2001
DOI: 10.5194/npg-8-301-2001
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Cyclostrophic vortices in polar regions of rotating planets

Abstract: Abstract. Multi-petal, rotating vortices can form in twodimensional flows consisting of an inviscid incompressible fluid under certain conditions. Such vortices are principally nonlinear thermo-hydrodynamical structures. The proper rotation of these structures which leads to time-dependent variations of the associated temperature field can be enregistred by a stationary observer. The problem is analyzed in the framework of the contour dynamics method (CDM). An analytical solution of the reduced equation for a … Show more

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Cited by 6 publications
(5 citation statements)
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References 27 publications
(25 reference statements)
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“…In the case of intense vortices λ ∼ 1, a cyclostrophic rather than geostrophic balance can take place. Solutions for localized cyclostrophic vortices are shown in [32], [75], [66], [68].…”
Section: Resultsmentioning
confidence: 99%
“…In the case of intense vortices λ ∼ 1, a cyclostrophic rather than geostrophic balance can take place. Solutions for localized cyclostrophic vortices are shown in [32], [75], [66], [68].…”
Section: Resultsmentioning
confidence: 99%
“…which says that for any specific ξ, ratio κ/ω is uniquely defined. Figure 3 plots Equation (26). For the presented model, the temperature excess τ follows from Equation ( 20) and Equation (23):…”
Section: Resultsmentioning
confidence: 99%
“…Within this framework-called the contour dynamics method (CDM) (see Refs. [18,[22][23][24][25][26][27])-the distribution of vorticity q for a vortex structure may be written as q = q 0 Θ(x, y). Function Θ(x, y) is a two-dimensional Heaviside step-function equal to one inside the domain in consideration and zero outside.…”
Section: Resultsmentioning
confidence: 99%
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