT=F and NMOM_I>=1 and LSPRO=F

• Concentration of graupel for LIMA :

Name	Description	Condition(s)
SEDI	sedimentation	NMOM_G>=2
RIM	heavy riming of cloud droplet on snow	NMOM_G>=2
ACC	accretion of rain on snow	NMOM_G>=2
CMEL	conversion melting of snow	NMOM_G>=2
CFRZ	conversion freezing of raindrop	NMOM_G>=2
WETG	wet growth of graupel	NMOM_G>=2
GMLT	raupel melting	NMOM_G>=2
WETH	wet growth of hail	NMOM_G>=2
COHG	conversion hail graupel	NMOM_G>=2
CEDS	adjustment to saturation	LPTSPLIT=F and NMOM_I>=1 and LSPRO=F

• Concentration of hail for LIMA :

Name	Description	Condition(s)
SEDI	sedimentation	NMOM_H>=2
WETG	wet growth of graupel	NMOM_H>=2
COHG	conversion hail graupel	NMOM_H>=2
HMLT	hail melting	NMOM_H>=2

• Concentration of free IFN for LIMA :

Name	Description	Condition(s)
HIND	heterogeneous nucleation by deposition	NMOM_I>=1 and LNUCL=T and LMEYERS=F
CEDS	adjustment to saturation	NMOM_I>=1 and LPTSPLIT=F and LSPRO=F
SCAV	scavenging	LSCAV=T

• Concentration of nucleated IFN for LIMA :

Name	Description	Condition(s)
HIND	heterogeneous nucleation by deposition	NMOM_I>=1 and LNUCL=T and (LMEYERS=F or jsv=NSV_LIMA_IFN_NUCL)
HINC	heterogeneous nucleation by contact	NMOM_I>=1 and LNUCL=T and LMEYERS=T and jsv=NSV_LIMA_IFN_NUCL
IMLT	melting of ice	LPTSPLIT=T or (NMOM_I>=1 and NMOM_C>=1)
CEDS	adjustment to saturation	NMOM_I>=1 and LPTSPLIT=F and LSPRO=F

with jsv the scalar variable number.

• Concentration of nucleated IMM for LIMA :

Name	Description	Condition(s)
HINC	heterogeneous nucleation by contact	NMOM_I>=1 and LNUCL=T and LMEYERS=F
CEDS	adjustment to saturation	NMOM_I>=1 and LPTSPLIT=F and LSPRO=F

• Homogeneous freezing of CCN for LIMA :

Name	Description	Condition(s)
HONH	haze homogeneous nucleation	NMOM_I>=1 and LNUCL=T and ( (LHHONI=T and NMOD_CCN>0) or (LPTSPLIT=F and NMOM_C>=1) )

• Supersaturation for LIMA :

Name	Description	Condition(s)
CEDS	adjustment to saturation	no condition

Electricity source terms

• Common source terms for electricity :

Name	Description	Condition(s)
NETUR	negativity correction induced by turbulence	CTURB=’TKEL’
NEADV	negativity correction induced by advection	no condition
NEGA	negativity correction	no condition
NECON	negativity correction induced by condensation	no condition

• Positive ions :

Name	Description	Condition(s)
DRIFT	ion drift motion	no condition
CORAY	cosmic ray source	no condition
ADJU	adjustement to saturation	CCLOUD(1:3)=’ICE’ and LRED=T and LADJ_BEFORE
DEPS	deposition on snow	no condition
DEPG	deposition on graupel	no condition
REVA	rain evaporation	NMOM_C>=1
DEPI	condensation/deposition on ice	CCLOUD(1:3)=’ICE’ and (LRED=F or LADJ_AFTER)
CEDS	adjustement to saturation	CCLOUD=’LIMA’
NEUT	neutralization	no condition
SUBI	sublimation of ice crystals	CCLOUD=’LIMA’ and LPTSPLIT=T
CORR2	supplementary correction inside LIMA splitting	CCLOUD=’LIMA’ and LPTSPLIT=T

