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Participants Institute  SCM email
Martin Kohler + Pier Siebesma ECMWF ECMWF new scheme Martin.Koehler@ecmwf.int
Jean-Yves Grandpeix LMD LMD Jean-Yves.Grandpeix@lmd.jussieu.fr
Sylvain Cheinet + Joao Teixeira LMD CT01 Sylvain.Cheinet@lmd.jussieu.fr
Isabelle Beau + Pascal Marquet Meteo-France METEO-FRANCE ARPEGE Climate pascal.marquet@meteo.fr
Jean-Marcel Piriou Meteo-France METEO-FRANCE ARPEGE NWP Jean-Marcel.Piriou@meteo.fr
Geert Lenderink KNMI RACMO/ECHAM lenderin@knmi.nl
Andreas Chlond + Frank Muller  Max-Planck, Hamburg ECHAM4/5 frank.mueller@dkrz.de
Enrique Sanchez + Joan Cuxart INM HIRLAM e.sanchez@inm.es
Pedro Soares University of Lisbon Meso-NH psoares@fc.ul.pt

 
 
SCM Turbulence  Massflux  Cloud Scheme 
ECMWF
 
 

 

K-profile, mixing theta, qv, u, v, dry formulation stability, implicit entrainment (parcels) Tiedke bulk massflux, entrainment and detrainment coeff equal/prescriped. 
Cl. base MF: convergence moist static energy
prognostic cloud scheme (cloud fraction (c.f.), liq water) , 
c.f. dependent on detrainment, BL turbulence, and stratiform condensation.
LMD 
 
 

 

Louis-type, mixing theta, qv (??), u, v. moist formulation stability Ri/linear in c.f., no top entrainment Emanuel multiple mass flux, entr/detr dynamical dep. on CAPE/ buoyancy sorting,
Cl. base MF: buoyancy parcel LFC (- 40 hPa) + CAPE.
Statist. cloudscheme dep. on qt,  progn. equation ql/qi, Sundqvist precipitation/evaporation.
ARPEGE
 
 
 

 


1.5 order TKE scheme (previously Louis-type, more recently 2nd order Mellor-Yamada). Mixing in: qv, dry static energy (Cp*T+g*z), u and v.Moist formulation for stability, depending on Q1 (norm. sat. deficit, Bougeault 82).
No top PBL entrainment (next Grenier)
Bougeault bulk mass flux,  prescribed entrainment/detrainment  function of height.
Cl. base MF: convergence moist static energy
Statist. cloudscheme stratiform + deep convective cloud amount. No progn equation ql/qi
RACMO/
ECHAM

 

 

TKE-l, mixing qv, ql, dry static energy, u, v. Moist stability linear in c.f., l based on N^2, implicit  entrainment Tiedke bulk massflux, entrainment and detrainment coeff not equal and prescriped. 
Cl. base MF: wstar closure.
Cloud fraction (statist.) dependent on qt. Variance qt dep. on mass flux, prognost. equa. ql/qi, large scale condensation/evap Sundqvist
ECHAM
 
 

 

TKE-l, mixing qv, ql, dry static energy, u, v. Moist stability linear in c.f., l based on Ri, implicit entrainment Tiedke bulk massflux, entrainment and detrainment coeff equal/prescriped. 
Cl. base MF: moisture convergence
Cloud fraction  dependent on relative humidity. prognost. equa. ql/qi, 
large scale condensation/evap Sundqvist
HIRLAM TKE-l Bulk Mass flux ??
Meso-NH 1.5 order TKE-l scheme. Lengthscale parcel method (B&L). Mixing in
theta, qv (??), u, v. Moist formulation stability. Stability function defined by Redelsperger and Sommeria (1981). 
Bougeault bulk mass flux,  entrainment and detrainment according Kain & Fritsch (1990). 
Closure: prescribed dependent on deep or shalloe convection
Statistical cloud scheme for cloud fraction. Prognostic equations for cloud liquid water / ice.