Transition from convective to absolute instability in Rayleigh–Bénard
convection in
the presence of a uni-directional Poiseuille flow is studied. The evaluation
of the long-time behaviour of the Green function in the horizontal plane allows the
determination
of regions of convective and absolute instability in the Rayleigh–Reynolds
number
plane as a function of Prandtl number. It is found that the mode reaching
zero
group velocity at the convective–absolute transition always corresponds
to transverse
rolls, while the system remains convectively unstable with respect to pure
streamwise
(longitudinal) rolls for all non-zero Reynolds numbers. Finally, the roll
pattern within
the entire wave packet and in particular near its centre is elucidated
and possible
connections between experiments and our findings are discussed.
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