Abstract

Double convection in rotating horizontal layers filled by a Navier–Stokes fluid mixture, heated and salted from below, is investigated. Onset of linear instability – for any value of the fluid and salt Prandtl numbers Pr, P1 – either via the Routh–Hurwitz conditions or via steady or oscillatory convection, is characterized. Introducing a new field connecting the perturbation fields to the temperature and salt concentration, in the cases P1=1 or Pr=1 or P1Pr=1, stability conditions in algebraic closed form are obtained. Linear stability is recovered as non-linear global asymptotic stability via the Auxiliary System Method.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call