ModelInvestigatorGridLevelsDynamicsConvection Scheme Lateral Boundary ConditionReference
RSM-NCEPHongPS28HYDGrellEXP/10 Jung et al. [1997]
RSM-ScrippsRoads, ChenMER28HYDA-SEXP/10 Juang and Kanamitsu [1994]
MM5LapentaLC32NONGrellLIN/4 Grell et al. [1993], Lakhtakia and Warner[1994]
MM5-ANLTaylorLC23NONGrellLIN/4 Grell et al. [1993], Lakhtakia and Warner[1994]
RegCM2PanLC14HYDGrellEXP/10 Giorgi et al. [1993a,b], Giorgi et al. [1996]
DARLAMMcGregor, KatzfeyPS18HYDModified A-SEXP/9 McGregor et al. [1993], McGregor and Walsh [1994]
HIRHAM4Christensen, LopezMER19HYDMFEXP/10 Christensen et al. [1997]
ClimRAMSListon, PielkePS20NONK-APAR/10 Pielke et al. [1992]
CRCM Caya, Laprise PS20NONKFDIF/9 Caya and Laprise [1999]
EMLuthi AC20HYDMFDIF/9 Luthi et al. [1996]
PROMESGaetner LC26HYDKFLIN/8 Gaertner et al. [2001]
SweCLIMJones RLL19HYDKFTANH/8 Jones and Willen [2001]
Dynamics;HYD, hydrostatic; NON, nonhydrostatic. Horizontal grid types; MER, Mercator (latitude-longitude); RLL, Rotated Latitude-Longitude; PS, polar stereographic; LC, Lambert conformal. Convection scheme; AS, Arakawa and Schubert [1974]; Grell [1993] and Grell et al. [1993]; MF, mass flux scheme following Tiedtke [1989]; KF, Kain-Fritsch Kain [1990]; CA, convective adjustment; KA, Kuo [1974]. Lateral BC: weighting function used blending large-scale and internal tendencies (LIN, linear decrease toward center of domain; EXP, exponential decrease; PAR, parabolic decrease; DIF, dynamical diffusion following Davies (1976); TANH, hyperbolic tangent profiles) and number of grid points in the blending region.

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