It is well known that buoyancy forces and centrifugal effects can render a
flow unstable to longitudinal vortex structures. Such competing instability
mechanisms can be found in flows such as the curved mixing layer formed by
the passage of two streams of fluid at different temperatures in the wake
of a curved body. Via an asymptotic consideration of the problem we are abl
e to characterize the interplay between these mechanisms. We are also able
to determine the level of convex curvature required to stabilize unstably s
tratified mixing layers and the level of concave curvature required to dest
abilize stably stratified mixing layers. (C) 1999 American Institute of Phy
sics. [S1070-6631(99)03806-4].