2018
DOI: 10.1017/jfm.2018.374
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‘Unforced’ Navier–Stokes solutions derived from convection in a curved channel

Abstract: Steady Boussinesq flow in a weakly curved channel driven by a horizontal temperature gradient is considered. Linear variation in the transverse direction is assumed so that the problem reduces to a system of ordinary differential equations. A series expansion in $G$, a parameter proportional to the Grashof number and the square root of the curvature, reveals a real singularity and anticipates hysteresis. Numerical solutions are found using path continuation and the bifurcation diagrams for different parameter … Show more

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Cited by 3 publications
(2 citation statements)
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“…Guided by our experience with flows linear in a transverse coordinate [11,12], we now investigate whether or not this solution is unique. The technique we use is to add a fictitious forcing term αF(η) to one or more of our equations and to find the solution as the continuation parameter α varies.…”
Section: Numerical Methods and Path-continuationmentioning
confidence: 99%
See 1 more Smart Citation
“…Guided by our experience with flows linear in a transverse coordinate [11,12], we now investigate whether or not this solution is unique. The technique we use is to add a fictitious forcing term αF(η) to one or more of our equations and to find the solution as the continuation parameter α varies.…”
Section: Numerical Methods and Path-continuationmentioning
confidence: 99%
“…These are readily solved numerically in §4, giving rise to a typical boundary layer profile. Drawing on experience with other flows linear in one coordinate [11,12], we use path-continuation techniques to locate a second solution, with a more elaborate structure. Solving a time-dependent problem in §5 reveals that the second of these solutions is unstable.…”
Section: Introductionmentioning
confidence: 99%