Traditional semi-implicit formulations of nonhydrostatic compressible
models may not be stable in the presence of steep terrain when pressur
e gradient terms are split and lagged in time. If all pressure gradien
t terms and the divergence are treated implicitly, the resulting wave
equation for the pressure contains off-diagonal cross-derivative terms
leading to a highly nonsymmetric linear system of equations. In this
paper we present a more implicit formulation of the Mesoscale Compress
ible Community (MC2) model employing a Generalized Minimal Residual (G
MRES) Krylov iterative solver and a more efficient semi-Lagrangian adv
ection scheme. Open boundaries now permit exact upwind interpolation a
nd the ability to reproduce simulations to machine precision is illust
rated for one-way nesting at equivalent resolution. Numerical simulati
ons of hydrostatic and nonhydrostatic mountain waves demonstrate the s
tability and accuracy of the new adiabatic kernel. The computational e
fficiency of the model is reported for ID Jacobi and 3D Alternating Di
rection Implicit (ADI) line relaxation preconditioners implemented wit
h a parallel data transposition strategy.