Centrifugal buoyancy forces in a container rotating about an axis aligned w
ith gravity lead to mean flows that interact with rotating convection. A mo
del of the interactions between these flows and the thermal instabilities t
hat occur in weakly nonlinear rapidly rotating convection is used to estima
te when, in terms of external parameters, centrifugal buoyancy has a substa
ntial influence on thermal convective instability. The significant physical
effects include the direct action of centrifugal buoyancy on the eddies th
emselves, the upwards advection of basic-state vertical shear by the pertur
bation rolls, and the alteration of the mean thermal stratification upon wh
ich eddies grow by the basic centrifugally induced circulation. It is shown
that the first effect is the most important for common laboratory settings
, and can lead to destabilization of the system at outer radii. Other manif
estations of centrifugal buoyancy include the generation of a positive offs
et of the mean temperature at the centre of the cell, and a reduction of th
is offset by heat fluxes arising from the centrifugally modified finite-amp
litude convective eddies.