Abstract
The three-dimensional stability of two-dimensional natural convection flows in a heated, square enclosure inclined to the horizontal is investigated numerically. First, the computational procedure is validated by comparison of base flow solutions to results reported in literature across a range of inclinations. A bi-global linear stability analysis is then conducted to investigate the stability of these two-dimensional base flows to infinitesimal three-dimensional perturbations, and the effect that buoyancy forces (defined by a buoyancy number RN) and enclosure inclination θ have on these stability characteristics. The flow is first observed to become three-dimensionally unstable at buoyancy number RN = 213.8 when θ is 180◦; this increases to RN = 2.54 × 104 at inclination θ = 58◦. It is found that the two-dimensional base flow is more unstable to three-dimensional perturbations with the critical RN corresponding to three-dimensional instability being significantly lower than its two-dimensional counterpart across all considered inclinations except 83◦ ≤ θ ≤ 88◦, where the most unstable mode is a two-dimensional oscillatory mode that develops in the boundary layers along the conducting walls. Eight different leading three-dimensional instability modes are identified, with inclinations 58◦ ≤ θ < 88◦ transitioning through an oscillatory mode, and inclinations 88◦ ≤ θ ≤ 180◦ transitioning through a stationary mode. The characteristics of the primary instability modes corresponding to inclinations 88◦ ≤ θ ≤ 179◦ indicate the presence of a Taylor-Görtler instability.
Original language | English |
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Article number | A8 |
Number of pages | 31 |
Journal | Journal of Fluid Mechanics |
Volume | 1003 |
DOIs | |
Publication status | Published - 13 Jan 2025 |
Keywords
- baroclinic flows
- buoyancy-driven instability
- convection in cavities