• Volumetric charge of cloud droplets :

Name	Description	Condition(s)
ADJU	adjustement to saturation	CCLOUD(1:3)=’ICE’ and LRED=T and LADJ_BEFORE
HON	homogeneous nucleation	no condition
AUTO	autoconversion into rain	NMOM_C>=1
ACCR	accretion of cloud droplets	NMOM_C>=1
RIM	riming of cloud water	no condition
WETG	wet growth of graupel	no condition
DRYG	dry growth of graupel	no condition
INCG	inductive charge transfer between cloud droplets and graupel	LINDUCTIVE=T
WETH	wet growth of hail	CCLOUD=’ICE4’
IMLT	melting of ice	no condition
BERFI	Bergeron-Findeisen	no condition
SEDI	sedimentation	LSEDIC=T
DEPI	condensation/deposition on ice	CCLOUD(1:3)=’ICE’ and (LRED=F or LADJ_AFTER)
CEDS	adjustement to saturation	CCLOUD=’LIMA’
NEUT	neutralization	no condition
R2C1	rain to cloud change after sedimentation	CCLOUD=’LIMA’ and LPTSPLIT=T and NMOM_C>=1 NMOM_R>=1
CORR2	supplementary correction inside LIMA splitting	CCLOUD=’LIMA’ and LPTSPLIT=T
CMEL	collection by snow and conversion into rain with T>XTT on ice	CCLOUD(1:3)=’ICE’ and LRED=T

• Volumetric charge of rain drops :

Name	Description	Condition(s)
SFR	spontaneous freezing	no condition
AUTO	autoconversion into rain	NMOM_C>=1
ACCR	accretion of cloud droplets	NMOM_C>=1
REVA	rain evaporation	NMOM_C>=1
ACC	accretion of rain on aggregates	no condition
CFRZ	conversion freezing of rain	no condition
WETG	wet growth of graupel	no condition
DRYG	dry growth of graupel	no condition
GMLT	graupel melting	no condition
WETH	wet growth of hail	CCLOUD=’ICE4’
HMLT	melting of hail	CCLOUD=’ICE4’
SEDI	sedimentation	no condition
NEUT	neutralization	no condition
R2C1	rain to cloud change after sedimentation	CCLOUD=’LIMA’ and LPTSPLIT=T and NMOM_C>=1 NMOM_R>=1
CORR2	supplementary correction inside LIMA splitting	CCLOUD=’LIMA’ and LPTSPLIT=T
CMEL	collection by snow and conversion into rain with T>XTT on ice	CCLOUD(1:3)=’ICE’ and LRED=T
RDSF	raindrop shattering by freezing	CCLOUD=’LIMA’ and LPTSPLIT=T and LRDSF=T

• Volumetric charge of ice crystals :

Name	Description	Condition(s)
ADJU	adjustement to saturation	CCLOUD(1:3)=’ICE’ and LRED=T and LADJ_BEFORE
HON	homogeneous nucleation	no condition
AGGS	aggregation of snow	no condition
AUTS	autoconversion of ice	no condition
CFRZ	conversion freezing of rain	no condition
WETG	wet growth of graupel	no condition
DRYG	dry growth of graupel	no condition
WETH	wet growth of hail	CCLOUD=’ICE4’
IMLT	melting of ice	no condition
BERFI	Bergeron-Findeisen	no condition
NIIS	non-inductive charge separation due to ice-snow collisions	no condition
NIIG	non-inductive charge separation due to ice-graupel collisions	no condition
SEDI	sedimentation	no condition
DEPI	condensation/deposition on ice	CCLOUD(1:3)=’ICE’ and (LRED=F or LADJ_AFTER)
CEDS	adjustement to saturation	CCLOUD=’LIMA’
NEUT	neutralization	no condition
CNVI	conversion of snow to cloud ice	CCLOUD=’LIMA’ and LPTSPLIT=T
SUBI	sublimation of ice crystals	CCLOUD=’LIMA’ and LPTSPLIT=T
HMS	Hallett-Mossop ice multiplication process due to snow riming	CCLOUD=’LIMA’ and LPTSPLIT=T
HMG	Hallett-Mossop ice multiplication process due to graupel riming	CCLOUD=’LIMA’ and LPTSPLIT=T
CIBU	collisional ice breakup	CCLOUD=’LIMA’ and LPTSPLIT=T and LCIBU=T
RDSF	raindrop shattering by freezing	CCLOUD=’LIMA’ and LPTSPLIT=T and LRDSF=T
CORR2	supplementary correction inside LIMA splitting	CCLOUD=’LIMA’ and LPTSPLIT=T

