NAM_BU_RRI

NAM_BU_RRI content

Fortran name

Fortran type

Default value

LBU_RRI

LOGICAL

.FALSE.

CBULIST_RRI

ARRAY(CHARACTER)

  • LBU_RRI : flag to activate budget for non-precipitating ice

  • CBULIST_RRI : list of source terms

Note

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

Source terms (except water microphysical schemes)

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_R=T

ADV

total advection

no condition

FRC

forcing

LFORCING=T

DIF

numerical diffusion

LNUMDIFTH=T

REL

relaxation

LHORELAX_RI=T

DCONV

KAFR convection

CDCONV=’KAFR’ or CSCONV=’KAFR’

HTURB

horizontal turbulent diffusion

CTURB=’TKEL’ and CTURBDIM=’3DIM’

VTURB

vertical turbulent diffusion

CTURB=’TKEL’

LIMA source terms

Name

Description

Condition(s)

SEDI

sedimentation of cloud

NMOM_I>=1 and LSEDI=T

HIN

heterogeneous ice nucleation

NMOM_I=1

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)

BERFI

Bergeron-Findeisen

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)

HMG

Hallett-Mossop ice multiplication process due to graupel 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)

DEPI

condensation/deposition on ice

LPTSPLIT=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)

WETH

wet growth of hail

LPTSPLIT=T or (NMOM_H>=1 and NMOM_I>=1 and NMOM_C>=1 and NMOM_S>=1)

CEDS

adjustment to saturation

no condition

NEGA

negativity correction

no condition

NETUR

negativity correction induced by turbulence

CTURB=’TKEL’

NEADV

negativity correction induced by advection

no condition

NECON

negativity correction induced by condensation

no condition

CORR2

supplementary correction inside LIMA splitting

LPTSPLIT=T

ICE3 / ICE4 source terms

Name

Description

Condition(s)

SEDI

sedimentation of cloud

no condition

HIN

heterogeneous ice nucleation

no condition

HON

homogeneous nucleation

no condition

AGGS

aggregation of snow

no condition

AUTS

autoconversion of ice

no condition

IMLT

melting of ice

no condition

BERFI

Bergeron-Findeisen

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’

DRYH

dry growth of hail

CCLOUD=’ICE4’ and LRED=T and CELEC=’NONE’

DEPI

condensation/deposition on ice

LRED=F or ( LRED=T and LADJ_AFTER=T) or CELEC/=’NONE’

CORR

correction

LRED=T and CELEC/=’ELE3’

ADJU

adjustment to saturation

LRED=T and LADJ_BEFORE=T and CELEC/=’ELE3’

NEGA

negativity correction

no condition

NETUR

negativity correction induced by turbulence

CTURB=’TKEL’

NEADV

negativity correction induced by advection

no condition

NECON

negativity correction induced by condensation

no condition