The Regional Atmospheric Modeling System (RAMS) is a multi-purpose modeling
system that has been used to simulate drizzle production in marine
stratocumulus [Feingold et al., 1996a; Stevens et al., 1998]
and Arctic boundary-layer stratus [Olsson et al., 1998;
Harrington et al., 1999]. In this investigation RAMS is set up as a
non-hydrostatic LES model combined with an explicit microphysics model
[Feingold et al., 1994]. The predicted variables include the three
velocity components (u, v, w), the Exner function (
), the
ice-liquid water potential temperature (
)
[Tripoli and
Cotton, 1981], and total water mixing ratio rt on a vertically stretched
Arakawa C-grid.