1995
DOI: 10.1063/1.868470
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Dynamics of a nonlinear dipole vortex

Abstract: A localized stationary dipole solution to the Euler equations with a relationship between the vorticity and streamfunction given as w=-++ @ is presented. By numerical integration of the Euler equations this dipole is shown to be unstable. However, the initially unstable dipole reorganizes itself into a new nonlinear -dipole, which is found to be stable. This new structure has a functional relationship given as o=c$+~@-y@. Such dipoles are stable to head-on collisions and they are capable of creating tripolar s… Show more

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Cited by 32 publications
(23 citation statements)
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“…The former consists of an anticyclonic core with two cyclonic satellites, while the latter is a dipole with a reduced global Rossby number, because of larger distance between the two vorticity cores, and essentially nonlinear scatter plot of B versus PV (cf. Hesthaven et al 1995). Recently, we have presented similar results for shock-modons with Ro = 0.4 (transonic one-layer AGM with a hydraulic jump) whose collisions lead to formation of a shock-tripole (Lahaye & Zeitlin 2012).…”
Section: Preliminary Discussion Of the Adjustment Experimentssupporting
confidence: 56%
See 1 more Smart Citation
“…The former consists of an anticyclonic core with two cyclonic satellites, while the latter is a dipole with a reduced global Rossby number, because of larger distance between the two vorticity cores, and essentially nonlinear scatter plot of B versus PV (cf. Hesthaven et al 1995). Recently, we have presented similar results for shock-modons with Ro = 0.4 (transonic one-layer AGM with a hydraulic jump) whose collisions lead to formation of a shock-tripole (Lahaye & Zeitlin 2012).…”
Section: Preliminary Discussion Of the Adjustment Experimentssupporting
confidence: 56%
“…This structure is coherent, as is clear from the scatter plot. As for its known bidimensional counterpart, it has a strongly nonlinear shape, which is the origin of the name (Hesthaven et al 1995;Kizner & Khvoles 2004b). …”
Section: Agm → Agm + Nagm Collisionmentioning
confidence: 96%
“…This solution was suggested about a century ago and has been widely used in various studies. Dipolar vortices in geophysical flows, however, are often slightly compressed in the direction of translation which has been confirmed by laboratory experiments [3,4] and numerical simulations [5,6]. For that reason, in more recent theoretical studies [7,8], the concept of Lamb and Chaplygin was generalized for barotropic f -and β-plane dipoles with elliptical separatrices.…”
Section: Introductionmentioning
confidence: 85%
“…Both are known in the context of 2D Euler equations 6,7 and, by extension, are expected in the QG equation. Yet, we observe them in full "compressible" RSW simulations, starting from definitely ageostrophic initial conditions.…”
Section: Agm Fi T Collisionsmentioning
confidence: 96%