2004
DOI: 10.1063/1.1637603
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The motion of a vortex near a gap in a wall

Abstract: Two models are presented for the motion of a vortex near a gap in an infinitely long straight barrier: a problem of geophysical significance. The first model considers a line vortex for which the trajectories are obtained analytically and are generalized to include simple ambient flows. The criterion determining whether in the absence of background flow a vortex originating far from the gap passes through or leaps across the gap is derived. The second model considers a finite area patch of constant vorticity a… Show more

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Cited by 32 publications
(42 citation statements)
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“…8 Idealised models which assume two-dimensional flow of an inviscid fluid have been used to construct the Hamiltonian, or Kirchhoff-Routh path function, 9 for a single point vortex near a gap, in an infinitely long and infinitesimally thin straight barrier in the rigid lid case (i.e., infinite Rossby radius). 10 The main result is that vortices that start far upstream of the gap at greater than half the gap width from the barrier leap across the gap. Vortices far upstream starting closer to the barrier pass through the gap.…”
Section: Introductionmentioning
confidence: 99%
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“…8 Idealised models which assume two-dimensional flow of an inviscid fluid have been used to construct the Hamiltonian, or Kirchhoff-Routh path function, 9 for a single point vortex near a gap, in an infinitely long and infinitesimally thin straight barrier in the rigid lid case (i.e., infinite Rossby radius). 10 The main result is that vortices that start far upstream of the gap at greater than half the gap width from the barrier leap across the gap. Vortices far upstream starting closer to the barrier pass through the gap.…”
Section: Introductionmentioning
confidence: 99%
“…It is an iterative method based on perturbing about the exact solution for the infinite Rossby radius case. 10 …”
Section: Appendix: Alternative Form Of the Integral Equation And Its mentioning
confidence: 99%
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“…This formulation has been used by Johnson & McDonald 4,5 who modelled vortex patches as point vortices in order to investigate the paths of ocean vortex patches in the vicinity of boundaries such as islands or coastal gaps. However, with the exception of a few contour dynamics calculations (e.g.…”
Section: Introductionmentioning
confidence: 99%