• Volumetric charge of snow :

Name	Description	Condition(s)
DEPS	deposition on snow	no condition
AGGS	aggregation of snow	no condition
AUTS	autoconversion of ice	no condition
RIM	riming of cloud water	no condition
ACC	accretion of rain on snow	no condition
CMEL	conversion melting	no condition
WETG	wet growth of graupel	no condition
DRYG	dry growth of graupel	no condition
NIIS	non-inductive charge separation due to ice-snow collisions	no condition
NISG	non-inductive charge separation due to snow-graupel collisions	no condition
WETH	wet growth of hail	CCLOUD=’ICE4’
SEDI	sedimentation	no condition
CNVI	conversion of snow to cloud ice	CCLOUD=’LIMA’ and LPTSPLIT=T
HMS	Hallett-Mossop ice multiplication process due to snow riming	CCLOUD=’LIMA’ and LPTSPLIT=T
CIBU	collisional ice breakup	CCLOUD=’LIMA’ and LPTSPLIT=T and LCIBU=T
NEUT	neutralization	no condition

• Volumetric charge of graupel :

Name	Description	Condition(s)
SFR	spontaneous freezing	no condition
DEPG	deposition on graupel	no condition
RIM	riming of cloud water	no condition
ACC	accretion of rain on graupel	no condition
CMEL	conversion melting	no condition
CFRZ	conversion freezing of rain	no condition
WETG	wet growth of graupel	no condition
DRYG	dry growth of graupel	no condition
INCG	inductive charge transfer between cloud droplets and graupel	LINDUCTIVE=T
NIIG	non-inductive charge separation due to ice-graupel collisions	no condition
NISG	non-inductive charge separation due to snow-graupel collisions	no condition
GMLT	graupel melting	no condition
WETH	wet growth of hail	CCLOUD=’ICE4’
SEDI	sedimentation	no condition
HMG	Hallett-Mossop ice multiplication process due to graupel riming	CCLOUD=’LIMA’ and LPTSPLIT=T
NEUT	neutralization	no condition

• Negative ions :

Name	Description	Condition(s)
DRIFT	ion drift motion	no condition
CORAY	cosmic ray source	no condition
ADJU	adjustement to saturation	CCLOUD(1:3)=’ICE’ and LRED=T and LADJ_BEFORE
DEPS	deposition on snow	no condition
DEPG	deposition on graupel	no condition
REVA	rain evaporation	NMOM_C>=1
DEPI	condensation/deposition on ice	CCLOUD(1:3)=’ICE’ and (LRED=F or LADJ_AFTER)
CEDS	adjustement to saturation	CCLOUD=’LIMA’
NEUT	neutralization	no condition
SUBI	sublimation of ice crystals	CCLOUD=’LIMA’ and LPTSPLIT=T
CORR2	supplementary correction inside LIMA splitting	CCLOUD=’LIMA’ and LPTSPLIT=T

Chemistry

Name	Description	Condition(s)
CHEM	chemistry activity	no condition
NEGA	negativity correction	no condition

Chemical aerosols

Name	Description	Condition(s)
NEGA	negativity correction	no condition

Blowing snow

Name	Description	Condition(s)
SNSUB	blowing snow sublimation	LBLOWSNOW=T and LSNOWSUBL=T
SNSED	blowing snow sedimentation	LBLOWSNOW=T