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Jean-Marcel Piriou Centre National de Recherches Météorologiques Groupe de Modélisation pour l’Assimilation et la Prévision. Update on model developments: Meteo-France NWP model / clouds and turbulence. CLOUDNET Workshop / Utrecht 21-22/10/2002. Global ARPEGE Aquaplanet mode. - PowerPoint PPT Presentation
Update on model developments: Meteo-France Update on model developments: Meteo-France NWP model / clouds and turbulenceNWP model / clouds and turbulenceUpdate on model developments: Meteo-France Update on model developments: Meteo-France NWP model / clouds and turbulenceNWP model / clouds and turbulence
CLOUDNET Workshop / Utrecht 21-22/10/2002
Jean-Marcel PiriouCentre National de Recherches MétéorologiquesGroupe de Modélisation pour l’Assimilation et la Prévision
PHYSICS
Global ARPEGEAquaplanet mode
SCM ARPEGE (EUROCS, GATE, TOGA,BOMEX, ARM, …)
LAM ALADIN / coupled / 10 km
Global stretched ARPEGE / 4DVAR-ass. / 20 to 200 km
Global regular ARPEGE / 4DVAR-ass. / 66 km
Present operational schemes
Under progress
Radiation Geleyn and Hollingsworth (1979), Ritter and Geleyn (1992)
More accurate infra-red exchanges between surface and layers
Grid-scale cloud scheme
Diagnostic in ql/i, all supersaturation removed, liquid/ice condensation T, melting/ freezing/ evaporation/ Kessler (1979), Clough and Franks (1991)
Prognostic ql/i, qr/s
Subgrid-scale cloud scheme (convection)
mass-flux scheme, CISK-type closure and triggering, water
vapour budget using a Kuo-type closure, downdrafts, momentum flux
Modified trigger functions (TKE, CIN)
Turbulence 1st order closure scheme after Louis (1979), Louis and al. (1981), using a flux-gradient K-theory with Ri dependency, variable roughness lengths over sea (Charnock)
PrognosticTKE scheme, mixing « Betts » conservative variables thetal and qt instead of theta and qv
Perspectives operational modelPerspectives operational model ( (GCM 20-200km GCM 20-200km
ARPEGEARPEGE + + LAMLAM 10km 10km ALADINALADIN))
• March towards new prognostic cloud and turbulence March towards new prognostic cloud and turbulence
variables: ql/i, qr/s, TKE, w_ud, w_ddvariables: ql/i, qr/s, TKE, w_ud, w_dd
• EUROCS: 3 transition cases (well posed lateral conditions EUROCS: 3 transition cases (well posed lateral conditions
to compare CRMs to GCMs or LAMs)to compare CRMs to GCMs or LAMs)
• Model to satellite, data assimilation cycleModel to satellite, data assimilation cycle
• CLOUDNET: (long time series, detailed profiles) colocated CLOUDNET: (long time series, detailed profiles) colocated
ql/i, qr/s, PBL depth, cloudiness, close TEMP data to ql/i, qr/s, PBL depth, cloudiness, close TEMP data to
provide in-situ validation of new microphysics / turbulenceprovide in-situ validation of new microphysics / turbulence
Perspectives 2: a CRM in operations around 2008!...Perspectives 2: a CRM in operations around 2008!...
• 2003: first tests of the existing CRM méso-NH2003: first tests of the existing CRM méso-NH physics in physics in
the the ALADIN-NH ALADIN-NH 2.5km2.5km dynamical core dynamical core need for need for
validations within CLOUDNET?validations within CLOUDNET?